Matches in DBpedia 2015-10 for { <http://dbpedia.org/resource/Pennine_Fault_System> ?p ?o }
Showing triples 1 to 32 of
32
with 100 triples per page.
- Pennine_Fault_System abstract "The Pennine Fault System is a NW-SE trending zone of faulting that forms the southwestern boundary to the Pennines in Cumbria. It was formed as a normal fault during Permian rifting, bounding the Vale of Eden basin, which has a half-graben geometry. It links through to the Dent Fault at its southeastern end. Rocks of Ordovician and Silurian age outcrop between the two main strands of the fault, forming the Cross Fell inlier.".
- Pennine_Fault_System wikiPageID "45763119".
- Pennine_Fault_System wikiPageLength "1297".
- Pennine_Fault_System wikiPageOutDegree "14".
- Pennine_Fault_System wikiPageRevisionID "652232508".
- Pennine_Fault_System wikiPageWikiLink Category:Geology_of_Cumbria.
- Pennine_Fault_System wikiPageWikiLink Category:Pennines.
- Pennine_Fault_System wikiPageWikiLink Cross_Fell.
- Pennine_Fault_System wikiPageWikiLink Cumbria.
- Pennine_Fault_System wikiPageWikiLink Dent_Fault.
- Pennine_Fault_System wikiPageWikiLink Fault_(geology).
- Pennine_Fault_System wikiPageWikiLink Graben.
- Pennine_Fault_System wikiPageWikiLink Inliers_and_outliers_(geology).
- Pennine_Fault_System wikiPageWikiLink Ordovician.
- Pennine_Fault_System wikiPageWikiLink Pennines.
- Pennine_Fault_System wikiPageWikiLink Permian.
- Pennine_Fault_System wikiPageWikiLink Rift.
- Pennine_Fault_System wikiPageWikiLink Silurian.
- Pennine_Fault_System wikiPageWikiLink Vale_of_Eden.
- Pennine_Fault_System wikiPageWikiLinkText "Pennine Fault System".
- Pennine_Fault_System hasPhotoCollection Pennine_Fault_System.
- Pennine_Fault_System wikiPageUsesTemplate Template:Reflist.
- Pennine_Fault_System subject Category:Geology_of_Cumbria.
- Pennine_Fault_System subject Category:Pennines.
- Pennine_Fault_System comment "The Pennine Fault System is a NW-SE trending zone of faulting that forms the southwestern boundary to the Pennines in Cumbria. It was formed as a normal fault during Permian rifting, bounding the Vale of Eden basin, which has a half-graben geometry. It links through to the Dent Fault at its southeastern end. Rocks of Ordovician and Silurian age outcrop between the two main strands of the fault, forming the Cross Fell inlier.".
- Pennine_Fault_System label "Pennine Fault System".
- Pennine_Fault_System sameAs m.0130s3r8.
- Pennine_Fault_System sameAs Q20127987.
- Pennine_Fault_System sameAs Q20127987.
- Pennine_Fault_System sameAs 奔宁山脉断裂带.
- Pennine_Fault_System wasDerivedFrom Pennine_Fault_System?oldid=652232508.
- Pennine_Fault_System isPrimaryTopicOf Pennine_Fault_System.