Answer;
-Normal fault
Explanation;
-Normal Faults have a crustal extension and rocks above steeply inclined fault surface slip down and over rocks beneath fault surface. Reverse Faults have a crustal compression and Rocks above steeply-inclined fault surface slip up and over rocks beneath fault surface. Strike-slip faults, on the other hand have a vertical surface and Rocks on one side of fault slip laterally past rocks on other side of fault
-The Sparta Fault system is a major structure approximately 64km long that bounds the eastern flanks of the Taygetos Mountain front (2.400m) and shapes the present-day Sparta basin. This fault is examined and described in terms of its geometry, segmentation, drainage pattern and postglacial finite throw, emphasizing also how these parameters vary along strike the fault.