Question

Distinguish between:
1. Converging and diverging tectonic plates.
2. Bhangar and Khadar
3. Western Ghats and Eastern Ghats

Answer 1

Hint: Structural Plate is a logical thought portraying the gigantic scope movement of 7 huge plates and the activities of a greater scope of more modest plates of Earth's lithosphere. Structural methods began this planet around $3.5$ billion years back. The model expands on the possibility of a mainland stream.

Complete answer:
Converging tectonic plate: The tectonic plates circulate towards each other in convergent plate barriers. The 2 plates coming together may additionally, both collide or can also slide beneath the other. The convergence of plated may additionally result in activities like earthquakes. The formation of the Himalayas is the result of the convergence of plates.
Divergent tectonic plates: Tectonic plates circulate away from every difference in divergent plate boundaries. The 2 plates drift faraway from each different, growing hole among the two. Divergence of plates may also result in volcanic eruptions. Formation of excellent Atlantic go with the flow is an end result of the divergence of plates.
Bhangar Soils: (old) The Bhangar Soils are positioned inside the higher reaches or about 30 meters above the flood stage. Those are coarser in texture. Those soils are much less fertile as these are decided on higher reaches.
Khadar Soils: (new) The Khadar soils are determined within the low areas of the valley, the backside of a valley which are flooded every 12 months. These soils are finer in texture. The Khadar soils are greater fertile as these are discovered in low areas.
Western Ghats: The Western Ghats shape the western arm of the peninsular plateau. These Ghats are normal and relatively higher in elevation than the Eastern Ghats. Advancing towards the south, their elevation is going on increasing. No essential river has reduced throughout them. The Western Ghats face the Arabian Sea and purpose heavy rainfall.
Eastern Ghats: The Ghats lie parallel to the Western coast and form the Jap aspect of the peninsular plateaus. The Eastern Ghats are comparatively stripped, resulting in low elevation. The Eastern Ghats face the Bay of Bengal and do not now purpose a whole lot of rainfall.

Note: Due to the fact they do no longer all circulate in the identical route, plates regularly directly collide or circulate laterally alongside each other, a tectonic surrounding that makes earthquakes common.