Homework #5 Due on Friday, March 6, 1998.
Sedimentary Rock Description
Instructions: Go to Bowman Hall (corner of Rose and Washington), to the Main Entrance on Washington St. (this entrance is the one with the big columns; you can't actually get into the building there, but it's still the main entrance). Carefully examine the rock that is used to make up the stairs, the columns, and the lowest 4 feet of the building in this area.
1. Sketch fossils. Look carefully for fossils in
this rock. Look at many different blocks of the rock to find several
good examples of fossils. They are mostly quite small and broken
into pieces. You probably won't be sure what type of fossil you are
seeing, but if it looks like an organized structure of some sort, and you
can find more than one example of it, it probably is a fossil. If you have
a magnifying glass, use it.
Sketch at least 5 different examples of fossils
you find, making sure that you represent at least two different types of
fossils. On each sketch, include a scale. For example,
if the fossil is only as big as this letter "O", try making your
sketch significantly bigger and including a note that shows how big the
actual fossil really was. Carefully describe each fossil in
a sentence or so.
2. Evidence for currents. Cross-bedding is found
in several of the rocks on the steps. The cross-bedding was apparently
made by small ripples, only a few centimeters high. On some of the
beds, you can find the cross-bedding on the top of the bed instead of on
the sides as it is shown in the book (see page 127). What do you
think cross-bedding might look like from the top?
Find two examples of cross-bedding
and sketch them, including a scale. Explain why you think this is
cross-bedding. Find something in the rock that you think might be
cross-bedding viewed from the top of a step, and sketch that too
(a third sketch). On some steps, you may be able to see both
sides and top on the same block of rock.
3. What kind of rock is this? Where did it form?
How hard is this rock? Try scratching it with your keys or a knife
and then with a copper penny. What mineral might make up the bulk
of this rock? What are fossils commonly made of? Is this a
chemical or detrital rock, do you think? What is the average grain
size?
Describe and give a name for
this rock, and explain carefully why you call it that. Then
explain what environment of deposition it might have formed in,
long ago. Explain why you suggest such an environment, including
what evidence you use to support your interpretation.