naaw. I'm building on the top of the hill and, the hill is 20 to 25 ft tall and slopes to the south in 40 or 50 ft of run. Here is a link to a file in Dropbox that gives the Geology. thanks to OG.
NOTE the area where the hill lies in labelled GC from the website. (
It appears the house will be sitting about 40 ft North of the southern edge of the Superior Lobe-- ice sheet furthest advance. Here is explanation of the ice sheets:
Here is a sat view of the property, too. With the home placement shown:
Really sandy soil beneath the upper humous, black top soil in the forest. Hill is forest, slopes down to grassland.
According to the U of MN website (Oldest Guy guided me to) the bottom of this 20 ft hill is apparently at the interface of where two Pleistocene ice sheets met. Here is the details of the materials on my land on the hill, the Superior Lobe:
Till/sand complex (Pleistocene)—A mixture of sediments including till, ice- contact sand and gravel, and minor lacustrine deposits; modified by subglacial processes. Superior lobe deposits are mixed with, or thinly overlain by, sediments of the Grantsburg sublobe. Topography is collapsed and irregular; abundant elongate ridges.
And the Des Moines Lobe left this stuff:
Sediment deposited by ice of the northwest-source Des Moines lobe—Deposits contain abundant gray, siliceous shale fragments. The till color is variable but typically is yellow-brown where oxidized.
MORE details: Yesterday I was meeting with the gravel pit owner ON SITE and he had a drilling crew mapping out his gravel in the forest just NORTH of me. They found there is about 15 ft of clay covering his 25 ft thick gravel source. On the ground at the bore hole was a big pile of the cleanest, purest sand. Nice and moist, uniform sand. Likely between the clay and the just hit gravel they were pounding into.