Origin of the active drumlin field at Múlajökull, Iceland: New insights from till shear and consolidation patterns
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文摘

Drumlin relief at Múlajökull reflects basal till deposition and erosion.

Surges deposit and shear till layers across the glacier forefield.

Till between drumlins is more consolidated than till within drumlins.

High effective stresses between drumlins cause erosion there during quiescent flow.

Patterns of till consolidation contradict leading models of drumlin formation.

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