Epra international Journal of Socio-Economic and Environmental Outlook (seeo) issn: 348-4101 Volume


part of the Zarafshan valley, which is connected to



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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 

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. 


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