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
Geikie describes loess as typically a "fine-grained, yellowish,
calcareous, sandy loam, consisting very largely of minute grains of
quartz with some admixture of argillaceous and calcareous matter."[48]
It is for the most part a wind-blown deposit. It is widely developed
over low-lying regions, but sweeps up to heights of 200 to 300 feet and
more above the bottoms of the great river valleys. Again, in many places
we find it heaped up under the lee of hills, the exposed windward slopes
of which bear no trace of it. Wherever there is loess we are likely to
find the remains of steppe plants and animals. The ancient steppe area
which generally covers, and probably extends considerably beyond, the
loess district, is the region occupied by most of the primitive
settlements. Even to-day it is less wooded than the rest of northern
Europe. Such steppe regions in the North German plain are the great
diluvial river terraces, especially the terraces of the Saale and Elbe
and the eastern edge of the Harz Mountains; in South Germany the lower
Alpine "Vorland" from Switzerland to lower Austria, the uplands of
Suabia and Franconia, the valleys of the Main and Neckar, and much of
northern Bohemia. These steppe regions of Germany, northern Austria, and
Switzerland extended southeastward in a zone following the Danube,
widening out in the great Hungarian plain into the vast steppe region
extending eastward from the Black Sea or Pontus. From this Pontic steppe
a band of more or less open country extended northward along the
Carpathians until it almost or quite joined the open regions of the Elbe
and along the Harz. A farther extension of this same band seems to have
opened the way from the Harz region through northwest Germany into
Belgium and northern France, and very probably into Brittany. We see at
once the importance of these long lines of open or thinly forested
country to the immigrations and settlement of Neolithic peoples.
Periodical floods or other conditions kept open many river valleys,
whose importance we shall estimate in a later chapter. All this land,
except the uplands of Suabia and Franconia, and some similar areas, was
comparatively fertile, the loess areas particularly so, and suited to a
primitive agriculture.
Public-domain text, read in full here on John Shaqi.
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