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Two Faces of Kachemak
Bay
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faces, one soft and young, the other ancient and craggy,
peer at one another across the blue waters of Kachemak
Bay. The rain-catching Kenai Mountains on the south
shore are grandfathers. They were formed when two tectonic
plates converged, thrusting jagged peaks skyward. In
contrast, the sandstone bluffs, long cobble and gravel
beaches, mudflats and stair step hills of the north
shore are youngsters. These are the offspring of stream
systems and receding glaciers. |
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Geology
Photo Gallery
Kachemak Bay North Shore to South Shore
William Wakeland Collection
Pratt Museum Photo Archives |

Kachemak Bay North Shore
William Wakeland Collection
Pratt Museum Photo Archives
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Copyright © 2004 Pratt Museum | All Rights
Reserved | Terms of Use
Web site created
by Elizabeth Kanter
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