How Does Trough Cross Bedding Form?
Trough cross bedding is a type of sedimentary structure that forms when sediment is deposited in a trough-shaped depression. The trough is typically formed by a current of water or wind, and the sediment is deposited as the current flows past. The resulting cross-bedding has a distinctive appearance, with layers of sediment that dip in the same direction.
The formation of trough cross bedding involves several essential aspects:
- The presence of a trough-shaped depression
- A current of water or wind
- The deposition of sediment as the current flows past
The following paragraphs will explore each of these aspects in more detail, providing a comprehensive understanding of how trough cross bedding forms.
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