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The Mooney site (Smithsonian trinomial: 21NR29) is a precontact Native American archaeological site on the Red River Levee in Norman County, Minnesota. It is a multicomponent site consisting of remains from both the Archaic and Woodland traditions. No diagnostic Archaic artifacts were found. However, animal remains and lithic materials recovered from one meter below the Woodland artifacts returned a carbon 14 date that provided the basis for the Archaic classification. The Woodland tradition is defined by a vertical scatter of materials, dated to about 1000 using thermoluminescence methods. Many animal bones were found at the site, reflecting a great emphasis on a wide range of hunting activity that focused on bison. Artifacts such as local and exotic lithic materials were found, as well as a wide variety of pottery and other ceramic remains. Much of the pottery followed the Sandy Lake model; however, some artifacts were placed in a new class of artisanship known as Red River Ware.
The Mooney site is a very large archaeological site, around 109 square meters, located in Norman County of northwest Minnesota. Its northern tip is located one hundred and fifty meters south of the Red River. It is a multicomponent site spanning the Plains Archaic and Woodland Periods which date to approximately 3400–940 B.P. It has produced evidence of big and small game hunting as well as fishing. It reflects at least two settlements over an unknown period of time but including a warm-season occupation. All but five acres (20,000 m2) of the site's surface have been disturbed by plowing. The northwestern and southern tips of the site were destroyed many years ago when soil was taken and used, for dike construction. Artifacts can still be found on the dike near the south side.
The Woodland remains show at least two settlements over an unknown amount of time; however, it is known that this time included some warm seasons. The majority of artifacts recovered from the Woodland period were pottery. Pottery was discovered at 1825 locations and at least 68 vessels are represented by the remains. Fifty-one of the vessels are thought to belong to a pottery classification known as Salt Lake ware. Salt Lake ware is a well known ceramic style common to central and eastern Minnesota and is defined by its straight rim and chord marked decoration style. Six other vessels are thought to belong to a style of pottery known as Sandy Lake Plain, which differs only slightly from the more abundant Salt Lake ware. Its only difference is a stick impressed decoration trend. However, thirteen vessels found at the Mooney site are very different than both the Sandy Lake Plain style and the Salt Lake style. The 6 odd vessels were given a new classification known as Red River ware and are distinguished by a rolled lip. Despite the large number of pottery found, lithic materials were scarce. Less than three hundred total stone tools and pieces of lithic debris were found. Of those, only 255 artifacts were from the Woodland period, which is the period from which the majority of the recovered pottery at the site dates. This puts the pottery to lithics remains at an astounding 5/1 ratio. The majority of the few stone remains found were made of native Swan River Chert and quartz. However, some exotic materials were found such as a piece of obsidian. In all, only three different kinds of stone tools were found at the site: bifaces, scrapers, and utilized flakes.
At 140–160 cm below ground, twenty four flakes and a spread of bone were found whose carbon date is around 3400 B.P. This date provides the basis for the Archaic classification of the artifacts, despite the fact that no tools or pottery had been found that linked the site to that tradition. The trail of human interaction was obvious with the findings of bone chips highly characteristic of hunting. There were also burnt bone chips and charcoal found at this depth, showing fire and cooking activities. Some bone fragments were identified as bison bone. This, matched with the other faunal remains found at the site, showed that the people that inhabited this area relied heavily on bison. This gives a strong connection between the Mooney site and all other Archaic sites in the area, such as Lockport and Cemetery point, as the primary subsistence source in all locations were bison.
The site is located in the Red River Valley near the middle portion of the Red River. The valley coincides with the southern extensions of the Lake Agassiz Plain. The valley is very flat and surrounded by beach deposits left by an ancient lake some 13,000-9,000 years ago. The Red River flows north to Lake Winnipeg, Manitoba. The levees of the river range to about 10 meters above the normal water level. The climate is continental with warm summers, about 21 degrees Celsius in July, and cold winters, about 13 degrees Celsius. It is predominantly prairie grassland. Around 95% of the valley was prairie before farming. In prehistoric times these large prairies supported large herds of buffalo that made life possible for the ancient peoples of the area. The other 5% of the land consisted of many gallery forests made up of elms, ash and oak that lined many waterways.
The Mooney site was excavated in June and July, 1983. The excavation was conducted by a small crew of eleven people and was headed by Dr. Michael G. Michlovic of Moorhead State University. The original excavation of the area was to be conducted in what is now the middle of the Mooney site. However, when the engineers dug the centerline of the proposed dike they found a great array of cultural debris. Deep tests (41*1 m units) showed that there was a deep component at the site directly below the proposed dike. This deep component is around 1.5m below the ground. The soil in this region is thick, poorly draining soil making the upper levels very difficult to get through, and reaching ones desired depth is very strenuous. As a result, the archeologist chose to use a backhoe to reach the deep undisturbed cultural levels at the site. The excavated soil was screened using 1/4” hardware cloth mesh because 1/4” is the smallest mesh that can be used on Red River clay. Of the 102 square meters at the Mooney site, 29 square meters were excavated. The excavation depth was approximately 160 cm. However, some units were excavated to slightly varying depths, averaging between 50–70 cm depending on the nature of the find. When all was said and done, nearly 85 cubic meters had been excavated, excluding the work of the backhoe.
The Grand Village of the Illinois, also called Old Kaskaskia Village, is a site significant for being the best documented historic Native American village in the Illinois River valley. It was a large agricultural and trading village of Native Americans of the Illinois confederacy, located on the north bank of the Illinois River near the present town of Utica, Illinois. French explorers Louis Joliet and Father Jacques Marquette came across it in 1673. The Kaskaskia, a tribe of the Illiniwek people lived in the village. It grew rapidly after a mission and fur trading post were established there in 1675, to a population of about 6,000 people in about 460 houses. Around 1691 the Kaskaskia and other Illiniwek moved further south, abandoning the site due to pressure from an Iroquois invasion from the northeast.
The Upper Mississippian cultures were located in the Upper Mississippi basin and Great Lakes region of the American Midwest. They were in existence from approximately A.D. 1000 until the Protohistoric and early Historic periods.
The Younge Site is an archeological site located in Goodland Township, Lapeer County, Michigan. It is classified as a Prehistoric Late Woodland site and was designated as a Michigan State Historic Site on October 29, 1971. It was added to the National Register of Historic Places on October 29, 1976.
Franktown Cave is located 25 miles 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 8000 years beginning about 6400 B.C. 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 recent as AD 1725.
The Juntunen Site, also known as 20MK1, is a stratified Prehistoric Late Woodland fishing village located on the western tip of Bois Blanc Island. It was listed on the National Register of Historic Places in 1978.
The Moccasin Bluff Site is an archaeological site located along Red Bud Trail and the St. Joseph River north of Buchanan, Michigan. It was listed on the National Register of Historic Places in 1977, and has been classified as a multi-component Prehistoric site with the major component dating to the Late Woodland/Upper Mississippian period.
The King Coulee Site is a prehistoric Native American archaeological site in Pepin Township, Minnesota, United States. It was listed on the National Register of Historic Places in 1994 for having state-level significance in the theme of archaeology. It was nominated for being a largely undisturbed occupation site with intact stratigraphy and numerous biofacts stretching from the late Archaic period to the Oneota period. This timeframe spans roughly from 3,500 to 500 years ago. The site yielded the oldest known evidence of domesticated plants in Minnesota: seeds dated to 2,500 years ago from the squash Cucurbita pepo.
The Schwerdt Site (20AE127) is located on the Kalamazoo River in Allegan County, Michigan. It is classified as a single-component Berrien Phase site dating to the late prehistoric period. The Berrien Phase is associated with the late Woodland but also has some Upper Mississippian influences.
The Griesmer site (La-3) is located on the Kankakee River in Lake County, Indiana, about a mile southeast of Schneider, in Northwestern Indiana. It is classified as a Prehistoric, multi-component site with Middle Woodland, Late Woodland and Upper Mississippian occupations. The deposits were not stratified, but observation of the types of artifacts present, together with radiocarbon dates, helped to define the sequence of occupations at the site.
The Fifield site (Pr-55) is located on Damon Run Creek in Porter County, northwestern Indiana. It is classified as a late Prehistoric, single-component Upper Mississippian Fisher village.
The Riviere au Vase site (20MB3) is located in Chesterfield Township, Macomb County, in southeastern Michigan. The site is on the Riviere au Vase near where it empties into Lake St. Clair. It is classified as a Prehistoric, Late Woodland site.
The Huber Site (11Ck-1) is located on Tinley Creek 2 miles west of Blue Island in Cook County, Illinois, near the city of Chicago. It is classified as a late Prehistoric site with Upper Mississippian affiliation.
The Anker Site (11Ck-21) is located on the Little Calumet River near Chicago, Illinois. It is classified as a late Prehistoric site with Upper Mississippian Huber affiliation.
The Hotel Plaza Site (Ls-36) is located near Starved Rock, on the Illinois River across from the Zimmerman Site (aka Grand Village of the Illinois. It is a multi-component site representing Prehistoric, Protohistoric and early Historic periods, with the main occupation being an early Historic component associated with the French Fort St. Louis.
The Plum Island Site (Ls-2) is located in the Illinois River near Starved Rock, LaSalle County, Illinois, in the vicinity of the Hotel Plaza site and the Zimmerman site. It is a multi-component site representing Prehistoric, Protohistoric and early Historic periods, with the main occupation being a late Prehistoric to early Historic component with Upper Mississippian affiliation.
The Fisher Mound Group is a group of burial mounds with an associated village site located on the DesPlaines River near its convergence with the Kankakee River where they combine to form the Illinois River, in Will County, Illinois, about 60 miles southwest of Chicago. It is a multi-component stratified site representing several Prehistoric Upper Mississippian occupations as well as minor Late Woodland and Early Historic components.
The Carcajou Point Site is located in Jefferson County, Wisconsin, on Lake Koshkonong. It is a multi-component site with Prehistoric Upper Mississippian Oneota and Historic components.
The Walker-Hooper Site (47-GL-65) is a multicomponent Prehistoric site complex located on the Grand River in the Upper Fox River drainage area in Green Lake County, Wisconsin. It consisted of at least 2 village sites and several mound groups. It was excavated by S.A. Barrett under the auspices of the Milwaukee Public Museum in 1921 and again in 1967 by Guy Gibbon of the University of Wisconsin-Milwaukee. The major component of the site is an Upper Mississippian Oneota palisaded village. Other components were also present, mainly Late Woodland but also including Archaic, Early Woodland and Middle Woodland.
The Fort Wayne Mound Site was a Prehistoric burial mound located on the grounds of the Ordinance Department of the former Fort Wayne in Detroit, Michigan. It was one of a series of mounds in Detroit, including the Springwells Mound Group, the Carsten Mound and the Great Mound at the River Rouge. By the mid-20th century only the Fort Wayne Mound was still standing. As of today it has been completely destroyed.
The Dabbs Site is an archaeological site located on a terrace in Cartersville, Georgia in the United States. It is a small excavation area where villages were historically established near flood plains along rivers and streams. The previous inhabitants and their specific cultural group are unknown, however, they left behind evidence of their practices in agriculture, hunting, and pottery making.