T212 How, and Under What Conditions, Does Weathering Influence Surface Processes?
Tuesday, 24 October 2017
8:00 AM - 12:00 PM
Chelan 2
A MICROMETER THICK COATING LAYER SLOWING THE WEATHERING RATE OF GLACIAL POLISH
Paper number: T212-10
Program: Technical Sessions
Time: 10:30 AM – 10:45 AM
Authors
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Greg StockYosemite National Park, El Portal, CA
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Emily E. BrodskyUniversity of California, Santa Cruz, Santa Cruz, CA
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Joseph Clancy WhiteUniversity of New Brunswick, Fredericton, NB
Abstract
Slip markers on the glacially polished surfaces, such as arcuate cracks and striations, indicate a role for abrasion during polish formation. At the small scales, bent and broken crystals in a damage zone beneath the coating layer provide evidence for abrasion at the nanoscale, which generates the fragments and amorphous matrix that ultimately comprise the coating layer. Flow and shear textures within the coating suggest that this composite material is smeared over the damage zone during ice sliding, forming the smooth surface.
The coatings are exceptionally impermeable, they shed water quickly and inhibit the colonization and growth of lichens and mosses, slowing chemical weathering. Although early work suggested that polish may perform a role in preservation, the structural origin of the impermeability had not previously been recognized.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-303677
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