Short reports

Ascent of Mount Tambora in August 2015 on Zollinger’s way – 200 years after the big eruption


Ascent through the dry savanna,view to the north on the Doro Tabeh Naë

Ascent through the dry savanna, view to the east

The aim of this year’s new expedition to the Tambora was the ascent from the east coast of the Sanggar peninsula over the east flank to the eastern rim of the caldera. The team of Georesearch Volcanedo (GRV) followed the way used by Zollinger as the first climber in 1847 after the big eruption and explored this way for the first time since 1847; because of the length of the distance to be travelled on foot, the partly very high temperatures and the lack of water it’s a particular challenge! As besides there were no exact geographic coordinates of the ascent, only the descriptions and the historical hand-drawn map of Heinrich Zollinger could be used to find the way. Starting on the east coast of the Sanggar peninsula up to the eastern rim of the caldera Zollinger’s stages could be realized very well. It was very interesting to examine the similarities, but also the changes in the landscape in comparison with Zollinger’s report. As our native helper team and we did not follow a common way, there were a lot of difficulties because of the area, about which Zollinger reported as well. In the end Zollinger as well as we could overcome these difficulties.

We would like to appreciate Zollinger’s achievement!

A current comparison with Zollinger’s description is in work.

Only a few steep meters to the eastern rim (2346 m)!
7 August 2015, Georesearch Volcanedo Germany

Tambora caldera July/August 2014

12 days of research in the Tambora caldera – a new record!

In July/August 2014 the research in the Tambora caldera was continued and deepened. The results will be published at a later date in other media.
The descent to the caldera floor was again carried out on the very difficult and dangerous inner southern flank. Besides, there were more earthquakes which caused significantly more landslides.


In the fore-ground one of the installed measuring stations on the caldera floor

Gases escaping under high pressure near the northern wall

Note:
The by the team of GRV and his native helpers tested and explored descent on the southern flank to the caldera floor between 2012 to 2014 was used again after our descent in August 2014 by a few people. Currently the way seems to be the only possible descent on the southern flank. Another descent at the southern flanc that should have been used once in the past can not longer be used due to landslides of the caldera wall. Nevertheless, because of the dangers mentioned in our short reports, we would like to warn expressly to descend without appropriate equipment and without competent guides which know the terrain.

Tambora caldera (Indonesia) October 2013


The Tambora caldera (Oct. 2013)

Descent on the inner southern flank

Volcano research under extreme conditions in the Tambora Caldera (Indonesia), short report on an expedition into one of the deepest calderas in the world

The eruption of Tambora (located on Sumbawa) in April 1815 was the largest volcanic event since the beginning of recorded history and has become well known due to the global climate changes.

The aim of our expedition was the large caldera of the Tambora formed in 1815. This about 1300m deep giant volcanic hole is considered as the deepest caldera in the world since one after christ. In 2012 we had already carried out a preliminary expedition to the southern inner flank of this volcano.

In October 2013 we succeeded under the leadership of Arne C. as the first German research team (GRV) in penetrating to the floor of the caldera where an ecosystem has developped largely uninfluenced by anthropogenic factors. The descent took place on the geologically very interesting inner southern flank from 2430m to 1340m altitude.
To the team also belonged the geoscientist Anke D.-R. who was the first European woman and worldwide the first woman conquering the almost impassable inner southern flank of this volcano.
So far only in a few cases people had reached the caldera floor because the terrain is difficult and extremely steep walls must be overcome. Moreover, these people could only stay on the caldera floor for a short time due to the enormous logistical problems. Therefore extensive scientific studies were almost impossible.

The descent into this fascinating caldera of this active stratovolcano was carried out with the help of a native team, elaborate logistics and the use of climbing techniques.
During the stay on the caldera floor cartographical work was performed (including the visible effects of the smaller eruptions which had taken place on the caldera floor since 1815), rock and water samples were collected, gas emissions were measured (gas and temperature measurements) and the flora and fauna of this ecosystem were examined. A weather station built on the caldera floor continuously recorded the weather data during our stay.
Beside numerous interesting studies the relatively high activity of Doro Api Toi (strong fumarole activity, high temperatures) and the gases escaping under high pressure on the lower north-east wall were particularly striking. The Doro Api Toi is a small volcanic cone formed in the southern part of the caldera floor about 1880.
Despite various hazards (landslides, debris flows, gas emissions) and difficult working conditions such as extremely high temperatures the team was able to achieve fundamental results for further research and to create a comprehensive illustrative documentation.
The stay within the Tambora caldera including the research of the caldera floor lastened nine days and is until now unique.


View from the caldera floor on the north wall

Preparation of gas measurements on the caldera floor on the south wall

Violent eruptive phase of Anak Krakatau on 2 and 3 Sept 2012


Anak Krakatau, 3.9.2012

Excerpts from the seismic records of this event (Krakatau observatory)

On 3 September 2012 we were able to observe at close range the violent explosive eruptions of Anak Krakatau. These were the strongest eruptions of Anak Krakatau which had been observed since 1996 (see Monthly Reports of the Smithsonian Institution). We had witnessed several eruptions of Anak Krakatau in the last years, but that eruption in early September exceeded all of what we had observed up to then. Between 10 am and 4 pm explosions like a gunfire took place without interruption.The eruption column partially reached a height of about two kilometers. The scenery was all the more impressive because lava flows entering the water led to a strong formation of steam and also to phreatomagmatic explosions with ash formation.

The information on this event spread in the Indonesian media were by the way sometimes not precise. Thus, the severity of the eruption may have been downplayed so as not to alarm the population on the west coast of Java who had been afraid because of the thunderclap-like noise and ground vibrations emanating from Anak Krakatau in the night of 2 to 3 September. We also felt significant vibrations in the soil at Carita during that night.

Even in the late afternoon of 3 September, we were the first science team stepping on Anak Krakatau during this eruptive phase with our companion Aris and other helpers. At that moment the volcano had reached a rather strombolian activity.

Until 6 September we made investigations on the volcanic island of Anak Krakatau. The 4 September we visited the summit region and the origin of the lava flow entering the water in the southeast. The volcano had become quiet now, so we dared to climb up. The climb sometimes turned out to be a little bit hard because of the fresh volcanic ash.

On 5 September at 11am a strong degassing began (we measured high SO2 and H2 values). This degassing continued until our departure on the morning of 6 September.

More detailed results of that “volcanic highlight” of the year 2012 will be published in another place at a later date.


Anak Krakatau, 3.9.2012

At the new lava flow on Anak Krakatau on 4 September (at 5.50 in the morning). The new lava flow has a total length of approximately 600m, it extends into the water about 100m. The “Child of Krakatoa” has thus grown in width!

All the photos and texts are the property of Georesearch Volcanedo.