(CLICK
PICTURE TO ENLARGE)
CRB and OPB: Columbia River and Oregon Plateau
Basalt
YSHS: Yellowstone Hotspot |
Steens Mountain, SE Oregon: Earliest Erupted Flows
of the Yellowstone Hotspot?
|
Monday 3:30-6:30 in
D250 EMS unless stated otherwise
1st Seminar: Hotspots, Large Igneous Provinces, and the Plume
Hypothesis (Rob Coe)
Coffin & Eldholm, 1993, Large Igneous
Provinces, Scientific American, October issue, 42-49.
(An easy-to-read, informative
introduction with nice graphics)
(A comprehensive review as of
1994, highly and still much cited, has all the essential background for this
seminar—look through it and keep it handy as a reference)
Link to an insightful
biographical sketch of J. Tuzo Wilson
2nd Seminar: Non-Plume Hypotheses for and Proposed Environmental Effects of LIPs (Rob Coe)
Anderson, 2005, Large igneous provinces,
delamination, and fertile mantle, Elements, 1, 271-275.
Wignall, 2001, Large igneous
provinces and mass extinctions, Earth Sci. Rev., 53, 1-33.
3rd Seminar:
Yellowstone LIP: Extent, Ages, Stratigraphy and Argument for a Shallow Source (Nick Jarboe)
Using Large-Scale Geophysical and Geological Features to Pinpoint Inception of Yellowstone Hotspot (Jonathan Glen, USGS)
4th Seminar:
Impact Mechanisms—Relevant or Irrelevant for the
Yellowstone LIP? (Cathy Plesko)
Jones, 2005, Meteorite impacts as
triggers of large igneous provinces, Elements, 1, 277-281.
Relation of YSHS to Basin and
Range Extension (Joe Colgan, USGS/Stanford)
5th Seminar:
Observations and Interpretations
of Upper Mantle Seismic Anisotropy (Samantha Hansen and Julie Rokosky)
Delamination Mechanisms and the
CRB Large Igneous Province (Cheryl Harrison)
Note: Supplementary Figure for Hales et al., 2005.
6th Seminar (Thursday May 11, 12:30-3:30, C332):
Seismic
Tomography of the Yellowstone Hotspot Region (Alex Hutko)
Thermochemical Plume Mechanisms
(Cheryl Harrison)
7th Seminar (Monday May 22, D250):
Eruption styles of YSHS basalt flows and pyroclastic
material (Darcy)
Self et al., 2005, Gas fluxes from flood basalt eruptions, Elements, 1, 283-287. (short)
Environmental effects of
Yellowstone hotspot LIP eruptions (Hilde Schwartz)
8th Seminar (Thursday May 25, 12:30-3:30, C332):
Yellowstone LIP Plume Hypothesis
(Nick Jarboe)
Yellowstone Hotspot: Model Constraints and Comparisons (Sarah Hall)
No assigned reading
9th Seminar (Monday June 5, D250):
Wrap up/Concluding Thoughts (Bob Christiansen, USGS)
New! 10 pages on
model for generation of the YSHS LIP and bimodal volcanism from:
Link to current version of schedule for future
seminars
Instructor:
Rob Coe rcoe@es.ucsc.edu 459-2393
The
world’s youngest Large Igneous Province, the Columbia River and Oregon Plateau
Basalt,
is a
continental flood basalt that has been attributed to the activity of the
Yellowstone hotspot.
Recent
symposia at the Goldschmidt and GSA meetings have shed much new light on this
topic.
Link to
2005 GSA Yellowstone Hotspot session abstracts
*
Where and when did the YSHS first erupt?
* Was
it catastrophic? Rate and mode of eruption.
*
Is there one volcanic track or two?
*
How has YSHS activity evolved?
*
Is the YSHS a plume or a shallow melting anomaly?
*
Are there diagnostic geophysical or geochemical signatures?
*
Did uplift precede or accompany eruption?
*
Was the YSHS a trigger for Basin and Range extension?
*
What were the climatic and biological effects?
Regular
meeting time will be arranged to fit students’ schedules. Sign up and/or email
me if you are interested,
and
come to the first organizational meeting, if you can, 12:00 Tues April 4 in 236
EMS to choose best time.