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Filtering by: Advisor Nolin, Anne E. Subject Periglacial processes -- Washington (State) -- Rainier, Mount

Recent periglacial debris flows from Mount Rainier, Washington

Creator:

Copeland, Elizabeth A.

Abstract:

Debris flow initiation is controlled by a complex interaction of geology, geomorphology, climate, and weather. In the Cascade Range of Pacific Northwest and mountainous areas globally, patterns of temperature and precipitation are being altered by climate change, which may in turn impact debris flow initiation. Temperature has increased and patterns...

Resource Type:

Masters Thesis

Full Text:

. Grant Anne W. Nolin Debris flow initiation is controlled by a complex interaction of
The changing glaciers of Mt. Hood, Oregon and Mt. Rainier, Washington : implications for periglacial debris flows

Creator:

Ellinger, Jonathan R.

Abstract:

Mountain glaciers are receding worldwide with numerous consequences including changing hydrology and geomorphology. This study focuses on changes in glacier area on Mt. Hood, Oregon and Mt. Rainier, Washington where damaging debris flows have occurred in glaciated basins. Landsat imagery is used to map debris-free ice on a decadal time...

Resource Type:

Masters Thesis

Full Text:

Debris Flows Abstract approved: _____________________________________________________ Anne W. Nolin
Meteorological conditions associated with rain-related periglacial debris flows on Mount Hood, Oregon and Mount Rainier, Washington

Creator:

Parker, Lauren E.

Abstract:

In November of 2006 an intense rainstorm of tropical origin, known colloquially as the "Pineapple Express," inundated the Pacific Northwest region of the United States, initiating numerous periglacial debris flows on several of the stratovolcanoes in the Cascade Range of Oregon and Washington. These debris flows rapidly aggrade channels, deposit...

Resource Type:

Masters Thesis

Full Text:

: _____________________________________________ Anne W. Nolin In November of 2006 an intense rainstorm of tropical origin, known