Smithsonian Institution
Global Volcanism Network Bulletin v. 20, no. 10, October 1995
Poas (Costa Rica)  High seismicity

Poas
Costa Rica
10.46N, 84.71W, summit elev. 2,708 m
All times are local (= GMT - 6 hours)

During October, tremor at Poas reached 101 hours; the last
time tremor rose over 12 hours/month was May-September 1994,
an interval when tremor ranged between 49 and 307
hours/month. The number of minor earthquakes, which were
predominantly of low frequency, continued to climb during
the month of October, reaching 9,838 events. This was a
value ~8% larger than the total for September, the previous
month with the most seismic activity in 1995 (see histogram,
Bulletin v. 20, no. 9).

The crater lake has risen consistently: by ~5 m during June-
October (ICE), and by ~30 cm in the last month (OVSICORI-
UNA). During October 1995, the fumarole on the W terrace
appeared to have decreased its emissions compared to recent
months (< 50-m-high steam plumes), and others on the lake~s
NW and SW sides also had diminished output. Fumaroles on the
S and SW crater wall produced steam columns reaching 100 m
tall. During October, bubbling in the lake still continued.
During October OVSICORI-UNA scientists measured the
temperatures at several sites: pyroclastic cone, 93 degrees
C; fumaroles on the S and SW sides of the crater, 95-97
degrees C; the lake in the inactive crater (Lake Botos), 15
degrees C; and the lake in the active crater, 30 degrees C.

Head scarps of landslides that emanate from the dome and
flow toward the lake displayed ongoing mass wasting; ICE
workers mentioned that this mass wasting may have been
triggered by recent heavy rains. In addition, ICE reported
that on 17 September (at 0548) a M 3.9 earthquake struck; it
had a depth of 5 km and an epicenter 1.6 km SW of the main
crater. At the summit, the earthquake~s intensity was MM
III-IV.

One of the most active volcanoes in Costa Rica, Poas is
located 35 km NW of San Jose. The summit area contains
several eroded calderas and two crater lakes, one clear and
the other, to the N, colored.

Information Contacts: OVSICORI-UNA (see Arenal); Mauricio
Mora, Escuela Centroamericana de Geologia, Universidad de
Costa Rica; G.J. Soto, ICE (see Arenal).