EXTENSION OF THE PREVIOUS TABLE.

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AGE
OF
MAM-
MALS.
POST
TERTIA-
RY.
PLEISTO-
CENE,
or
Quater-
nary.
Recent
and
Pre-
Historic.
Blown Sand and Shingle.
Alluvium and River Deltas.
Burtle Beds of Somerset.
Clay, with Scrobicularia of Pagham, Morecombe, &c.
Submerged Forests of Bristol Channel, &c.
Peat Bogs of Ireland and Peat Beds of England.
Post
Glacial
Raised Beaches.
Cave Deposits Cave Earth and Loam.
Stalagmite and Bone-breccia.
River Gravels, Brick Earths, and Freshwater Clays, with Mammalian Remains.
Gravels of Bedford Levels, Salisbury, and other Old Valley Gravels and Alluvia.
Tufa and Shell-marl.
Glacial Kaimes or Kames of Scotland.
Eskers or Escars of Ireland.
Drift (Upper Boulder Clay or Till, Marine Gravels, Lower Till and Moraines), Scotch and Welsh, Loess of the Rhine, &c.
Pre-
glacial
Forest Bed of Norfolk Shore.
KAINO-
ZOIC,
OR
TERTIA-
RY.
PLIO-
CENE.
Crag Mammaliferous Crag Norwich and Chillesford Crag (Newer Pliocene).
Red Crag
Coralline Crag (Suffolk Crag) (Older Pliocene).
MIOCENE. Leaf Bed of Mull.
Lignite of Antrim.
Bovey Beds, with Lignite.
EO-
CENE.
Upper
Eocene.
Hemp-
stead
Beds
Corbula Beds. Fluvio-Marine Series.
Upper Freshwater and Estuary Marls.
Middle
Lower
Bem-
bridge
Beds
Bembridge Marls.
Limestone.
Middle
Eocene.
Osborne
Beds
St. Helen's Sands.
Nettlestone Grits.
Headon
Beds
Upper Headon Beds.
Middle
Lower
Bagshot
Beds
UpperBagshot Sand.
Middle Barton Clay.
Bracklesham Beds.
Lower Sand and Pipeclay, with Plants.
Lower
Eocene.
London
Tertia-
ries
London Clay and Bognor Beds (Upper London Tertiaries).
Ol shelly, with Bala Limestone, Shale, and Slate)
Llandeilo Llandeilo Flags and Limestone, &c.
Tremadoc Slates.
Lingula
Beds
Lingula Flags. (Primordial Zone of Barrande).
EOZOIC. Cambrian. Cambrian Harlech Grits, &c.
Purple Slates and Grits (St. David's).
Llanberis Grits and Slates.
Longmynd Rocks.
Red Sandstone and Conglomerate (Scotland).
Laurentian Fundamental Gneiss of the Outer Hebrides and of the N.W. coast of Scotland, &c., containing the oldest known fossil, Eozoon Canadense.

                                                                                                                                                                                                                                                                                                           

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