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The Ake Site is a name for a prehistoric archaeological location near the town of Datil in the San Augustine Basin of Catron County, New Mexico, United States. It was listed on the New Mexico Register of Cultural Properties in 1975, and listed on the National Register of Historic Places in 1976. The Ake Site is particularly important for the age and length of its use by prehistoric peoples. It has been dated during the Clovis period between 10,999 BC and 8000 BC, and during the Folsom period between 7999 BC and 5999 BC, making it among the oldest sites in the American Southwest.
Obsidian Cliff, also known as 48YE433, was an important source of lithic materials for prehistoric peoples in Yellowstone National Park near Mammoth Hot Springs, Wyoming, United States. The cliff was named by Philetus Norris, the second park superintendent in 1878. It was declared a National Historic Landmark in 1996.
The Thunderbird Archaeological District, near Limeton, Virginia, is archaeological district described as consisting of "three sites—Thunderbird Site, the Fifty Site, and the Fifty Bog—which provide a stratified cultural sequence spanning Paleo-Indian cultures through the end of Early Archaic times with scattered evidence of later occupation."
The Katcef Archeological Site is an archaeological site near Crofton in Anne Arundel County, Maryland. It is a series of overlapping base camp sites dating from the Clovis phase of the Paleoindian period, through to the Late Woodland period. The primary era of site utilization was during the Late Archaic period.
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.
This is a list of the National Register of Historic Places listings in Androscoggin County, Maine.
This is a list of the National Register of Historic Places listings in Millard County, Utah.
The Burro Mesa Archeological District encompasses a quarry in Big Bend National Park used by Native Americans as a source of chert for chipped-stone tools. The quarry was used intermittently beginning in the paleoindian period starting about 12,000 to 13,000 years ago. The chert is found in a variety of colors and rests on top of tuff beds which themselves contain veins of kaolinite that was suitable for making claystone ornaments and beads. The quarry area is carpeted with lithic debris from the initial knapping process by which chert was rough-shaped into material of suitable size and shape for later refinement at more convenient locations.
Shoop Site is a prehistoric archaeological site in Jackson Township and Wayne Township, Dauphin County, Pennsylvania. It is the site of a large Paleoindian campsite, dated to 9,000-9,500 BC. It was first discovered in the 1930s by George Gordon, and also studied by Frank Soday who later discovered the Quad Site.
Shawnee-Minisink Site is a prehistoric archaeological site located in Smithfield Township, Monroe County, Pennsylvania. It was the site of a Paleoindian camp site.
Hell Gap is a deeply stratified archaeological site located in the Great Plains of eastern Wyoming, approximately thirteen miles north of Guernsey, where an abundant amount of Paleoindian and Archaic artifacts have been found and excavated since 1959. This site has had an important impact on North American archaeology because of the large quantity and breadth of prehistoric Paleoindian and Archaic period artifacts and cultures it encompasses. It was designated a National Historic Landmark in 2016.
The Witt Site is an archaeological site near Tulare Lake in Kings County, California. It was found by Donald Witt, who collected artifacts of concave points, crescents, and fossilized elephant, bison, and horse bones. The site was apparently a good location for ambushing large mammals coming to the lake.
The Last Supper Cave, near Denio, Nevada, United States, is an archeological site that is listed on the National Register of Historic Places. It was listed on the National Register in 1975, for its potential to yield information in the future.
The Carrier Mills Archaeological District is a group of prehistoric archaeological sites located along the Saline River south of Carrier Mills, Illinois. The sites were inhabited over the period from 2500 B.C. to 700 A.D. The oldest three sites date from the Late Archaic period, which encompassed the first 1500 years of occupation at the district; these sites include two small campsites and a larger base camp. Several sites were inhabited during the Early Woodland period, which lasted until 500 B.C.; these sites are distinguished by fragments of pottery, which was developed during this period. The Early Woodland period sites are likely to have been a part of the Crab Orchard culture, a local subtype of the Hopewell tradition. A number of sites date from the Middle Woodland Period, which spanned from 300 B.C. to 500 A.D.; these sites appear to have adopted the technology, but not the traditions, of the Hopewell culture. A single projectile point from the Late Woodland period has also been recovered from the site.
The LaGrange Rock Shelter is an archaeological site located on private property between Leighton and Muscle Shoals in Colbert County, Alabama near the original campus of LaGrange College. The shelter measures 70 feet long by 15 feet deep and is located beneath a sandstone outcrop overlooking a dense series of Paleoindian sites in the valley below, which may have led to it being chosen for excavation.
The Spiller Farm Paleoindian Site, designated Site 4.13 by the Maine Archaeological Survey, is a prehistoric archaeological site in Wells, Maine. Located overlooking a stream on the Spiller Farm property on Branch Road, it is an extensive site at which a fine collection of stone artifacts has been found, dating to c. 8,000 BCE. The site was listed on the National Register of Historic Places in 2003.
The McCune Mound and Village Site is a prehistoric archaeological site located in Whiteside County, Illinois near the city of Sterling. The site consists of a single mound, 3 metres (9.8 ft) high and 23 metres (75 ft) in diameter, and five depressions that may have been housing sites. The site was occupied by Upper Mississippian peoples from roughly 1200 to 1500 A.D.; it is considered part of the Langford tradition, a subset of Upper Mississippian culture found in northwestern Illinois. Modern archaeologists first documented the site in 1961. As a relatively intact site with a single-component habitation, the site was considered to have the potential to provide significant information on the Langford tradition.
The Black Mountain Archeological District is a region of the Bighorn Basin near Shell, Wyoming that contains archeological sites associated with chert deposits used in making tools and weapons. Covering 530 acres (210 ha), the area was occupied from about 11,500 years ago in the Paleoindian Period to the Late Prehistoric Period of 1500 to 400 years ago. The sites have not yielded more recent artifacts. The area contains six rock shelters, two campsites at canyon bottoms and one interfluve campsite, as well as the Black Mountain and East Spring Creek chert quarries. The local chert comes from the Phosphoria Formation, and is red in color. The district was placed on the National Register of Historic Places on July 2, 1987.
The Paint Rock Canyon Archeological Landscape District is a 5,340-acre (2,160 ha) area of Native American archeological sites on the west side of the Bighorn Mountains of Wyoming. The area contains sites ranging from the late Paleoindian period of about 9000 years before present to late Prehistoric times. The sites include open campsites and rock shelters. The district was added to the National Register of Historic Places on July 12, 1990.
The Southsider Shelter is a Native American rock shelter archeological site in Big Horn County, Wyoming.. The site has occupied from the late Paleoindian period to the Late Prehistoric period. Artifacts include projectile points and chipped stone. The site was added to the National Register of Historic Places on August 1, 2012.
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