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Bothwell Lodge State Historic Site is a state-owned property located north of Sedalia, Missouri, United States, preserving the 31-room, 12,000-square-foot summer home, Bothwell Lodge, built for Sedalia attorney John Homer Bothwell. The site offers tours and trails for hiking and mountain biking.
The Southwest Missouri Prehistoric Rock Shelter and Cave Sites Discontiguous Archeological District is a historic district spread out over discontiguous sites in four Missouri counties. It includes 20 contributing sites. It was listed on the National Register of Historic Places in 1991. [1] [2]
This article comprises three sortable tables of the significant mountain peaks of Missouri. This article defines a significant mountain peak as a summit with at least 100 meters (328.1 feet) of topographic prominence , and a major summit as a summit with at least 500 meters (1640 feet) of topographic prominence.
The United States Congress designated the Bell Mountain Wilderness in 1980. The wilderness area now has a total of 9,027 acres (36.53 km 2). Bell Mountain is located within the Potosi-Fredericktown Ranger District of the Mark Twain National Forest, south of Potosi, Missouri in the United States.
The Campbell Archeological Site (), is an archaeological site in Southeastern Missouri occupied by the Late Mississippian Period Nodena phase from 1350 to 1541 CE. The site features a large platform mound and village area, as well as several cemeteries.
The Riverbluff Cave is a paleontological site discovered in the United States, near Springfield, Missouri.The entrance is filled with stalactites, stalagmites and columns. . The cave is about 830,000 years old (making it the oldest known fossil cave site in the US [1]) and 610 m long, featuring Pleistocene fossils, notably of the short-faced bear (Artcodus simus) the largest bear species on ...
The News-Leader compiled a list of 10 spots throughout the Ozarks, including Missouri State University and Dogwood Canyon, with the best fall foliage.
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.
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