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- Q1199509 subject Q7034677.
- Q1199509 subject Q7163795.
- Q1199509 subject Q8430225.
- Q1199509 abstract "In geology, the sedimentary structures known as cross-bedding are the (near-) horizontal units that are internally composed of inclined layers. This is a case in geology in which the original depositional layering is tilted, and the tilting is not a result of post-depositional deformation. Cross-beds or "sets" are the groups of inclined layers, and the inclined layers are known as cross strata.Cross bedding forms during deposition on the inclined surfaces of bedforms such as ripples and dunes, and indicates that the depositional environment contained a flowing medium (typically water or wind). Examples of these bedforms are ripples, dunes, anti-dunes, sand waves, hummocks, bars, and delta slopes. Cross-bedding is widespread in many environments. Environments in which water movement is fast enough and deep enough to develop large-scale bed forms fall into three natural groupings: rivers, tide-dominated coastal and marine settings.".
- Q1199509 thumbnail Amer0038_-_Flickr_-_NOAA_Photo_Library.jpg?width=300.
- Q1199509 wikiPageExternalLink bar.htm.
- Q1199509 wikiPageExternalLink seds.
- Q1199509 wikiPageWikiLink Q1069.
- Q1199509 wikiPageWikiLink Q12758989.
- Q1199509 wikiPageWikiLink Q185816.
- Q1199509 wikiPageWikiLink Q1982302.
- Q1199509 wikiPageWikiLink Q1994702.
- Q1199509 wikiPageWikiLink Q215839.
- Q1199509 wikiPageWikiLink Q2362281.
- Q1199509 wikiPageWikiLink Q25391.
- Q1199509 wikiPageWikiLink Q28337.
- Q1199509 wikiPageWikiLink Q390511.
- Q1199509 wikiPageWikiLink Q4022.
- Q1199509 wikiPageWikiLink Q43197.
- Q1199509 wikiPageWikiLink Q4879253.
- Q1199509 wikiPageWikiLink Q5468750.
- Q1199509 wikiPageWikiLink Q5744137.
- Q1199509 wikiPageWikiLink Q586117.
- Q1199509 wikiPageWikiLink Q5988006.
- Q1199509 wikiPageWikiLink Q7034677.
- Q1199509 wikiPageWikiLink Q7127148.
- Q1199509 wikiPageWikiLink Q7163795.
- Q1199509 wikiPageWikiLink Q81659.
- Q1199509 wikiPageWikiLink Q8430225.
- Q1199509 comment "In geology, the sedimentary structures known as cross-bedding are the (near-) horizontal units that are internally composed of inclined layers. This is a case in geology in which the original depositional layering is tilted, and the tilting is not a result of post-depositional deformation.".
- Q1199509 label "Cross-bedding".
- Q1199509 depiction Amer0038_-_Flickr_-_NOAA_Photo_Library.jpg.