11.7: Student Responses
- Page ID
- 5670
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\(\newcommand{\avec}{\mathbf a}\) \(\newcommand{\bvec}{\mathbf b}\) \(\newcommand{\cvec}{\mathbf c}\) \(\newcommand{\dvec}{\mathbf d}\) \(\newcommand{\dtil}{\widetilde{\mathbf d}}\) \(\newcommand{\evec}{\mathbf e}\) \(\newcommand{\fvec}{\mathbf f}\) \(\newcommand{\nvec}{\mathbf n}\) \(\newcommand{\pvec}{\mathbf p}\) \(\newcommand{\qvec}{\mathbf q}\) \(\newcommand{\svec}{\mathbf s}\) \(\newcommand{\tvec}{\mathbf t}\) \(\newcommand{\uvec}{\mathbf u}\) \(\newcommand{\vvec}{\mathbf v}\) \(\newcommand{\wvec}{\mathbf w}\) \(\newcommand{\xvec}{\mathbf x}\) \(\newcommand{\yvec}{\mathbf y}\) \(\newcommand{\zvec}{\mathbf z}\) \(\newcommand{\rvec}{\mathbf r}\) \(\newcommand{\mvec}{\mathbf m}\) \(\newcommand{\zerovec}{\mathbf 0}\) \(\newcommand{\onevec}{\mathbf 1}\) \(\newcommand{\real}{\mathbb R}\) \(\newcommand{\twovec}[2]{\left[\begin{array}{r}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\ctwovec}[2]{\left[\begin{array}{c}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\threevec}[3]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\cthreevec}[3]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\fourvec}[4]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\cfourvec}[4]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\fivevec}[5]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\cfivevec}[5]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\mattwo}[4]{\left[\begin{array}{rr}#1 \amp #2 \\ #3 \amp #4 \\ \end{array}\right]}\) \(\newcommand{\laspan}[1]{\text{Span}\{#1\}}\) \(\newcommand{\bcal}{\cal B}\) \(\newcommand{\ccal}{\cal C}\) \(\newcommand{\scal}{\cal S}\) \(\newcommand{\wcal}{\cal W}\) \(\newcommand{\ecal}{\cal E}\) \(\newcommand{\coords}[2]{\left\{#1\right\}_{#2}}\) \(\newcommand{\gray}[1]{\color{gray}{#1}}\) \(\newcommand{\lgray}[1]{\color{lightgray}{#1}}\) \(\newcommand{\rank}{\operatorname{rank}}\) \(\newcommand{\row}{\text{Row}}\) \(\newcommand{\col}{\text{Col}}\) \(\renewcommand{\row}{\text{Row}}\) \(\newcommand{\nul}{\text{Nul}}\) \(\newcommand{\var}{\text{Var}}\) \(\newcommand{\corr}{\text{corr}}\) \(\newcommand{\len}[1]{\left|#1\right|}\) \(\newcommand{\bbar}{\overline{\bvec}}\) \(\newcommand{\bhat}{\widehat{\bvec}}\) \(\newcommand{\bperp}{\bvec^\perp}\) \(\newcommand{\xhat}{\widehat{\xvec}}\) \(\newcommand{\vhat}{\widehat{\vvec}}\) \(\newcommand{\uhat}{\widehat{\uvec}}\) \(\newcommand{\what}{\widehat{\wvec}}\) \(\newcommand{\Sighat}{\widehat{\Sigma}}\) \(\newcommand{\lt}{<}\) \(\newcommand{\gt}{>}\) \(\newcommand{\amp}{&}\) \(\definecolor{fillinmathshade}{gray}{0.9}\)1. Sample M1 has the following texture:
a. slaty cleavage
b. schistose foliation
c. gneissic banding
d. lineation
e. non-foliated
2. Sample M1 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
3. The dark minerals in Sample M1 are:
a. flat biotite micas
b. tabular amphiboles
c. flat muscovite micas
d. tabular feldspars
4. A possible protolith for Sample M1 is:
a. an ultramafic rock
b. basalt
c. limestone
d. granite
e. sandstone
5. Sample M2 has the following texture:
a. slaty cleavage
b. schistose foliation
c. gneissic banding
d. lineation
e. non-foliated
6. Sample M2 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
7. Sample M3 has the following texture:
a. slaty cleavage
b. schistose foliation
c. gneissic banding
d. lineation
e. non-foliated
8. Sample M3 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
9. A possible protolith for Sample M3 is:
a. bituminous coal
b. basalt
c. shale
d. clay
e. rhyolite
f. sandstone
10. Sample M3 is an example of:
a. high grade of metamorphism
b. intermediate grade of metamorphism
c. low grade of metamorphism
11. Sample M3 is used for:
a. road construction
b. statues
c. roof tiles
d. barbequing
12. Sample M4 has the following texture:
a. slaty cleavage
b. schistose foliation
c. gneissic banding
d. lineation
e. non-foliated
13. Sample M4 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
14. Sample M4 is mainly composed of this mineral:
a. biotite mica
b. amphibole
c. muscovite mica
d. calcite
e. quartz
15. Sample M4 is an example of:
a. high grade of metamorphism
b. intermediate grade of metamorphism
c. low grade of metamorphism
16. Sample M5 has the following texture:
a. slaty cleavage
b. schistose foliation
c. gneissic banding
d. lineation
e. non-foliated
17. Sample M5 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
18. Sample M5 is mainly composed of this mineral:
a. biotite mica
b. amphibole
c. muscovite mica
d. calcite
e. quartz
19. A possible protolith for Sample M5 is:
a. diorite
b. quartz
c. limestone
d. shale
e. sandstone
20. Sample M6 is mainly composed of this dark mineral:
a. biotite mica
b. amphibole
c. muscovite mica
d. calcite
e. quartz
21. Sample M6 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
22. A possible protolith for Sample M6 is:
a. basalt
b. granite
c. sandstone
d. limestone
e. shale
23. Sample M6 is an example of:
a. high grade of metamorphism
b. intermediate grade of metamorphism
c. low grade of metamorphism
24. Sample M7 has the following texture:
a. slaty cleavage
b. schistose foliation
c. gneissic banding
d. lineation
e. non-foliated
25. Sample M7 is called:
a. marble b. quartzite c. schist d. gneiss
e. slate f. anthracite coal g. amphibolite
26. A possible protolith for Sample M7 is:
a. basalt
b. granite
c. sandstone
d. limestone
e. shale
27. According to Figure 11.11, what mineral is unstable in the staurolite zone?
a. chlorite
b. muscovite
c. biotite
d. garnet
28. Refer again to Figure 11.11; which index minerals will not be found together in the same rock?
a. chlorite and garnet
b. chlorite and kyanite
c. biotite and staurolite
d. biotite and muscovite
29. Sample M1 from your rock kit is most likely an example of:
a. hydrothermal metamorphism
b. contact metamorphism
c. regional metamorphism
d. shock metamorphism
30. Sample M7 from your rock kit is most likely an example of:
a. fault zone metamorphism
b. contact metamorphism
c. regional metamorphism
d. shock metamorphism
31. Type 8 56 22.28N 126 55 54.33E in the search bar of Google Earth. Zoom out to an eye altitude of ~1700 miles. What type of metamorphism is likely in this area?
a. shock metamorphism
b. contact metamorphism
c. regional metamorphism
d. dynamic metamorphism
32. The agents of metamorphism in this region, are most likely:
a. chemically reactive fluids
b. temperature
c. pressure
d. both temperature and pressure
33. Type 35 06 53.42N 119 38 47.59W in the search bar of Google Earth. Zoom out to an eye altitude of ~8500ft. What type of metamorphism is likely in this area?
a. fault zone metamorphism
b. contact metamorphism
c. regional metamorphism
d. shock metamorphism
34. Evidence of metamorphism at this location could be from the discovery of:
a. gneiss
b. quartzite
c. tektites
d. mylonite
35. Type 35 01 38.93N 111 01 21.93W in the search bar of Google Earth. Zoom out to an eye altitude of ~12,000ft. What type of metamorphism is likely in this area?
a. fault zone metamorphism
b. contact metamorphism
c. regional metamorphism
d. shock metamorphism
36. Evidence of metamorphism at this location could be from the discovery of:
a. gneiss
b. quartzite
c. tektites
d. mylonite