Результат схождения и расхождения литосферных плит.
Ответы на вопрос
Когда плиты расходятся, тогда из недр земли в образующийся проем поступает лава, таким образом образуются хребты. Например в Атлантическом окиане образовался срединно- атлантический хребет.
Result of Convergence and Divergence of Lithospheric Plates
The result of the convergence and divergence of lithospheric plates is a fundamental concept in plate tectonics, explaining the movement and interaction of the Earth's outer shell. Here's a detailed explanation based on the search results:
Convergence of Lithospheric Plates: When lithospheric plates converge, they can interact in several ways, leading to various geological features and phenomena. Convergence occurs at convergent plate boundaries, where plates move toward each other. The following are the key results of lithospheric plate convergence:
1. Subduction Zone Formation: - One plate may be forced beneath the other in a process known as subduction, leading to the formation of subduction zones. - This process can result in the formation of deep ocean trenches and volcanic arcs. - Source: 2. Mountain Building: - Convergence can lead to the uplift and formation of mountain ranges as a result of the collision and compression of lithospheric plates. - The Himalayas are a prominent example of mountains formed by the convergence of the Indian and Eurasian plates. - Source: 3. Earthquakes and Volcanic Activity: - The convergence of plates can result in intense seismic activity and volcanic eruptions due to the immense pressure and friction generated at the plate boundary. - Source: Divergence of Lithospheric Plates: When lithospheric plates diverge, they move away from each other, leading to the formation of new crust. Divergence occurs at divergent plate boundaries, such as mid-ocean ridges. The following are the key results of lithospheric plate divergence:
1. Seafloor Spreading: - Divergence at mid-ocean ridges leads to the upwelling of magma from the mantle, creating new oceanic crust as the plates move apart. - This process is known as seafloor spreading and results in the formation of mid-ocean ridges. - Source: 2. Rift Valley Formation: - Divergence can lead to the formation of rift valleys on continents, where the lithosphere is being pulled apart. - The East African Rift is a notable example of a rift valley formed by the divergence of the African Plate. - Source: 3. Creation of Ocean Basins: - The continuous divergence of plates can lead to the formation of new ocean basins as the crust spreads and cools, creating a new ocean floor. - Source: In summary, the convergence and divergence of lithospheric plates result in a wide range of geological phenomena, shaping the Earth's surface and contributing to processes such as mountain building, seafloor spreading, and the formation of geological hazards like earthquakes and volcanic activity.
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