Volcanoes: What They Are And What They Teach
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Stratified tufEs. c. Dykes of r!hyolite, ■witt their edges passing into pitclastone, rf. Pumiceous agglomerate.
Fig. 53 represents a clifif-section in the island of Salina, one of the Liparis, exhibiting evidence that a Fig. 53. — Sea-cliff at II Capo, the nokth-east point of Salina, showing stratified agglomerates traversed by numerous UYKES, THE WHOLE BeInG UNCONFORMABLY OVERLAID BY STRATI- FIED AQUEOUS DEPOSITS.
PAET PLAYED BY DYKES IN CONE-BUILDING. 133 series of volcanic agglomerates trave...rsed by dykes of Andesite have been denuded and covered by a recent stratified deposit.
In the formation of these great composite cones, a minor but by no means insignificant part is played by the dykes, or lava-filled fissures, which are seen traversing the mass in all directions. That dyke- fissures often reach the surface of a volcanic cone, and that the material which injects them then issues as a lava-stream, is illustrated by fig. 54. The formation Fig. 54. — Section observed in the Val del Bove, Etna, showlng A basaltic dyke, from the upper part of which a lava- CUKKENT HAS FLOWED.
What to read after Volcanoes: What They Are And What They Teach?
You can find similar books in the "Read Also" column, or choose other free books by Judd, John W. (John Wesley), 1840-1916 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Stratified tufEs. c. Dykes of r!hyolite, ■witt their edges passing into pitclastone, rf. Pumiceous agglomerate.
Fig. 53 represents a clifif-section in the island of Salina, one of the Liparis, exhibiting evidence that a Fig. 53. — Sea-cliff at II Capo, the nokth-east point of Salina, showing stratified agglomerates traversed by numerous UYKES, THE WHOLE BeInG UNCONFORMABLY OVERLAID BY STRATI- FIED AQUEOUS DEPOSITS.
PAET PLAYED BY DYKES IN CONE-BUILDING. 133 series of volcanic agglomerates trave...rsed by dykes of Andesite have been denuded and covered by a recent stratified deposit.
In the formation of these great composite cones, a minor but by no means insignificant part is played by the dykes, or lava-filled fissures, which are seen traversing the mass in all directions. That dyke- fissures often reach the surface of a volcanic cone, and that the material which injects them then issues as a lava-stream, is illustrated by fig. 54. The formation Fig. 54. — Section observed in the Val del Bove, Etna, showlng A basaltic dyke, from the upper part of which a lava- CUKKENT HAS FLOWED.
What to read after Volcanoes: What They Are And What They Teach?
You can find similar books in the "Read Also" column, or choose other free books by Judd, John W. (John Wesley), 1840-1916 to read onlineMoreLess
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