Field Survey of the 2018 Anak Krakatau Tsunami on the Islands in the Sunda Strait

Total Page:16

File Type:pdf, Size:1020Kb

Field Survey of the 2018 Anak Krakatau Tsunami on the Islands in the Sunda Strait https://meetingorganizer.copernicus.org/EGU2020/EGU2020‐11838.html Field Survey of the 2018 Anak KrakatauFritz et al., 2020 Tsunami on the Islands in the Sunda Strait Hermann M. Fritz1, Tubagus Solihuddin2, Costas E. Synolakis3,4, Gegar S. Prasetya5, Jose C. Borrero6, Vassilis Skanavis3, Semeidi Husrin2, Widjo Kongko7, Dinar C. Istiyanto7, August Daulat2, Dini Purbani2, Hadiwijaya L. Salim2, Rahman Hidayat2, Velly Asvaliantina2, Maria Usman5, Ardito Kodijat9 1 School of Civil and Environmental Eng., Georgia Institute of Technology, Atlanta, GA 30332, USA 2 Marine Research Centre, Ministry of Marine Affairs and Fisheries, Jakarta 14430, Indonesia 3 Dept. of Civil and Env. Eng., University of Southern California, Los Angeles, CA 90089, USA 4 Dep. of Environmental Engineering, Technical University of Crete, Chanea 73100, Greece 5 Indonesian Tsunami Scientific Community, Jakarta 12950, Indonesia 6 eCoast Ltd., 47 Cliff St., Raglan 3225, New Zealand 7 Agency for the Assessment and Application of Technology (BPPT), Yogyakarta 55284, Indonesia 8 Coordinating Ministry for Maritime Affairs – Jakarta 10340, Indonesia 9 IOC‐UNESCO, Indian Ocean Tsunami Information Center (IOTIC), Jakarta 12110, Indonesia 1 Volcanic Tsunamis: Fritz et al., 2020 Krakatau 1883 and 2018 Krakatau 1883 remnant Rakata Anak Krakatau Before (Photo: September 2018) VolcanicAnak Krakatau Tsunamis Before –Krakatau 1883 (Photos: September 2018) Fritz et al., 2020 Meeting at Marine Research Center (MRC): Fritz et al., 2020 Ministry of Marine Affairs and Fisheries (MoMAF) and Coordinating Ministry of Maritime Affairs (CMoMA) 4 TIDE STATION POINTS Slide: Widjo Kongko #Lon. (deg) Lat. (deg.) Sta. Name G.A.K 1 105.8410 ‐6.1893 Serang 2 105.9530 ‐6.0176 Ciwandan 3 104.2130 ‐5.5204 Bangkunat 4 104.6190 ‐5.5003 Kota Agung 5 105.3190 ‐5.4713 Panjang Fritz et al., 2020 Fritz Water Elevation (m) Widjo Slide: ‐ ‐ ‐ 0.6 0.4 0.2 0.2 0.4 0.6 0.8 Water Elevation (m) 0 1 ‐ ‐ ‐ ‐ ‐ 1.00 0.80 0.60 0.40 0.20 0.00 0.20 0.40 0.60 0.80 22/12/2018 7:00:00 et MARIGRAM: al., 22/12/2018 7:00:00 Kongko 22/12/2018 8:00:00 2020 22/12/2018 8:00:00 22/12/2018 9:00:00 22/12/2018 9:00:00 22/12/2018 10:00:00 22/12/2018 10:00:00 22/12/2018 11:00:00 22/12/2018 11:00:00 Ciwandan 22/12/2018 12:00:00 22/12/2018 12:00:00 22/12/2018 13:00:00 22/12/2018 13:00:00 22/12/2018 14:00:00 22/12/2018 14:00:00 22/12/2018 15:00:00 22/12/2018 15:00:00 22/12/2018 16:00:00 (105.953E, Time 22/12/2018 16:00:00 Time (105.953E, 22/12/2018 17:00:00 (UTC+7:00 Ciwandan (UTC+7:00 22/12/2018 17:00:00 Ciwandan 22/12/2018 18:00:00 / WIB) 22/12/2018 18:00:00 6.0176S) 6.0176S) 22/12/2018 19:00:00 / WIB) 22/12/2018 19:00:00 22/12/2018 20:00:00 22/12/2018 20:00:00 22/12/2018 21:00:00 22/12/2018 21:00:00 22/12/2018 22:00:00 22/12/2018 22:00:00 22/12/2018 23:00:00 22/12/2018 23:00:00 23/12/2018 0:00:00 23/12/2018 0:00:00 23/12/2018 1:00:00 23/12/2018 1:00:00 23/12/2018 2:00:00 23/12/2018 2:00:00 G.A.K 23/12/2018 3:00:00 23/12/2018 3:00:00 23/12/2018 4:00:00 23/12/2018 4:00:00 23/12/2018 5:00:00 23/12/2018 5:00:00 23/12/2018 6:00:00 23/12/2018 6:00:00 23/12/2018 7:00:00 23/12/2018 7:00:00 Sunda Strait Islands Tsunami Field Survey 7 Rakata Island Maximum 85 m runup 8 Fritz et al., 2020 Rakata Island Fritz et al., 2020 9 Rakata Island Fritz et al., 2020 10 Rakata Island Fritz et al., 2020 11 Rakata Island Fritz et al., 2020 12 Rakata Island Fritz et al., 2020 13 Rakata Island Fritz et al., 2020 14 Rakata Island Fritz et al., 2020 15 Rakata Island Fritz et al., 2020 16 Rakata Island Fritz et al., 2020 17 Fritz et al., 2020 Rakata Island 18 Rakata Island Fritz et al., 2020 19 Krakatau Volcanic Complex 20 Fritz et al., 2020 Panjang Island Fritz et al., 2020 21 Panjang Island Fritz et al., 2020 22 Panjang Island Fritz et al., 2020 23 Anak Krakatau Volcano Fritz et al., 2020 24 Anak Krakatau Volcano Fritz et al., 2020 25 Sertung Island Fritz et al., 2020 Rakata Anak Krakatau 26 Sertung Island Fritz et al., 2020 27 Sertung Island Fritz et al., 2020 28 Sertung Island Fritz et al., 2020 29 Sertung Island Fritz et al., 2020 30 Sebesi Nearest Inhabited Island 31 Fritz et al., 2020 Sebesi Island Fritz et al., 2020 32 Sebesi Island Fritz et al., 2020 33 Sebesi Island Fritz et al., 2020 34 Sebesi Island Fritz et al., 2020 35 Waymuli, Sumatra Fritz et al., 2020 36 Fritz et al., 2020 Waymuli, Sumatra 37 Panaitan Island, Ujung Kulon National Park 38 Fritz et al., 2020 Panaitan Island, Ujung Kulon National Park Fritz et al., 2020 39 Panaitan Island, Ujung Kulon National Park 40 Fritz et al., 2020 Panaitan Island, Ujung Kulon National Park 41 Fritz et al., 2020 Ujung Kulon National Park 42 Fritz et al., 2020 Ujung Kulon National Park Fritz et al., 2020 43 Ujung Kulon National Park Fritz et al., 2020 44 Ujung Kulon National Park Fritz et al., 2020 45 Eyewitness Interview Fritz et al., 2020 46 Sunda Strait Islands Tsunami Field Survey 47 Fritz et al., 2020 2018 Sunda Strait tsunami CONCLUSIONS Fritz et al., 2020 • ITST collected 87 tsunami heights February 4‐9, 2019 • Maximum 85 m runup on Rakata and an 83 m runup on Sertung. • Flow depth reached more than 11 m above ground on Sertung. • On Sebesi Island located 15 km northeast of the source tsunami runup heights remained below 10 m. • Tsunami heights exceeding 10 m were observed in the Ujung Kulon National Park located 50 km southwest. • The runup distributions on the islands encircling Anak Krakatau highlight the directivity of the collapse towards the southwest. • Inundation and damage were mostly limited to within 400 m of the shoreline given the relatively short wavelengths of volcanic tsunamis. • The team interviewed numerous eyewitnesses based on established protocol and educated residents about tsunami hazards. • Community‐based education and awareness programs are essential to save lives in locales at risk from locally generated tsunamis. • Regrowth of Anak Krakatau will determine the future tsunami hazard • PAGEOPH Borrero et al., 2020 tentatively accepted for publication Acknowledgments Fritz et al., 2020 This work is supported by • National Science Foundation NSF RAPID award CMMI‐1906162 • Any opinions, findings, and conclusions or recommendations expressed herein are those of the author(s) and do not necessarily reflect the views of the National Science Foundation Terima Kasih ‐ Questions Fritz et al., 2020.
Recommended publications
  • Tsunami Hazard Related to a Flank Collapse of Anak Krakatau Volcano
    Downloaded from http://sp.lyellcollection.org/ by guest on January 2, 2019 Tsunami hazard related to a flank collapse of Anak Krakatau Volcano, Sunda Strait, Indonesia T. GIACHETTI1,3*, R. PARIS2,4,6, K. KELFOUN2,4,6 & B. ONTOWIRJO5 1Clermont Universite´, Universite´ Blaise Pascal, Geolab, BP 10448, F-63000 Clermont-Ferrand, France 2Clermont Universite´, Universite´ Blaise Pascal, Laboratoire Magmas et Volcans, BP 10448, F-63000 Clermont-Ferrand, France 3CNRS, UMR 6042, Geolab, F-63057 Clermont-Ferrand, France 4CNRS, UMR 6524, LMV, F-63038 Clermont-Ferrand, France 5Coastal Dynamics Research Center, BPDP-BPPT, 11th Floor, Building 2, BPPT, Jl, M. H. Thamrin no 8, Jakarta 10340, Indonesia 6IRD, R 163, LMV, F-63038 Clermont-Ferrand, France *Corresponding author (e-mail: [email protected]) Abstract: Numerical modelling of a rapid, partial destabilization of Anak Krakatau Volcano (Indonesia) was performed in order to investigate the tsunami triggered by this event. Anak Krakatau, which is largely built on the steep NE wall of the 1883 Krakatau eruption caldera, is active on its SW side (towards the 1883 caldera), which makes the edifice quite unstable. A hypothetical 0.280 km3 flank collapse directed southwestwards would trigger an initial wave 43 m in height that would reach the islands of Sertung, Panjang and Rakata in less than 1 min, with amplitudes from 15 to 30 m. These waves would be potentially dangerous for the many small tourist boats circulating in, and around, the Krakatau Archipelago. The waves would then propagate in a radial manner from the impact region and across the Sunda Strait, at an average speed of 80–110 km h21.
    [Show full text]
  • Hendy Kusmarian
    Dihimpun dan disunting oleh Hendy Kusmarian 0 34 Zamrud Khatulistiwa Harga Rp 105.000 Penghimpun & Penyunting: Hendy Kusmarian WA 081.359.652.401 Tukar Rumah Keliling Indonesia http://abiysuryaonline.com Dipersembahkan untuk semua anak bangsa yang mencintai tanah air yang sangat indah ini Buku ini disusun menyambut Hari Ulang Tahun ke-73 Republik Indonesia di tahun 2018 ini. 300 halaman penuh foto warna tentang detil-detil geografis, sejarah, ekonomi, sosial, budaya, dan pariwisata dari ke-34 provinsi Indonesia. Disusun menurut abjad mulai Aceh sampai Yogyakarta. Seluruh isi buku ini bersumber dari Wikipedia bahasa Indonesia di https://id.wikipedia.org Semua anak bangsa kini bisa mendapat penghasilan ekstra dari ebook ini. Dengan mempromosikan ebook ini lewat link afiliasi unik Anda, Anda akan menerima komisi 50% untuk tiap pembelian ebook ini yang Anda hasilkan. Untuk itu Anda harus lebih dulu menjadi mitra afiliasi dari Ratakan.com, yaitu Marketplace Produk Digital Indonesia. Silakan kunjungi https://www.ratakan.com untuk membuat akun Anda gratis. Setelah itu anda bisa mulai mempromosikan dan meraup komisi dari puluhan produk digital lainnya, bukan hanya ebook ini. Tolong cetak dan jilid secara khusus ebook ini demi kenyamanan Anda dalam membaca dan agar mudah dibawa-bawa dalam petualangan Anda menjelajah negeri. 1 Daftar Isi 1. Aceh ………………………………………………………………………………………………. 3 2. Bali ………………………………………………………………………………………………... 16 3. Banten ……………………………………………………………………………………………. 24 4. Bengkulu …………………………………………………………………………………………. 34 5. Gorontalo
    [Show full text]
  • Socio-Cultural Relations Between India and Indonesia
    Proceeding of the International Seminar and Conference 2015: The Golden Triangle (Indonesia-India-Tiongkok) Interrelations in Religion, Science, Culture, and Economic. University of Wahid Hasyim, Semarang, Indonesia. August 28-30, 2015 Paper No. C.9 Socio-Cultural Relations Between India and Indonesia Mohd Tahseen Zaman Department of Islamic Studies, Jamia Millia Islamia University Jamia Nagar, New Delhi-110025, India Phone: +91(11)26981717, 26984617, 26984658, 26988044, 26987183, Fax: +91(11)2698 0229 [email protected] Abstract- India and Indonesia are two nations that from its inception, have a strong historical relation; cultural as well as intellectual. Both have some in common and similarities in many aspects. In India and Indonesia there are multiple religions, beliefs, ethnicities, languages, cultures that share and interact each other. The most interesting thing is both have shared cultural relations manifested in daily life. Some historians assumed that India‟s influence on Indonesian‟s culture is quite dominant, moreover, until the nineteenth century the Malay people received everything from India: their religion, their political system, astrology, medicine, literature, art and technical skills. Therefore this study is basically based on historical investigation and focuses on cultural analysis between Indonesia and India. Keywords: culture, shared, inception, ties Introduction The socio-cultural relations between India and Indonesia are very old. The Indian cultural impact has been seen in the all sphere of Indonesian‟s people life. They share lot of religious and cultural similarity with India. According to historical evidences the contact between India and Indonesia has been established during the beginning of the Christian era. “Traders from India, particularly from its eastern and southern coastal regions, travelled far and wide in the pursuit of trade and established trade relations with the countries of the region which is now known as Southeast Asia, and then was known as Dvipantara of Suvarndvipa.
    [Show full text]
  • Reconstruction of the 2018 Anak Krakatau Collapse Using Planetscope Imaging and Numerical Modeling
    Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Reports 2020 Reconstruction of the 2018 Anak Krakatau collapse using PlanetScope imaging and numerical modeling Davide Saviano Michigan Technological University, [email protected] Copyright 2020 Davide Saviano Recommended Citation Saviano, Davide, "Reconstruction of the 2018 Anak Krakatau collapse using PlanetScope imaging and numerical modeling", Open Access Master's Thesis, Michigan Technological University, 2020. https://doi.org/10.37099/mtu.dc.etdr/989 Follow this and additional works at: https://digitalcommons.mtu.edu/etdr Part of the Geology Commons, Geomorphology Commons, Tectonics and Structure Commons, and the Volcanology Commons RECONSTRUCTION OF THE 2018 ANAK KRAKATAU COLLAPSE USING PLANETSCOPE IMAGING AND NUMERICAL MODELING By Davide Saviano A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE In Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2020 © 2020 Davide Saviano This thesis has been approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE in Geology. Department of Geological & Mining Engineering & Sciences Thesis Co-Advisor: Dr. Simon A. Carn Thesis Co-Advisor: Dr. Gianluca Groppelli Committee Member: Dr. Roohollah R. Askari Department Chair: Dr. John S. Gierke Table of Contents Abstract ............................................................................................................................... v 1 Introduction ..............................................................................................................
    [Show full text]
  • GEOGRAFI DAN IKLIM Kabupaten Pandeglang Dalam Angka 2018| I
    GEOGRAFI DAN IKLIM Kabupaten Pandeglang Dalam Angka 2018| i Kabupaten Pandeglang Dalam Angka Pandeglang Regency in Figures 2018 ISSN: 2085-6059 No. Publikasi/Publication Number: 3601.1804 Katalog/Catalog: 1102001.3601 Ukuran Buku/Book Size: 14,8 cm x 21 cm Jumlah Halaman/Number of Pages: xxxvii + 361 halaman /pages Naskah/Manuscript: Badan Pusat Statistik Kabupaten Pandeglang BPS-Statistics of Pandeglang Regency Gambar Kover oleh/Cover Designed by: Badan Pusat Statistik Kabupaten Pandeglang BPS-Statistics of Pandeglang Regency Ilustrasi Kover/Cover Illustration: Tugu Jam, Pandeglang/ Clock Monumen, Pandeglang Diterbitkan oleh/Published by: © BPS Kabupaten Pandeglang/BPS-Statistics of Pandeglang Regency Dicetak oleh/Printed by: Percetakan Rajawali, Pandeglang Dilarang mengumumkan, mendistribusikan, mengomunikasikan, dan/atau menggandakan sebagian atau seluruh isi buku ini untuk tujuan komersial tanpa izin tertulis dari Badan Pusat Statistik Prohibited to announce, distribute, communicate, and/or copy part or all of this book for commercial purpose without permission from BPS-Statistics Indonesia ii | Pandeglang Regency in Figures 2018 GEOGRAFI DAN IKLIM PETA WILAYAH KABUPATEN PANDEGLANG MAP OF PANDEGLANG REGENCY Kabupaten Pandeglang Dalam Angka 2018| iii iv | Pandeglang Regency in Figures 2018 GEOGRAFI DAN IKLIM KEPALA BPS KABUPATEN PANDEGLANG CHIEF STATISTICIAN OF PANDEGLANG REGENCY Tri Tjahjo Purnomo, M.Si. Kabupaten Pandeglang Dalam Angka 2018| v vi | Pandeglang Regency in Figures 2018 GEOGRAFI DAN IKLIM KATA PENGANTAR Publikasi Kabupaten Pandeglang Dalam Angka 2018 merupakan publikasi rutin yang diterbitkan setiap tahun oleh BPS Kabupaten Pandeglang. Publikasi ini berisi kumpulan data yang sebagian besar merupakan data sekunder, yaitu data yang diperoleh dari Instansi, Dinas/Perusahaan baik Pemerintah maupun Swasta yang berada di wilayah Kabupaten Pandeglang.
    [Show full text]
  • 2020 Conservation Outlook Assessment
    IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Ujung Kulon National Park - 2020 Conservation Outlook Assessment Ujung Kulon National Park 2020 Conservation Outlook Assessment SITE INFORMATION Country: Indonesia Inscribed in: 1991 Criteria: (vii) (x) This national park, located in the extreme south-western tip of Java on the Sunda shelf, includes the Ujung Kulon peninsula and several offshore islands and encompasses the natural reserve of Krakatoa. In addition to its natural beauty and geological interest – particularly for the study of inland volcanoes – it contains the largest remaining area of lowland rainforests in the Java plain. Several species of endangered plants and animals can be found there, the Javan rhinoceros being the most seriously under threat. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 02 Dec 2020 GOOD WITH SOME CONCERNS The values for which Ujung Kulon National Park (UKNP) was inscribed on the World Heritage List are all still present, however, based on the situation on the ground and the assessment of the current state, some of the values of UKNP appears to be of high concern. Management is considered to be mostly effective, and has for at least the past two decades succeeded in completely averting Rhino poaching. However, the current situation of the Javan Rhino as a species is considered to be critical, and urgent and significant management intervention is required to ensure that its population is able to grow, including through the establishment of a second population elsewhere in its historic range. The main threat to the Rhino is the overabundance of the palm Arenga obtusifolia (Langkap). Experiments to control Arenga in the Javan Rhino Study and Conservation Area (JRSCA) are starting to show positive results, and in 2019 more than 200 hectares had been subject to control measures.
    [Show full text]
  • The Tale of Lampung Submerged
    The Newsletter | No.61 | Autumn 2012 8 | The Study The tale of Lampung submerged I beg you, good sirs, everyone and all, Do not deride me for erroneous recall. The reason this story I do now narrate, Is to remind all of Lampung’s sad fate.2 As the history books have recorded, one of the world’s most cataclysmic volcanic outbursts was the 1883 eruption of Mount Krakatau, situated in the Sunda Strait that separates the Indonesian islands of Sumatra and Java. The eruption nearly wiped out the entire island of Krakatau, but after a number of submarine eruptions starting in 1927 it became clear that a new island was starting to emerge in the original location. Known as Gunung Anak Krakatau (‘The Child of Krakatau’), it is, like its predecessor, an active volcano, which continues to grow consistently. Suryadi THE FIRst KNOWN MENTION of Krakatau in the West is on and the accompanying tsunami swept the shores of Sunda some works that are relatively recent, such as Simon the 1584 map by Lucas Janszoon Waghenaer, who labeled the Strait, with waves reaching heights of forty meters at the Winchester’s bestselling book, Krakatoa: The Day the area ‘Pulo Carcata’.3 Since then the name Krakatau has been var- shore, taking the lives of – to cite the words of the colonial-era World Exploded: August 27, 1883 (London: Viking, 2003), iously represented as Rakata, Krakatoa, and more rarely Krakatoe journalist, A. Zimmerman – “thirty-seven Europeans and over suggesting that interest in Krakatau is still very much and Krakatao. Its first known eruption occurred in 416 A.D.
    [Show full text]
  • Tectonic Features of the Southern Sumatra-Western Java Forearc of Indonesia
    TECTONICS, VOL. 21, NO. 5, 1047, doi:10.1029/2001TC901048, 2002 Tectonic features of the southern Sumatra-western Java forearc of Indonesia H. U. Schlu¨ter, C. Gaedicke, H. A. Roeser, B. Schreckenberger, H. Meyer, and C. Reichert Bundesanstalt fu¨r Geowissenschaften und Rohstoffe (BGR), Hannover, Germany Y. Djajadihardja Agency for the Assessment and Application of Technology (BPPT), Jakarta, Indonesia A. Prexl Veritas DGC Ltd., Crawley, UK Received 23 November 2001; revised 19 April 2002; accepted 28 May 2002; published 12 October 2002. [1] Multichannel reflection seismic profiles along the Earth: Plate boundary—general (3040); 8158 Tectonophysics: active Sunda Arc, where the Indo-Australian plate Evolution of the Earth: Plate motions—present and recent (3040); subducts under the overriding Eurasian margin 9320 Information Related to Geographic Region: Asia; KEYWORDS: revealed two accretionary wedges: The inner wedge I Indonesia, Sunda forearc, subduction, sediments, seismics, geo- is of assumed Paleogene age, and the outer wedge II is dynamics. Citation: Schlu¨ter H. U., C. Gaedicke, H. A. Roeser, of Neogene to Recent age. The inner wedge I is B. Schreckenberger, H. Meyer, C. Reichert, Y. Djajadihardja, and composed of tectonic flakes stretching from southeast A. Prexl, Tectonic features of the southern Sumatra-western Java forearc of Indonesia, Tectonics, 21(5), 1047, doi:10.1029/ Sumatra across the Sunda Strait to northwest Java, 2001TC901048, 2002. implying a similar plate tectonic regime in these areas at the time of flake development
    [Show full text]
  • Ujung Kulon National Park Indonesia
    UJUNG KULON NATIONAL PARK INDONESIA This National Park is on the Sunda Straits at the extreme southwestern tip of Java. It covers the Ujung Kulon peninsula, several offshore islands and the volcanic nature reserve of the island of Krakatau. It is one of the last remaining extensive stands of lowland rainforest in Java, and the last main habitat of the seriously threatened Javan rhinoceros. It is also a beautiful area, containing several other endangered species of plants and animals and is of geological interest, particularly for the study of volcanoes. COUNTRY Indonesia NAME Ujung Kulon National Park NATURAL WORLD HERITAGE SERIAL SITE 1991: Inscribed on the World Heritage List under Natural Criteria vii and x STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] IUCN MANAGEMENT CATEGORY Ujung Kulon National Park: II National Park Krakatau Nature Reserve: Ia Strict Nature Reserve BIOGEOGRAPHICAL PROVINCE Java (4.22.13) GEOGRAPHICAL LOCATION The Ujung Kulon National Park is a peninsula in the Sunda Straits between Java and Sumatra at the extreme southwestern tip of Java. The western boundary encloses the Ujung Kulon Peninsula, the offshore islands of Pulau Handeuleum and Pulau Peucang with the island of Pulau Panaitan 10km northwest across the Panaitan Strait, and the Krakatau Nature Reserve some 60km north across the Sunda Straits. The eastern boundary runs along the eastern foothills of the Gunung Honje massif. Ujung Kulon lies at approximately 6° 45'S by 105° 20'E and Krakatau at approximately 6° 06'S by 105° 25'E. DATES AND HISTORY OF ESTABLISHMENT 1921: Krakatau declared a Nature Reserve; 1937: Pulau Panaitan/Pulau Peucang Nature Reserve established under Decree GB/17/Stbl/420; 1958: Ujung Kulon Nature Reserve established under Decree 48/kpts/Um/4/58; 1967: Gunung Honje Nature Reserve established; 1980: Ujung Kulon Peninsula, Panaitan Island, South Gunung Honje, North Gunung Honje and the Krakatau Islands Nature Reserves proposed as a National Park.
    [Show full text]
  • Livelihood and Economic Institution Transformation: a Historical Review (A Case Study at Coastal Fishing Community of Ujung Kulon)
    Jan. 2015. Vol. 4, No.9 ISSN 2307-227X International Journal of Research In Social Sciences © 2013-2015 IJRSS & K.A.J. All rights reserved www.ijsk.org/ijrss LIVELIHOOD AND ECONOMIC INSTITUTION TRANSFORMATION: A HISTORICAL REVIEW (A CASE STUDY AT COASTAL FISHING COMMUNITY OF UJUNG KULON) MIRAJIANI1, EKAWATI SRI WAHYUNI2, ARIF SATRIA2, SAHARUDDIN2, TRIDOYO KUSUMASTANTO3 1 Doctor Candidate, Study Program of Rural Sociology, Bogor Agricultural University, Bogor, Indonesia 2Lecturer, Bogor Agricultural University, Bogor, Indonesia 3Prof, Bogor Agricultural University, Bogor, Indonesia E-mail : [email protected] ABSTRACT Development program in fishing village has an impact on livelihood and economic institution transformation of coastal fishing community in Ujung Kulon, Banten Province, Indonesia. The research aims to study the livelihood and economic institution transformation occurred in coastal fishing community through historical review related to development process that change the society’s economic system as a whole. Research method used is qualitative research with research type of study case. Research result found that fishing community has undergone livelihood transformation as a part of social transformation occurred as an impact of development. The livelihood transformation consists of livelihood change in some of the society from subsistence farmer and forest product collector into various livelihood societies. Livelihood strategy is applied through multiple livelihood patterns where fishing is combined with other livelihoods. In addition, fisherman households develop livelihood strategy based on the utilization of productive employment in their household (multiple actors or straddling strategy); where each member of the fisherman household has role in the livelihood. Further, fishing community at Ujung Kulon coastal area changes the economic institution as an adaptive mechanism required for society in the social transformation process occurred.
    [Show full text]
  • Krakatau: Genetic Consequences of Island Colonization
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Utrecht University Repository Krakatau: genetic consequences of island colonization (Krakatau: genetische gevolgen van eiland kolonisatie) (met een samenvatting in het Nederlands) Proefschrift ter verkrijging van de graad van doctor aan de Universiteit Utrecht op gezag van de Rector Magnificus, Prof Dr. W.H. van Gispen, ingevolge het besluit van het College voor Promoties in het openbaar te verdedigen op maandag 13 Mei 2002 des middags te 12:45 uur door Tracey Louise Parrish geboren op 9 juni 1971 te Nowra, Australië Promotor: Prof.dr. J. M. M. van Damme Faculteit Biologie Universiteit Utrecht Copromotors: Dr P.J van Dijk en Dr H.P. Koelewijn Nederlands Instituut voor Ecologie Centrum voor Terrestrische Ecologie, Heteren Printed by Ponsen and Looijen BV, Wageningen, The Netherlands ISBN 90-6464-952-9 The research in this thesis was carried out at the department of Plant Population Biology at the Netherlands Institute of Ecology-Center for Terrestrial Ecology, Heteren and was funded through the ‘Biodiversity in Disturbed Ecosystems’ priority program of the Netherlands Organization for Scientific Research (NWO). This thesis is for Mum and dedicated to Dad. Visit http://www.krakatau.org Email: [email protected] Contents Chapter 1 General introduction. 1 Chapter 2 Genetic diversity in five tree species on the Krakatau islands: 116 years after forest destruction and recolonization. (submitted to Molecular Ecology) 25 Chapter 3 Genetic differentiation in five tree species in sites from Java, Sumatra and Krakatau: inferences about gene flow between isolated populations. 59 Chapter 4 Genetic evidence for natural hybridization between species of dioecious Ficus on island populations 83 (with M.
    [Show full text]
  • The Morphological Development of Krakatau Volcano, Sunda Strait, Indonesia
    THE MORPHOLOGICAL DEVELOPMENT OF KRAKATAU VOLCANO, SUNDA STRAIT, INDONESIA BY ADJAT SUDRl,'DJA T '3 0 p.,UG 198(1 THE MORPHOLOGICAL DEVELOPMENT OF KRAKATAU VOLCANO, SUNDA STRAIT, INDONESIA BY ADJAT SUD!UJ'DJAT r , BJDANG BmLJOGRAFI DAN DEPOSIT Tanggal : . Group I \ THE MORPHOLOGICAL DEVELOP1~ENT OF KRAKATAU VOLCANO 1 SUNDA STRAIT, INDONESIA ) by 2) Adj at Sudradj at ABSTRACT A morphologic development of Anak Krakatau after the 1883 Plinian eruption was studied based on the available bathymetric charts (Verbeek, 1885; Symo ns, 1888; Escher, 1919) and terres­ trial surveys 1arried o ut by the Vo lcanological Survey of Indo­ nesia. Additio jal information ",· a5 also gathered from t.ne .. ae..x-~ .~'l. ~ .phO~ . t 03r aphic interpretation of th ~ a rea. Within the first 30 ye a r . (1888-1919) after the eruption no sig nificant changes of. the s eafloor configuration have beentdQ.ticed . around Krakatau isl and complex. The submarin'e crater's bottom see mina1y sho wed a deepening o f a ~pr o ximately 20 meters perhaps clo sely relatedwiththe cODpacti ~ n and bedding · in of the volca- nic deposits filled in the crater. The volcanic depvsits prcdu- ced by the newly-bo rn Anak Kray. atau volcano filled in particular­ ly the northe ast e rn upper inner slope of the craterwiti1a rate next o f 1 t o 3.5 0 a nnua lly d urin:; tho ;'l0 year period (1-9J.9··1940). A study on the morphologic development of Anak Krakatnu since i t s birth p h a se .(1927-19 30 ) t o February 1981 revealed the· _ chang es of elevatio n and size of Anak Krakatau Island.
    [Show full text]