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The name was given to the valley by miners after the Black Hills Gold Rush of 1874–1877. The gold rush directly led to the Great Sioux War of 1876 (Black Hills War), in which the US Army drove the Lakota Sioux and Cheyenne people from their traditional lands in the Black Hills. Pactola was eventually left behind by the miners in search of ...
Sitting Bull Crystal Caverns was a limestone cave complex nine miles south of Rapid City, South Dakota on the way to Mount Rushmore and by the Wind Cave National Park. From 1934 to 2015, the cave was open for the public to tour daily from Memorial Day weekend to Labor Day weekend. [1] [2]
John Eli Perrett (February 9, 1866 or 1868 – February 26, 1943), better known as Potato Creek Johnny, [a] was an American frontiersman and gold miner, best known for having discovered one of the largest gold nuggets ever discovered in the Black Hills in 1929. From then until the end of his life, Potato Creek Johnny became a local celebrity ...
The Monument, formerly known as Rushmore Plaza Civic Center and Rushmore Plaza, is a 500,000-square-foot (46,000 m 2) [1] exhibition center, in Rapid City, South Dakota.The Monument is the main event center for the Black Hills Region, serving Western South Dakota, South West North Dakota, North West Nebraska, and Eastern Wyoming.
Pactola Lake is the largest and deepest reservoir in the Black Hills, located 15 miles west of Rapid City, South Dakota, United States.Constructed in 1952, the dam and waters are managed by the Bureau of Reclamation, with the surrounding land managed by the US Forest Service as part of Black Hills National Forest, which operates a visitor center located on the south side of the dam. [2]
Mystic is located in the Black Hills in Pennington County, South Dakota.It is on Castle Creek, about 20 miles (32 km) west of Rapid City and 12 miles (19 km) north of Hill City, at the intersection of Mystic Road/County Road 231 and George Frink Road.
The faults and joints are associated with the uplift of the Black Hills approximately 58 to 54 million years ago. After main cave dissolution, a thick layer of calcite lined the walls about 2.5 million years ago. [11]: 12 During cave development and afterwards, speleothems and speleogens formed, including the "jewels" or spar.
Off U.S. Route 16, geographically located 1.5 miles (2.4 km) northeast of Rockerville bearing 2 miles (3.2 km) southwest of Colonial Pine Hills, is the Stratosphere Bowl. [2] A geological depression located in the narrow middle valley of Spring Creek, made famous in the 1930s serving as a discharge site for the Explorer II being two US Army and ...
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