Posteruption glacier development within the crater of Mount St. Helens, Washington, USA

  title={Posteruption glacier development within the crater of Mount St. Helens, Washington, USA},
  author={Steve P. Schilling and Paul E. Carrara and Ren A. Thompson and E. Y. Iwatsubo},
  journal={Quaternary Research},
  pages={325 - 329}
Emplacement of a silicic lava dome through a crater glacier: Mount St Helens, 2004–06
Abstract The process of lava-dome emplacement through a glacier was observed for the first time after Mount St Helens reawakened in September 2004. The glacier that had grown in the crater since the
Formation and evolution of newly formed glaciovolcanic caves in the crater of Mount St. Helens, Washington, USA
Abstract. A new and extensive system of glaciovolcanic caves has developed around the 2004–2008 lava dome in the crater of Mount St. Helens, Washington, USA. These systems offer a rare view into a
Modeling the dynamic response of a crater glacier to lava-dome emplacement: Mount St Helens, Washington, USA
Abstract The debris-rich glacier that grew in the crater of Mount St Helens after the volcano’s cataclysmic 1980 eruption was split in two by a new lava dome in 2004. For nearly six months, the
Surface exposure dating of moraines in the Kromer valley (Silvretta Mountains, Austria)-evidence for glacial response to the 8.2 ka event in the Eastern Alps?
10Be dating of a pronounced glacier advance (‘Kromer Stadial’) in the western part of the Silvretta Mountains (western Austria) yielded ages ranging from 8010±360 to 8690±410 years with a mean age
Geomorphology and surface geology of Mount St. Helens volcano
ABSTRACT Mount St. Helens is a stratovolcano of the Cascadia volcanic arc well known worldwide for its volcanic collapse and eruption in 1980, which caused considerable destruction and changed the
Glaciers and Perennial Snowfields of the U.S. Cordillera
Of more than 8,000 glaciers and perennial snow-fields on 21 mountain ranges in the western U.S. (excluding Alaska), only 120 are larger than 1 km2, and just one exceeds 10 km2. Where changes in size
Mass Addition at Mount St. Helens, Washington, Inferred From Repeated Gravity Surveys
Relative gravity measurements were made at 12 sites on Mount St. Helens and 4 sites far afield during the summers of 2010, 2012, 2014, and 2016. Positive residual gravity changes of 0.05–0.06 ± 0.01
The geologic, geomorphic, and hydrologic context underlying options for long-term management of the Spirit Lake outlet near Mount St. Helens, Washington
Grant, Gordon E.; Major, Jon J.; Lewis, Sarah L. 2017. The geologic, geomorphic, and hydrologic context underlying options for long-term management of the Spirit Lake outlet near Mount St. Helens,
Assessing the Use of Optical Satellite Images to Detect Volcanic Impacts on Glacier Surface Morphology
This study investigates the potential of using optical satellite images to detect volcanic impacts on glaciers, with a view to utilise detected changes in glacier surface morphology to improve glacier-clad volcano monitoring and eruption forecasting.


Post-eruption erosion and deposition in the 1980 crater of Mount St Helens, Washington, determined from digital maps
The crater of Mount St Helens shows one of the world's highest known rates of mass wasting. On many summer days, rockfall is almost continuous, and many large rock and dirty-snow avalanches have
Regularities in Growth of the Mount St. Helens Dacite Dome, 1980 - 1986
The dacite dome at Mount St. Helens grew episodically between October 18, 1980, and October 22, 1986, chiefly by extrusion of thick flows but also by endogenous growth resulting from intrusion into
Atmosphere, Weather and Climate
In this updated sixth edition the authors focus on the current concern of human impacts on the environment. The topics of greenhouse gases, the destruction of the ozone layer, carbon cycles, and the
Effects of volcanism on the glaciers of Mount St. Helens
_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ D1 Specific Effects of Volcanic Activity on Glaciers-Cont. Introduction______________________________ 1 May 19 to October 6
Photogrammetric analysis of 1984 -89 surface altitude change of the partially debriscovered Eliot Glacier
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