FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1566187224> ?p ?o ?g. }

• W1566187224 abstract "The mapped area of Cumbria represented on Sheets SD 68 NW and NE includes the settlements of Killington, Middleton and Gawthrop. Larger settlements border the area: Sedbergh 2 km to the north, Dent 0.5 km to the east and Barbon 2.5 km to the south. The area is bounded to the east by the Dent Fault, and is completely traversed by two other major faults, the Barbon Fault and the Firbank Fault. These faults divide the solid geology into three major sectors and one minor sector, the stratigraphical continuity of which can only be inferred outside the area.The oldest rocks at outcrop occur as a small sliver along the Dent Fault, comprising Dent Group calcareous mudstones and volcanic rocks and Tranearth Group laminated mudstones; the two groups are also separated by a fault. The major outcrop sector between the Dent and Barbon fault zones comprises turbidite sandstones and subordinate mudstones of the uppermost Coniston Group and a lower division of the Bannisdale Formation, passing up into a mudstone-rich upper Bannisdale Formation. The distinction between the Coniston and lower Bannisdale units is difficult, and based mainly on the lamination characteristics of the their hemipelagic mudstone.The outcrop between the Barbon and Firbank faults comprises mudstones with thin sandstones assigned to the upper part of the Bannisdale Formation. This lithology is also present at the base of the succession west of the Firbank Fault, though most of the outcrop here comprises the overlying sandstone-rich Kirkby Moor Formation. Reddening of the upper parts of this formation also affects part of the upper Bannisdale Formation across the Firbank Fault: the reddening is therefore interpreted as secondary, and not diagnostic of a ‘Scout Hill Formation”.The Lower Palaeozoic rocks are deformed by a weak Acadian cleavage striking generally ESE, and by open kilometric-scale folds. These structures are cut by the major north-south Variscan faults.Till occurs in upland valleys and in the major valleys of the Lune and Dee, where it is moulded into drumlins. The River Lune has extensive spreads of post-glacial alluvium." @default.
• W1566187224 created "2016-06-24" @default.
• W1566187224 creator A5034232928 @default.
• W1566187224 creator A5056136156 @default.
• W1566187224 date "2006-01-01" @default.
• W1566187224 modified "2023-09-27" @default.
• W1566187224 title "Geological notes and local details for 1:10 000 scale Sheet SD 68 NW (Middleton) and part of Sheet SD 68 NE (Gawthorp)" @default.
• W1566187224 cites W1496511960 @default.
• W1566187224 cites W1970060948 @default.
• W1566187224 cites W1972689231 @default.
• W1566187224 cites W1978638710 @default.
• W1566187224 cites W1980002621 @default.
• W1566187224 cites W1980803189 @default.
• W1566187224 cites W1981362466 @default.
• W1566187224 cites W1988316493 @default.
• W1566187224 cites W1995837230 @default.
• W1566187224 cites W2002247269 @default.
• W1566187224 cites W2015427230 @default.
• W1566187224 cites W2020651766 @default.
• W1566187224 cites W2028908132 @default.
• W1566187224 cites W2044976489 @default.
• W1566187224 cites W2045566522 @default.
• W1566187224 cites W2054172914 @default.
• W1566187224 cites W2060383733 @default.
• W1566187224 cites W2062235206 @default.
• W1566187224 cites W2069543243 @default.
• W1566187224 cites W2069792044 @default.
• W1566187224 cites W2075452266 @default.
• W1566187224 cites W2088577797 @default.
• W1566187224 cites W2091976778 @default.
• W1566187224 cites W2094989242 @default.
• W1566187224 cites W2095216120 @default.
• W1566187224 cites W2099138586 @default.
• W1566187224 cites W2099363443 @default.
• W1566187224 cites W2100110977 @default.
• W1566187224 cites W2101316946 @default.
• W1566187224 cites W2104867885 @default.
• W1566187224 cites W2110056522 @default.
• W1566187224 cites W2115113119 @default.
• W1566187224 cites W2115671741 @default.
• W1566187224 cites W2116184951 @default.
• W1566187224 cites W2116863437 @default.
• W1566187224 cites W2116926688 @default.
• W1566187224 cites W2118014644 @default.
• W1566187224 cites W2119755187 @default.
• W1566187224 cites W2123109140 @default.
• W1566187224 cites W2132279339 @default.
• W1566187224 cites W2140590419 @default.
• W1566187224 cites W2143718374 @default.
• W1566187224 cites W2147986211 @default.
• W1566187224 cites W2148321239 @default.
• W1566187224 cites W2153428905 @default.
• W1566187224 cites W2153619194 @default.
• W1566187224 cites W2164544947 @default.
• W1566187224 cites W2170702800 @default.
• W1566187224 cites W2170804303 @default.
• W1566187224 cites W2170845550 @default.
• W1566187224 cites W2171243662 @default.
• W1566187224 cites W2300173779 @default.
• W1566187224 cites W2947325100 @default.
• W1566187224 cites W2972825379 @default.
• W1566187224 cites W587044336 @default.
• W1566187224 cites W593754389 @default.
• W1566187224 cites W611599641 @default.
• W1566187224 cites W751945933 @default.
• W1566187224 hasPublicationYear "2006" @default.
• W1566187224 type Work @default.
• W1566187224 sameAs 1566187224 @default.
• W1566187224 citedByCount "0" @default.
• W1566187224 crossrefType "journal-article" @default.
• W1566187224 hasAuthorship W1566187224A5034232928 @default.
• W1566187224 hasAuthorship W1566187224A5056136156 @default.
• W1566187224 hasConcept C106804226 @default.
• W1566187224 hasConcept C114793014 @default.
• W1566187224 hasConcept C122792734 @default.
• W1566187224 hasConcept C127313418 @default.
• W1566187224 hasConcept C151730666 @default.
• W1566187224 hasConcept C169212394 @default.
• W1566187224 hasConcept C17409809 @default.
• W1566187224 hasConcept C175551986 @default.
• W1566187224 hasConcept C178790620 @default.
• W1566187224 hasConcept C185592680 @default.
• W1566187224 hasConcept C2781311116 @default.
• W1566187224 hasConcept C5900021 @default.
• W1566187224 hasConcept C6494504 @default.
• W1566187224 hasConcept C82586738 @default.
• W1566187224 hasConceptScore W1566187224C106804226 @default.
• W1566187224 hasConceptScore W1566187224C114793014 @default.
• W1566187224 hasConceptScore W1566187224C122792734 @default.
• W1566187224 hasConceptScore W1566187224C127313418 @default.
• W1566187224 hasConceptScore W1566187224C151730666 @default.
• W1566187224 hasConceptScore W1566187224C169212394 @default.
• W1566187224 hasConceptScore W1566187224C17409809 @default.
• W1566187224 hasConceptScore W1566187224C175551986 @default.
• W1566187224 hasConceptScore W1566187224C178790620 @default.
• W1566187224 hasConceptScore W1566187224C185592680 @default.
• W1566187224 hasConceptScore W1566187224C2781311116 @default.
• W1566187224 hasConceptScore W1566187224C5900021 @default.
• W1566187224 hasConceptScore W1566187224C6494504 @default.
• W1566187224 hasConceptScore W1566187224C82586738 @default.

• next