Monday,
May 13, 2024
6:00 - 7:30 pm
Note: ETGS members participating virtually will receive an email with info for attending/logging into the meeting.
May 2024 Presentation
The Channeled Scablands of the Northwestern US - Geologic Puzzle or Formation by
Unique Processes.
By
Dr. Robert D. Hatcher, Jr.
Distinguished Scientist and Professor Emeritus
Earth and Planetary Sciences
UT-Knoxville
Abstract
The Channeled Scablands in western
Montana, northern Idaho, eastern and central Washington, and central
Oregon consist of areas of a sq km or larger that have been scoured
to Columbia River basalt bedrock separated by areas of several sq km
of thick rich soil (Palouse), boulders up to the size of small
houses that resemble glacial erratics (in a non-glaciated region),
dry waterfalls, and extensive aerial (loess), fluvial, and lake
deposits. They occur along the Columbia River Valley and shaped the
course of the Pleistocene river. Geologists of the early 20th
Century had concluded that they formed by slow uniformitarian
processes, but in the 1920s J. Harlen Bretz (Univ. Chicago)
suggested that they formed from large floods from failure of ice
dams along the Clark Fork River in western Montana. These floods
ice-dam lakes drained glacial Lake Missoula, whose existence had
been documented a few years before by geologist Joseph T. Pardee (USGS).
Pardee's data were seminal in supporting Bret's hypothesis. The
geological community, however, refused to accept Bretz's ideas for
decades - considering them an outrageous hypothesis - until the
1970s when the idea became accepted because of the huge amount of
confirming data that Pardee, Bretz,
and other geologists and NASA photos revealed. Bretz was finally
awarded the GSA Penrose Medal in 1979 for his work, two years before
he died.
Biography
Education: Vanderbilt University, Nashville, Tennessee B. A. 1961 (majors:
geology, chemistry; minor math), M. S. 1962 (geology), University of
Tennessee, Knoxville, Tennessee Ph. D. 1965 (structural geology; two
foreign languages required)
Professional Employment: Geologist, Humble Oil and Refining Company
(1965-66), Clemson University (1966-78, Assistant Professor to Full
Professor), Florida State University (1978-80, Full Professor),
University of South Carolina (1980-86, Full Professor), and
University of Tennessee-Knoxville and Oak Ridge National Laboratory
Distinguished Scientist (1986-2000), UT Distinguished Scientist and
Professor (2000-2018). University of Tennessee Distinguished
Scientist and Professor Emeritus 2018- Present.
Research Interests: Primary research goal is to gain a better
understanding of the evolution of continental crust, mostly through
the study of mountain chains and mature crust. Most of my research
has been concentrated in the southern and central Appalachians, but
large amounts of time have been spent visiting and studying other
mountain chains, and Precambrian continental crust. My primary
interest is in the mechanics and kinematics of large faults, which
form a natural transition into a related long-term interest in the
geologic controls of petroleum occurrence in the Appalachians,
radioactive waste management, the causes of intraplate seismicity
and geologic evidence for determination of recurrence intervals for
intraplate earthquakes. While I am a structural geologist, most of
my research is interdisciplinary, integrating stratigraphic,
geochronologic, geochemical, and geophysical data into structural
studies. I am primarily a field geologist, however, and field data
form the basis for all other supporting studies. I have been
involved for many years with geophysicists and geologists in other
academic institutions and the USGS in the geologic interpretation of
seismic reflection and potential field (aeromagnetic and gravity)
data.
Research Support: Received over $5M in grants and contracts from the
National Science Foundation, Nuclear Regulatory Commission, U.S.
Department of Energy, U.S. Department of the Interior, state
geological surveys, and private industry.
Professional Service (Abbreviated): Editor (with W. A. Thomas)
Geological Society of America Bulletin (1982-88); President,
Geological Society of America (1993); President, American Geological
Institute (1996); Trustee, GSA Foundation (1999-2007), Chair of the
GSA Foundation Board (2005-07); National Academy of
Sciences/National Research Council Board on Radioactive Waste
Management (1990-96); Federal Advisory Committee on Nuclear Reactor
Safety Research (Nuclear Regulatory Commission, 1993-96); Federal
Advisory Committee for the National Cooperative Geologic Mapping
Program (Department of the Interior, 1996-2006); Federal Advisory
Committee Oak Ridge Site Specific Advisory Board (2009-2015; have
also served on numerous committees of GSA, AAPG, AGU, and other
organizations. Fellow: AAAS, Geological Society of America,
Geological Association of Canada.
Medals and Awards: Geological Society of America Distinguished
Service Award (1988, the first ever awarded), AAPG I. C. White Award
(1997), honorary citizen of West Virginia (by the Governor, 1998),
John T. Galey Award by the Eastern Section of the American
Association of Petroleum Geologists (2001), American Geological
Institute Ian Campbell Medal (2006), Geological Society of America
Penrose Medal (2006), and American Geological Institute Marcus
Milling Legendary Geoscientist Medal (2014). The latter three medals
constitute the highest levels of career recognition/achievement
possible in my profession.
Publications: Author or co-author of >200 scientific publications,
including 10 books.
Graduate Students: 53 M. S. theses and 18 Ph. D. dissertations
completed since began working in graduate departments in 1978.
Greetings, and welcome to the May 13, 2024 ETGS hybrid meeting.
If you attend via Zoom as a courtesy please mute your cell phone or the microphone in your laptop/tablet to minimize background noise and feedback echoes. We will also make an effort to mute all participants - at least until the presentation is finished. Please use the chat feature to type any comments or questions you may have. We recommend that you send questions for the speaker to "everyone" so all participants can see the question. In the interest of time, we may hold the Q&A at the end of the presentation.
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