
В чём особенность геологического строения уральских гор


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Geological Structure of the Ural Mountains
The Ural Mountains are a mountain range that runs approximately from north to south through western Russia, from the coast of the Arctic Ocean to the Ural River and northwestern Kazakhstan. The geological structure of the Ural Mountains is characterized by several key features.
1. Age and Formation: The Ural Mountains are relatively old and are considered to be a fold mountain range. They were formed during the Late Carboniferous and Early Permian periods as a result of the collision between the Eurasian and Siberian tectonic plates.
2. Composition: The Ural Mountains are primarily composed of metamorphic and igneous rocks. The central part of the range consists of ancient crystalline rocks, while the flanks are made up of sedimentary rocks.
3. Height and Peaks: The Ural Mountains reach an average elevation of around 2,500 feet (750 meters), with the highest peak, Mount Narodnaya, rising to an elevation of 6,217 feet (1,895 meters).
4. Mineral Resources: The Ural Mountains are rich in various mineral resources, including iron ore, copper, gold, and gemstones. These resources have historically played a significant role in the region's economy.
5. Tectonic Activity: While the Ural Mountains are not currently experiencing significant tectonic activity, their formation was the result of intense tectonic forces during the collision of the Eurasian and Siberian plates.
6. Biodiversity: The Ural Mountains are home to a diverse range of flora and fauna, including several endemic species. The region's unique geological structure has contributed to the development of distinct ecosystems and habitats.
In summary, the Ural Mountains are characterized by their ancient age, diverse geological composition, rich mineral resources, and unique biodiversity, making them a significant geological and ecological feature of the Eurasian continent.


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