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OpenStudy (anonymous):
Mountains resulting from sideways pressure on the crust are:
volcanic
fault block
dome
folded
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OpenStudy (anonymous):
hey!! your back
OpenStudy (study312):
anytime
OpenStudy (anonymous):
nice
OpenStudy (study312):
wow a medal already
OpenStudy (anonymous):
yep for coming back
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OpenStudy (study312):
it's A
OpenStudy (anonymous):
thanx
OpenStudy (anonymous):
Igneous intrusions injected between horizontal layers are:
batholiths
dikes
sills
cones
OpenStudy (anonymous):
pleazz
OpenStudy (study312):
Igneous intrusions that are concordant (parallel to bedding planes of country rocks) are known as sills, whereas dykes cut through the bedding.
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OpenStudy (whpalmer4):
no, the first one is NOT A
OpenStudy (study312):
It's fault isn't it @whpalmer4
OpenStudy (anonymous):
why
OpenStudy (whpalmer4):
no, folded. volcanic mountains are formed by magma coming up through the crust. folded mountains occur where plates collide and crumple
OpenStudy (study312):
Dang that was on the tip of my tongue
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OpenStudy (anonymous):
ok
OpenStudy (anonymous):
gneous intrusions injected between horizontal layers are:
batholiths
dikes
sills
cones
OpenStudy (anonymous):
how bout this one
OpenStudy (study312):
It's sills I already answered that one I thought
OpenStudy (anonymous):
k thanx
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OpenStudy (study312):
thats it?
OpenStudy (anonymous):
Igneous rocks are made mainly of compounds of:
carbon and hydrogen
silicon and oxygen
carbon and silicon
carbon and oxygen
OpenStudy (anonymous):
this ???
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