Volcan Alcedo

A Profile of the Volcano

Tortoises in the Mist
Alcedo has the largest population of giant tortoises
in the Galapagos. The caldera is in in the background. Note the
domal morphology of the tortoise's shell and how it is similar
to the shape of the volcanoes.
Alcedo is in the middle of Isabela island, which is formed by
the coalescence of 6 shield volcanoes. Alcedo is probably the
most interesting petrologic feature in the Galapagos, because
it has erupted an entire suite of diverse rocks, including basalt,
icelandite, dacite, and rhyolite. A plinian, mixed magma deposit
covers much of the eastern flank of the volcano, and several obsidian
flows lie in the caldera and on the flank.
Here is a 5 m section of plinian airfall from the
main phase pumice eruption.
- Geist DJ, Howard KA, Jellinek AM, Rayder S (1994) The eruptive
history of Volcán Alcedo, Galápagos Archipeligo:
a case study of rhyolitic oceanic volcanism. Bull Volcanol 56:
243-260
- Geist, D, Howard, KA, and Larson, P (1995) The generation
of oceanic rhyolites by crystal fractionation: the basalt-rhyolite
association at Volcan Alcedo, Galapagos Archipelago. J Petrol
36, 965-982.
- Nordlie BE, Colony WE (1973) Fumarole with periodic water
fountaining, Volc_n Alcedo, Galapagos Islands. Geol Soc Am Bull
84: 1709-1720
- McBirney, AR, Cullen, AB, Geist, D, Vicenzi, EP, Duncan, RA,
Hall, ML, and Estrella, M (1985) The Galapagos volcano Alcedo:
a unique oceanic caldera, J Volcanol Geotherm Res 26, 173-177.
The Geologic Maps
of the volcano are awesome!
Check out the excellent analyses from
Alcedo - OR-
Download
an Excel file of geochemical data.
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