About: Northumberland Trough

Facets (new session)
Description
Metadata
Settings
- Rule:
- Inverse Functional Properties:
- "Same As":

About: Northumberland Trough Goto Sponge NotDistinct Permalink

An Entity of Type : owl:Thing, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
QRcode icon

http://dbpedia.demo.openlinksw.com/describe/?url=http%3A%2F%2Fdbpedia.org%2Fresource%2FNorthumberland_Trough&invfp=IFP_OFF&sas=SAME_AS_OFF

The Northumberland Trough, also known as the Northumberland Basin, is an element of the structural geology of northern England, the origin of which dates back to the Carboniferous period when a block and basin province was established throughout the Pennine region.

Attributes	Values
rdfs:label	Northumberland Trough (en)
rdfs:comment	The Northumberland Trough, also known as the Northumberland Basin, is an element of the structural geology of northern England, the origin of which dates back to the Carboniferous period when a block and basin province was established throughout the Pennine region. (en)
dcterms:subject	Geology of the Pennines Carboniferous England Geology of Northumberland
Wikipage page ID	62304118 (xsd:integer)
Wikipage revision ID	925805156 (xsd:integer)
Link from a Wikipage to another Wikipage	Carboniferous England Crust (geology) Batholith Fault (geology) Half-graben Horst and graben Sedimentary basin Geology of the Pennines Alston Block Carboniferous England Granite Geology of Northumberland Geological Structure of Great Britain Structural geology Solway Basin The Pennines dbr:Cheviot_Block
sameAs	Northumberland Trough Northumberland Trough
dbp:wikiPageUsesTemplate	dbt:Geology-stub dbt:Reflist
has abstract	The Northumberland Trough, also known as the Northumberland Basin, is an element of the structural geology of northern England, the origin of which dates back to the Carboniferous period when a block and basin province was established throughout the Pennine region. The trough is an ENE-WSW aligned half-graben, an asymmetric depositional basin. It is defined to the south by the Stublick and Ninety Fathom faults, which separate the trough from the Alston Block. To the north, where its depth is least, the trough's boundary with the is less well-defined; nevertheless, the south-easterly down-throwing Featherwood and Alwinton faults can be identified along this margin. To the west, the trough is continuous with the Solway Basin. The surrounding blocks are buoyed up by granite batholiths maintaining these regions of the upper crust as areas of raised relief. (en)
prov:wasDerivedFrom	wikipedia-en:Northumberland_Trough?oldid=925805156&ns=0
page length (characters) of wiki page	1649 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Northumberland_Trough
is Link from a Wikipage to another Wikipage of	Alston Block Trough (geology) Northumberland Basin
is Wikipage redirect of	Northumberland Basin
is foaf:primaryTopic of	wikipedia-en:Northumberland_Trough

Faceted Search & Find service v1.17_git139 as of Feb 29 2024

Alternative Linked Data Documents: ODE Content Formats:

RDF

ODATA

Microdata

About

OpenLink Virtuoso version 08.03.3330 as of Mar 19 2024, on Linux (x86_64-generic-linux-glibc212), Single-Server Edition (378 GB total memory, 53 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software