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Arbuthnott-Garvock Group

The Arbuthnott-Garvock Group (or Arbuthnot-Garvock Group) is a Devonian lithostratigraphic group (a sequence of rock strata) in central Scotland. The name is derived from the village of Arbuthnott in Aberdeenshire and the Hill of Garvock near Laurencekirk.[1] The group comprises the previously separate overlying Garvock Group and the underlying Arbuthnott Group.

Arbuthnott-Garvock Group
Stratigraphic range: ?Lochkovian-Pragian, (Devonian)
TypeGroup
Unit ofOld Red Sandstone Supergroup
Sub-unitsCatterline Conglomerate, Scone Sandstone, Craighall Conglomerate, Ruchil Flagstone and Craig of Monievreckie Conglomerate formations
UnderliesCromlix Mudstone Formation of Strathmore Group
OverliesCrawton Volcanic Formation and other units
Thickness2400 - 3150m
Lithology
Primarysandstone
Othermudstone, siltstone, conglomerate
Location
RegionArgyll, Fife, Angus, Aberdeenshire
CountryScotland
Extentalong northern margin of Central Lowlands, south of Highland Boundary Fault from Kintyre to Aberdeenshire
Type section
Named forArbuthnott and Hill of Garvock near Laurencekirk, both in Aberdeenshire

Outcrops edit

These rocks are exposed in the west in southern Kintyre between Campbeltown and Southend and in an arcuate belt between Machrie and Sannox on the Isle of Arran. They occur in a southwest–northeast trending belt parallel to and just south of the Highland Boundary Fault between Helensburgh and Blairgowrie via Aberfoyle and Callander and as far as the southern edge of Stonehaven on the Scottish east coast. An extensive area in the east between Stonehaven and Dundee is underlain by these rocks including the Brechin, Forfar and Arbroath areas. A further belt of country between Forfar and Dunblane through Perth and extending into northern Fife is underlain by these rocks.[2]

Lithology and stratigraphy edit

The Group comprises numerous formations including the Catterline Conglomerate, Scone Sandstone, Craighall Conglomerate, Ruchil Flagstone and Craig of Monievreckie Conglomerate formations laid down during the Lochkovian to Pragian stages of the Devonian Period.[3]

References edit

  1. ^ http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=ATGK (BGS on-line lexicon of rock units)
  2. ^ http://mapapps.bgs.ac.uk/geologyofbritain/home.html? Geology of Britain viewer
  3. ^ British Geological Survey 1:50,000 scale geological map (Scotland) sheets

arbuthnott, garvock, group, arbuthnot, garvock, group, devonian, lithostratigraphic, group, sequence, rock, strata, central, scotland, name, derived, from, village, arbuthnott, aberdeenshire, hill, garvock, near, laurencekirk, group, comprises, previously, sep. The Arbuthnott Garvock Group or Arbuthnot Garvock Group is a Devonian lithostratigraphic group a sequence of rock strata in central Scotland The name is derived from the village of Arbuthnott in Aberdeenshire and the Hill of Garvock near Laurencekirk 1 The group comprises the previously separate overlying Garvock Group and the underlying Arbuthnott Group Arbuthnott Garvock GroupStratigraphic range Lochkovian Pragian Devonian TypeGroupUnit ofOld Red Sandstone SupergroupSub unitsCatterline Conglomerate Scone Sandstone Craighall Conglomerate Ruchil Flagstone and Craig of Monievreckie Conglomerate formationsUnderliesCromlix Mudstone Formation of Strathmore GroupOverliesCrawton Volcanic Formation and other unitsThickness2400 3150mLithologyPrimarysandstoneOthermudstone siltstone conglomerateLocationRegionArgyll Fife Angus AberdeenshireCountryScotlandExtentalong northern margin of Central Lowlands south of Highland Boundary Fault from Kintyre to AberdeenshireType sectionNamed forArbuthnott and Hill of Garvock near Laurencekirk both in AberdeenshireOutcrops editThese rocks are exposed in the west in southern Kintyre between Campbeltown and Southend and in an arcuate belt between Machrie and Sannox on the Isle of Arran They occur in a southwest northeast trending belt parallel to and just south of the Highland Boundary Fault between Helensburgh and Blairgowrie via Aberfoyle and Callander and as far as the southern edge of Stonehaven on the Scottish east coast An extensive area in the east between Stonehaven and Dundee is underlain by these rocks including the Brechin Forfar and Arbroath areas A further belt of country between Forfar and Dunblane through Perth and extending into northern Fife is underlain by these rocks 2 Lithology and stratigraphy editThe Group comprises numerous formations including the Catterline Conglomerate Scone Sandstone Craighall Conglomerate Ruchil Flagstone and Craig of Monievreckie Conglomerate formations laid down during the Lochkovian to Pragian stages of the Devonian Period 3 References edit http www bgs ac uk lexicon lexicon cfm pub ATGK BGS on line lexicon of rock units http mapapps bgs ac uk geologyofbritain home html Geology of Britain viewer British Geological Survey 1 50 000 scale geological map Scotland sheets Retrieved from https en wikipedia org w index php title Arbuthnott Garvock Group amp oldid 942445986, wikipedia, wiki, book, books, library,

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