What is the dividing line of the plain, and what is the plain of the Ural Mountains? The Ural Mountains are the dividing line between Asia and Europe, and also the dividing line between the Eastern European Plain and the Western Siberian Plain. The dividing line between Asia and Europe is Urals-ural river-Caspian Sea-Caucasus-Turkish Strait.
To the west of the Ural Mountains is the Eastern European Plain, and to the east is the Western Siberian Plain.
What is the dividing line of the Urals? The Urals are the dividing line between Europe and Asia. It extends from the Baydaratz Bay in the Kara Sea of the Arctic Ocean to the southern kazakh steppe, with a total length of more than 2,000 kilometers, and is located between the Eastern European Plain and the Siberian Plain. From north to south, the mountains are divided into polar and sub-polar Urals and northern, central and southern Urals. The average altitude is 500 ~1200m; The sub-polar People's Peak (1894m) is the highest peak in the Urals. The mountain range is 40 ~ 150km wide. The middle section is low and flat, which is an important passage between Europe and Asia. The western slope of the Ural Mountains is gentle and the eastern slope is steep. There are obvious differences in mineral resources and the distribution of animals and plants on both sides of the Ural Mountains. The Ural Mountains are also the watershed of Volga River, ural river River and Dongpo ob river River Basin.
Ural mountains:
The Ural Mountains are a mountain range in Russia, which generally runs in the north-south direction. It is located in central and western Russia, and it is the border mountain range between Europe and Asia. It stretches for more than 2,500 kilometers from the coast of the Kara Sea in the Arctic Ocean to the Ural Valley in the south. Width 40 ~ 150km. Generally north-south. Between the Eastern European Plain and the Western Siberian Plain, it is the watershed between the Volga River and the ural river and ob river basins.
Before the orogeny, it was the Ural Sea between the European plate and the Siberian plate. The two plates moved towards each other and were squeezed and folded into mountains. After that, the action is repeated, the structure is complex, and it continues to rise slowly. This mountain is mainly composed of igneous rocks, metamorphic rocks and sedimentary rocks. The peaks are mostly round, mainly low and Zhongshan, with an altitude of 500 ~ 1200m. The highest peak, Naroda Peak, is1895m above sea level. The western slope of the mountain range is gentle and the eastern slope is steep. It has a mountainous continental climate.
The western part of the Ural Mountains is the Russian Plain, and the eastern part is the Siberian Plain. It extends to the Kara Sea to the north and to the south, and the Caspian Sea is not far from the starting point of the mountains. Here it transitions to the grasslands of Kazakhstan. From its southern end to its northern end, it is 2500 kilometers long. At its northern end, it runs parallel to ob river and flows eastward into the sea.
Where is the Ural Mountains, the boundary mountain between Europe and Asia? The Urals Mountains are the famous dividing line of the Urals Mountains in Europe and Asia. On one side is the Urals Mountains in the Russian plain, and on the other side is the Western Siberia Plain. Most of them are in Russian territory, starting from the coast of the Kara Sea in the Arctic Ocean in the north, reaching the middle reaches of ural river in the south, and finally reaching the territory of Kazakhstan. It twists and turns more than 2,000 kilometers, with a width of about 40 ~ 65,438+050 kilometers, which is the watershed between the Volga River and the ural river and ob river basins.
Russian historian and geographer Tajishev was the first person to define the Ural Mountains as the dividing line between Europe and Asia. On-the-spot investigation in the Ural Mountain found that there are great differences between animals and plants in the east and west sides of the Ural Mountain. The carp in the river flowing west is red, while the carp in the river flowing east is white. So he concluded that the eastern foot of the Ural Mountains is the dividing line between Europe and Asia. Later, this statement was gradually accepted by people, and the Eurasian boundary pillar appeared at the eastern foot of the Urals. The monument is more than 3 meters high and is very eye-catching.
According to the local meaning, Urals means "land of gold". In fact, the word "Urals" comes from Turkic, which means "belt". Indeed, the Ural Mountains, like a narrow ribbon left by someone in the northern plain of Eurasia, extend from the Kara coast to the Kazakh plain. In the northwest, the Ural Mountains are connected with the mountains of Syndicate Island through the Derived Mountains and Wagaqi Island, and the continuation part of the southern Ural Mountains is Mugzare Mountain.
The Urals is an ancient folded mountain range. The Paleozoic Urals was an geosyncline, and for a long time it was the sea of Wang Yang. The ocean has changed the boundary and depth, and a large amount of materials have gradually deposited in the Urals. Soon, two more orogenic movements took place in this area. The first time was Caledonian fold. Although this folding has also affected most areas, it has little impact on the Urals. The second time is Hercynian fold, which has the greatest influence, starting from the eastern Urals and extending to the western slope. Hercynian folds in the eastern Urals are much stronger than those in the west, with serious folds and compressions, often lying upside down, deep faults and intrusion of thick granite magma. After the Hercynian orogeny, folded mountains were produced in the Ural geosyncline, and then the area continued to rise, eventually becoming a vast continent.
The Ural Mountains is a complete mountain system, which consists of many north and south mountains extending parallel to each other. Generally, there are two or three parallel mountains, and some places will increase to four or five. The South Ural Mountain is very complicated, with at least six mountains, and there is a narrow lowland between the mountains to become a valley.
The general feature of Ural Mountain topography is that the east and west slopes are asymmetrical, and the west slope is relatively gentle, gradually transforming to the Russian plain, while the east slope suddenly drops to the Siberian plain, causing the main watershed mountains to move eastward and approach the Siberian plain. In addition, the name of this watershed is very different in different parts of the Urals. In the south of Urals, it is called Urals Mountain, and in the north of Urals, it is called Boyasso Mountain. This watershed is not high above sea level, and the highest peak of the mountain range is generally located west of the watershed. The reason for this result is that the river erosion on the west slope is very strong. Most of the rivers on the western slope are winding. In the upper reaches, the river tends to run north and south, flowing along the valley to the lowlands, then turning sharply to the west, often crossing the mountains, and then either flowing north and south or keeping the original east-west direction. Many rivers are even older than mountains, and the downcut of rivers and the uplift of mountains occur at the same time.
Due to the small absolute height, the Ural Mountains are mainly composed of lowlands and Zhongshan. The top of the mountain is flat, some peaks are dome-shaped, and the outline of the hillside is very gentle. In the polar Urals and northern Urals, rocky seas are widely distributed.
The climate of Ural Mountain extends from north to south, and its types also show zonal evolution. The northern part is a frozen prototype and the southern part is a grassland type. The climate difference between north and south is most obvious in summer. But generally speaking, the Ural Mountains are not high, and the width from east to west is not large, which has not created conditions for the formation of the unique mountain climate of the Ural Mountains. The precipitation difference between the eastern and western slopes of the Ural Mountain is also obvious. The precipitation on the west slope is larger than that on the east slope, and it is warmer and wetter. Nevertheless, the mountainous terrain criss-crossing the Urals makes its local climate extremely complicated. Mountains with different heights, mountains with different slopes, valleys and basins all have unique climates. In winter or transitional season, cold air sinks along the slope and stays in the basin, so inversion in mountainous areas is very common.
Due to the change of climatic conditions, the plants on the Urals Mountain also showed zonal evolution. There are many kinds of forests on the mountain, including coniferous forest, broad-leaved forest and lobular forest. The vast forest is like the rolling Great Green Wall, extending from the polar regions to the south along the mountains. At the peak, it is separated by mountain tundra, and the southern mountain area is separated by grassland. Nevertheless, they still crossed the mountains and covered this fertile land. All kinds of animals live in it, and mountains become their natural barriers. Common animals are brown bears, minks, wolves, squirrels, otters and so on. , and hazel chicken, grouse, black lark.
The present landscape of Ural Mountain has also experienced a long development process. At first, the hilly plain was raised on the position of Ural Mountain, a bit like the hills of modern Kazakhstan. The eastern and southern parts of the plain are still shallow seas. It was very hot then. Evergreen tropical forests and rare plants such as palm and laurel grow in Ural Mountain. Subsequently, the evergreen flora in poltava was replaced by temperate deciduous plants, and a large number of oak trees, beeches, chestnuts and birch trees flourished day by day. At the same time, the Ural Mountain gradually rose from the dome and low hills to Zhongshan, and the plateau plant belt was also formed. Later, the climate became colder and colder, the ice age approached, coniferous forests gradually increased, and the proportion of birch forests also increased.
According to the geological and geomorphological features, the Ural Mountains can be divided into four main landscape areas: polar Ural Mountains, northern Ural Mountains, central Ural Mountains and southern Ural Mountains.
The permafrost region of the polar ural mountains extends from the northernmost part of the mountains to 64 30 ′ north latitude, and the polar ural mountains and their derived mountains form an arc protruding eastward. Derived mountains are characterized by domes and low hills, which are separated from the polar Urals by low-altitude tundra. To the south, the plateau gradually rises, and the highest peak, the People's Peak, stands among the mountains. Subsequently, the width of the polar Urals gradually increased, forming at least five or six parallel mountains. The Ural Mountains in the polar regions have a flat and highly undisturbed ground, covered with glacial traces, and their edges are cut by deep valleys, and the alpine topography is also widely distributed. Modern glaciers are mainly concentrated near Sablja and People's Peak, and the jagged tops and slopes are eroded by steep ice buckets and ice nests. The climate here is cold and humid, and there are large snowdrifts in low-lying areas. There are few plants here, and most of them are patches of moss, lichen and shrub tundra near the foothills. The middle of the mountains is full of rubble and there is almost no vegetation. In the south, there are some sparse larches and spruces on both sides of the valley.
The Taigarin region in the northern Ural Mountains starts from the southern foot of Sablja Mountain and extends to Kangri Akov Mountain and Koswa Mountain. Generally, it consists of two longitudinal mountains. There is a watershed in the east-Boya Suowei Mountain, the highest peak of the Northern Urals Mountain-Fengshan stands on the west side of the mountain range. Three or four ancient planation planes in the northern Ural Mountains are particularly obvious. Terraces are widely distributed in mountainous areas, and the number and size of terraces, the length and height of broad slopes not only vary greatly at the top of each mountain, but also have significant differences in the mountains of the same mountain range. Generally speaking, the climate in northern Urals is relatively cold and humid with abundant precipitation, which also creates favorable conditions for plant growth in northern Urals. The dark coniferous forest here is gloomy. When the wind blows, Lin Tao bursts and makes strange noises. Wolverines wander in the forest, and crows and birds fly around the treetops.
The Ural Mountain in the middle is very special. The Urals Mountain seems to yield here, the altitude becomes lower, and the north-south trend of the mountain gradually changes to the southeast trend, so that the middle Urals Mountain and the south Urals Mountain merge into a large arc protruding eastward and surround the Ufa Plateau in Russia. The neotectonic movement in the middle part of Ural Mountain is inactive, and it can only be a low quasi-plain, with isolated peaks, gentle contour lines, wide river valleys and serious river erosion. Some places stand on cliffs overlooking the slowly flowing river, which is very spectacular. There are many lakes here, and the water is as clear as sapphire. Coniferous forests and broad-leaved forests are densely covered on the mountain, and the crowns squeeze each other, so there is no sunlight at all. The mountain spring whimpers and the water gurgles. Great changes have taken place in the animal kingdom here, and all kinds of animals have suddenly increased, including hedgehogs, nighthawks, orioles and red snakes.
In the southern part of the Ural Mountains, the altitude suddenly rises. Although the peaks of many peaks are relatively flat, they are more complicated because of the mountain terraces, and steep rocky slopes can be seen everywhere. There are many lakes scattered at the foot of the mountain with magnificent scenery. It's hot and dry here in summer. It's cold in winter and the snow is thick. In the cold winter, rivers freeze and form ice piles, resulting in a large number of deaths of zokor and some birds. Although the terrain in the southern Urals is cut and the rocks are steep, the forests and grasslands here are ingeniously integrated, and the forests are usually distributed at the highest places with rocks.
Ural Mountain is the oldest mining area in Russia. The mountains are rich in mineral resources, such as ferrous metals, non-ferrous metals and rare metals, and the output of jadeite, jasper, malachite, crystal, Ziyingshi and topaz is also great. Therefore, some people call the South Ural Mountain a stone belt. In addition, there are many coal, oil, asbestos and chemical raw materials.
The Ural Mountain is shaded by trees, with flowing water and beautiful scenery, which attracts many tourists to climb here and enjoy the charming wild interest. The vast and lush grasslands and peculiar lava landforms here are good places for sightseeing.
Where are the Urals? What happened in this mountain range, paranormal? The Ural Mountains are actually the Ural Mountains in Russia, with a general north-south trend. It is located in the Ural Mountains in central and western Russia, which is the border between Europe and the Ural Mountains. 1959 On the evening of February 2nd, nine skiers were killed in the northern Ural Mountains. Their captain was Diart Love. They had an accident while climbing the dead Dongling Mountain, and the whole team died. Later investigation on this matter showed that these climbers' tents.
One of the skulls was broken, two ribs were broken, a tongue was missing, and some people were wrapped in shabby clothes. These clothes seem to have been cut from the dead. It starts from the coast of Kerala in the Arctic Ocean in the north and reaches the Ural Valley in the south, with a total length of more than 2,500 kilometers and a width of 40- 150 kilometers. It is roughly north-south, and it is the Volga River between the Eastern European Plain and the Western Siberian Plain.
Before the orogeny, there was the Ural Sea between the European plate and the Siberian plate. The two plates moved, squeezed and folded into mountains. After that, many movements, complicated structures and slowly rising movements continued. Mountain peaks are mainly composed of igneous rocks, metamorphic rocks and sedimentary rocks. The peaks are mostly round, mainly low and Zhongshan, with an altitude of 500 ~ 1200m. The highest peak, Naroda Peak, is 1, 895 meters above sea level. The western slope of the mountain range is relatively gentle and the eastern slope is relatively steep.
This is a mountainous continental climate, with the Russian plain in the west and the Siberian plain in the Urals in the east. It extends to the Kara Sea to the north and to the south. The sea is not far from the starting point of the mountain. Here, it transitions to the grasslands of Kazakhstan. From the southern end to the northern end, the total length is 2500 kilometers. At its northern end, it is parallel to ob river in the east.
The question of where the Urals Mountains are and what supernatural events happened in this mountain range is explained here today.
What are some introductions about the Ural Mountains? Of the seven continents in the world, only Eurasia is closely linked. The Ural Mountains are the dividing line between Europe and Asia.
The Ural Mountains, which stretches for more than 2,000 kilometers, starts from Bedaratz Bay in the Kara Sea of the Arctic Ocean in the north and reaches kazakh steppe in the south, and spans between the Eastern European Plain and the Siberian Plain. From north to south, the whole mountain range is divided into five parts: polar, sub-polar Urals and northern, central and southern Urals. Generally speaking, the mountain is not high, with an average elevation of 500 ~ 1200m. The people's peak is 1894 meters above sea level, which is the highest peak in the ural mountains. The mountain range is 40 ~ 150km wide. The middle section is low and flat, which is an important passage between Europe and Asia.
The Backbone of Europe-Alps
The Alps are the highest and most majestic mountains in Europe. It starts from Nice in the southeast of France in the west, passes through Switzerland, southern Germany and northern Italy, and reaches the Vienna Basin in the east, stretching for 1, 200 kilometers. 120~200 kilometers wide, and the widest point can reach 300 kilometers. The mountain is steep, with an average elevation of about 3000 meters. The main peak Mont Blanc is located between France and Italy, with an altitude of 48 10 meters. Named after the perennial snow on the summit, it is a famous peak in Europe. Many peaks are rocky with sharp tinder, and there are many deep glacial valley and moraine lakes in the mountainous areas. Up to now, there are more than 1000 modern glaciers in the Alps, with a total area of 3,600 square kilometers, which is larger than Luxembourg, a European country.