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Antelope creek at Stanton Arizona?

Geological Features of Rich Hill with Antelope Creek at Stanton, Arizona​

Rich Hill, located near Stanton, Arizona, is known for its significant geological features and gold mining history. The area is characterized by the following geological aspects:

Gold Mining History:
  • Rich Hill is famous for the quality and quantity of gold that has been found in its vicinity. The drainages surrounding Rich Hill are the legendary Weaver and Antelope creeks that have been the source of successful placering operations for a century or more.
  • The area has been a significant gold mining location for nearly 150 years, with gold being found in the gulches and washes in and around Rich Hill, especially along the Antelope and Weaver Creek areas.
  • The discovery of gold nuggets the size of potatoes on the top of Rich Hill led to it becoming the richest gold placer discovery in Arizona. Miners also found deposits of gold in nearby Weaver and Antelope Creeks.
Geological Composition:
  • The Weaver Mountains, where Rich Hill is located, are composed principally of Precambrian granites and schists that contain numerous gold-bearing veins considered to be of Laramide age.
  • Rich Hill lies between the deeply eroded canyons at Antelope Creek on the west and Weaver Creek on the east.
Formation of Antelope Canyon:
  • Antelope Canyon, located in the vicinity, was formed by the erosion of Navajo Sandstone due to flash flooding and other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways.
In summary, Rich Hill and its surrounding area, including Antelope Creek, are characterized by their rich gold mining history, the geological composition of the Weaver Mountains, and the formation of nearby natural wonders such as Antelope Canyon.
 

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