BEGIN:VCALENDAR VERSION:2.0 PRODID:-//ChamberMaster//Event Calendar 2.0//EN METHOD:PUBLISH X-PUBLISHED-TTL:P3D REFRESH-INTERVAL:P3D CALSCALE:GREGORIAN BEGIN:VEVENT DTSTART;VALUE=DATE:20140823 DTEND;VALUE=DATE:20140824 TRANSP:TRANSPARENT X-MICROSOFT-CDO-ALLDAYEVENT:TRUE SUMMARY:Sauk County Landscape DESCRIPTION:How did the Wisconsin Dells form? Why is Devils Lake where it is - so high in the landscape? Why is the lower Wisconsin River valley bounded by steep bedrock bluffs? Why are there such wide sand plains along the lower Wisconsin River? Was the ground once deeply and permanently frozen? Did the Wisconsin River once flow toward the east? When and how often have glaciers advanced into the area? Why is there a Driftless Area? Come join a discussion of these questions and many others that will help you understand the geologic history and the origin of the Sauk County Landspace!\n\n\n\nDr. John W. Attig\n\nEmeritus Professor of Geology\n\n More than 30 years doing research on the origin of Wisconsin landscapes and geological history of Wisconsin.\n Co-author of the book Roadside Geology of Wisconsin X-ALT-DESC;FMTTYPE=text/html:How did the Wisconsin Dells form? Why is Devils Lake where it is - so high in the landscape? Why is the lower Wisconsin River valley bounded by steep bedrock bluffs? Why are there such wide sand plains along the lower Wisconsin River? Was the ground once deeply and permanently frozen? \;Did the Wisconsin River once flow toward the east? When and how often have glaciers advanced into the area? Why is there a Driftless Area? Come join a discussion of these questions and many others that will help you understand the geologic history and the origin of the Sauk County Landspace!
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\nDr. John W. Attig
\nEmeritus Professor of Geology\n\n LOCATION:River Hills Community Church 1111 Sycamore Street Sauk City\, WI 53583 UID:e.1184.2320 SEQUENCE:3 DTSTAMP:20260429T063117Z URL:http://members.saukprairie.com/events/details/sauk-county-landscape-08-23-2014-2320 END:VEVENT END:VCALENDAR