Servando De la Cruz-Reyna
William I. Rose Jr.
Susan Bagley
David L. Finnegan
William H. Zoller
Thomas J. Casadevall
1984
<p><span>Explosive eruptions of Volcán El Chichón in Chiapas, Mexico on March 28 and April 3–4, 1982 removed 0.2 km</span><sup>3</sup><span> of rock to form a 1-km-wide 300-m-deep summit crater. By late April 1982 a lake had begun to form on the crater floor, and by November 1982 it attained a maximum surface area of 1.4 × 10</span><sup>5</sup><span> m</span><sup>2</sup><span> and a volume of 5 × 10</span><sup>6</sup><span> m</span><sup>3</sup><span>. Accumulation of 4–5 m of rainfall between July and October 1982 largely formed the lake. In January 1983, temperatures of fumaroles on the crater floor and lower crater walls ranged from 98 to 115°C; by October 1983 the maximum temperature of fumarole emissions was 99°C. In January 1983 fumarole gas emissions were greater than 99 vol. % H</span><sub>2</sub><span>O with traces of CO</span><sub>2</sub><span>, SO</span><sub>2</sub><span>, and H</span><sub>2</sub><span>S. The water of the lake was a hot (</span><i>T</i><span> = 52–58°C), acidic (pH = 0.5), dilute solution (34,046 mg L</span><sup>−1</sup><span> dissolved solids; Cl/S = 20.5). Sediment from the lake contains the same silicate minerals as the rocks of the 1982 pyroclastic deposits, together with less than 1% of elemental sulfur. The composition and temperature of the lake water is attributed to: (1) solution of fumarole emissions; (2) reaction of lake water with hot rocks beneath the lake level; (3) sediments washed into the lake from the crater walls; (4) hydrothermal fluids leaching sediments and formational waters in sedimentary rocks of the basement; (5) evaporation; and (6) precipitation.</span></p>
application/pdf
10.1016/0377-0273(84)90061-1
en
Elsevier
Crater lake and post-eruption hydrothermal activity, El Chichón Volcano, Mexico
article