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Tectonic uplift. Former sea bottom that raised during the 2013 Bohol earthquake - the water used to extend to the mangroves at right. Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in the mean elevation of a region can only occur in response to ...
Uplift Universe. The Uplift Universe is a fictional universe created by American science fiction writer David Brin. A central feature in this universe is the process of biological uplift . His books which take place in this universe are: There is also a short story, "Aficionado" [ 1] (originally titled "Life in the Extreme"), published in 1998 ...
Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy ( glacial isostatic adjustment, glacioisostasy ...
Oceanic crust: 0–20 Ma. 20–65 Ma. >65 Ma. Orogeny ( / ɒˈrɒdʒəni /) is a mountain - building process that takes place at a convergent plate margin when plate motion compresses the margin. An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges.
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The Laramide orogeny was caused by subduction of a plate at a shallow angle. The orogeny is commonly attributed to events off the west coast of North America, where the Kula and Farallon Plates were sliding under the North American plate. Most hypotheses propose that oceanic crust was undergoing flat-slab subduction, that is, subduction at a ...
The Uplift Storm trilogy, also called The Uplift Trilogy is a series of novels set in David Brin's Uplift Universe. [1] The entire trilogy is one long tale, with no gaps in the timeline between volumes.
River erosion can be driven by tectonic uplift, climate, or potentially both mechanisms. It is difficult in many areas, however, to decisively pinpoint whether tectonism or climate change can individually drive tectonic uplift, enhanced erosion, and therefore terrace formation. In many cases, simplifying the geologic issue to tectonic-driven vs ...