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CH 11.1 How Rocks Deform

Name:________________________Date:_____
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Across
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A fold in which the youngest layer is in the center of the fold; commonly seen as a bowl shape
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Materials that respond to stress by breaking or fracturing
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The rock below the fault plane
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The area on the fold where the limbs meet
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A type of stress that squeezes and shortens a rock
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An isostatic adjustment where the lithosphere rises
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The rock above the fault plane
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Occurs when the rock on either side of a fault plane slides horizontally in response to shear stress
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A bend in a rock layer resulting from stress
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A fold in which both limbs are horizontal or almost horizontal
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A type of reverse fault in which the fault plane is at a low angle or is nearly horizontal
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A plane on a fold that could slice the fold in two symmetrical halves; they're rare
Down
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A break along which the surrounding rock moves
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Occurs when the buoyant force on the lithosphere and gravity are equal
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A type of stress that stretches and pulls a rock apart
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Materials that respond to stress by bending or deforming without breaking
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A fault in which the hanging wall moves downward relative to the footwall
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The fault created when compression causes the hanging wall to move upward relative to the footwall
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A fold in which the oldest layer is in the center of the fold
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Distorts a rock by pushing parts of the rock in opposite directions
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The surface or plane along which the motion of a fault occurs
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The sloping side of a fold
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Any change in the shape or volume of rock that results from stress
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The term that means a fold appears to be lying on its side
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A break along which there is no movement of the surrounding rock