THE STATE OF INTERNATIONAL RELATIONSHIP BETWEEN THE FORMATION AND ACTIVITY OF MOUNTAIN GLACES OF UZBEKISTAN

Аннотация

This article describes the systematic study of the base surfaces in the formation and development of mountain glaciers of Uzbekistan and their current state. KEYWORDS: - Glacier, deaf, trog, karling, slope, relief, base, base surface, Piskom, river, erosion, moraine nest, moraine lakes, glacial language. glaciers is clearly felt along the landscapes of the I NTRODUCTION areas occupying the fourth-order base surfaces. These include low average annual temperatures, At the points noted, it is possible to observe the high rainfall, hydrological flow density, diversity irregular scattering of large-sized erratic rocks of flora composition, and the presence of a along with paleomorenous mounds. All of this separate area of rare species growing at high suggests that due to the large scale of the altitudes, such as akkayin, Turkestan spruce. Paleomuzs in ancient times and the cold paleoclimate, the glaciers "fell" to the areas that Basis surfaces are areas of accumulation of covered the surfaces of the fourth order base at hydrological currents formed in accordance with that time. Hence, it can be noted that these the order of river erosion, rivers that form rivers. surfaces appear as accumulation zones of Therefore, the surfaces of the base (Latin for paleomuzs. The direct impact of mountain basis - Geological Dictionary, Volume I, 1955) CURRENT RESEARCH JOURNAL OF PEDAGOGICSISSN 22 – 2767-3278 https://masterjournals.com/index.php/crjp CURRENT RESEARCH JOURNAL OF PEDAGOGICS 2(12): 22-25, December 2021 DOI: https://doi.org/10.37547/pedagogics-crjp-02-12-05 ISSN 2767-3278 ©2021 Master Journals Accepted 09thDecember, 2021 & Published 14thDecember, 2021 have different orders depending on how large the effects of neotectonic movements are clearly the river valleys cover in different areas and how felt. However, against the background of tectonic deep the erosion cuts have left. Glaciers also play movements, we can observe that the topography an important role in the formation of these created by the activity of mountain glaciers also orders, especially at the points where cryogenic plays a leading role in the overall regions are present. Because the formation of geomorphological structure of the region. In hydrological flow is directly related to the particular, the fact that the rivers often have a presence of glaciers for such areas. Our map, flat ridge - the beginning of the troughs, as well “Peculiarities of Development of Mountain as the fact that the bottom of the trough valleys is Glaciers in Uzbekistan along Base Surfaces,” covered with many moraine deposits - gives it a shows that there are four types of base surfaces unique landscape. for the Piskom, Surkhandarya, and Kashkadarya Behind the mound of moraines are often valleys. This means that mountain glaciers and accumulated water basins, which are their derivatives are formed in close connection characteristic of the upper parts of almost all with these base surfaces. This situation manifests trog valleys in the systematic form of small itself in the form of a specific geomorphological moraine lakes. Even in the recent geological pattern, and the areas where the processes of periods, when paleocryogenic conditions erosion, transport and accumulation of mountain prevailed throughout the region, it can be glaciers occur are clearly distinguished by the understood that the second-order areas of the order of the base surfaces. base surfaces were involved as part of the active T transport activities of mountain glaciers. This is HE MAIN RESULTS AND FINDINGS because the trough valleys are composed of The isobasites bordering the first-order base several stems, in which sometimes still surfaces cover areas adjacent to high-altitude longitudinally scattered moraine grooves further watersheds and watersheds, which are complicate the relief. For example, this situation conducive to the formation of mountain glaciers, has been repeatedly observed during our field over which firn fields, tops of glaciers, and observations along the upper reaches of the sometimes deaf-type glaciers are located. As Onaolgansoy, Urungachsoy, Kaptarkumush, mountain glaciers are actively developing Badaqsay rivers. erosion work across these areas, relief patterns The isobasite curve bounding the tertiary base formed under the influence of glacial erosion, surfaces ran along the lower parts of the such as ridges, deaf, carling, have been widely mountains. Due to the fact that these areas are developed. This means that the first-order base located far away from the geographical points surfaces are emerging as the main forming and where mountain glaciers exist today, glacial actively developing areas of mountain glaciers. landscape landscapes along these areas are For this reason, it is distinguished by its richness somewhat sparse. But their impact is still being of relief views formed due to mountain glaciers. felt. Traces left by paleomuzs in particular are The second-order base surfaces fo