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Rabbitkettle Formation
From Wikipedia, the free encyclopedia
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The Rabbitkettle Formation is a geologic formation in the Yukon, comprising thin bedded silty and occasionally siliciclastic limestones deposited in deep (below storm wave base) waters.[2][1] It preserves fossils dating back to the Ordovician period.
According to [1] it:
- Starts in the Late Cambrian; ends in late Tremadoc
- reaches 750m in thickness
- transitional slope facies
- Alternation of black calcareous mudstones and grey, burrowed wackestones
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