Influence of Catchment Properties on Stability of Frozen...

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Cordilleran Section of the Geological Society of America 111 th Annual Meeting – May 11-13, 2015 Alaska Department of Natural Resources Division of Geological & Geophysical Surveys and University of Alaska Fairbanks Influence of Catchment Properties on Stability of Frozen Debris Lobes Ronald P. Daanen, Margaret M. Darrow and Trent D. Hubbard.

Transcript of Influence of Catchment Properties on Stability of Frozen...

Page 1: Influence of Catchment Properties on Stability of Frozen ...dggs.alaska.gov/webpubs/dggs/po/text/po2015_012.pdf · Cordilleran Section of the Geological Society of America 111th Annual

Cordilleran Section of the Geological Society of America 111th Annual Meeting – May 11-13, 2015

Alaska Department of Natural Resources Division of Geological & Geophysical Surveys

andUniversity of Alaska Fairbanks

Influence of Catchment Properties on Stability of

Frozen Debris Lobes

Ronald P.Daanen,MargaretM.Darrowand

TrentD.Hubbard.

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Overview

• FrozendebrislobesintheDietrichRiverValley,southcentralBrooksRange

• Justification• Catchmentswithandwithoutlobes• Sedimentmovementfactors• Sedimentstabilizationfactors• Summary

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Frozen debris lobes

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Why are these features here? Why are they not in all catchments? What creates their dynamic nature?

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Catchments without lobes

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This is why we need to know more

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40m

FDL‐A

270m

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Dietrich River valley

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Glacier-filled Dietrich River valley

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Catchments draining into the valley

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Catchments

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Blue without frozen debris lobe Red with frozen debris lobe

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Slope and sediment movement

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Slope comparison

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Blue marker = without frozen debris lobeRed marker = with frozen debris lobe

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Aspect: Vegetation and permafrost

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North- versus south-facing slopes

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South‐facing North‐facing

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Annual precipitation

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Annual discharge

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Channel morphology

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Summary

• Catchmentswithoutlobes• Steeperslopes• Higherelevation• Greaterdischarge

• Catchmentswithlobes• Mediumslopeswithabreakinslopewhereupperpartoflobestarts

• Sedimentstabilizationthroughvegetationandpermafrost

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Summary

• Whatwilllikelydestabilizefrozendebrislobes?• Lossofvegetation• Warmerground• Warmerclimate• Lossofpermafrost• Wetterclimate(warmergroundandlubricationoftheshearzone)

• Anthropogenicincreaseinslope

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The expected result

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Alluvial Fan

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Current frozen debris lobe in transition

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Lobe 42

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Thank you for your attention.Questions?

WewouldliketothanktheStateofAlaska,US‐DOT,andAlyeskafortheir

supportofthisresearch.5/11/2015 GSA–Cordilleran section – 111th Annual Meeting – Alaska Division of Geological & Geophysical Surveys 21