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Lag deposit information


Lag deposit in Soria, Spain

A lag deposit is the deposition of material winnowed by physical action. Aeolian processes, fluvial processes, and tidal processes can remove the finer portion of a sedimentary deposit leaving the coarser material behind.

Lag deposits are found in processes such as central island formation in streams and rivers.[1] One theory of desert pavement formation is that they are an aeolian lag deposit. Armored beaches and inlets can be composed in part by lag deposits of shells or cobbles created when tidal forces strip away the finer sand and silt.[2]

  1. ^ Miller, Luna B. Leopold, M. Gordon Wolman, John P. (1995). Fluvial processes in geomorphology (Dover ed.). New York: Dover Publications. pp. 285–287. ISBN 0486685888.{{cite book}}: CS1 maint: multiple names: authors list (link)
  2. ^ eds., Richard A. Davis Jr., Robert W. Dalrymple (2011-10-20). Principles of tidal sedimentology. Dordrecht: Springer. p. 307. ISBN 9789400701236. {{cite book}}: |last= has generic name (help)CS1 maint: multiple names: authors list (link)

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Lag deposit

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A lag deposit is the deposition of material winnowed by physical action. Aeolian processes, fluvial processes, and tidal processes can remove the finer...

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Mosasaurus

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low-sediment conditions. A third hypothesis proposes that the layer is a lag deposit of Cretaceous sediments forced out by a strong impact by a tsunami, and...

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Aeolian landform

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Aeolian landforms are produced by either the erosive or depositive action of wind. These features may be built up from sand or snow, or eroded into rock...

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Otodus chubutensis

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shelf of Onslow Bay, North Carolina, USA: implications for processes of lag deposit formation". Ichnos. 27 (2): 122–141. doi:10.1080/10420940.2019.1697257...

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Climate of Mars

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ice sublimates (turns directly to a gas) and leaves behind a lag of dust. The lag deposit caps the underlying material so with each cycle of high tilt...

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Chenier

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behind lag deposits of mainly bivalve and gastropod shells separated out from the finer substrate beneath. Waves and currents then heap these deposits to...

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Composition of Mars

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was overlying rock, and then became concentrated on the surface as a lag deposit. The concentration of spherules in bedrock could have produced the observed...

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Polygonal patterned ground

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showing formation of high center polygons. Ice-rich mantle develops a lag deposit. Stresses create cracks. Increased sublimation along cracks causes troughs...

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History of Swindon

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and likely sets of sarsen erratic boulders, presumably derived as a lag deposit from long dissolved chalk and possibly moved by very ancient glaciations...

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Bravoceratops

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over an area of ten square metres; the site is thought to have been a lag deposit of a river, only most durable extremities able to survive preservation...

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Ellisdale Fossil Site

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sequence in a lag deposit consisting of siderite pebbles, poorly graded sand, and lignite. The fossil layer is considered a single-event storm deposit based on...

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Asteroidal water

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impurities in ice may form a crust after its parent ice escapes: a lag deposit. On a geologic scale, the larger asteroids can shield water, phyllosilicate...

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Latitude dependent mantle

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for a very long time before all the ice is gone because a protective lag deposit forms on the top. The mantle contains ice and dust. After a certain amount...

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Cylindracanthus

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(2010-07-14). "Osteichthyans from an Arkadelphia Formation–Midway Group lag deposit (Late Maastrichtian–Paleocene), Hot Spring County, Arkansas, U.S.A."...

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Danuri

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and interpret their nature ShadowCam will search for frost, ice, and lag deposits by mapping reflectance with resolution and signal-to-noise ratios comparable...

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Hell Creek Formation

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Edmontosaurus. This is surprisingly consistent in (1) the two major lag deposits (MOR loc. HC-530 and HC-312) in the Apex sandstone and Jen-rex sand where...

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Caumasee

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(Romansh: Lag la Cauma or Lai da Cauma) is a lake near Flims, in the Grisons, Switzerland. It is one of the lakes on the Flims Rockslide deposits. The lake...

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Glaciers on Mars

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ice sublimates (turns directly to a gas) and leaves behind a lag of dust. The lag deposit caps the underlying material so with each cycle of high tilt...

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Nankoweap Formation

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disc-shaped pebbles of Dox Sandstone and occasional pebbles of basalt lava. A lag deposit of gravel composed of white to yellowish, small pebble to cobble size...

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486958 Arrokoth

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which they were eroded due to the sublimation of volatiles, exposing lag deposits of darker material irradiated by sunlight. Another bright region (rm)...

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Sinus Meridiani

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was overlying rock, and then became concentrated on the surface as a lag deposit. The concentration of spherules in bedrock could have produced the observed...

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Paleobiota of the Hell Creek Formation

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Edmontosaurus. This is surprisingly consistent in (1) the two major lag deposits (MOR loc. HC-530 and HC-312) in the Apex sandstone and Jen-rex sand where...

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Potash

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expeditions discovered the reserves in the 1950s but commercial exploitation lagged until Deng Xiaoping's Reform and Opening Up Policy in the 1980s. The 1989...

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North African climate cycles

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000-year cycle that lags the maximum in precession insolation by roughly 5000 to 6000 years. To explain these cyclic freshwater diatom deposits we have to look...

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Nilosyrtis Mensae

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ice sublimates (turns directly to a gas) and leaves behind a lag of dust. The lag deposit caps the underlying material so with each cycle of high tilt...

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Two Medicine Formation

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or rock body, in northwestern Montana and southern Alberta that was deposited between 83.5 ± 0.7 Ma and 70.6 ± 3.4 Ma (million years ago), during Campanian...

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Deuteronilus Mensae

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ice sublimates (turns directly to a gas) and leaves behind a lag of dust. The lag deposit caps the underlying material so with each cycle of high tilt...

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