As part of the school curriculum, students studycontinents. The most interesting is Eurasia. Why is that? First of all, it is the largest continent on Earth. If you take into account its size, it is not surprising that in this territory there are sites with different terrain and climate. It is also worth paying attention to the geological structure of the area.
In this article, the features of the relief of Eurasia will be considered. So, let's get started.
Eurasia, as already mentioned, is the mosta large continent on the planet. Its area is measured by huge scales, which make up almost 40% of the entire land. If you express this in figures, then the size of this territory was almost 55 million square meters. km. About 100 countries are on this continent. Its position on the map can be found from the following coordinates: between 1 ° 16 "north and 77 ° 43" s. w .; 9 ° 31 "W and 169 ° 42" W. e.
It should be noted that the continent is unique not onlyits size. Eurasia is the only continent on the planet that is washed by all four oceans of the Earth. Also interesting is the fact that on its territory two parts of the world are united - Europe and Asia. And since they lie in different geographical belts, the relief and climate of Eurasia on the entire extent is very different.
I would like to highlight the fact that Eurasiadiffers significantly in geological structure from the rest of the continents. It is based on several plates and platforms. The time interval of formation falls on the Cenozoic and Mesozoic eras. Geologically, the continent is considered the youngest.
Structure of Eurasia:
Also on the territory of the mainland there are largeCracks and faults, which predominate in the Siberian region (for example, Tibet, Lake Baikal). Volcanoes can erupt in folded belts and earthquakes occur, as evidenced by the peculiarities of the relief of Eurasia. In these territories, because of the unusual structure of the earth's crust, there are the richest mineral deposits, such as tin, tungsten, natural gas, oil, various ores and others.
The features of the mountainous relief are:that, unlike other continents, where the hills are mostly located on the outskirts, here they are in the very depths, separated by two folded belts: the Pacific and the Albian-Himalayan. The first of them stretches almost throughout the eastern part. An intensified movement of the earth's crust has been noticed up to now.
When describing the relief of Eurasia, it is worthIt should be noted that the average heights vary within 830 m. It is here that the highest point of the planet is Everest (8 848 m). Other mountain formations are no less significant:
In addition to the mountain peaks, there are also plains on the mainland. Let's look at them.
The relief of Eurasia directly influences the formation ofclimate. Considering that the size of the continent is quite large, the climate diversity is clearly expressed here. Almost all climatic zones pass through the territory of Eurasia.
In the north singles out polar and subpolar. Towards the south, they are replaced by a temperate belt, which, in turn, becomes subtropical. The tropical belt extends from the Mediterranean and Red Seas up to India. Subequatorial dominates the territory of India and Indochina, capturing the southern part of China. And the last climatic zone is equatorial. It covers the territory of the islands of southeast Asia.
In the center of the continent, there is a sharp climate change at different times of the year. It's cold in winter and warm in summer. The difference between the upper and lower limits of temperature is 50-70 ° C.
Studying the climate, it is important to take into account the relief of Eurasia. Mountainous formations are clear boundaries of weather conditions. For example, in the direction from north to south the territory is entirely occupied by a huge Alpine-Himalayan mountain belt. In winter, the ridges do not let cold winds pass, and in summer - warm ones. In the north of the Himalayas, the minimum amount of precipitation is up to 100 mm per year, but at the foot of the east this figure reaches a record 1,000 mm. Near the city of Cherapunji is the most damp spot on the planet. The amount of precipitation here is about 12 000 mm per year.
Winter in areas that are limited to mountainousarrays, warm. The temperature here rarely drops below -5 ° C. But the flat terrain from November to March-April is under the influence of cold cyclones. This season is characterized by precipitation in the form of snow, accompanied by low temperatures, sometimes reaching minus 45-50 ° C.
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