Skip to Main Content

Earth Science Digital Image Library - Chatter Marks and Glacial Polish

Digital Profile

Earth Science Digital Image Library - Chatter Marks and Glacial Polish

Grade Levels

3rd Grade, 4th Grade, 5th Grade, 8th Grade

Course, Subject

Science and Technology and Engineering Education, Science

Topic

image 250 width
Erosion

Description

large
At the base of glacial ice, blocks may press so heavily against bedrock that they cause it to fracture resulting in a string of cuspate joints called chatter marks (1989, Van Diver, Bradford, Roadside Geology of New York). The smooth, even surface known as glacial polish, was produced by the movement of abrasive laden glacial ice on bedrock. Arrow illustrates ice flow direction on the Shawangunk Conglomerate (Middle – Upper Silurian).

Location

image 250 width
Minnewaska State Park, near New Paltz, Ulster County, NY.

Credits


With support from the Center for Applied Technologies in Education, The Earth Science Digital Image Library is an initiative authored by Russell Agostaro, Newburgh Enlarged City School District, Newburgh, New York.

Description

large
The Earth Science Digital Image Library is an archive of quality digital images for teacher and/or student reference in their studies of Earth Science. For additional information about the image, please click on a link below:
Loading
Please wait...

Insert Template

Information