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(This page is somewhat "old"; more up-to-date information about research is
at the Electron Microprobe Lab page
Research Interests and Projects
Volcanic eruptions and early peoples of the Alaska
Peninsula:
I am working toward development of a tephrochronology for the
Cold Bay
region of the Alaska Peninsula, in collaboration with Dave Mickelson
and
his students Tina Dochat (Ph.D. 1997) and Eric Carson. As many of the
tephra layers present here are from Unimak volcanoes to the
southwest,
proximal tephras from Unimak are important. This project is also tied
in
with the anthropological research being carried out by H. Maschner
(Dept
of Anthropology) and associates in the Izembek Lagoon area and on
Unimak Island.
Aleutian Volcanic Action
Akutan Volcano 3/96
198 KB image of Akutan
Photo by U.S.G.S.
For more details on active Aleutian volcanoes:
Alaska Volcano
Observatory
Aleutian arc volcanism:
I have been studying Shishaldin
Volcano,
one of the largest Aleutian volcanic centers, since 1984. Unlike other
Aleutian volcanoes, Shishaldin has erupted a wide range of lavas and
pyroclastics -- 3 types of basalts as well as dacite, with apparently
little andesite. A major question in arc petrology concerns the
significance of high alumina basalts, which generally have abundant
plagioclase phenocrysts, and their relation to high magnesian basalts.
A variety of tools are used, including major and trace element
geochemistry, mineral chemistry, phase equilibria, plus the recently
developed crystal size distribution technique.
Shishaldin page with
photos
Sulfur-rich Volcanic Eruptions
and Magmatic Anhydrite
Some recent volcanic eruptions
have been recognized as having high sulfur contents, which may
have
significant climatic effects. I have been studying anhydrite-bearing
pumices from the 1985 eruption of Nevado del Ruiz (Colombia) and
the
1991 eruption of Mt. Pinatubo. As anhydrite phenocrysts rapidly
dissolve away after several rainy seasons, the presence of such
sulfur-rich eruptions in the geologic record is poorly known. The
discovery of anhydrite inclusions within other phenocrysts (e.g.,
plagioclase, hornblende, or orthopyroxene as shown in this BSE
image),
however, may provide a valuable clue to
discovering past sulfur-rich eruptions. The host minerals for the
inclusions can also provide important clues to the pre-eruption
magmatic conditions (e.g., pressure, temperature and melt water
content).
Magmatic anhydrite page
Courses Taught:
Geology 875-004: Explosive Volcanism, Volcanic Ash, and
Tephrochronology Graduate seminar, Spring 1996, for students
from Geology, Geography, Soil Science, Anthropology, and
Atmospheric
Sciences
Syllabus, readings and software
Geology 777: Electron Microprobe Analysis
This 2-credit course is taught once a year and provides a theoretical
background to an understanding and appreciation of the operation of
the
electron microprobe. Actual hands-on training for running the SX50
is
provided at the time that a user requires it.
Syllabus, readings and software
SELECTED PUBLICATIONS
Fournelle J, Carmody R and Daag A (1996) Anhydrite-bearing
Pumices from the June 15, 1991 Eruption of Mount Pinatubo:
Geochemistry, Mineralogy, and Petrology, in Fire and Mud: Eruiptions
and
Lahars from Mount Pinatubo, Philippines, Edited by Newhall and
Punongbayan, PHIVOLCS-University of Washington, p. 845-863
Fournelle J, Marsh BD and Myers JD (1994) Age, character and
significance of Aleutian Arc Volcanism, in Plafker and Berg (ed)
Cordilleran Orogen: Alaska (Volume G-1 of The Decade of North
American
Geology, published by the Geological Society of America).
Fournelle J and Marsh BD (1991) Shishaldin Volcano: Aleutian
high-alumina basalts and the plagioclase accumulation question.
Geology 19:234-237.
Fournelle J (1990) Anhydrite in Nevado del Ruiz November 1985
pumice:
relevance to the sulfur problem. Journal of Volcanology and
Geothermal
Research 42:189-201.
I run the UW-Madison electron microprobe lab, which consists of a
state of
the art Cameca SX50 electron microprobe #485 (installed in late
1993),
and associated equipment.
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