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Banda Islands, Indonesia
INSULARITY AND ADAPTATION INVESTIGATING THE ROLE OF EXCHANGE AND INTER-ISLAND INTERACTION IN THE BANDA ISLANDS, INDONESIA Emily J. Peterson A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2015 Reading Committee: Peter V. Lape, Chair James K. Feathers Benjamin Marwick Program Authorized to Offer Degree: Anthropology ©Copyright 2015 Emily J. Peterson University of Washington Abstract Insularity and Adaptation Investigating the role of exchange and inter-island interaction in the Banda Islands, Indonesia Emily J. Peterson Chair of the Supervisory Committee: Professor Peter V. Lape Department of Anthropology Trade and exchange exerted a powerful force in the historic and protohistoric past of Island Southeast Asian communities. Exchange and interaction are also hypothesized to have played an important role in the spread of new technologies and lifestyles throughout the region during the Neolithic period. Although it is clear that interaction has played an important role in shaping Island Southeast Asian cultures on a regional scale, little is known about local histories and trajectories of exchange in much of the region. This dissertation aims to improve our understanding of the adaptive role played by exchange and interaction through an exploration of change over time in the connectedness of island communities in the Banda Islands, eastern Indonesia. Connectedness is examined by measuring source diversity for two different types of archaeological materials. Chemical characterization of pottery using LA-ICP-MS allows the identification of geochemically different paste groups within the earthenware assemblages of two Banda Islands sites. Source diversity measures are employed to identify differences in relative connectedness between these sites and changes over time. -
Ambon – Banda Sea – Alor- Maumere
DAY ITINERARY WITH MV MERMAID I BIODIVERSITY SPECIAL RING DIVES OF FIRE – AMBON – BANDA SEA – ALOR- MAUMERE DAY 1 Check-in on board Mermaid I. After arriving at Ambon and a safety briefing. You will do dives two dives at Ambon Bay in some fabulous muck dives with critters galore. This area is known for many rare and unusual species including the psychedelic frogfish and 2 Rhinopias. DAY 2-3 The next two days will be spent in the Banda Islands, formerly known as the Spice dives Islands. Many of the dive sites around the Banda islands are wall dives. The walls are covered in massive gorgonians, soft corals, barrel sponges and have some very 7 interesting swim throughs. But there are other attractive dive sites such as pinnacles with enormous groups of schooling pyramid butterflyfish, triggerfish and pelagic fishes such as tunas passing through, spectacular hard coral reefs next to the volcano, and great muck dives with lots of mandarin fish at the local jetty. The Banda Islands are much more than diving. It is also a cultural and historical experience. You will spend one morning walking around the village of Banda Neira the main island, with a local guide, visiting the local museum, the old Dutch fort, the old colonial governor’s house, the local fish market and a nutmeg plantation, where you will have breakfast. DAY 4 Manuk – Snake Volcano – sometimes has more snakes than Gunung Api. Still no need dives to be afraid! The site also offers a black sand reef dive with loads of fish and pretty hard corals. -
Ocean Wave Characteristics in Indonesian Waters for Sea Transportation Safety and Planning
IPTEK, The Journal for Technology and Science, Vol. 26, No. 1, April 2015 19 Ocean Wave Characteristics in Indonesian Waters for Sea Transportation Safety and Planning Roni Kurniawan1 and Mia Khusnul Khotimah2 AbstractThis study was aimed to learn about ocean wave characteristics and to identify times and areas with vulnerability to high waves in Indonesian waters. Significant wave height of Windwaves-05 model output was used to obtain such information, with surface level wind data for 11 years period (2000 to 2010) from NCEP-NOAA as the input. The model output data was then validated using multimission satellite altimeter data obtained from Aviso. Further, the data were used to identify areas of high waves based on the high wave’s classification by WMO. From all of the processing results, the wave characteristics in Indonesian waters were identified, especially on ALKI (Indonesian Archipelagic Sea Lanes). Along with it, which lanes that have high potential for dangerous waves and when it occurred were identified as well. The study concluded that throughout the years, Windwaves-05 model had a magnificent performance in providing ocean wave characteristics information in Indonesian waters. The information of height wave vulnerability needed to make a decision on the safest lanes and the best time before crossing on ALKI when the wave and its vulnerability is likely low. Throughout the years, ALKI II is the safest lanes among others since it has been identified of having lower vulnerability than others. The knowledge of the wave characteristics for a specific location is very important to design, plan and vessels operability including types of ships and shipping lanes before their activities in the sea. -
Regional Maritime Issues, Can the Indian Ocean Be Collaboratively Managed?
Regional Maritime Issues, Can the Indian Ocean be Collaboratively Managed? First Admiral Anuar bin Mohamed Assistant Chief of Staff Human Resource, Royal Malaysian Navy Can the Indian Ocean be Collaboratively Managed? It covers an area of 68.556 million sq km, which includes amongst others, the Andaman The Hypothesis: Collaboration could not be Sea, Arabian Sea, Bay of Bengal, Flores Sea, fully achieved in IOR, as long as there is a great Great Australian Bight, Gulf of Aden, Gulf of power politics that enhance the geopolitical and Oman, Java Sea, Mozambique Channel, Persian geostrategic struggles in the region. Gulf, Red Sea, Savu Sea, Strait of Malacca and Timor Sea. This is viewed through the lens of neo-realism, where the structural defects would eventually By comparison, it consists of an area that is make efforts for collaboration/cooperation almost 7 times the size of the United States. impossible. Bordering this ocean and the states around it is the 66,526 km coastlines. In arguing this, we need to understand the features of the IOR iot determined factors that In a nutshell, it covers 30% of the global ocean would affect the argument. area home to 30% of the world’s population and 30% of the world’s coral reef cover. Background Geographically : Economically: This ocean hosts abundant of natural Indian Ocean Region (IOR) has unique resources of oil and gas fields, fish, shrimp, characteristics compared to other oceanic sand and gravel aggregates, placer deposits and regions. poly-metallic nodules. It is the third largest of the world's five oceans, It also provide various major sea routes after the Pacific and the Atlantic Ocean. -
Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
An Atlas of Oceanic Internal Solitary Waves (February 2004) Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Indonesian Seas • Bali Sea • Flores Sea • Molucca Sea • Banda Sea • Java Sea • Savu Sea • Cream Sea • Makassar Strait Overview The Indonesian Seas are the regional bodies of water in and around the Indonesian Archipelago. The seas extend between approximately 12o S to 3o N and 110o to 132oE (Figure 1). The region separates the Pacific and Indian Oceans. Figure 1. Bathymetry of the Indonesian Archipelago. [Smith and Sandwell, 1997] Observations Indonesian Archipelago is most extensive archipelago in the world with more than 15,000 islands. The shallow bathymetry and the strong tidal currents between the islands give rise to the generation of internal waves throughout the archipelago. As a result there are a very 453 An Atlas of Oceanic Internal Solitary Waves (February 2004) Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO large number of internal wave sources throughout the region. Since the Indonesian Seas boarder the equator, the stratification of the waters in this sea area does not change very much with season, and internal wave activity is expected to take place all year round. Table 2 shows the months of the year during which internal waves have been observed in the Bali, Molucca, Banda and Savu Seas Table 1 - Months when internal waves have been observed in the Bali Sea. (Numbers indicate unique dates in that month when waves have been noted) Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec 12111 11323 Months when Internal Waves have been observed in the Molucca Sea. -
Structural and Stratigraphic Evolution of the Savu Basin, Indonesia
Structural and stratigraphic evolution of the Savu Basin, Indonesia JAMES W. D. RIGG* & ROBERT HALL SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK *Corresponding author (e-mail: [email protected]) Abstract: The Savu Basin is located in the Sunda–Banda fore-arc at the position of change from oceanic subduction to continent–arc collision. It narrows eastward and is bounded to the west by the island of Sumba that obliquely crosses the fore-arc. New seismic data and published geological observations are used to interpret Australia–Sundaland convergence history. We suggest the basin is underlain by continental crust and was close to sea level in the Early Miocene. Normal faulting in the Middle Miocene and rapid subsidence to several kilometres was driven by subduction rollback. Arc-derived volcaniclastic turbidites were transported ESE, parallel to the Sumba Ridge, and then NE. The ridge was elevated as the Australian continental margin arrived at the Banda Trench, causing debris flows and turbidites to flow northwards into the basin which is little deformed except for tilting and slumping. South of the ridge fore-arc sediments and Australian sedimentary cover were incorporated in a large accretionary complex formed as continental crust was thrust beneath the fore-arc. This is bounded to the north by the Savu and Roti Thrusts and to the south by a trough connecting the Java Trench and Timor Trough which formed by south-directed thrust- ing and loading. The Savu Basin is situated in the fore-arc of the Roti and the Savu Basin connects the Timor Trough Sunda–Banda Arc (Fig. -
Observed Estimates of Convergence in the Savu Sea, Indonesia James T
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. C1, 3001, doi:10.1029/2002JC001507, 2003 Observed estimates of convergence in the Savu Sea, Indonesia James T. Potemra,1 Janet Sprintall,2 Susan L. Hautala,3 and Wahyu Pandoe4,5 Received 11 June 2002; revised 25 September 2002; accepted 10 October 2002; published 2 January 2003. [1] The Indonesian seas are known to be a region where various Pacific and Indian Ocean water masses converge and are transformed into uniquely characterized Indonesian Sea Water (ISW). The volume of Pacific surface waters that are stored in the Indonesian seas and the timescales for this volume to change are important factors in the formulation of ISW that ultimately enters the Indian Ocean as the Indonesian throughflow (ITF). In this study, data from a recent deployment of pressure gauges surrounding the Savu Sea are used to estimate volume, heat, and freshwater convergence within approximately the upper 100 m. A pair of gauges on the northeastern side (North Ombai and South Ombai) is used to estimate inflow from the Banda Sea through the Ombai Strait, and two pairs (Sumbawa/North Sumba and South Sumba/Roti) are used to estimate outflow to the Indian Ocean via the Sumba and Savu/Dao Straits. The data are used in conjunction with numerical model results to show that at times, for example, November and December of 1996, there can be up to a 10 Sv imbalance between the inflow and the outflow transport. Most of the variability in estimated convergence occurs intraseasonally and seems to be controlled by the flow through the Sumba Strait on the eastern side of the sea. -
Bay of Bengal: from Monsoons to Mixing Ocethe Officiala Magazinen Ogof the Oceanographyra Societyphy
The Oceanography Society Non Profit Org. THE OFFICIAL MAGAZINE OF THE OCEANOGRAPHY SOCIETY P.O. Box 1931 U.S. Postage Rockville, MD 20849-1931 USA PAID Washington, DC ADDRESS SERVICE REQUESTED Permit No. 251 OceVOL.29, NO.2,a JUNEn 2016 ography Register now to attend this conference for international scientific profes- sionals and students. Virtually every facet of ocean color remote sensing and optical oceanography will be presented, including basic research, technological development, environmental management, and policy. October 23–28, 2016 | Victoria, BC, Canada Registration is open! The oral presentation schedule is available on the conference website Submission of abstracts for poster presentation remains open through summer 2016. www.oceanopticsconference.org Bay of Bengal: From Monsoons to Mixing OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Susanto, R.D., Z. Wei, T.R. Adi, Q. Zheng, G. Fang, B. Fan, A. Supangat, T. Agustiadi, S. Li, M. Trenggono, and A. Setiawan. 2016. Oceanography surrounding Krakatau Volcano in the Sunda Strait, Indonesia. Oceanography 29(2):264–272, http://dx.doi.org/10.5670/oceanog.2016.31. DOI http://dx.doi.org/10.5670/oceanog.2016.31 COPYRIGHT This article has been published in Oceanography, Volume 29, Number 2, a quarterly journal of The Oceanography Society. Copyright 2016 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA. -
Indonesia's Transformation and the Stability of Southeast Asia
INDONESIA’S TRANSFORMATION and the Stability of Southeast Asia Angel Rabasa • Peter Chalk Prepared for the United States Air Force Approved for public release; distribution unlimited ProjectR AIR FORCE The research reported here was sponsored by the United States Air Force under Contract F49642-01-C-0003. Further information may be obtained from the Strategic Planning Division, Directorate of Plans, Hq USAF. Library of Congress Cataloging-in-Publication Data Rabasa, Angel. Indonesia’s transformation and the stability of Southeast Asia / Angel Rabasa, Peter Chalk. p. cm. Includes bibliographical references. “MR-1344.” ISBN 0-8330-3006-X 1. National security—Indonesia. 2. Indonesia—Strategic aspects. 3. Indonesia— Politics and government—1998– 4. Asia, Southeastern—Strategic aspects. 5. National security—Asia, Southeastern. I. Chalk, Peter. II. Title. UA853.I5 R33 2001 959.804—dc21 2001031904 Cover Photograph: Moslem Indonesians shout “Allahu Akbar” (God is Great) as they demonstrate in front of the National Commission of Human Rights in Jakarta, 10 January 2000. Courtesy of AGENCE FRANCE-PRESSE (AFP) PHOTO/Dimas. RAND is a nonprofit institution that helps improve policy and decisionmaking through research and analysis. RAND® is a registered trademark. RAND’s publications do not necessarily reflect the opinions or policies of its research sponsors. Cover design by Maritta Tapanainen © Copyright 2001 RAND All rights reserved. No part of this book may be reproduced in any form by any electronic or mechanical means (including photocopying, -
05. Dida Kusnida.Cdr
Geo-Science J.G.S.M. Vol. 17 No. 2 Mei 2016 hal. 99 - 106 Depositional Modification in Seram Trough, Eastern Indonesia Modifikasi Pengendapan di Palung Seram, Indonesia Timur Dida Kusnida, Tommy Naibaho, and Yulinar Firdaus Marine Geological Institute of Indonesia, Jl. Dr. Djundjunan 236, Bandung-40174 [email protected] Naskah diterima : 1 Maret 2016, Revisi terakhir : 3 Mei 2016, Disetujui : 4 Mei 2016 Abstract - Seismic reflection profiles considered to Abstrak - Penampang rekaman seismik yang dianggap represent the morphotectonics of the study area and mewakili morfotektonik daerah studi dan diverifikasi verified by surficial sedimentary data presented in this dengan data sedimen permukaan yang disajikan dalam paper directed to understand the sedimentary depositional tulisan ini diarahkan untuk memahami dinamika dynamics. Seismic data interpretation results show the pengendapan sedimen. Hasil penafsiran data seismik gradation and sediment facies cycles in accordance with menunjukan gradasi dan siklus fasies sedimen sesuai the episode of tectonic activities, which is characterized by dengan episod aktivitas tektonik yang dicirikan oleh the avalanche of the Seram Trough base-of slopes longsoran material lereng Palung Seram. Data seismik materials. Seismic data reveal more than 1250 meters menunjukan lebih dari 1250 meter sedimen secara akustik acoustically chaotic to laminated, indicate fine-grained kaotik hingga berlapis, mencirikan sedimen berbutir sediments between slumps at its base of slope and fine halus antara slam pada lereng bagian bawah dan sedimen marine sediments at the trough floor. Thus, it suggests that marin halus pada lantai palung. Dengan demikian, diduga the Seram Trough is in the process of differential vertical bahwa Palung Seram berada dalam proses pergerakan movement causing depositional modification due to the vertikal diferensial yang menyebabkan terjadinya accretionary prism growths. -
Project Report Report of the CLIVAR ITF Task Team Meeting
Project Report Report of the CLIVAR ITF Task Team Meeting Jakarta, Indonesia 12th – 14th March 2012 March 2013 WCRP Informal/Series Report No. 20/2013 ICPO Informal Report 193/13 CLIVAR is a component of the World Climate Research Programme (WCRP). WCRP is sponsored by the World Meterorological Organisation, the International Council for Science and the Intergovernmental Oceanographic Commission of UNESCO. The scientific planning and development of CLIVAR is under the guidance of the JSC Scientific Steering Group for CLIVAR assisted by the CLIVAR International Project Office. The Joint Scientific Committee (JSC) is the main body of WMO-ICSU-IOC formulating overall WCRP scientific concepts. Bibliographic Citation INTERNATIONAL CLIVAR PROJECT OFFICE, 2013: IFT Task Team. International CLIVAR Publication Series No 193. (not peer reviewed). 6 Table of Contents 1. Introduction .......................................................................................................................................... 8 2. The CLIVAR ITF Task Team ............................................................................................................ 9 3. Outcomes of the ITF-TT Workshop: March 2012 .................................................................... 9 3.1 Indonesian Throughflow Inflow Research ....................................................................................... 10 3.1.1 Makassar throughflow: ............................................................................................................................... -
SESSION I : Geographical Names and Sea Names
The 14th International Seminar on Sea Names Geography, Sea Names, and Undersea Feature Names Types of the International Standardization of Sea Names: Some Clues for the Name East Sea* Sungjae Choo (Associate Professor, Department of Geography, Kyung-Hee University Seoul 130-701, KOREA E-mail: [email protected]) Abstract : This study aims to categorize and analyze internationally standardized sea names based on their origins. Especially noting the cases of sea names using country names and dual naming of seas, it draws some implications for complementing logics for the name East Sea. Of the 110 names for 98 bodies of water listed in the book titled Limits of Oceans and Seas, the most prevalent cases are named after adjacent geographical features; followed by commemorative names after persons, directions, and characteristics of seas. These international practices of naming seas are contrary to Japan's argument for the principle of using the name of archipelago or peninsula. There are several cases of using a single name of country in naming a sea bordering more than two countries, with no serious disputes. This implies that a specific focus should be given to peculiar situation that the name East Sea contains, rather than the negative side of using single country name. In order to strengthen the logic for justifying dual naming, it is suggested, an appropriate reference should be made to the three newly adopted cases of dual names, in the respects of the history of the surrounding region and the names, people's perception, power structure of the relevant countries, and the process of the standardization of dual names.