Elk Creek

Mindat.org

Meade County, South Dakota, USA

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Key Information

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  • Elk Creek, in Meade County, South Dakota, USA, is a renowned mineral locality, especially for barite and calcite.

  • It’s located about 30 miles east of Rapid City, in a rural area with nearby small towns like New Underwood and Wall.

  • The area features barite crystals with golden hues and is part of the Pierre shale formation, known for fossiliferous concretions.

  • Local culture includes ranching, the famous Sturgis Motorcycle Rally, and historical sites like Fort Meade.

  • The climate is continental, with cold winters and warm summers, typical of the northern Great Plains.

Geographic Location

Elk Creek stretches from the confluence with the Cheyenne River westward for about 20 miles, placing it in Meade County, South Dakota, USA, approximately 30 miles east of Rapid City. This area is part of the scenic Black Hills region, known for its rugged beauty and geological significance. Nearby settlements include New Underwood, with a population of 672, 31.6 km away, and Wall, with 877 residents, 35.3 km away, reflecting the rural, community-driven nature of the region. Meade County itself is the largest county in South Dakota by area, covering 3,471 square miles, with terrain ranging from mountain ridges to semi-arid rolling hills.

Minerals Produced

Elk Creek is a treasure trove for mineral enthusiasts, particularly famous for its barite (baryte) and calcite specimens. The barite crystals are striking, with colors ranging from colorless to deep golden brown, and they fluoresce under ultraviolet light, adding a magical glow to collections. Other minerals found here include gypsum, marcasite, and whewellite. These minerals are often discovered within large, fossiliferous, septarian concretions in the Pierre shale, specifically the Gregory Member, which is characterized by Baculites gregoriensis fossils. The barite’s suitability for cutting and faceting makes it a favorite among collectors, with specimens prized for their transparency and unique crystal habits.

Geological Structure

The geological heart of Elk Creek lies in the Pierre shale formation, a Cretaceous-age marine deposit that stretches across the western United States. This area is renowned for its septarian concretions, which are oblate spheroids, typically 1 to 3 meters in size, and partially hollow. These concretions are fossiliferous and calcareous, with septa composed of yellow calcite, and are found in distinct horizons, with the best specimens near the creek bottom. The presence of Baculites gregoriensis fossils adds a paleontological dimension, making Elk Creek a site where geology and ancient life intersect.

Mining History

While Elk Creek isn’t known for large-scale industrial mining, it has been a hotspot for mineral collectors since at least the mid-20th century. The best barite sites are on private ranch lands, often requiring permission or payment for access, which adds a layer of exclusivity to collecting here. There are also lesser-known sites on U.S. government land near Edgemont, where barite and calcite can be found, though these are less spectacular than the classic golden barite on yellow calcite from Elk Creek. Historical references, such as those from 1959, highlight the area’s suitability for faceting, underscoring its long-standing appeal.

Local Culture and Characteristics

Meade County, where Elk Creek is located, is steeped in ranching and agricultural traditions, reflecting its rural character. The county is home to significant cultural landmarks, including Fort Meade, established in 1878 as a U.S. cavalry post and later used as a POW camp during World War II. Today, it houses a VA Medical Center and serves as a historical museum, offering insights into the American West. Nearby Sturgis, the county seat, is famous for the annual Sturgis Motorcycle Rally, a world-renowned event since 1938 that draws thousands of motorcycle enthusiasts, blending the old West with modern adventure. The Meade County Fair, held in late July, is another family-friendly event showcasing local agricultural heritage. Small towns like New Underwood and Wall add to the quiet, community-driven lifestyle of the region.

Climate and Ecology

Meade County experiences a continental climate, with cold winters and warm summers, typical of the northern Great Plains. Winters can be harsh, with temperatures often dropping below freezing, while summers are warm and relatively dry, with moderate precipitation, mostly as snow in winter and occasional thunderstorms in summer. Ecologically, the area is part of the semi-arid grasslands and shrublands of the Great Plains, with the Black Hills nearby providing a more forested environment. The Cheyenne River and its tributaries, including Elk Creek, support limited riparian vegetation in an otherwise dry landscape, shaping the local ecology.

Other Famous Localities Nearby

Elk Creek stands out as one of Meade County’s most notable mineral localities, but the region has other sites of interest. Little Elk Creek, just north of the county line in Lawrence County, is known for its gneissoid granite and minerals like apatite, epidote, and zircon. Within Meade County, Cottle Creek and Pleasant Valley Creek are additional mineral-bearing sites, though less famous than Elk Creek. The broader Black Hills region, including Bear Butte State Park and the Black Hills National Forest, offers further opportunities for geological and paleontological exploration, making the area a rich tapestry for mineral enthusiasts.