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The state of balance between the thickness of the crust and the depth at which it floats on the asthenosphere is called
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
The increasing weight of mountains causes the crust to
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
Downcurved folds in rock are called
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
The type of stress that squeezes rocks together is
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
Gently dipping bends in rock formations with horizontal layers are called
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
The type of stress that pulls rocks apart is called
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
The force that changes the shape and volume of rocks is
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
A thick, ocean-floor deposits of sand, gravel, and rocks from a river is called a
compression
monoclines
sink
synclines
shearing
Geosyncline
stress
tension
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