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- W1966276409 abstract "Abstract The sandstone occurring in the southern portion of the Vale of the Nith forms the north-west extremity of the great triassic formation which, commencing south of Appleby in Westmoreland, passes northward, having the mountain limestone for its eastern boundary, until it reaches Dumfriesshire. Its western boundary is also mountain limestone until it comes in contact with the eastern extremity of the West Cumberland coal-field, from whence it turns westward, skirting the edge of this formation, until it reaches the sea near to the entrance of the Solway Firth, under which it passes and again reappears in the southern portion of Dumfriesshire. The eastern/imit of the new red sandstone in Dumfriesshire is the parish of Canobie, where it is seen in the bed of the river Esk at Canobie Bridge. Its northern extremity in this parish is met with a little higher up the river at a place called Knottyholm, near to which the Canobie coal-field commences. The new red sandstone forms the southern portion of this parish ; from whence it ranges westward, and passing through the greater portion of the parish of Half Morton, is again seen and worked extensively in the adjoining parish of Kirkpatrick Fleming. The upper portion of this parish consists of mountain limestone, which forms the northern boundary of the sandstone, and this limestone extends for a considerable distance in a southwesterly direction, forming the northern extremity of the sandstone in the parishes of Annan and Cummertrees. The sandstone occupies the whole of the former parish except a small portion of its northern part, and in the latter it is confined to the southern end. Besides the parishes already mentioned, of which it constitutes a part, it occupies exclusively the parishes of Gretna and Dornock which lie upon the margin of the Solway Firth. The parish of Ruthwell, west of Cummertrees, and bordering the Firth, is composed principally of mountain limestone, and it is probable that near here the sandstone again passes raider the waters of the Solway before it reappears in Caerlaverock, west of Ruthwell ; and here commences that portion of the new red sandstone to which this account more immediately refers." @default.
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- W1966276409 date "1850-02-01" @default.
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- W1966276409 title "On the New Red Sandstone of the Southern Portion of the Vale of the Nith" @default.
- W1966276409 doi "https://doi.org/10.1144/gsl.jgs.1850.006.01-02.41" @default.
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