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Debated: Wave-Cut or Weathering or Both?

May 30th, 2012
Debated: Wave-Cut or Weathering or Both?
This is a saprock-bedrock boundary at water table in coastal rock platform at Sunset Bay (A) and alluvial rock platform at Days Creek (B), Ore. Credit: G. Retallack and J. Roering.

The June GSA TODAY science article is now online and open access at http://www.geosociety.org/gsatoday/. In this issue, Gregory Retallack and Joshua Roering of the University of Oregon enter the long-standing debate as to whether rock platforms along coasts and rivers are the product of physical erosion or chemical weathering above the water table.

Although the notion of wave-cut or stream-cut platforms is firmly entrenched in the literature, Retallack and Roering present the case that a more important role is played by subaerial chemical weathering. Using data from intertidal and riverside rock platforms in southwest Oregon, they show that the platforms correspond to the saprock-bedrock boundary and remain within the zone of modern water table and intertidal fluctuation despite continuing tectonic uplift. Above this zone of frequent wet/dry cycling, the rock is weakened by subaerial weathering, producing a sharp decrease in rock strength. Hence, in this case, waves and floods do not cut rock but remove clasts already weakened by weathering to expose the local water table as a bedrock surface.

More information:
Wave-cut or water-table platforms of rocky coasts and rivers? Gregory J. Retallack and Joshua J. Roering, Dept. of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA. doi: 10.1130/GSATG144A.1.

Provided by Geological Society of America

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