Endogenetic domes of obsidian – perlite rhyolitic lavas, limited in diameter and height, with few phenocrysts of plagioclase, hornblende, biotite, magmatic eroded quartz and magnetite.
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Endogenetic domes of obsidian – perlite rhyolitic lavas, limited in diameter and height, with few phenocrysts of plagioclase, hornblende, biotite, magmatic eroded quartz and magnetite.
