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In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result of post-depositional deformation.…
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cross-beds sediment water dunes bed direction layers ripples beds flow environment forms paleocurrent tabular environments rivers bedforms side angle sand
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| ripples | instance of | which are known as cross-strata.Cross-bedding forms during deposition on the inclined surfaces of bedforms | 0.80 | text |
| dunes | instance of | which are known as cross-strata.Cross-bedding forms during deposition on the inclined surfaces of bedforms | 0.80 | text |
| ripples or dunes in a flowing fluid | instance of | FormationCross-bedding is formed by the downstream migration of bedforms | 0.80 | text |
| Cross-bedding | related to External links | USGSThe Bibliography | 0.60 | section |
| Cross-bedding | related to External links | Aeolian Research | 0.60 | section |
| Cross-bedding | related to Formation | The | 0.60 | section |
| Cross-bedding | related to Formation | At | 0.60 | section |
| Cross-bedding | related to Formation | Repeated | 0.60 | section |
| Cross-bedding | related to Geometries | The | 0.60 | section |
| Cross-bedding | related to Geometries | Tabular | 0.60 | section |
| Cross-bedding | related to Geometries | Trough | 0.60 | section |
| Cross-bedding | related to Internal sorting patterns | Cross-bedded | 0.60 | section |
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