The mountain chains provide evidence to support the theory of continental drift by confirming that if the "mountain chains" that are now separated by "bodies of water "on different continents", would match up if these continents are placed next to each other.
<u>Explanation:</u>
According to Alfred Wegener, the one who proposed the "continental drift theory", it is evident from the similarity in the physical attributes of a few mountain chains that they were once "part of the same continent".
Other than that, the findings of identical minerals in various mountain chains also support the authenticity of the "continental drift theory".
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The base level is the lower limit of the erosional process and the ultimate base level is the plains that result from the projection of sea level under the landmass. This process of erosion creates a peneplain.
The base level is dynamic and changes according to the following factors as sea-level changes, tectonic factors, river captures, and sedimentation.
Peneplinasare low featureless deposits that are created by the terminus of the dream where the sediments are merged with the sea.
