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Geologic map of the Michigan Basin. The Michigan Basin is a geologic basin centered on the Lower Peninsula of the U.S. state of Michigan.The feature is represented by a nearly circular pattern of geologic sedimentary strata in the area with a nearly uniform structural dip toward the center of the peninsula.
Crossroads Village is a living history museum in Genesee County, Michigan, near Flint. It is operated by the Genesee County Parks and Recreation Commission alongside the Huckleberry Railroad. Initially proposed as a Flint River recreational area and a farm museum, it was opened as a historical village in 1976.
The Konza Prairie Biological Station is a 8,616-acre (3,487 ha) protected area of native tallgrass prairie in the Flint Hills of northeastern Kansas. "Konza" is an alternative name for the Kansa or Kaw Indians who inhabited this area until the mid-19th century. [1] The Konza Prairie is owned by The Nature Conservancy and Kansas State University.
Grand Mere State Park is a public recreation and nature preservation area in the southwestern part of the U.S. state of Michigan near Stevensville. The state park is located adjacent to Interstate 94. Protected from Lake Michigan by the dunes to the west, the park has many natural features not found throughout the rest of the state. [3]
The camp was used from 1935 to 1941 as a Michigan Social Welfare Community Organization site to house workers employed in the forest. In 1967, the Iron County Sportsman Club purchased the camp. Camp Gibbs contains 16 single-story wood-frame, gable -roof buildings, plus the sites of three other buildings that have been demolished.
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Fort Custer State Recreation Area is a 3,033-acre (12 km 2) State Recreation Area located between Battle Creek and Kalamazoo, Michigan.The area features lakes, the Kalamazoo River, over 25 miles of multi-use trails, second growth oak barrens and dry-mesic southern (oak-hickory) forests.
View of Lake Superior from Brockway Mountain, near Copper Harbor in Keweenaw County The peninsula measures about 150 miles (240 km) in length and about 50 miles (80 km) in width at its base. The ancient lava flows of the Keweenaw Peninsula were produced during the Mesoproterozoic Era as a part of the Midcontinent Rift between 1.096 and 1.087 ...