Geodiversity refers to the full variety of natural geologic (rocks, minerals, sediments, fossils, landforms, and physical processes) and soil resources and processes that occur in the park. A product of the Geologic Resources Inventory, the NPS Geodiversity Atlas delivers information in support of education, Geoconservation, and integrated management of living (biotic) and non-living (abiotic) components of the ecosystem.
Geologic Features and Processes
[Site Under Development]
Pea Ridge National Military Park, authorized on July 20, 1956, commemorates a pivotal 1862 Union victory over Confederate troops (including ~1,000 Cherokee and Choctaw-Chickasaw Indians) to maintain control of Missouri during the American Civil War. This battle was crucial to the Mississippi campaign. The military park covers 4,300.35 acres (Federal: 4,278.75 acres) of rolling hills in northwestern Arkansas. Located in Benton County, the park is 7 km (4.5 miles) northeast of Rogers and Bentonville, Arkansas. The military park also includes a small, 56-acre outlying unit that is unnamed.
The park sits on the boundary between the Pea Ridge and Garfield 7.5-minute quadrangles between the Big Sugar Creek and Little Sugar Creek drainages. The dominant physiographic landforms in the park are Elkhorn Mountain (elevation > 490 m, 1,600 ft) and Round Mountain (elevation >460 m, 1,520 ft). These are erosional remnants of a large-scale plateau. The stratigraphy of the area includes nearly flat-lying, relatively undeformed sedimentary strata. The primary geologic unit in the park vicinity is the Mississippian-age Boone Formation. This unit is susceptible to karstification including cave and sinkhole development. Locally, this limestone-rich unit is capped by resistant sandstones, possibly of the Batesville Sandstone unit. This resistant unit caps the highest hills in the region. Dissected plateaus, ridges separated by valleys and ravines, and gently rolling open areas characterize the landscape at the military park. These landforms had strong connections to the historical context of the area.
Pea Ridge National Military Park is a part of the Ozark Plateaus Physiographic Province and shares its geologic history and some characteristic geologic formations with a region that extends well beyond park boundaries.
Geologic Resources Inventory
- Scoping summaries are records of scoping meetings where NPS staff and local geologists determined the park’s geologic mapping plan and what content should be included in the report.
- Digital geologic maps include files for viewing in GIS software, a guide to using the data, and a document with ancillary map information. Newer products also include data viewable in Google Earth and online map services.
- Reports use the maps to discuss the park’s setting and significance, notable geologic features and processes, geologic resource management issues, and geologic history.
- Posters are a static view of the GIS data in PDF format. Newer posters include aerial imagery or shaded relief and other park information. They are also included with the reports.
- Projects list basic information about the program and all products available for a park.
Related ArticlesPea Ridge National Military Park
National Park Service Geodiversity Atlas
The servicewide Geodiversity Atlas provides information on geoheritage and geodiversity resources and values within the National Park System. This information supports science-based geoconservation and interpretation in the NPS, as well as STEM education in schools, museums, and field camps. The NPS Geologic Resources Division and many parks work with National and International geoconservation communities to ensure that NPS abiotic resources are managed using the highest standards and best practices available.
For more information on the NPS Geodiversity Atlas, contact us.
Series: National Park Service Geodiversity Atlas
Last updated: October 29, 2019