Write a final report of the Ppc, lower & upper Trw& Trt. This should include the following:• Abstract and conclusions (completeness, accuracy)
• Introduction (statement of problem)
• Geologic setting (you can use outside sources for this section)
• Rock descriptions and depositional environments (Make sure to include
measurements for all features+ Include units photos) (a paragraph for each unit)
• Structural descriptions and interpretation
• Discussion and geologic history
• Language usage and required elements (refs., fig. captions, etc. can be from the slides
with appropriate caption and reference)
• Reference
To write the report, you should first go over formation units given in the slides and
examine and interpret them. The report MUST be written based on your observations
and interpretations seen on the units not from outside sources.
Slides:
https://drive.google.com/drive/folders/1AJaLfGUSUf84lK0Rqr0kRMXDuMDBYtcq?usp=
sharing
Note:
The park city (Ppc) formation has 4 units, lower & upper Woodside shale (Trw) formation has 4
units, and Triassic Thayne (Trt) formation has 1 unit. Also, keep an eye to the report format fig
above.
Here is an introduction section example but you MUST rewrite completely again
Introduction:
The main focus of the study is to examine the environmental formation of Limekiln
Gluch, Dry Creek and Cephalopod Gluch geological areas. With various techniques, the
identified location is USGS 7.5’ Fort Douglas UT quadrangle map using a scale of 1:12000. This
is done by using, sketching stratigraphic columns, measuring bedding attitudes, taking photos
and interpreting the geological history. The sketching of stratigraphic columns was necessary to
estimate the geological age scale of the area or crop, and the relative locations of these units with
respect to one another. The measured strike and dip were important to plot the bedding data into
the base map. The photos were primary key as they helped to get a consist measurements of the
observed crops and their geological features. Finally, the interpreting the geological history was
a great tool to understand the big picture of the observed units.