Geothermic gradient is the rate of increasing temperature with respect to increasing the depth in the earths interior. away from tech tonic plates boundaries, it is about 25-40 c/km (72-87 degrees f/mi) of depth near the surface in most of the world.
An intrusive landform can become exposed to air by the weathering of the upper lying landmasses by different agents of weather like wind, frost, temperature, etc
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Geothermic gradient is the rate of increasing temperature with respect to increasing the depth in the earths interior. away from tech tonic plates boundaries, it is about 25-40 c/km (72-87 degrees f/mi) of depth near the surface in most of the world.
An intrusive landform can become exposed to air by the weathering of the upper lying landmasses by different agents of weather like wind, frost, temperature, etc
Explanation: