![]() This intrusive area consists mainly of stocks and laccoliths ranging from the late Cretaceous to the mid- Tertiary ( ). The Little Rockies are a dissected domal structure due to the laccolithic intrusion of phosphycitic rock ( Landusky and Zortman Historic Context ( This site may be offline.) ). The Little Rocky Mountains are part of the Central Montana Alkalic Province that extends from Yellowstone National Park to the northeast Canadian border. ![]() The western boundary of the reservation is dominated by three buttes Twin Buttes, Wild Horse Butte and Snake Butte ( Fort Belknap Reservation ( more info) ). The southern part of Fort Belknap drains into the Missouri River and consists of rolling grassland, river "breaks", and the Bearpaw and Little Rocky Mountain ranges which reach an elevation of approximately 6,000 feet ( Fort Belknap Indian Community: Community Environmental Profile ( more info) ). Most of the reservation drains into the Milk River (northern boundary of reservation) and consists of flat treeless glacier plains and alluvial bottom lands. The Fort Belknap Reservation covers alluvial bottom land, glacial till plains, and the Bearpaw and Little Rocky Mountain ranges. ( Fort Belknap Reservation ( more info) ). Elevations within the reservation range from 2,300 ft. ![]() The southern portion of Fort Belknap is located in the Little Rocky Mountains ( Fort Belknap Reservation ( more info) ). Located at approximately 48 degrees N and 108 degrees W, most of the reservation is located on the northern Great Plains ( more info). Figure 1: Cross Section of Fort Belknap Reservation.
0 Comments
Leave a Reply.AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |