Earth Science Digital Image Library - Chatter Marks and Glacial Polish
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
Related Academic Standards
Topic
Erosion
Description
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
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
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: