Oyahué, is a massive andesitic
stratovolcano with a summit
dacitic lava dome. A large
Pleistocene debris-avalanche
deposit extending westward
from the Ollagüe volcano
separates the Salar de San
Martín from the Salar de
Ollagüe. Three youthful-looking
silicic lava flows mark late post-
collapse eruptions, but show
evidence of glaciation and are
thought to pre-date the last glacial advance at about 11,000 years ago. A
youthful-looking scoria cone on the lower WSW flank, La Poruñita, was initially
considered to be of Holocene age.however Wörner et al. Active sulfur mines
on the upper western and southern flanks of Ollagüe are reached by a road
that climbs to about 5500 m elevation. No historical eruptions have been
recorded from Ollagüe; activity has been restricted to periods of intense
fumarolic activity, and a persistent steam plume emanates from a fumarole on
the south side of the summit dome.
(Global Volcanic Program)
Summit Elevation: 5868 m
Latitude: 21.30°S
Longitude: 68.18°W
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