Convolute Bedding Geology Formation

By | November 14, 2019

Part of Speech

Noun

Essential Aspects of Convolute Bedding Geology Formation

Convolute bedding is a type of sedimentary structure that forms when soft sediment is deformed by the movement of water or ice. It is characterized by irregular, wavy layers of sediment that can be folded, crumpled, or even overturned. Convolute bedding is often found in turbidites, which are deposits of sediment that have been transported by gravity flows. It can also be found in other types of sedimentary deposits, such as deltaic and fluvial deposits, where rapid changes in flow conditions have caused soft sediment to deform.

Convolute bedding is a diagnostic feature of certain types of sedimentary environments. For example, the presence of convolute bedding in turbidites indicates that the sediment was deposited by a turbulent flow that caused the soft sediment to deform. Convolute bedding can also be used to determine the direction of flow in a sedimentary deposit, as the folds and crumples in the bedding can be used to infer the direction of the current or ice movement that caused the deformation.

Convolute bedding is an important geological feature that can tell geologists a lot about the processes that have shaped a sedimentary deposit. By studying convolute bedding, geologists can learn about the flow conditions during deposition, the direction of flow, and the type of sedimentary environment in which the deposit was formed.

Essential Aspects

Some of the essential aspects of convolute bedding geology formation include:

  • The type of sediment that is involved. Convolute bedding can form in any type of sediment, but it is most common in sandy and muddy sediments.
  • The amount of water or ice that is present. The amount of water or ice that is present can affect the severity of the deformation.
  • The速度 of the water or ice. The speed of the water or ice can also affect the severity of the deformation.
  • The direction of the water or ice movement. The direction of the water or ice movement can also affect the orientation of the convolute bedding.


A Convolute Bedding In Fine Grained

A Convolute Bedding In Fine Grained Sandstone Note That The Beds Scientific Diagram

Varieties Of Convolute Laminated Layers

Varieties Of Convolute Laminated Layers Interbedded With Undisturbed Scientific Diagram

Convolute Bedding Stock Image E410

Convolute Bedding Stock Image E410 0148 Science Photo Library

Convolute Lamination Within The Tiskre

Convolute Lamination Within The Tiskre Formation A Scientific Diagram

Learning Geology Post Depositional

Learning Geology Post Depositional Modification Of Sedimentary Layers

Convolute Lamination In The French Alps

Friday Field Photo 145 Convolute Lamination In The French Alps Wired

Convolute Laminations And Load

Convolute Laminations And Load Structures In Turbidites As Indicators Of Flow Reflections Decelerations Against Bounding Slopes Examples From The Marnoso Arenacea Formation Northern Italy Annot Sandstones South Eastern France Sciencedirect

Soft Sediment Deformation In Sandstone

Soft Sediment Deformation In Sandstone A Contorted Strata Giving Rise Scientific Diagram

Bedding And Lamination Geology Is The Way

Bedding And Lamination Geology Is The Way

Aecore Photograph Showing Interbedded

Aecore Photograph Showing Interbedded Occurrence Of Deformed Convolute Scientific Diagram

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