part of the Zarafshan valley, which is connected to
the coastal zone of Khorezm, is represented by the
Kyzylkum formations, the Zarafshan river and its
tributaries, large and small water basins. Its northern,
north-eastern
and
north-western
regions
are
mountainous. Only the southern part has a plain on
the surface of the territory. It is the eastern
geographical feature that is reflected in the Tashkent
Valley. In other words, the Tashkent-Mirzachul
lowland is a mountainous region located in the
middle part of the Syrdarya, in the lower part of the
Chirchik and Akhangaron valleys. The geographical
position and paleography and ecology of the valley
are determined by the Chirchik and Akhangaron
valleys.
The Fergana Valley stands out in the
manifestation of the geographical features of
Uzbekistan. The Fergana Valley is located between
the Tianshan and Alay Mountains, surrounded by
mountains
and
has
a
unique
geographical
environment, natural conditions and ecology (12)
CONCLUSION The content of the above historical data
allows us to conclude the following:
- The final conclusions about the
paleogeography and ecology of the first Stone Age,
which is the first stage in the history of the primitive
community system.
-People of the Early Stone Age are located
in areas adjacent to the shores of caves, springs and
reservoirs
in
certain
areas
with
favorable
geographical environment, climate and ecology. As a
result, ethnic processes have defined geographical
areas.
