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coralline could not have fixed itself; if the Crania had been

covered up with chalk mud; and could not have lived had itself been

so covered it follows; that an inch of chalk mud could not have

accumulated within the time between the death and decay of the soft

parts of the sea…urchin and the growth of the coralline to the full

size which it has attained。  If the decay of the soft parts of the

sea…urchin; the attachment; growth to maturity; and decay of the

Crania; and the subsequent attachment and growth of the coralline;

took a year (which is a low estimate enough); the accumulation of

the inch of chalk must have taken more than a year: and the deposit

of a thousand feet of chalk must; consequently; have taken more

than twelve thousand years。



The foundation of all this calculation is; of course; a knowledge

of the length of time the Crania and the coralline needed to attain

their full size; and; on this head; precise knowledge is at present

wanting。  But there are circumstances which tend to show; that

nothing like an inch of chalk has accumulated during the life of a

Crania; and; on any probable estimate of the length of that life;

the chalk period must have had a much longer duration than that

thus roughly assigned to it。





Thus; not only is it certain that the chalk is the mud of an

ancient sea…bottom; but it is no less certain; that the chalk sea

existed during an extremely long period; though we may not be

prepared to give a precise estimate of the length of that period in

years。  The relative duration is clear; though the absolute

duration may not be definable。  The attempt to affix any precise

date to the period at which the chalk sea began; or ended; its

existence; is baffled by difficulties of the same kind。  But the

relative age of the cretaceous epoch may be determined with as

great ease and certainty as the long duration of that epoch。



You will have heard of the interesting discoveries recently made;

in various parts of Western Europe; of flint implements; obviously

worked into shape by human hands; under circumstances which show

conclusively that man is a very ancient denizen of these regions。



It has been proved that the old populations of Europe; whose

existence has been revealed to us in this way; consisted of

savages; such as the Esquimaux are now; that; in the country which

is now France; they hunted the reindeer; and were familiar with the

ways of the mammoth and the bison。  The physical geography of

France was in those days different from what it is nowthe river

Somme;'69' for instance; having cut its bed a hundred feet deeper

between that time and this; and; it is probable; that the climate

was more like that of Canada or Siberia; than that of Western

Europe。



The existence of these people is forgotten even in the traditions

of the oldest historical nations。  The name and fame of them had

utterly vanished until a few years back; and the amount of physical

change which has been effected since their day; renders it more

than probable that; venerable as are some of the historical

nations; the workers of the chipped flints of Hoxne or of Amiens '70'

are to them; as they are to us; in point of antiquity。



But; if we assign to these hoar relics of long…vanished generations

of men the greatest age that can possibly be claimed for them; they

are not older than the drift; or boulder clay; which; in comparison

with the chalk; is but a very juvenile deposit。  You need go no

further than your own sea…board for evidence of this fact。  At one

of the most charming spots on the coast of Norfolk; Cromer; you

will see the boulder clay forming a vast mass; which lies upon the

chalk; and must consequently have come into existence after it。

Huge boulders of chalk are; in fact; included in the clay; and have

evidently been brought to the position they now occupy; by the same

agency as that which has planted blocks of syenite from Norway side

by side with them。



The chalk; then; is certainly older than the boulder clay。  If you

ask how much; I will again take you no further than the same spot

upon your own coasts for evidence。  I have spoken of the boulder

clay and drift as resting upon the chalk。  That is not strictly

true。  Interposed between the chalk and the drift is a

comparatively insignificant layer; containing vegetable matter。

But that layer tells a wonderful history。  It is full of stumps of

trees standing as they grew。  Fir…trees are there with their cones;

and hazel…bushes with their nuts; there stand the stools of oak and

yew trees; beeches and alders。  Hence this stratum is appropriately

called the 〃forest…bed。〃



It is obvious that the chalk must have been up…heaved and converted

into dry land; before the timber trees could grow upon it。  As the

boles of some of these trees are from two to three feet in

diameter; it is no less clear that the dry land this formed

remained in the same condition for long ages。  And not only do the

remains of stately oaks and well…grown firs testify to the duration

of this condition of things; but additional evidence to the same

effect is afforded by the abundant remains of elephants;

rhinoceroses; hippopotomuses and other great wild beasts; which it

has yielded to the zealous search of such men as the Rev。 Mr。 Gunn。'71'



When you look at such a collection as he has formed; and bethink

you that these elephantine bones did veritably carry their owners

about; and these great grinders crunch; in the dark woods of which

the forest…bed is now the only trace; it is impossible not to feel

that they are as good evidence of the lapse of time as the annual

rings of the tree…stumps。



Thus there is a writing upon the walls of cliffs at Cromer; and

whoso runs may read it。  It tells us; with an authority which

cannot be impeached; that the ancient sea…bed of the chalk sea was

raised up; and remained dry land; until it was covered with forest;

stocked with the great game whose spoils have rejoiced your

geologists。  How long it remained in that condition cannot be said;

but 〃the whirligig of time '72' brought its revenges〃 in those days

as in these。  That dry land; with the bones and teeth of generations

of long…lived elephants; hidden away among the gnarled roots and

dry leaves of its ancient trees; sank gradually to the bottom of

the icy sea; which covered it with huge masses of drift and boulder

clay。  Sea…beasts; such as the walrus; now restricted to the

extreme north; paddled about where birds had twittered among the

topmost twigs of the fir…trees。  How long this state of things

endured we know not; but at length it came to an end。  The upheaved

glacial mud hardened into the soil of modern Norfolk。  Forests grew

once more; the wolf and the beaver replaced the reindeer and the

elephant; and at length what we call the history of England dawned。



Thus you have within the limits of your own county; proof that the

chalk can justly claim a very much greater antiquity than even the

oldest physical traces of mankind。  But we may go further and

demonstrate; by evidence of the same authority as that which

testifies to the existence of the father of men; that the chalk is

vastly older than Adam himself。



The Book of Genesis informs us that Adam; immediately upon his

creation; and before the appearance of Eve; was placed in the

Garden of Eden。  The problem of the geographical position of Eden

has greatly vexed the spirits of the learned in such matters; but

there is one point respecting which; so far as I know; no

commentator has ever raised a doubt。  This is; that of the four

rivers which are said to run out of it; Euphrates and Hiddekel '73'

are identical with the rivers now known by the names of Euphrates

and Tigris。



But the whole country in which these mighty rivers take their

origin; and through which they run; is composed of rocks which are

either of the same age as the chalk; or of later date。

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