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Subject Item

n2:ENVO_00000167

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owl:Class

rdfs:label

bar

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n2:ENVO_00000012

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Geonames:H.BNK TGN:23191 FTT:210 Geonames:U.SHLU FTT:209 FTT:208 Geonames:U.BNKU Geonames:T.BAR Geonames:U.SHSU FTT:1195 FTT:5 Geonames:U.TNGU FTT:206 Geonames:H.SHOL EcoLexicon:bar TGN:21531 SWEETRealm:Bar Geonames:U.BKSU TGN:21480 TGN:21177

obo:hasRelatedSynonym

bank (hydrographic) Shoal sand spit shoals transverse bar hooked spit undersea shoal longshore bar barrier island ball tongue bank recurved spit marsh bar sand bar offshore bar shoal patches sand hom hook bar cuspate spit bay head bar sand bank bar (physiographic) sand lobe sandbar banks (seafloor) spit BAR bay bar tongue (seafloor) point cuspate bar barrier beach bay barrier baymouth bar shoal

n2:IAO_0000115

A linear shoaling landform feature within a body of water. Bars tend to be long and narrow (linear) and develop where a current (or waves) promote deposition of granular material, resulting in localized shallowing (shoaling) of the water. Bars can appear in the sea, in a lake, or in a river. They are typically composed of sand, although could be of any granular matter that the moving water has access to and is capable of shifting around (for example, soil, silt, gravel, cobble, shingle, or even boulders). The grain size of the material comprising a bar is related: to the size of the waves or the strength of the currents moving the material, but the availability of material to be worked by waves and currents is also important.

obo:hasBroadSynonym

seafloor feature

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ENVO

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ENVO:00000167