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The Boston Mountains are the source of rivers and streams that flow out from the mountains in all directions. Within a 3 miles (4,800 m) radius of a point just west of the summits discussed above are located the sources of the White River, the Buffalo River, the Kings River, War Eagle Creek, and Little Mulberry Creek.
Little Cobbler Mountain (North Cobbler Mountain) – Elevation 1,447 ft (441 m) Big Cobbler Mountain (South Cobbler Mountain) – Elevation 1,562 ft (476 m) 38°50′19″N 77°57′10″W / 38.8387°N 77.9528°W / 38.8387; -77.9528 ( Big Cobbler Mountain (South Cobbler Mountain
War Eagle is an unincorporated community in Benton County, Arkansas, United States. [1] It is the location of (or is the nearest community to) War Eagle Bridge, which carries CR 98 over War Eagle Creek and is listed on the National Register of Historic Places. [2] Variant names were "Blackburn Mill", "Wareagle", and "War Eagle Mills". [1]
A rural Ozarks scene. Phelps County, Missouri The Saint Francois Mountains, viewed here from Knob Lick Mountain, are the exposed geologic core of the Ozarks.. The Ozarks, also known as the Ozark Mountains, Ozark Highlands or Ozark Plateau, is a physiographic region in the U.S. states of Missouri, Arkansas, and Oklahoma, as well as a small area in the southeastern corner of Kansas. [1]
The route runs through the Boston Mountains (a subsection of The Ozarks) in Arkansas for 38 miles (61 km) in Crawford and Washington Counties. [1] [2] The route begins at Alma and runs north to Fayetteville. The route includes the Bobby Hopper Tunnel, the only road tunnel in Arkansas. This portion of I-49 was completed in 1999, when it was part ...
The stream source area is in Madison County in the Boston Mountains just west of the community of Boston and north of Arkansas Route 16 at an elevation of about 2,100 feet (640 m). [3] The stream flows northwest passing under and then running parallel to Arkansas Route 23 passing the communities of Witter and Aurora.
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The Ouachita Mountains (/ ˈ w ɒ ʃ ɪ t ɔː /), simply referred to as the Ouachitas, are a mountain range in western Arkansas and southeastern Oklahoma.They are formed by a thick succession of highly deformed Paleozoic strata constituting the Ouachita Fold and Thrust Belt, one of the important orogenic belts of North America. [3]