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| Deposition:
supra-glacial and sub-glacial
ice marginal
lacustrine
Landforms:
outwash fans and outwash plains, kames, lake plains, eskers
Meltwater Deposits Map
Image credit: USGS Groundwater Atlas of the United States http://capp.water.usgs.gov/gwa/ch_j/J-summary.htmlSurficial Deposits Map
Relief Map
Baraboo Range: syncline formed from highly resistant Precambrian quartzite
Devils Lake
glacial ice blocked both ends of Devils Lake Gorge
Johnstown Moraine still blocks gorge
Lake basins
ice dammed drainage
proglacial lakes formed between retreating ice and Johnstown Moraine
Lewiston Basin & Merrimac Basin
Lewiston Basin ice dam failed - outburst flood flowed from Lewiston Basin into Merrimac Basin and down Wisconsin River
helped form present-day Lake Wisconsin
flat lake bottom; silty sediment; postglacial gullies eroded along margins
Tunnel channels
Johnson Ponds
marginal ice frozen to bed; farther back find thawed ice bed
meltwater from thawed bed zone carved tunnel channel through frozen bed zone
sand & gravel deposited in channel along with ice blocks from tunnel roof
result: deep kettles form lakes, shallow kettles form marshes
tunnel channels along Johnstown Moraine north of Baraboo: kettles & outwash fans
Glacial ice blocked Wisconsin River forming lake
Depending on lake level and ice margin position, lake drained to:
northwest to East Fork Black River, or
southwest through Devils Lake Gorge to Wisconsin River
Lake drained catastrophically in a matter of days to weeks
water broke through Johnstown Moraine & underlying weakly cemented sandstone forming Wisconsin Dells
Broad, flat sand plain; sandy, silty sediment up to 300 feet thick