Glacial Grooves - New York City
About This Item
Photo of glacial grooves in New York City. Glacial grooves, also known as glacial striation, are parallel lines or grooves in a bedrock surface. They are formed by the deposition of loose rock material that was once embedded in a glacier that has passed over the rock surface.
- Created by
- Pestrong, Ray
- Date
- Type
- Slide
- Format
- TIFF
- Source
- Ray Pestrong Geosciences Slide Collections, San Francisco State Unviersity
- Locale
- New York
- Rights
- Public
- Views
- 2272
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