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Journal articles on the topic 'Krakatoa (Indonesia)'

Author: Grafiati

Published: 4 June 2021

Last updated: 30 January 2023

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1

Bosnak, Judith, and Rick Honings. "‘Behoed ons arme volk voor de vulkaan-poëten’." De Moderne Tijd 4, no. 3 (2020): 382–422. http://dx.doi.org/10.5117/dmt2020.3-4.012.honi.

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Abstract ‘Save our poor people from the vulcano poets’. The literary reception of the Krakatoa disaster of 1883 in the Netherlands and Indonesi On August 27, 1883, the volcano Krakatau in the Dutch East Indies erupted and collapsed, causing the deaths of tens of thousands, mainly as a result of devastating tsunamis. The Krakatau eruption was one of the first disasters to take place beyond the Dutch boundaries that received so much attention in the Netherlands. Because the Indies were a Dutch colony, a response of the motherland was rather logical. In many places, charity activities were organi

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Jayaratne, Ravindra, Aldhiansyah Muhammad Fauzi, Hendra Achiari, and Tomoya Shibayama. "MODELLING OF KRAKATOA TSUNAMI WAVE PROPAGATION AND COMMUNITY ENGAGEMENT BASED ON SWOT ANALYSIS IN SOUTHERN LAMPUNG, INDONESIA." Coastal Engineering Proceedings, no. 36v (December 28, 2020): 30. http://dx.doi.org/10.9753/icce.v36v.currents.30.

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The eruption of Krakatoa which occurred on the 22 December 2018 caused an avalanche from the Gunung Anak Krakatau (GAK) body into the sea, causing a tsunami in the Sunda Strait. The tsunami affected Lampung (Sumatra) and Banten (Java) provinces in Indonesia. Based on the field observations made by Takabatake et al. (2019) in the southern part of Lampung, it was identified that there were severely damaged areas in Lampung; i.e. East Way Muli, Central Way Muli, and Kunjir villages. A numerical model was developed to simulate past and future tsunami wave propagation scenarios. In addition, the st

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3

Abdurrachman, Mirzam, Sri Widiyantoro, Bambang Priadi, and Taufik Ismail. "Geochemistry and Structure of Krakatoa Volcano in the Sunda Strait, Indonesia." Geosciences 8, no. 4 (2018): 111. http://dx.doi.org/10.3390/geosciences8040111.

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Kholailah, Hilda, Septi Wulandari, and Rossi Lara Murtiningsih. "Pengaruh Sektor Pariwisata Terhadap Perekonomian Masyarakat dan Kebersihan Lingkungan (Studi Kasus : Pantai Grand Elty Krakatoa Resort Kalianda, Lampung Selatan)." Holistic Journal of Management Research 5, no. 1 (2022): 38–61. http://dx.doi.org/10.33019/hjmr.v5i1.2771.

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Abstrak Pariwisata merupakan sebuah industri yang perkembangannya kian pesat setiap tahunnya. Di Indonesia sektor Pariwisata dikembangkan sebagai sektor yang menjanjikan mendatangkan pendapatan bagi Negara terlebih didaerah-daerah yang memiliki sumber daya alam, maupun sumber daya budaya yang melimpah. Berbagai potensi digali untuk menarik minat wisatawan untuk datang berkunjung sehingga dapat mengharapkan mampu meningkatkan kesejahteraan masyarakat. Tujuan dalam penelitian ini adalah untuk mengidentifikasi potensi sumber daya alam yang dapat dimanfaatkan. Objek yang akan di identifikasi

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Heidarzadeh, Mohammad, Takeo Ishibe, Osamu Sandanbata, Abdul Muhari, and Antonius B. Wijanarto. "Numerical modeling of the subaerial landslide source of the 22 December 2018 Anak Krakatoa volcanic tsunami, Indonesia." Ocean Engineering 195 (January 2020): 106733. http://dx.doi.org/10.1016/j.oceaneng.2019.106733.

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Lara, Jaime. "Francis Alive and Aloft: Franciscan Apocalypticism in the Colonial Andes." Americas 70, no. 02 (2013): 139–63. http://dx.doi.org/10.1017/s0003161500003205.

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The seventeenth century opened with a bang, literally. In the year 1600, on the first Friday in the season of Lent, sometime between noon and 3:00 PM (that is, at the hour of the accustomed Lenten penitential processions), the Peruvian volcano of Huaynapudna began a protracted series of explosions and eruptions. It was the largest recorded volcanic eruption in the Western Hemisphere, greater by far than that of Mount Vesuvius in 79 CE, or Mount St. Helens in 1980, and only slightly smaller than the colossal eruption of Krakatoa, Indonesia, in 1883. The event sent both Christian Spaniards and n

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Lara, Jaime. "Francis Alive and Aloft: Franciscan Apocalypticism in the Colonial Andes." Americas 70, no. 2 (2013): 139–63. http://dx.doi.org/10.1353/tam.2013.0096.

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The seventeenth century opened with a bang, literally. In the year 1600, on the first Friday in the season of Lent, sometime between noon and 3:00 PM (that is, at the hour of the accustomed Lenten penitential processions), the Peruvian volcano of Huaynapudna began a protracted series of explosions and eruptions. It was the largest recorded volcanic eruption in the Western Hemisphere, greater by far than that of Mount Vesuvius in 79 CE, or Mount St. Helens in 1980, and only slightly smaller than the colossal eruption of Krakatoa, Indonesia, in 1883. The event sent both Christian Spaniards and n

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8

Ali, Muhammad, Teuku Rasyif, and Teuku Mahlil. "Landslide tsunami impact assessment toward human lives using numerical modelling: A case study from Banten, Indonesia." E3S Web of Conferences 340 (2022): 01015. http://dx.doi.org/10.1051/e3sconf/202234001015.

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After the eruption of Mount Anak Krakatoa, December 22, 2018, which was accompanied by a large landslide into the waters of the Sunda Strait, resulting a tsunami that hit South Coast of Lampung and West of Banten. According [1], 437 peoples were death, 31,942 peoples were injured and 10 peoples were lost due to this disaster. The tsunami impact toward human lives was calculated by using the human instability equation [3] and TUNAMI Two Layer model was applied to simulate the landslide and propagation of tsunami [2]. The simulation results were validated with observations and field measurements

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9

Lee, Han Soo, Ricard Diago Sambuaga, and Constanza Flores. "Effects of Tsunami Shelters in Pandeglang, Banten, Indonesia, Based on Agent-Based Modelling: A Case Study of the 2018 Anak Krakatoa Volcanic Tsunami." Journal of Marine Science and Engineering 10, no. 8 (2022): 1055. http://dx.doi.org/10.3390/jmse10081055.

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On 22 December 2018, the volcanic eruption of Anak Krakatoa in the Sunda Strait, Indonesia, triggered a tsunami causing 437 deaths. The highest death toll and the second highest number of damaged houses were recorded in Panimbang. This study proposes optimum evacuation shelters to reduce the mortality rate. A digital elevation model (DEM) and information dataset are used. The suggested horizontal evacuation shelters (HESs) are places of worship, schools, and government offices. Multimodal agent-based modelling (ABM), to analyse the sensitivity of parameters and the effect of vertical evacuatio

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Adrian, Adrian. "MODEL SPASIAL KERENTANAN DIKAWASAN PESISIR SELATAN TELUK BETUNG KOTA BANDAR LAMPUNG TERHADAP BENCANA TSUNAMI." Jurnal SPATIAL Wahana Komunikasi dan Informasi Geografi 15, no. 1 (2016): 23–28. http://dx.doi.org/10.21009/spatial.151.04.

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ABSTRACT Bandar Lampung is an area in Indonesia which has a high level of Tsunami threat. It is due to the position of Bandar Lampung which is located relatively near the meeting point of Indo-Australian plate dan the Eurasian plate; both are plates are relatively active. Other causes are earthquake threat and the existence of Krakatoa which is potential to generate earthquakes which are followed by a Tsunami. The data analysis showed that the potential Tsunami hazard in the coastal city of Bandar Lampung is the predicted distance run up the marinade tsunami that reached a height of 20 m

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11

Putra, Rediyanto, Sumadi Sumadi, Rahma Rina Wijayanti, Berlina Yudha Pratiwi, and Oryza Ardhiarisca. "Rhetoric in sustainability report at PT Krakatau Steel Indonesia." Journal of Economics, Business & Accountancy Ventura 21, no. 3 (2019): 333. http://dx.doi.org/10.14414/jebav.v21i3.1234.

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This research was motivated by the implementation of Corporate Social Responsibility (CSR) activities at PT. Krakatau Steel, having suffered losses for five consecutive years. The objective of this study is to understand and prove the use of rhetorical communication techniques in the sustainability report by PT Krakatau Steel (public limited company). The data were taken from the sustainability report of PT Krakatau Steel from 2012 until 2016. This research uses qualitative approach with interpretive method. The analysis was done by means of a semiotic analysis of Charles Sanders Pierce. The r

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Hanifa, R. A. K., and L. I. Bernawis. "Study of Bathymetry and Seabed Morphology Changes Around Anak Krakatau Waters of 2018 Post-Eruption." IOP Conference Series: Earth and Environmental Science 925, no. 1 (2021): 012061. http://dx.doi.org/10.1088/1755-1315/925/1/012061.

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Abstract Anak Krakatau is an active volcanic mountain located in the Sunda Strait, Indonesia. On December 22, 2018, this mountain erupted and the flank collapses off into the water. This changes the bathymetry and morphology of the seabed around the waters of Anak Krakatau volcano. This study uses bathymetry data surrounding the Anak Krakatau waters from the Indonesian Navy Hydrographic and Oceanographic Center (PUSHIDROSAL) in 2016 and 2019. The data were obtained by survey using Echosounder Multibeam System MBES EM2040 and EM302. By means of surface analysis method (hillshade), the data were

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Hoffman-Rothe, Arne, Malte Ibs-von Seht, Rudolf Knieβ, et al. "Monitoring Anak Krakatau Volcano in Indonesia." Eos, Transactions American Geophysical Union 87, no. 51 (2006): 581. http://dx.doi.org/10.1029/2006eo510002.

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14

Gardner, M. F., V. R. Troll, J. A. Gamble, et al. "Crustal Differentiation Processes at Krakatau Volcano, Indonesia." Journal of Petrology 54, no. 1 (2012): 149–82. http://dx.doi.org/10.1093/petrology/egs066.

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15

Kristianto, N. Indrastuti, A. Basuki, et al. "Potential Eruption and Current Activity of Anak Krakatau Volcano, Indonesia." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012021. http://dx.doi.org/10.1088/1755-1315/873/1/012021.

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Abstract Anak Krakatau Volcano is located in the Sunda Strait known for its paroxysmal eruption in 1883. During the January - November 2019 period, seismicity was dominated by types of quakes which indicated the occurrence of magma supply (VA and VB), near-surface volcanic activity (LF, Hybrid, Harmonic Tremors), and volcanic activity above the volcanic surface (eruptions, emission, and continuous tremors). In the period December 2019 - July 2020, there was an increase in the types of quakes near the surface (LF, Hybrid) and the types of quakes on the surface (emission and continuous tremors).

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16

Putra, Singgih Afifa, Ario Damar, and Agustinus M. Samosir. "Colonization of Coral Communities in the Krakatau Islands Strict Marine Nature Reserve, Indonesia (Kolonisasi Komunitas Karang di Kepulanan Krakatau)." ILMU KELAUTAN: Indonesian Journal of Marine Sciences 19, no. 2 (2014): 63. http://dx.doi.org/10.14710/ik.ijms.19.2.63-74.

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Pulau-pulau Krakatau memiliki dinamika secara geomorfologi, dan berbagai perubahan fisik yang berlangsung memberikan dampak terhadap biota, termasuk pada proses dan tingkat pergantian suksesi komunitasnya. Tujuan penelitian ini untuk menjelaskan kondisi terkini dan proses kolonisasi komunitas karang, termasuk status kerusakan komunitas karang dan disturbansi lingkungan yang mempengaruhinya. Line intercept transect dilakukan di enam stasiun pada dua kedalaman yang berbeda yakni 5 dan 10m. Sedangkan observasi terhadap komunitas koral dilakukan dengan perekaman video. Hasil penelitian ini menunju

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VACHON, Max, and Takuya ABE. "Colonization of the Krakatau Islands (Indonesia) by Scorpions." Acta Arachnologica 37, no. 1 (1988): 23–32. http://dx.doi.org/10.2476/asjaa.37.23.

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Tagawa, H., E. Suzuki, T. Partomihardjo, and A. Suriadarma. "Vegetation and succession on the Krakatau Islands, Indonesia." Vegetatio 60, no. 3 (1985): 131–45. http://dx.doi.org/10.1007/bf00039928.

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19

Kurniawan, Wahyu, Daryono, IDK Kerta, Bayu Pranata, and Tri Winugroho. "Monitoring and analysis of seismic data during the 2018 sunda strait tsunami." E3S Web of Conferences 331 (2021): 07006. http://dx.doi.org/10.1051/e3sconf/202133107006.

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The tsunami of Sunda Strait occurred on December 22, 2018, at 21:03 West Indonesia Time (zone). An eruption of Mount Anak Krakatau caused an eruption that triggered a landslide on the slopes of Mount Anak Krakatau covering an area of 64 hectares that hit the coastal area of western Banten and southern Lampung and resulted in 437 deaths, 14.059 people were injured, and 33.721 people were displaced. Before the tsunami, signal transmissions (gaps) at the Lava seismograph station installed on the body of Mount Anak Krakatau experienced broken so that Mount Anak Krakatau Observation Post could not

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Babu, Arun, and Shashi Kumar. "InSAR Coherence and Backscatter Images Based Analysis for the Anak Krakatau Volcano Eruption." Proceedings 24, no. 1 (2019): 21. http://dx.doi.org/10.3390/iecg2019-06216.

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The Anak Krakatau Island and volcano caldera are located at the Sunda Strait between the Java and Sumatra Islands of Indonesia. The volcano started erupting on 22 December 2018, and collapse of the volcano resulted in Tsunami. The large tidal waves caused mass destruction and loss of life in the Java and Sumatra islands. The objective of this study was the interferometric SAR coherence and backscatter images based analysis of Anak Krakatau Island using Sentinel-1 SAR data. Seven datasets of ESA’s Sentinel-1 C-band satellite acquired from 25 November 2018 to 24 January 2019 were used in this st

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Ardian, D. N., H. Darmawan, Wahyudi, et al. "Grain size, mineralogical, and geochemistry of the 1996-2018 Volcanic Products of Anak Krakatau Volcano, Indonesia." IOP Conference Series: Earth and Environmental Science 1071, no. 1 (2022): 012017. http://dx.doi.org/10.1088/1755-1315/1071/1/012017.

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Abstract Anak Krakatau Volcano is the only active volcano on Krakatau Volcanic Complex. It is located in the Sunda Strait as part of the Quaternary volcanic arc as a result of the Indo-Australian plate subduction under the Eurasian plate. The volcanic activity of the Anak Krakatau volcano since 1927 is considered to be very active with a combination of explosive and effusive eruptions. Lava flow tends to be concentrated in the southwestern part, except for the 1996 lava flow (north) and 1993 lava flow (northeast). In 2018 there was an eruption accompanied by flank collapse on the southwestern

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MANSUR, Suraya, Nurhayani SARAGIH, Siti SUSILAWATI, Yusiatie UDUD, and Endri ENDRI. "Consumer Brand Engagement and Brand Communications on Destination Brand Equity Maritine Tourism in Indonesia." Journal of Environmental Management and Tourism 12, no. 4 (2021): 1032. http://dx.doi.org/10.14505//jemt.v12.4(52).16.

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This study aimed to understand the influence of consumer-brand engagement and brand communication on destination brand equity, survey to maritime tourism of Ujung Kulon and Anak Krakatau, Banten. The population chosen in this study is the Instagram followers of Ujung Kulon and Krakatau Banten.The total of the samples are 96 respondents chosen using purposive sampling. This study used inferential statistic tests, which were divided into two: The correlation Test and Linear Regression Test. This study used a correlational survey method Approach. This research used a quantitative approach and a p

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Firdaus, Azhar, Suraya Abdulwahab Afiff, and Herdiansyah. "Community Resilient from Anak Krakatau Eruption: Lesson Learn from The Tale of Lampung Submerged to Increase Environmental Awareness." IOP Conference Series: Earth and Environmental Science 1111, no. 1 (2022): 012073. http://dx.doi.org/10.1088/1755-1315/1111/1/012073.

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Abstract Natural disasters in Indonesia have a high frequency because a whole land and sea in Indonesia be hemmed in tectonic and volcanic plates. Some natural disasters are not caused by those plates, such as landslides, floods, hurricanes, etcetera. In the research location (beginning of 2018), there was a natural disaster called the silent tsunami caused by landslides at Mount Anak Krakatau in the middle of the ocean. In large quantities, these landslides produced high waves in the coastal area in Lampung and Banten, and there was no early warning system for this silent tsunami. The article

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PARTOMIHARDJO, Tukirin, Edi MIRMANTO, Soedarsono RISWAN, and Eizi SUZUKI. "Drift Fruits and Seeds on Anak Krakatau Beaches, Indonesia." Tropics 2, no. 3 (1993): 143–56. http://dx.doi.org/10.3759/tropics.2.143.

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Nagai, Kaori, Taro Arikawa, Kwanchai Pakoksung, Fumihiko Imamura, Masashi Watanabe, and Pan Huang. "VOLCANIC ERUPTION-INDUCED TSUNAMI AT ANAK KRAKATAU VOLCANO, SUNDA STRAIT, INDONESIA." Coastal Engineering Proceedings, no. 36v (December 28, 2020): 33. http://dx.doi.org/10.9753/icce.v36v.currents.33.

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On 22 December 2018, a volcanic eruption occurred at Anak Krakatau, Sunda Strait, Indonesia, which induced a tsunami. At the coastal area in the Sunda Strait, the destructive tsunami destroyed many structures and killed more than 400 people approximately 30 to 40 min after the eruption. In this event, it has been reported that many residents start to evacuate after seeing tsunami because alert of tsunami was not occurred. It is difficult to escape from a tsunami after seeing it waves, so early evacuation become important. Previously, many studies which handle Krakatau volcanic eruption induced

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New, Tim R. "Colonization, succession and conservation: the invertebrates of Anak Krakatau, Indonesia, and contrast with Surtsey." Surtsey research 13 (2015): 31–39. http://dx.doi.org/10.33112/surtsey.13.3.

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Surveys of selected terrestrial invertebrates on Anak Krakatau, Indonesia, during the 1980s/1990s exemplify the variety of colonization and successional processes contributing to foundation of new ecological communities. Both aeolian and vegetation-based successions are important, but interpretation is hampered by lack of knowledge of the fauna of species-rich source areas in this tropical environment. Major disturbances from increased visitor numbers contaminate the natural processes, and volcanic activity is an ever-present influence. The monitoring and inventory studies needed to provide a

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Marpaung, Fredric Mangatur Haulian. "Dampak Perilaku Oportunistik Manajerial dan CorporateGovernance Terhadap Kebijakan Dividen." Jurnal IPTEK 3, no. 1 (2019): 182–86. http://dx.doi.org/10.31543/jii.v3i1.143.

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PT. Krakatau Steel, Tbk., perusahaan terbesar di Asia Tenggara, dan salah satu kontributor pendapatan untuk Indonesia dari 80% keuntungan penjualan mereka. Tapi dari tahun 2012 sampai 2014 penjualan mereka akan menurun disebabkan banyak faktor. Dan akan membuat pendapatan perusahaan juga turun. Penelitian ini bertujuan untuk mengetahui dampak perilaku manajerial oportunistik dan corporategovernance terhadap kebijakan dividen pada PT. Krakatau Steel, Tbk. Penelitian ini menggunakan teknik analisis regresi berganda. dampak kepemilikan institusional, dewan komisaris independen, jumlah komisaris,

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Gross, CL. "The Reproductive Ecology of Canavalia rosea (Fabaceae) on Anak Krakatau, Indonesia." Australian Journal of Botany 41, no. 5 (1993): 591. http://dx.doi.org/10.1071/bt9930591.

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Pioneer plant species are expected to have higher fruit-to-flower ratios than plants found in more established habitats. This was not found to be the case with Canavalia rosea on Anak Krakatau, Indonesia. Canavalia rosea is a pantropical pioneer plant species of beach habitats. On Anak Krakatau fruit-set in C. rosea in July 1992 ranged between 10 and 19% and a study of pollination and resource levels was undertaken to determine the cause of low fruit-to-flower ratios. An examination of flowering and fruiting phenology, breeding system and floral visitors revealed that low fruit-set in the popu

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Choi, B. H., E. Pelinovsky, K. O. Kim, and J. S. Lee. "Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption." Natural Hazards and Earth System Sciences 3, no. 5 (2003): 321–32. http://dx.doi.org/10.5194/nhess-3-321-2003.

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Abstract. The 1883 Krakatau volcanic eruption has generated a destructive tsunami higher than 40 m on the Indonesian coast where more than 36 000 lives were lost. Sea level oscillations related with this event have been reported on significant distances from the source in the Indian, Atlantic and Pacific Oceans. Evidence of many manifestations of the Krakatau tsunami was a subject of the intense discussion, and it was suggested that some of them are not related with the direct propagation of the tsunami waves from the Krakatau volcanic eruption. Present paper analyzes the hydrodynamic part of

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YOSHIDA, Hajime. "The Spider Family Theridiidae(Arachnida:Araneae) from the Krakatau Islands, Indonesia." Acta Arachnologica 43, no. 2 (1994): 139–44. http://dx.doi.org/10.2476/asjaa.43.139.

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Whittaker, R. J., M. B. Bush, and K. Richards. "Plant Recolonization and Vegetation Succession on the Krakatau Islands, Indonesia." Ecological Monographs 59, no. 2 (1989): 59–123. http://dx.doi.org/10.2307/2937282.

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Harvey, Mark S. "Pseudoscorpions from Krakatau Islands and adjacent regions, Indonesia (Chelicerata: Pseudoscorpionida)." Memoirs of the Museum of Victoria 49, no. 2 (1988): 309–53. http://dx.doi.org/10.24199/j.mmv.1988.49.13.

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Higashi, Teruo, Susumu Richard Anraku, Nobufumi Miyauchi, Akio Shinagawa, Muhamad Rachman Djuwansah, and Achmad Sule. "Formation of Ca/Mg-Humates in Troporthents, Krakatau Islands, Indonesia." Soil Science and Plant Nutrition 33, no. 1 (1987): 137–42. http://dx.doi.org/10.1080/00380768.1987.10557558.

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34

Linqi, Xia, and R. Clocchiatti. "Magmatic inclusions in phenocrystals from andesitic lavas, Krakatau volcano, Indonesia." Chinese Journal of Geochemistry 5, no. 4 (1986): 331–46. http://dx.doi.org/10.1007/bf02866709.

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35

Camus, G., A. Gourgaud, and P. M. Vincent. "Petrologic evolution of Krakatau (Indonesia): Implications for a future activity." Journal of Volcanology and Geothermal Research 33, no. 4 (1987): 299–316. http://dx.doi.org/10.1016/0377-0273(87)90020-5.

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Setiawati, Astriana Rahmi, Jamalam Lumbanraja, Septi Nurul Aini, Dermiyati Dermiyati, Henrie Buchari, and Zuldadan Naspendra. "Texture and Chemical Properties of Two Depth Soils in a Toposequence of Anak Krakatau Before December 2018 Eruption." JOURNAL OF TROPICAL SOILS 25, no. 2 (2020): 71. http://dx.doi.org/10.5400/jts.2020.v25i2.71-81.

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Anak Krakatau volcano is one of the famous volcanic mountains located in the sea to the south part of the Province of Lampung, Indonesia. The volcano was derived from the active Krakatau caldera that first appeared on the surface in 1930 or 47 years after the eruption of Krakatau in 1883. The materials produced by the Anak Krakatau eruption were very interesting related to soil forming materials, especially their physical and chemical properties. The objectives of this study were to present information about the texture and chemical properties of soil from Anak Krakatau Mountain taken at the s

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Natalia, Happy Christin, Danni Gathot Harbowo, and Rinaldi Ikhram. "Potensi Geodiversity di Sekitar Kawasan Anak Krakatau-Way Kambas, Provinsi Lampung, Sebagai Kandidat Geopark Indonesia." Journal of Science and Applicative Technology 5, no. 1 (2021): 47. http://dx.doi.org/10.35472/jsat.v5i1.318.

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The global significance of Krakatau Volcanic Complex and Way Kambas National Park is the best potential areas to be developed as part of a world heritage, particularly as UNESCO Global Geopark. Both of these objects are in the Lampung Province, Indonesia. Soon, it is necessary to identify and make an inventory of key sites that could become the theme of the area. The study of geodiversity and scientific valuation was carried out which referred to the Technical Guidelines for the Assessment of Indonesia Geological Heritage Resources, 2019. Based on these studies and assessments, there are 14 ke

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GREENSLADE, PENELOPE. "Correction to the identification of a pioneer species of Collembola found on Anak Krakatau in 1931." Zootaxa 1846, no. 1 (2008): 59. http://dx.doi.org/10.11646/zootaxa.1846.1.6.

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The first species of Collembola to be recorded from Anak Krakatau Island in Indonesia was Lepidosira calolepis (Börner, 1913). It was listed as Mesira calolepis by Womersley (1932) and was said to be abundant at the time of collection on the island. This small island was produced in 1929 in the Krakatau Archipelago by volcanic activity some three miles from Krakatau itself (Bristowe 1931). The type species of Mesira Shcherbakov, M. squamoornata, was found to belong to the genus Seira Lubbock (Gisin 1960). As M. calolepis had a two-toothed mucro, it could not belong to Seira and instead was fou

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HAYASHI, Toshio. "The Spider Family Clubionidae(Arachnida: Araneae) from the Krakatau Island, Indonesia." Acta Arachnologica 45, no. 1 (1996): 63–72. http://dx.doi.org/10.2476/asjaa.45.63.

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40

Bani, Philipson, Adrien Normier, Clémentine Bacri, et al. "First measurement of the volcanic gas output from Anak Krakatau, Indonesia." Journal of Volcanology and Geothermal Research 302 (September 2015): 237–41. http://dx.doi.org/10.1016/j.jvolgeores.2015.07.008.

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"Antibiotic-resistance patterns of soil bacteria (Gram-negative rods) from the Krakatau Islands (Rakata) and West Java, Indonesia, in 1984." Philosophical Transactions of the Royal Society of London. B, Biological Sciences 322, no. 1211 (1988): 317–26. http://dx.doi.org/10.1098/rstb.1988.0127.

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The explosive eruption of the Indonesian island of Krakatau (Krakatoa) in 1883 almost certainly led to the total destruction of the fauna, flora and microorganisms of the three remaining islands, Rakata (Rakata Besar), Sertung and Panjang (Rakata Kecil). The Ujung Kulon peninsula of Java, 100 km to the south, was much less affected by the volcanic activity. Soil bacteria (Gram-negative rods, GNR) from Rakata (the post-1883 remnant of Krakatau) and the Ujung Kulon peninsula of Java were examined for their antibiotic-resistance patterns. A total of 27 patterns (‘resistotypes’) was detected, base

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Kirchenbaur, M., S. Schuth, A. R. Barth, et al. "Sub-arc mantle enrichment in the Sunda rear-arc inferred from HFSE systematics in high-K lavas from Java." Contributions to Mineralogy and Petrology 177, no. 1 (2021). http://dx.doi.org/10.1007/s00410-021-01871-9.

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AbstractMany terrestrial silicate reservoirs display a characteristic depletion in Nb, which has been explained in some studies by the presence of reservoirs on Earth with superchondritic Nb/Ta. As one classical example, K-rich lavas from the Sunda rear-arc, Indonesia, have been invoked to tap such a high-Nb/Ta reservoir. To elucidate the petrogenetic processes active beneath the Java rear-arc and the causes for the superchondritic Nb/Ta in some of these lavas, we studied samples from the somewhat enigmatic Javanese rear-arc volcano Muria, which allow conclusions regarding the across-arc varia

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43

"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 20, no. 3 (1995). http://dx.doi.org/10.5479/si.gvp.bgvn199503-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 20, no. 6 (1995). http://dx.doi.org/10.5479/si.gvp.bgvn199506-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 20, no. 7 (1995). http://dx.doi.org/10.5479/si.gvp.bgvn199507-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 21, no. 1 (1996). http://dx.doi.org/10.5479/si.gvp.bgvn199601-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 21, no. 9 (1996). http://dx.doi.org/10.5479/si.gvp.bgvn199609-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 21, no. 11 (1996). http://dx.doi.org/10.5479/si.gvp.bgvn199611-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 22, no. 7 (1997). http://dx.doi.org/10.5479/si.gvp.bgvn199707-262000.

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"Report on Krakatau (Indonesia)." Bulletin of the Global Volcanism Network 24, no. 2 (1999). http://dx.doi.org/10.5479/si.gvp.bgvn199902-262000.

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