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Geography 393
Geology 393
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393 WE OBJECTIVES
For
Geology 393 you are to devise a detailed workplan (see
Itinerary and
Costs for base),
and place sufficient
reference
diagrams and documentation forms into your
field
book,
enabling you to record the appropriate type,
quantity, and utility of formation and fossil data at all sites. Please develop proficiency with instrumentation and
relevant samples (in Science D328) BEFORE you venture into the field.
ALL
data (GPS measurements, photographs, literature, etc.) are joint property of all trip
participants, and you will share it without reservation with all other 393 students and
faculty on this excursion. Upon our return, there will be an electronic public
folder holding such information for all participants at \\GeoDept1\Classes\Geo393\.
Use these materials to develop your
technical report and poster for
presentation.

WE ASSIGNMENTS: This is a writing emphasis (WE)
course, but with rather different assignments than in conventional classroom
courses. My principal objectives for iterative
field writing are:
•
PLANNING: logistics, itinerary, budget, and
contingencies workplan. Audience: project
reviewer; draft: F14DEC07; final: F21DEC07
• IMPLEMENTATION: documentation log
sufficient that another person, without contact with the author, could
accurately reconstruct/replicate all field activities at any time in the
future. Additionally, real-time evaluation (and adjustment as necessary)
of accomplished tasks, with written declaration of immediate intentions,
is necessary in
progress
reports.
Audience: field supervisor; progress reports:
S05JAN, T08JAN, F11JAN, Su13JAN; log: W16JAN (return F18JAN)
• ANALYSIS: compilation, reflection,
interpretation, evaluation, and communication of excursion findings in
either a technical report and a collaborative poster
exhibit. Audience: professional public; draft:
F18JAN; final: F25JAN
The
Park Service
needs
volunteers to assist them in a variety of necessary projects that
funding cuts prevent the Big Bend staff from accomplishing. Your field notes
and reports will go to the Park officials in February to provide
such service assistance.
Prior
geology students have been able to successfully discern the sedimentary and igneous
formations of Mariscal Mountain (2000) quite
well. Nearby Talley Mountain
(2004),
however, was anomalous, even though the Maxwell geology
map shows it as just another igneous formation. Apparently,
something in its composition caused its reflectance to differ from the
igneous rock of Mariscal. Similarly,
Dominguez Mountain (2005) was an igneous formation that differed from
both Mariscal and Talley.
Later,
students performed a brief geologic survey of the Park's westernmost
extremity, at
Mesa de
Anguila
(2006).
Then
students focused substantial upon the fossil deposits in the Cretaceous
formations in eastern Big Bend's
Cuesta Carlota
(2007),
and began tracing the Cretaceous-Tertiary (K-T) boundary marking the end of the
dinosaurs.
Your task
will be to visit,
identifying fossils or making other geological observations, to map the
relatively new (~1980)
Rosillo Flats
addition. Ross Maxwell's geology
map of the 1960s did not include this then-private land. You in 2008
will begin mapping Rosillo geologic formation contacts, further trace the
K-T boundary, and seek Park boundary monuments.
-
current
weather (Big Bend National Park)
Comfort/Health
Indices Calculator
For unfamiliar geophysical terms, see the external web site for a
Geology Glossary and the
external web site for a
Meteorological
Glossary. There is also an external web site
having an extensive Ecological Glossary.
Heywood
[email] maintains this page, last updated 23NOV07. We
monitor our cell phone from 6 to 8 PM CST when in
range.
That number is (715)
459-8181. |