
Порівняйте карти ,,Будова земної кори "та"Фізична карта світу".Які гірські області утворюються на
межі літосферних плит?Тихоокеанська і Північноамериканська,Індо-Австралійська та Євразійська

Ответы на вопрос

Индо-австралийская и Евразийская - Гималаи



Comparison of "Structure of the Earth's Crust" and "Physical Map of the World"
The "Structure of the Earth's Crust" map and the "Physical Map of the World" provide different types of information about the Earth's surface.
The "Structure of the Earth's Crust" map focuses on the composition and structure of the Earth's crust. It typically shows the different layers of the Earth's crust, such as the continental crust and the oceanic crust, as well as the boundaries between these layers. This map may also include information about tectonic plates and their movements.
On the other hand, the "Physical Map of the World" provides a broader view of the Earth's surface features. It typically shows the physical characteristics of the Earth, such as mountains, rivers, deserts, and plains. This map may also include information about landforms, such as valleys, canyons, and plateaus.
While both maps provide valuable information about the Earth's surface, they focus on different aspects. The "Structure of the Earth's Crust" map emphasizes the composition and structure of the Earth's crust, while the "Physical Map of the World" provides a more general overview of the Earth's physical features.
Mountain Ranges Formed at the Boundaries of Lithospheric Plates
Mountain ranges often form at the boundaries of lithospheric plates, where tectonic forces cause the Earth's crust to fold, uplift, and deform. The specific mountain ranges formed at the boundaries of the Pacific and North American, Indo-Australian, and Eurasian plates are as follows:
1. Pacific and North American Plates: The boundary between the Pacific Plate and the North American Plate is marked by the San Andreas Fault in California, USA. This fault is a transform boundary, where the plates slide past each other horizontally. While the San Andreas Fault itself does not form a mountain range, the tectonic forces associated with this boundary have uplifted the Coast Ranges and the Sierra Nevada Mountains in California.
2. Indo-Australian and Eurasian Plates: The boundary between the Indo-Australian Plate and the Eurasian Plate is marked by the collision zone between the Indian subcontinent and the Eurasian continent. This collision has resulted in the formation of the Himalayas, the highest mountain range in the world. The Himalayas stretch across several countries, including India, Nepal, Bhutan, and China.
It's important to note that the formation of mountain ranges is a complex process influenced by various geological factors. The boundaries mentioned above are just a few examples of where mountain ranges have formed due to plate tectonics.
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