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The Indian Field United Methodist Church is located on U.S. Highway 15 about 2 miles (3 km) north of the campground and just south of U.S. Highway 178. [5] This church began in 1787. Its first building was about 3 mi (5 km) east of the unincorporated Rosinville community at the intersection of U.S. Highways 15 and 178.
The 200-square-foot (19 m 2) rock is a part of the vertical Wingate sandstone cliffs that enclose the upper end of Indian Creek Canyon, and is covered by hundreds of petroglyphs—one of the largest, best preserved and easily accessed groups in the Southwest. The petroglyphs feature a mixture of human, animal, material and abstract forms.
Chalk Creek is a 27.3-mile-long (43.9 km) [2] river flowing east from the Collegiate Peaks mountain range in Chaffee County, Colorado. Mount Antero borders the southern side of the river, while Mount Princeton borders the northern side.
Cliffs of the Neuse State Park is a North Carolina state park near Seven Springs, North Carolina, in Wayne County covering 1,097 acres (4.4 km 2) [1] along the southern banks of the Neuse River. It has a swimming area, camp sites, hiking trails, fishing areas, and picnic areas.
High Cliff State Park is a 1,187-acre (480 ha) Wisconsin state park near Sherwood, Wisconsin.It is the only state-owned recreation area located on Lake Winnebago. [2] The park got its name from cliffs of the Niagara Escarpment, a land formation east of the shore of Lake Winnebago that stretches north through northeast Wisconsin, Upper Michigan, and Ontario to Niagara Falls and New York State.
Indian Lake is a 12-mile (19 km) long, 4,255-acre (1,722 ha) reservoir with a southwest to northeast orientation in the towns of Indian Lake and Lake Pleasant in Hamilton County, in the Adirondack Park of New York State, in the United States. The hamlet of Indian Lake is located 2 miles (3.2 km) north of the north end of Indian Lake.
Indian Creek is a climbing area in the northern part of the Bears Ears National Monument in the canyonlands area of San Juan County, Utah, United States. [ 2 ] [ 3 ] that is renowned for its sandstone crack climbing .
The colors in the cliffs are created by the large amounts of minerals in the rock. The cliffs are composed of the Munising Formation of 500-million-year-old Cambrian Period sandstone. The Munising Formation sits atop Precambrian sandstone of the Jacobsville Formation. The mottled red Jacobsville Formation is the oldest rock in the park.