Skip to main content
College of Physical and Mathematical Sciences
Department of Geological Sciences

Fault Core

Scarp core.jpeg

(Photo by Bill Harris)

The impermeable core zone of the fault is seen near Rock Canyon. This pulverized and sheared rock has been re-cemented together by dissolved calcite moving along the fault in water. The fault forms a barrier to the movement of water through the fault. However, water moves quite easily along or parallel to the fault.

Wasatch Fault Menu

Home Page
Introduction
Tertiary Paleomap
Fault Scarp
Fault from Space
Basin and Range
Wasatch Fault and BYU
Wasatch Fault Animation
Tertiary Tectonics
Extension Clay Animation
Geologic Map