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dc.contributor.authorTerhune, Patrick
dc.contributor.authorBenowitz, Jeff
dc.contributor.authorBemis, Sean P.
dc.contributor.authorBurkett, Corey
dc.contributor.authorO'Sullivan, Paul B.
dc.date.accessioned2014-05-09T16:39:16Z
dc.date.available2014-05-09T16:39:16Z
dc.date.issued2014-04-29
dc.identifier.urihttp://hdl.handle.net/11122/3482
dc.description.abstractThe Denali Fault is a major strike-slip fault extending from British Colombia, into western Alaska. Mount McKinley, at 6,114 m, is the highest peak in North America and is located to the south of a bend in the Denali Fault (Fig.1). To the north, at the apex of the bend in the fault, Peters Dome (3,221 m) is the highest peak and north-side peak elevations rapidly decrease moving away from the bend’s apex.en_US
dc.language.isoen_USen_US
dc.titlePersistent topographic development along a strike-slip fault system: The Mount McKinley restraining benden_US
dc.typePosteren_US
refterms.dateFOA2020-01-24T14:37:19Z


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