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Structured Geological Glossary: Structures

structure The shapes and position of rocks and their relationships to each other.
tectonics The study of the movements and deformation of the crust on a large scale, including epeirogeny, metamorphism, folding, faulting, and plate tectonics.
outcrop A segment of bedrock exposed to the atmosphere.
exposure A place where rocks can be seen in their natural position and not covered by debre, vegitation, or man-made objects.
stress A quantity describing the forces acting on each part of a body in units of force per unit area. Striation
strain "Change in a volume of a system induced by deformation; it is positive for dilation and negative for contraction and is distinct from regolith or volume reduction, which may be an isovolumetric removal of soluble constituents in solution without deformation."
deformation General term for folding, faulting, and other processes resulting from shear, compression, and extension of rocks.
plastic deformation Permanent deformation (change in size or shape) of soft, but solid rock by folding or flowing without fracturing
fracture Any break in rock along which no significant movement has occurred.
axis A plane intersecting the point where a folded bed shows maximum curvature.
diapir Forceful, upward intrusion of a rock mass into overlying rock. In the case of an igneous diapir, the intruding rock may be magma or a crystal-rich mush, either of which is less dense than the surrounding rock.
astrobleme A circular erosional feature that has been ascribed to the impact of a meteorite or comet.
lineament A linear (relatively straight) topographic feature or features such as a fault, line of dense vegetation, or a chain of aligned volcanoes.
paleorift Dead or dormant rift structure with no remaining transient or thermal phenomena (recent or contemporary magmatism or enhanced heat flow).
detachment plane The surface along which a landslide disconnects from its original position.
folded mountain belt A long linear zone of the Earth's crust where the rocks have been higly deformed by horizontal stresses or the intrusion of molten rock.
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