Volcanos
Volcanos
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In our eReader you can find the full English version of the book. Read Volcanos 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 Volcanos
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It is of precisely the same composition — tuff, interbedded with some very scoriaceous trachytic lavas ; and some of its curving bays indicate more than one crateri- form hollow, now so &r cut up by the erosion of the sea as to be with difficulty traceable.
Ischia, — A short way off, in the same south-west direction, the much larger island of Ischia rises in aU the dignity of a true volcanic mountain. The summit-heights of the island, called Monte Epomeo, attain 2600 feet above the sea. They ar...e peaked and precipitous, chiefly composed, as is the greater part of the island, of a trachytic tuff, of a greenish tint, from containing much augitic matter, and in parts apparently con- solidated by heat, and passing into earthy trachyte. On several points of the lower flanks of the mountain eruptions have taken place in recent times. Indeed its early history shows that the inhabitants were more than once destroyed or driven away by the violence of the earthquakes and eruptions to which it was then subject.
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You can find similar books in the "Read Also" column, or choose other free books by George Poulett Scrope to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
It is of precisely the same composition — tuff, interbedded with some very scoriaceous trachytic lavas ; and some of its curving bays indicate more than one crateri- form hollow, now so &r cut up by the erosion of the sea as to be with difficulty traceable.
Ischia, — A short way off, in the same south-west direction, the much larger island of Ischia rises in aU the dignity of a true volcanic mountain. The summit-heights of the island, called Monte Epomeo, attain 2600 feet above the sea. They ar...e peaked and precipitous, chiefly composed, as is the greater part of the island, of a trachytic tuff, of a greenish tint, from containing much augitic matter, and in parts apparently con- solidated by heat, and passing into earthy trachyte. On several points of the lower flanks of the mountain eruptions have taken place in recent times. Indeed its early history shows that the inhabitants were more than once destroyed or driven away by the violence of the earthquakes and eruptions to which it was then subject.
What to read after Volcanos?
You can find similar books in the "Read Also" column, or choose other free books by George Poulett Scrope to read onlineMoreLess
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