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- W2313357352 abstract "The Eel Burn flows into the sea about one and one-third miles west of the harbour of North Berwick. Immediately to the east of Eel Burn, and extending for a distance of 1100 feet (see Fig. 1) many large and irregular patches of rock are exposed on the shore. When the Ordnance Survey of North Berwick was made in 1856, and revised in 1903, these rocks were only represented, with the exception of the Black Murphies, by a few ragged lines on the map, indicating that the rocks were then almost hidden by the sand. It was necessary, therefore, to remap that part of the shore. These same rocks, however, must have been well exposed during the last Geological Survey, as special reference is made to them in the Memoir ( Geology of East Lothian, p. 82). All the rocks exposed in the area, extending about 2200 feet east of the Eel Burn, consist of basaltic lava of the Markle type, sometimes quite solid, and in other places more or less vesicular. Sediments overlie the lava in very considerable patches. These dip to the west as indicated on the map, and are mostly hard, and in many parts highly silicified, as is indeed mentioned in the Memoir referred to above.The basalt in the neighbourhood of the Eel Burn has been very much modified through metasomatic change by means of infiltration of silica and carbonates. This liability to metasomatic change is doubtless due, in the first place, to the original physical" @default.
- W2313357352 created "2016-06-24" @default.
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- W2313357352 date "1928-01-01" @default.
- W2313357352 modified "2023-09-25" @default.
- W2313357352 title "Metasomatism in basalt near Eel Burn, North Berwick" @default.
- W2313357352 doi "https://doi.org/10.1144/transed.12.1.117" @default.
- W2313357352 hasPublicationYear "1928" @default.
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