The surface of Earth is being reshaped constantly. Mountainous uplands are broken down by water and wind producing sediment that is moved by rivers to lowlands. Some of this sediment is deposited along the way, some is delivered to the coast and continental shelf, and some makes its way to the ultimate sink, the deep sea
Here is the original post:
Linking Erosional and Depositional Landscapes
If you enjoyed this post, make sure you subscribe to my RSS feed!