See the ‘Abstracts’ page for links to seven new abstracts related to Mount Baker. Abstracts from the Fall 2009 GSA annual meeting in Portland were authored by Melissa Park and others, 2009 (Sherman Crater ice-penetrating radar); Dave Tucker and others, 2009 (Carmelo Crater ice-penetrating radar); Nikki Moore and Sue DeBari, 2009 (mafic magma evolution); and Emily Mullen and Ian McCallum, 2009 (lead isotope studies).
Abstracts from the Fall American Geophysical Union meeting in San Francisco deal with new seismic studies at Mount Baker, including a seismic swarm from the summer of 2009: Jackie Caplan-Auerbach, W.A. Thelen, and Seth Moran (2 abstracts). Nichols, Malone, Moran, Thelen, and Vidale tell us about deep long-period earthquakes in the Cascades, mostly beneath Mount Baker. Click on the title of the abstracts to read the texts.
A report and photos were provided to MBVRC by Dr. Jeff Witter, Vancouver, B.C. Jeff studies gas emissions at active volcanoes. He heads up the International Volcano Monitoring Fund, a non-profit organization that seeks to assist third world volcano monitoring programs.
Troy Baggerman successfully defended his Masters thesis at WWU this spring. Troy studied the genesis of andesite at Mount Baker, paying particular attention to trace element and Rare Earth Element geochemistry. An abstract of his research is available on the abstracts page (Baggerman, T. and DeBari, S.M., 2007- ). Troy and his advisor Sue DeBari have submitted a paper to Journal of Volcanology and Geothermal Research. Troy will probably really miss his many hours in the lab crushing his collected rocks for chemical analyses.
Melissa Park was awarded $30,000 in research and scholarship funds from the National Science Foundation in June 2009. Melissa, a Western Washington University Geology graduate student, will continue her ice-penetrating radar and glacier-stake project to study movement, volume, and potential melting hazards associated with the glacier inside Mount Baker's Sherman crater.
Melissa’s NSF Graduate Fellowship will provide her with up to $30,000 per year for three years to fund her studies and research. The grant allows her to compensate field assistants for their time and oh-so-valuable efforts in hauling her ice-penetrating radar and camping gear to Sherman Crater, as well as supporting her academic costs at WWU.
"Not only will the financial aspect allow me to concentrate on my research during my years at Western, but the NSF Fellowship is also well recognized," she said. "This will open many doors for me in my future studies."
Melissa is a native of Noumea in the South Pacific. She received her bachelor's degree from WWU in Geology in 2008, and hopes to earn a doctorate in Glaciology after she finishes her master's degree at Western.
The remote reaches of Sandy Creek, on Mount Baker’s eastern flank, were mapped during a three-day traverse this September by Dave Tucker and Keith Kemplin. The valley, which drains the Squak Glacier, was the largest unknown area left to be detailed for the Mount Baker geologic map being prepared by Wes Hildreth of the USGS. Mapping showed the relative distribution of Mount Baker and older Black Buttes lava flows in the deglaciated basin below the receding ice tongue, and will provide more detail than shown on the current small scale map (Hildreth and others, 2003, page 748). The traverse also determined the distribution of a series of a few large debris flows, in aggregate as much as 20 m thick, down to an elevation of 2400 feet. These are probably remobilized volcaniclastic deposits from glacial outburst floods, rather than lahars spawned by eruptions. The valley-filling volcaniclastics in Sandy Creek are younger than the Boulder Creek assemblage just to the north: there is no SC ash (ca. 8800 14C years BP) covering the Sandy Creek fan, but Mount Mazama layer O (6800 14C years BP) is present.
In 2007, Brendan Hodge (Western Washington University) made a GPS resurvey of Mount Baker benchmarks as part of his MS thesis. This survey determined that since 1981, Mount Baker has deflated. Over a three week period this past summer, he installed and surveyed six new benchmarks to augment and expand the geodetic network on Mount Baker. New benchmarks were installed at locations lower and further from the summit of Mount Baker in order to better detect deformation resulting from a deep source. The destroyed benchmark at Sherman Crater, dating to 1975, was also replaced to provide a baseline measurement near the center of geothermal activity. This mark could also be used as reference for ongoing research with Sherman Crater. These surveys were supported by Dr. Juliet Crider with field assistance from Melissa Park and others.
An extended period of melting that lasted nearly to the end of September dramatically revealed the rim of Carmelo crater, the ice-filled crater under the summit ice cap at Mount Baker. This crater was active while Baker’s edifice was being built-up in the latest Pleistocene. The rim stretches across the entire width of the Roman Wall, at about 10,600. A pair of rock samples were collected from this pile of ejecta by American Alpine Institute climbing guide Forest McBrian. Snowfall at the end of September 2009 has already buried the ‘Gray Band’ for the year. Assuming the rim is again revealed next year, a detailed study will be made. The crater rim has been observed in particularly dry years since about 2003. They also show in a 1912 photo, and on a 1940 vertical aerial photo. Both photos are in the MBVRC archive.
Several Mount Baker webcam links have been added on the ‘links page’. These show views of Mount Baker from three different angles.
A highlight of the May 2007 Cordilleran GSA meeting at Western Washington University was the large number of research papers presented at the special symposium on Baker research. Abstracts from the symposium, and a few from other sessions, are listed on the Abstracts page. The field guide, edited by WWU's Dave Tucker and Pete Stelling, includes a field trip by Dave, Kevin Scott, and David Lewis that visits Holocene lava, lahar and debris avalanche deposits on the east flank of Mount Baker. The meeting guidebook is available from GSA.
On July 26th, a large mass of snow and ice broke off the east slope of Sherman Peak just below the summit. Sherman Peak is the high triangular peak on the south rim of Sherman Crater, just south of the deep East Breach. The slide quickly rode over outcrops of rock and hydrothermally altered pyroclastics, and became a muddy slurry. The dark, wet mass slid east down the Boulder Glacier for three kilometers before it stopped just short of the glacier terminus. A party of climbers was preparing to cross the glacier and witnessed the debris flow, which they said shook the ground and made a deafening roar. Such slides are periodic events at this precise location, and may be due to thermal activity in the source area. Frank and others (1975) estimated a volume of 35,000 m3 for a very similar slide. Dr. Jackie Caplan-Auerbach at Western Washington University has studied these phenomena in Alaska, and will continue this work at Mount Baker. Images of the slide deposit are dramatic. More images can be see on page 4 of John Scurlock's website. See also a paper describing earlier debris avalanches:
Frank, D., Post, A., and Friedman, J. D., 1975, Recurrent geothermally induced debris avalanches on Boulder Glacier, Mount Baker, Washington; Journal of Research, US Geological Survey, v. 3 n. 1, pp. 77-87
image by John Scurlock