Magnitude and timing of downstream channel aggradation and degradation in response to a dome-building eruption at Mount Hood, Oregon

Bulletin of the Geological Society of America

Volumn 123, Issue 1-2, 2011, Pages 3-20

  Pierson, Thomas C ^a   Pringle, Patrick T ^b   Cameron, Kenneth A ^c  

^a CASCADES VOLCANO OBSERVATORY   (United States)

^b Centralia College   (United States)

^c Oregon Department Environmental Quality   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CHANNEL RESPONSE; DOWNSTREAM CHANNELS; EXPLOSIVE ERUPTION; HEAD WATERS; INCISED VALLEY; LATERAL CONFINEMENT; LONGITUDINAL PROFILE; RAINFALL INTENSITY; RAINFALL REGIME; RIVER AGGRADATION; RIVER BED; SEDIMENT LOADING; SEDIMENT WAVES; VOLCANICLASTIC SEDIMENTS;

DEGRADATION; DOMES; LANDFORMS; RAIN; RIVER POLLUTION; SEDIMENT TRANSPORT; SEDIMENTOLOGY; SOIL CONSERVATION; STRATIGRAPHY; THUNDERSTORMS;

RIVERS;

AGGRADATION; CANYON; CHANNEL MORPHOLOGY; DEGRADATION; DEPOSITION; DOME; HEADWATER; INCISED VALLEY; LAHAR; PRECIPITATION INTENSITY; PYROCLASTIC FLOW; SEDIMENT TRANSPORT; SEDIMENT WAVE; SEDIMENTATION; SEDIMENTOLOGY; STRATIGRAPHY; VOLCANIC ERUPTION; VOLCANICLASTIC DEPOSIT;

CASCADE RANGE; MOUNT HOOD; OREGON; UNITED STATES;

EID: 79251518263     PISSN: 00167606     EISSN: 00167606     Source Type: Journal    
DOI: 10.1130/B30127.1     Document Type: Article

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