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Academic literature on the topic 'Volcanoes – Indonesia'
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Journal articles on the topic "Volcanoes – Indonesia"
1
Wibisono, Aryo Bayu, Bayu Suryo Ridho Saputro, and Puspita Sari Sukardhani. "Infographic Design As An Effective Communication Model For Volcano Eruption Disaster's Socialization." JURNAL ILMU KOMUNIKASI, no. 2 (December 7, 2018): 11–17. http://dx.doi.org/10.33005/jkom.v0i2.19.
Full textAbstract:
Indonesia is an archipelago surrounded by cluster of volcanoes known as the ring of fire. Indonesian volcanoes located within the range of the fire ring has the natural disaster potential of volcano eruption. The main concern in this study is the number of tribes people / communities in Indonesia who live in the slopes of the volcano, and the other factor is the fact that people living on the slopes are mostly came from low-education background, making it difficult for the government to socializing the danger. This study will discuss the design and stages of appropriate communication to convey the volcano eruption socialization to the tribes that live in the volcano area using the visual language of infographic. The case studies of this research will take a sampling of the Tengger tribe who inhabit the area of Mount Bromo as one of the active volcano on the Java island, Indonesia. The data retrieving methods used in this study are in-depth interviews, direct observation, and the collection of related books and journal literature. Contributions and model of this research is expected to be applicable to inform people who inhabit the volcano areas in Indonesia of the proper action to take when the volcano eruption strikes.
2
Agustin, Fitriani, and Sutikno Bronto. "Volkanostratigrafi Inderaan Jauh Kompleks Gunungapi Gede dan Sekitarnya, Jawa Barat, Indonesia." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (2019): 9. http://dx.doi.org/10.33332/jgsm.2019.v20.1.9-16.
Full textAbstract:
Remote sensing technology greatly helps to identify the various of volcano features, including active, old and ancient volcanoes. The aim of this paper is intended to introduce various volcanic features in the Gede Volcano Complexs (GVC) and souronding area; compose volcanostratigraphy; and estimate the history of the volcanoes. The method used is a visual interpretation 9 meters spatial resolution of Digital Elevation Model (DEM) TerraSar-x image. Indonesian Stratigraphy Nomenclature Guide 1996 was implemented in vocanostratigraphy unit classification, involving Arc, Super Brigate, Brigate, Crown and Hummockly. Based on the interpretation the DEM image, volcanostratigraphic unit the Gede Volcano Complex consists of Bregade Masigit (Br. M.), which consists of Joklok (Gm.J.) and Gegerbentang (Gm.G.) Hummocs; Crown Lingkung (Kh.L.) consisting of Pangrango (Gm.P.), Situ Gunung (Gm Sg.), Cikahuripan (Gm.Ck.), Pasir Prahu (Gm.Ph) Hummocs; Gege Crown (Kh.G.), which is located in the east of Lingkung Crown. The Gede Crown consists of Gumuruh humock (Gm.Gh.), Gunung Gede lava flows (LG 1,2,3,4,5), and giant debrise avalances (gv-G). The geological mapping based volcanostratigraphy is very useful for exploration of mineral and energy resources, as well as geological hazards.Keywords : volcanostratigraphy, DEM TerraSar-x image, Gunung Gede Complexs.
3
Agustin, Fitriani, and Sutikno Bronto. "Volkanostratigrafi Inderaan Jauh Kompleks Gunungapi Gede dan Sekitarnya, Jawa Barat, Indonesia." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (2019): 9. http://dx.doi.org/10.33332/jgsm.geologi.20.1.9-16.
Full textAbstract:
Remote sensing technology greatly helps to identify the various of volcano features, including active, old and ancient volcanoes. The aim of this paper is intended to introduce various volcanic features in the Gede Volcano Complexs (GVC) and souronding area; compose volcanostratigraphy; and estimate the history of the volcanoes. The method used is a visual interpretation 9 meters spatial resolution of Digital Elevation Model (DEM) TerraSar-x image. Indonesian Stratigraphy Nomenclature Guide 1996 was implemented in vocanostratigraphy unit classification, involving Arc, Super Brigate, Brigate, Crown and Hummockly. Based on the interpretation the DEM image, volcanostratigraphic unit the Gede Volcano Complex consists of Bregade Masigit (Br. M.), which consists of Joklok (Gm.J.) and Gegerbentang (Gm.G.) Hummocs; Crown Lingkung (Kh.L.) consisting of Pangrango (Gm.P.), Situ Gunung (Gm Sg.), Cikahuripan (Gm.Ck.), Pasir Prahu (Gm.Ph) Hummocs; Gege Crown (Kh.G.), which is located in the east of Lingkung Crown. The Gede Crown consists of Gumuruh humock (Gm.Gh.), Gunung Gede lava flows (LG 1,2,3,4,5), and giant debrise avalances (gv-G). The geological mapping based volcanostratigraphy is very useful for exploration of mineral and energy resources, as well as geological hazards.Keywords : volcanostratigraphy, DEM TerraSar-x image, Gunung Gede Complexs.DOI: 10.33332/jgsm.2019.v20.1.9-16
4
Agustin, Fitriani, and Sutikno Bronto. "Volkanostratigrafi Inderaan Jauh Kompleks Gunungapi Gede dan Sekitarnya, Jawa Barat, Indonesia." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (2019): 9. http://dx.doi.org/10.33332/jgsm.geologi.v20i1.386.
Full textAbstract:
Remote sensing technology greatly helps to identify the various of volcano features, including active, old and ancient volcanoes. The aim of this paper is intended to introduce various volcanic features in the Gede Volcano Complexs (GVC) and souronding area; compose volcanostratigraphy; and estimate the history of the volcanoes. The method used is a visual interpretation 9 meters spatial resolution of Digital Elevation Model (DEM) TerraSar-x image. Indonesian Stratigraphy Nomenclature Guide 1996 was implemented in vocanostratigraphy unit classification, involving Arc, Super Brigate, Brigate, Crown and Hummockly. Based on the interpretation the DEM image, volcanostratigraphic unit the Gede Volcano Complex consists of Bregade Masigit (Br. M.), which consists of Joklok (Gm.J.) and Gegerbentang (Gm.G.) Hummocs; Crown Lingkung (Kh.L.) consisting of Pangrango (Gm.P.), Situ Gunung (Gm Sg.), Cikahuripan (Gm.Ck.), Pasir Prahu (Gm.Ph) Hummocs; Gege Crown (Kh.G.), which is located in the east of Lingkung Crown. The Gede Crown consists of Gumuruh humock (Gm.Gh.), Gunung Gede lava flows (LG 1,2,3,4,5), and giant debrise avalances (gv-G). The geological mapping based volcanostratigraphy is very useful for exploration of mineral and energy resources, as well as geological hazards.Keywords : volcanostratigraphy, DEM TerraSar-x image, Gunung Gede Complexs.DOI: 10.33332/jgsm.2019.v20.1.9-16
5
Agustin, Fitriani, and Sutikno Bronto. "Volkanostratigrafi Inderaan Jauh Kompleks Gunungapi Gede dan Sekitarnya, Jawa Barat, Indonesia." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (2019): 9. http://dx.doi.org/10.33332/jgsm.v20i1.386.
Full textAbstract:
Remote sensing technology greatly helps to identify the various of volcano features, including active, old and ancient volcanoes. The aim of this paper is intended to introduce various volcanic features in the Gede Volcano Complexs (GVC) and souronding area; compose volcanostratigraphy; and estimate the history of the volcanoes. The method used is a visual interpretation 9 meters spatial resolution of Digital Elevation Model (DEM) TerraSar-x image. Indonesian Stratigraphy Nomenclature Guide 1996 was implemented in vocanostratigraphy unit classification, involving Arc, Super Brigate, Brigate, Crown and Hummockly. Based on the interpretation the DEM image, volcanostratigraphic unit the Gede Volcano Complex consists of Bregade Masigit (Br. M.), which consists of Joklok (Gm.J.) and Gegerbentang (Gm.G.) Hummocs; Crown Lingkung (Kh.L.) consisting of Pangrango (Gm.P.), Situ Gunung (Gm Sg.), Cikahuripan (Gm.Ck.), Pasir Prahu (Gm.Ph) Hummocs; Gege Crown (Kh.G.), which is located in the east of Lingkung Crown. The Gede Crown consists of Gumuruh humock (Gm.Gh.), Gunung Gede lava flows (LG 1,2,3,4,5), and giant debrise avalances (gv-G). The geological mapping based volcanostratigraphy is very useful for exploration of mineral and energy resources, as well as geological hazards.Keywords : volcanostratigraphy, DEM TerraSar-x image, Gunung Gede Complexs.
6
Bani, P., M. Hendrasto, H. Gunawan, and S. Primulyana. "Sulfur dioxide emissions from Papandayan and Bromo, two Indonesian volcanoes." Natural Hazards and Earth System Sciences 13, no. 10 (2013): 2399–407. http://dx.doi.org/10.5194/nhess-13-2399-2013.
Full textAbstract:
Abstract. Indonesia hosts 79 active volcanoes, representing 14% of all active volcanoes worldwide. However, little is known about their SO2 contribution into the atmosphere, due to isolation and access difficulties. Existing SO2 emission budgets for the Indonesian archipelago are based on extrapolations and inferences as there is a considerable lack of field assessments of degassing. Here, we present the first SO2 flux measurements using differential optical absorption spectroscopy (DOAS) for Papandayan and Bromo, two of the most active volcanoes in Indonesia. Results indicate mean SO2 emission rates of 1.4 t d−1 from the fumarolic activity of Papandayan and more than 22–32 t d−1 of SO2 released by Bromo during a declining eruptive phase. These DOAS results are very encouraging and pave the way for a better evaluation of Indonesian volcanic emissions.
7
Bani, P., M. Hendrasto, H. Gunawan, and S. Primulyana. "Sulfur dioxide emissions from Papandayan and Bromo, two Indonesian volcanoes." Natural Hazards and Earth System Sciences Discussions 1, no. 3 (2013): 1895–912. http://dx.doi.org/10.5194/nhessd-1-1895-2013.
Full textAbstract:
Abstract. Indonesia hosts 79 active volcanoes, representing 14% of all active volcanoes worldwide. However, little is known about their passive degassing into the atmosphere due to isolation and access difficulties. Existing SO2 emission budgets for the Indonesian archipelago are based on extrapolations and inferences as there is a considerable lack of field assessments of degassing. Here, we present the first SO2 flux measurements using DOAS for Papandayan and Bromo, two of the most active volcanoes in Indonesia. Results indicate mean SO2 emission rates of 1.4 t d−1 from the fumarolic activity of Papandayan and more than 22–32 t d−1 of SO2 released by Bromo during a declining eruptive phase.
8
Iguchi, Masato, Surono, Takeshi Nishimura, et al. "Methods for Eruption Prediction and Hazard Evaluation at Indonesian Volcanoes." Journal of Disaster Research 7, no. 1 (2012): 26–36. http://dx.doi.org/10.20965/jdr.2012.p0026.
Full textAbstract:
We report methods, based on geophysical observations and geological surveys, for the prediction of eruptions and the evaluation of the activity of 4 volcanoes in Indonesia. These are Semeru, Guntur, Kelud and Sinabung volcanoes. Minor increases in tilt were detected by borehole tiltmeters prior to eruptions at the Semeru volcano depending on the seismic amplitude of explosion earthquakes. The results show the possibility of prediction of the type and magnitude of eruption and the effectiveness of observation with a high signalto-noise ratio. The establishment of background data is important for evaluating volcanic activity in longterm prediction. Typical distributions of volcanic and local tectonic earthquakes were obtained around the Guntur volcano, where geodetic monitoring by continuous GPS observation is valuable. The cumulative volume of eruptive products is valuable for evaluating the potential for future eruption. The eruptive rate of the Kelud volcano is ca 2×106m3/y (dense rock equivalent), but the volume of the 2007 eruption was only 2×107m3, suggesting a still high potential for eruption. Based on geological surveys and dating, an eruption scenario is proposed for the activity of Mt. Sinabung, where phreatic eruptions occurred in 2010 after a historically long dormancy.
9
Sarjito, Aris. "Crisis Management Policy of Natural Disaster." Advances in Social Sciences Research Journal 7, no. 9 (2020): 183–92. http://dx.doi.org/10.14738/assrj.79.8985.
Full textAbstract:
Abstract
 Indonesia is the country that has the most active volcanoes in the entire world. The Eurasian Plate, the Pacific Plate, and the Indo-Australian Plate are three active tectonic plates that cause collision zones to form these volcanoes. Indonesia is estimated to have 129 volcanoes, all of which are carefully monitored by the Centre for Volcanology and Geological Disaster Mitigation. This is done because several volcanoes in Indonesia continue to show activity. Moreover, it is estimated that more than five million people live in the "danger zone" of a volcano where they must be immediately evacuated if the mountain shows significant upward activity (Indonesia-Investment, 2019). However, efforts to reduce the risk of natural hazards remain largely uncoordinated in different types of hazards and do not necessarily focus on areas with the highest disaster risk.
 This paper uses a descriptive qualitative approach as the main writing approach and uses crisis management theory by Rosenthal, that crisis management involves efforts: (1) to prevent a crisis from occurring; (2) to prepare better protection against the impact of crisis agents; (3) to make effective responses to the actual crisis; and (4) to provide plans and resources for post-crisis recovery and rehabilitation.
 The results of this study are: (1) to accelerate forest recovery, the government can engage the community with security and welfare approach; (2) natural disaster management is the main responsibility of the government; (3) In crises due to natural disasters, form a team that is responsive to critical situations. This team was formed by involving government agencies, community leaders, and NGOs; and (4) to increase the government's capacity to reduce the impact of natural disasters, assessment of potential damage, the establishment of an early warning system, and the improvement of disaster-resistant capabilities are needed.
 Keywords: Crisis Management; Natural Disaster; Policy.
10
Nakada, Setsuya, Fukashi Maeno, Mitsuhiro Yoshimoto, et al. "Eruption Scenarios of Active Volcanoes in Indonesia." Journal of Disaster Research 14, no. 1 (2019): 40–50. http://dx.doi.org/10.20965/jdr.2019.p0040.
Full textAbstract:
Eruption scenarios were prepared as possible sequences in event trees for six active volcanoes in Indonesia, that are located near populated areas or have erupted in recent years (Galunggung, Guntur, Kelud, Merapi, Semeru, and Sinabung). The event trees prepared here show sequences of possible eruption phenomena without probabilities on branches and cover sequences experienced in historical and pre-historical eruptions based on archives and field research results. Changing magma discharge rates during eruption sequences were considered for the event tree of Merapi. This conceptual event tree can also be used as a short-term event tree in which forecasting the coming eruption became possible with geophysical and geochemical monitoring data. Eruption event trees prepared for selected time windows cannot illustrate all plausible hazards and risks associated with an eruption. Therefore, hazards and risks generated from an eruption should be considered in different domains from the event tree.