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Homework
Assignment #1 GEOLOGY 100
Part
1 (due several days
before exam via email; consult syllabus for due date):
Use your lecture notes,
handouts, textbook, and
online chapter study guides
to answer the Part 1
Review Questions below.
Please
follow these guidelines in preparing your Part 1 review question responses:
Type out complete responses to each question.
Copy the questions and your responses,
paste them into the body of an email, and send them to
dsbarrie@yahoo.com
(do not attach as a separate file) by 11:59 pm on the assignment due date for
your section (see syllabus). Include plenty of space between your answers.
Include the following information in the subject
line of your email: last name, class, day(s) your class meets, homework set #
(e.g., Barrie GEOL 100 MW, Hmk 1)
Part
2 (due at beginning of
class on exam day, via hardcopy):
Earthworks workbook scenarios #1, #2, #3.
Part 1 Review Questions
-
Discuss four important characteristics of a scientific theory.
-
What distinguishes science from other fields of knowledge?
-
What
are Earth's principal compositional layers?
-
How do
these layers differ in terms of chemical composition and density?
-
How do
continental and oceanic crust differ in terms of density and composition?
-
What elements is each Earth layer enriched in?
-
Summarize the theory of plate tectonics.
-
Distinguish between the lithosphere and asthenosphere.
-
Describe the relative motion of two plates at various types of plate
boundaries, including subduction zones, collision zones, transform
boundaries, and divergent boundaries.
-
Summarize, in detail, the evidence that supports the theory of plate
tectonics.
-
What processes are thought to drive plate motions?
-
What
defining characteristics do all minerals possess?
-
Explain how the basic chemical building block of the silicate minerals—the
silicate tetrahedron--is put together. What is the chemical formula for
this structure? Why is the large negative of this structure important?
-
List
the silicate structure (e.g., isolated tetrahedra, single chains, double
chains, sheets, 3-D framework, etc.) of each of these minerals: olivine,
pyroxene, amphibole, biotite/muscovite, quartz, plagioclase feldspar (plag),
potassium feldspar (K-spar).
-
Understand the difference between the ferromagnesian and non-ferromagnesian
silicate minerals in terms of composition.
-
Describe some important mineral properties used to identify common minerals
in hand specimen.
-
What
is the order of crystallization (in terms of temperature) of various
minerals from a mafic magma as predicted by Bowen's Reaction Series?
-
Explain the different ways that magmas can change composition.
-
Distinguish between felsic, intermediate, and mafic magmas/igneous rocks in
terms of silica content, potassium (K) and sodium (Na) content, calcium (Ca)
content, and iron (Fe)/Magnesium (Mg) content. No need to list actual
percentates, just relative proportions (i.e., high, medium, or low).
-
What,
besides temperature, affects melting and crystallization?
-
What are the intrusive/extrusive equivalents for igneous rocks of felsic,
intermediate, and mafic composition?
-
Know
the factors that control the eruptive style of a volcano.
-
What
is the basic textural difference between plutonic and volcanic rocks in
terms of crystal size? What does this difference tell us about cooling
history?
-
Discuss the differences between the various volcano types, including shield
volcanoes, cinder cones, and stratovolcanoes.
-
Which type of volcano is most common at subduction zones? Which type is
most explosive? Which types are associated with mafic magma? Which type is
associated with intermediate magma?
-
Distinguish
the two main types of weathering, and list several examples each of
mechanical and chemical weathering processes.
-
Explain how the susceptibility of common silicate minerals to chemical
weathering relates to Bowen’s Reaction Series.
-
Explain how mechanical and chemical weathering act together (i.e., reinforce
each other) to disintegrate and decompose a rock mass.
-
Which type of weathering predominates in arid environments? In humid
environments?
Important Vocabulary (no need to
define these terms; just be familiar with them)
|
observation |
magma mixing |
|
hypothesis |
viscosity |
|
theory |
intrusive vs. extrusive |
|
law |
magma vs. lava |
|
Density |
felsic, intermediate, mafic |
|
inner core |
ultramafic |
|
mantle |
phaneritic |
|
oceanic crust |
aphanitic |
|
continental crust |
porphyritic |
|
lithosphere |
pyroclastic |
|
asthenosphere |
glassy |
|
divergent plate boundary |
granite & rhyolite |
|
divergent plate boundary |
diorite & andesite |
|
transform plate boundary |
gabbro & basalt |
|
subduction zone |
obsidian |
|
collision zone |
volcanic ash & tuff |
|
convection |
pumice |
|
ridge push |
shield volcano |
|
slab pull |
stratovolcano
(composite cone) |
|
trench
suction |
cinder cone |
|
hot spot (mantle plume) |
mechanical weathering |
|
mineral |
chemical weathering |
|
silicate tetrahedron |
|
|
atom/ion |
|
|
partial melting |
|
|
assimilation |
|
|
crystal settling |
|
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