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Statements

Subject Item
dbr:Gala_Group_(geology)
rdfs:label
Gala Group (geology)
rdfs:comment
The Gala Group is a Silurian lithostratigraphic group (a sequence of rock strata) in the Southern Uplands of Scotland and northernmost England. The name is derived from Gala Water, a tributary of the River Tweed. The rocks of the Gala Group have also previously been known as the Queensberry Grits and the Strangford Group. Graded beds variously of wackestone, siltstone and mudstone are interpreted as turbidites and have been matched with the Central Belt turbidites which are seen in the Ards Peninsula in Northern Ireland. The strata are generally near-vertical and are bounded to the north by the Orlock Bridge Fault and to the south by the Laurieston Fault. Graptolites are found in a few beds.
dbp:name
Gala Group
dcterms:subject
dbc:Geology_of_England dbc:Geologic_formations_of_the_United_Kingdom dbc:Geological_groups_of_the_United_Kingdom dbc:Geology_of_Scotland dbc:Silurian_System_of_Europe
dbo:wikiPageID
51276978
dbo:wikiPageRevisionID
1115440914
dbo:wikiPageWikiLink
dbr:Scotland dbr:Orlock_Bridge_Fault dbr:River_Tweed dbc:Geology_of_England dbr:Siltstone dbc:Geology_of_Scotland dbr:Rhuddanian dbr:Turbidite dbc:Geological_groups_of_the_United_Kingdom dbr:Gala_Water dbc:Geologic_formations_of_the_United_Kingdom dbr:Silurian dbr:Group_(stratigraphy) dbr:Lithostratigraphy dbr:England dbr:Mudstone dbr:Moffat_Shale_Group dbr:Northern_Ireland dbr:Ards_Peninsula dbr:Wackestone dbc:Silurian_System_of_Europe dbr:Graptolite dbr:Rock_strata dbr:Southern_Uplands
owl:sameAs
yago-res:Gala_Group_(geology) wikidata:Q28434528 n13:2eCwZ
dbp:underlies
bounds Orlock Bridge Fault
dbp:wikiPageUsesTemplate
dbt:Short_description dbt:Refend dbt:Reflist dbt:Infobox_rockunit dbt:Cite_book dbt:Refbegin
dbp:age
Rhuddanian - Telychian Silurian
dbp:country
Scotland, England
dbp:thickness
360000.0
dbp:type
dbr:Group_(stratigraphy)
dbo:abstract
The Gala Group is a Silurian lithostratigraphic group (a sequence of rock strata) in the Southern Uplands of Scotland and northernmost England. The name is derived from Gala Water, a tributary of the River Tweed. The rocks of the Gala Group have also previously been known as the Queensberry Grits and the Strangford Group. Graded beds variously of wackestone, siltstone and mudstone are interpreted as turbidites and have been matched with the Central Belt turbidites which are seen in the Ards Peninsula in Northern Ireland. The strata are generally near-vertical and are bounded to the north by the Orlock Bridge Fault and to the south by the Laurieston Fault. Graptolites are found in a few beds.
dbp:namedfor
dbr:Gala_Water
dbp:overlies
dbr:Moffat_Shale_Group
dbp:prilithology
turbidites
prov:wasDerivedFrom
wikipedia-en:Gala_Group_(geology)?oldid=1115440914&ns=0
dbo:wikiPageLength
2229
foaf:isPrimaryTopicOf
wikipedia-en:Gala_Group_(geology)