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Petrologic Monitoring of 1981 and 1982 Eruptive Products from Mount St. Helens
Katharine V. Cashman and Joseph E. Taggart
New Series, Vol. 221, No. 4618 (Sep. 30, 1983), pp. 1385-1387
Published by: American Association for the Advancement of Science
Stable URL: http://www.jstor.org/stable/1691847
Page Count: 3
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New material from the dacite lava dome of Mount St. Helens, collected soon after the start of each successive extrusion, is subjected to rapid chemical and petrologic analysis. The crystallinity of the dacite lava produced in 1981 and 1982 is 38 to 42 percent, about 10 percent higher than for products of the explosive 1980 eruptions. This increase in crystallinity accompanies a decrease in the ratio of hornblende to hornblende plus orthopyroxene, which suggests that the volatile-rich, crystal-poor material explosively erupted in 1980 came from the top of a zoned magma chamber and that a lower, volatile-poor and crystal-rich region is now being tapped. The major-element chemistry of the dacite lava has remained essentially constant (62 to 63 percent silica) since August 1980, ending a trend of decreasing silica seen in the products of the explosive eruptions of May through August 1980.
Science © 1983 American Association for the Advancement of Science