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Fault (geology) Satellite image of a fault in the Taklamakan Desert. The two colorful ridges (at bottom left and top right) used to form a single continuous line, but have been split apart by movement along the fault. In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant ...
Behavioral geography is an approach to human geography that examines human behavior by separating it into different parts. In addition, behavioral geography is an ideology/approach in human geography that makes use of the methods and assumptions of behaviorism to determine the cognitive processes involved in an individual's perception of or response and reaction to their environment.
Cognitive geography is an interdisciplinary study of cognitive science and geography. It aims to understand how humans view space, place, and environment. It involves formalizing factors that influence our spatial cognition to create a more effective representation of space. These improved models assist in a variety of issues, for example ...
Psychogeography is the exploration of urban environments that emphasizes interpersonal connections to places and arbitrary routes. It was developed by members of the Letterist International and Situationist International, which were revolutionary groups influenced by Marxist and anarchist theory as well as the attitudes and methods of Dadaists and Surrealists.
Theory. Basic Fault is a theory created by Michael Balint, which suggests that every human's basic fault is caused in one's childhood. Specifically, a negative event or trauma that occurs in one's childhood between them and an adult, causing a fixation on objects, intense and often overwhelming emotions and the incapacity to deal with stress.
The latter fault scarp (white line at the base of the tan hills) was formed in the 1983 Borah Peak earthquake. A fault scarp is a small step-like offset of the ground surface in which one side of a fault has shifted vertically in relation to the other. [1][2] The topographic expression of fault scarps results from the differential erosion of ...
Lifted fault-block geology Tilted fault-block formation in the Teton Range. Fault-block mountains often result from rifting, an indicator of extensional tectonics. These can be small or form extensive rift valley systems, such as the East African Rift zone. Death Valley in California is a smaller example.
The Garlock Fault moves at a rate of between 2 and 11 mm a year, with an average slip of around 7 millimeters. While most of the fault is locked, certain segments have been shown to move by aseismic creep, which is motion without resulting earthquakes. The Garlock is not considered to be a particularly active fault, seldom producing any shaking ...