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Sherburne County Heritage Center Interpretive Plan Final Report 2005
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Sherburne County Heritage Center Interpretive Plan Final Report 2005
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(Major sources: Daniel S. Wovcha, et. al., Minnesota's St. Croix River Valley and Anoka <br />Sandplain: A Guide to Native Habitats (1995): 4-13; and Thomas Jackson, Soil Survey of <br />Sherburne County, Minnesota, (USDA, NRCS) at <br />http://www.sherbumeswcd.org/sherb_MN.pdf , accessed February 19, 2005. When <br />disagreements in some glacial history details emerged, I used the Soil Survey, but this needs <br />to be explored further, especially the different explanations for Elk River moraine hills.) <br />Theme statement <br />Theme 2: Being on the edge where three ecological land types meet enabled easy <br />transportation and access to natural resources and economic resources. <br />Subthemes <br />2.1. The glacial history of Sherburne County created the soils and topography that, together <br />with climate and human manipulation, created our native plant communities and future land <br />use opportunities. <br />Contemporary visitor relevance: The audience study indicated high interest in natural <br />history, the story of how sand came to Sherburne County, and how the land shaped the lives <br />of people in the county. The study also strongly indicated an interest in interactivity, <br />immersion, and sensory experiences. <br />Desired Learner Outcomes <br />1. Some visitors will be able to describe at least three different glacial features that exist in <br />Sherburne County. (cognitive) <br />2. Some visitors will be able to explain how the sandy soils came to Sherburne County. <br />(cognitive) <br />3. Hearing the sounds, immersed in the fog and coolness of the zone and impressed by the <br />size and power of glaciers, some visitors will respond to the natural forces that created <br />the county landscape by telling other members of their group how these sensory <br />experiences affected understanding of glaciation. (affective) <br />Visitor Experience <br />Visitors walk through a tunnel of ice (ca. 10 feet), with booming and grinding sounds of <br />glacial retreat. (This grinding helped create sand.) It is also desirable to have a localized <br />"cool zone" and steam machine within the tunnel. Sound, steam, and cool gusts of wind can <br />all be initiated by motion or pressure activated sensors. As they emerge on the other side, <br />visitors walk on sand and are initially surrounded by the sound of rushing water. On one side <br />a diorama of an engorged Mississippi River rushes noisily past, slowly changing in <br />synchrony with the film on the other side of the pathway. On the other side, they see back <br />projection images that show the changing landscapes in Sherburne County after glaciation. <br />Using comparable landscapes that still exist in other places, perhaps Alaska, show <br />photos/film changing from a contemporary glacier; to a Black Spruce parkland; then a dense <br />pine woodland; a prairie and oak savannah landscape, a dry, sandy, windy landscape; and <br />finally a contemporary film of a level plain of sand with prairie, scattered burr oaks and in <br />the distance, an occasional shallow lake and tamarack bog. Brief narration will tell how the <br />Sherburne County Historical Society Heritage Center Interpretive Plan, April 21, 2005, page 25 <br />
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