1. Brittle deformation is generally seen in ____. (1 point)rocks with strong internal molecular bondsgypsum and shalerocks far below Earth’s surfacelimestone and schist2. The type of deformation in which the object permanently changes size and shape without fracturing is called ____. (1 point)brittle deformationductile deformationelastic deformationstress deformation3. A fault in which the hanging wall moves down relative to the footwall is a ____. (1 point)normal faultreverse faultthrust faultstrike-slip fault4. Orogenesis is a ____. (1 point)theory that explains the formation of strike-slip faultstype of faultinggeneral term for the processes that produce mountainstype of anticline
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1. Brittle deformation is seen in - Rocks that are present far below the earth's surface.
2. The kind of deformation because of which the object changes its shape and size permanently without any fracturing is called as - Ductile deformation.
3. The type of fault in which the hanging wall will go down in relative to the footwall is called as - Normal fault.
4. Orogenesis is a - general term that is used to describe the processes in which mountains and mountain belts are produced.
2. The kind of deformation because of which the object changes its shape and size permanently without any fracturing is called as - Ductile deformation.
3. The type of fault in which the hanging wall will go down in relative to the footwall is called as - Normal fault.
4. Orogenesis is a - general term that is used to describe the processes in which mountains and mountain belts are produced.
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