A Treatise On Geology volume 1
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In our eReader you can find the full English version of the book. Read A Treatise On Geology volume 1 Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book A Treatise On Geology volume 1
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Serpentine occurs at Portsoy, in lona, Lewis, and Zetland, in Connemara, &c. Very long and re- markable trap dykes run east and west through the mica 122 A TREATISE ON GEOLOGY. CHAP. VI.
schist and carboniferous limestones of Mayo and Sligo. Mineral veins are not so abundant in these rocks in Scotland, as in Saxony, Bohemia, &c. : it is generally near the granitic masses that they occur at all. The lead mine of Strontian is one of the most remarkable ; it may be looked upon as a metalliferous d...yke. Neither hot springs nor mineral waters are common in the British tracts of gneiss or mica schist.
General Inference. The preceding statements are sufficient to allow of our forming an incomplete notion of the origin and formation of the rocks contained in the gneiss and mica schist system. On a first view of the phenomena, granitic rocks of various composition appear to have been disintegrated, the separated minerals, quartz, felspar, mica, c. , agitated in a peculiar manner in water, re-aggregated in laminae, and partially collected into beds.
What to read after A Treatise On Geology volume 1?
You can find similar books in the "Read Also" column, or choose other free books by John Phillips to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Serpentine occurs at Portsoy, in lona, Lewis, and Zetland, in Connemara, &c. Very long and re- markable trap dykes run east and west through the mica 122 A TREATISE ON GEOLOGY. CHAP. VI.
schist and carboniferous limestones of Mayo and Sligo. Mineral veins are not so abundant in these rocks in Scotland, as in Saxony, Bohemia, &c. : it is generally near the granitic masses that they occur at all. The lead mine of Strontian is one of the most remarkable ; it may be looked upon as a metalliferous d...yke. Neither hot springs nor mineral waters are common in the British tracts of gneiss or mica schist.
General Inference. The preceding statements are sufficient to allow of our forming an incomplete notion of the origin and formation of the rocks contained in the gneiss and mica schist system. On a first view of the phenomena, granitic rocks of various composition appear to have been disintegrated, the separated minerals, quartz, felspar, mica, c. , agitated in a peculiar manner in water, re-aggregated in laminae, and partially collected into beds.
What to read after A Treatise On Geology volume 1?
You can find similar books in the "Read Also" column, or choose other free books by John Phillips to read onlineMoreLess
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