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The Monongahela National Forest is a national forest located in the Allegheny Mountains of eastern West Virginia, USA. It protects over 921,000 acres of federally managed land within a 1,700,000 acres proclamation boundary that includes much of the Potomac Highlands Region and portions of 10 counties.
The Gauley River is a 105-mile-long (169 km) river in West Virginia. It merges with the New River to form the Kanawha River, a tributary of the Ohio River. The river features numerous recreational whitewater areas, including those in Gauley River National Recreation Area downstream of the Summersville Dam.
The Williams River is a tributary of the Gauley River, 33 miles (53 km) long, in east-central West Virginia, USA. Via the Gauley, Kanawha and Ohio Rivers, it is part of the watershed of the Mississippi River, draining an area of 132 square miles (342 km²) in a sparsely populated region of the southern Allegheny Mountains and the unglaciated portion of the Allegheny Plateau.
The Cranberry River is a tributary of the Gauley River located in southeastern West Virginia in the United States. It is a part of the Mississippi River watershed, by way of the Gauley, Kanawha, and Ohio Rivers, draining an area of 74 square miles (192 km2).
The Meadowcroft Rockshelter is an archaeological site which is located near Avella in Jefferson Township, Pennsylvania. The site is a rock shelter in a bluff overlooking Cross Creek, and contains evidence that the area may have been continually inhabited for more than 19,000 years. If accurately dated, it would be one of the earliest known sites with evidence of a human presence and continuous human occupation in the New World.
The Stanfield-Worley Bluff Shelter, located on private property in Colbert County in northwestern Alabama, United States, is one of the most important prehistoric sites excavated in the state due to the archeological evidence deposited by the Paleo-Indians who once occupied the rock shelter. Lying in Sanderson Cove along a tributary of Cane Creek approximately seven miles (11 km) south of the Tennessee Valley, the shelter and the high bluffs of the surrounding valley provided a well-protected environment for the Native American occupants.
Gatecliff Rockshelter (26NY301) is a major archaeological site in the Great Basin area of the western United States that provides remarkable stratigraphy; it has been called the "deepest archaeological rock shelter in the Americas". Located in Mill Canyon of the Toquima Range in the Monitor Valley of central Nevada, Gatecliff Rockshelter has an elevation of 7,750 feet (2,360 m). David Hurst Thomas discovered Gatecliff Rockshelter in 1970 and began excavations in 1971. Full scale excavations occurred at Gatecliff Rockshelter for about seven field seasons in which nearly 33 feet (10 m) of sediments were exposed for a well-defined stratigraphic sequence. The well-preserved artifacts and undisturbed sediments at Gatecliff Rockshelter provides data and information have been applied to a range of research topics. Based on the analysis of the artifacts at Gatecliff Rockshelter, it can be determined that it was most likely a short-term field camp throughout prehistory. The latest evidence for human usage at Gatecliff occurs between ca. 5500 B.P. to 1250 B.P.
The Prehistory of West Virginia spans ancient times until the arrival of Europeans in the early 17th century. Hunters ventured into West Virginia's mountain valleys and made temporary camp villages since the Archaic period in the Americas. Many ancient human-made earthen mounds from various mound builder cultures survive, especially in the areas of Moundsville, South Charleston, and Romney. The artifacts uncovered in these areas give evidence of a village society with a tribal trade system culture that included limited cold worked copper. As of 2009, over 12,500 archaeological sites have been documented in West Virginia.
The Cranberry Wilderness is a 47,815-acre (19,350 ha) U.S. wilderness area in the Monongahela National Forest of southeast West Virginia, United States. Its name derives from the nearby Cranberry Glades as well as from the Cranberry River and Cranberry Mountain. In addition to being wilderness, it is a designated black bear sanctuary.
Barton Village Site, also known as the Herman Barton Indian Village Archeological Site, is a large, multi-component archaeological site near Cumberland in Allegany County, Maryland.
The LoDaisKa site is a prominent archaeological site in the U.S. state of Colorado, located within a rockshelter near Morrison. The rockshelter was first inhabited by people of the Archaic through the Middle Ceramic period, generally spanning 3000 BC to 1000 AD.
Franktown Cave is located 25 miles (40 km) south of Denver, Colorado on the north edge of the Palmer Divide. It is the largest rock shelter documented on the Palmer Divide, which contains artifacts from many prehistoric cultures. Prehistoric hunter-gatherers occupied Franktown Cave intermittently for 8,000 years beginning about 6400 BC The site held remarkable lithic and ceramic artifacts, but it is better known for its perishable artifacts, including animal hides, wood, fiber and corn. Material goods were produced for their comfort, task-simplification and religious celebration. There is evidence of the site being a campsite or dwelling as recently as AD 1725.
The Trinchera Cave Archeological District (5LA9555) is an archaeological site in Las Animas County, Colorado with artifacts primarily dating from 1000 BC to AD 1749, although there were some Archaic period artifacts found. The site was added to the National Register of Historic Places in 2001 and is located on State Trust Lands.
The Cherry Creek Rockshelter is an archaeological site in central Colorado, located within modern-day Castlewood Canyon State Park near Franktown, Colorado. Current research indicates that it was used by Native American inhabitants beginning in the Archaic period. The site is situated on the Palmer Divide, which allowed for a unique prehistoric environment that contributed to an abundance of food and water sources, as well as lithic materials for tool-making. These factors, combined with the structure and situation of the shelter itself, made the site a particularly attractive environment for prehistoric peoples to settle in. Archaeological study of the site began in 1955, with the most current original research concluding in 2002.
Site AU-154 is an archaeological site in Shenandoah National Park, in Augusta County, Virginia, United States.
The Paine Run Rockshelter (44-AU-158) is an archaeological site in Shenandoah National Park, in Augusta County, Virginia, United States.
The Rockhouse Cliffs Rockshelters are a pair of rockshelters in the far southern region of the U.S. state of Indiana. Located amid broken terrain in the Hoosier National Forest, the shelters may have been inhabited for more than ten thousand years by peoples ranging from the Early Archaic period until the twentieth century. As a result of their extensive occupation and their remote location, they are important and well-preserved archaeological sites and have been named a historic site.
Craig Run East Fork Rockshelter is a historic archaeological site located near Mills Mountain, Webster County, West Virginia. It is one of a number of prehistoric rock shelters on the Gauley Ranger District, Monongahela National Forest, that are known to have been utilized prehistorically from the Middle Archaic through the Late Woodland period, c. 6000 B.C. – 1200 A.D. In more recent history, the Craig Run rock shelter is known to have served as a stable for a donkey which was employed in the locust post industry.
The Hidden Valley Rockshelter (44-BA-31) is a significant archaeological site located near the community of Warm Springs in Bath County, Virginia, United States. A large rockshelter located near the Jackson River, it has been occupied by humans for thousands of years, and it has been named a historic site.
Durst Rockshelter State Natural Area is a privately owned state natural area located roughly 1 mile (1.6 km) north of Leland, Wisconsin. The property encompasses a rock shelter inhabited by pre-Columbian Native Americans. Archaeological excavations at the rock shelter have uncovered projectile points and ceramic artifacts. The oldest artifacts date to the Archaic period from roughly 4000 to 3500 B.C., though the site was inhabited by multiple cultural groups across several periods of development. The rockshelter is surrounded by a mesic forest split by a sandstone ridge.
References
- 1 2 "National Register Information System". National Register of Historic Places . National Park Service. July 9, 2010.
- ↑ Anne M. Jensen (January 1993). "National Register of Historic Places Inventory Nomination Form: Rockshelters on the Gauley Ranger District, Monongahela National Forest" (PDF). State of West Virginia, West Virginia Division of Culture and History, Historic Preservation.
