
Each of 3 student groups visited 2 locations on the Northshore and presented their findings. I was unable to attend the trip, so I thoroughly enjoyed the video presentations:
Students shared findings with other groups to complete packets of questions/information.
Winnetka Grand Canyon - using a topographic map, create a vertical profile of one of the ravines. See "R" is for Ravines for more information.

Glencoe Beach - How are bluffs formed? What is a moraine and how are they formed?
Southern Winnetka - Using the topographic map calculate the approximate gradient of the Highland Park moraine in southern Winnetka.
Gradient = slope = rise/run

Wilmette Sand spit
The spit was created thousands of years ago when Lake Chicago was at a high water mark (60 ft. higher than Lake Michigan today). Longshore currents swept around the tip of the Highland Park moraine and deposited sediment beyond it, called a sandspit. Visually document the sandspit and the dune field on the grounds of Westmoreland Country Club.


Continue with Paradigm Shift presentations.
Library research: Chicago as an archetypal American city and "culture factory"
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