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