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Home > Explore! > Bedrock Geology > Field Localities > Grindle Point > Figure 7
Figure 7. This natural surface above high water was worn down and striated during the last Ice Age. As the continental glacier moved across the surface, embedded stones at its base scraped and gouged the bedrock surface, leaving these parallel marks. These marks are about 14,000 years old. Show highlights. (MGS photo by Henry Berry.) Last updated on January 4, 2008 |
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