Analyses the sequential development of landforms in either Karst or Coastal region.
The sequential development of landforms in a Karst region typically follows the following stages: Initial topography: The initial topography in a Karst region is typically characterized by flat-lying, homogenous beds of soluble rock such as limestone or dolomite. Underground drainage: As precipitation infiltrates into the soluble rock, it dissolves it and creates a network of …
Analyses the sequential development of landforms in either Karst or Coastal region. Read More »