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- W2051281016 abstract "Notwithstanding the fact that the rocks in and around North Berwick are exposed at the surface in an extensive series of fine natural sections, and also that the district has long been a favourite resort of geologists, there yet remains considerable uncertainty with regard to the position in the Lower Carboniferous Rocks of many of the minor subdivisions which are so admirably displayed in the coast section there. Practically the only point in the whole coast line, from Aberlady to Dunbar, whose geological position can be fixed with any degree of certainty, is represented by the limestones seen at the first-named locality. These certainly pertain to the lower part of the Yoredale Rocks, and are not, as many people still continue to believe, equivalent in time to any part of the Mountain Limestone, properly so called, of the North of England. In the neighbourhood of Edinburgh and in Fife these Yoredale Limestones overlie the Oil Shale Series, which has, in both localities, a thickness of several thousands of feet, and which, it may be added, is represented in Northumberland by the Scremerston Coal Measures. Beneath these comes the great series of estuarine and marine sandstones and shales, which are known in Northumberland as the Fell Sandstones, and around Edinburgh as the Granton Sandstone Series. These have an aggregate thickness of at least 2000 feet. In turn these overlie the Cement Stone Series, or the Ballagan Beds of the West of Scotland. These, again, are developed to a considerable thickness in" @default.
- W2051281016 created "2016-06-24" @default.
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- W2051281016 date "1897-01-01" @default.
- W2051281016 modified "2023-09-27" @default.
- W2051281016 title "Remarks upon a recent boring for water at North Berwick" @default.
- W2051281016 doi "https://doi.org/10.1144/transed.7.3.236" @default.
- W2051281016 hasPublicationYear "1897" @default.
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