Ural mountains.
The Ural Mountains vein is the partitioning line among Eurasia and Asia. North Arctic, the Kara Sea from Baydaratskaya Bay, south to the Kazakh steppe, broadening in excess of 2000 km, between the fields of Eastern Europe and the Siberian plain. From north to south, the mountain range is separated into 5 areas of the Arctic and Subarctic Urals and the Northern, Central and Southern Urals.
Normal stature is 500-1200 meters; Renmin 1894 meters high in the subarctic is the most elevated top in the Urals. The width of the mountain goes from 40 to 150 km. The focal part is low and level, which is a significant entry among Europe and Asia.
The western slant of the Ural Mountains is gentler and the eastern incline more extreme. There are particular contrasts in the appropriation of mineral assets, verdure on the two sides of the Urals. The Ural Mountains are likewise a partition between the Volga and Ural streams and the Ob River on the eastern incline.
Presentation about the Ural Mountains.
The Ural Mountains are a mountain range that runs generally from north to south in Russia, situated in the focal and western piece of Russia and is a mountain range that isolates Europe and Asia. From the Arctic Ocean along the Kara Sea in the north to the Ural River Valley in the south, it extends for in excess of 2,500 kilometers. It is 40 to 150 kilometers wide. It is generally confronting north and south. Between the Plain of Eastern and Western Siberia Plain, it is a detachment between the Volga streams, the Urals and the Ob River.
Prior to the arrangement development, the Urals were between the European and Siberian plates, as the two plates advanced toward one another and were packed and collapsed in the mountains. From that point forward, it moved a few times, the structure was confounded, and the upward development gradually proceeded. The mountain is for the most part made out of molten rocks, just as transformative rocks and sedimentary rocks.
The pinnacles are for the most part round, overwhelmed by low and medium mountains, by and large 500 to 1,200 meters above ocean level. The most noteworthy pinnacle, Naroda Peak, is 1,895 meters above ocean level. The mountain's western incline is gentler, and the eastern slant more extreme. It has a rocky mainland atmosphere.
Toward the west of the Ural Mountains.
There is the Russian Plain and toward the east the Siberian Plain. Toward the north expands the Kara Sea, south of the Caspian Sea from the earliest starting point of the mountains not far away. Here it moves to the steppes of Kazakhstan. It is 2,500 kilometers in length from its southern finish to its northern end, and at its northern end it matches the Ob River and goes east to the ocean.
Mountains are commonly not high, with a normal tallness of 500-1200 meters; The width of the mountains is 40-150 kilometers. The center segment is low and level, with a delicate slant in the west and a lofty slant in the eastern Urals. The cross-country division landmark, multiple meters high, remains before Donglu Hill, under 10 meters from the railroad. Because of the diverse geological conditions, there are particular contrasts in the dissemination of mineral assets, fauna and greenery on the two sides of the Ural Mountains.
The Ural Mountains are a mother lode of minerals in Russia. Their eastern slant contains minerals, for example, magnetite, copper, aluminum, platinum and asbestos, and their western incline contains potash, oil and flammable gas. .
The eastern and western inclines of the mountains have various temperatures and the normal yearly precipitation in the western slant is 300 mm more than that on the eastern slant there are huge broadleaf woods, coniferous timberlands and woodlands develop. Linden, oak, maple, birch and other tree species. It is a pine plant, and broadleaf woods are uncommon.
Ural Mountain Geology.
The Ural Mountains were shaped during the Carboniferous time frame, and Siberia around then was a free landmass, which slammed into a piece of Pangea around then, and Europe today, and shaped the Ural Mountains. Up until this point, Europe and Siberia are as yet associated. The island of Xindi between the Kara Sea and the Barents Sea is really an expansion of the Ural Mountains.
Jebels initially started to shape during the underlying rise of the Hersenian development (around 250 million years back). Around 280 million years back, a high mountain zone was raised here, and disintegrated into a semi-plain. The Alpine development made new mountains, the most remarkable of which was the subarctic stature of the Ola Mountain.
The western incline of the Wola Mountain Range is made of mid-Paleozoic sedimentary rocks (sandstones and limestones) that are around 350 million years of age. Toward the west of the Ural Mountains is the CIS Ural Depression toward the finish of the Paleozoic (around 300 million years prior), a ton of dissolved materials were alluvialized here; In 1988, numerous spots showed up on the western slant of the mountain to be porches. Get off the arrival Seth-Ola. The western slant is covered with karst (a totally disintegrated limestone zone) and gypsum, with gigantic caverns and underground streams. On the eastern slant, layers of molten shakes and layers of sedimentary shakes on the other hand cover, the two of which framed in the Middle Paleozoic period.
These stones structure Nizhny Tagil - Magnitogorsk anticlinorium (Tagil-Maqnitogorsk Synclinorium, a gathering of stone curves and stone bowls, which can likewise shape a little bowl), it is the entire mountain range in the biggest anticlinorium. In the Ural Mountains and Nanwu La Dongpo is twisted into slopes of wide, practically level lower regions in a practically plain style, where rock is regularly found in an outcrop, and coho is frequently appalling. Toward the north, the semi-fields are covered underneath the delicate, delicate, and fine residue of the West Siberian Plain.
The territory is firmly identified with the stone development: steep slopes and low, level edges made of quartzite, schist and gabbro, are difficult to climate. Single tops are normal; There are a few bottoms among north and south, and practically every one of them are valleys. On the western incline of the mountain range, the karst landscape is profoundly evolved, with numerous caverns, bowls, and underground streams.
Be that as it may, there are a couple karst developments on the eastern slant, however some stone arrangements transcend the level ground. Toward the east, expansive edges brought down into a semi-plain interface the focal Wola Mountain and South Wola Mountain.
Swears
The Ural heartbeat can be isolated into five sections:
1. The Arctic district, Mount Ula, reaches out from Mount Konstantinov Kamen to the Kolga River (around 390 kilometers (240 miles)); Most of the mountains are 1000 to 1100 meters above ocean level (3300 ~ 3600 feet), the most noteworthy top in Mount Payer (Mount Payer) is 1,472 meters (4,829 feet).
2, the following segment is the sub-polar Ural (Nether-Polar Urals), which broadens south into Hugh Gore Creek (Shchugor River), at an elevation of in excess of 225 kilometers (more than 140 miles). Mountains exist all through this period the most noteworthy pinnacles, for example, Mount Narodnaya (1,895 meters Narodnaya Mountain, 6,217 ft) and Karpinsk (1,878 mt. Karpinsk, rise (6,161 ft)). This is the situation for the initial two pieces of the Alps, the ice sheets spotting the profound, perpetual permafrost.
3. The southernmost is the North Ula Mountain, which stretches out south to the Usfa River and is in excess of 547 km (340 miles) in length; Most of the pinnacles arrive at 3,300 feet, and the most elevated pinnacle is Mount Turboziz. Telpos-Iz) arrives at 1,617 meters (5,305 feet).
4, the lower augmentation of the Southern Urals to the Ufa River (Ufa River), longer than 322 km (200 mi); High mountains are infrequently more than 488 meters (1,600 feet), yet the most elevated top at Jishan (Sredny Baseg) is 994 meters (3,261 feet). The highest points of the pinnacles are exceptionally level, and some detached remaining parts show up.
5 - South Wola Mountain, west of the Wola River, is around 547 kilometers (340 miles) in length; It comprises of equal slopes 1189 meters (3,900 feet) high, and the most noteworthy point is Mount Yamantau (Mount Yamantau) with a stature of 1,640 meters (5,380 feet). The finish of this part is the expansive level of Mt Mugujal (under 610 meters (2000 feet) above ocean level)
Atmosphere in the Ural Mountains.
The atmosphere is mainland, described by a polarization of temperature, either high or extremely low; From north to south and from west to east, this element is steadily apparent. The atmosphere in the Pahoe Mountains and the Wola Mountains (particularly in winter) is impacted by the guideline of the Arctic Ocean and the North Atlantic Ocean; In the Mugujal Mountains and the South Wola Mountains, summers are sweltering and dry from Central Asia. Wind.
Waterway to you in the Ural Mountains.
The breezes in the Urals are generally westerly breezes, which bring precipitation from the Atlantic Ocean. Despite the fact that the mountain is low, it significantly influences the conveyance of water and gas, as the western incline gets more water and gas than the eastern slant. On the western slants of the subarctic Wula Mountains and the northern Wula Mountains, the precipitation is incredibly plentiful, up to 1,000 mm (40 in). In the north and south, precipitation slowly diminishes, coming to around 457 mm (18 in).
Since the cold and dry demeanor of a Siberian twister in winter is exceptionally solid, the precipitation in summer is the biggest. The eastern slant is freezing; Throughout the Urals, winters are longer than summer. Normal temperature in January: - 21 ° C (- 6 ° C) in the north and - 15 ° C (5 ° C) in the south. Indeed, the normal temperature contrast in July is more prominent: 10 degrees (50 degrees Celsius) in the north and 22 degrees (72 degrees Celsius) in the south. (4)
A stream in the Ural Mountains.
The Ural Mountains are additionally on the watersheds between the Volga and Ural waterways and the Ob River on the eastern incline.
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