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CHAPTER XIII.

66
THE STORY OF THE CRAGS."

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Meaning of the term "crag "—Where these beds are found—
Their number-The Pliocene period-The Coralline, Red,
and Norwich Crags-Suffolk the bed of a tolerably deep sea
-Fauna of the Coralline Crag sea-Ancient sea-urchins-
Where now living-Time since Coralline Crag was formed
-Abundance of mollusca in Coralline Crag sea- -The As-
tartes-Pectunculus Cyprina-Number of species of mol-
lusca An ancient sea-bed, and what it teaches -
"dredging" required "Sea Mats" - Fascicularia — Ex-
tremes in Coralline Crag sea-Marine currents-The oldest
crag-Physical conditions of Pliocene period-Migration of
mollusca southerly-Coralline Crag shells in West Indies-
Ditto in Mediterranean-Thickness of Coralline Crag-How
formed-The Red Crag-Origin of name-]
e-Denudations of
Coralline Crag previous to it-An ancient land surface in
Suffolk and Norfolk-How the "coprolite " beds were formed
Mollusca of the Red Crag - "Southern forms
"Northern" ditto--Refrigeration of climature--Corals--Cowrie
shells-False current bedding in Red Crag-Physical geo-
graphy of ditto-The chalk of Norfolk-A shallow estuary
over site of Norwich-Evidence of river communication-The
Norwich Crag-Its fluvio-marine character-Difference in
fossils from previous crags-Abundance of littoral shells—
Tellina - Mactra - Cerithium - Fresh-water shells - Pla-
norbis, Paludina - Lymnea, &c.-Land-snails -Census of
Norwich crag-Ancient land-animals in Norfolk-The Al-
deby Crag-Its fossils-Increase of "Northerly" mollusca
-Evidence of rigorous climate-The Upper Norwich Crag,
and its lessons-Pliocene and Pleistocene periods-Analy-
zation of shells of crags-Number of extinct species in ditto
-The Be'gium crags-The " Box-stones" of Suffolk-Their
origin-Evidence of a broken-up deposit-Pliocene strata in
Sicily-English shells in ditto-How they came there-
Evidence of volcanic disturbance-Formation of Mount Etna
-Height of Pliocene beds on its flanks-Refrigeration of
climate in northern hemisphere-Preparation for the long
Arctic winter-The introduction of the Glacial epoch 222-237

CHAPTER XIV.

THE STORY OF A BOULDER.

Its restless life-The Glacial period-Extent of Glacial de-
posits "Noah's flood"-The "Northern Drift”—Connection
of Tertiary life-forms with existing species-Sand, gravel,
and clay-Evidence of extreme cold-Recapitulation of slow
refrigeration of climate during Tertiary epoch-The Norfolk
"Forest-bed "-Its fauna and flora-The bed of the German
Ocean once a green wood-Strange animals which lived in
ditto-An Arctic climate introduced into Britain-England
under a wintry sea-Scotland and the north of England
under an ice-sheet-Greenlandic circumstances in Britain-
Description of Greenland glaciers-Icebergs-The Cromer
cliffs-Thickness of Lower Boulder Clay--Iceberg action in
drift-The Atlantic sea-floor-The Gulf stream-Depth to
which England was submerged-How ascertained-Moel
Tryfaen-An old sea-beach on ditto-Re-emergence of the
land-Arctic mollusca in British seas-Raised sea-beaches-
Stranding of ancient Icebergs-Dropping of large boulders
-Migration of Arctic plants-The "chalky" Boulder Clay
-The "Heavy Lands," how formed-Denudation of mud
sheet into valleys-Post-glacial deposits-Ice-grooves and
scratches-England still connected with the Continent-No
straits of Dover yet formed-The Mammoth-The Hairy
Rhinoceros-Land connection with Ireland and England-
The Irish Elk-The Reindeer, Muskdeer-Lemming, &c.
-Arctic plants living on British mountains-How they got
there, and when-Glaciers in Scotland, Cumberland, Lan-
cashire and Wales - The Swiss glaciers - The desert of
Sahara once a sea-English mollusca inhabiting it-For-
mation of the desert sands-A warmer climate sets in-
Migration of existing fauna and flora - Where from -
Separation of Ireland from England-Of England from the
Continent-Bone caves- -Appearance of MAN-Flint im-
plements-Migration and extinction of Mammoth, &c.
-Formation of rich subsoils-Results of the glacial
period.

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"We turned, we wound

About the cliffs, the copses, out and in,

Hammering and clinking, chattering stony names
Of shale and hornblende, rag, and trap, and tuff,
Amygdaloid and trachyte, till the sun

Grew broader towards his death, and fell, and all
The rosy heights came out above the lawns."

TENNYSON'S Princess.

HERE are few rock substances on the surface of the globe which have received more discussion and been more investi

gated than myself. I am somewhat proud of the attention I have received in this respect, for most of the leading geologists of every country, during the last century, have devoted themselves to the task of seeking out my antecedents. I am acquainted with a whole library of books, all most learnedly written, and various of them proving the reverse of the other, which have been penned on this inexhaustible subject. Even yet the question can hardly be regarded as finally settled. Every now

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and then some moot point or another crops up to engage the attention of philosophers, but, thanks to the progress of other sciences, the investigation of these is no longer confined to verbal expressions. It is not a little amusing to remember the hot discussions which were held over me at the beginning of the present century. Philosophers though they professed to be, the disputants resembled political squabblers more than anything else. One set declared I was born amid fire; the other that I was of purely watery origin. Each party believed in their own ipse dixit, and, as nothing could be absolutely proved, backed their own opinions by personalities. Somehow or other the former sect, who were called Plutonists, got the better of the latter, who were termed Neptunists. (The origin of these phrases my listeners will not find it difficult to understand.) But my Plutonic commentators carried their victory too far. Not content with proving that I was not a mere aqueous rock, they proceeded to declare I was nothing more nor less than one which had cooled down from a fused condition, something like iron slag; nay, it was even urged that I was older than any other rock, and the theorists mapped out an idea which existed for many years afterwards, chiefly owing to its remarkable novelty-showing how the whole universe was formerly one great cosmical fog; that this diffused matter was condensed into suns, planets, and satellites, each of which existed for ages in a molten condition, owing

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