Because the lines and angles of reflection are always equal to the lines and angles of incidence. If a person stands in a direct line before a mirror, the line through which the light travels from him to the mirror is the line of incidence. Incidence—falling on. "Blessed be the Lord, who daily loadeth us with benefits, even the God of our salvation."—Psalm lxviii. The line of reflection is the line in which the rays of light are returned from the image formed in the glass to the eye of the observer. Reflection—a turning back. The angle of incidence is the angle which rays of light, falling on a reflecting surface, make with a line perpendicular to that surface. The angle of reflection is the angle which is formed by the returning rays of light, and a line perpendicular to the reflecting surface. It is always equivalent to the angle of incidence. Take a marble and roll it across the floor, so that it shall strike the wainscot obliquely. Let A in the diagram represent the point from which the marble is sent. The marble will not return to the hand, nor will it travel to the line B, but will bound off, or be reflected, to C. Now B is an imaginary line, perpendicular to the reflecting surface; and it will be found that the path described by the marble in rolling to the surface and rebounding from it, form, with the line B, two angles that are equal. These represent the angles of incidence and of reflection, and explain why the reflection of a person standing at A before a mirror, would be seen by another person standing at C. This simple law in optics explains a great many interesting phenomena, and therefore it should be clearly impressed upon the memory. "And God made two great lights; the greater light to rule the day, and the lesser light to rule the night: he made the stars also."—Gen. i. Because the eye of the observer is in the line of the reflection. They do, but our eyes are not then in the line of the reflection. It is obvious from the foregoing diagram that the evening rays of reflection fall upon the eyes of spectators, while the reflections at noon are so perpendicular that they are lost. Because, when near the horizon, they are brought into comparison with the sizes of terrestrial objects; but when near the meridian they occupy the centre of a vast field of sky, and as there are no objects of comparison surrounding them, they appear smaller. This is one "Reason Why," assigned by some observers. But there is also another reason to be found in the fact that, when the sun or moon is near the horizon, we view it through a greater depth of atmosphere than we do when at "There is no darkness nor shadow of death, where the workers of iniquity may hide themselves."—Job xxxiv. Because light travels only in straight lines, and as the sun descends, the direction of his rays becomes more oblique, thereby causing longer shadows. There are various kinds of natural optical illusions:— The mirage, in which landscapes are seen reflected in burning sands. The fata morgana, in which two or three reflections of objects occur at the same time. The Ærial spectra, or Ærial reflections, &c. The optical illusions above enumerated owe their origin to various "In the morning ye say, it will be foul weather to-day, for the sky is red and lowering."—Matt. xvi. Because the coming and the departing rays of the sun are refracted and reflected by the upper portions of the atmosphere. (See Fig. 13.) The time varies with the refracting and reflecting power of the atmosphere, from twenty minutes to sixty minutes. But the sun's position is usually eighteen degrees below the horizon when twilight begins or ends. The white light of the sun falls upon the earth without change; it is then reflected back by the earth, and as it passes through the atmosphere portions of it are again returned to us, and this double reflection produces a polarised condition of light which imparts to vision the sensation of a delicate blue. (See 549.) Because they reflect back to us the solar beam unchanged. Because the light vapours of the air, which are condensed as the sun sets, refract the rays of light, and produce red rays. The refraction which produces red requires only a moderate degree of density. Because there is a larger amount of vapour in the air, which produces a different degree of refraction, resulting in yellow. Because it shows that the air is heavy with vapours. The refraction that produces yellow requires a greater degree of density. "When it is evening ye say it will be fair weather, for the sky is red."—Matt. xvi. Because the redness shows that the vapours in the air towards the West, or wet quarter, are light, as is evidenced by the degree of refraction of the sun's rays. Because it shows that towards the East, or dry quarter, the air is charged with vapour, and therefore probably at other points the air has reached saturation. Because it shows that the vapours in the air are not very dense. Because it shows that in the West, or wet quarter, the air is saturated to the rain point. Because it shows that the rain is falling in the East, and as that is a dry quarter, it will soon be over. Rainbows are always seen in opposition to the sun. |