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

------------------------------------------------------------------------------------------------------------------------------------------------------ 
EPRA International Journal of Socio-Economic and Environmental Outlook (SEEO) ISSN: 2348-4101 
Volume: 9 | Issue: 2| February 2022 | SJIF Impact Factor: 7.426 | Journal DOI: 10.36713/epra0314 | Peer-Reviewed Journal 
2022 EPRA SEEO | www.eprajournals.com | Journal DOI URL: https://doi.org/10.36713/epra0314
58 
obtained during excavations during the field 
operations carried out by the groups in our country, 
played an important role in covering the location of 
mankind in the Early Stone Age, daily life and the 
history of ethnic processes. It is known from the 
results of archeological research that in the territory 
of our country, the mountains and foothills are 
located around the springs. 
Excavations in Uzbekistan in the early 
Stone Age since the 1960s have uncovered 1 million-
year-old artifacts from hunters who practiced daily 
around a spring on the left bank of the Kyzylolma 
River south of the Chatkal Mountains in the 
Akhangaran Valley of the Tashkent oasis. The results 
of archeological research show that the area around 
Kulbulok is open - flat, ecologically friendly, and the 
spring is rich in organic matter. In the 1980s, U. 
Islamov carried out excavations in the Selungur cave 
(length 120, width 34, height 25 m) located in the 
village of Haydarkon, Fergana Valley. The tools and 
anthropological items found in the excavations 
belong to the Kuyi stage of the Ashel period. 
According to archeological literature, in the territory 
of Navoi region in the settlements of Uchtut, Ijond 
and Vaush were found material objects belonging to 
the Early Stone Age. 
Material objects belonging to the lower 
stage of the Ashel period were found in the cultural 
strata of Esen-2.3, Korayuduy and Churuk-12 
settlements around the real Shakyrakhta basin of 
Ustyurt (7). Researchers note that Central Asia in 
early Paleolithic settlements has also been studied in 
other historical geographical areas. For example, in 
the Vakhsh Valley of Tajikistan, in the area adjacent 
to the eastern shore of the Caspian Sea, Karatangir, 
Yangaja, in Kyrgyzstan, the Onarchadarya River, in 
front of the Karatog in southern Kazakhstan, the 
settlements of the Ashel period were found. (8) 
While the historical and cultural regions that make up 
the territory of Uzbekistan formed as a result of 
geological processes were one of the geographical 
locations, it is not difficult to observe the degree of 
difference in geographical location in natural 
physical cartography. In addition to the main territory 
of Uzbekistan, the paleogeography and ecology of 
the Fergana and Tashkent valleys, as well as the left-
bank serum of Khorezm, are radically different. The 
physical and geographical features of the Ustyurt 
Plateau, located in the western part of Uzbekistan, are 
radically 
different 
from 
the 
historical 
and 
geographical regions. The Ustyurt Plateau is located 
between the Caspian and the Aral Sea, with a total 
area of 200,000 m2 and 70.3 thousand km2 of 
Karakalpakstan; 
It is known from the results of 
archeological research that the climatic conditions 
and ecological situation of the Ustyurt Plateau during 
the Pleistocene glaciers have the potential to be 
assimilated by humans. According to historical data, 
in the lower stage of the Ashel period, the Ustyurt 
Plateau was located along the shores of the rivers, 
which were drained by humans around the 
Shahpakhta basins. So, one of the most important 
geographical features of Ustyurt is the absence of low 
and high mountains, rivers. The geographical 
position and ecology of the land surface, which is 
connected to the Ustyurt Plateau by its southern and 
south-eastern sides, are radically different. 
First, the geographical features of the 
north-western and north-eastern regions were 
explained by the Sultan-Uvays mountain range, the 
Karatag Kokcha mountain range. In the VI-IV 
millennia BC on the right bank there were low-lying 
Kyzylkum barkhans, several reservoirs from Shura 
khan to the Aral Sea. Later paleogeography of the 
Khorezm-Tashhavuz plain was formed here. 
The geographical position of the western