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The Lake of the Ozarks Community Bridge is a continuous truss bridge in Lake Ozark. The bridge is over 2,695 ft (821 m) long and 72 ft (22 m) wide. [ 31 ] Built in 1998, it is one of the newest bridges in the Lake of the Ozarks area, primarily built to connect the east (towards Lake Ozark and Osage Beach) and west sides (towards Sunrise Beach ...
Lake of the Ozarks State Park is a public recreation area on the Grand Glaize Arm of the Lake of the Ozarks; it is the largest state park in Missouri. [4] [ A] The park includes 85 miles (137 km) of shoreline on the lake (which has a total of 1,150 miles (1,850 km) of shoreline—mostly privately owned); two swimming beaches with imported sand, 12 trails, the Ozark Caverns, a boat launch, and ...
The James River is a source of drinking water for the city of Springfield. Lake Springfield is the primary source of water for the cooling system at the James River Power Plant which sits by the dam. The lake is a popular fishing and kayaking destination with docks and access points made by the Missouri Conservation Department.
Printable version; In other projects ... Lake of the Ozarks (13 P) T. ... (2 C, 14 P) Pages in category "Bodies of water of the Ozarks"
Grandglaize Creek is a creek and tributary to the Osage River that forms the Grand Glaize Arm of the Lake of the Ozarks in Missouri. The creek flows for 10 miles (16 km) before reaching the Lake of the Ozarks, and the Grand Glaize Arm extends another 15 miles (24 km) before reaching the Osage River within the lake.
Rainy Creek is a stream in Benton and Camden Counties in the U.S. state of Missouri. [1] It is a tributary of the Osage River within the waters of the Lake of the Ozarks.. The stream headwaters arise in Camden County on the west flank of Canefield Ridge and just north of the Climax Springs Lookout Tower and Missouri Route 7 at an elevation of about 980 feet [2] (at
The park also features caves, sinkholes, and bluffs overlooking the lake. It is a prominent example of karst topography, which is geological formation shaped by the dissolution of a layer or layers of soluble bedrock. [5] A 70-acre (28 ha) portion of the park was designated as the Ha Ha Tonka Karst Natural Area in 1981. [6]
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