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A palaeomagnetic and mineral magnetic study of the Speeton Shell Bed, North Yorkshire
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SUMMARY
A palaeomagnetic and mineral study of the estuarine sands of the upper exposure of the Speeton Shell Bed (late Pleistocene, pre-Devensian) provides independent evidence that the bed is not
in situ
and has undergone a rotation consistent with the effects of ice push. Variation in magnetic susceptibility also supports suggestions that the upper parts of the Speeton Shell Bed have been weathered. A previously unrecorded shrinkage crack horizon indicates that the depositional history of the Speeton Shell Bed may have been more complex than previously thought.
Geological Society of London
Title: A palaeomagnetic and mineral magnetic study of the Speeton Shell Bed, North Yorkshire
Description:
SUMMARY
A palaeomagnetic and mineral study of the estuarine sands of the upper exposure of the Speeton Shell Bed (late Pleistocene, pre-Devensian) provides independent evidence that the bed is not
in situ
and has undergone a rotation consistent with the effects of ice push.
Variation in magnetic susceptibility also supports suggestions that the upper parts of the Speeton Shell Bed have been weathered.
A previously unrecorded shrinkage crack horizon indicates that the depositional history of the Speeton Shell Bed may have been more complex than previously thought.
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