The Quarterly journal of the Geological Society of London . A-Harker Mu-Lt-ei-r^ Bros . lith. SRCTICNS OF METAMORPHOSED FLOCKS NKAFi THE SHAH :» THE seAP GRANITE AND ASSOCIATED KOCKS. 327 Fig. 4 [873]. Liine-aiigite-roek in the metamorphosed Upper Coniston Lime-stoue at the same locality ; showing coloiirlcss aiigite, both in crystal-line aggregates with good cleavage and in granules and granularpatches. 8ee pp. .}14-3ir). Fig. 5 [1218]. Si)ottcd schist in the metamorphosed Brathay Flags, north ofWasdale Beck, about 3oU yards from the granite ; showing little spotscomparatively
The Quarterly journal of the Geological Society of London . A-Harker Mu-Lt-ei-r^ Bros . lith. SRCTICNS OF METAMORPHOSED FLOCKS NKAFi THE SHAH :» THE seAP GRANITE AND ASSOCIATED KOCKS. 327 Fig. 4 [873]. Liine-aiigite-roek in the metamorphosed Upper Coniston Lime-stoue at the same locality ; showing coloiirlcss aiigite, both in crystal-line aggregates with good cleavage and in granules and granularpatches. 8ee pp. .}14-3ir). Fig. 5 [1218]. Si)ottcd schist in the metamorphosed Brathay Flags, north ofWasdale Beck, about 3oU yards from the granite ; showing little spotscomparatively free from the secondary brown mica. This figure isjuagnified UK) diameters. See p. 319. Fig. (> [1223J. Quartzite, with colourless lime-augite, in the metamorphosedLower Coldwell beds (grits) just north of Packhouse Hill, about 580yards from the granite. The pyroxene occurs in distinct roundedgranules and in finely granular patches. See p. 321. Discussion. Prof. BoNNEYsaid that it was almost impossible to discuss a paper ofsuch wide bearings, but it a
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
