Pre Cambrian Rocks of Southeast Newfoundland
Pre Cambrian Rocks of Southeast Newfoundland
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The general run of the fragments FIG. 8. Coarse basalt breccia; west side of Blue Hills, south of Conception Bay would probably average a few inches in diameter. In general, the rhyolitic breccias and the basaltic breccias contain few foreign fragments, especially the coarser beds; yet beds in which angular fragments of rhyolite and basalt and crystals of orthoclase and plagioclase are mingled are frequent; and rhyolitic breccias and basaltic breccias are often found interbedded.
PRE-CAMBRIAN R...OCKS OF NEWFOUNDLAND 463 Crystal tuffs are of frequent occurrence interbedded with the breccias and tuffs. They are remarkable, in view of their great age and the vicissitudes which they have undergone, for the frequent presence of a perfectly preserved vitroclastic structure in their groundmass, whether rhyolitic or basaltic in nature. These devitrified glass shards are such a prominent feature of some of the tuffs from the vicinity of Red Rock Lake near Brigus that they JT IG g Microphotograph of vitroclastic groundmass of rhyolitic crystal tuff; near Red Rock Lake, south of Brigus, Conception Bay.
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To quickly assess the difficulty of the text, read a short excerpt:
The general run of the fragments FIG. 8. Coarse basalt breccia; west side of Blue Hills, south of Conception Bay would probably average a few inches in diameter. In general, the rhyolitic breccias and the basaltic breccias contain few foreign fragments, especially the coarser beds; yet beds in which angular fragments of rhyolite and basalt and crystals of orthoclase and plagioclase are mingled are frequent; and rhyolitic breccias and basaltic breccias are often found interbedded.
PRE-CAMBRIAN R...OCKS OF NEWFOUNDLAND 463 Crystal tuffs are of frequent occurrence interbedded with the breccias and tuffs. They are remarkable, in view of their great age and the vicissitudes which they have undergone, for the frequent presence of a perfectly preserved vitroclastic structure in their groundmass, whether rhyolitic or basaltic in nature. These devitrified glass shards are such a prominent feature of some of the tuffs from the vicinity of Red Rock Lake near Brigus that they JT IG g Microphotograph of vitroclastic groundmass of rhyolitic crystal tuff; near Red Rock Lake, south of Brigus, Conception Bay.
What to read after Pre Cambrian Rocks of Southeast Newfoundland?
You can find similar books in the "Read Also" column, or choose other free books by A F Arthur Francis Buddington to read onlineMoreLess
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