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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 Lake of the Ozarks is located on the Ozark Plateau, with Bagnell Dam lying at an elevation of 659 feet (201 m) above sea level. [6] [17] It lies in central Missouri on the Salem Plateau of the Ozarks. [18] The lake extends across four Missouri counties, from Benton County in the west through Camden and Morgan Counties to Miller County in ...
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Map all coordinates using OpenStreetMap. ... Pages in category "Lakes of Missouri" ... Spanish Lake (Missouri) V. Valley Water Mill Pond
NPS map of the Riverways Rocky Falls on Rocky Creek, a tributary of the Current River. The Ozark National Scenic Riverways is a recreational unit of the National Park Service in the Ozarks of southern Missouri in the U.S. The park was created by an Act of Congress in 1964 to protect the Current and Jacks Fork rivers, and it was formally ...
Taum Sauk Mountain State Park is a Missouri state park located in the St. Francois Mountains in the Ozarks. The park encompasses Taum Sauk Mountain , the highest point in the state . [ 4 ] The Taum Sauk portion of the Ozark Trail connects the park with nearby Johnson's Shut-ins State Park [ 5 ] and the Bell Mountain Wilderness Area , which ...
Devils Well is a sinkhole cave near Akers in the U.S. state of Missouri, containing an underground lake that is the largest in the state. [1] It is a part of the Ozark National Scenic Riverways and can be viewed by the public any day during daylight hours. The U.S. Park Service has set up a metal staircase and a switch-activated light; however ...
Meramec Caverns is the collective name for a 4.6-mile (7.4 km) cavern system in the Ozarks, near Stanton, Missouri. [1] The caverns were formed from the erosion of large limestone deposits over millions of years.