From: Benjamin Van Wyk De VriesDate: Fri, 1 Dec 1995 09:48:51 MST Subject: Cerro Negro activity report Cerro Negro Saturday -Sunday 25/26th November I apologise for the delay in sending this information, which was caused by computer failure. The data has already been reported in Nicaragua. B. van Wyk de Vries.
The eruption plume of Cerro Negro was clearly visible, as on earlier days, from Managua. It was a diffuse grey column, turning horizontal at about 2000m, where white clouds formed and drifted westwards over the Pacific coast. From La Paz Centro at 09:00 hrs distinct pulses of ash could be seen rising from the crater. These were dark grey, on exit from the crater, forming mushroom shapes, before drifting westwards and being incorporated into the plume. When passing below the plume near Leon, at 09:30 hrs no ashfall was encountered.
Ash fall has been reported in Leon and Corinto, however, and subsequent observations showed that there is great variation in the amount of fine material ejected. A times only massive bombs are thrown out, while at others strong explosions sent up dense ash clouds. Ash and scoria are falling continuously on the west base of the cone, with occasional periods of heavy fall, with <5 cm-size highly vesicular scoria. Heavy ash emission lasted from single pulses to several hours.
From Rota (the most popular tourist entrance to the volcano) the new cone was clearly visible at 10:00 hrs and an unusual spinelike protrusion was jutting out on the northern edge of the crater. (This was later found to be a lava dome).
Pulses of ash and bombs had a frequency of 20 per minute, a characteristic periodicity in this eruption. Pulses were strong enough to maintain a constant fountain of bombs, some of which were large and visibly red at 5km. Bombs rose to a maximum of 600 m. Explosions were audible at this distance.
The lava flow which was observed forming between Cerro La Mula and Cerro Negro
on 23rd November had advanced westwards about 500m down a small valley and was
moving at about 1m per hour between 10:30 and 20:00 hrs 25/11. We have called
this La Mula flow. The flow was about 30m wide. By 06:00 26/11 the flow had
stopped advancing, red glow was still visible in cracks. A tree at the front
was not burnt and remained intact at the last observation at 12:00 26/11.
Occasional creaks and falling rocks still occurred.
At 11:00 hrs little ash was emitted. Pulses continued to throw bombs in a near
continuous fountain. Some bombs were metres across and deformed and broke up in
flight. Most were still ejected vertically, but a significant number were now
exiting at low angles and falling low on the flanks. Sharp whooshing sounds
occurred with some pulses accompanied with burning gas.
The new cone had grown considerably, and was about 30-50 m below the old crater
summit. The crater was about 40m across. Bombs fell mostly on the cone and
rolled down to the base. The small breach where the lava flow of 23/11 exited
was partly covered by a new blocky flow, which appeared to come straight
from the new cone, though no exit vent was visible. (I believe it was produced
by accumulated, still liquid ejecta beginning to flow outwards, as seen on
22/11). The flow had advanced to half way down the flank and was covering
another blocky lava, which had reached the base.
To the east of the lava exit a dome about 100m wide and 40m high had grown.
This initially had a serrated, spined, pyramidal shape, but changed rapidly
throughout the day. By 18:00 hrs it had become table shaped. Blocks were
continually spalling off the dome, which also sustained a continuous rain of
bombs from the new cone. Three small but thick lava tongues extended to the
base of the cone from the dome, and were advancing slowly. A small, thinner
lava tongue was following the east side of the thick lavas.
The two flows seen moving northwards on the 23rd had reached about 1 to 1.5 km
from the volcano. The western lobe was the largest, being about 400m wide and
3-5 m thick at the front. It had a small lobe extending down the gully below
Cerro La Mula and another extending eastwards into a depression in the old
northern lava field. Forward movement was visible in red plastic lava exposed
at the front and over a three hour period the flow advanced about 12m.
The eastern lobe has extended into forest at the east side of the old northern
lava field and was moving at about the same rate at the other lobe. A low ash
covered area with a small cinder cone separated the two lobes. The sides of
each flow were slowly (about 1m per hour) encroaching on this and thickening.
>From the cinder cone all the thick lava lobes below the dome could be seen
advancing. Many areas of the dome were glowing red.
More information and diagrams/ photographs will be made available on the WWW soon and a comprehensive report is being prepared for the Global Volcanism Program. Any enquiries about this report should be addressed to B. van Wyk de Vries at, The Open University, Milton Keynes, UK. Tel +44 1908 652558, Fax +44 1908 655151, email b.van-wyk-de-vries@open.ac.uk Or to Wilfried Strauch at INETER, Managua Tel +505 2 492761 Fax +505 2 496987 email wil@ineter.nic