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Bedform information


Current ripples preserved in sandstone of the Moenkopi Formation, Capitol Reef National Park, Utah, United States.

A bedform is a geological feature that develops at the interface of fluid and a moveable bed, the result of bed material being moved by fluid flow. Examples include ripples and dunes on the bed of a river. Bedforms are often preserved in the rock record as a result of being present in a depositional setting. Bedforms are often characteristic to the flow parameters,[1] and may be used to infer flow depth and velocity, and therefore the Froude number.

  1. ^ Southard, J B (1991). "Experimental Determination of Bed-Form Stability". Annual Review of Earth and Planetary Sciences. 19: 423–455. Bibcode:1991AREPS..19..423S. doi:10.1146/annurev.ea.19.050191.002231.

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Bedform

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A bedform is a geological feature that develops at the interface of fluid and a moveable bed, the result of bed material being moved by fluid flow. Examples...

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Antidune

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An antidune is a bedform found in fluvial and other channeled environments. Antidunes occur in supercritical flow, meaning that the Froude number is greater...

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Pyroclastic surge

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Hall, Minard; Ramón, Patricio; Dingwell, Donald B. (2013-10-13). "Dune bedforms produced by dilute pyroclastic density currents from the August 2006 eruption...

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Sedimentary structures

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varying speeds and velocities produce different structures, are called bedforms. In the lower flow regime, the natural progression is from a flat bed,...

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Ripple marks

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In geology, ripple marks are sedimentary structures (i.e., bedforms of the lower flow regime) and indicate agitation by water (current or waves) or directly...

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Sedimentary rock

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characteristic of turbidity currents. The surface of a particular bed, called the bedform, can also be indicative of a particular sedimentary environment. Examples...

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Martian soil

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regolith components identified at landing sites. Typical examples include: bedform (a feature that develops at the interface of fluid and a moveable bed such...

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Dune

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next blows in the dominant direction. Draas are very large-scale dune bedforms; they may be tens or a few hundreds of metres in height, kilometres wide...

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Aeolian processes

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represented by sand-flow maps. These are based on meteorological observations, bedform orientations, and trends of yardangs. They are analogous to drainage maps...

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Daniel Parsons

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R. et al., in press, 'The Role of Bio-physical Cohesion on Subaqueous Bedform Size', Geophysical Research Letters, February, 2016. Malarkey, J., Baas...

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Oxbow lake

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slope Stream pool Thalweg Bedrock river Canyon Knickpoint Plunge pool Bedforms Ait Antidune Dune Current ripple Regional processes Aggradation Base level...

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Fluvial sediment processes

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such as ripples, dunes, or antidunes on the river or stream bed. These bedforms are often preserved in sedimentary rocks and can be used to estimate the...

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Rhode Island Sound

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models to make topographical depictions of unknown glacial features and bedforms. Newfound glacial features include an ice-sculptured bedrock surface, residual...

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Sandstone

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Lithification Siltation Turbidity currents By structure Sedimentary structures Bedforms cross-bedding duness graded bedding ripple marks Alluvial fan Alluvial...

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Coast

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with tidal currents. Wave action is much more important for determining bedforms of sediments deposited along mesotidal and microtidal coasts than in macrotidal...

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Floodplain

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slope Stream pool Thalweg Bedrock river Canyon Knickpoint Plunge pool Bedforms Ait Antidune Dune Current ripple Regional processes Aggradation Base level...

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Braided river

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23 April 2011. Blodgett, R.H.; Stanley, K.O. (1980). "Stratification, Bedforms, and Discharge Relations of the Platte Braided River System, Nebraska"...

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Sedimentation

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Lithification Siltation Turbidity currents By structure Sedimentary structures Bedforms cross-bedding duness graded bedding ripple marks Alluvial fan Alluvial...

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Cyclic steps

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Cyclic steps are rhythmic bedforms associated with Froude super-critical flow instability. They are a type of sediment wave, and are created when supercritical...

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Dry Mesa Quarry

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flow velocities determined from grain size and bedforms. The river flow direction, based upon bedform orientations and bone elongation statistics, was...

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Sediment

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Lithification Siltation Turbidity currents By structure Sedimentary structures Bedforms cross-bedding duness graded bedding ripple marks Alluvial fan Alluvial...

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Sediment transport

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and viscosity, and can therefore not exert very much shear on its bed. Bedforms are generated by aeolian sediment transport in the terrestrial near-surface...

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Geology of Mars

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Rebecca M.; Stack, Kathryn M. (2021). "A Rock Record of Complex Aeolian Bedforms in a Hesperian Desert Landscape: The Stimson Formation as Exposed in the...

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Shallow water marine environment

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the smallest grains at the top. Also, Ripples, which are the smallest bedform type, and dunes, which are similar to ripples except are larger. Carbonaceous...

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Torres Strait

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Broadcasting Corporation. Retrieved 9 May 2015. Harris, P. T. (1988). "Sediments, bedforms and bedload transport pathways on the continental shelf adjacent to Torres...

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Camas prairie

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current ripples spread out and merge on the basin floor. These sedimentary bedforms are best seen in aerial images and at low sun angles. These giant current...

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Climate of Mars

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descend from the polar high to transport ice and create large wavelength bedforms. The spiral shape comes from Coriolis effect forcing of the winds, much...

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Parting lineation

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also the primary indicator of the lower part of the upper flow regime bedform. Parting lineation is a sedimentary structure commonly found on the surface...

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Drumlin

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ISBN 978-0-902246-04-1. Shaw, John (April 2002). "The meltwater hypothesis for subglacial bedforms". Quaternary International. 90 (1): 5–22. Bibcode:2002QuInt..90....5S....

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