The Meeting-Place of Geology and HistoryDawson, John William, Sir
Religion
The Meeting-Place of Geology and History
Dawson, John William, Sir
Deluge; Prehistoric peoples
I should, perhaps, have noticed here the worked flints found so
abundantly in some parts of the south of England, which have long
attracted the attention of collectors, and have in some cases been
referred to glacial or pre-glacial times. I believe, however, they are
all really post-glacial, though in some cases belonging to the earliest
portion of that period.[13]
[13] Prestwich on 'Ightham Beds,' _Journ. Geol. Soc._, 1893; Dawkins,
_Journ. Anthrop. Soc._, 1894.
We may close the present chapter by presenting to the eye in a tabular
form the series of events included in the pleistocene and modern periods
of the great cenozoic time.
LATER CENOZOIC, OR TERTIARY PERIOD
(_In Ascending Order, or from the Older to the Newer_)
Newer Pliocene.--A continental period of long duration, elevated land,
much erosion, much volcanic action.
Pleistocene.--Irregular elevation and depression of the land, ending in
wide submergence with cold climate. Glaciers on all mountains near to
coasts and ice-drift over submerged plains. Glacial period, with an
inter-glacial mild period in the middle and great submergence of the
continents toward the close.
Anthropic.--_Palanthropic_, or post-glacial, in which the land emerges
and attains a very wide extension, and is inhabited by a varied
mammalian fauna. Man appears in Europe, Asia, and North Africa.
Terminated by a recurrence of cold and great subsidence, deluging all
the lower lands. _Neanthropic._--Area of continents smaller than in the
previous period. Surviving races of men and species of animals repeople
the world. Modern races of men and modern animals.
CHAPTER IV
THE PALANTHROPIC AGE[14]
[14] Called by some 'Palæolithic,' from the use of implements like that
figured on p. 41.
We have now to inquire more particularly what we can learn as to the
earliest men known to us, those who appeared in Western Asia and Europe
at the close of the glacial period, when the cold had passed away and a
genial climate had succeeded, and when the continents of the northern
hemisphere had attained to their largest dimensions, were clothed with a
rich vegetation and tenanted by an abundant mammalian fauna, including
many large and important creatures now extinct.
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