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Western Ghats | Eastern Ghats |
1.The western ghats are continuous chains of mountains and can be crossed through passes only. | 1. The Eastern ghats are not continuous and are cut by rivers falling into the Bay of Bengal. |
2.The height ranges from 900-1600 meters. | 2.Their height is lower than the western ghats, height ranges from 600 to 900 meter |
3.Most of the Peninsular rivers originate from western ghats. | 3. No major river originates from Eastern ghats. |
4. The soil is highly fertile. | 4. The soil is not so fertile here. |
5. The onset of monsoon is felt by the western ghats. | 5. The retreating of the monsoon is felt here in October and November. |
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Igneous rocks rocks are referred to as the primary rocks, because they represent the rocks which directly or indirectly provided materials for the formation of other types of rocks.
Magma erupts from volcanic eruptions and on reaching earths crust it is called lava and solidifies by cooling.Thus, cooling and solidification are the two distinct processes involved in the formation of igneous rocks.
In rock cycle the first rock that is formed is igneous rocks from them sedimentary rocks are formed and after that metamorphic rocks formed.
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Troposphere | Stratosphere |
1. It is the lowermost layer of the atmosphere. | 1. It is the second layer of the atmosphere above the earth. |
2. Its height varies from 8 km at the poles to 18 km at the equator. | 2. Its height goes upto 50 km. |
3. In this layer the temperature decreases at the rate of 1°C per 165 metres. | 3. In this layer temperature is very low and mainly constant. |
4. It is a zone of convection currents. | 4. It is the non-convective zone of the atmosphere. |
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Utsav Kumar Shukla 6 years ago
2Thank You