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<br />12 <br /> <br />Site 38 – OIN 1893, 9420, 9422, 9462, 9670, 9671: <br />This larger site is an abandoned tree nursery located immediately adjacent to the Red River of <br />the North that measures approximately 38.3 acres in size, and there are some erosional issues <br />in multiple locations along the river. Much of the site along the river falls within the 10-year flood <br />inundation boundary. The site is comprised of three primary soil types, with the majority being <br />mapped as Fargo silty clay (I229A), found on 0-1% slopes, with Fargo being its major <br />component (80%). Fargo is described as a clayey, poorly drained, hydric soil. The second most <br />abundant soil type is Cashel silty clay (I293B), which is found in 0-6% slopes and occasionally <br />flooded. The major soil component (80%) is Cashel, a loamy overflow that is non-hydric, but <br />somewhat poorly drained. Third most abundant, found primarily along the riverbank is mapped <br />as Wahpeton silty clay (I451D), which is described as being found on 1-15% slopes and <br />occasionally flooded. The major components are listed as Wahpeton (35%), which is a <br />moderately well drained, non-hydric clayey soil, and Cashel (25%), a somewhat poorly drained, <br />non-hydric loamy overflow soil. This is a unique site that has some trees already in place, but <br />with additional plantings, the site would increase riparian buffer benefits to the Red River system <br />and would allow for the erosional issues onsite to be addressed. The sloped areas adjacent to <br />the river would be supplemented with the Bank Stabilization strategy (orange polygon, approx. <br />0.8 acres) and transition into Floodplain Forest strategy (green polygon, approx. 37.5 acres) on <br />the higher elevations, farther from the river. There is a plant species list of remaining trees on <br />the nursery property (Appendix C), of which several species of Lilac (highlighted yellow in <br />Appendix C) have been identified as potentially harmful due to their invasive nature and would <br />need to be removed or girdled in place at the time of planting. Existing fencing and concrete <br />driveway/entrance would also require removal. <br /> <br />Site 39 – OIN 1200 <br />This site is located immediately adjacent to the Sheyenne River and measures approximately <br />0.34 acres. There are significant erosional issues on the western end along the river. The entire <br />site lies outside of the 10-year flood inundation boundary, and the majority of the site is <br />comprised of Fairdale silt loam (I480A), which is described as being a clayey substratum found <br />on 0-3% slopes and rarely flooded. The major components are listed as Fairdale (78%), which <br />is a moderately well drained, non-hydric loamy overflow, and LaDelle (10%), a moderately well <br />drained, non-hydric loamy soil. Although this is a smaller property, it would provide additional <br />riparian buffer benefits to the Sheyenne River and would allow for the erosional issues onsite to <br />be addressed. The sloped areas adjacent to the river would be planted using the Bank <br />Stabilization strategy (orange polygon, approx. 0.2 acres) and transition into Floodplain Forest <br />strategy (green polygon, approx. 0.13 acres) farther from the river. <br /> <br />Site 41 – OIN 1885, 9416 <br />This site is a former homesite/flood buyout property, located adjacent to the Red River of the <br />North and measures approximately 8 acres. Much of the eastern side of the site falls within the <br />10-year flood inundation boundary, and the majority of the site is comprised of Wahpeton silty <br />clay (I248A), which is described as being found on 0-2% slopes and occasionally flooded. The <br />major component (70%) is listed as Wahpeton, which is a moderately well drained, non-hydric,