
On 14 July CVGHM reported that, since the Alert Level for Kaba was raised on 20 October 2009, seismicity had fluctuated but decreased overall. During September 2009-May 2011, when weather permitted, white plumes were seen rising 25-300 m above the crater rim, and during June-July 2011 diffuse white plumes rose 50 m above the crater rim. The Alert Level was lowered to 1 (on a scale of 1-4) on 12 July.
Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)
Increased seismicity and whitish vapor emissions
Deep volcanic earthquakes, seismic tremor, and five small explosions with corresponding ash emission were reported from Kaba in August 2000 (BGVN 25:11). Since then, Kaba has been quiet, but even in its normal state it almost always emits whitish plumes 25-100 m high.
On 20 October 2009, the Center of Volcanology and Geological Hazard Mitigation (CVGHM) reported that seismic activity from Kaba increased in August and remained elevated into September and October. Inflation was also detected. When weather permitted, diffuse white plumes were seen rising ~ 25-50 m above the summit crater complex and drifting E. Based on the deformation and increased seismicity, CVGHM raised the Alert Level to 2 (on a scale of 1-4).
From January through August 2009, the frequency of deep volcanic earthquakes averaged 85 events per month, but in August the number of events rose to 257 per month. During August-September, whitish plumes remained similar to September-October. In September seismicity fluctuated but tended to increase. Earthquakes and total tremors recorded at Kaba's monitoring post are shown in table 2.
Table 2. Summary of Kaba seismic data recorded during 12 September-20 October 2009. Courtesy of CVGHM.
| Dates (2009) | Deep volcanic earthquakes (Count, Characteristics) | Shallow volcanic earthquakes (Count, Characteristics) | Notes |
| Beginning on 12 September | 343 | 55 | -- |
| 1-17 October | 253. Max. amplitudes of 1-18 mm; S-wave minus P-wave arrival times ("S-P") of 0.2-3.5 s with signals lasting 4-35 s. | 271. Max. amplitudes 0.5-15 mm, durations of 2.5-11 s. | -- |
| 18 October | 68. Max. amplitude of 1-19 mm; S-P times of 0.2-3 s, and a duration of 3.5-47 s. | 67. Max. amplitudes 0.8-16 mm, durations of 2.5-13 s. | -- |
| 19 October | 50. Max. amplitudes of 0.5-18 mm; S-P 0.5-2 s, and a duration of 2-15 s. | 127. Max. amplitudes 0.5-15 mm, durations of 2.5-10 s. | Volcanic tremor registered during 0640-0900 local time; max. amplitudes 0.5-2 mm. |
| 20 October | 29. Max. amplitudes of 0.5-18 mm; S-P 0.5-2 seconds and a duration of 2-15 s. | 21. Max. amplitudes 0.5-15 mm, durations of 2.5-10 s. | Continuous tremor with amplitudes of 1-7 mm; the most prevalent amplitudes 1-3 mm. During clear weather, whitish plumes rose ~ 25 m. |
Deformation measurements taken using an EDM (electronic distance measurement) method were as follows: Biring station, shorter by 10 cm; Voelsang station, longer by 0.4 cm; and Kaba station, shorter by 2 cm.
Measurements of the crater water temperature on 15 October showed a reading of 72°C, with a pH of 3.24. The sulfurous and associated solfatara areas recorded a temperature of around 106-107°C. There was no other activity in the area of the crater.
Information Contacts: Center of Volcanology and Geological Hazard Mitigation (CVGHM), Jalan Diponegoro 57, Bandung 40122, Indonesia (URL: http://portal.vsi.esdm.go.id/joomla/).
On 14 July CVGHM reported that, since the Alert Level for Kaba was raised on 20 October 2009, seismicity had fluctuated but decreased overall. During September 2009-May 2011, when weather permitted, white plumes were seen rising 25-300 m above the crater rim, and during June-July 2011 diffuse white plumes rose 50 m above the crater rim. The Alert Level was lowered to 1 (on a scale of 1-4) on 12 July.
Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)
On 20 October, CVGHM reported that seismic activity from Kaba increased in August and remained elevated in September and October. Inflation was also detected. When weather permitted, diffuse white plumes were seen rising 25-50 m above the crater rim and drifting E. Based on the deformation and increased seismicity, CVGHN raised the Alert Level to 2 (on a scale of 1-4).
Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)
Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.
Only solfataric activity accompanies 17 December earthquake
Some press reports indicated that increased activity from Kaba and neighboring Bukit Daun volcanoes preceded a destructive 17 December earthquake. Adjat Sudradjat and Suparto Siswowidjoyo report that no unusual volcanic activity took place. Thick white solfataric vapor was emitted from two craters (Kaba Lama and Kaba Besar) on Kaba, which last erupted in 1956. Temperatures of solfataras and a crater lake at Kaba were measured on several occasions in the past nine years (table 1). Active fumaroles are present on Bukit Daun, but the volcano has not erupted in historic time.
Table 1. Temperatures of solfataras and a crater lake at Kaba, 1971, 1976, and 1978. Courtesy of VSI.
| Area | 1971 | 1976 | 1978 |
| Solfataras | 110°C | 156°C | 123°C |
| Crater Lake | 45°C | -- | 34°C |
Information Contacts: A. Sudradjat, VSI; Suparto S., Java and Sumatra Observatory, VSI.
Explosions and light gray ash
This report covers activity at Kaba documented by the Volcanological Survey of Indonesia (VSI) during August 2000. Deep volcanic earthquakes dominated seismicity during the second week of August. On 17 August seismographs recorded harmonic tremor with a maximum amplitude of 14 mm. Visual observations were hindered by clouds around the summit until the third week of the month. During 22-28 August, conditions were clear and a light gray ash plume rose 200 m above the summit. Five small explosion earthquakes were registered on 26-27 August, corresponding to the same number of observed ash emissions. By the end of August, the number of deep volcanic earthquakes decreased. Kaba remained at a hazard status of 2 (on a scale of 1-4) throughout the month.
Information Contacts: Dali Ahmad, Volcanological Survey of Indonesia (VSI), Jalan Diponegoro No. 57, Bandung 40122, Indonesia (Email: dali@vsi.esdm.go.id, URL: http://www.vsi.esdm.go.id/).
Increased seismicity and whitish vapor emissions
Deep volcanic earthquakes, seismic tremor, and five small explosions with corresponding ash emission were reported from Kaba in August 2000 (BGVN 25:11). Since then, Kaba has been quiet, but even in its normal state it almost always emits whitish plumes 25-100 m high.
On 20 October 2009, the Center of Volcanology and Geological Hazard Mitigation (CVGHM) reported that seismic activity from Kaba increased in August and remained elevated into September and October. Inflation was also detected. When weather permitted, diffuse white plumes were seen rising ~ 25-50 m above the summit crater complex and drifting E. Based on the deformation and increased seismicity, CVGHM raised the Alert Level to 2 (on a scale of 1-4).
From January through August 2009, the frequency of deep volcanic earthquakes averaged 85 events per month, but in August the number of events rose to 257 per month. During August-September, whitish plumes remained similar to September-October. In September seismicity fluctuated but tended to increase. Earthquakes and total tremors recorded at Kaba's monitoring post are shown in table 2.
Table 2. Summary of Kaba seismic data recorded during 12 September-20 October 2009. Courtesy of CVGHM.
| Dates (2009) | Deep volcanic earthquakes (Count, Characteristics) | Shallow volcanic earthquakes (Count, Characteristics) | Notes |
| Beginning on 12 September | 343 | 55 | -- |
| 1-17 October | 253. Max. amplitudes of 1-18 mm; S-wave minus P-wave arrival times ("S-P") of 0.2-3.5 s with signals lasting 4-35 s. | 271. Max. amplitudes 0.5-15 mm, durations of 2.5-11 s. | -- |
| 18 October | 68. Max. amplitude of 1-19 mm; S-P times of 0.2-3 s, and a duration of 3.5-47 s. | 67. Max. amplitudes 0.8-16 mm, durations of 2.5-13 s. | -- |
| 19 October | 50. Max. amplitudes of 0.5-18 mm; S-P 0.5-2 s, and a duration of 2-15 s. | 127. Max. amplitudes 0.5-15 mm, durations of 2.5-10 s. | Volcanic tremor registered during 0640-0900 local time; max. amplitudes 0.5-2 mm. |
| 20 October | 29. Max. amplitudes of 0.5-18 mm; S-P 0.5-2 seconds and a duration of 2-15 s. | 21. Max. amplitudes 0.5-15 mm, durations of 2.5-10 s. | Continuous tremor with amplitudes of 1-7 mm; the most prevalent amplitudes 1-3 mm. During clear weather, whitish plumes rose ~ 25 m. |
Deformation measurements taken using an EDM (electronic distance measurement) method were as follows: Biring station, shorter by 10 cm; Voelsang station, longer by 0.4 cm; and Kaba station, shorter by 2 cm.
Measurements of the crater water temperature on 15 October showed a reading of 72°C, with a pH of 3.24. The sulfurous and associated solfatara areas recorded a temperature of around 106-107°C. There was no other activity in the area of the crater.
Information Contacts: Center of Volcanology and Geological Hazard Mitigation (CVGHM), Jalan Diponegoro 57, Bandung 40122, Indonesia (URL: http://portal.vsi.esdm.go.id/joomla/).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
Synonyms |
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| Kaaba | ||||
Cones |
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| Feature Name | Feature Type | Elevation | Latitude | Longitude |
|
Hitam
Melintang, Bukit |
Stratovolcano | 1907 m | 3° 31' 39" S | 102° 36' 4" E |
| Kaba | Stratovolcano | 1926 m | 3° 30' 56" S | 102° 37' 16" E |
Craters |
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| Feature Name | Feature Type | Elevation | Latitude | Longitude |
|
Lama, Kawah
Kaba Besar Kawa Hidup |
Crater | 1715 m | 3° 30' 55" S | 102° 37' 34" E |
|
Mati, Kawa
Kaba Kecil Kaba Ketjil Kawah Baru |
Crater | 1695 m | 3° 30' 43" S | 102° 37' 56" E |
|
Vogelsang, Kaba
Pendapuran, Kaba Penjeluang, Kaba Penyeluang, Kaba Vogelenzang |
Crater | 1680 m | 3° 30' 38" S | 102° 38' 15" E |
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There is data available for 13 Holocene eruptive periods.
| Start Date | Stop Date | Eruption Certainty | VEI | Evidence | Activity Area or Unit |
|---|---|---|---|---|---|
| 2000 Aug 22 (?) | 2000 Aug 27 (?) | Confirmed | 1 | Historical Observations | |
| 1956 Mar 22 | 1956 Mar 28 | Confirmed | 2 | Historical Observations | |
| 1952 Apr 1 | 1952 Apr 28 | Confirmed | 2 | Historical Observations | |
| 1950 Mar 16 ± 15 days | 1951 Apr 16 ± 15 days | Confirmed | 1 | Historical Observations | Kaba Vogelsang |
| 1939 Nov 19 | 1941 Mar 14 | Confirmed | 2 | Historical Observations | Kaba Baru, Kaba Lama |
| [ 1918 Aug 9 ] | [ Unknown ] | Uncertain | 2 | ||
| 1907 | Unknown | Confirmed | 2 | Historical Observations | Kaba Baru |
| 1873 | 1892 Nov 1 ± 30 days | Confirmed | 2 | Historical Observations | Kaba Volgelsang and Kaba Baru |
| 1868 Oct | 1869 | Confirmed | 2 | Historical Observations | Kaba Baru ? and Kaba Vogelsang |
| 1853 Nov | Unknown | Confirmed | 2 | Historical Observations | |
| [ 1838 ] | [ Unknown ] | Uncertain | |||
| 1834 Nov | Unknown | Confirmed | 2 | Historical Observations | |
| 1833 Nov 24 | 1833 Nov 25 | Confirmed | 2 | Historical Observations |
There is no Deformation History data available for Kaba.
There is no Emissions History data available for Kaba.
There are no samples for Kaba in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
|
WOVOdat
Single Volcano View Temporal Evolution of Unrest Side by Side Volcanoes |
WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore. |
| Large Eruptions of Kaba | Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA). |
| MIROVA | Middle InfraRed Observation of Volcanic Activity (MIROVA) is a near real time volcanic hot-spot detection system based on the analysis of MODIS (Moderate Resolution Imaging Spectroradiometer) data. In particular, MIROVA uses the Middle InfraRed Radiation (MIR), measured over target volcanoes, in order to detect, locate and measure the heat radiation sourced from volcanic activity. |
| MODVOLC Thermal Alerts | Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. When one is found the date, time, location, and intensity are recorded. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales. |
| EarthChem | EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS). |