2009 Portland GSA Annual Meeting (18-21 October 2009)

Paper No. 17
Presentation Time: 9:00 AM-6:00 PM

UNUSUAL VOLCANIC PRODUCTS FROM THE 2008 ERUPTION AT VOLCAN LLAIMA, CHILE


SWEENEY, Dawn C.1, CALDER, Eliza1, CORTES, Joaquin1, VALENTINE, Greg1, WHELLEY, Patrick1, LARA, Luis L.2 and HUGHES, Meghan1, (1)Department of Geology, University at Buffalo, 411 Cooke Hall, Buffalo, NY 14260, (2)Servicio Nacional de Geología y Minería, Santa María 0104, Santiago, RM, Chile, dcs34@buffalo.edu

Volcan Llaima, a snow-covered basaltic andesite stratocone in southern Chile (38º 41' S, 71º 44' W, 3179 m a.s.l.), erupted on 1 January 2008 with a fire fountain display lasting 14 hours. Elevated activity continues to date with mild to moderate strombolian activity occurring from two nested scoria cones in the summit crater and with occasional lava flows from crater overflow. The eruption displayed contrasting styles of activity emanating from different parts of the edifice that may provide some unique insight into the upper level plumbing system. Furthermore, the activity has provided an excellent chance to study the transition of a normally passive degassing system into a violent eruptive cycle. A field study of the eruptive products from this eruption was completed in January 2009, where sampling was carried out from the tephra fall, lava flows, lahar deposits and even small pyroclastic flow deposits. The scoria samples collected suggest a mixture of two magmas involved in the initial violent, fire fountaining activity from the summit. Additionally, they exhibit a variety of unusual textures, including rapidly-quenched, dense lava 'balls', generated at the front of the lava flows traveling through ice, as well as cauliflower-textured tephra from explosive eruptions though ice. This presentation comprises our observations and preliminary interpretations concerning the processes that occurred during this unique eruption.