On the Volcanoes And Volcanic Phenomena of the Hawaiian Islands

Cover On the Volcanoes And Volcanic Phenomena of the Hawaiian Islands
On the Volcanoes And Volcanic Phenomena of the Hawaiian Islands
James Dwight Dana
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ffitchcock, about 75 feet an hour.
In a communication to the Commercial Advertiser for Novem- ber 20th,* the formation of the aa or clinker fields is described as follows by Judge Hitchcock. '' The whole broad front of the then sluggish stream was a mass of solidified lava twelve to thirty feet m height, moving slowly along by breaking and bearing onward the crusted covering ; along the whole line of its advance it was one crash of rolling, sliding, tumbling, red-hot rock, no liquid rock being
...in sight ; there were no explosions, but a tremendous roaring, like ten thousand blast fumances all at work at once. The rough blocks lie piled together in the wildest confusion, many as large as ordinary houses. They [clinker-fields] form only when the movement is slow." 1882. — In this year (the month not stated) Capt. 0. E. But- ton made his visit to the summit (Report, page 139). He found ''no volcanic action whatever," "not even a wisp of steam issuing from any point ;" and he makes no mention of any cinder cone at the bottom.

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