Current Status of the Seabird Colony on Suanggi Island, Banda Sea
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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. -
Report on Biodiversity and Tropical Forests in Indonesia
Report on Biodiversity and Tropical Forests in Indonesia Submitted in accordance with Foreign Assistance Act Sections 118/119 February 20, 2004 Prepared for USAID/Indonesia Jl. Medan Merdeka Selatan No. 3-5 Jakarta 10110 Indonesia Prepared by Steve Rhee, M.E.Sc. Darrell Kitchener, Ph.D. Tim Brown, Ph.D. Reed Merrill, M.Sc. Russ Dilts, Ph.D. Stacey Tighe, Ph.D. Table of Contents Table of Contents............................................................................................................................. i List of Tables .................................................................................................................................. v List of Figures............................................................................................................................... vii Acronyms....................................................................................................................................... ix Executive Summary.................................................................................................................... xvii 1. Introduction............................................................................................................................1- 1 2. Legislative and Institutional Structure Affecting Biological Resources...............................2 - 1 2.1 Government of Indonesia................................................................................................2 - 2 2.1.1 Legislative Basis for Protection and Management of Biodiversity and -
50156-001: Muara Laboh Geothermal Power Project
Draft Environmental Impact Assessment Report (ANDAL) Project Number: 50156-001 October 2013 INO: Muara Laboh Geothermal Power Project Prepared by PT Greencap NAA Indonesia for PT Supreme Energy Muara Laboh (PT SEML) This environmental impact assessment report is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. Your attention is directed to the “Term of Use” section of this website. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. Environmental Impact Assessment (ANDAL) Geothermal Development Activities for 250 MW Muara Laboh Geothermal Power Plant in South Solok Regency, West Sumatra Province October, 2013 Environmental Impact Assessment (ANDAL) Geothermal Development Activities for the 250 MW Muara Laboh Geothermal Power Plant (PLTP) in South Solok Regency, West Sumatra Province October, 2013 PREFACE PT Supreme Energy Muara Laboh (PT SEML), a company owned by PT Supreme Energy, GDF Suez (a company domiciled in France), and Sumitomo Corporation (a company domiciled in Japan), plan to conduct "Geothermal Development Activities for the 250 MW Muara Laboh Geothermal Power Plant in South Solok Regency, West Sumatra Province". The planned Geothermal Development Activities generally include the development and operation of geothermal power plant and the construction of supporting facilities. It is expected that the planned activities will give benefits in supporting the policy of Indonesian Government on energy diversification. -
Indonesia Komodo Islands / Spice Islands / Raja Ampat
INDONESIA KOMODO ISLANDS / SPICE ISLANDS / RAJA AMPAT October | Saturday - Thursday Notes Day 1 Saturday Labuan Bajo Inclusion Arrive at Labuan Bajo to a warm welcome. Board Aqua Blu and Dinner cruise to Gili Lawa Daut as the sun sets. Embarkation time 2:00pm Recommended Flight Bali to Labuan Bajo Wings Air – IW 1830* Day 2 Sunday Ropa, Kelimutu Volcano Lake Excursion Inclusion Colored lakes within the three calderas of a long dormant volcano Breakfast, Lunch, Dinner are on impressive display at the Kelimutu volcano, an otherworldly series of geologic cauldrons. The twisting road to the summit winds through incredible forests and criss-crosses mountain streams. Day 3 Monday North Lembata Inclusion Snorkel the extensive reef complex of Bacatan or dive at the Breakfast, Lunch, Dinner western end of the end for its specutacular deep dropoff. Trek or bike along a country lane between two villages in Lewoto. Enjoy a sumptous dinner onboard before departing North Lembata for an overnight crossing to Alor. www.aquaexpeditions.co m Day 4 Tuesday Pantar & Alor Inclusion Arrive at Alor, home to many picturesque fishing villages and Breakfast, Lunch, Dinner surrounded by clear water over vibrant coral reefs that are a diver’s and snorkeler’s favorite. Centuries-old tradition comes to life in the traditional dance performances by the friendly Abui Tribe. Sail overnight to Wetar. Day 5 Wednesday Wetar (The Forgotten Islands) Inclusion There is plenty to do and see along this rarely visited rugged Breakfast, Lunch, Dinner coastline of Wetar, which features impressive wall dives to meet sharks, schools of pelagic fishes, majestic manta and mobular rays. -
Disaster Preparedness Tips (A Guide Book for Personal Safety in the Field with Special Reference to Indonesia)
Disaster Preparedness Tips (A guide book for personal safety in the field with special reference to Indonesia) Canadian Red Cross Indonesia Mission Tsunami Recovery Operations Banda Aceh, Indonesia July 2009 Disaster Preparedness Tips (A guide book for personal safety in the field with special reference to Indonesia) Compiled/Edited By Shesh Kanta Kafle Disaster Risk Reduction Program Manaager Canadian Red Cross Indonesia Mission Tsunami Recovery Operations Banda Aceh, Indonesia July 2009 2 Contents Earthquake What is an earthquake? 4 What causes an earthquake? 4 Effects of earthquakes 4 How are earthquakes measured? 5 How do I protect myself in an earthquake? 6 Things to do before an earthquake occurs 8 Things to do during an earthquake 8 Earthquake zones 10 Tsunami What is a tsunami? 11 What causes a tsunami? 11 History of Tsunami in West coast of Indonesia 11 How do I protect myself in a Tsunami? 12 What to do before a Tsunami 12 What to do after a Tsunami 12 Flood What is a flood? 13 Common types of flooding 13 Flood warnings 13 How do I protect myself in a flood? 15 Before a flood 15 During a flood 15 Driving Flood Facts 16 After a flood 16 Volcano What is a volcano? 18 How is the volcano formed? 18 How safe are volcanoes? 18 Risk zones around and active volcano 18 When you are in the house 20 When you are in the field 21 In vehicles 21 Safety recommendations when visiting an active volcano 21 Precautions in the danger zone 22 References 26 Annex 3 Earthquake What is an earthquake? An earthquake is a sudden tremor or movement of the earth’s crust, which originates naturally at or below the surface. -
Austronesians in Papua: Diversification and Change in South Halmahera–West New Guinea
Austronesians in Papua: Diversification and change in South Halmahera–West New Guinea by David Christopher Kamholz A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Linguistics in the Graduate Division of the University of California, Berkeley Committee in charge: Professor Andrew Garrett, Chair Professor Larry Hyman Professor Johanna Nichols Fall 2014 Austronesians in Papua: Diversification and change in South Halmahera–West New Guinea Copyright 2014 by David Christopher Kamholz 1 Abstract Austronesians in Papua: Diversification and change in South Halmahera–West New Guinea by David Christopher Kamholz Doctor of Philosophy in Linguistics University of California, Berkeley Professor Andrew Garrett, Chair This dissertation presents a new subgrouping of South Halmahera–West New Guinea (SHWNG) languages. The 38 SHWNG languages form a small, poorly known branch of Austronesian. The Austronesian family originated in Taiwan and later spread into In- donesia, across New Guinea, and to the remote Pacific. In New Guinea, approximately 3500 years ago, Austronesian speakers first came into contact with so-called Papuan languages—the non-Austronesian languages indigenous to New Guinea, comprising more than 20 families. The Austronesian languages still extant from this initial spread into New Guinea fall into two branches: SHWNG and Oceanic. In great contrast to Oceanic, only a few SHWNG languages are well-described, and almost nothing has been reconstructed at the level of Proto-SHWNG. Contact with Papuan languages has given the SHWNG lan- guages a typological profile quite different from their linguistic forebears. Chapter 1 puts the SHWNG languages in context, describing their significance for Aus- tronesian and their broader relevance to historical linguistics. -
The Tectonic History of the Banda Arcs, Eastern Indonesia: a Review
J. geol. Soc. London, Vol. 136, 1979, pp. 519-527,2 figs. Printed inNorthern Ireland. The tectonic history of the Banda Arcs, eastern Indonesia: a review M. S. Norvick SUMMARY: The Banda Sea is underlain by a small marginal oceanic plate, which is believed to have formed during the early Tertiary. Unlike other marginal seas to the N, the spreading of the Banda platelet was restricted by surrounding continental blocks. Its present complexity is a result of late Miocene-earlyPliocene collision and obduction of theBanda Sea island arc system over the leading edge of the Australian-lrian continental plate. Transcurrent faultingon the northern limb of the collision zone may have accentuated curvature of the arc. Subduction and volcanicitv ceased after collision in the Timor and Seram sectors, but are still active at the eastern extremity of the arc. Adouble spiral line of geologicallyvery complex, based on bathymetry (Mammerickx et al. 1976), reg- small, mountainous islands make up the Banda Arcs ional gravity (Vening Meinesz 1954; Chamalaun et al. of eastern Indonesia (Fig. 1). Although onshore out- 1976; Milsom 1977)and earthquake distribution crop information is scattered, and geophysical data on (Hamilton 1974a; Cardwell & Isacks1978). Seismic the deep seas that cover 90% of the area sparse, the lineshave been published across the Timor region tectonic history of the region has stimulated discussion (Branson1974; Beck & Lehner1974; Crostella & formany years, and produced different (sometimes Powell 1975) and the Seram Trough (Audley-Charles conflicting) interpretations. The present review attempts& Carter 1978). Two 1976 oceanographic surveys run to reinterpretto critically thedata and some of by Scripps(‘Indopac’ programme) and CCOP (‘Val- theplate tectonic theories on theevolution of the divia’ cruise) collected valuable seismic refraction and Banda Arcs in the light of recent geological mapping reflection data over the deep water areas (Purdy et al. -
Lithosphere Structure and Dynamics of the Banda Arc Collision Zone, Eastern Indonesia
GeowgicaL Soci£ty of MalayJUz - circum-Pacific Council for Energy a/lu MineraL I!':0urc~ Tectonic Fl'flITUwork and Energy Ruourcu of tbe W(Jtern Margin of the PacifIC Btum November 27 December 2, 1992, Kuo.Ia Lumpur, MalayJUz Lithosphere structure and dynamics of the Banda Arc collision zone, Eastern Indonesia ADRIAN RICHARDSON Geological Research in Southeast Asia, Department of Geology Royal Holloway and Bedford New College, Egham, Surrey, TW20 O~X, England Present Address: Shellinternationale Petroleum MaatschapplJ B.V. Postbus 162, 2501, AN Den Haag, Oostduinlaan 75, Nederland Abstract: Timor and adjacent islands in Eastern Indonesia are the site of a currentl~ active col~ision between the Australian continental shelf and the volcanic islands of the Banda Arc. PreVIously pubhshed sedimentological and micro-paleontological data from the islands and the subduction trench date the start of this collision at 2.5 to 3 Ma. Previously published work on seismicity in the Banda Arc shows the geometry of the subduction zone to be fairly simple and continuous down to below 650 km depth. In this paper, the geometry of both the top and bottom surfaces of the subd~cting sla~ is mapp~d to a hl:gh~r degree of accuracy than before. The edge of Australia, which was preVIously a rifted paSSIve margm, IS shown to be markedly thickened in the collision zone itself and has been subducted to a depth of about 200 km. In addition, it appears that the subduction zone has major lateral and vertical discontinuities at depth. It is proposed that these discontinuities reflect slab separation during a previous micro continental collisional event some 10 to 7 million years ago and that this collision was related to the transfer of continental lithosphere from the Indo-Australian plate to the South East Asian plate. -
The Archaeology of Sulawesi Current Research on the Pleistocene to the Historic Period
terra australis 48 Terra Australis reports the results of archaeological and related research within the south and east of Asia, though mainly Australia, New Guinea and Island Melanesia — lands that remained terra australis incognita to generations of prehistorians. Its subject is the settlement of the diverse environments in this isolated quarter of the globe by peoples who have maintained their discrete and traditional ways of life into the recent recorded or remembered past and at times into the observable present. List of volumes in Terra Australis Volume 1: Burrill Lake and Currarong: Coastal Sites in Southern Volume 28: New Directions in Archaeological Science. New South Wales. R.J. Lampert (1971) A. Fairbairn, S. O’Connor and B. Marwick (2008) Volume 2: Ol Tumbuna: Archaeological Excavations in the Eastern Volume 29: Islands of Inquiry: Colonisation, Seafaring and the Central Highlands, Papua New Guinea. J.P. White (1972) Archaeology of Maritime Landscapes. G. Clark, F. Leach Volume 3: New Guinea Stone Age Trade: The Geography and and S. O’Connor (2008) Ecology of Traffic in the Interior. I. Hughes (1977) Volume 30: Archaeological Science Under a Microscope: Studies in Volume 4: Recent Prehistory in Southeast Papua. B. Egloff (1979) Residue and Ancient DNA Analysis in Honour of Thomas H. Loy. M. Haslam, G. Robertson, A. Crowther, S. Nugent Volume 5: The Great Kartan Mystery. R. Lampert (1981) and L. Kirkwood (2009) Volume 6: Early Man in North Queensland: Art and Archaeology Volume 31: The Early Prehistory of Fiji. G. Clark and in the Laura Area. A. Rosenfeld, D. Horton and J. Winter A. -
USAID SEA) PROJECT QUARTERLY REPORT SECOND Quarter of FY2019 (01 Jan – 31 Mar 2019
USAID SUSTAINABLE ECOSYSTEMS ADVANCED (USAID SEA) PROJECT QUARTERLY REPORT SECOND Quarter of FY2019 (01 Jan – 31 Mar 2019) MARCH 2019 This publication was produced for review by the United States Agency for International Development (USAID). Prepared by Tetra Tech. The authors’ views expressedc in this publication do not necessarily reflet the vi e ws of the United States Agency for International Development or the United States Government. Contract Number : AID-497-C-16-00008 Project Title : USAID Sustainable Ecosystems Advanced (SEA) Project Contract Period : March 21, 2016 to March 22, 2021 Prepared for : USAID Indonesia Submitted to : Celly Catharina, Contracting Officer’s Representative (COR) [email protected] Submitted by : Tetra Tech 159 Bank Street, Suite 300, Burlington, VT 05401, USA Tel: 802-495-0282, Fax: 802 658-4247 www.tetratech.com/intdev Submitted on : April 15, 2019 Revised version : May 23, 2019 Tetra Tech Contacts: Alan White, Chief of Party [email protected] Tiene Gunawan, Deputy Chief of Party [email protected] Gina Green, Project Manager [email protected] Cover photos: (Clockwise from top left) Presentation of boat registration certficates in Labuan Village, Sawai (USAID SEA / Yasmina Enita); Consumable fresh fish, Sorong, West Papua (USAID SEA / Asril Djunaidi); Basic dive training for project stakeholders in Sula, Maluku (CTC / Evi Nurul Ihsan); Behavior change communications pre-test assessment (USAID SEA / Chris Rotinsulu). TABLE OF CONTENTS List of Tables ........................................................................................................................................................................................... -
Provenance of Permian-Triassic Gondwana Sequence Units
GR-01538; No of Pages 12 Gondwana Research xxx (2015) xxx–xxx Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Provenance of Permian–Triassic Gondwana Sequence units accreted to the Banda Arc in the Timor region: Constraints from zircon U–Pb and Hf isotopes Christopher J. Spencer a,b,⁎, Ron A. Harris a, Jonathan R. Major a,c a Department of Geological Sciences, Brigham Young University, Provo, UT 84602, USA b Department of Applied Geology, Curtin University, Perth, WA 6845, Australia c Bureau of Economic Geology, University of Texas at Austin, Austin, TX 78713, USA article info abstract Article history: Analysis of zircons from Australian affinity Permian–Triassic units of the Timor region yield age distributions with Received 17 June 2015 large age peaks at 230–400 Ma and 1750–1900 Ma, which are similar to zircon age spectra found in rocks from NE Received in revised form 30 September 2015 Australia and crustal fragments now found in Tibet and SE Asia. It is likely that these terranes, which are now Accepted 14 October 2015 widely separated, were once part of the northern edge of Gondwana near what is now the northern margin of Available online xxxx Australia. The Cimmerian Block rifted from Gondwana in the Early Permian during the initial formation of the Handling Editor: A.R.A. Aitken Neo-Tethys Ocean. The zircon age spectra of the Gondwana Sequence of NE Australia and in the Timor region are most similar to the terranes of northern Tibet and Malaysia, further substantiating a similar tectonic affinity.