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Concise Ancient History of Indonesia.Pdf
CONCISE ANCIENT HISTORY OF INDONESIA CONCISE ANCIENT HISTORY O F INDONESIA BY SATYAWATI SULEIMAN THE ARCHAEOLOGICAL FOUNDATION JAKARTA Copyright by The Archaeological Foundation ]or The National Archaeological Institute 1974 Sponsored by The Ford Foundation Printed by Djambatan — Jakarta Percetakan Endang CONTENTS Preface • • VI I. The Prehistory of Indonesia 1 Early man ; The Foodgathering Stage or Palaeolithic ; The Developed Stage of Foodgathering or Epi-Palaeo- lithic ; The Foodproducing Stage or Neolithic ; The Stage of Craftsmanship or The Early Metal Stage. II. The first contacts with Hinduism and Buddhism 10 III. The first inscriptions 14 IV. Sumatra — The rise of Srivijaya 16 V. Sanjayas and Shailendras 19 VI. Shailendras in Sumatra • •.. 23 VII. Java from 860 A.D. to the 12th century • • 27 VIII. Singhasari • • 30 IX. Majapahit 33 X. The Nusantara : The other islands 38 West Java ; Bali ; Sumatra ; Kalimantan. Bibliography 52 V PREFACE This book is intended to serve as a framework for the ancient history of Indonesia in a concise form. Published for the first time more than a decade ago as a booklet in a modest cyclostyled shape by the Cultural Department of the Indonesian Embassy in India, it has been revised several times in Jakarta in the same form to keep up to date with new discoveries and current theories. Since it seemed to have filled a need felt by foreigners as well as Indonesians to obtain an elementary knowledge of Indonesia's past, it has been thought wise to publish it now in a printed form with the aim to reach a larger public than before. -
Dutch Donors Hand Over More Than 600 UN-HABITAT Houses on the Remote Island of Simeulue
United Nations Human Settlements Programme Programme des Nations Unies pour les établissements humains INDONESIA JL. T.M. Pahlawan No. 3A, Banda Aceh, Telephone : +62 651 25258 PRESS RELEASE Dutch donors hand over more than 600 UN-HABITAT houses on the remote island of Simeulue Sambai, Simeulue Island, Indonesia, 5 July – In a joyful ceremony in Sambai village on Simeulue Island UN-HABITAT, UNDP and the Aceh Rehabilitation and Reconstruction Agency celebrated the completion of houses together with Dutch donors and survivors of the Indian Ocean Tsunami. Daniel Biau (UN-HABITAT,right) and Simon Field (UNDP) plant a tree in front of a reconstructed house The director of the Regional and Technical Cooperation Division Nairobi, Daniel Biau, who visited Aceh Province to commemorate two years of UN-HABITAT’s and UNDP’s Aceh Nias Settlements Support Programme praised the successful collaboration work between UN- HABITAT, UNDP, the Aceh Nias Rehabilitation and Reconstruction Agency (BRR) and the people of Simeulue and their local authorities. The Aceh Nias Settlements Support Programme (ANSSP) has so far completed reconstruction of 3,500 houses and more than 1,000 are currently under construction in cooperation with the Asian Development Bank (ADB). In Simeulue, an island off the west coast of Sumatra, the recovery process has been particularly challenging. On the remote island the number of casualties was relatively small, because oral tradition had passed on the knowledge that people must run uphill after earthquakes to avoid tsunami waves. However, the destruction, which the disaster had left behind, was overwhelming. Whole villages had been wiped out. The shipment of material by sea and on the few bad roads was difficult and skilled workers were hard to find. -
Fujinoetal-Margeo-Simeulue.Pdf
Marine Geology 357 (2014) 384–391 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Ambiguous correlation of precisely dated coral detritus with the tsunamis of 1861 and 1907 at Simeulue Island, Aceh Province, Indonesia Shigehiro Fujino a,⁎, Kerry Sieh b,1, Aron J. Meltzner b,1,EkoYuliantoc, Hong-Wei Chiang d,1 a Active Fault and Earthquake Research Center, National Institute of Advanced Industrial Science and Technology (AIST), Site C7 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan b Tectonics Observatory, California Institute of Technology, Pasadena, CA 91125, USA c Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung, Indonesia d High-precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan, ROC article info abstract Article history: Precise U–Th dates from coral detritus in two pre-2004 tsunami deposits on Simeulue Island in Aceh Province Received 7 March 2014 allow us to correlate the deposits with historically documented tsunamis in the recent few centuries, but because Received in revised form 19 September 2014 of potential discordance between the death dates of the corals and deposition of the sand layers, ambiguity in this Accepted 28 September 2014 correlation remains. Pits at coastal lowland sites exposed sand layers beneath the 2004 tsunami deposit at Available online 22 October 2014 Busung and Naibos on southern Simeulue Island. The layers share sedimentological characteristics with the de- Communicated by J.T. Wells posit of the 2004 tsunami, and are interpreted as pre-2004 tsunami deposits. Historical accounts document earth- quakes and tsunamis in 1907 and 1861 and suggest that the 1907 tsunami was larger locally than any others Keywords: historically. -
Ecosystem Approach to Disaster Risk Reduction Ecosystem Approach to Disaster Risk Reduction
Towards a disaster free India Ecosystem Approach to Disaster Risk Reduction Ecosystem Approach to Disaster Risk Reduction Edited by Anil K. Gupta Sreeja S. Nair National Institute of Disaster Management (Ministry of Home Affairs, Govt. of India) Towards a disaster free India IIPA Campus, New Delhi - 110 002 India Copyright @NIDM, 2012. Contents of the book can be freely used, cited, translated and referred in any academic, research and capacity development purpose with proper citation of this publication and the respective chapter contributors. Citation Gupta, Anil K. and Nair, Sreeja S. (2012). Ecosystem Approach to Disaster Risk Reduction, National Institute of Disaster Management, New Delhi, Pages 202 International Training-Workshop Organized by NIDM, UN-PEDRR, UNEP, IUCN, CADRI, UNDP Published by National Institute of Disaster Management, New Delhi Ecosystem Approach to Disaster Risk Reduction iii Foreword Available data regarding disasters and their impacts during last decade clearly indicate an exponential increase in the vulnerability of the society and land to disasters Environmental degradation epitomized by deforestation, loss of biodiversity, deterioration of drainage pattern, unscientific development, etc have been some of the major factors for the increased vulnerability of the society and the land to natural disasters besides aggravating their causative hazards. The capacity of a society to resist the impact of these forces decides the degree of loss to it by hazard and this depends on the precautions the society has taken during various stages of development. Thus, disasters are inextricably linked to the development and it is up to an extent on how the development pattern takes concern of environment. -
The Indian Ocean Tsunami: Economic Impact, Disaster Management and Lessons
The Indian Ocean Tsunami: Economic Impact, Disaster Management and Lessons Prema-chandra Athukorala and Budy P. Resosudarmo Division of Economics Research School of Pacific and Asian Studies Australian National University E-mail: [email protected] [email protected] Abstract: The purpose of this paper is to document and analyze the immediate economic impact of the Indian Ocean tsunami generated by the Sumatra-Andaman earthquake of 26 December 2004 and the disaster management process in the immediate aftermath of the disaster with a focus on the two worst affected countries – Indonesia (Aceh province) and Sri Lanka. The 26 December Tsunami is unique among large disasters in recorded human history, not only because of the sheer number of causalities and massive displacement of people, but also because of the unprecedented international donor response and the logistic challenges faced by international organizations and aid agencies in organizing and coordinating relief efforts. Our preliminary findings points to the importance of educating the public about simple precautions in the event of a disaster and enforcement of coastal environmental regulations as disaster prevention policies. The findings also makes a strong case for designing policies and programs, as an integral part of national development strategy, for mitigating the impact of natural disasters on the poor and highlights the need for combining international aid commitments with innovative approaches to redressing problems of limited aid absorptive capacity in disaster affected countries. Key Words: tsunami, disaster management, Indonesia, Sri Lanka JEL Classification: I32, O53 Q54 Forthcoming in Asian Economic Papers 1 2 The Indian Ocean Tsunami: Economic Impact, Disaster Management and Lessons∗ Sociologist, psychologists, historians, and policy planners have all devoted considerable attention to the nature, sources, and consequences of disaster and recovery, but the professional economic literature is distressingly sparse. -
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International Seminar for UNESCO Integral Study of the Silk Roads: Roads of Dialogue: “India and the Roman world between 1st and 4th Century A.D.”, “India’s Cultural Relationship with East and Southeast Asia during the 4th to 13th Century A.D.”. 19-24 December 1990. Madras, India. Trade Contacts with the Indonesian Archipelago: 6th to 14th Centuries E. Edwards McKinnon Sea routes from South India and Sri Lanka to the Indonesian islands of Sumatra, Java, Bali, Kalimantan, Sulawesi and beyond appear to have been established by the beginning of the Christian era. Tangible evidence for such contacts appears in the form of Romano-Indian rouletted ware of the first or second centuries A.D. found in the Buni area of West Java (Walker & Santoso 1977) and, more recently, from controlled excavations at Sembiran on the north coast of Bali (Ardika 1989). An early bronze Buddha of Amaravati type from Sulawesi indicates possible connections with Sri Lanka by the c5. Evidence of Indianising influences, from Sanskrit inscriptions written in Tamil Grantha characters of the early/mid fifth century, appears in East Kalimantan and West Java. Monsoons: the crossing of the Oceans. The monsoon winds, which carried ships across the Indian Ocean, blow for six months of the year in one direction and for the other six in the opposite way. Although the changeover periods are somewhat squally, with unsteady winds, the monsoons themselves provide favorable conditions to blow ships from Arabia to China and back. From the end of October to January or February, the northeast monsoon carried ships from Java and Sumatra to Sri Lanka and South India in relatively fine weather. -
Draft GHI Guide
Preparing Your Community for Tsunamis A Guidebook for Local Advocates page 1 GHI Tsunami Guidebook, DRAFT April 5 2007 Simeulue Island: Local Knowledge Saves Lives On December 26, 2004 a tsunami, caused by a large earthquake under the sea off of Indonesia, spread throughout the Indian Ocean. It killed over 230,000 people in Indonesia, Thailand, India, Sri Lanka and elsewhere and destroyed the homes and livelihoods of many more. That day Simeulue Island, Indonesia was one of the many places inundated with the tsunami’s destructive waves. But the tsunami’s impact in Simuelue Island was not like what happened in other places: only seven people were killed by the tsunami in Simeulue out of a population of nearly 80,000. Why? Because the island’s residents had passed down stories about earlier tsunamis to strike the island, warning people to head to high ground if they felt strong earthquake shaking. These stories were known to most island residents from childhood. And on December 26, people on the island followed the guidance of these stories and saved their lives. The earthquake that triggered the 2004 mega-tsunami was centered only 40 kilometers away from the northern part of Simeulue. The first tsunami waves struck the northern coast of the island about ten minutes after the earthquake and caused widespread damage to buildings, which had already been evacuated. In 2004, no official tsunami warning system was in place for Simeulue, or any other part of the Indian Ocean. But even if one had existed, it would have been unlikely to warn the island’s residents quickly enough to evacuate people before the first waves struck. -
Postseismic Slip Following the 2005 Nias-Simeulue, Sumatran Indonesia Earthquake
Postseismic slip following the 2005 Nias-Simeulue, Sumatran Indonesia earthquake Ya-Ju Hsu1, Mark Simons1, Jean-Philippe Avouac1, Kerry Sieh1, John Galetzka1, Yehuda Bock2, Danny Natawidjaja3 and Linette Prawirodirdjo2 1. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. 2. Institute of Geophysics and Planetary Physics, University of California San Diego, California, U.S.A. 3. Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung, Indonesia. Abstract The March 28, 2005 Nias-Simeulue Mw 8.7 earthquake ruptured the plate boundary megathrust on the northwest coast of Sumatra, southeast of the December 26, 2004 Mw 9.1 Aceh-Andaman earthquake. The availability of 3-component continuous GPS data and microatoll observations of vertical displacements for this event, all located above or near the region of coseismic rupture, permits us to address a disparate suite of questions regarding the mechanical nature of the megathrust. For the first time, we unambiguously determine that significant post-seismic slip occurred updip from the coseismic rupture, consistent with the notion that the shallow-most portions of the subduction interface primarily slips aseismically. Generally, the regions of major coseismic and postseismic slip are mutually exclusive and after 9 months many portions of the megathrust are still slipping at rates several times the long-term average interseismic rate. The observed relationship between the spatial and temporal evolution of cumulative postseismic displacement and the cumulative number of aftershocks is consistent with a model in which the location and number of aftershocks is driven by induced afterslip and not directly by coseismic stress changes. -
Downloaded from Brill.Com09/30/2021 05:45:05PM Via Free Access 100 Research Note
Bijdragen tot de Taal-, Land- en Volkenkunde 170 (2014) 99–106 bki brill.com/bki Research Note ∵ A Wall in the Woods* Note on the Recently Discovered Site at Kreung Jeureungeh, North Aceh R. Michael Feener Visiting Associate Professor, Department of Near Eastern Languages and Civilizations, Harvard University, Cambridge, MA [email protected] Abstract This short note presents a preliminary report on a recently discovered site in North Aceh. It presents some initial information and illustrations of an usual stone formation, and communicates some potential readings of it drawing on perspectives from geog- raphy, vulcanology, and the broader archaeological and historical contexts of northern Sumatra. Keywords Indonesia – Sumatra – Aceh – archaeology – history This brief note is to call attention to a recent find at a previously unknown site in northeast Sumatra.The broad area stretching between the modern cities of Medan and Banda Aceh is known for some particularly rich archaeological sites, including a number of Hoabinhian shell middens (McKinnon 1991), and * I would like to thank Nanda Amalia, Oskar Jailani, Geuchik Abdul Manaf, Mukhtar, Qamarul- lah and Yus from Sawang for their help in accessing the site. I am also grateful to John Miksic, © r. michael feener, 2014 | doi: 10.1163/22134379-17001006 This is an open access article distributed under the terms of the Creative Commons Attribution-Noncommercial 3.0 Unported (CC-BY-NC 3.0) License. Downloaded from Brill.com09/30/2021 05:45:05PM via free access 100 research note figure 1 The ‘wall’ at Kreung Jeureungeh an extensive collection of medieval Muslim tombstones at Pasai, just outside Lhokseumawe, North Aceh (Guillot and Kalus 2008). -
TRADISI LISAN NANDONG SIMEULUE: PENDEKATAN ANTROPOLINGUISTIK DISERTASI Oleh TASNIM LUBIS
TRADISI LISAN NANDONG SIMEULUE: PENDEKATAN ANTROPOLINGUISTIK DISERTASI Oleh TASNIM LUBIS NIM: 158107006 PROGRAM DOKTOR (S3) LINGUISTIK FAKULTAS ILMU BUDAYA UNIVERSITAS SUMATERA UTARA MEDAN 2019 TRADISI LISAN NANDONG SIMEULUE: PENDEKATAN ANTROPOLINGUISTIK DISERTASI Diajukan sebagai salah satu syarat untuk memperoleh gelar doktor dalam Program Doktor Linguistik pada Fakultas Ilmu Budaya Universitas Sumatera Utara di bawah pimpinan Rektor Universitas Sumatera Utara Prof. Dr. Runtung Sitepu, S.H., M.Hum. untuk dipertahankan di hadapan sidang Terbuka Senat Universitas Sumatera Utara Oleh TASNIM LUBIS NIM: 158107006 Program Doktor (S3) Linguistik FAKULTAS ILMU BUDAYA UNIVERSITAS SUMATERA UTARA MEDAN 2019 Diuji pada Ujian Disertasi Terbuka (Promosi) Tanggal: 14 Januari 2019 PANITIA PENGUJI DISERTASI Pemimpin Sidang: Prof. Dr. Runtung Sitepu, SH., M.Hum. (Rektor USU) Ketua : Prof. Dr. Robert Sibarani, M.S. (USU Medan) Anggota : Prof. Dr. Syahron Lubis, M.A. (USU Medan) Dr. Phil. Ichwan Azhari, M.S. (UNIMED Medan) Dr. Eddy Setia, M.Ed.TESP. (USU Medan) Dr. Mulyadi, M.Hum. (USU Medan) Dr. Dwi Widayati, M.Hum. (USU Medan) Dr. Bukhari Daud, M.Ed. (UNSYIAH Banda Aceh) TRADISI LISAN NANDONG SIMEULUE: PENDEKATAN ANTROPOLINGUISTIK ABSTRAK Nandong Simeulue (NS) adalah tradisi lisan dalam masyarakat Simeulue berupa pantun dan puisi yang mengandung nasehat-nasehat dan cerita-cerita. Untuk menganalisis tradisi lisan NS, digunakan pendekatan antropolinguistik yang merupakan interdisipliner antara bahasa dan perilaku (praktik) berbicara. Dengan menggunakan parameter antropolinguistik yaitu keterhubungan, kebernilaian dan keberlanjutan, maka penelitian ini bertujuan untuk mendeskripsikan performansi NS, mengevaluasi kandungan tradisi lisan NS, dan menemukan model revitalisasinya agar NS dapat dilestarikan dan diwariskan kepada generasi penerus. Metode yang digunakan adalah metode etnografi yang dikemukakan oleh Spradley. -
Sibling Earthquakes Generated Within a Persistent Rupture Barrier on the Sunda Megathrust Under Simeulue Island
Geophysical Research Letters RESEARCH LETTER Sibling earthquakes generated within a persistent 10.1002/2016GL071901 rupture barrier on the Sunda megathrust Key Points: under Simeulue Island • The 2002 Mw 7.3 and 2008 Mw 7.4 Simeulue earthquakes are “sibling” 1 1 1 1 1 earthquakes that resemble each Paul M. Morgan , Lujia Feng , Aron J. Meltzner , Eric O. Lindsey , Louisa L. H. Tsang , other and largely overlap and Emma M. Hill1,2 • These two ruptures slipped an isolated, locked asperity within a 1Earth Observatory of Singapore, Nanyang Technological University, Singapore, 2Asian School of the Environment, persistent rupture barrier to great Nanyang Technological University, Singapore earthquakes • The rupture terminations and seismic asperity under Simeulue may be structurally controlled by Abstract A section of the Sunda megathrust underneath Simeulue is known to persistently halt a subducting morphological high rupture propagation of great earthquakes, including those in 2004 (Mw 9.2) and 2005 (Mw 8.6). Yet the of the slab same section generated large earthquakes in 2002 (Mw 7.3) and 2008 (Mw 7.4). To date, few studies have investigated the 2002 and 2008 events, and none have satisfactorily located or explained them. Using Supporting Information: near-field InSAR, GPS, and coral geodetic data, we find that the slip distributions of the two events are • Supporting Information S1 not identical but do show a close resemblance and largely overlap. We thus consider these earthquakes •DataSetS1 •DataSetS2 “siblings” that were generated by an anomalous “parent” feature of the megathrust. We suggest that •DataSetS3 this parent feature is a locked asperity surrounded by the otherwise partially creeping Simeulue section, •DataSetS4 perhaps structurally controlled by a broad morphological high on the megathrust. -
The Northern Sumatra Earthquake of March 28, 2005
EERI Special Earthquake Report — August 2005 Learning from Earthquakes The Northern Sumatra Earthquake of March 28, 2005 Editor’s Note: Beginning with the killed around 1,000 people while they occurred. Right after the earth- March issue and in each one sub- were either sleeping or trying to run quake, electric power was cut off sequently, we presented six reports from the second and third fl oors. In and telecommunication disrupted. by the many teams that observed Simeulue, some house shops col- In Gunung Sitoli and Teluk Dalam, the effects of the December 26, lapsed, and about 100 people were Nias, the damage was concentrated 2004, earthquake and tsunami in killed. There was a rush to exit in certain areas close to the beach. countries around the Indian Ocean. houses and run to higher places be- In Simeulue the damage was also This report adds information on cause the people feared a tsunami concentrated in areas close to the structural damage, largely from similar to that of December 26, 2004. beach. Strong aftershocks (32 km shaking, on two islands west of There was a local tsunami, but not from Gunung Sitoli [M 6.0] and 41 Sumatra in a subsequent large of the size or ferocity of the previous km from Sinabang (M 5.5]) did not earthquake in roughly the same one. cause any further damage to either epicentral area as the December damaged or undamaged buildings. quake. Publication of this report is Nias Island is part of North Sumatra supported by funds from the Na- Province and Simeulue Island is part tional Science Foundation through of Aceh Province.