Figure 2.8: Aerial view of College Fjord in Prince William Sound of Alaska. During lowered sea level and cooler climate, the glacier at the head of the fjord would have extended through the valley and acted to carve out the valley by eroding sediment from the sides and base of the valley.
Originally uploaded in Integrate:Teaching for Sustainability:InTeGrate Modules:Coastal Processes, Hazards and Society:Student Materials.
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Sep7 16