Volcanoes: What They are and what They TeachC. K. Paul, 1881 - 381 Seiten |
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Seite xiv
... flowed . • 128 130 130 131 131 132 132 · · 133 134 55. Basaltic dykes projecting from masses of stratified scoriæ in the sides of the Val del Bove , Etna 56. Sheets of igneous rock ( basalt ) intruded between beds of sandstone , clay ...
... flowed . • 128 130 130 131 131 132 132 · · 133 134 55. Basaltic dykes projecting from masses of stratified scoriæ in the sides of the Val del Bove , Etna 56. Sheets of igneous rock ( basalt ) intruded between beds of sandstone , clay ...
Seite 26
... flowed to a considerable distance beyond its base . The largest of these lava - floods over- whelmed and destroyed the two villages of Massa di Somma and San Sebastiano , besides many country houses in the neighbourhood . A very marked ...
... flowed to a considerable distance beyond its base . The largest of these lava - floods over- whelmed and destroyed the two villages of Massa di Somma and San Sebastiano , besides many country houses in the neighbourhood . A very marked ...
Seite 95
... flowed slowly down a steep slope and heaped itself up at the bottom , as its fluidity was not complete enough to enable it to move on a slighter incline . An examination of the interior of such imperfectly fluid lavas affords fresh ...
... flowed slowly down a steep slope and heaped itself up at the bottom , as its fluidity was not complete enough to enable it to move on a slighter incline . An examination of the interior of such imperfectly fluid lavas affords fresh ...
Seite 97
... flowed to the distance of several miles from the base of the moun- tain in a very short time . But other Vesuvian lavas have been in such a viscid condition that their rate of movement has been so extremely slow as to be almost ...
... flowed to the distance of several miles from the base of the moun- tain in a very short time . But other Vesuvian lavas have been in such a viscid condition that their rate of movement has been so extremely slow as to be almost ...
Seite 99
... flowed from Vesuvius in 1872 is illus- trated in the photograph copied in fig . 5 ( facing page 24 ) , in which the three lava - currents are each seen to be surmounted by enormous vapour - clouds rising to the height of several ...
... flowed from Vesuvius in 1872 is illus- trated in the photograph copied in fig . 5 ( facing page 24 ) , in which the three lava - currents are each seen to be surmounted by enormous vapour - clouds rising to the height of several ...
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Häufige Begriffe und Wortgruppen
active volcanoes andesites appear atmosphere augite Auvergne basaltic basic lavas canic carbonic acid cavities centre character Cheaper Edition chemical Cloth composed composition condition crater crater-rings crystalline crystals Demy 8vo denuding forces depth dykes earth's crust earth's surface enormous eruption Etna exhibit exist fact Fcap feet formation formed fragments Frontispiece gases geological periods geologists glassy globe granitic igneous Illustrations incandescent interior Island lapilli Large post 8vo lava-currents lava-streams line of fissure Lipari liquid mass melaphyres metallic meteorites microliths miles minerals Monte Nuovo ocean origin parasitic cones Poems portions present pressure price 35 produced pumice quantities rhyolites rock-masses scoria-cones scoriæ Second Edition seen sides silica slope Small crown 8vo solid steam Stromboli structure substances subterranean summit take place temperature Third Edition tion trachytic tuffs vapour vast Vesuvius volcanic action volcanic cones volcanic districts volcanic forces volcanic mountains volcanic outbursts volcanic phenomena volcanic vents vols
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