The crater lake and hydrothermal system of Mount Pinatubo, Philippines: evolution in the decade after eruption

@article{Stimac2001TheCL,
  title={The crater lake and hydrothermal system of Mount Pinatubo, Philippines: evolution in the decade after eruption},
  author={J. Stimac and F. Goff and D. Counce and A. C. L. Larocque and D. Hilton and U. Morgenstern},
  journal={Bulletin of Volcanology},
  year={2001},
  volume={66},
  pages={149-167}
}
The June 1991 eruption of Mount Pinatubo, Philippines breached a significant, pre-eruptive magmatic-hydrothermal system consisting of a hot (>300 °C) core at two-phase conditions and surrounding, cooler (<260 °C) liquid outflows to the N and S. The eruption created a large, closed crater that accumulated hydrothermal upwellings, near-surface aquifer and meteoric inflows. A shallow lake formed by early September 1991, and showed a long-term increase in level of ~1 m/month until an artificial… Expand
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