THE ROCKIES AND PACIFIC COAST.

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XXI.

THE ROCKIES AND PACIFIC COAST.

The Lone Star State—The Sunset Route—Port Arthur—Galveston—Houston—Dallas—Fort Worth—Great Staked Plain—Austin—San Antonio—The Alamo—David Crockett—James Bowie—Sam Houston—Cattle Ranches—Rio Grande River—El Paso—Arizona—Tucson—Phoenix—Prehistoric Cities—Yuma—Canyons of the Colorado—Colorado Desert—Southern California—San Bernardino Valley—San Diego—Coronado Beach—The Early Missions—Climate and Scenery—Los Angeles—Santa Monica Bay—San Gabriel Valley—Santa Barbara—Monterey Bay—Del Monte—Santa Cruz—Santa Clara Valley—San JosÉ—Lick Observatory—San Joaquin Valley—Stockton—Gold Mining—The Big Trees—Yosemite Valley—Rocky Mountains—The Atchison Route—Indian Territory—Oklahoma—Raton Pass—Las Vegas—Santa FÉ—Albuquerque—Mesa Encantada—Flagstaff—Mojave Desert—The Union Pacific Route—Cheyenne—Colorado—Denver—Boulder Canyon—Clear Creek Canyon—Colorado Springs—Pike's Peak—Manitou—Garden of the Gods—Pueblo—Veta Pass—Cripple Creek—Leadville—Grand Canyon of the Arkansas—Marshall Pass—Black Canyon of the Gunnison—Wyoming Fossils—Utah—Echo and Weber Canyons—Ogden—Great Salt Lake—Salt Lake City—The Mormons—Promontory Point—Nevada—Virginia City—Comstock Lode—Lake Tahoe—Donner Lake—Sacramento—The Northern Pacific Route—Butte—Anaconda Mine—Helena—Idaho—Spokane—Columbia River—Oregon—Snake River Canyon—ShoshonÉ Falls—The Dalles—Cascade Locks—The Great Northern Route—The Canadian Pacific Route—Regina—Moose Jaw—Medicine Hat—Calgary—Banff—Mount Stephen—Kicking Horse Pass—Rogers Pass—Mount Sir Donald—Glacier House—Eagle Pass—Great Shuswap Lake—Kamloops—Thompson Canyon—Fraser Canyon—Vancouver—Victoria—Gulf of Georgia—Alaska—Fort Wrangell—Sitka—Juneau—Treadwell Mine—Muir Glacier—Lynn Canal—Chilkoot and Chilkat—Skaguay and Dyea—The Yukon River—The Klondyke—St. Michaels—Cape Nome—Puget Sound—Port Townsend—Everett—Seattle—Tacoma—Mount Tacoma—Mount St. Helens—Portland—Crater Lake—Mount Shasta—Benicia—Mare Island—Oakland—University of California—Menlo Park—Leland Stanford, Jr., University—San Francisco—Point Lobos—The Golden Gate.

THE LONE STAR STATE.

Westward from the Mississippi River the "Sunset Route" to the Pacific leads across the sugar plantations of Louisiana. This Southern Pacific railway passes many bayous having luxuriant growth of bordering live oaks, magnolias and cypress, hung with festoons of Spanish moss, crosses the Atchafalaya River at Morgan City, and beyond, skirts along the picturesque and winding Bayou Teche in a region originally peopled by colonies of French Acadian refugees from Nova Scotia. Ultimately the route crosses Calcasieu River at Lake Charles, and thirty-eight miles beyond, goes over the Sabine River into the "Lone Star State" of Texas, the largest in the Union. The name of Texas comes from a tribe of Indians found there when La Salle made the first European settlement on the coast at Fort St. Louis on Lavaca River in 1685, but after the Spanish occupation in the eighteenth century the country was long known as the New Philippines, that being the official designation in their records. At the mouth of Sabine River is Sabine Lake, where Port Arthur has been established as a prosperous railway terminal, having access to the Gulf by a ship canal with terminating jetties, deepening the channel outlet to the sea. Farther along the coast is Galveston, the chief Texan seaport, built on the northeastern extremity of Galveston Island, which spreads for thirty miles in front of the spacious Galveston Bay, covering nearly five hundred miles surface. The entrance from the sea is obstructed by a bar through which the Government excavated at great expense a channel, flanked by stone jetties five miles long. It is a low-lying city with wide, straight streets, embowered in luxuriant tropical vegetation, while the equable winter temperature makes it a charming health-resort. A magnificent sea-beach spreads along the Gulf front of the island for many miles. Galveston, in September, 1900, was swept by a most terrific cyclone and tidal wave, destroying thousands of lives and a vast number of buildings.

Texas was a Province of Mexico, under Spanish and afterwards Mexican rule, and its many attractions in the early nineteenth century brought a large accession of colonists to the eastern portions from the adjacent parts of the United States. The Americans became so numerous that in 1830 the Mexican Congress prohibited further immigration, and the result was a revolt in 1835, the organization of a Provisional Government, a war which ended in the defeat of the Mexicans in the battle of San Jacinto in 1836, and the final independence of Texas. The people then sought annexation to the United States, but the State was not admitted until 1845, the Mexican War following. Two men of that time were prominent in Texas, Stephen F. Austin, who brought the first large colony from the United States settling on the Colorado and Brazos Rivers, and Sam Houston, who, after being Governor of Tennessee, migrated to Texas, led the revolt, commanded their army, and was made the first President of the independent State. The latter has his name preserved in the active city of Houston on Buffalo Bayou, a tributary of Galveston Bay, and about fifty miles northwest of Galveston. Houston is a busy railway centre, handling large amounts of cotton, sugar and timber, and is rapidly expanding, having sixty thousand people.

The Trinity River is the chief affluent of Galveston Bay, flowing down from Northern Texas, and having upon its banks another busy railway centre, Dallas, with fifty thousand people and an extensive trade. About thirty miles above, on Trinity River, is the old Indian frontier post of Fort Worth, now a town of forty thousand population and the headquarters of the cattle-raisers of Northern Texas. For many miles in all directions are the extensive cattle ranges, and to the north and west spreads the "Great Staked Plain," a vast plateau elevated nearly five thousand feet above the sea, covering some fifty thousand square miles, and being surrounded by a bordering escarpment of erosion to the lower levels, much resembling palisades. The stakes driven by the early Spaniards to mark their way are said to have given this plain its name, and it has now become an almost limitless cattle pasturage. When Austin's American colony settled on the Colorado River west of Houston, his name was given the town which was ultimately selected as the State Capital, where there are now twenty thousand people who look out upon the magnificent view of the Colorado Mountains. Here is the Texas State University with seven hundred and fifty students, and one of the finest State Capitols in the country, a splendid red granite structure, which was built by a syndicate in exchange for a grant of three million acres of land, the building occupying seven years in construction and costing $3,500,000. Two miles above the city an enormous dam seventy feet high encloses the waters of Colorado River for the water supply and manufacturing power, and thus makes Lake McDonald, twenty-five miles long. A heavy storm and flood in the spring of 1900 broke this dam and let out the lake, causing great loss of life and damage in the city.

Eighty miles southwest of Austin is the ancient city of San Antonio, known as the "cradle of Texas liberty," a Spanish town upon the San Antonio and San Pedro Rivers, small streams dividing it into irregular parts, the former receiving the latter and flowing into the Gulf at Espiritu Santo Bay. There are sixty thousand people in San Antonio, of many races, chiefly Americans, Mexicans and Germans, and it is a leading wool, cattle, horse, mule and cotton market. The Spaniards penetrated into this region in the latter part of the seventeenth century and established one of their usual joint religious-military posts among the Indians upon the plan of colonization then in vogue. The Presidio or military station was called San Antonio de Bexar, while during the early eighteenth century there were founded various religious Missions, the chief being by Franciscan monks, the Mission of San Antonio de Valero. There are four other Missions in and near the city, dating from that early period, their ancient buildings partly restored, but some of them also considerably in ruins. To the eastward of San Antonio River was built in a grove of the alamo or cottonwood trees in 1744 a low, strong, thick-walled church of adobÉ for the Franciscans, called from its surroundings the Alamo. When the Texans revolted, they held San Antonio as an outpost with a garrison of one hundred and forty-five men, commanded by Colonel James Bowie, the famous duellist and inventor of the "bowie knife," who was originally from Louisiana. Bowie fell ill of typhoid fever, and Colonel Travis took command. Among the garrison was the eccentric David Crockett of Tennessee, who had been a member of Congress, and joined them as a volunteer. General Santa Anna marched with a large Mexican army against them, arriving February 22, 1836, and the little garrison retired within the church of the Alamo, which they defended against four thousand Mexicans in a twelve days' siege. The final assault was made at daylight, March 6th, a lodgment was effected, and until nine o'clock a battle was fought from room to room within the church, a desperate hand-to-hand conflict at short range, and not ceasing until every Texan was killed; but this was not until two thousand three hundred Mexicans had fallen. Upon the memorial of this terrible contest, at the Texas State Capital, is the inscription: "ThermopylÆ had her messenger of defeat, but the Alamo had none." This butchery caused a thrill of horror throughout the United States. "Remember the Alamo" became the watchword of the Texans, much aid was sent them, and the succor, coming from the desire to avenge the massacre, contributed largely to their ability to defeat the Mexicans in the subsequent decisive battle on San Jacinto River, down near Galveston Bay, which was fought in April. The old Church of the Alamo, since restored, is preserved as a national monument on the spacious Alamo plaza. The name of Houston, the Texan leader, is given to Fort Sam Houston, the United States military post on a hill north of San Antonio. The old Alamo is the shrine of Texas; and as visitors stroll around the place they are weirdly told how the spirits of the departed heroes, Crockett, Bowie, Travis and others, when the storms rage at night about the ancient building, wander through the sacristy with the heavy measured tread of armed troopers. It was in the midst of a storm that the Mexicans broke through a barred window and thus gained entrance in the siege. On the southern border of San Antonio are the extensive Fair Grounds, where Roosevelt's Rough Riders, largely recruited from the neighboring Texan ranches, were organized for the Spanish War in 1898. The most extensive Texas cattle ranches are south and west of San Antonio, the largest of them, King's Ranch, near the Gulf to the southward, covering seven hundred thousand acres, and being stocked with three thousand brood mares and a hundred thousand cattle.

ARIZONA.

The railway from San Antonio goes westward across the cattle ranges to the Rio Pecos, flowing for eight hundred miles down from the Rockies in a region largely reclaimed by irrigation, and then falling into the Rio Grande del Norte, the national boundary between Texas and Mexico. This noble stream, the Spanish "Grand River of the North," comes out of Colorado and New Mexico, and is eighteen hundred miles long. The Southern Pacific Railway crosses the Pecos on a fine cantilever bridge three hundred and twenty-eight feet high, and reaches the Rio Grande a short distance beyond, following it up northwest and passing the Apache Mountains, where at Paisano it crosses the summit grade at five thousand and eight feet elevation, the highest pass on this route to the Pacific coast. It finally reaches El Paso on the upper Rio Grande, a town of twelve thousand people, having on the Mexican bank of the river, with a long wooden bridge between, the twin town of Juarez, or El Paso del Norte, the road over the bridge being the chief route of trade into Mexico. The original Spanish explorer, Juan de Onate, named this crossing "the Pass of the North" in 1598, and after long waiting it has finally developed into an active town in cattle raising and silver mining, and also a health-resort, its balmy atmosphere being most attractive. The muddy river by its periodic inundations has made a very fertile intervale, which has a population of sixty-five thousand, and here are seen picturesque Mexican figures, the men in peaked sombreros and scarlet zarapes, and the women with blue rebozas. Beyond, the route crosses the southwest corner of New Mexico and enters Arizona, passing amid the mountain ranges to Tucson, the chief town of the Territory, having six thousand people, a quaint and ancient Spanish settlement, which has considerable Mexican trade. It was originally an appanage to the old Spanish mission of St. Xavier, nine miles southward, and it now thrives on its cattle trade, mining and magnificent climate, being also the location of the Territorial University.

To the northwest, in the well-irrigated valley of Salt River, is Phoenix, the capital of Arizona, with fifteen thousand population, the irrigation systems having produced great fertility in the adjacent region. The Salt River is a tributary of the Gila, the latter flowing out westward to the Colorado. In these Arizona valleys have been disclosed the remains of several prehistoric cities, chiefly located on a broad and sloping plain beginning at the confluence of the Salt with the Gila, and stretching down to the Mexican boundary. At Casa Grande is a famous ruin of a prehistoric temple with enormous adobÉ walls, the Government having made a reservation for its protection. These people were worshippers of the sun, and there have been discovered the remains of many towns with large population, the Gila Valley for ninety square miles disclosing these ruins, which are relics of the Stone age. Irrigation canals made by these prehistoric people, the oldest in the world, are also found throughout the region. Extensive explorations of these ancient cities have been made, and several have been named, among them Los Acequias, Los Muertos and Los Animos, the last being the largest, and there being strong evidence that it was destroyed by an earthquake which killed many thousands of the inhabitants. The railway follows the Gila Valley westward to its confluence with the Colorado, and here at the California boundary is Yuma, another of the early Spanish missions to the Indians, situated just north of the Mexican border, the Yuma Indians still living on a reservation adjoining the Colorado, their name meaning "the sons of the river." This town has its tragic history, for in 1781 the Indians made a savage raid upon the mission, destroyed the buildings and massacred the missionary priests.

The Colorado and its tributaries drain nearly the whole of Arizona, and it is one of the most remarkable rivers in the world. Its head branches have their sources in Wyoming, Colorado and Utah, uniting in the latter State, flowing four hundred miles across Arizona and seventy miles into Mexico to discharge through a delta into the Gulf of California. The river and most of its tributaries in Arizona pass through canyons that are among the wonders of the world, exposing to view geological strata of all the formations in their regular places to the thickness of twenty-five thousand feet. At first, the Colorado flows out of Utah and south into Arizona for one hundred and eighty miles, passing through the Marble Canyon, so called from the limestone walls, nearly four thousand feet deep. It then turns westward by irregular course, flowing nearly two hundred and fifty miles through the Grand Canyon, the most stupendous in existence, and having at places six thousand feet depth and walls spreading at the surface five or six miles apart. These huge walls are terraced and carved into myriads of pinnacles and towers, often brilliantly colored, and far down in the bottom the river is seen like a silvery thread of foam. Major Powell, who first explored it in 1869, went through in a boat. He calls it "the most profound chasm known on the globe," and believes the river was running there before the mountains were formed, and that the canyon was made by the erosion of the water acting simultaneously with the slow upheaval of the rocks. The river has a rapid flow in the canyon, winding generally through a lower chasm and having a descent of five to twelve feet to the mile, sometimes with placid reaches, but frequently plunging down rapids filled with rocks. The surrounding country is largely volcanic, with lava-beds and extinct craters. When the visitor first approaches the brink of the great chasm, he is almost appalled with the sight. There seem to be scores of deep ravines and enclosed mountains, the main wall opposite being miles away, and the intervening space filled with peaks and ridges of every imaginable shape and color, rising from the abyss below. There is a trail down the side of the canyon, a steep and narrow path winding along the face of the Grand View Gorge, giving startling glimpses into ravines thousands of feet deep, and disclosing the massive magnificence of this enormous abyss. Down goes the trail, one gorge opening below another until the verge of the final gorge is reached, in which the river runs at a depth of a thousand feet farther. Everything is desolate, the vegetation sparse, and a few stunted trees appearing, while the river, which seemed from above to be only a far distant silvery streak down below, is expanded by the nearer view into large proportions. This Grand Canyon of the Colorado is one of the most wonderful constructions of nature in its stupendous size and extraordinary character; with the myriads of pinnacles, towers, castles, walls, chasms and profound depths it contains and the gorgeous coloring given most of the surfaces. It is among the greatest of the attractions that America, the land of wonders, presents to the seeker after the picturesque.

SOUTHERN CALIFORNIA.

Beyond the California boundary the Southern Pacific Railway traverses the broad Colorado desert. This is a barren, sandy wilderness, growing nothing but yuccas and cactus, and is depressed far below the sea-level. It is an inland salt-water lake that has mostly dried up, the belief being that it was formerly an extension of the Gulf of California. The railway route beyond passes between the San Jacinto and San Bernardino Mountains, crossing the latter. These peaks rise over eleven thousand feet, and beyond is the pleasant fruit-growing San Bernardino Valley, originally settled by the Mormons in 1851. To the southward is Riverside, in the fertile district where the seedless navel oranges are successfully cultivated, the groves giving an attractive exhibition of orange-growing. Here is the famous Magnolia Avenue, one hundred and thirty feet wide and ten miles long, with its double rows of pepper trees, and extending all the way through orange groves. In its park is one of the finest cacti collections in existence. Adjacent is Redlands, also a flourishing orange-growing city, its sidewalks bordered by stately palms, rose-bushes, pepper trees and century plants, while everywhere are orange trees in their perpetual livery of brilliant green. Around it encircle the high San Bernardino Mountains, thoroughly protecting the fertile valley. To the southward the route then runs out to the Pacific Ocean bound to Southern California, and following down the coast near San Juan passes Dana's Point, over which, in the early Californian days, the hides were thrown for shipment, as narrated by Dana in Two Years Before the Mast. Ultimately it reaches the grand bay of San Diego, near the Mexican boundary, which, next to San Francisco, is the best harbor on the Pacific coast.

Here, spreading along the shores of the beautiful bay, is the ancient Spanish town of San Diego, long sleepy, but lately enjoying a "boom" when it found itself becoming a popular watering-place. To the northward is the old Mission of San Diego, the first settlement by white men in California, noted for its prolific olive groves. In the town of adobÉ houses lived "Ramona" of whom Helen Hunt Jackson has written, and there are still preserved here the original church bells sent out from Spain to the colony. The outer arm of San Diego Bay is Coronado Beach, a narrow tongue of sand, stretching twelve miles northward, and ending in spacious expansions known as the North and South Beaches. Upon the South Beach is the famous watering-place of Coronado, with its great hotel alongside the ocean, the tower commanding an extensive view, and its spacious surrounding flower-gardens being magnificently brilliant. There are Botanical Gardens, a Museum and an interesting ostrich farm, with railways for miles along the pleasant shores, and at Point Loma are the lighthouses guarding the entrance from the sea, the uppermost, elevated five hundred feet, being the highest lighthouse in the world. Down near the Mexican boundary is the suburb of National City, surrounded by olive groves, and the visitors sometimes cross over the border to visit the curious Mexican village of Tia Juana, a name which being freely translated means "Aunt Jane." Extensive irrigation works serve the country around San Diego, and the great Sweetwater Dam, ninety feet high, closing a gorge, makes one of the largest water reservoirs in existence.

This wonderful land of California into which we have come has a name the meaning of which is unknown. One Ordonez de Montalva in 1510 published a Spanish romance wherein he referred to the "island of California, on the right hand of the Indies, very near the Terrestrial Paradise." When Cortez conquered Mexico, his annalist, Bernal Diaz del Castillo, gave this name, it is said in derision, about 1535, to the lower peninsula of California, then supposed to be an island, it having been discovered the previous year by the Spanish explorer Ximenes. The Jesuit missionaries came in the seventeenth century to the lower peninsula, and in the eighteenth century to California proper. It is an enormous State, stretching nearly eight hundred miles along the Pacific, and inland for a width of two hundred or more miles. It is mainly a valley, between the Coast Range of mountains on the west and the Sierra Nevada, meaning the "snowy saw-tooth mountains," on the east. The Sacramento and San Joaquin Rivers flow in the central valley, which stretches north and south for five hundred miles. To the southward the mountain ranges join, and below them is the special and favored region of Southern California. When first settled, there were established from San Diego up to Sonoma twenty-one Jesuit Missions, whose ruins and old buildings are now found so interesting, and these early establishments converted the Indians, of whom it is said that the charming climate offered them no inducements to develop savagery, so that when the conversion time came they were easily made serfs for the Missions, and worked in a way that few other Indians ever did. There are two California seasons, the rainy and the dry, the former lasting from November to May, while there is almost unchanging dry weather from May till October. The rainy season, however, is not as in the tropics, where there are deluges daily, but it means that then it will rain if ever, and there are in fact days without rain at all. California is a land of climatic attractiveness, where, as it has been well said, "it is always afternoon." Through vast irrigation systems, despite the dry season, much of the surface has been made a garden. Water runs everywhere copiously down from the mountains, and the shrubbery of all parts of the world has been brought hither and successfully grown. The region presents an universal landscape of foliage and flowers, luxuriant beyond imagination. In Southern California the wild flowers, of which the golden poppy is one of the most prominent, are extraordinary in their number, variety and brilliancy. "The greatest surprise of the traveller," writes Charles Dudley Warner, "is that a region which is in perpetual bloom and fruitage, where semi-tropical fruits mature in perfection, and the most delicate flowers dazzle the eye with color the winter through, should have on the whole a low temperature, a climate never enervating, and one requiring a dress of woollen in every month."

Cloister of Mission, San Juan Capistrano

LOS ANGELES AND SAN JOAQUIN.

The metropolis of this land of sunshine, fruits and flowers, fifteen miles back from the sea, is La Puebla de la Nuestra Senora la Reina de Los Angeles, or "the City of Our Lady, the Queen of the Angels;" a lengthy title which the matter-of-fact Americans some time ago happily shortened into Los Angeles. From it Los Angeles River flows south to the sea at San Pedro Bay. The Spaniards founded the town in 1781, but it had only a sleepy existence until 1880, when the railways came along, and it became a centre of the pleasure and health-resorts, and the extensive fruit growing of Southern California, expanding so rapidly that it has seventy thousand people. Originally, the houses were of adobÉ, but now it has many fine buildings and a magnificent development of residences, the whole city being embowered in luxuriant vegetation. In the neighborhood are petroleum wells and asphalt deposits, while the adjacent district has many irrigation canals. Down on the ocean shore is San Pedro, the port of Los Angeles, where the harbor has been improved by a large outlay, and twenty miles away is the beautiful mountainous island of Santa Catalina, a popular resort, which is in reality an ocean mountain top. Santa Monica Bay, to the southwest, is the coast bathing-place of Los Angeles, and near by is the popular Redondo Beach, with its spacious Chautauqua Assembly Building. Pasadena is a charming suburb of the city off to the northeast, a perpetual garden and favorite place of residence. It is in San Gabriel Valley, over which rises the great Sierra Madre Range, eleven thousand feet high, the glossy green orange groves on its sides gradually melting into the white snow-capped summits of this towering mountain wall. A railway ascends Echo Mountain north of Pasadena, on which is the Lowe Observatory. To the southeast is the old San Gabriel Mission in the valley, surrounded by vineyards and orchards.

San Buenaventura was another Mission, and is now a health-resort at the coast outlet of Ventura valley, and beyond is Santa Barbara, the "American Mentone," one of the most charming California resorts. The old Spanish Mission, with its towers and corridors, is famous, and was built in 1786, being well-preserved and having a few of the Franciscan monks yet in charge. A curiosity of the neighborhood is La Parra Grande, the "Great Vine," having a trunk four feet in diameter and covering a trellis sixty feet square, its annual product being eight thousand pounds of grapes. Farther along the coast is the charming Bay of Monterey, with the Spanish town of Monterey on its southern shore. In 1770 the Mission of San Carlo de Monterey was founded here, and it was the Mexican capital of California until the American conquest in 1846, then depending chiefly on a trade in tallow and hides. It has not grown much since, however, and the old adobÉ buildings have not undergone change in a half-century. It is now a popular resort, having the noted Hotel Del Monte, the "Hotel of the Forest," located in spacious and exquisite grounds, the park embracing seven thousand acres. Upon the northern side of Monterey Bay is Santa Cruz, its chief town, also a summer-resort, having a background made by the Santa Cruz Mountains. This was a Mission founded in 1791, and five miles northward is the Santa Cruz grove of big trees, containing a score of redwoods or sequoias, of a diameter of ten feet or more, the largest being twenty-three feet. Within a hollow in one of these trees General Fremont encamped for several days in 1847. To the northward is the prolific fruit region, the Santa Clara Valley, where Mission Santa Clara was founded in 1777. The city of this valley is San JosÉ, with twenty thousand people, distantly surrounded by mountains, and, like all these places, a popular resort. The Calaveras Mountains are to the eastward, and here, on Mount Hamilton, twenty-six miles southeast, is the Lick Observatory, at forty-two hundred feet elevation. It was founded by a legacy of $700,000 left by James Lick, of San Francisco, and is attached to the University of California, being among the leading observatories of the world. It has one of the largest and most powerful refracting telescopes in existence, the object-glass being thirty-six inches in diameter. Mr. Lick is buried in the foundation pier of this great telescope which he erected. There is a magnificent view from the Observatory, which is exceptionally well located, its white buildings, shining in the sunlight, seen from afar.

Across the Coast Range of mountains, eastward from San JosÉ, is the extensive San Joaquin Valley, noted as the "granary of California," two hundred miles long and thirty to seventy miles wide between the mountain ranges. It produces almost limitless crops of grain, fruits and wines. Through this great valley the San Joaquin River flows northward, and the Sacramento River southward in another valley as spacious, and uniting, they go out westward to San Francisco Bay. We are told that in the days when the earth was forming, the sea waves beat against the slopes of the Sierra Nevada, but ultimately the waters receded, leaving the floor of this vast valley of central California stretching nearly five hundred miles between the mountain ranges. The first comers among the white men dug gold out of its soils, but now they also get an enormous revenue from the prolific crops. Railways traverse it in all directions. The chief city is Stockton, at the head of navigation on the San Joaquin, a town of twenty thousand people, having numerous factories. Here in the slopes and gulches of the Sierras, stretching far away, were the first gold-mines of California, when the discoveries of the "Forty-niners" set the world agog. Here, at Jackson, was tapped the famous "Mother Lode," the most continuous and richest of the three gold belts extending along the slope of the Sierras, and so-called by the early miners because they regarded it as the parent source of all the gold found in the placers. This lode is in some parts a mile wide, and extends a hundred miles, being here a series of parallel fissures filled with gold-bearing quartz-veins, while farther south they unite in a single enormous fissure. The mineral belts paralleling it on both sides are rich in copper and gold. The country all about is a mining region with prolific "diggings" everywhere, and smokes arising from the stamp-mills at work reducing the ores. Here are Tuttletown and Jackass Hill, the home of "Truthful James," and the localities made familiar by Bret Harte and Mark Twain. Here is Carson Hill, there having been picked up on its summit the largest gold-nugget ever found in California, worth $47,000. What this gold-mining has meant is shown by the results, aggregating since California first produced the metal a total of nearly $1,350,000,000 gold given the world. As the San Joaquin Valley is ascended, it develops its wealth of grain-fields, orchards and vineyards, and displays the grand systems of irrigation which have contributed to produce so much fertility.

Eastward from San Joaquin Valley are the famous groves of Big Trees, the gigantic sequoias, which Emerson has appropriately called the "Plantations of God." There are two forests of giants in Calaveras and Mariposa Counties displaying these enormous trees, of which it is significantly said that some were growing when Christ was upon the earth. The Calaveras Grove, the northernmost, is at an elevation of forty-seven hundred feet above the sea, upon a tract about two-thirds of a mile long and two hundred feet wide, there being a hundred large trees and many smaller. The tallest tree standing is the "Keystone State," three hundred and twenty-five feet high and forty-five feet in circumference. The "Mother of the Forest," denuded of its bark, is three hundred and fifteen feet high and sixty-one feet girth, while the "Father of the Forest," the biggest of all, is prostrate, and measures one hundred and twelve feet in circumference. There are two trees three hundred feet high, and many exceeding two hundred and fifty feet, the bark sometimes being a foot and a half thick. This grove, however, being less convenient, is not so much visited as the Mariposa Grove to the southward. It is in Mariposa (the butterfly) County, at sixty-five hundred feet elevation, and near the Yosemite Valley. The tract of four square miles is a State Park, there being two distinct forests a half-mile apart. The lower grove has a hundred fine trees, the largest being the "Grizzly Giant," of ninety-four feet circumference and thirty-one feet diameter, the main limb, at two hundred feet elevation, being over six feet in diameter. The upper grove contains three hundred and sixty trees, and the road between the groves is tunnelled directly through one of them, which is twenty-seven feet in diameter. Through this living tree, named "Wawona," the stage-coach drives in a passage nearly ten feet wide. These trees are not so high as in Calaveras Grove, but they are usually of larger girth. The tallest is two hundred and seventy-two feet, ten exceed two hundred and fifty feet, and three are over ninety feet in circumference, while twenty are over sixty feet. Many of the finest have been marred by fires. There are eight groves of these Big Trees in California, these being the chief.

YOSEMITE VALLEY.

Into the San Joaquin flows Merced River, coming from the eastward down out of the Sierras through the famous Yosemite Valley. Most of its waters are diverted by irrigation canals leading for many miles over the floor of the broad San Joaquin Valley. The road to the Yosemite leads eastward up the slope, crosses the crest, and at Inspiration Point, fifty-six hundred feet elevation, gives the first view, then steeply descending to the river bank, it enters the western portal. Yosemite is a corruption of the Indian word "A-hom-e-tae," which means the "full-grown grizzly bear," and is supposed to have originally been the name of an Indian chief. This magnificent canyon, on the western slope of the Sierra Nevada, is a deep gorge eight miles long, traversed by Merced River, its nearly level floor being about thirty-eight hundred feet above the sea-level. The enclosing rocky and almost vertical walls rise from three thousand to five thousand feet above the river, the space between varying from a half-mile to two miles. Over the valley floor winds the beautiful green current of the diminutive Merced, bordered by trees and vegetation, the surface being generally grass-grown. The high vertical walls, the small amount of dÉbris at their foot, and the character of the Yosemite chasm itself, have led the geologists to ascribe its formation not to erosion or glacial action, but to a mighty convulsion in the granite rocks, whereby part of them subsided along lines of fault-crossing nearly at right-angles. The observer, standing on the floor, can see no outlet anywhere, the almost perpendicular walls towering on high in every direction.

The Valley is a Government Park, which also includes the watershed of the streams flowing into it. Originally it was the home of the Digger Indians, a tribe of ShoshonÉs, and a rather low type, of whom a few still survive. It was first seen by white men in 1851, when a detachment of troops pursuing these Indians came unexpectedly upon it. The attractions soon became widely known, and visitors were numerous, especially after the opening of the Pacific Railways. Entering the Valley, the most striking object is its northwestern buttress, the ponderous cliff El Capitan, rising thirty-three hundred feet, at a very narrow part, its majestic form dominating the view. There are two vertical mountain walls almost at right angles, these enormous bare precipices facing west and south. On the opposite side, forming the other portal, rise the imposing Cathedral Rocks, adjoined by the two slender Cathedral Spires of splintered granite, nearly three thousand feet high. Over these rocks on their western side pours the Bridal Veil Fall, about seventy feet wide, and descending vertically six hundred and thirty feet. As the winds often make the foaming column flutter like a white veil, its title has been appropriately given. Adjoining El Capitan descends the Ribbon Fall, or the Virgin's Tears, falling two thousand feet, but losing much of its waters as the summer advances. Eastward of El Capitan are the peaks called the Three Brothers, the highest also named the Eagle Peak, rising three thousand feet. To the eastward of this peak and in a recess near the centre of the Valley are the Yosemite Falls, one of the highest waterfalls in the world. Yosemite Creek, which comes over the brink with a breadth of thirty-five feet, descends twenty-five hundred feet in three leaps. It pours down a vertical wall, the Upper Fall descending nearly fifteen hundred feet without a break, the column of water swaying as the winds blow with marvellous grace of motion, the eddying mists fading into light summer clouds above. The Middle Fall is a series of cascades descending over six hundred feet, and the Lower Fall is four hundred feet high. This is one of the grandest features of the Valley, but its vigor, too, dwindles as the season advances. There is a high and splendid ice cone formed at the foot of the Upper Fall in the winter. Alongside, upon a projection called Yosemite Point, at over thirty-two hundred feet elevation, is given one of the best views of the famous Valley.

At the head of the Yosemite, it divides into three narrow tributary canyons, each discharging a stream, which uniting form the Merced. The northernmost is the Tenaya, and overshadowing it rises the huge North Dome, more than thirty-seven hundred feet high, having as an outlying spur the Washington Column. Opposite, and forming the eastern boundary of the valley, is the South or Half Dome, of singular shape, towering almost five thousand feet, and like El Capitan, at the other extremity, being a most remarkable granitic cliff. Its top is inaccessible, although once it was scaled by an adventurous explorer by means of a rope attached to pegs driven into the rock. It is one of the most extraordinarily formed mountains in existence, standing up tall, gaunt and almost square against the sky, the dominating pinnacle of the upper valley. Upon the southern side rises Glacier Point, nearly thirty-four hundred feet, giving a splendid view over the valley, having to the westward the Sentinel Dome, nearly forty-three hundred feet high, ending in the conspicuous face of the Sentinel Rock. Thus environed by vast cliffs, this grand valley displays magnificent scenery. Within the upper canyons are also attractions, that of the Merced River, the central gorge displaying the Vernal and Nevada waterfalls. The Vernal Fall is seventy feet wide and descends three hundred and fifty feet, having behind it the Cap of Liberty, a picturesque cliff. Farther up the river is the Nevada Fall, a superb cataract, having a slightly sloping descent of six hundred feet. Just within Tenaya Canyon is the Mirror Lake, remarkable for its wonderful reflections of the North and South Domes and adjacent mountains. Some distance to the eastward is the Cloud's Rest, a peak rising more than six thousand feet above the valley and nearly ten thousand feet above sea-level, that is ascended for its splendid view of the surrounding mountains and the enclosing walls of the valley, which can be plainly seen throughout its length, stretching far away towards the setting sun. This view of the Yosemite surpasses all others in its comprehensiveness and grandeur.

THE ROCKIES

The great "backbone" of the American Continent is the Rocky Mountains, and the summits of its main range make the parting of the waters, the "Continental Divide." Its name of the Rockies is appropriate, for on these mountains and their intervening plateaus, naked rocks are developed to an extent rarely equalled elsewhere in the world. The leading causes of this are the great elevation and extreme aridity, the scanty moisture preventing growth of vegetation, and the high altitudes promoting denudation of the rock-material disintegrated at the surface. Enormous crags and bold peaks of bare rocks, mostly compose the mountains, while the streams flow at the bases of towering precipices in deep chasms and canyons filled with broken rocks. Being unprotected by vegetation, the winds sweep the hills clean of soil and sand, the steep slopes of the valleys are strewn with fragments of the enclosing cliffs, and the rivers are usually without flood-plains or intervales, where soils may gather. In the extensive and highly-elevated plateaus, the streams usually run in the bottoms of deep canyons, their channels choked with dÉbris. Added to this the whole Rocky Mountain region has in the past been a scene of great volcanic activity, many extinct volcanoes appear, broad plains are covered with lava, and scoria and ashes are liberally deposited all about. The aridity is not a feature of the Pacific coast ranges, however, for the moisture from that ocean abundantly supplies water; there are good soils, and in the northern parts usually dense forests. The Rocky Mountain system extends from Mexico up to Alaska and the Arctic Ocean, its greatest development being between 38° and 42° north latitude, where the various ranges cover a breadth of a thousand miles. The highest peak of the Rockies is Mount Logan, in British America, on the edge of Alaska, rising nineteen thousand five hundred and thirty-nine feet. In the United States these mountains rise from a general plateau extending across the country, and reaching its maximum elevation of about ten thousand feet in Colorado, whilst towards the north the surface descends, entering Canada at an elevation of four thousand feet. The plateau descends westward into the basin of the Colorado River, then the surface rises in Nevada to six thousand feet, and thence farther westward it gradually descends to the base of the Sierra Nevada in California. To the eastward the plateau throughout steadily descends in the long, undulating and generally treeless slope of the Great Plains to the Mississippi, the many tributaries of the Father of Waters carving their valleys down through its surface. There are numerous mountain ranges, plateaus and parks, under different names in this extensive mountain region, and the higher peaks in the United States generally rise to thirteen to fifteen thousand feet elevation. These mountains and the plains to the eastward compose the vast arid region constituting fully two-fifths of the United States, where irrigation is necessary to agriculture, and, in consequence, less than ten per cent. of this large surface bears forests of any value. We are told that so scant is the moisture, if the whole current of every water-course in this district were utilized for irrigation it would not be possible to redeem four per cent. of the land. Some of this surface, however, bears grasses and plants that, to an extent, make pasturage. The precious metals and other useful minerals are found in abundance, and various parts of the region have been developed by the many valuable mines, making their owners enormous fortunes.

Through this vast mountain district, over deserts and along devious defiles, a half-dozen great railways lead from the Mississippi Valley to the Pacific slope. The Southern Pacific Railway we have already followed from New Orleans across to Southern California. Northward from its route at El Paso a railway leads through New Mexico to the next great transcontinental line, the Atchison system, coming from Chicago by way of Kansas City and Santa FÉ southwestward The main line traverses Kansas, and branches go south into the Indian Territory and Oklahoma. In the former are the reservations of the civilized tribes of Indians originally removed from east of the Mississippi—the Choctaws, Cherokees, Creeks, Chickasaws and Seminoles, with some others—who number nearly two hundred thousand souls, most of them engaged in agriculture. To the westward, south of Kansas and Colorado, is the "Boomers' Paradise" of Oklahoma, or the "Beautiful Land," a fertile and well-watered region, originally part of the Indian reserved lands, but bought from them by the Government. People from Kansas long had a desire to occupy this prolific land, and only with great difficulty were they kept out. The portion first got ready was opened to settlement by proclamation at noon on April 22, 1889, a large force of troops being in attendance to preserve order. Over fifty thousand people crossed the boundaries and entered the Territory the first day, taking up farms and starting towns. The "Cherokee Strip" along the northern line was subsequently obtained and opened to settlement in September, 1893, when ninety thousand people rushed in. These great invasions of the "Oklahoma boomers" became historic, cities of tents springing up in a night; but while there then was much suffering and privation from want of food and shelter, yet the new Territory has since become a most successful agricultural community.

The Atchison route, after crossing Kansas, enters Colorado, passing La Junta and Trinidad, and then turning southward rises to the highest point on the line, crossing the summit of the Raton Pass, at an elevation of seventy-six hundred and twenty feet, by going through a tunnel, and emerging on the southern side of the mountain in New Mexico. The railway is then laid along the slope of the Santa FÉ Mountains, and on their side are Las Vegas Hot Springs, about forty of them being in the group, their waters used both for bathing and drinking, and having various curative properties. The Glorieta Pass is subsequently crossed at seventy-five hundred feet elevation, and beyond is Santa FÉ, the capital of New Mexico. This is a curious and antique town, the oldest in the United States next to St. Augustine in Florida. It was an Indian pueblo or town in the very early times, and in 1605 the Spaniards came along, captured it, reduced the Indians to slavery, and worked the valuable gold and silver mines. In 1680 the Indians revolted, expelled the Spaniards and destroyed their churches and buildings, but they recovered control a few years later. There are now about seven thousand people of all races, having a good trade, and being chiefly employed in mining. It is a quaint old place, with crooked and narrow streets and adobÉ houses surrounding the central Plaza, on one side of which is the ancient Governor's Palace, a long, low adobÉ structure of one story, wherein the Governors of Spanish, Mexican and American rule have lived for nearly three centuries. It contains various historical paintings and relics, and here General Lew Wallace wrote Ben Hur while Governor of New Mexico in 1880.

Beyond Santa FÉ is the Rio Grande River, which the railway follows down through a grazing country past Albuquerque, its mart for wool and hides. Turning westward an arid region is traversed, with an occasional pueblo, and near Laguna is the famous Mesa Encantada, or the "Enchanted Table Land." This eminence rises precipitously four hundred and thirty feet above the surface, and is only accessible by ladders and ropes. The summit gives evidence of former aboriginal occupancy, and the tradition of the neighboring Acomas Indians is that their ancestors lived upon it, but were forced to abandon the village when a storm had destroyed the only trail and caused those remaining on the summit to perish. To the westward the "Continental Divide" is crossed at seventy-three hundred feet elevation, but with nothing indicating the change, as it is on a plateau. The Navajo Indian Reservation is crossed, Arizona entered and traversed, and at the Flagstaff Station is the Lowell Observatory, and here the nearest route is taken to the Grand Canyon of the Colorado. There rises to the northward the huge San Francisco Mountain, a fine extinct volcano, while off to the southwest are the great United Verde Copper Mines, among the largest in the world, and the town of Prescott, in a rich mineral region. The Colorado River is crossed into California, and then the railway traverses the wide Mojave Desert towards the Pacific coast.

DENVER AND ITS SURROUNDINGS

The Union Pacific Railway route across the Continent was the first constructed, the Government giving large subsidies in money and land grants. It was opened in 1869, and greatly encouraged travel to the Pacific coast. The Union Pacific main line starts at Council Bluffs and Omaha on the Missouri River and crosses Nebraska into Wyoming. Here is Cheyenne, a leading cattle-dealers' town on the edge of the Rockies, five hundred miles west of the Missouri, where there are fifteen thousand people. Fort Russell, an Indian outpost at the verge of the Black Hills, is to the northward. At Cheyenne, the main Union Pacific line is joined by the Denver Pacific branch, which starts on the Missouri River at Kansas City, traverses Kansas, passing Fort Riley and the Ogden Monument there, marking the geographical centre of the United States, and enters Colorado, and at Denver turns northward to Cheyenne.

Denver is the great city of the Rockies, whose snow-capped summits are seen to the westward in a magnificent and unbroken line, extending in view for one hundred and seventy miles from Pike's Peak north to Long's Peak, with many intervening summits, most of them rising over fourteen thousand feet. Denver stands on a high plateau, through which the South Platte River flows, and it is at nearly fifty-three hundred feet elevation. This "Queen City of the Plains" was settled by adventurous pioneers as a mining camp in 1858, and through the wonderful development of mining the precious metals has had rapid growth, so that now there is one hundred and seventy thousand population. It has many manufactures and some of the most extensive ore-smelting works in the world, the annual output of gold and silver being enormous. The high elevation and healthy climate make it a favorite resort for pulmonary patients. There are many fine buildings, and a noble State Capitol with a lofty dome, erected at a cost of $2,500,000, and standing on a high hill, so that it gives a superb outlook. The city was named in honor of General James W. Denver, who was an early Governor of Kansas and served in the Civil War. He first suggested the name of Colorado for the Territory (now a State), and thus his name was given its capital. Denver has built for its water-works, forty-eight miles south of the city, the highest dam in the world, two hundred and ten feet, enclosing a gorge on the South Platte to make an enormous reservoir holding an ample supply.

Being so admirably located, Denver is a centre for excursions into one of the most attractive mountain regions in America. The great Colorado Front Range, or eastern ridge of the Rockies, stretches grandly across the country and has behind it one range after another, extending far westward to the Utah Basin. Towering behind the Front Range is the Saguache Range, the chief ridge of the Rockies, which makes the Continental Divide. Among these complicated Rocky Mountain ranges are various extensive Parks or broad valleys, nestling amid the peaks and ridges, which were originally the beds of inland lakes. Out of this mountain region flow scores of rivers in all directions, the affluents of the Mississippi to the east, the Rio Grande to the south, and the Colorado and the Columbia westward. All of them have carved down deep and magnificent gorges, two to five thousand feet deep, and in places the wonderful results of ages of erosion are displayed in the peculiar constructions of vast regions, and in special sections, where the carvings by water, frost and wind-forces have made weird and fantastic formations in the rocks on a colossal scale, as in the "Garden of the Gods." These mountains and gorges are also filled with untold wealth, and the mines, producing many millions of gold and silver, have attracted the population chiefly since the Civil War, so that the whole district around and beyond Denver is a region of mining towns, which are reached by a network of railways disclosing the grandest scenery, and in many parts the most startling and daring methods of railroad construction. Whenever land can be reclaimed for agriculture or grazing on the flanks of the mountains and in the protected valleys and parks, it is done, so that the district has extensive irrigation canals, in some parts diverting practically all the available flow of water in the streams. This is particularly the case with the Upper Arkansas River, such diversion of the headwaters in Colorado having robbed the river of its water to such a degree that the people of Kansas, whither it flows on its route to the Mississippi, are greatly annoyed and have protracted litigation about it.

COLORADO ATTRACTIONS.

Northwest from Denver is the picturesque Boulder Canyon, and here at the mining town of Boulder is the University of Colorado, with six hundred students. Beyond are Estes Park, one of the smaller enclosed parks among the mountains, having Long's Peak on its verge, rising fourteen thousand two hundred and seventy feet. Westward from Denver is the Clear Creek Canyon, and the route in that direction leads through great scenic attractions, past Golden, Idaho Springs and Georgetown, where silver-mining and health-resorts divide attention, the mountains also displaying several beautiful lakes. Beyond, the railway threads the Devil's Gate, climbing up by remarkable loops, and reaches Graymont at ten thousand feet elevation, having Gray's Peak above it rising fourteen thousand four hundred and forty feet. In this district is the mining town of Central City, while to the northwest is the extensive Middle Park, of three thousand square miles area, a popular resort for sportsmen. Southward from Denver the railway route passes the splendid Casa Blanca, a huge white rock, a thousand feet long and two hundred feet high, and crosses the watershed between the Platte and the Arkansas, at an elevation of over seventy-two hundred feet. Here, amid the mountains, seventy-five miles from Denver, upon a plateau at six thousand feet elevation, is the famous city of Colorado Springs, having twenty-five thousand people and being a noted health-resort. It is pleasantly laid out, with wide, tree-shaded streets, like a typical New England village spread broadly at the eastern base of Pike's Peak. Here live large numbers of people who are unable to stand the rigors of the climate on the Atlantic coast, and it has been carefully preserved as a residential and educational city, saloons being prohibited, with other restrictions calculated to preserve its high character. The settlement began in 1871, but there are no springs nearer than Manitou, several miles away in the spurs of Pike's Peak. The climate of Colorado Springs is charming, and it has, on the one hand, a magnificent mountain view, and on the other a limitless landscape eastward and southward, across the prairie land. Here are the Colorado College and other public institutions, and the National Printers' Home, supported by the printers throughout the country. In the pretty Evergreen Cemetery is buried the authoress, Helen Hunt Jackson, who died in 1885.

Probably the best known summit of the Rockies is Pike's Peak, rearing its snowy top over Manitou, and about six miles westward from Colorado Springs, to an elevation of nearly fourteen thousand two hundred feet. As it rises almost sheer, in the Colorado Front Range, this noble mountain can be seen from afar across the eastern plains. A cog-wheel railway nine miles long ascends to the summit from Manitou, rising seventy-five hundred feet. There is a small hotel at the top, and a superb view over the mountains and glens and mining camps all around. In 1806 General Zebulon Pike, then a captain in the army, led an exploring expedition to this remote region and discovered this noble mountain, which was given his name. Forests cover the lower slopes, but the top is composed of bare rocks, usually snow-covered. Below it a huge tunnel is being bored through the range to connect Colorado Springs with the Cripple Creek mining district to the westward. Manitou has a group of springs of weak compound carbonated soda, resembling those of Ems, and beneficial to consumptive, dyspeptic and other patients. They are at the entrance of the romantic Ute Pass, a gorge with many attractions, which was formerly the trail of the Ute Indians in crossing the mountains. Nearby, upon the Mesa, or "table-land," is the "Garden of the Gods," a tract of about one square mile, thickly studded with huge grotesque cliffs and rocks of white and red sandstones, their unique carving being the result of the erosive processes that have been going on for ages. They are all given appropriate names, and its Gateway is a passage just wide enough for the road, between two enormous bright red rocks over three hundred feet high. Farther south on the Arkansas River is Pueblo, an industrial city of thirty thousand people in a rich mining district, where there is a Mineral Palace, having a wonderful ceiling formed of twenty-eight domes, into which are worked specimens of all the Colorado minerals. The route then crosses the Veta Pass at ninety-four hundred feet elevation, whereon is the abrupt bend known as the "Mule Shoe Curve," and beyond this it descends into the most extensive of the Colorado Parks, the San Luis, covering six thousand square miles. Sentineling its western side is the triple-peaked Sierra Blanca, the loftiest Colorado Mountain, rising almost fourteen thousand five hundred feet. The Rio Grande flows to the southward, and there is Alamosa, and up in the mountains Creede, an extraordinary development of recent silver mining, which began its career when the ore was discovered in 1891, has seven thousand people, and has produced $4,000,000 silver in a year.

Gateway, Garden of the Gods, Colorado

Following up the Arkansas River from Pueblo, a route goes northward behind and west of Pike's Peak into the Cripple Creek district, situated at an elevation of nearly ten thousand feet among the mountains, where in 1890 was a remote cattle ranch. The next year gold was found there, a new population rushed in, and it has since become a leading gold producer, its output of fourteen to twenty millions of gold annually almost turning Colorado from a silver to a gold State. There is now a population of twenty thousand, and the town has many substantial buildings. Westward the route crosses the Continental Divide and descends into the extensive South Park, covering two thousand square miles, reaching Leadville beyond, renowned as a mining camp that has developed into one of the highest cities of the world. In the early Colorado days this was the great gold placer mining camp of California Gulch. Afterwards it produced enormous quantities of silver from the extensive carbonate beds discovered in 1876, and the population expanded to thirty thousand, its name being changed to Leadville. Of late, its gold mining has again become profitable, and its population now is about fifteen thousand, the yield of silver, which once reached $13,000,000 annually, being much reduced owing to the decline in value. To the westward, the Colorado Midland Railway crosses the Continental Divide by the Hagerman Pass, at eleven thousand five hundred and thirty feet elevation, the highest elevation of any railway route across the Rockies. It descends rapidly to Aspen, where $8,000,000 of silver and gold are mined in a year. North of Leadville is the noted Mountain of the Holy Cross, fourteen thousand two hundred feet high, named from the impressive cruciform appearance of two ravines crossing at right angles and always filled with snow.

The Grand Canyon of the Arkansas is one of the most magnificent gorges in the Rocky Mountains. This river above Pueblo forces its passage through a deep pass known in the narrowest part as the Royal Gorge, where the railway is laid alongside the boiling and rushing stream, with rocky cliffs towering twenty-six hundred feet above the line. It ascends westward, beyond the sources of the Arkansas, crossing the Continental Divide by the Marshall Pass, at ten thousand eight hundred and fifty-eight feet elevation, the route up there showing, in its abrupt and bold curves, great engineering skill. The Pass is always covered with snow, and the descent beyond it is to the mining town of Gunnison. The Gunnison River is followed down through its magnificent gorge, the Black Canyon giving a splendid display for sixteen miles of some of the finest scenery of the Rockies. The river is an alternation of foaming rapids and pleasant reaches, and within the canyon is the lofty rock pinnacle of the Currecanti Needle. The adjacent gorge of the Cimarron, a tributary stream, gives also a splendid display of Rocky Mountain wildness, and below it the river passes through the Lower Gunnison Canyon, bounded by smooth-faced sandstone cliffs, and finally it falls into Grand River, one of the head-streams of the Colorado. The combined magnificence of these canyons and mountains makes the environment of the Colorado mining region one of the most attractive scenic districts in America. The railways have arranged a route of a thousand miles through the mountains, starting from Denver, under the title of "Around the Circle," which crosses and recrosses the Continental Divide, threads the wonderful canyons, surmounts all the famous passes over the tops of the Rocky ranges, and includes the most attractive scenery of the district.

WYOMING FOSSILS.

The Union Pacific Railway, westward from Cheyenne in Wyoming, gradually ascends the slope and crosses the Continental Divide at Sherman, the pass being elevated eighty-two hundred and forty-five feet. Here, alongside the track, is the monument erected in memory of Oakes and Oliver Ames of Massachusetts, to whose efforts the construction of this pioneer railway across the Continent was largely due. Upon the western slope of the mountains the descent is to the Laramie Plains, an elevated plateau in Wyoming which is one of the best grazing districts of the country. In the midst of the region on the Big Laramie River is Laramie City, with ten thousand people, a prominent wool and cattle mart. To the north and west high mountains rise, out of which the river flows, and in this district is the great fossil region of Wyoming. This state is the most prolific producer of the skeletons of the enormous beasts that roamed the earth in prehistoric times. About ninety miles northwest of Laramie City are the greatest fossil quarries in existence, and the scientific hunters from all the great museums have been finding rich treasures there. We are told that in an early geological period Wyoming had numerous lakes and swamps and a semi-tropical climate. These huge animals then inhabited the lakes and swamps in large numbers. In dying, they sank into the mud, and their bones were covered by other deposits and became petrified. The extensive deposits of these bones are found where are supposed to have been the mouths of great water-courses, the huge animals, after death, having floated to where they are deposited in such large numbers. The belief is that through the geological eras these animals became covered with possibly twenty thousand feet of rock. Afterwards, the process by which the Rocky Mountains were formed tilted these rock beds, and the subsequent erosion of the strata brought to light these bone-deposits, made millions of years ago. For many years the scientists have been exhuming these skeletons, and have recovered the bones of over three hundred different species. They are of all sizes and characters, and here has been found the most colossal animal ever discovered on the earth, a dinosaur, nearly one hundred and thirty feet long, and thirty-five feet high at the hips and twenty-five feet at the shoulders. The skeleton of this immense creature, who is called a diplodocus, weighs twenty tons, and it is believed that when living he weighed sixty tons, having a neck thirty feet long and a tail twice that length. Yet his head was very small, and the weight of the brain was not over five pounds. In comparison with the mammoth, heretofore regarded as so large, this huge beast, whose foot covered a square yard of earth, was in size as a horse is compared to a dog. Such are the contributions Wyoming is making to our great museums of science.

To the southward of the Laramie Plains is the Colorado North Park, among the mountains of that State, having an area of over two thousand square miles. Beyond, the railway route goes westward among hills and over the plateaus. This route is not as picturesque as some of the other Pacific railways, but in crossing the Continent it discloses very curious scenery. At places there are great Buttes, water-worn and rounded, rising in isolated grandeur; the plains and terraces are carved into elongated and wide depressions, as if abandoned rivers had run through them; there are long and regular embankments, strange hills of fantastic form, huge mounds, broken-down pyramids, vast stone-piles, and the most strange and extraordinary fashionings of nature, showing both water and fire to have been at work. Then the route passes the snow-clad Uintah Mountains to the southward, and crossing the Wahsatch range, enters Utah, traversing its remarkable enclosed basin, where the waters have no outlet to the sea, but flow into salt lakes which lose their surplus supplies by evaporation in the summer. Beyond, is the wild and picturesque Echo Canyon, with the green valley of Weber River and the Weber Canyon. Here is the gigantic Castle Rock, a rugged stone-pile fantastically carved by nature, having a giant doorway and all the semblance of a mountain fortress. Here is also the "One Thousand Mile Tree," on the northern side of the road, being that distance west of Omaha. In the Echo Gorge is the Hanging Rock, where Brigham Young, as the Mormon Pilgrims journeyed to their Utah home, is said to have preached the first sermon to them in the "Promised Land." The old-time emigrant trail passes through these canyons alongside the railway and the river. A remarkable sight within the Weber Canyon is the Devil's Slide, where on the face of an almost perpendicular red mountain, eight hundred feet high, there is inlaid a brilliantly white strip of limestone about fifteen feet wide, all the way from top to bottom, having enclosing white walls, the whole work being as regularly constructed as if built by a stonemason. Beyond, we come to Ogden, a busy industrial town of twenty thousand people, the western terminus of the Union Pacific Railway, and having another railroad leading thirty-seven miles southward to Salt Lake City.

GREAT SALT LAKE.

In the centre of the Rockies, occupying a large portion of Utah and adjacent States, is the "Great Basin," which, as remarked, has no drainage outlet for its waters. The geologists tell us that in ancient times this region was covered by two extensive lakes, one of them in the Pleistocene era occupying the now desert interior basin of Utah. This extinct lake, whose ancient shores can be distinctly traced, has been named Lake Bonneville. When at its greatest expansion, it covered twenty thousand square miles, and the waters were nearly a thousand feet deep, overflowing to the northward into a branch of ShoshonÉ River through a deep pass, and going thence to the Pacific. The waters of this lake, by climatic changes, gradually dwindled, the loss by evaporation overcame the rainfall supply, the overflow ceased, and then the lake dried up, revealing the desert bottom. Of its waters there now remain the Great Salt Lake of Utah, about eighty miles long and from thirty to fifty miles wide, very shallow, averaging only twenty feet depth, and not over fifty feet in the deepest place, having monotonously flat shores on the desert plateau, elevated forty-two hundred feet above the sea. Its dimensions vary according to the rainfall, the surface rising and falling in various periods of years. Several streams flow in, among them the Jordan River, forty miles long, draining Utah Lake to the southward. The waters are densely salt, varying from fourteen to twenty-two per cent. as the lake is high or low (compared with three to four per cent. in the ocean), and it is estimated to contain four hundred million tons of salt. Not a fish can live there excepting a small brine shrimp. A bath in the lake is novel, as the density makes the body very buoyant, easily floating head and shoulders above the water.

To this desert region, after being driven from Nauvoo on the Mississippi, Brigham Young brought his first Mormon colony by a long journey across the plains and mountains, a band of one hundred and forty-three persons, arriving in July, 1847, Utah then being Mexican territory. They organized the State of Deseret, and it afterwards became a Territory of the United States. By prodigious labors, constructing irrigation canals to bring in the mountain streams, they made the soil productive, and now it is one of the most fertile valleys in the country. Almost the whole flow of the Jordan River is thus used for irrigation. Colonies and proselytes were brought in from various parts of the world, until two hundred thousand Mormons came to Utah, and after protracted conflicts with the Government, polygamy was declared illegal, and its discontinuance was ordered by proclamation of the Mormon President. Twelve miles from the Great Salt Lake is the Utah capital and Mormon Zion, Salt Lake City, where the Latter-Day Saints and Gentiles together exceed fifty thousand. Its prosperity is largely due to the extensive mining interests of the surrounding country. The lofty Wahsatch Mountains are close to the city on the northern and eastern sides, while to the south, seen over a hundred miles of almost level plain, is a magnificent range of snow-covered mountains, this being the perpetual and awe-inspiring view from all parts of the city. The streets are wide and lined with shade trees, the residences surrounded by gardens, and irrigation canals border all the thoroughfares, so that the whole place is embosomed in foliage, and the delicious green adds to its scenic attractiveness. The Temple Block of ten acres, the sacred square of the Mormons, is the centre from which the streets are laid towards the four cardinal points of the compass. A high adobÉ wall surrounds it, and here is the great Mormon Temple of granite, which was forty years building, and cost over $4,000,000, having three pointed towers at each end, the loftiest being surmounted by a gilded figure of the Mormon angel Moroni. Here is also the Mormon Tabernacle, a huge oval-shaped structure, surmounted by a roof rounded like a turtle-back, the interior accommodating twelve thousand people. This is their great meeting-place, and they also have a smaller Assembly Hall for religious services. These are the chief buildings of Salt Lake City. To the eastward in the suburbs is the military post of Fort Douglas, where the troops are barracked that guard the Mormon capital. In the earlier period, when there were fears of trouble, a large garrison was kept at this extensive fortification to maintain government control.

OGDEN TO SACRAMENTO.

Westward from Ogden in Utah the Union Pacific route to California is continued upon the Southern Pacific system, that company having absorbed the original Central Pacific road. It passes Corinne, the largest Gentile city in Utah, and then through the Promontory Mountains, on the northern verge of Great Salt Lake. It was at Promontory Point on May 10, 1869, that the railway builders of this original transcontinental line, coming both ways, met, and joined the tracks. The last tie was made of California rosewood, trimmed with silver, and the last four spikes were of silver and gold. The final golden spike was driven with a silver hammer in the presence of a large and silent assemblage. The locomotives coming from the East and the West met, as Bret Harte has written:

"Pilots touching—head to head

Facing on the single track;

Half a world behind each back!"

Beyond, the Great American Desert, an alkaline waste, is crossed, the State of Nevada is entered, the Humboldt River is followed for awhile, and then Truckee River is ascended through the Pleasant Valley, leading into the Sierra Nevada, the lower mountain slopes covered with magnificent forests and the railroad protected from avalanches by snow-sheds. The Humboldt River has no outlet. It spreads out in an extensive sheet of water known as the "Carson Sink" and evaporates. At Reno is the Nevada State University, and as this is a silver region there are extensive smelting mills. Thirty-one miles southward is Carson, the capital of Nevada, and twenty-one miles farther the famous silver-mining town of Virginia City, with ten thousand people, built half-way up a steep mountain slope and completely surrounded by mountains. Virginia City stands directly over the noted Comstock Lode, and here are the Bonanza Mines, which were such prolific producers in the great silver days. This lode has produced over $450,000,000, chiefly silver, and it is drained by the Sutro Tunnel, nearly four miles long, which cost $4,500,000 to construct. Nearby, on the California boundary, and at six thousand feet elevation, is the beautiful Lake Tahoe, one of the loveliest sheets of water in the world, twenty-two miles long, very deep, surrounded by snow-clad mountains, and yet it never freezes, its outlet being the Truckee River. In a region of many lakes, it is known as "the gem of the high Sierras." To the westward of Reno is another lovely sheet of water, Donner Lake, embosomed in the lap of towering hills, its name coming from an early explorer, Captain Donner, who, with many of his party, perished on its shores during a heavy snowstorm in 1846. The top of the Sierra Nevada is crossed through a tunnel at Summit Station, elevated seven thousand feet, and beyond there is a complete change both in climate and vegetation, the descent being rapid and the transition from arctic snows to sub-tropical flowers very quick. The line is in many places carved out of the faces of startling precipices, and here it rounds the famous beetling promontory known as Cape Horn. Then, coming down among the orchards and vineyards, it enters the wide and fertile Sacramento Valley, and almost at sea-level comes to the capital of California, the city of Sacramento, built on the eastern bank of Sacramento River just below the mouth of the American River. It is a busy city with thirty thousand people, and has a large and handsome State Capitol.

TRANSCONTINENTAL ROUTES.

The Northern Pacific Railway, the next route northward, after following up the Yellowstone River to Livingston, at the entrance to Yellowstone Park in Montana, ascends the Belt Mountains, crossing them through Bozeman Tunnel at an elevation of nearly fifty-six hundred feet. This range is an outlying eastern spur of the Rockies. The road passes the mining town of Butte, there being forty thousand people in the neighboring settlements. Here are many gold, silver and copper mines, including the great Anaconda Mine, which was sold in 1898 to the company at present working it for $45,000,000, the product of the mine being silver and copper. The Butte copper output is two hundred and fifty million pounds annually, and the smelting-works at Anaconda are the largest in the world. At Three Forks, not far away, is the confluence of the Madison, Jefferson and Gallatin Rivers, forming the Missouri. Beyond is Helena, the capital of Montana, built in the Prickly Pear Valley near the eastern base of the main Rocky Mountain range and having fifteen thousand population. This is in another rich mining district, and the "Last Chance Gulch," running through the city, has yielded over $30,000,000 gold, while all around are gold, silver, copper and lead-deposits. Twenty-four miles from Helena, the main range of the Rockies is crossed by the Mullen's Pass tunnel at fifty-five hundred and fifty feet elevation. At Gold Creek in the valley beyond, the last golden spike of the Northern Pacific Railway was driven in September, 1883, uniting the tracks which had advanced from the east and west and met there. President Henry Villard made this the occasion of great festivity, bringing many train-loads of distinguished men to the ceremony, and shortly afterwards the company, which was heavily in debt, went into a Receivership. The railroad follows the Missoula and Pend d'Oreille (the "earring") Rivers, which unite in Clark's Fork, a tributary of the Columbia River, and enters Idaho, "the gem of the mountains," or, as called by the Nez Perces, Edah-hoe; finally coming to Spokane in Washington State. This busy manufacturing town of over twenty thousand people was burnt in 1889, but has entirely recovered from the calamity. The Spokane River descends one hundred and fifty feet in two falls within the town, furnishing an admirable water-power. To the southwest is the confluence of the Snake and Columbia Rivers, and beyond, the railway penetrates the defiles of the Cascade Mountains, the northern prolongation of the California Coast range, the Northern Pacific line finally terminating at Tacoma on Puget Sound.

The great Columbia is the chief river draining the western slopes of the Rockies. It has a broad estuary, and in May, 1792, Captain Robert Gray of Boston, coasting along the shore in his bark "Columbia Rediviva," discovered it, was baffled more than a week before he could cross the shallow bar at its mouth, and gave it the name of his vessel. The Spaniards marked his discovery on one of their maps without any head to the river, recording alongside in Spanish y-aun se ignora—meaning "and it is not yet known" where the source of the river is situated. The famous Danish geographer, Malte-Brun, reading this, made the mistake of recognizing the word ignora as Oregon, and published it in the early nineteenth century as the name of the country, to which it has stuck. Thus is Oregon, like California, a name given without meaning. The Columbia is an enormous river, over twelve hundred miles long, rising in Otter Lake, just north of the Dominion boundary, making a long loop up into British America, then coming down into the United States between the Rockies and the Cascades with another broad western loop, and swinging around to the southeast, finally turning westward to form the boundary between Oregon and Washington State to the Pacific. The chief tributary is Snake River, known also as Lewis Fork, which comes out of the western verge of the Yellowstone Park, makes an extensive southern bend through Idaho and is nine hundred miles long, being a most remarkable river. West of the Rockies is an enormous area, estimated at two hundred and fifty thousand square miles, that has been subjected to volcanic action, being overflowed by what is known as the "Columbia lava," in deposits from one-half mile to a mile in thickness. Through this region the Snake River has carved out its extraordinary canyon in places four thousand feet deep, and in some respects rivalling the canyons of the Colorado. Down in the bottom of this gigantic fissure can be seen the ancient rocky formation of the mountains, elsewhere covered by the sheet of lava. The curious sight is also given of various tributaries sinking under the strata of lava and ultimately coming out through the sides of the canyon, pouring their waters down into the main river far below.

Within this canyon the Snake River goes over the noted ShoshonÉ Falls, a series of cataracts. The first one is the Twin Falls descending one hundred and eighty feet, then the river goes down the Bridal Veil of eighty feet descent, and finally it pours in grandeur over the great ShoshonÉ Falls, nearly a thousand feet wide, and descending two hundred and ten feet, a most magnificent cataract. After the confluence with the Columbia, the latter river leaves the region of sands and lava for the rocks and mountains, and here are the Dalles. These are mainly flagstones that make troughs and fissures, and compress the channel. At first the river, a mile wide, goes over a wall twenty feet high and stretching completely across, and the enormous current is compressed not far below into a narrow pass only a hundred and thirty feet wide and nearly three miles long, encompassed by high perpendicular cliffs of such regular formation that they seem as if constructed of masonry. The Dalles make crooked, trough-like channels through which the waters wildly rush. The amazing way in which the agile fish are able to ascend these rapids and cataract through all the turmoil, seeking the quiet river reaches above, caused the Indians to call the place the Salmon Falls. Here is the town of the Dalles, the supplying market for the Idaho mining district, an active manufacturing place with five thousand people. There are various islands in these rapids, most of them having been used for Indian burial-places and some having numerous graves. Below, the Columbia presents very fine scenery in passing the defiles of the Cascade Mountains, and to the southward is the noble form of Mount Hood, rising over eleven thousand feet, displaying glaciers and having snow-covered peaks all about. At the Cascade Locks the Columbia descends another rapid, where huge rocks buffet the turbulent waters, the whirling foaming torrent wildly rushing among them. Here the descent is twenty-five feet, and the Government has improved the navigation by a spacious ship canal a mile long, built at a cost of $4,000,000. Enormous cliffs, some of grand and imposing form, environ the river in passing through these Cascade Mountains, some rising twenty-five hundred feet. We are told these mountains were first named from the numerous cascades which pour in from tributary streams coming over the cliffs and through the crevices of this tremendous chasm. Often a dozen of these fairy waterfalls can be seen in a single river reach, some dissolving into spray before half-way down, others stealing through crooked crannies, and many being tiny threads of glistening foam apparently frozen to the mountain side. Here is Undine's Veil pouring over a broader ledge, and the Oneonta, Horse Tail, La Tourelle and Bridal Veil cataracts, with the far-famed Multnomah Fall, the most beautiful of all, eight hundred feet high, descending with graceful gentleness over the massive cliffs a long and filmy yet matchless thread of silver spray. Emerging, the Columbia receives the Willamette River, coming up from the south on the western verge of the Cascades, and then proceeds grandly by its broad estuary to the Pacific.

Near the Canadian border the Great Northern Railway crosses the continent, surmounting the Rockies at the lowest elevation of any of the transcontinental lines. Starting from St. Paul, it traverses the Devil's Lake country in Montana, passes Fort Buford on the Upper Missouri, and crosses the Rockies at fifty-two hundred feet elevation. Beyond is the Kootenay gold district, and the road comes to Spokane, crosses the Columbia River and surmounts the Cascades at thirty-three hundred and seventy-five feet elevation, the mountain top being pierced by a three-mile tunnel. Then traversing sixty miles of fine forests, the railway terminates at Everett on Puget Sound.

THE CANADIAN PACIFIC ROUTE.

The Canadian Pacific Railway, crossing the Continent in the Dominion of Canada, west of Winnipeg traverses the prairies of Manitoba and Assiniboia until they gradually blend into the rounded and grass-covered foothills of Alberta, finally rising nearly a thousand miles west of the Red River into the snow-capped peaks of the Rockies. This is the garden region of the Canadian Northwest for wheat-growing and cattle-grazing, and it stretches in almost limitless expanse a fertile empire far northward to Edmonton and Prince Albert, with branch railways leading up there, the rich black soils testifying the wealth in the land. At Regina is the capital of the Northwest Territory, three hundred and fifty-seven miles west of Winnipeg, the headquarters of the Canadian "North West Mounted Police," a superb body of one thousand picked men who control the Indians and maintain order in the Northwest Territory. The Lieutenant-Governor residing here is a potentate governing a wide domain spreading out to the Rockies and up to the North Pole. The town which is his capital is scattered rather loosely over the prairie. In early times a hardy pioneer came to this frontier, and at the crossing of a little stream west of Regina his cart broke down. The Cree Indians watched him mend it, and afterwards spoke of the stream in their language as "The creek where the white man mended the cart with a moose jawbone." This elaborate name has since been contracted into Moose Jaw, a town where a branch line comes into the Canadian Pacific up through Dakota from St. Paul and Minneapolis. The route farther westward is in the land of the Crees, and crosses the South Saskatchewan River at Medicine Hat, a settlement which the matter-of-fact people call "The Hat" for short. The Indians say that the Great Spirit had a breathing-place in the river nearby, where it never was frozen even in the coldest winters. He always appeared in the form of a serpent, and once, when a chief was walking on the shore, the serpent came and told him if he would throw his squaw into the opening as a sacrifice, he would become a great warrior and medicine man. He was ambitious, but did not wish to lose her, so he threw his dog in, but the indignant serpent demanded the squaw. The Indian told her of the conditions, she consented to the sacrifice, her dead body was thrown in, and after a night of vigil the chief received from the serpent a warrior's medicine hat, handsomely trimmed with ermine, and was always after victorious. Thus the locality became the Medicine Hat, and the Indians watch the river in severe winters, glad to find the spot is not frozen and that the Great Spirit still has his breathing-place and remains with them.

To the westward the snow-capped Rockies become visible, and here are the reservations of the Blackfeet Indians, who were the most warlike tribe of the region, and hunted the buffalo as far south as the Missouri. The memory of Crowfoot, their leading chief, is preserved in the name of the railway station. The Bow River, an affluent of the Saskatchewan, is followed up to Calgary, the centre of the ranching district of Alberta, a town at thirty-four hundred feet elevation, having high mountains overhanging its western verge. Here are branch railways north and south, leading along the eastern foothills of the Rockies, which are filled with herds of cattle and horses, the roads going up to Edmonton and down into the United States. The warm "Chinook" winds from the Pacific coast, coming through the mountain passes, temper the cold, making the balmy atmosphere favoring grass and animals alike. The Pacific route follows the Bow River Valley into the heart of the mountains, with magnificent snow-covered peaks all about, their saw-like edges, gaunt crags and almost denuded surfaces justifying their name of the Rockies.

BANFF.

The display of mountain scenery along the Canadian Pacific line in passing through the Rockies is the finest in North America, coming largely from two causes, each contributing to the grandeur and impressiveness of the view. The width of the Rocky Mountain ranges in Alberta and British Columbia is not much over three hundred miles, while in the United States they are scattered and spread over a thousand miles of space with intervening tameness. The railway passes also are lower in British Columbia, so that the adjacent peaks rise higher above the valleys, making them really grander mountains for the spectator, who is thus brought to the very bases of such stalwart peaks as Mount Stephen and Mount Sir Donald, rearing their snow-covered summits on high for a mile and a half above his head. Both in concentration and elevation, as well as by the terrific wildness of the Kicking Horse and Rogers Passes, by which the ranges are crossed, the magnificence of this part of the Rockies is displayed. Just within the eastern verge of the mountains are the Banff Hot Springs, which, with their environment, make the "Canadian Rocky Mountains Park." This reservation covers the Bow River Valley and adjacent mountains. The winding river comes from its glacier sources in the west through a broad deep fissure. This is crossed almost at right angles by another valley, having the Spray River coming up from the south through it to join the Bow, while to the north the floor-level of this valley is higher, but without any distinctive stream. These valleys and their enclosing peaks are all formed on a scale of stupendous magnificence, yet so clear is the atmosphere that distance is dwarfed, making the views perfect. Going down to the river bank, where the deep, trough-like gorges come together, it is found that the action of the waters has thoroughly displayed the geological formation of these mountains, the enormous rock strata standing up inclined from the perpendicular generally at an angle of about 30°, being all tilted towards the eastward. Where these strata-edges and ends are eroded, they are cut off almost vertically, and thus they rise on high into sharp jagged peaks like saw-teeth. Stunted firs cover much of the lower slopes, but the tops are all bare, being rough, or denuded and smoothed rocks, snow-clad, excepting where the slope is too steep to hold it.

Along the winding canyon from the northwest rushes the Bow River, sliding in noisy turmoil, with ample spray and silvery foam, down a series of cascades, making a most beautiful cataract, then turning sharply at a right angle to the northeast to go around the end of a mountain. The bright green waters in full volume swiftly glide around the bend and away through the narrow gap formed between two towering cliffs into a deep gorge several miles long. The smaller, but even more swiftly-darting Spray River, dashes along rapids and joins the Bow just at the bend. Such is the scene giving the central point of beauty within this grand amphitheatre of high mountains, overlooked from an elevated plateau above the waterfall, where the landscape is finest. The Rocky Mountains Park includes about two hundred and sixty square miles of streams, lakes and enclosing mountains, improved by many miles of good roads and bridle-paths to develop its beauties. The original attraction was the Banff warm sulphur springs, appearing along the side and base of Sulphur Mountain, rising on the southern bank of Bow River above the waterfall. The temperature of the waters changes little from 90°, and they are extensively used for bathing, being recommended for rheumatic troubles. One spring of copious flow is a pool within a capacious dome-shaped cavern, hollowed out of a mound of calcareous tufa. This is the crater of an extinct geyser, the orifice at the top, which had been its vent, being availed of for light and ventilation. High up among the mountains to the eastward is the Devil's Lake, a beautiful crescent-shaped sheet of water much like a river, eleven miles long, and enclosed by towering peaks.

BANFF TO VANCOUVER.

Westward from Banff the main range of the Rockies is crossed at an elevation of fifty-three hundred feet, the Continental Divide. The Bow River Valley is followed up to Mount Stephen, which is encircled to the northward. This splendid duomo-like mountain rises thirteen thousand two hundred feet, being named after George Stephen, Lord Mountstephen, the first president of the railway. In approaching, there are passed scores of towering snow-clad peaks. At Laggan, among them, at more than six thousand feet elevation, are three gems of the mountains, the Lakes of the Clouds—Louise, Mirror and Agnes. At the summit of the pass a rustic signboard bears the words "The Great Divide," marking the backbone of the Continent, whence tiny rills flow alongside the railway in both directions, a little brook leading eastward down to the Bow, whose waters go out to Hudson Bay and the Atlantic, while to the westward another diminutive stream is the head of Wapta River, flowing into the Columbia and thence to the Pacific. Three pretty green lakes start the Wapta or Kicking Horse River, its northern branch coming from a huge glacier nine miles long, and its volume expanding from a hundred cascades and brooks tumbling down from the snowbanks and ice-fields all about. Then it crosses the flat floor of a deep valley, which soon develops into a series of terrific gorges, as with rapids and cataracts the stream suddenly drops into an abyss and foams and roars deep down in an impressive canyon. The railway repeatedly crosses this stupendous chasm in getting down the Kicking Horse Pass, giving grand views of high mountains all around, and after a scene of true alpine magnificence it comes out at the broad valley of the Columbia. This river goes northward between the Rockies and the Selkirks, the next western range, and turning westward penetrates them and flows southward on their western flanks into the United States.

Our railway route next goes up the Beaver River gorge to cross the Selkirks through the Rogers Pass at forty-three hundred feet elevation, where Mount Sir Donald guards the Pass. It traverses a region displaying grand scenery, mounting high above the streams, the gorge filled with giant trees between Mounts Sir Donald and Hermit, with frequent airy bridges thrown across the subsidiary ravines, down which come sparkling cataracts. This narrow gorge has frequent avalanches, so that much of the road is covered by ponderous snow-sheds. This is the Rogers Pass, displaying savage grandeur, and was first entered by white men from British Columbia under Major Rogers in 1883, when the railway route was surveyed. It is also reserved for a Canadian National Park. The Hermit Mountain overlooks the pass from the north, while on the south side a range extends westward to the ponderous and lofty pyramidal top of Mount Sir Donald, rising ten thousand seven hundred feet, named for Sir Donald Smith, Lord Strathcona, President of the Bank of Montreal. Alongside is the great glacier of the Selkirks, whose waters flow into the deep valley of the Illecillewaet River, the "Dancing Water," by which the railway goes westward out of the mountains. Having crossed the summit of the pass, the railway makes a short curve into this valley, and gives a grand view of the great glacier covering all of its head. Here is the Glacier House, on a flat surface of delicious greensward alongside the line, having a silvery cascade pouring for a thousand feet down the opposite mountain. Beyond, the Illecillewaet descends rapids and the railway has a difficult task in getting down the steep and contorted gorge by startling loops until, finally emerging from the mountain fastness on the western slope of the Selkirks, it comes a second time to the open Columbia Valley, the river now flowing with greater volume southward towards the United States. Across the Columbia is the Gold range, the third mountain ridge to be crossed. This is done by the Eagle Pass, less difficult than the other passes through the Rockies, the crossing being made at two thousand feet elevation, and the route descending westward along Eagle River and several pleasant lakes that make its source and cover the floor of the higher valley. This stream leads into the Great Shuswap Lake, the largest body of water in British Columbia, spreading its sinuous arms like an octopus among the mountain ridges. This lake has over two hundred miles of coast-line, and is drained westward by Thompson River. To the southward it has a tributary flowing out of the long and slender Okanagan Lake, a sheet of water among the mountains extending seventy miles and having fertile shores.

The Coast range of the Rockies is still beyond us, the fourth and last ridge of these wonderful mountains, through which the Canadian Pacific makes its way by going down the remarkable canyons of Thompson and Fraser Rivers for nearly three hundred miles. At the junction of the two forks of the Thompson is the town of Kamloops, its Indian name meaning "the confluence." It is in a good ranching district, and like all the settlements in British Columbia has quite an elaborate "China-town." Beyond Kamloops the Thompson canyon is entered, a desolate gorge almost without vegetation, through which a rapid torrent rushes, the high steep shores being composed of a rotten rock which water and frost have moulded into strange and fantastic shapes, while the stream constantly burrows more deeply into it. The mud-colored banks are thus carved into massive turrets, cones and pyramids, with groups of impressive columns standing on high, having colossal ranks of ghostly statues looking down from above. In one place a grand semicircular group of cowled and hooded monks with their backs to the river are kneeling apparently around a gigantic altar. Almost every conceivable form has been wrought by the running waters on these precipitous bluffs. Not a tree is seen, and all seems bleak desolation. At the Black Canyon the scene is mournfully terrific, the walls composed of an almost black sand, wherein the whirling river rapids have scooped out immense amphitheatres mounting almost perpendicularly for a thousand feet. Then a change comes, the steep and barren walls developing varieties of color, being streaked with creamy white, red, purple, yellow, maroon, dark brown and black in richest form, as the waters have run the different hued soils over them from top to bottom, the rushing river below being a bright emerald. It is a picture of parti-colored desolation, the gaudy hues and strange forms of these precipitous cliffs being the gorgeous exhibition of a most beautiful desert. This remarkable canyon is followed nearly a hundred miles until the Thompson flows into the Fraser River.

The Fraser Canyon is deep, and carries a larger river among higher mountains. Its shores are steep, but are composed of firmer rocks, along which the railway is constructed largely on galleries, with frequent tunnels. Deep in the fissure are Indians spearing for salmon, and an occasional Chinaman may be seen on a sand-bar washing out the silt to find gold, as both these rivers bring down gold-bearing sands. The rocky development of the Fraser and the magnitude of its canyon increase as it plunges deeper among the higher Coast range mountains. For thirty miles below North Bend, a place where enough flat land is left on a terrace for a little railway station, is the most impressive portion, and the final scene of grandeur on this route through the Rockies. Almost perpendicular enclosing mountains tower above, and the river is compressed by high walls of black rocks, so steep that the road is placed upon a shelf hewn out along them. Through this deep, contracted canyon the river winds, at times confined into such narrow crooked straits that the water rushes in swiftly-moving massive billows like the Niagara rapids. Tunnels pierce the jutting cliffs, bridges and walls carry the railway along, and at intervals wild cascades leap through fissures down the mountain sides. The ever-present and industrious Indians are seen in most perilous positions down by the river catching the bright-colored salmon, which they hang upon rude drying-poles among the crags. There is a brief little village, now and then, along this dreary canyon, where there may be a sparse bit of flat terrace, enabling a few white people to live in company with Indians and Chinamen, the "Joss House" of the Celestial and his queer-looking cemetery, with its tall poles and streamers to keep away the dreaded birds and evil spirits, being conspicuous. Thus the river forces its passage through the Coast range, until at Yale the mountains recede, the canyon gradually broadens into a flat intervale between distant ridges, and there are farms and pastures. As the railway emerges from the mountains, the gleaming white dome of the isolated snow-capped Mount Baker is seen glistening under the sunlight sixty miles away just beyond the United States border. The Fraser River finally flows into the Gulf of Georgia, after a course of six hundred miles through the mountains from the northward, the chief river of British Columbia. It was named for Simon Fraser of the Northwest Fur Company, who explored it to its source amid incredible hardships and difficulties in 1808. The finest timber grows throughout this region. The railway terminates at the city of Vancouver, on Burrard Inlet, a fine harbor of the Gulf of Georgia, founded in 1885, and having eighteen thousand people, with considerable manufactures and an extensive trade. The lower Fraser River is a great salmon-canning region, the shores having many canning-factories, while at New Westminster, the chief town, are large sawmills, the two products of this district being fish and lumber, and the Chinese, who are numerous, doing most of the labor.

BOUND TO ALASKA.

Westward from the Gulf of Georgia is Vancouver Island, stretching parallel to the coast and nearly three hundred miles long, the larger part of it being composed of mountains, some reaching an elevation of over seven thousand feet. It has fine forests and valuable coal mines at Nanaimo and Wellington, which furnish fuel supplies along the Pacific coast. The redoubtable Spanish adventurer, Juan de Fuca, discovered it in 1592, and his name was given the strait at its southern extremity, separating the island from the United States. The Spaniards held it until near the close of the eighteenth century, when Captain George Vancouver came with a squadron and it was surrendered to the English by the Spanish Governor Quadra, its name afterwards being called for many years Quadra and Vancouver, after the two officers. Upon a little harbor at the southeastern extremity in 1842, the Hudson Bay Company established Fort Victoria, which has since become the capital of the Province of British Columbia. This is a pleasant city of twenty-five thousand population, having an extensive Chinese quarter. To the westward is the important British naval station and dockyard of Esquimalt, upon an admirable land-locked harbor of large capacity.

For over a thousand miles, a series of internal waters behind large islands, with bays, straits and archipelagoes, lead northward from the Gulf of Georgia to Alaska, making one of the most admirable scenic routes in America. Their shores are high mountains covered with superb forests, and the voyage over these waters is most attractive. From the Gulf of Georgia the route passes through Discovery Passage, the Seymour Narrows (where the tide rushes sometimes at twelve knots an hour), Johnstone Strait, Broughton Strait, and Queen Charlotte Sound. North of Vancouver Island there is a short passage on the open sea and then Fitzhugh Sound is entered, opening into the Lama Passage and Seaforth Channel to Millbank Sound, where there is another brief open sea journey. Then various interior waters lead to Greenville Channel and Chatham Sound. High mountains are everywhere, and deep, narrow fiords run far up into the land, the journey displaying so much magnificent scenery that the mind soon becomes satiated with the excessive supply of unadulterated grandeur. In this region is the Nasse River, where in the spring the Indians catch the Oulichan or "candle-fish," which gives them light, this fish being so full of oil that when dry and provided with a wick it burns like a candle. Just beyond is the boundary of Alaska at fifty-four degrees forty minutes north latitude, the famous "fifty-four forty or fight" boundary of 1843, when the United States claimed that Oregon extended up to the Russian territory at that latitude, but afterwards abandoned the claim. Alaska is a very large country, exceeding one-sixth the area of the United States, and was bought from Russia by Secretary Seward in 1867 for $7,200,000, a price then deemed extravagant, but the purchase has been enormously profitable. The name is derived from the Indian Al-ay-ek-sha, meaning the "Great land." Besides its large extent of main land, it includes some fifteen thousand islands, and its enormous river, the Yukon, flowing into the Behring Sea, has a delta sixty miles wide at its mouth, is three thousand miles long, and is navigable for almost two thousand miles. Although Alaska's productiveness seems just beginning to be realized, yet it has yielded in gold and furs, fish and other products, since the purchase, over $150,000,000.

Sitka, Alaska, from the Sea

Within Alaska, the route of exploration continues through Clarence Strait to the Alexander Archipelago, comprising several thousand islands, many of which are mountainous, and about eleven hundred of the larger ones have been charted. Here is Fort Wrangell, seven hundred miles from Victoria, on one of the islands, a little settlement named after Baron Wrangell, the Russian Governor of Alaska in 1834. Upon landing, the visitors see the Indians and their chief curiosity, the "totem poles," erected in front of their houses, and carved with rude figures emblematic of the owner and his ancestors. These poles are twenty to sixty feet in height, and two to five feet in diameter. The natives are divided into clans, of which the Whale, the Eagle, the Wolf and the Raven are the chief representatives and are said to have been the progenitors. These are also carved on the poles and show the intermarriages of ancestors, the leading families having the most elaborate poles. Beyond Fort Wrangell are Soukhoi Channel and Frederick Sound, leading into Chatham Strait, having on its western side Baranoff Island, on the outer edge of which is Sitka Sound. Here is Sitka, the capital of Alaska, in a well-protected bay dotted with pleasant islands in front and having snow-covered mountains for a high background. Alexander Baranoff founded the town in 1804, the first Russian Governor of Alaska, and there are now about twelve hundred inhabitants, mostly Indians. The old wooden Baranoff Castle, which was the residence of the Russian Governors, is on a hill near the landing-place. The main street leads past the Greek Church, surmounted with its bulbous spire, having six sweet-toned bells brought from Moscow, and adjoining it are various old-time log houses built by the early Russians. The church is still maintained by the Russian Government. The visitors buy curiosities and invest their small change in the Indians who get up monotonous dances or exciting canoe races for their amusement. It is a curious fact that, owing to the Kuro Siwo, or Japanese warm current coming across the Pacific, Sitka has a mild and most equable climate, the summer temperature averaging 54° and the winter 32°, the thermometer seldom falling to zero.

The Stephens Passage leads north from Frederick Sound, and into it opens Taku Inlet, a large fiord displaying fine glaciers. Here at Holkham Bay in 1876 began the first placer gold-mining in Alaska. Just beyond is Gastineaux Channel, between the mainland and Douglas Island. Upon its eastern bank, nine hundred miles from Victoria, is Juneau, the largest town in Alaska, having fifteen hundred population, about half of them whites; an American settlement, begun in 1880 under Yankee auspices, and named after the nephew of the founder of Milwaukee, Wisconsin. The people are mostly gold-miners. The little white houses are on a narrow strip of comparatively level land along the shore, having a high and precipitous mountain behind. Juneau deals in furs and Chilkat blankets, the latter, when genuine, being made of the hair of mountain-goats and colored with native dyes. It is also a starting-point for the Klondyke and Yukon regions. Across the narrow strait, upon Douglas Island, is the famous Treadwell gold-mine, having three enormous ore-crushing mills, the largest in the world, aggregating nearly eight hundred stamps. This is a huge mountain of gold-ore which John Treadwell bought in 1882 from its owner for $430. It has paid since then $9,000,000 in dividends, and now with increased output crushes three thousand tons of ore daily, netting $4 gold per ton, and pours into the laps of the Rothschilds, its present owners, probably $2,000,000 annually from the enlarged product. The ore actually in sight in the mountain is estimated to be worth five times as much as was originally paid for the whole of Alaska. There is a native Indian cemetery adjoining Juneau, having curious little huts containing the cremated remains of the dead, with each one's personal effects.

THE GREAT MUIR GLACIER.

Passing west of Douglas Island and through Icy Strait to Glacier Bay, a magnificent view is presented. Snow-covered mountains rise six and seven thousand feet all around, and to the northwest is the imposing Mount Fairweather range, elevated over fifteen thousand feet. Glacier Bay extends forty-five miles up into the land, its width gradually contracting from twelve to three miles. Small icebergs and floes cover much of the surface, as they are constantly detached from the glaciers descending into it. At the head of the bay is the greatest curiosity of Alaska and the most stupendous glacier existing,—the Muir Glacier,—named in honor of Professor John Muir, the geologist of the Pacific coast, who first saw it in 1879 and thoroughly explored it in 1890. When Vancouver was here at the close of the eighteenth century he wrote that a wall of ice extended across the mouth of the bay. The belief is that the glacier once filled the entire bay and has gradually receded. Near the middle of the bay is Willoughby Island, a rock two miles long and fifteen hundred feet high, showing striated and polished surfaces and glacial grooves from bottom to top. This glacier far exceeds all the Swiss ice-fields put together, and it enters the sea with a front one mile and a half wide and two to three hundred feet high. Unlike the dirty terminal moraines of the Swiss glaciers, this is a splendid wall of clear blue and white ice, built up in columns, spires and huge crystal masses, displaying beautiful caves and grottoes. It goes many hundreds of feet below the surface of the water, and from its front, masses of ice constantly detach and fall into the bay with noises like thunder or the discharge of artillery. Huge bergs topple over, clouds of spray arise, and gigantic waves are sent across the water. Every few minutes this goes on as the glacier, moving forward with resistless motion, breaks to pieces at the end. The field of ice making this wonderful glacier is formed by nine main streams and seventeen smaller arms. It occupies a vast amphitheatre back among the mountains, thirty to forty miles across, and where it breaks out between the higher mountains to descend to the sea is about three miles wide. The superficial area of this mass of ice is three hundred and fifty square miles. It moves forward from seven to ten feet daily at the edges and more in the centre, and in August, when it loses the most ice, the estimate is that about two hundred millions of cubic feet fall into the bay every day. It loses more ice in the summer than it gains in the winter, and thus steadily retrogrades. The visitors go up to its face, although it cannot be ascended there, and then landing alongside approach it through a lateral moraine, and can there ascend to the top and walk upon the surface. The character and appearance of this famous glacier were much changed by an earthquake in 1899. Among the attractions are the mirages that are frequent here, which have been the origin of the "Phantom City," which early explorers fancifully described as upon Glacier Bay. Other huge glaciers also enter these waters, among them the Grand Pacific, Hugh Miller and Gelkie Glaciers.

THE KLONDYKE AND CAPE NOME.

Northward from the Gastineaux Channel stretches the grand fiord of the Lynn Canal for sixty miles. Snow-crowned mountains surround it, from whose sides many glaciers descend. At the upper end this Canal divides into two forks—the Chilkoot and Chilkat Inlets, at 59° north latitude. This begins the overland route to the Klondyke gold region, and upon the eastern inlet, Chilkoot, are on either bank the two bustling little towns that have grown out of the Klondyke immigration—Skaguay on the eastern and Dyea on the western shore. Each of them has three to four thousand people, with hotels, lodging-places and miners' outfitting shops. Dyea is the United States military post, with a garrison, and here begin the trails across the mountain passes to the upper waters of the Yukon. A railway is constructed over White's Pass to Bennett Lake, and is now the chief route of travel. Pyramid Harbor and Chilkat with salmon-canning establishments are on Chilkat Inlet. Beyond White's Pass, which crosses the international boundary, the land descends in British America to the headwaters of the Yukon River, which are navigated northwest to Dawson and Circle City and other mining camps of the Klondyke region, where the prolific gold-fields have had such rich yields, there having been $40,000,000 gold taken out in two years. The Yukon flows a winding course westward to Norton Sound on the Bering Sea, discharging through a wide-spreading delta. The port of St. Michaels is to the northward. There are two routes to the Klondyke from San Francisco—via Skaguay and overland a distance of about twenty-three hundred miles, and via St. Michaels and up the Yukon forty-seven hundred miles.

The Alaskan coast beyond the Muir Glacier is bordered by the great St. Elias mountain range, rising in Mount Logan to nineteen thousand five hundred and thirty-nine feet, the highest of the Rockies, and in Mount St. Elias nearer the coast to eighteen thousand and twenty-four feet. From the broad flanks of St. Elias the vast Malaspina Glacier flows down to Icy Bay on the Pacific Ocean. There are mountains all about this region, which the official geographers are naming after public men, among them being Mount Dewey. To the westward the vast Alaska peninsula projects far out, dividing the Pacific Ocean from the Bering Sea, terminating in the Fox Islands, of which Ounalaska is the port, and having the Aleutian Islands spreading beyond still farther westward. It is a remarkable fact, indicating the vast extent of the United States, that the extremity of the Aleutian group is as far in latitude westward from San Francisco as the Penobscot River and coast of Maine are eastward. To the north is the Bering Strait, having the Russian East Cape of Siberia projecting opposite to the Alaskan Cape Prince of Wales to guard the passage into the Arctic Ocean. Here, upon the southern shore of the protruding end of Alaska, and fronting Norton Sound up almost under the Arctic Circle, is the noted Cape Nome, the latest discovered gold-field, about a hundred miles northwest of St. Michaels. Fabulous golden sands are spread out in gulches and on the beaches, and Nome City has become quite a settlement. This is the latest El Dorado to which such an enormous rush of prospectors and gold-hunters was made in the early spring of 1900, many thousands filling up every available steamer that could be got to sail northward. The prolific output of these gold-bearing sands is said to exceed the Klondyke in its yield, and this will be the golden Mecca until somebody crosses over into Siberia or goes up nearer the North Pole, and finds there a new deposit of treasure. Already it is said that Nome City spreads practically for twenty miles along the sea-beach, and that the industrious miners are getting much gold by dredging far out under the sea, and expect to secure fifty millions annually from this remote but extraordinary region.

Nome City, like everywhere else that the hardy American pioneer raises the flag for discovery and settlement, has its newspaper, the Gold Digger, and this enterprising publication thus poetically describes the new El Dorado of the Arctic seas, the "Golden Northland":

"High o'er the tundra's wide expanse,

Mount Anvil lifts its God-wrought crown,

Bold guardian of a shining shore,

That's ever garbed in golden gown.

"Here nature, lavish with her store

To those of nerve and strong of hand,

Outpours a glittering stream of wealth

To all the miners of the land.

"The ledge-ribbed hills on ev'ry side,

To feasts of ore invite mankind,

Nor Bering's waves may bar the way

To golden courses milled and mined.

"The fresh'ning breezes from the Pole

Bear far the miners' joyous cry,

As point of pick turns back the sod

'Neath which the glist'ning nuggets lie.

"Here may the rover of the hills

Find fickle Fortune's long sought stream,

And revel in the boundless wealth

That's ever been his life-long dream.

"O, tundra, beach and lavish stream!

O'er thee a world expectant stands;

With Midas measure may'st thou fill

The myriad eager, outstretched hands."

Wonderful is our latest American Continental possession—the rich territory of Alaska. Limitless are its resources, unmatchable its possibilities. One of its admirers thus sounds its praises: "In scenery, Alaska dwarfs the world. Think of six hundred and seventeen thousand square miles of landscape. Put Pike's Peak on Mount Washington or Mount Mitchell and it would hardly even up with Mount Logan. All the glaciers of Switzerland and the Tyrol dwindle to pitiful summer ice-wagon chunks beside the vast ice empires of Glacier Bay or mighty Malaspina. Think of a mass of blue-green ice forty miles long by twenty-five miles wide, nearly the size of the whole State of Rhode Island, and five thousand feet thick, glittering resplendently in the weird, dazzling light of a midnight sun. Imagine cataracts by scores from one thousand to three thousand feet high; ocean channels thousands of feet deep, walled in by snow-capped mountains; sixty-one volcanoes, ten of them still belching fire and smoke; boiling springs eighteen miles in circumference, used by hundreds of Indians for all their cooking; schools of whales spouting like huge marine fire-engines and tumbling somersaults over each other like big lubberly boys, weighing one hundred to two hundred thousands of pounds each; rivers so jammed with fish that tens of thousands of them are crowded out of the water high up on the shore; and woods alive with elk, moose, deer, bear, and all sorts and conditions of costly fur-clad aristocrats of the fox, wolf, lynx and beaver breeds. Growing country, this of ours."

PUGET SOUND TO SAN FRANCISCO.

Captain George Vancouver, already referred to, who named Vancouver Island, had among his officers a Lieutenant Puget. From him came the name of Puget Sound, stretching eighty miles southward from Vancouver Island and the Strait of Juan de Fuca into Washington State, ramifying into many bays and inlets, and having numerous islands. The Sound covers two thousand square miles and has eighteen hundred miles of coast line, being a splendid inland sea with admirable harbors. Its peculiar configuration makes very high tides, sometimes reaching twelve to eighteen feet. At the entrance near the head of the Strait of Juan de Fuca is the United States port of entry, Port Townsend, in a picturesque situation with the large graystone Custom House on the bluff, a conspicuous structure. Three formidable forts, Wilson, Casey and Flagler, guard the entrance from the sea. Opposite, on the eastern shore of the Sound, is Everett with a fine harbor, the terminal of the Great Northern Railway. To the northwest, a sentinel outpost of the Cascade Range, rises Mount Baker, nearly eleven thousand feet high. To the southward, on the circling shores of Elliott Bay, is Seattle, named after an Indian chief and founded in 1852, built on a series of terraces rising above the water, the chief commercial city of Puget Sound, and having sixty thousand population. On the southeastern arm of the Sound, called Commencement Bay, is Tacoma, the terminal of the Northern Pacific Railway, with fifty thousand people. Its Indian name comes from its great lion, Mount Tacoma (sometimes called Rainier), a giant of the Cascades, rising fourteen thousand five hundred and twenty feet, and in full view to the southeast of the city. Fourteen glaciers flow down its sides, the chief one, Nisqually Glacier, seven miles long, on the southern slope, being considered the finest on the coast south of Alaska. This mountain, like other peaks of the Cascades, is an extinct volcano, its crater still emitting sulphurous fumes and heat. Mount St. Helens, not far away, which was in eruption in 1898, is regarded as the most active volcano in the range, its massive rounded dome rising over nine thousand feet. Across on the southwestern shore of Puget Sound is the capital of Washington State, Olympia, with five thousand people.

Portland, the chief town of Oregon, is but a short distance south of Puget Sound, on the Willamette River, twelve miles from its confluence with the Columbia, and at the head of deep-sea navigation, one hundred and ten miles from the ocean. This is the leading business centre of the Pacific northwest, having seventy thousand people and extensive trade. It is finely situated, and from the heights on its western border is given a most superb view of the Cascades, the range grandly stretching over a hundred miles. The Mazama Club of earnest mountain explorers at Portland have done much to make known to the world the scenery and grandeur of these attractive mountains. Fifteen miles up the Willamette, at Oregon City, are the Falls, where that river descends forty feet in a splendid horseshoe cataract, displaying great beauty and furnishing valuable power. To the southward is Salem, on the Willamette, the capital of Oregon, having five thousand population. The "Oregon trail," as the route from San Francisco into this region was called, ascends the Rogue River, so named from the Indians of the region, crosses the Siskiyou Mountain, and descends on the southern side to the headwaters of the Sacramento. To the eastward, near the California boundary, high up in the Cascades, is the strangely constructed Crater Lake. It is at over sixty-two hundred feet elevation, and occupies an abyss produced by the subsidence of an enormous volcano, being six miles long and four wide. A perpendicular rocky wall one to two thousand feet high entirely surrounds it, and the water, without outlet or apparent inflow, is fully two thousand feet deep and densely blue in color. In the centre is Wizard Island, rising eight hundred and fifty feet, an extinct volcanic cone, thus presenting one crater within another. The district containing this wonderful lake has been made a reservation called the Oregon National Park. Some distance to the southward, the whole country being mountainous and the lower slopes covered with forests of splendid pines, is the grand snow-covered dome of Mount Shasta, one of the noblest of the Cascades (in California called the Coast Range), rising fourteen thousand four hundred and forty feet, a huge extinct volcano, having a crater in its western peak twenty-five hundred feet deep and three-quarters of a mile wide. Beyond, the Sacramento Valley stretches far away southward, passing Chico and Marysville, to Sacramento. It was to the eastward, near Coloma, that the first discovery of California gold was made in February, 1848, on the farm of Colonel Sutter, the county having been appropriately named El Dorado.

SAN FRANCISCO BAY AND CITY.

The San Joaquin and Sacramento Rivers, having united, flow westward into Suisun Bay, thence by a strait to the circular and expansive San Pablo Bay, which in turn empties into San Francisco Bay. On the strait connecting Suisun and San Pablo Bays is Benicia, where lived the famous pugilist John C. Heenan, the "Benicia Boy," and the immense forge-hammer he wielded is on exhibition there. At the head of San Pablo Bay is Napa, or Mare Island, the location of the Navy Yard. Upon the mainland opposite is Vallejo, whence a railway runs up the fertile Napa Valley, through orchards and vineyards and among mineral springs, to Calistoga. Near here is the strange Petrified Forest, where there are scattered upon a tract of four square miles the remains of a hundred petrified trees. The Bay of San Francisco is a magnificent inland sea, fifty miles long and ten miles wide, connected with the Pacific Ocean by the strait of the Golden Gate, five miles long and a mile wide. The bay is separated from the ocean by a long peninsula, having the city of San Francisco on the inside of its northern extremity. Over opposite, on the eastern shore of the bay, is Oakland, the terminal of the Southern Pacific Railway routes from the East, a city of fifty thousand people, named from the numerous live-oaks growing in its gardens and along the streets. It has extensive manufactures and a magnificent view over the expansive bay and city of San Francisco and the distant Golden Gate, where the enclosing rocky shores can be seen rising boldly, the northern side to two thousand feet height. In the Oakland suburbs is Berkeley, where are some of the College buildings of the University of California, founded in 1868 and having twenty-three hundred students, many of them women. The attractive grounds cover two hundred and fifty acres, and the endowments exceed $8,000,000. South of Oakland is the pleasant suburban town of Alameda. On the western shore of the bay, south of San Francisco, is Menlo Park, a favorite place of rural residence for the wealthy San Francisco people, having many handsome villas and estates with noble trees. Here is Palo Alto or the "tall tree," taking its name from a fine redwood tree near the railway, an estate of over eight thousand acres, which is the location of the noted Leland Stanford, Jr., University. This is the greatest educational endowment in America, having a fund of over $30,000,000, the gift of Senator and Mrs. Leland Stanford in memory of their only son. The University has twelve hundred students, many being women. The buildings, which in a manner reproduce the architecture of the ancient Spanish Missions, are of buff sandstone, surmounted by red-tiled roofs, picturesquely contrasting with the oaks and eucalyptus trees which are so numerous and the many tropical plants that have been brought there. The Palo Alto estate is one of the great California stock-farms.

Two Franciscan monks in 1776 founded on this famous bay the Indian Mission of San Francisco de Assis, often called the Mission Dolores, and in course of time there started upon the shore, which had much wild mint growing about, the village of Yerba Buena, named from it the "good herb." Just about the time this lonely little village had got a small Spanish population and built a few houses, Richard Henry Dana came into the bay in 1835 on the voyage which he so pleasantly recounts in Two Years Before the Mast. He then prophetically wrote: "If ever California becomes a prosperous country, this bay will be the centre of its prosperity. The abundance of wood and water; the extreme fertility of its shores; the excellence of its climate, which is as near to being perfect as any in the world; and its facilities for navigation affording the best anchoring-grounds in the whole Western coast of America, all fit it for a place of great importance." In the summer of 1846, during the Mexican War, the American navy made various important occupations on the California coasts, and a man-of-war came into San Francisco Bay and took possession for the United States. The next year the name of the village was changed to San Francisco. There were about six hundred inhabitants here when gold was discovered in 1848, and most of them at once left for the gold-fields; but the favorable location for trade soon attracted a large population and an extensive commerce. The young city had the usual mishaps from fires, suffering from a half-dozen serious conflagrations in its early career; while the peculiar character of the population made it then so lawless that twice the better element had to take summary control of the municipal government by "Vigilance Committees," who did not hesitate to promptly execute notorious criminals. There are now three hundred and fifty thousand people, the heterogeneous population including almost every nationality in the world.

San Francisco is in a fine situation on the shore of the bay and the steep hills to the westward, and is gradually spreading across the peninsula towards the ocean. It is, in fact, built on a succession of hills, of which a group extends westward from the bay, varying in height from less than two hundred to over nine hundred feet. Conspicuous among them are the Telegraph Hill, Nob Hill, Park Peak, the Mission Peaks and others. For the purpose of readily climbing these hills, the cable street railway and its peculiar "grip" were invented and first put into successful operation, and a British visitor writes of San Francisco that "one of its most characteristic sights is the cable cars crawling up the steep inclines like flies on a window-pane." The country around is treeless, with little fertile land, owing to the copious rivers of sand which steadily flow over it, being blown from the seashore by the strong westerly trade-winds. Thus have naturally come the historical San Francisco "sand lots," the scene of public meetings and not infrequent disturbances in former times. An immense amount of grading, cutting down hills, filling gullies, and reclamations of overflowed lands was necessary in building the city; and over $50,000,000 has been expended in improving the site which, as nature fashioned it, was so illy fitted for a city. The great charm is the spacious bay environed by mountains, furnishing such an admirable harbor, and across it the ferry steamers ply in all directions. Upon it, guarding the Golden Gate entrance, are Alcatraz Island, Goat Island and Angel Island, strongly fortified, while Fort Mason is on the heights north of the city, overlooking the famous strait. The charming waters of the noble bay are thus rhythmically described by Ada Abbott Dunton:

"How beautiful the waters of the Bay

Lie shimmering, gem-embossed and turquoise-blue,

Rippling and twinkling! Emerald shores in view

Reflected from its surface. This calm day

Utters no note of discord. Far away

And overhead, the tireless, winged sea-mew

Skims languidly the air, sun-warmed anew

And freshly blown with each succeeding day.

"O San Francisco Bay! Upon thy shore,

What wondrous argosies are anchored here!

What giant masts are silhouetted fair

'Gainst the eternal blue which bendeth o'er,

As though a Titian hand were carving clear,

Majestic monuments in upper air."

The great "Ferry Depot," an ornamental structure with a high tower, is the centre of the San Francisco harbor front, whence the steamboats ply across the spacious bay. From this, the chief business highway, Market Street, stretches far southwest to the Mission Peaks, rising over nine hundred feet and nearly four miles away. Northward, Kearney Street with the leading stores extends past Telegraph Hill, rising almost three hundred feet and giving a magnificent outlook from the summit. Upon Market Street, in Yerba Buena Park, is the magnificent City Hall, completed in 1896 at a cost of over $4,000,000 and containing a library of one hundred thousand volumes. There is a Branch Mint of the United States which coins much of the gold mined on the Pacific Slope. The ancient church of the Mission Dolores, built of adobÉ is still preserved with the little churchyard. Upon Nob Hill are many of the finest residences, while to the northwestward is the Presidio, originally the Mexican and now the United States Military Reservation, adjoining the Golden Gate for some four miles, and a park of almost three square miles where troops are garrisoned. Here the military band plays in the afternoon and the walks and drives afford beautiful views. The Chinese Quarter of San Francisco, where there is a population of about fifteen thousand, is a characteristic feature, the inhabitants swarming in tall tenements divided by narrow alleys. Its attractions, however, are of a kind usually prepared with a view to induce contributions from visitors.

THE GOLDEN GATE.

The Golden Gate Park, a half-mile wide, stretches from the city three miles to the ocean shore, the western extremity being mainly the sand-dunes of the coast, while the eastern portions have been reclaimed, improved and planted with trees. Here are tasteful monuments. The author of the Star-Spangled Banner, Francis Scott Key, is commemorated by Story, and the Spanish discoverer of the Pacific Ocean, Vasco NuÑez de Balboa, by Linden, unveiled in 1898. Here also rises Strawberry Hill, an eminence giving an unrivalled outlook. Adjoining the park are the great cemeteries of the city, Laurel Hill and the Lone Mountain, with others, the Presidio being to the northward. To the westward, on the ocean front, is the historic landmark of the coast—Point Lobos, or the "wolves"—having on its elevated surface the Sutro Heights, where the sandhills have been converted into a fine estate and garden, and out in the sea, a cable's length from shore, are the celebrated Seal Rocks, which are nearly always covered with seals basking in the sun. Some are very large, and their movements are quite interesting, their curious barking being distinctly heard above the roar of the surf. To the northward of Point Lobos is the ocean entrance to the Golden Gate. The portals are a mile apart, and seen from the sea its guardian heights rise two thousand feet on the left hand, stretching up to the peak of Tamalpais to the northward. On the right hand the heights are lower, but still lofty. The slopes are bare and sandy, and between them within the strait can be distinctly seen the island fortress of Alcatraz, guarded on the one hand by Goat Island and on the other by the high green slopes of Angel Island. Up on the Presidio proudly floats high above the shore the American flag standing out in the breeze. Behind it is the great city. This Golden Gate seen from within, looking westward, is a narrow pass, giving a vista view of the broad Pacific, its waves rolling towards us thousands of miles from the distant shores of China and Japan.

Here ends this pleasant recital. The desire has been to give an idea of the vast and wonderful land we live in, and to impress the noble and patriotic thought of Thoreau's so essential to all of us: "Nothing can be hoped of you, if this bit of mould under your feet is not sweeter to you than any other in the world." We have travelled over this broad land of ours from the tropics to the Arctic Sea, and from the Atlantic to the Pacific, and as our journey closes, with Whittier can sing:

"So shall the Northern pioneer go joyful on his way;

To wed Penobscot's waters to San Francisco's Bay;

To make the rugged places smooth, and sow the vale with grain;

And bear, with Liberty and Law, the Bible in his train:

The mighty West shall bless the East, and sea shall answer sea,

And mountain unto mountain call, Praise God, for we are free!"

THE END.

                                                                                                                                                                                                                                                                                                           

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