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Washita Battlefield National Historic Site protects and interprets the site of the Southern Cheyenne village of Chief Black Kettle where the Battle of Washita occurred. The site is located about 150 miles (241 km) west of Oklahoma City, Oklahoma, near Cheyenne, Oklahoma.
The Black Kettle National Grassland, in Roger Mills County, Oklahoma, and Hemphill County, Texas, contains 31,286 acres (12,661 ha) of which 30,710 acres (12,430 ha) are in Oklahoma. [ 1 ]
Black Kettle (Cheyenne: Mo'ohtavetoo'o) [1] (c. 1803 – November 27, 1868) was a leader of the Southern Cheyenne during the American Indian Wars.Born to the Northern Só'taeo'o / Só'taétaneo'o band of the Northern Cheyenne in the Black Hills of present-day South Dakota, [2] he later married into the Wotápio / Wutapai band (one mixed Cheyenne-Kiowa band with Lakota Sioux origin) of the ...
The Battle of the Washita River (also called Battle of the Washita or the Washita Massacre [4]) occurred on November 27, 1868, when Lt. Col. George Armstrong Custer's 7th U.S. Cavalry attacked Black Kettle's Southern Cheyenne camp on the Washita River (the present-day Washita Battlefield National Historic Site near Cheyenne, Oklahoma).
The lake and the adjacent Black Kettle Recreation Area [5] are all part of the Black Kettle National Grassland, [6] [7] which is managed by the Cibola National Forest. [8] The lake is about 80 acres in size. [3] Popular species of fish caught here include flathead catfish, black drum, and blue catfish. [9]
The Cibola National Forest is organized into several divisions over three states. The Rita Blanca National Grassland 92,989 acres (376.3 km 2) in Dallam County, Texas, and Cimarron County, Oklahoma, Black Kettle National Grassland 31,286 acres (126.6 km 2) in Roger Mills County, Oklahoma, and Hemphill County, Texas, and McClellan Creek National Grassland 1,449 acres (5.9 km 2) in Gray County ...
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A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased ...