From a distance, it is a mountain, and up close, it is a river, and it describes what kind of area i

This refers to the scene of the Qinghai-Tibet Plateau: because the altitude of the Qinghai-Tibet Plateau is too high, there are many mountains on the Qinghai-Tibet Plateau from afar, but when you are on the plateau, because the relative height of the altitude is very small, for example, the main peak of Tanggula Mountain is more than 6,000 meters above sea level, but on the plateau, the relative height is about 2,000 meters, not to mention those non-main peak mountains, which are only a few hundred meters high, so the Qinghai-Tibet Plateau is also endless, so it is a mountain from afar, and it is a flat land --- Sichuan from a distance!

Tibetan Plateau

From a distance, it is a mountain, and up close is a Sichuan search", referring to the Qinghai-Tibet Plateau. Because the altitude of the Qinghai-Tibet Plateau is too high, there are many mountains on the Qinghai-Tibet Plateau from a distance, but when you are in the plateau, because the relative altitude of the altitude is very small, such as Tanggula Mountain.

The elevation of the main peak is more than 6,000 meters, but on the plateau, the relative height is about 2,000 meters, so the Qinghai-Tibet Plateau is also endless, so it is a mountain from a distance, and it is a river from a distance.

Geography of the Tibetan Plateau:

The general characteristics of the climate of the Qinghai-Tibet Plateau are as follows: strong radiation, more sunshine, low temperature, less accumulated temperature, the temperature decreases with the increase of altitude and latitude, and the diurnal temperature range of air leakage is large. Dry and wet are distinct, and it rains at night; The winter is dry and cold, and there are many winds; Summers are cool, rainy and hailstormy.

The distribution of rivers on the Tibetan Plateau is mainly affected by climate and topography. In addition to the abundant precipitation in the southeast, the inland areas are fed by rivers and rely mainly on the melting of glaciers or snow.

The water resources of the Qinghai-Tibet Plateau exist in the form of rivers, lakes, glaciers, groundwater and other water bodies, with river runoff as the main body.

The geographical distribution of land resources on the Qinghai-Tibet Plateau is obvious, and the quantity composition is extremely unbalanced. Land suitable for grazing accounts for the total land area, land suitable for forest, land suitable for agriculture, and land area that is not suitable for use for the time being.

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Problem description: It looks like a mountain from a distance", this understands, but"Up close, it's a tomato Xunchuan""What does chuan mean?

Analysis: This refers to the scene of the Qinghai-Tibet Plateau: because the altitude of the Qinghai-Tibet Plateau is too high, there are many mountains on the Qinghai-Tibet Plateau from afar, but when you are in the plateau, because the relative height of the altitude is very small, for example, the main peak of Tanggula Mountain is more than 6,000 meters above sea level, but on the plateau, the relative height is about 2,000 meters, not to mention those non-main peak mountains, it is only a few hundred meters high, so the Qinghai-Tibet Plateau is also endless, so it is a mountain from a distance, and it is a flat land --- Sichuan up close!

"Looking at mountains from afar, and seeing rivers up close" describes the Qinghai-Tibet Plateau. This is because the Qinghai-Tibet Plateau has a high altitude, and from a distance, it looks like a high mountain range; The Qinghai-Tibet Plateau is a snow-capped mountain, and after the snow melts, it forms a series of ravines, so up close, the ups and downs are not large, constituting a river.

The Qinghai-Tibet Plateau is densely populated with mountains and rivers, the terrain is steep and changeable, and the terrain is complex, and its average altitude far exceeds that of the surrounding areas at the same latitude. The Qinghai-Tibet Plateau is uneven in the mountains, and the drop is huge. In general, the topography of the Qinghai-Tibet Plateau is high in the west and low in the east.

Compared with the undulating edge of the plateau, there is a lower undulating area in the interior of the plateau.

The Tibetan Plateau is a huge mountain system consisting of mountain systems and plateau planes. Due to the influence of gravity and external gravitational force in the formation process of the plateau, the plateau surface has been deformed to varying degrees, so that the topography of the whole plateau shows a tendency of inclination from northwest to southeast. The edge of the plateau is strongly cut to form the low-altitude areas of the Tibetan Plateau, where mountains, valleys and rivers are interspersed and the terrain is fragmented.

The Qinghai-Tibet Plateau is widely covered with glaciers, snow-capped mountains, and gentle undulations on the mountain plateau. The Qinghai-Tibet Plateau is high in the northwest and low in the southeast, and the north and south are east-west trending mountains (north: Kunlun Mountains, etc., south:

Gangdis Mountains, etc.), with north-south trending mountains (Hengduan Mountains) to the east, arc-shaped mountains (Himalayas) to the west, and relatively intact plateaus to the northwest.

This sentence refers to the characteristics of the Qinghai-Tibet Plateau, because the altitude of the Qinghai-Tibet Plateau is too high, so there are many mountains on the Qinghai-Tibet Plateau from a distance, but when you are on the plateau, because the relative height of the altitude is very small, for example, the main peak of Tanggula Mountain is more than 6,000 meters above sea level, but on the plateau, the relative height is about 2,000 meters, not to mention those non-main peak mountains, which are only a few hundred meters high, so the Qinghai-Tibet Plateau is also endless, so it is said that it is a mountain from a distance, and it is a river from a distance.

The general climate characteristics of the Qinghai-Tibet Plateau are as follows: strong radiation, more sunshine, low temperature, less accumulated temperature, the temperature decreases with the increase of altitude and latitude, and the diurnal temperature range is large. Dry and wet are distinct, and it rains at night; The winter is dry and cold, and there are many winds; Summers are cool, rainy and hailstormy.

Kawa means plain, flat land.

Due to the high altitude of the Qinghai-Tibet Plateau, therefore, the mountains inside the plateau are generally relatively low in height, and between the mountain ranges, the ups and downs are gentle, so there is "a mountain from a distance, and a river from a distance".

This refers to the scene of the Qinghai-Tibet Plateau: because the altitude of the Qinghai-Tibet Plateau is too high, there are many mountains on the Qinghai-Tibet Plateau from afar, but when you are on the plateau, because the relative height of the altitude is very small, for example, the main peak of Tanggula Mountain is more than 6,000 meters above sea level, but on the plateau, the relative height is about 2,000 meters, not to mention those non-main peak mountains, which are only a few hundred meters high, so the Qinghai-Tibet Plateau is also endless, so it is a mountain from afar, and it is a flat land --- Sichuan from a distance!

The Hengduan Mountains are mainly ancient glacial erosion and accumulation landforms. There are many intermountain basins and lakes in the Hengduan Mountains, and ancient glacial erosion and accumulation landforms are widely distributed, and modern glaciation and gravity landforms such as landslides, landslides and debris flows are common. At the same time, it is one of the main belts in China, and the famous Xianshui River, Anning River and Xiaojiang are all distributed in this area.

The Hengduan Mountains are located on the axis of the Kang-Yunnan Axis between the trough area of western China and the platform area of eastern China. The Indochinese movement uplifted the folds into land and formed a series of fault basins. Jurassic and Cretaceous strata are deposited in the basin.

The Yanshan movement folded and fractured again. Until the middle of the Tertiary period, the earth's crust slowly rose and was leveled by long-term denudation, forming a vast flat. From the end of the Tertiary to the beginning of the Quaternary, the tectonic movement was extremely active, the unified plane deformed and disintegrated, and the height difference of the ridge valley tended to be obvious.

The Quaternary underwent several glaciations. The hilly plateau and the summit surface can be connected into a unified "base surface", with mountains on the "base surface" and river valleys and basins below. There is a huge difference in the height of the Hengduan Mountains and valleys. The ridge of Qionglai Mountain is more than 3,000 meters above sea level, the main peak Siguniang Mountain is 6,250 meters above sea level, and the relative height difference of its southeast slope is more than 5,000 meters.

Pursue hard, but you will still suffer blows, and there are people who persevere to the end and succeed. More discomfort and disaster! Seeking the heart and cultivating to understand life: people are not easy to be born, and they are under control.