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- Danube_Canyon abstract "The Danube Canyon (also known as the Viteaz Canyon) is a large submarine canyon which indents the shelf in the northwestern part of the Black Sea. It developed seawards during the late Pleistocene seaward along the Danube valley. The canyon continues into the most recent central channel in the relict Danube fan at the bottom of the Black Sea and has been the major route of the transport of the deposit from Danube river to the Danube fan.Near the shelf break zone the canyon is approximately 350m deep.".
- Danube_Canyon wikiPageID "20932426".
- Danube_Canyon wikiPageRevisionID "580275908".
- Danube_Canyon hasPhotoCollection Danube_Canyon.
- Danube_Canyon subject Category:Black_Sea.
- Danube_Canyon comment "The Danube Canyon (also known as the Viteaz Canyon) is a large submarine canyon which indents the shelf in the northwestern part of the Black Sea. It developed seawards during the late Pleistocene seaward along the Danube valley.".
- Danube_Canyon label "Danube Canyon".
- Danube_Canyon sameAs m.05b1yf4.
- Danube_Canyon sameAs Q5221255.
- Danube_Canyon sameAs Q5221255.
- Danube_Canyon wasDerivedFrom Danube_Canyon?oldid=580275908.
- Danube_Canyon isPrimaryTopicOf Danube_Canyon.