- Explain how erosion and isostasy create a relatively thin and stable continental crust.
Your answer:
- How do the sequences of sedimentary rocks in cratons differ from those in mountain belts?
Your answer:
- What is the sequence of events that accounts for a mountain belt that is bounded on either side by a craton?
Your answer:
- The mountain belt that forms the western part of North America is called the
Your answer:
Appalachians
North American Cordillera
Andes
Himalaya
- The craton
Your answer:
covers the central part of the United States and Canada
has only 1,000-2,000 m of sedimentary rock overlaying basement rock
has rock beneath any sedimentary rock that is old plutonic and metamorphic rock
all of the above
- Which is not a stage in the history of a mountain belt?
Your answer:
subsidence
orogenic
accumulation
uplift and block-faulting
- To explain fold and thrust belts, simultaneous normal faulting, and how once deep-seated metamorphic rocks rise to an upper level in a mountain belt, geologists use a model called
Your answer:
ectonism
rogeny
gravitational collapse and spreading
faulting
- Which is not a type of terrane?
Your answer:
accumulated
exotic
suspect
accreted
- Which of the following is a source for terranes?
Your answer:
microcontinents
ocean crustal fragments
fragments of distant continents
all of the above
- Place these stages of mountain belt development in order: a. uplift and block faulting b. orogeny c. accumulation d. erosion to a craton
Your answer:
a,b,c,d
c,b,a,d
a,d,c,b
d,b,c,a