E. F. McBride
Geo. 420K
Spring, 2000

 

PROCESS WHAT  WHY  HOW RECOGNIZED
Transgression  Landward migration of shoreline Rise in SL; subsidence Upward deepening facies
Regression Seaward migration of shoreline Lowered SL; basin uplift Upward shallowing facies
Progradation  Sediment interface moves seaward Deposition rate exceeds dispersal Upward shallowing facies 
Erosion (degradation) Erosion  Removal of sediment Scour surface; missing fossils

efmcbride@mail.utexas.edu
Geological Sciences
U. Texas at Austin