The New Stone Age in Northern EuropeTyler, John M. (John Mason)
History
The New Stone Age in Northern Europe
Tyler, John M. (John Mason)
Stone age -- Europe
Even during epochs of glacial advance conditions in France and in the
German zone must have been better than we should expect. Some kind of
grazing or browsing pasturage must have been rich and abundant to
support large animals like the reindeer or even the woolly mammoths
characteristic of the second and third glacial epochs, which furnished
abundant food for prehistoric hunters. Farther south the glacial epochs
may well have been times of heavy rainfall, transforming the Sahara
desert and the dryer steppes and plateaus of Asia into veritable
gardens.
The retreating ice left behind it a land covered with rocks, clays,
gravels, and sands brought by the glaciers and their streams. Here and
there basins had been gouged out where lakes or ponds long remained--as
in Maine and Minnesota to-day--to be later drained, or, if shallow, to be
overgrown with sphagnum and changed into great bogs. Scattered thickets
of shrubs and stunted hardy trees, poplars, willows, and others
occurred. In sheltered and well-drained valleys and mountainsides the
trees grew larger and even forests began to appear. This tundra
landscape still characterizes wide areas of northern Canada and
Siberia.[19]
The tundra was followed by steppe conditions, where elevation of land to
the north and northwest had cut off the tempering oceanic winds. The
climate was harsh, dry, continental, with cold winters and hot summers.
The winds carried great storms of dust and piled it up in drifts in
valleys and on suitably situated mountainsides in the form of loess, so
important to the future agricultural development of Europe, though its
most massive accumulation is seen in China, which received and held the
driftings from the great elevated plains of central Asia. As the climate
became moister, if the temperature did not fall too low, steppe finally
gave way to the meadow and forest of modern Europe. Tundra, steppe, and
forest had each its special types of animal as well as plant life. The
characteristic tundra animal is the reindeer, though musk-ox, woolly
mammoth, and others were wide-spread at this time. The peculiar steppe
animal is the horse. The characteristic forest and meadow animals are
the deer and their allies; the wolf and bear; the wild boar and cattle
seem to be at home in forest and glade and along the streams.
In France, where there was far less glaciation, the succession of
tundra, steppe, and forest is less apparent. Here we find a mingling of
varied forms which have come in from very different regions, driven from
their original homes by change of climate or drawn by favorable
conditions.
Public-domain text, read in full here on John Shaqi.
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