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Apr 11, 2024 · A basin is an area of depressed elevation generally surrounded by land at higher elevations. Basins can be on dry land or be filled with freshwater or saltwater. Over time, the land surrounding a basin erodes and the resulting sediment begins to fill the basin.
- 12.3: Basins, Sea Level, and Accommodation Space
All basins have limited space. The interplay between...
- 35.1: The History of the San Andreas Fault and the Basin and ...
Two important and related features were first recognized as...
- 12.3: Basins, Sea Level, and Accommodation Space
Apr 11, 2024 · All basins have limited space. The interplay between tectonic changes, global sea level, local water level, and sediment accumulation all affect changes in space within any given basin. This “accommodation space” is the volume of available within a basin to accommodate influxes of sediment.
- Introduction
- Basin and Range
- San Andreas Fault System
- Final Thoughts
- Further Reading
What happens when a mid-ocean ridge is subducted? The basics of plate tectonicsare essential to introductory geology. Two essential aspects are the idea that ocean basins grow via seafloor spreading at mid-ocean ridges and close via subduction. But what happens when these two processes combine? The answer to this is complicated, and is best exempli...
The Basin and Range is a singular geologic province that covers a large portion of the southwest United States and western Mexico. It is probably the best modern example of a wide rift; a continental divergent boundary where the deformation is spread out. Unlike typical (narrow) rifts, like the East African Rift, where the normal faulting due to te...
The other cause of extension in the Basin and Range has to do with the creation of the San Andreas Fault System, a complicated but vital piece of the story in understanding the modern plate boundary between the North American and Pacific Plates. In 1970, still in the infancy of the development of the theory of Plate Tectonics, Tanya Atwater publish...
For beginning geology students on the west coast of North America, the seemingly simple question “What plate boundary is on the western edge of the continent?” is a difficult one to answer. In California, the San Andreas Fault is the plate boundary, running east of Los Angeles and west of San Francisco, but in actuality the plate boundary is diffus...
https://www.nps.gov/articles/basinrange.htmNPS site on the Basin and Range Atwater, Tanya. “Implications of plate tectonics for the Cenozoic tectonic evolution of western North America.” Geological Society of America Bulletin81, no. 12 (1970): 3513-3536. Axen, Gary J., Wanda J. Taylor, and John M. Bartley. “Space-time patterns and tectonic controls...
Apr 11, 2024 · Two important and related features were first recognized as a result of studying Basin and Range extension: the detachment fault and the metamorphic core complex. Detachment faults, also called low-angle normal faults, were very controversial when they were first described.
Jan 22, 2020 · Updated on January 22, 2020. In geology, a basin is defined as a bounded area where the rock within the boundaries dips inward toward the center. By contrast, a range is a single line of mountains or hills forming a connected chain of land higher than the surrounding area.
- Amanda Briney
Many of the islands in the Aegean are ranges between basins that stand high enough to poke above sea level. Thus, whereas the dominant feature in a rift valley is the deep wide valley itself, the ranges and valleys are of comparable importance in basin and range topography.
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The Rio Grande rift and Basin and Range Province are two of the most iconic extensional domains on Earth; the Basin and Range Province is the archetypal example of a wide rift, and the neighboring Rio Grande rift is one of the classic modern examples of a narrow continental rift (e.g., Buck, 1991).
