Eruptive history of Sundoro volcano, Central Java, Indonesia since 34 ka

Prambada, Oktory; Arakawa, Yoji; Ikehata, Kei; Furukawa, Ryuta; Takada, Akira; Wibowo, Haryo Edi; Nakagawa, Mitsuhiro; Kartadinata, Mochamad Nugraha

doi:10.1007/s00445-016-1079-3

Cited by 13 publications

(8 citation statements)

References 18 publications

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“…The most recent noneruptive activity was in 2011. Prambada et al (2016) reconstructed the eruption history of the Sundoro Volcano by correlating PDC deposits, pyroclastic fall deposits, and lava based on stratigraphy, petrology, and the radiocarbon ages of 20 charcoal samples. That study resulted in clarification of the timing of eruptions from 34 ka to the present and allowed the eruptive activity to be divided into 12 groups.…”

Section: Sundoro Volcano Activitymentioning

confidence: 99%

Stratigraphy and Tectonics of the Sengkang Basin, South Sulawesi

Suyono

Kusnama

2010

Indonesian J. Geosci.

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This study applies the charcoalification measurement method to infer the emplacement temperature of pyroclastic flow deposits erupted from the Sundoro Volcano, Indonesia. This pyroclastic flow partially covered the Liyangan archeological site, a site where Hindu temples were constructed approximately 1,000 years ago. Five samples of charcoal collected from this area were analyzed for reflectance and elemental composition. Charcoalification temperatures were determined based on mean random optical reflectance values (Ro) plotted on published Ro-Temperature curves. Charcoalification temperatures were also estimated using a published formula based on the charcoal's hydrogen to carbon (H/C) ratio. These two methods for determining pyroclastic flow deposition temperatures indicated that the pyroclastic deposits that entombed the Liyangan archeological site ranged from 295° to 487°C when they were deposited. This study used very simple, rapid, precise, and low-cost methods of charcoalification temperature measurement to infer the emplacement temperature of a pyroclastic deposit. This estimation procedure could be applied widely to predict emplacement temperatures in volcanic area in Indonesia to enhance volcanic hazard mitigation.

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Section: Sundoro Volcano Activitymentioning

confidence: 99%

Stratigraphy and Tectonics of the Sengkang Basin, South Sulawesi

Suyono

Kusnama

2010

Indonesian J. Geosci.

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“…The morphology of G. Sundoro shows an ideal stratocone with an overlapping eruptive crater on its summit. Some parasitic cones of G. Sundoro are distributed on the southwestern to western flanks, such as Kembang, Kekep, Watu, Arum, and Kebonan (Prambada et al, 2016). Meanwhile, G. Sumbing morphology consists of four volcanic edifices, from the oldest to youngest Old Sumbing, Beser Cone, Gianti Cone, and Young Sumbing (Sukhyar, 1989).…”

Section: Regional Geologymentioning

confidence: 99%

“…Sukhyar et al (1992) defined the hummocky hills as a volcanic activity much older than G. Sumbing and G. Sundoro. Sitorus et al (1994) in the Geological Map of Sumbing Volcano mentioned that these hummocky hills deposits belong to Petarangan Debris Avalanche, while Prambada et al (2016) believe that they are the product of G. Sumbing.…”

Section: Introductionmentioning

confidence: 99%

Source Determination of Debris Avalanche Deposit based on the Morphology and Distribution of Hummocky Hills on the Northeastern Flank of G. Sundoro and G. Sumbing, Central Java, Indonesia

Rahayu,

Wibowo,

Moktikanana

et al. 2023

IJG

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The presence of hummocky hills as a typical product of debris avalanche deposits is prominently visible in the northeastern flank of G. Sundoro and G. Sumbing, Temanggung, Central Java. In an attempt to better understand the past behavior of both G. Sundoro and G. Sumbing, we identify the source of the debris avalanche deposit. Interpretation is performed on the basis of the assumption of two possible sector collapse sources, i.e., G. Sundoro and G. Sumbing. The Sumbing source scenario is assumed as freely spreading type considering 1) distribution of the hummocky hills are relatively on the northeastern flank of the volcano, and 2) the present crater structure on the summit of the volcano which is opening to the northeast. The Sundoro source scenario is assumed as valley-filling type considering the distribution of the hummocky hills are relatively on the eastern flank of Sundoro extended to the far distal area and bounded by older high topography of G. Sumbing and North Serayu Mountains. The source identification was done on the basis of field observation of the deposit lithological characteristics combined with image analysis, including hummocky hills morphometry, displacement angle, and spatial distribution. Image analysis identifies approximately 645 hummocky hills ranging from 1,851 mz to 623,828 mz and average of 23,482 m2. Petrographic analysis of 5 representative block lava samples shows variation of olivine basalt, pyroxene andesite, to hornblende andesite. The results show that big size hummocky hills dominate the western side, while small size on the east. Displacement angle varied following the valley orientation with typical downslope topography. These suggested that the hummocky hills were originated from G. Sundoro as a valley-filling debris avalanche deposit.

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“…Wright et al, 2010;Favalli et al, 2012;Wadge et al, 2012;Head et al, 2013. Hubbard et al, 2003;Rowan et al, 2003;Watanabe & Matsue, 2003;Byrnes et al, 2004: Torres et al, 2004Dmochowski, 2005;Capra, 2006;Mars & Rowan, 2005;Rowan et al, 2006;Coolbaugh et al, 2007;Davila et al, 2007;Hubbard et al, 2007;Kervyn et al, 2007;Carter et al, 2008;Kervyn et al, 2008c;Saepuloh et al, 2008;Schneider et al, 2008;Carter & Ramsey, 2009;Baliatan & Obille, 2009;Bogie et al, 2010;Brandmeier, 2010;Kobayashi et al, 2010a;Piscini et al, 2010;Chadwick et al, 2011;Davila-Hernandez et al, 2011;Wadge & Burt, 2011;Wantim et al, 2011;Diaz-Castellon et al, 2012;Graettinger et al, 2013;Lara et al, 2013;Watt et al, 2013;Boyce et al, 2014;Mars, 2014;Tayebi et al, 2014;Castruccia & Clavero, 2015;Selles et al, 2015;Folguera et al, 2016;Oikonomidis et al, 2016;Prambada et al, 2016;Suminar et...…”

Section: Geothermalunclassified

The Spatial and Spectral Resolution of ASTER Infrared Image Data: A Paradigm Shift in Volcanological Remote Sensing

Ramsey

Flynn

2020

Remote Sensing

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During the past two decades, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument on the Terra satellite has acquired nearly 320,000 scenes of the world’s volcanoes. This is ~10% of the data in the global ASTER archive. Many of these scenes captured volcanic activity at never before seen spatial and spectral scales, particularly in the thermal infrared (TIR) region. Despite this large archive of data, the temporal resolution of ASTER is simply not adequate to understand ongoing eruptions and assess the hazards to local populations in near real time. However, programs designed to integrate ASTER into a volcanic data sensor web have greatly improved the cadence of the data (in some cases, to as many as 3 scenes in 48 h). This frequency can inform our understanding of what is possible with future systems collecting similar data on the daily or hourly time scales. Here, we present the history of ASTER’s contributions to volcanology, highlighting unique aspects of the instrument and its data. The ASTER archive was mined to provide statistics including the number of observations with volcanic activity, its type, and the average cloud cover. These were noted for more than 2000 scenes over periods of 1, 5 and 20 years.

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Eruptive history of Sundoro volcano, Central Java, Indonesia since 34 ka

Cited by 13 publications

References 18 publications

Stratigraphy and Tectonics of the Sengkang Basin, South Sulawesi

Stratigraphy and Tectonics of the Sengkang Basin, South Sulawesi

Source Determination of Debris Avalanche Deposit based on the Morphology and Distribution of Hummocky Hills on the Northeastern Flank of G. Sundoro and G. Sumbing, Central Java, Indonesia

The Spatial and Spectral Resolution of ASTER Infrared Image Data: A Paradigm Shift in Volcanological Remote Sensing

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