Converging tectonic plates | Diverging tectonic plates |
1. The plates that come towards each other and form divergent boundary are called converging tectonic plates | 1. The plates that move away from each other and form divergent boundary are called diverging tectonic plates. |
2. In the event of two plates coming together they may either collide and crumble, or one may slide under the other. | 2. They do not collide and rumble. They also do not slide under the other. |
Bhangar | Khadar |
1. Bhangar is o;ld alluvial soil. | 1. Khadar is newer alluvial soil. |
2. This soils found far from the river basins. | 2. This soil is found close to the river basins. |
3. This soil is less fertile and therefore, not suitable for agriculture. | 3. This soil is very fertile and therefore, very suitable for agriculture. |
Western Ghats | Eastern Ghats |
1. The Western Ghats are formed on the western side or arm of the peninsular plateau. | 1. The Eastern Ghats are formed on the eastern side or arm of the peninsular plateau. |
2. The western Ghats are regular and continuous and can be crossed through passes only. | The Eastern Gjhats are discontinuous and irregular and dissected by rivers draining into the Bay of Bengal. |
3. They lie parallel to the Malabar coast. | 3. They lie parallel to the Coromandel coast. |
4. They are comparatively higher in elevation. Their average elevation is 900 - 1600 meters. | 4. They have comparatively lower elevation. Their average elevation is 600 meters. |
5. The highest peaks in the Western Ghats are the Anai Mudi and the Doda Betta. | 5. The highest peak in the Eastern Ghats is Mahendragiri. |