The structure of the Earth’s crust of Eurasia

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1. The structure of the earth’s crust of South America As a result of the split of Gondwana 180 million years ago, South America separated from Africa and began to move westward. So there was the South American lithospheric plate. Thus, at the heart of South America is the “remnant” of Gondwana – the ancient South American platform, occupying the entire eastern part of the […]...
2. The structure of the earth’s crust of North America North America along with Eurasia is the remnant of the ancient continent of the northern hemisphere of Laurasia, which began to split into modern continents at the end of the Mesozoic era about 100 million years ago. The oldest and largest in area tectonic structure of North America is the North American platform, which is […]...
3. The structure of the earth’s crust of Africa The relief depends on the structure of the earth’s crust, which was formed for a long time. Under the influence of internal and external processes, the main tectonic structures of Africa emerged and deposits of various minerals were formed to the origin. Covered 2-3 billion years ago, Africa’s high mountain systems under the influence of […]...
4. Relation between the forms of the Earth relief and the structure of the lithosphere The lithosphere is the hard shell of the Earth, consisting of the earth’s crust and the upper layer of the mantle. Forty years ago, a scientific theory of lithospheric plates arose. According to this theory, the lithosphere is broken by giant cracks into separate blocks – lithospheric plates. The boundaries of the plates pass along […]...
5. The structure of the earth’s crust of Australia Australia is located in the central part of the Indo-Australian lithospheric plate. Consequently, this is the only continent on which there are no active volcanoes, and earthquakes occur very rarely and do not have destructive power. Australia, like Africa, is the remnant of the ancient mainland of Gondwana, about 180 million years ago split into […]...
6. Basic facts on the topic “Physiographic location, discovery, study and relief of Eurasia” The physiographic position of Eurasia is determined by its size, a large extent from west to east and from north to south. Eurasia lies in all climatic belts of the Earth. It is the only continent that is washed by the waters of all four oceans. The coastline of the continent is strongly dissected, there […]...
7. The relief and minerals of South America 1. What processes form the relief of the east of the continent? To answer this question, you need to compare two maps – a map of the structure of the earth’s crust and a map of the modern relief. Look at these maps and compare the structure of the earth’s crust in the east and […]...
8. Relief of Eurasia Due to the complexity of the structure of the earth’s crust and the long history of its development, the surface of Eurasia is more diverse than other continents. Here are the largest plains The earth and the highest mountains, the deepest depression on land and the largest lowland of the world, which lies below the […]...
9. The structure of the earth’s crust and the subglacial relief of Antarctica The structure of the earth’s crust. In the middle of XX century. among scientists there were discussions about what is hidden under the glacial armor of Antarctica: the ocean, the archipelago or the continuous continent. The final answer was given by studies of the earth’s crust. So it was established that the Earth’s crust of […]...
10. The coastline of Eurasia The coasts of Eurasia are strongly dissected. The length of the coastline of Eurasia is more than 2.5 times longer than the Earth’s equator. Near the coast of the mainland there are large sea areas. In the Atlantic Ocean – the Northern, Norwegian, Baltic, Mediterranean, Black, Sea of ​​Azov. In the Arctic – Barents. Karskoe, […]...
11. Features of the Eurasian landform, its development 1. How does the relief of Eurasia differ from the relief of other continents? In Eurasia, as on all other continents, there are mountains and plains. Here are the highest mountains and the most extensive plains. From the plains and plateaus of North and Central Asia, the peninsulas of the South-West, South and South-East Eurasia […]...
12. Origin of continents and oceans 1. Which structure has the lithosphere? What phenomena occur on the boundaries of its plates? The lithosphere is heterogeneous in structure and consists of the earth’s crust and the upper part of the Earth’s mantle. The Earth’s crust is divided into oceanic and continental crust. The continental crust is much thicker than the oceanic crust […]...
13. General information about Eurasia The area is 54.6 million km2. The population is -4.95 billion people. The highest point at sea level is the city of Jomolungma, 8850 m. The lowest point from sea level is the surface of the Dead Sea. The longest river is the Yangtze River, 5800 km. The largest lake is the Caspian Sea. The […]...
14. Basic facts on the topic “Natural areas of Eurasia” The natural zones of Eurasia are replacing each other from north to south – from the arctic deserts to the moist equatorial forests, but not all of them are stretched by a continuous strip from west to east. This is due to the variety of climatic conditions and the features of the relief on the […]...
15. Patterns of the distribution of natural areas in Eurasia Since the territory of Eurasia lies in all climatic zones of the Northern Hemisphere, all natural zones known on the planet were formed here. On the mainland, in contrast to North America, the latitude zonation of natural zones is more apparent, that is, their change from the equator to the poles. In addition, due to […]...
16. Physiographic location of Eurasia Eurasia is the largest land mass on our planet. In terms of area, it occupies more than 1/3 of the Earth’s total land area. Like North America, Eurasia is located entirely in the Northern Hemisphere relative to the equator. Its extent from west to east is impressive: the continent crosses not only the zero, but […]...
17. Influence of the underlying surface on the climate of Eurasia The relief has a significant impact on the climate of the continent. The predominance of flat areas in the west of Eurasia contributes to the development of humid Atlantic air masses deep into the land. Their influence is felt even beyond the Ural Mountains, although considerably weakened. On the Eastern European Plain, cold Arctic air […]...
18. Geological structure, minerals and climate of Oceania The geological structure of the islands of Oceania and their origin are closely related to the structure of the bottom of the Pacific Ocean. In the west of the Pacific, the Pacific and Indo-Australian plates converge, forming uplifts. In the places of their collision, earthquakes and volcanism are observed. Most of the islands of Oceania […]...
19. Climatic zones and regions of Eurasia The great extent of Eurasia from north to south determines the formation over its territory of all types of air masses of arctic, temperate, tropical, equatorial. Therefore, the continent is located in all climatic zones of the northern hemisphere. The considerable length of the continent from west to east predetermines the difference in the climate […]...
20. Distribution of water resources in Eurasia. River basins Distribution of water resources on the mainland. Due to significant climatic differences in Eurasia, the water of the dry land is very unevenly distributed on its territory. Their thickest network is observed on the ocean coasts. With the advance deep into the continent, the number of reservoirs decreases. But the level of water supply in […]...
21. Influence of geographical latitude on the climate of Eurasia The climate of Eurasia is very diverse. The north of the continent lies beyond the Arctic Circle, the southern parts – between the Southern Tropic and the equator. This determines the location of Eurasia in all thermal and climatic zones of the Earth. As in North America, with the progress from north to south, the […]...
22. The influence of atmospheric circulation on the climate of Eurasia The climate of the continent is affected by the constant movement of air due to the formation of areas of high and low atmospheric pressure, especially the western transport – the constant wind of temperate latitudes. From the area of ​​high pressure over the Atlantic Ocean, it brings moist sea air to the continent. Marine […]...
23. Political map of Eurasia The state borders of the countries of Eurasia have been constantly changing throughout the history of mankind. In Europe, the ancient civilizations of Greece, the Roman Empire, on the territory of Asia – Babylon. Assyria, India and China. Numerous military campaigns, wars of conquest, the annexation of new lands led to the disappearance of some […]...
24. Relief of North America The relief of North America is closely connected with its tectonic structures. The ancient and young platforms in the modern relief correspond to the plains, the regions of folding in the extreme West and East – the mountains. Plains occupy 2/3 of the surface. The Canadian shield corresponds to the relief of the Laurentian Upland, […]...
25. Relief of Africa The structure of the earth’s crust of the continent determines its relief. Considering the physical map of Africa, we can conclude that the continent consists of elevated plains. Lowlands and high mountains are few. Lowlands are located mainly along the coasts of the seas and oceans. The eastern part of Africa occupies a rather high […]...
26. Physiographic location of North America The location of North America on the earth’s surface differs significantly from the physico-geographical position of the continents of tropical latitudes. This explains the dissimilarity of its nature with the nature of the continents studied by us. The lines of the equator and the zero meridian do not apply to North America. It is entirely […]...
27. Relief and minerals of North America 1. Explain the location of large relief forms on the mainland. Why are the Cordilleras located in the west of the mainland? Map the physical map of North America with a map of the structure of the earth’s crust. The North American platform is expressed in relief by the Central and Great Plains, and the […]...
28. Minerals of Eurasia In Eurasia, there are all kinds of minerals that humanity uses. This is due to the size of the continent and the complex structure of the earth’s crust. Large deposits of iron ore are discovered in France, on the Scandinavian Peninsula, on the Eastern European Plain, in Kazakhstan, Siberia, on the Dekan plateau in India. […]...
29. The minerals of Africa The occurrence of minerals is associated with the geological structure of the continent. On the shields, where the crystalline rocks of the foundation of the platform come to the surface, and deposits of ore minerals are found in the folding belts of different ages. The so-called “copper belt”, which extends through all of East Africa […]...
30. Natural areas of Eurasia 1. What is the law of natural zoning in the territory of Eurasia? This geographical law in the territory of Eurasia is most clearly manifested in the sequence of alternation of natural zones. One natural zone replaces another when moving from north to south. 2. It is known that in the forests more vegetative mass […]...
31. Inner waters of Eurasia 1. Why are large areas covered in Eurasia with modern glaciers? The northern islands and peninsulas of Eurasia, as well as the belt of high mountains in the south are covered with snow and ice, which do not melt throughout the year. This is due to the conditions that are necessary for the formation and […]...
32. Altitude zonation of the mountains of Eurasia The change in the altitude belts depends on the natural zone at the foot of the mountains and their height. Thus, in the north of Eurasia, four belts are replacing each other from the foot to the top: forests, cedar pine belt, mountain tundra and perennial snow. With the advance to the south, the number […]...
33. Lakes of Eurasia In Eurasia there are many lakes. The largest in terms of area lakes in the world include Baikal, Balkhash and Ladoga. However, the unconditional world leader is the Caspian Lake, which because of its considerable size is even called the sea. In Eurasia, along with giant lakes, there are thousands of small ones that resemble […]...
34. Physical and geographical location of Africa Africa is the continent of heat, impenetrable thickets of equatorial forests, huge savannas and endless deserts. The uniqueness of nature is determined by the peculiarities of the location of Africa on our planet, that is, its physical and geographical position. Physico-geographical position – the location of the territory with respect to a variety of natural […]...
35. Common features of Africa’s climate Africa is the hottest continent of the world. This is due primarily to the fact that most of its territory is in a hot thermal belt between the tropics. Here throughout the year the sun is high above the horizon and twice a year, anywhere in Africa between the North and South Tropics is at […]...
36. The relief of South America The geological structure of South America is connected with its relief. At first glance at the physical map of the continent, it can be divided into three parts: lowland – in the center, plateau – in the east, highland – in the west. Platforms on the east of the continent correspond to large plains. On […]...
37. Key facts on the topic “South America” The continents of South and North America form a single part of oppression. The northern part of South America crosses the equator, the middle part – the Southern Tropic, and the southern part of the continent reaches 54 ° S. extending into temperate latitudes. Part of the world America was discovered by Christopher Columbus in […]...
38. Glaciers of Eurasia and permafrost Glaciers. In the north of Eurasia and high in the mountains is widespread modern glaciation. Cover glaciers are found on the islands of Iceland. New Earth. Spitsbergen, Franz Josef Land. There are mountain glaciers in the mountains that reach the snow line: in the Alps, Scandinavian mountains, the Caucasus, the Pamirs, Tien Shan, the Himalayas. […]...
39. Climatic zones of the Earth The amount of solar radiation decreases from the equator to the poles, and the air masses are formed depending on the geographical latitude. Therefore, each latitude is characterized by its signs of climate. In this way, according to latitude, climatic belts are singled out – huge territories within which the main climate indicators hardly change. […]...
40. Interesting facts about “Eurasia” The first map, which depicted Europe, Asia and part of Africa, was made by the ancient Greek scientist Eratosthenes of Cyrene. She was very imperfect. The land occupied most of the map. The Bosphorus is the narrowest intercontinental strait in the world. Its width is 750-3700 m. The name means “bullish ford”. The Kerch Strait, […]...