RESEARCH METHODS In the literature of the XX century and the
beginning of the XX century, the methods of
scientific and objective coverage of the first stages of
the ancient Stone Age in the territory of Uzbekistan,
historical
analysis,
chronological
sequence,
generalization are used.
CONCLUSIONS AND FEEDBACK The article analyzes the geographical
location of the territory of Uzbekistan under the
influence of geological processes that took place in
the first stage of the ancient Stone Age, as well as
data recorded in the geological-geographical and
archeological literature. The map of natural
geography of Central Asia shows that the main
irrigated agricultural area of Uzbekistan is located
between the Syrdarya and Amudarya rivers, so it
differs from other historical and geographical areas
through the Kyzylkum plain. The right bank of
Khorezm is connected with the southern coast of the
Aral Sea from Shurakhan to the Kyzylkum desert.
Paleozoic and Cenozoic era where the historical
processes took place in the last Cenozoic era are of
great
importance.
According
to
geological
discoveries, 4-3 million years ago there was lowland
in the Kyzylkum-Aral and Sariqamish-Aral regions,
which was part of the Great Turan Plain. {2} The
importance
of
geological
geography
and
archeological sources in the study of the location,
geography and ecology of primitive hunting in the
territory of Uzbekistan in the Early Stone Age is
enormous. It is possible to involve clarifications in
the scientific solution of ecological problems.
According to the results of geological and
geographical research, there are differences in the
geographical location and ecological processes of
Uzbekistan. Based on the results of archeology, it is
important to study the relationship between man and
the environment, peleogeography and anthropogenic
landscape factors. Certain regions of Uzbekistan have
allowed men to settle and the geographical features,
climate and favorable ecology have allowed them to
work and live there.
According to historical data, in the
Quaternary period, the Central Asian region was flat
during the Danube, Gyunts, and Gyunts-mindel
periods, and was covered with ice in the Pleistocene
(Glaciers) Mindal, Mindel-riss, Riss, Riss-vyurm,
and Vyurm stages (500-10 thousand years). (3). The
geographical location of the natural and economic
regions of Uzbekistan consisted of mountainous and
flat areas. An archeological expedition of various
names has been organized in cooperation with the
Center and scientific centers of Uzbekistan. Materials