SUMMARYType: shield with caldera |
GEOLOGIC HISTORYThe Galapagos Islands lie on the Nezca plate just south of the Galapagos Ridge spreading center. They are also thought to overlie a mantle hotspot, presently beneath the volcanicly active western Galapagos Islands. Marchena is a low, 12 x 16 km island, with a central caldera 6 km in diameter that has been nearly filled with young basalt flows. Historic Activity: No historic eruptions had been recorded from the volcano, but several fumaroles were active and many flows appeared to be quite young. Recent Activity: An eruption started on Sept. 25, 1991, first observed from a ship. Lava flows reached the ocean and covered much of the caldera's SW floor, suggesting that a circumferential fissure several kilometers long had been active on the W to SW rim, supplying lava to both the caldera floor and the outer flank. Lava was still entering ocean on Nov. 8, 1991. Data Sources
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Last Update: 2/13/00 |