Fayalite in the obsidian of Lipari

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ID: 301939
1890
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Abstract
THE Lipari islands have long been celebrated for their acid lavas and pumices; and it was for the purpose of beooming acquainted with their c!'aters and flows of these rocks that one of the writers recently visited this far famed locality.The obsidian flows that terminated the volcanic activit.Y which built up the craters of snow-white pumice stretch their glassy streams down the steep mountain slopes into the sea.Their upper surface presents a rough and forbidding tract of sharp angular blocks, which appear to have suffered very little change since the solidification of the lava.This portion of the obsidian is filled with small gas bubbles that give it a gray color, and a more or less banded and laminated strncture.
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openalex_W2328361104 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. P. Iddings, S. L. Penfield
Journal american journal of science
Year 1890
DOI
10.2475/ajs.s3-40.235.75
URL
https://doi.org/10.2475/ajs.s3-40.235.75
Keywords Keywords not found

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