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The Sunken Village Archeological Site, designated by the Smithsonian trinomial 35MU4, is an archaeological site on Sauvie Island in Multnomah County, Oregon, United States. The site consists of a remarkably well-preserved Chinookan village, dating back more than 700 years. It is a major example of a wet archaeological site, in which cultural materials were preserved in an anaerobic freshwater environment. Finds at the site include well-preserved basketry. The site was declared a National Historic Landmark in 1989.
The Palugvik Site, also known as Palugvik Archeological District, is an archaeological site on Hawkins Island in Prince William Sound, near Cordova, Alaska, within Chugach National Forest. The site, first excavated in 1930, was the first to provide a view of prehistoric human habitation in Prince William Sound, the ancestral home of the Chugach people, and is one of the two primary sites for identifying the sequence of occupation in the area. The site was declared a National Historic Landmark in 1962, and listed on the National Register of Historic Places in 1966.
The Mack Canyon Archeological Site is a prehistoric archeological site in Sherman County, Oregon, United States. Consisting of an extensive series of pit houses in a sheltered canyon, the site was occupied seasonally in winter by Columbia River tribes for about 7,000 years from after 5000 BCE to the early 19th century CE.
Takli Island is an island off the southern coast of the Alaska Peninsula in the Shelikof Strait of southwestern Alaska. It is located at the mouth of Amalik Bay, off the mainland portion of Kodiak Island Borough, in Katmai National Park and Preserve. The area was first archaeologically investigated in the 1960s, when the prehistory of the area was little known, and the island's sites are type sites for a series of archaeological cultures.
The Cronin Point Site is an archeological site located in Nehalem Bay State Park near Manzanita, Oregon, United States, that was occupied probably between 1600 and 1800 CE. The site is characterized by a significant quantity of burned, fire-cracked rock, indicating the presence of hearths and other cultural activities associated with occupation and a possible village site. Artifacts in the site include stone flaking debris, and a smaller number of projectile points, glass pieces, bone pieces, and shell fragments. Notably, the site also includes shards of Chinese and Japanese ceramicware, datable by their design to ca. 1550–1680 CE, which link the Cronin Point Site to the Nehalem Beeswax Shipwreck. The site spans both submerged and exposed areas; auger-based studies suggest that occupation of the site ended abruptly, likely when the land it rests on subsided due to a large earthquake.
The Smuggler Cove Shell Midden is an archeological site located in Oswald West State Park near Neahkahnie Beach, Oregon, United States. First documented by archeologists in 1976, the midden has been found to contain remains of mussels, barnacles, and chiton to a depth of approximately 30 centimeters (12 in). Radiocarbon dating of a single sample of shell debris indicates that the Smuggler Cove campsite was occupied around 1660 CE, approximately the same date as the supposed wreck of a European ship at nearby Nehalem Spit, suggesting the site may preserve information from both before and after first contact between local people and Europeans. The site has been heavily damaged by construction of recreational facilities and coastal erosion, but a significant portion remains with potential to contribute to future research. Data generated from the site may help answer questions related to environmental change in the Oregon Coast region, settlement and subsistence patterns, emergence of ethnographic patterns among coastal people, the change in cultural patterns from before to after contact with European Americans, and other topics.
Indian Fish Trap State Preserve, also known as the Indian Fish Weir, is a historic site located near the Amana Colonies in rural Iowa County, Iowa. The fish weir is an array of rocks in a V-shaped formation in the Iowa River. It is the only structure of this kind in Iowa.
The Spruce Tree Site is an archeological site located in Nehalem Bay State Park near Manzanita, Oregon, United States. The site likely represents a precontact/postcontact Nehalem Tillamook campsite used for subsistence activities, including fishing, hunting, food processing, tool manufacture, and related tasks. Radiocarbon dating based on a single sample suggests it may have been occupied as early as 1490 CE. The site has yielded rock flake debris, burned rock, and charcoal, while the presence of glass beads and small fragments of ceramic provide information potential related to early contacts between Europeans and the peoples of the Oregon coast. The porcelain fragments may also link it to the Nehalem Beeswax Shipwreck. The site has been partially eroded, but significant cultural deposits remain above the water line. Submerged stumps amid the site indicate significant subsidence of over 1 meter, possibly related to a large earthquake, which can help answer research questions about the effect of seismic activity on the peoples and landscapes of the Oregon coast as well as on the preservation of cultural remains.
The High Point Shell Midden is a prehistoric archeological site located in Samuel H. Boardman State Scenic Corridor near Carpenterville, Oregon, United States. The midden is located on a strategic high point overlooking the Pacific coast, and is visible in the eroding cliff face. Radiocarbon dating indicates that the site was occupied c. 1070 CE and again c. 1385 CE, but additional dating may extend this chronology. Although shell deposits are evident without excavation, it is likely that evidence of other activities related to site occupation may be found on the periphery of the midden. The site has potential to produce scientific data related to several topics, including "site formation processes, landscape evolution, and changes in settlement, subsistence, technology, and society among the Native American cultures of the Oregon Coast."
The Tahkenitch Landing Site is a prehistoric archeological site located in Oregon Dunes National Recreation Area near Gardiner, Oregon, United States. Stratified remains up to 2 meters deep show the site has served various functions including shell midden and probably village over a history spanning 7000 to 8000 years, up to as late as 1858 CE. It also bears evidence of dramatic environmental changes including estuarine development, dune formation, and a transition from estuarine to lacustrine habitats. It was the first site on the Oregon coast to yield cultural remains older than about 3000 BP, and as such is one of the most significant sites on the Pacific coast of Oregon and North America.
References
- ↑ Knoerl, John; Miller, Diane; Shrimpton, Rebecca H. (1990), Guidelines for Restricting Information about Historic and Prehistoric Resources, National Register Bulletin, National Park Service, U.S. Department of the Interior, OCLC 20706997 .
- 1 2 3 Byram, Scott; Erlandson, Jon (August 17, 1999), National Register of Historic Places Registration Form: 35-CS-130, The Osprey Site (redacted PDF), archived (PDF) from the original on April 12, 2021, retrieved April 11, 2021.
- ↑ National Park Service (March 16, 2001), Weekly List of Actions Taken on Properties: 3/05/01 through 3/09/01, archived from the original on October 6, 2015, retrieved October 28, 2015.
