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Broken Bow Lake is a reservoir in southeastern Oklahoma, located on Mountain Fork River and 9 miles (14 km) northeast of the town of Broken Bow in McCurtain County. It is one of the largest fresh water lakes within the state of Oklahoma, and a popular tourist destination for locals and visitors from neighboring Texas and Arkansas .
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Broken Bow Reservoir is located within the state park. Broken Bow spillway overlook Bridge across Mountain Fork River A vista of Broken Bow Lake. Beavers Bend State Park is a 3,482 [2] acres (14.09 km 2) Oklahoma state park located in McCurtain County. It is approximately 10.5 miles (16.9 km) north of Broken Bow on SH-259A. [3]
The Upper Mountain Fork River offers 31.7 miles (51.0 km) of canoeing or kayaking from near Hatfield, Arkansas to Broken Bow Lake. This part of the river has class I and II rapids. clear water, fishing for smallmouth bass and other species, and excellent scenery with pine forests covering the hills and bluffs along the river's course.
Lake Eufaula: On a peninsula in Lake Eufaula. Lodge and cabins are closed. Now known as Arrowhead Area at Lake Eufaula State Park. Beavers Bend State Park: McCurtain: 3,482 1,409: 1935: Mountain Fork River, Broken Bow Lake: Bernice State Park: Delaware: 88 36: 1970: Grand Lake o' the Cherokees: Now known as the Bernice Area at Grand Lake State ...
The town of 219 — just north of Broken Bow, with Broken Bow Lake directly to the east — becomes laden with as many as 50,000 visitors on the weekends. ... there were 400 cabins for rent in the ...
Hochatown State Park was named after the small town of Hochatown.Present-day Hochatown is actually the second community in the area to bear the name. The original community was forced to relocate to its current location on U.S. Route 259 when Broken Bow Lake was created through the damming of Mountain Fork River by the United States Army Corps of Engineers in the late 1960s.
The Coastal Plain is the largest geographic area of the state, and covers roughly 45% of North Carolina. The Coastal Plain begins along the fall line , a line that marks the boundary between metamorphic/igneous rocks of the Piedmont province (to the west) and sedimentary rocks of the Coastal Plain province (to the east).
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