Home | About the LGM | For Students | For Visitors to Campus | Resources
Peffer Park: Modern Stream Processes

Look in the photograph below: if you look downstream along the cut bank, you will see that the glacial till forms a steep bank. The steepness of this bank indicates that the till

Picture of a point bar of sand and gravel with a cutbank of galcial till.

In the photograph below, you should be able to pick out point bars of sand and gravel (foreground) and a cut bank of glacial till (background).

Picture of Glacial Till forming a teep bank.

Places of interest | Previous | Next stop



MU Homepage | Ask a Geologist | Geology Dept Homepage | Contact us | Facebook | Site Map
Last Updated: September 16, 2010
Designed by Capstone Students in the Bachelor of Arts in Technical and Scientific Communication