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Basal slip involves the movement of crystal planes over each other in a preferred direction, usually parallel to the basal plane, allowing for plastic deformation in materials like metals. Internal plastic flow refers to the movement of dislocations within the material, leading to permanent deformation without fracture. While basal slip is more common in crystalline materials with well-defined crystal structures, internal plastic flow can occur in various materials with defects and dislocations.

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What are 3 types of glacier movement?

Three types of glacier movement are basal sliding, internal deformation, and flow. Basal sliding occurs when the glacier moves over a layer of meltwater at its base. Internal deformation involves the slow movement of ice crystals within the glacier. Flow refers to the overall movement of the glacier downslope due to gravity.


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The internal capsule passes between the diencephalic and the basal ganglia, and through parts of the basal ganglia which is what gives them their striped appearance. The corpus striatum is another term for the caudate nucleus and the lentiform nucleus collectively. The corpus striatum us a part if the basal ganglia. ( islands of grey matter within the white matter if the brain) So pretty much the internal fibers pass through it!


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The basal surface of weathering refers to the base or bottom layer of material that is undergoing weathering processes such as physical or chemical breakdown. This layer is often in contact with the underlying bedrock or parent material, and serves as the point where weathering processes begin. The basal surface plays a crucial role in shaping landscapes and influencing the movement of weathered material.


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