The Hormuz Formation, Hormuz Series, Hormuz Evaporites or Hormuz Group is a sequence of evaporites that were deposited during the Ediacaran to Early Cambrian, a period previously referred to as the In
Salt glaciers (dark grey areas) derived from Hormuz halites, extruding from anticlinal crests in the Zagros Mountains of southern Iran
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust
Satellite image of a fault in the Taklamakan Desert. The two colorful ridges (at bottom left and top right) used to form a single continuous line, but have been split apart by movement along the fault.
Hanging wall and footwall
Cross-section diagram of a listric fault
Cross-section diagram of multiple listric faults in a cliff wall