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valley throughout the county with coarse alluvium, which underlies two broad terraces parallel to <br />the Mississippi River, an example of which is notable in the Capstone Homes project area. The <br />sand in these areas are course in texture near the river and become increasingly finer in texture the <br />further the distance from the river. In various places, it is underlain by strata of calcareous gravel, <br />which was representative of what was found during the current archaeological survey (Grimes <br />1968). <br /> <br />The project area is comprised of Hubbard loamy sand ranging between 0 to 2 percent and 2 to 12 <br />percent slopes, Dickman sandy loam ranging between 0 to 2 percent and 2 to 6 percent slopes, and <br />Nymore loamy coarse sand on 12 to 25 percent slopes. The Hubbard loamy sand series consists of <br />excessively drained sandy floodplain outwash found on stream terraces and hillslopes. The typical <br />soil profile for the series consists of loamy sand from 0 to 20 centimeters, loamy sand from 20 to <br />50 centimeters, loamy sand from 50 to 82 centimeters, and sand from 82 to 200 centimeters. The <br />Dickman sandy loam series consists of somewhat excessively drained floodplain outwash found <br />on stream terraces. The typical soil profile for the series consists of sandy loam from 0 to 30 <br />centimeters, sandy loam from 30 to 45 centimeters, and sand from 45 to 152 centimeters. The <br />Nymore loamy coarse sand series consists of excessively drained floodplain outwash found on <br />stream terraces. The typical soil profile for the series consists of loamy coarse sand from 0 to 18 <br />centimeters, loamy sand from 18 to 66 centimeters, and sand from 66 to 152 centimeters (NRCS <br />2020). <br /> <br />3.2 Regional Flora and Fauna <br /> <br />Vegetation in the area at the time of Euro-American settlement consisted of Big Wood species in <br />both the south and west portions of the region. Most specifically, the trees were deciduous <br />hardwood species, primarily oak, mixed with deciduous-coniferous forest in the northern part of <br />the region (Anfinson 1990) which also contained maple, basswood, and hickory. As Euro- <br />American settlers moved through the area and cleared portions of forest, prairie land became more <br />abundant. White-tailed deer, bison, elk, beaver, bear, prairie chickens, and a variety of fish and <br />waterfowl would have been commonly available resources (Anfinson 1990). Specific to the site <br />area, the majority of the trees on the sand plain consisted of bur oak and northern pin oak, as well <br />as mixed hardwoods which grow in areas of glacial till, specifically in the areas where the Hayden <br />soil series is prominent (Grimes 1968). Large areas of hardwoods invaded areas of native grasses <br />in the outwash plains along the Mississippi River. The Hubbard series discussed above developed <br />in these areas. <br /> <br />4.0 CULTURAL HISTORY <br /> <br />The Minnesota State Historic Preservation Office (SHPO) has developed statewide contexts <br />Minnesota Archaeological Site Form (Minnesota Office of the State Archaeologist 2016). <br />Generally, they describe the history of the state and assist in predicting where specific types of <br />sites may occur. <br />Phase I Archaeological Survey of Proposed Capstone Homes Housing Development 7 <br />Ramsey, Anoka County, Minnesota <br />Nienow Cultural Consultants, LLC <br /> <br />