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I N D I a N O C E a N P H I L I P P I N E S

SOUTHEAST ASIA H 100 Hefei 120 140 E Shanghai JAPAN N Chang Jiang East N MekongG Chengdu Wuhan D A U Hangzhou S M A Chongqing China N Ningbo D P ( J A P A N ) N A P A J ( O Zigong Sea - S Nanchang N H Wenzhou A A L S N ra C H I N A H put Changsha S I ) O BONIN Brahma Guiyang Okinawa N T ISLANDS A Fuzhou O Naha P - INDIA U A J - Kunming Taipei Y ( DAITO- SHOTO- Xiamen ait K VOLCANO Str U (JAPAN) Y ISLANDS Xi Jiang R Guangzhou Shantou Tropic of Cancer Ta iw a n Irrawaddy Taiwan Nanning Kao-hsiung Mandalay Hong Kong S.A.R. Zhanjiang Macau Hanoi S.A.R. Okino-tori- BURMA Pratas shima Akyab Haiphong Island Luzon (JAPAN) 20 n LAOS Strait 20 Gulf of BABUYAN ISLANDS Salwee Chiang To n k i n Hainan Mai Vientiane Dao C Vinh H P h i l i p p i n e A ÎN Rangoon E Pathein Mekong A Hue PARACEL Luzon N ISLANDS THAILAND N Da Nang S e a A Nakhon M Mawlamyine IT Ratchasima I VIETNAM Q Manila U Dawei Bangkok E South Coco Channel CAMBODIA Nha ANDAMAN Trang Mindoro ISLANDS Phnom Penh China Samar (INDIA) P H I L I P P I N E S Andaman Ho Chi Minh Sea Panay Iloilo City Cebu Sea Gulf of Long Palawan Bacolod Xuyen Thailand SPRATLY Negros FED. STATES OF ISLANDS Sulu Sea Cagayan de Oro NICOBAR Mindanao ISLANDS Phuket Koror MICRONESIA (INDIA) Songkhla Zamboanga Davao Great Channel Kota Kinabalu George Town Bandar Seri Banda Aceh Strait of Malacca Ipoh Begawan PALAU MALAYSIA BRUNEI N o r t h KEPULAUAN Celebes Medan Kuala Lumpur NATUNA P Sea P a c i f i c E MALAYSIA G Melaka Pulau Simeulue U O c e a n N Kuching B o r n e o Manado U Singapore Pulau Nias N SINGAPORE Halmahera G Pontianak Molucca Equator 0 A 0 M N Selat Samarinda Sea Padang Pulau Palu B Sorong Bangka O Pulau Siberut A Sumatra Karimata Sulawesi R I (Celebes) L KEPULAUAN S Ceram Banjarmasin Makassar Strait Jayapura MENTAWAI A N Palembang U Billiton Kendari PEGUNUNGAN Buru Ambon MAOK Tanjungkarang- Makassar C E Telukbetung Java Sea New Guinea Jakarta C I N D O N E S I A Banda Sea KEPULAUAN PAPUA A Selat Sunda Semarang Madura ARU NEW Flores Sea S GUINEA Bandung Java Surabaya Lombok Bali Flores Dili Arafura Denpasar Merauke Sumbawa EAST TIMOR Selat Lombok Kupang Sea Christmas Island Sumba Timor (AUSTRALIA) Cocos Timor (Keeling) Islands Sea Ashmore and Darwin (AUSTRALIA) Cartier Islands (AUSTRALIA) Gulf of I n d i a n O c e a n Carpentaria Scale 1:32,000,000 at 5ºN Mercator Projection A U S T R A L I A 0 500 Kilometers 20 20 Port Hedland G R E A T S A N D Y 0 500 Miles Karratha Mount Isa Boundary representation is not necessarily authoritative. D E S E R T Names in Vietnam are shown without diacritical marks. 100 120 140 802914AI (R02106) 6-02.

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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.
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The Tsunami Deposits of the September 28, 2018 Palu Earthquake, Sulawesi, Indonesia
Geophysical Research Abstracts Vol. 21, EGU2019-6290, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. The tsunami deposits of the September 28, 2018 Palu earthquake, Sulawesi, Indonesia. Adam D. Switzer (1,2), Jedrzej M. Majewski (1,2), Rachel YS. Guan (1,2), Benazir Benazir (3), Ella Meilianda (3), Peter R. Parham (1), Jessica Pilarczyk (4), Hermann Fritz (5), Robert Weiss (6), Benjamin P. Horton (1,2) (1) Earth Observatory of Singapore, Nanyang Technological University, Singapore ([email protected]), (2) Asian School of the Environment, Nanyang Technological University, Singapore, (3) Tsunami and Disaster Mitigation Research Center, Syiah Kuala University, Banda Aceh, Indonesia, (4) Centre for Natural Hazards Research, Department of Earth Sciences, Simon Fraser University, Canada, (5) School of Civil and Environmental Engineering, Georgia Institute of Technology, USA, (6) School of Geosciences, Virginia Polytechnic Institute and State University, USA On 28 September 2018, a large, shallow, magnitude 7.5 earthquake struck north of Palu, Central Sulawesi, In- donesia at 6:03 pm local time. The earthquake generated a tsunami with inundation depths up to 10 m high and inundation distances in excess of 400m. The tsunami was likely generated by a combination of minor fault dis- placement and multiple submarine landslides. In addition to the tsunami the region experienced co-seismic coastal subsidence that in places exceeded 1m and likely exacerbated the inundation of tsunami waves in some areas including Palu city. During a post tsunami survey in November 2018 we sampled four transects for sediment anal- ysis; two in Palu City and one each on the eastern and western coasts of Palu Bay.
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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.
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The 2018 Mw 7.5 Palu Earthquake: a Supershear Rupture Event Constrained by Insar and Broadband Regional Seismograms
remote sensing Article The 2018 Mw 7.5 Palu Earthquake: A Supershear Rupture Event Constrained by InSAR and Broadband Regional Seismograms Jin Fang 1, Caijun Xu 1,2,3,* , Yangmao Wen 1,2,3 , Shuai Wang 1, Guangyu Xu 1, Yingwen Zhao 1 and Lei Yi 4,5 1 School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China; [email protected] (J.F.); [email protected] (Y.W.); [email protected] (S.W.); [email protected] (G.X.); [email protected] (Y.Z.) 2 Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University, Wuhan 430079, China 3 Collaborative Innovation Center of Geospatial Technology, Wuhan University, Wuhan 430079, China 4 Key Laboratory of Comprehensive and Highly Eﬃcient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China; [email protected] 5 Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China * Correspondence: [email protected]; Tel.: +86-27-6877-8805 Received: 4 April 2019; Accepted: 29 May 2019; Published: 3 June 2019 Abstract: The 28 September 2018 Mw 7.5 Palu earthquake occurred at a triple junction zone where the Philippine Sea, Australian, and Sunda plates are convergent. Here, we utilized Advanced Land Observing Satellite-2 (ALOS-2) interferometry synthetic aperture radar (InSAR) data together with broadband regional seismograms to investigate the source geometry and rupture kinematics of this earthquake. Results showed that the 2018 Palu earthquake ruptured a fault plane with a relatively steep dip angle of ~85◦.
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Guest Experience
Guest Experience Contents The Amanwana Experience 3 Spa & Wellness 29 During Your Stay 5 Amanwana Spa Facilities 29 A New Spa Language 30 Aman Signature Rituals 32 Amanwana Dive Centre 7 Nourishing 33 Grounding 34 Diving at Amanwana Bay 7 Purifying 35 Diving at the Outer Reefs 8 Body Treatments 37 Diving at Satonda Island 10 Massages 38 Night Diving 13 Courses & Certifications 14 Moyo Conservation Fund 41 At Sea & On Land 17 Island Conservation 41 Species Protection 42 Water Sports 17 Community Outreach & Excursions 18 Camp Responsibility 43 On the Beach 19 Trekking & Cycling 20 Amanwana Kids 45 Leisure Cruises & Charters 23 Little Adventurers 45 Leisure Cruises 23 Fishing 24 Charters 25 Dining Experiences 27 Memorable Moments 27 2 The Amanwana Experience Moyo Island is located approximately eight degrees south of the equator, within the regency of Nusa Tenggara Barat. The island has been a nature reserve since 1976 and measures forty kilometres by ten kilometres, with a total area of 36,000 hectares. Moyo’s highest point is 600 meters above the Flores Sea. The tropical climate provides a year-round temperature of 27-30°C and a consistent water temperature of around 28°C. There are two distinct seasons. The monsoon or wet season is from December to March and the dry season from April to November. The vegetation on the island ranges from savannah to dense jungle. The savannah land dominates the plateaus and the jungle the remaining areas. Many varieties of trees are found on the island, such as native teak, tamarind, fig, coral and banyan.
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Local Trade Networks in Maluku in the 16Th, 17Th and 18Th Centuries
CAKALELEVOL. 2, :-f0. 2 (1991), PP. LOCAL TRADE NETWORKS IN MALUKU IN THE 16TH, 17TH, AND 18TH CENTURIES LEONARD Y. ANDAYA U:-fIVERSITY OF From an outsider's viewpoint, the diversity of language and ethnic groups scattered through numerous small and often inaccessible islands in Maluku might appear to be a major deterrent to economic contact between communities. But it was because these groups lived on small islands or in forested larger islands with limited arable land that trade with their neighbors was an economic necessity Distrust of strangers was often overcome through marriage or trade partnerships. However, the most . effective justification for cooperation among groups in Maluku was adherence to common origin myths which established familial links with societies as far west as Butung and as far east as the Papuan islands. I The records of the Dutch East India Company housed in the State Archives in The Hague offer a useful glimpse of the operation of local trading networks in Maluku. Although concerned principally with their own economic activities in the area, the Dutch found it necessary to understand something of the nature of Indigenous exchange relationships. The information, however, never formed the basis for a report, but is scattered in various documents in the form of observations or personal experiences of Dutch officials. From these pieces of information it is possible to reconstruct some of the complexity of the exchange in MaJuku in these centuries and to observe the dynamism of local groups in adapting to new economic developments in the area. In addition to the Malukans, there were two foreign groups who were essential to the successful integration of the local trade networks: the and the Chinese.
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Kareba Palu Koro News on Central Sulawesi Emergency Response
december 2018 - II issue #4 KAREBA PALU KORO NEWS ON CENTRAL SULAWESI EMERGENCY RESPONSE The impact of flash flood (11/12) in Salua. Photo: Titik Susana Ristiawaty/ERCB FLASH FLOOD IN SALUA, BATHING WASHING AND LATRINE FACILITIES WERE SWEPT AWAY On Tuesday 11 December evening, again flash flood struck and more,” said Dewi. Salua Village, Kulawi Sub-District, Sigi District, especially in RT “With this current situation, where should we stay now?” Dewi (neighborhood cluster) 1 and RT 2 which are located in Hamlet 3 continued talking and wiping her tears while looking at her (Note: a hamlet is divided into several RWs and one RW consists ruined house. of several RTs.) The event occurred at 7.30 p.m. local time when There are 79 households impacted by the flash flood. The 79 the community were praying in a local mosque and they were houses are damaged and 40 among them are seriously damaged shocked by the sound of roaring water. and could not be inhabited. The height of the muddy water is as “When I was praying last night, suddenly I heard a women high as the knee of an adult. Small bars of wood are mixing with crying and screaming, saying that the water had reached the mud and the flood water. community settlement,” said Jusman Lahudo (59), a Salua Village “Up to now (12 p.m. local time) the water is still flowing in Salua community member. According to him, the flash flood was Village and some heavy equipment are trying to clean up the the hugest and the worst one ever since 1992.
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Selection of LNG Receiving Ports
Chapter 4 Selection of LNG Receiving Ports January 2021 This chapter should be cited as ERIA (2021), ‘Selection of LNG Receiving Ports’, in Kimura, S., et al. (eds.), Feasible Solutions to Deliver LNG to Midsized and Large Islands in Indonesia. ERIA Research Project Report FY2020 no.18, Jakarta: ERIA, pp.22-30. Chapter 4 Selection of LNG Receiving Ports In this chapter, we proposed the locations of LNG receiving ports by using a methodology that considers several factors. First, we looked at the forecasted LNG demand in Eastern Indonesia as estimated in chapter 3. Second, in each region we gathered all seaports that are geographically close to the existing or planned-to-be-developed natural gas–fired or dual- engine power plants. Third, we gathered information on the profile of those seaports. Finally, considering the specifications of the model LNG carrier vessels, we selected several seaports as LNG receiving ports based on the accessibility of those seaports. In section 4.1, we presented the initial candidates for LNG receiving terminals (ports) based on the location of the existing seaports, the forecasted LNG demand and the existing and planned GPPs. In section 4.2, we selected LNG carrier vessels and presented their characteristics. Finally, in section 4.3, we presented the selected receiving ports based on their accessibility for the model ships. 1. Regions and the Potential LNG Receiving Ports Chapter 3 identified 21 regions that include cities and small islands where potential LNG demand for power generation would likely be generated in the future, i.e. in the 2040 horizon.
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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.
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Reprinted from the Proceedings of the 4Th Pacific Science Congress, Java, 1929; from Vol
Reprinted from the Proceedings of the 4th Pacific Science Congress, Java, 1929; from Vol. III, 1930, pp. 1-6 (preprint, pp. 1-6, issued at Congress, May, 1929). The Hydrographic and Faunal Independence of certain isolated deepwater seas in Eastern Asia. by CARL L. HUBBS University of Michigan, U. S. A. One of the most fascinating phases of zoogeography, since the publication of WALLACE'S "Island Life", has been a comparison of the faunas of isolated regions. The faunas of islands are not the only ones segregated from one another : so also are those of mountain tops, of rivers, of continents and oceans themselves. Among the most interesting cases are those of isolated deepwater basins-freshwater lakes, saline inland seas, deep fjords, and partially enclosed seas, such as the Black Sea and the Mediterranean Sea. It is probable that a number of such seas exist in the highly complicated Indopacific region. Two seas of this sort have interested me, and they form a striking contrast with one another. The Sea of Japan, nearly enclosed by land or by straits which nowhere are depressed as much as 180 meters below sea level, receives through Chosen Strait at its south end a branch of the warm Kuro Shiwo, and through its northern straits cold subarctic waters, which of course dip down beneath the warm layers coming up from the south. DR. CHARLES HENRY GILBERT, whose recent death was a severe blow to the zoology of the Pacific, has related to me the taking by the Albatross during its 1906 cruise in Japan, of tropical pelagic animals over a subarctic bottom fauna.
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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.
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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.
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