Figure 7.
A model for the formation of the Buzzards Bay and Sandwich glaciotectonic end moraines by advancing ice (represented by horizontal arrow). The thrust moraine is formed by adding thrust sheets at the base of the moraine.
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Figure 7. A model for the formation of the Buzzards Bay and Sandwich glaciotectonic end moraines by advancing ice (represented by horizontal arrow). The thrust moraine is formed by adding thrust sheets at the base of the moraine. |
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