Matches in DBpedia 2014 for { <http://dbpedia.org/resource/Cross-bedding> ?p ?o. }
Showing items 1 to 32 of
32
with 100 items per page.
- Cross-bedding abstract "In geology, the sedimentary structures known as cross-bedding refer to (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.".
- Cross-bedding thumbnail Grant_1929_crossbedding.png?width=300.
- Cross-bedding wikiPageExternalLink seds.
- Cross-bedding wikiPageExternalLink bar.htm.
- Cross-bedding wikiPageID "5843584".
- Cross-bedding wikiPageRevisionID "597386681".
- Cross-bedding hasPhotoCollection Cross-bedding.
- Cross-bedding subject Category:Cross-bedding.
- Cross-bedding subject Category:Geology.
- Cross-bedding subject Category:Sedimentary_rocks.
- Cross-bedding subject Category:Sedimentology.
- Cross-bedding type Abstraction100002137.
- Cross-bedding type Material114580897.
- Cross-bedding type Matter100020827.
- Cross-bedding type Part113809207.
- Cross-bedding type PhysicalEntity100001930.
- Cross-bedding type Relation100031921.
- Cross-bedding type Rock114696793.
- Cross-bedding type SedimentaryRock114698000.
- Cross-bedding type SedimentaryRocks.
- Cross-bedding type Substance100019613.
- Cross-bedding comment "In geology, the sedimentary structures known as cross-bedding refer to (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 label "Cross-bedding".
- Cross-bedding label "Schrägschichtung".
- Cross-bedding sameAs Schrägschichtung.
- Cross-bedding sameAs m.0f8lq8.
- Cross-bedding sameAs Q1199509.
- Cross-bedding sameAs Q1199509.
- Cross-bedding sameAs Cross-bedding.
- Cross-bedding wasDerivedFrom Cross-bedding?oldid=597386681.
- Cross-bedding depiction Grant_1929_crossbedding.png.
- Cross-bedding isPrimaryTopicOf Cross-bedding.
