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Agenda - Council - 09/14/2021
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Agenda - Council - 09/14/2021
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Council
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09/14/2021
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the Mississippi River. The sands in these areas are course in texture near the river and become <br />increasingly finer in texture the further the distance from the river. In various places, it is underlain <br />by strata of calcareous gravel, which was representative of what was found during the current <br />archaeological survey (Grimes 1968). <br />The project area is comprised of Anoka loamy fine sand, Nymore loamy sand, Nymore loamy <br />sand, and Nymore loamy coarse sand. The Anoka loamy fine sand series consists of well drained <br />soils on 0 to 2 percent slopes found on outwash plains. The typical soil profile consists of loamy <br />fine sand from 0 to 20 inches, followed by fine sand from 20 to 152 inches. The Nymore loamy <br />sand series consists of excessively drained soils found on 0 to 12 percent slopes on stream terraces. <br />The typical soil profile consists of loamy sand from 0 to 66 inches, followed by sand from 66 to <br />152 inches. The Nymore loamy coarse sand series consists of excessively drained soils found on <br />12 to 25 percent slopes on stream terraces. The typical soil profile for the series reflects that of the <br />Nymore loamy sand series (NRCS 2021). <br />3.2 Regional Flora and Fauna <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 />4.0 CULTURAL HISTORY <br />The Minnesota State Historic Preservation Office (SHPO) has developed statewide contexts <br />examining Minnesota's Prehistoric through recent past. These contexts are laid out on the <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 />Native American contexts are commonly divided into three major traditions: Paleoindian, Archaic, <br />and Woodland. Late Woodland is further subdivided into Plains Village, Mississippian, and <br />Oneota Traditions. These divisions are based on significant changes in how these communities <br />lived, with a special focus on subsistence strategies. Historic contexts are generally divided into <br />Contact and Post -Contact periods. The Contact period begins with early European exploration and <br />Phase I Archaeological Survey of Trott Brook Property <br />Ramsey, Anoka County, Minnesota <br />Nienow Cultural Consultants, LLC <br />6 <br />
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