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Clyde Sea Loch

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Journal Article
Published: 01 October 2008
Scottish Journal of Geology (2008) 44 (2): 183–190.
... deposits of the Firth of Clyde and its sea lochs . Report of the institute of Geological Sciences, 73/9 , HMSO , London . FORMAN , S.L. & POLYAK , L. 1997 . Radiocarbon content of pre-bomb marine mollusks and variations in the 14 C reservoir age for coastal areas of the Barents...
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Journal Article
Published: 01 September 1974
Journal of the Geological Society (1974) 130 (5): 475–478.
...MAXWELL R. DOBSON; DANIEL EVANS Abstract Geophysical surveys in the Malin Sea have revealed the presence of two asymmetric fault bounded basins, here termed the Loch Indaal basin and the Rathlin trough. They extend in a NE–SW direction between Northern Ireland and Western Scotland, and are thought...
Journal Article
Published: 01 February 2013
Geological Magazine (2013) 150 (4): 673–698.
... still further bolstered by the manner in which the N-trending faults continue through the Spango Gap to Greenock and thence across the Clyde estuary into the HBF zone SW of Loch Lomond (British Geological Survey, 1990 ; Fig. 8 ). The Old Red Sandstone and Carboniferous rocks of the Toward Point...
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Journal Article
Published: 01 November 2013
Scottish Journal of Geology (2013) 49 (2): 117–132.
... becoming yoked to the North Channel Basin of the Irish Sea ( British Geological Survey 1985 ). The Clyde Basin is floored mainly by the Permian and Triassic (New Red Sandstone) rocks that occupy most of the bedrock surface of the Firth, and the crude annulation of their submarine outcrops betrays the basin...
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Journal Article
Published: 01 November 1986
Journal of the Geological Society (1986) 143 (6): 927–934.
..., an anomaly partly attributed to organic matter in the water. Although biogenic suspended matter may originate in river waters, much is shown to be derived from micro-organisms in the lochs which abound in the basin. A direct relationship between the total surface area of the lochs and the sediment yield...
Journal Article
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 15–28.
... the Clyde Plateau Volcanic Formation. The magmatic pulses are synchronous with synrift phases in the Northumberland–Solway Basin. Volcanism continued in mid- to Late Carboniferous time contemporaneous with dextral strike-slip tectonics, in contrast to a post-rift tectonic setting in northern England. After...
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Journal Article
Published: 01 May 2001
Scottish Journal of Geology (2001) 37 (1): 3–10.
...John A. Howe; Julian Overnell; Mark E. Inall; Andrew D. Wilby Synopsis Loch Etive in Argyll on the west coast of Scotland, is a 30 km long, up to 145 m deep sea loch of glacial origin. A unique side-scan sonar image with new accompanying bathymetric data of the upper basin of the loch has been...
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Journal Article
Published: 01 May 2002
Scottish Journal of Geology (2002) 38 (1): 31–40.
... deposits in the Clyde area are apparently absent. Deposition of mud was locally >20 mm per year in the firths of Forth and Tay, and >7 mm per year in the Cromarty Firth. These figures are comparable to those obtaining both in offshore estuarine basins during the decline of sea-level from the highest...
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Journal Article
Published: 23 September 2015
Scottish Journal of Geology (2015) 51 (2): 165–176.
.... The Highland Boundary Fault, although a fairly straight and prominent feature to the NE, becomes displaced and difficult to follow in the area to the SW where it is accompanied by many splays trending roughly N–S. The area, in and around the Firth of Clyde, has been regarded as the product of a locked phase...
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Journal Article
Published: 01 May 2000
Journal of the Geological Society (2000) 157 (3): 635–640.
...‐temperature polytype dickite occurs in a region from the Firth of Clyde to Perthshire, in association with dyke swarms, whilst kaolinite occurs elsewhere. The original kaolinite precipitation was focused along the high permeability fault zone now marked by the Highland Boundary Fault Zone and its presumed...
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Journal Article
Published: 01 December 2001
Journal of Micropalaeontology (2001) 20 (2): 179–182.
... , various localities), Brady (1865 , Shetland), Heron-Allen & Earland (1916 , Scottish coastal areas), Edwards (1982 , North Minch Channel), Murray (1985 , shelf west of the Outer Hebrides to Fair Isle Channel) and Hannah & Rogerson (1997 , Clyde Sea). Of these, only Heron-Allen & Earland...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP344.21
EISBN: 9781862395923
... Holocene, followed by a warming of the climate and, latterly ( c . 2000 ka BP), increasing humidity. In the more recent past, human activities such as deforestation, fishing, aquaculture and industry have been recorded in the fjord sediments. Fjords, generally known in Scotland as sea lochs, form...
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Series: Engineering Geology Special Publications
Published: 09 June 2020
DOI: 10.1144/EGSP29.7
EISBN: 9781786204653
... or sea-level fall; negative values are relative land subsidence or sea-level rise. Figures in brackets are the trends that take into account modelled changes in tidal range during the Holocene. Fig. 7.9. Raised marine superficial deposits around the former Clyde Sea Loch, Glasgow, Scotland...
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Journal Article
Published: 14 August 2015
Scottish Journal of Geology (2015) 51 (2): 116–124.
... of the Clyde area . Geological Magazine , 4 , 305 – 315 . Underhill J.R. 2009 . Role of intrusion-induced salt mobility in controlling the formation of the enigmatic ‘Silverpit Crater’, UK Southern North Sea . Petroleum Geoscience , 15 , 197 – 216 , http://doi.org/10.1144/1354-079309-843...
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Journal Article
Published: 01 May 1986
Journal of the Geological Society (1986) 143 (3): 509–520.
...-east of Glasgow at levels which increase upstream from 60m to 180m OD. This variation in height reflects a succession of lake levels as the wasting Clyde valley glacier retreated north-westwards. Eventual failure of the glacier west of Glasgow allowed the sea access to the lower Clyde valley. Evidence...
Journal Article
Published: 01 November 2010
Scottish Journal of Geology (2010) 46 (2): 169–180.
... fluctuations in depth, sea floor conditions and water quality. An ‘embayment’ in the palaeoenvironment of the Index Limestone, seen by draping the interpretations over a 3D computer model of the subsurface, was associated with the Kerse Loch Fault, where penecontemporaneous displacement and an inferred...
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Journal Article
Published: 01 November 2000
Scottish Journal of Geology (2000) 36 (2): 105–109.
... Review . GCR Series No. 1, Joint Nature Conservation Committee, Peterborough. SNH/BGS 1993–1999 . Edinburgh, Skye, Cairngorms, Loch Lomond to Stirling, Orkney and Shetland, East Lothian and the Borders, Arran and the Clyde Islands and Scotland – the Creation of its Natural Landscape – A Landscape...
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Journal Article
Published: 28 June 2018
Scottish Journal of Geology (2018) 54 (2): 99–114.
... and Clyde Sea waters flowing northward along the coastline of western Scotland from the North Channel ( Inall et al. 2009 ). Of these, the strongest influence is from the SCC, being persistent all year round ( Inall et al. 2009 ). Tidal action is also very strong in the region, with M2 and M4 maximum...
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Journal Article
Published: 01 February 1987
Journal of the Geological Society (1987) 144 (1): 179–185.
..., Scotland Journal of Sedimentary Petrology 1984 54 373 93 Farrow G. Clokie J. Molluscan grazing of sublittoral algal bored shells and the production of carbonate mud in the Firth of Clyde, Scotland Transactions of the Royal Society of Edinburgh 1979 70 139 48 Ferentinos G...
Journal Article
Published: 01 August 2010
Mineralogical Magazine (2010) 74 (4): 601–622.
... of the Stevenston-Coylton dyke towards the Cleveland dyke: a small section is shown (blue, dotted) in the Midland Valley. C – Crawford; K – Kilbirnie; S – Scunthorpe; SML – St Mary's Loch; TL – Troston Loch. MacGregor ( 1930 , p. 293) suggested that the dyke which runs from Hawick to Acklington ( Fig. 1 b...
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