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- W4230493893 abstract "This lies to the south of Unst ; it is interesting as forming the connecting link which unites the rock masses of Fetlar with those of Unst. Its western extremity is composed of diallagic rocks, containing crystals of that mineral (Hb) very inferior to those of Balta : its middle portion consists of various rocks of the chloritic series ; towards the east there is seen a bed of graphitic slate (H) quite similar to, and doubtless the continuation of one which appears near Trista V oe in Fetlar." @default.
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- W4230493893 date "1878-09-01" @default.
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- W4230493893 title "XIII. The Geognosy and Mineralogy of Scotland" @default.
- W4230493893 doi "https://doi.org/10.1180/minmag.1878.002.10.03" @default.
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