Global Earthquake Map.Pdf (PDF | 3.58

Total Page:16

File Type:pdf, Size:1020Kb

Global Earthquake Map.Pdf (PDF | 3.58 GLOBAL EARTHQUAKE HAZARD MAP January 02, 2015 to Feburary 05, 2015 27°30'0"W 23°20'0"E 74°10'0"E 125°0'0"E Greenland SeaGreenland Sea Greenland Sea Greenland ¯ Arctic Circle IcelandIceland N Iceland N " Finland " 0 Russia 0 ' ' 0 Sweden 0 3 Faroe Islands Norway 3 ° ° 2 2 6 6 Estonia Latvia Denmark Isle Of Man Lithuania Ireland United Kingdom Belarus Canada Netherlands Poland Kazakhstan-Xinjiang Border RegionRussia Kuril Islands Germany Belgium Sakhalin,Russia Luxembourg Czech Ukraine Jersey Slovakia Romania Kazakhstan Kuril Islands Austria Hungary Mongolia Saint Pierre And Miquelon France Switzerland Moldova Kuril Islands SloveniaCroatia Romania Northern Xinjiang, China Hokkaido, Japan Region Bosnia And HerzegovinaYugoslavia Kyrgyzstan Northern Xinjiang, China Italy Azerbaijan Andorra Bulgaria Vatican City Macedonia Georgia Uzbekistan Kyrgyzstan Albania Greece ArmeniaAzerbaijan Tajikistan Southern Xijing China Korea (DPRK) Portugal Spain Greece Turkey Turkmenistan TajkistanTajkistan Hindu Kush Region Afghanistan Tajikistan Crete,Greece Hindu Kush Region AfganistanTajikistan Korea, Republic of Malta Indian Held Kashmir Japan Near East Coast of Honshu Japann Cyprus Syria Hindu Kush Region, Afganistan Tunisia China Lebanon Afghanistan Iraq Kyushu Japan Palestine Iran Southeast of Honshu, Japan Morocco Sichuan China Southeast of Honshu, Japan IsraelJordan Southeast of Honshu, Japan Southern IranSouthern Iran Kuwait Algeria Pakistan Nepal Near Nawabshah Bhutan Myanmar Libya Egypt Bahrain Qatar Western Sahara Tropic of Cancer Saudi Arabia United Arab Emirates Bangladesh Taiwan India Macau Myanmar Philippine Islands Region Mauritania Oman Laos Wake Island Mali Niger Philippines Northern Mid Atlantic Ridge Yemen Luzon Philippine Cape Verde Chad Eritrea Thailand Northern Mariana Islands Senegal N Sudan N " Barbados Gambia Guam " 0 Cambodia 0 ' Burkina Faso ' 0 Guinea-bissau Djibouti Negros, Philippines 0 4 Vietnam 4 ° Guinea ° 1 1 1 Benin Nigeria Somalia 1 Venezuela Sierra Leone Togo Ethiopia Cote D'ivoireGhana Sri Lanka PalauAru Islands Region, Indonesia Maldives Liberia Central African Republic Marshall Islands Legend Cameroon Celebes Sea Micronesia Guyana Northern Sumatra, Indonesia Brunei Darussalam Suriname Northern Sumatra,Indonesia Malaysia French Guiana Northern Molucca Sea Halmahera, Indonesia Halmahera, IndonesiaNorthern Molucca Sea Kiribati Earthquake 2015 Equatorial Guinea Singapore Equator Halmahera, Indonesia North of Solomon Islands Sao Tome And Principe Congo Uganda Kenya Indonesia Halmahera, Indonesia Gabon Equator Minahassa Peninsula,Sulawesi Nauru Magnitude Rwanda Congo, DR 62 km NW of Male Island Burundi Banda Sea Eastern New Guinea Region, P.N.G. Seychelles Sunda Strait Indonesia Banda Sea 2.5 - 3.3 Flores Sea Tanzania Papua New Guinea British Indian Ocean Territory Sumbawa Region, Indonesia East Timor Solomon Islands Christmas Island 3.3 - 4.3 Comoros Brazil Angola Cocos Islands Malawi Mayotte Zambia VanuatuVanuatu Islands Saint Helena 4.3 - 5.1 Mozambique Bolivia Vanuatu Island Zimbabwe Madagascar China Mauritius Southeast of Loyalty Island Reunion New Caledonia 5.1 - 5.7 Botswana Fiji Paraguay Namibia Tropic of Capricorn Southeast of Loyalty Islands Australia Swaziland Argentina 5.7 - 6.9 Tajikistan South Africa Lesotho Norfolk Island Uruguay World Boundary S S " " 0 0 ' United States ' 0 0 1 1 ° ° 9 South Island, New Zealand 9 3 Creation Date: February 06, 2015 3 Projection/Datum: WGS 84 Geographic New Zealand Page Size: A3 0 1,000 2,000 4,000 Afghanistan 0 Kilometers French Southern Territories Data Source(s): Falkland Islands 30 PMD: Pakistan Metrological Department India 330 South Georgia And The SoDuthIS SaCndLwAichI MIsl ER: ALL RIGHTS RESERVED Pakistan This product is the sole property of ALHASAN SYSTEMS 60 [www.alhasan.com] - A Knowledge Management, Business 300 Psychology Modeling, and Publishing Company. The product is brought to you free of cost in digital format for information purposes only. The product might have not been prepared for Antarctic Circle or be suitable for legal, engineering, or surveying purposes. 270 90 For further detail and metadata information please call +92.51.282.0449/835.9288|[email protected] ALHASAN SYSTEMS at +92.51.282.0449 / 835.9288 or Antarctica All Rights Reserved - Copyright 2015 email us at [email protected] www.alhasan.com 27°30'0"W 23°20'0"E 74°10'0"E 125°0'0"E.
Recommended publications
  • British Strategic Interests in the Straits of Malacca, 1786-1819
    BRITISH STRATEGIC INTERESTS IN THE STRAITS OF MALACCA 1786-1819 Samuel Wee Tien Wang B.A., Simon Fraser University, 1991 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of History O Samuel Wee Tien Wang 1992 SIMON FRASER UNIVERSITY December 1992 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL NAME: Samuel Wee DEGREE: TITLE OF THESIS: British Strategic Interests in the Straits of Malacca, 1786-1819 EXAMINING COMMITTEE: CHAIR: J. I. Little ~dhardIngram, Professor Ian Dyck, Associate ~hfessor Chdrles Fedorak - (Examiner) DATE: 15 December 1992 PARTIAL COPYRIGHT LICENSE 1 hereby grant to Simon Fraser University the right to lend my thesis, project or extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without my written permission. Title of Thesis/Project/Extended Essay British Strategic Interests in the Straits of Malacca Author: (signature) Samuel Wee (name) (date) ABSTRACT It has almost become a common-place assumption that the 1819 founding of Singapore at the southern tip of the strategically located Straits of Malacca represented for the English East India Company a desire to strengthen trade with China; that it was part of an optimistic and confident swing to the east which had as its goal, the lucrative tea trade.
    [Show full text]
  • Dating of Neogene Igneous Rocks in the Halmahera Region: Arc Initiation and Development
    Dating of Neogene igneous rocks in the Halmahera region: arc initiation and development SIMON BAKER & JEFFREY MALAIHOLLO SE Asia Research Group, Department of Geological Sciences, University College, London WC1E 6BT, UK Abstract: Potassium-argon ages of Neogene to Recent igneous rocks from the Halmahera region record a history of intra-oceanic arc development since the late Middle Miocene following an earlier phase of collisional plutonism. Arc formation from the Middle Miocene onwards was due to the east-directed subduction of the Molucca Sea plate beneath the Philippine Sea plate as it arrived at the Eurasian margin. The distribution of ages within the Neogene arc indicates a northward migration of volcanic activity during the Late Miocene to Pliocene. Results of the dating work show that after collision with the Australian margin at c. 22 Ma there was a period of volcanic quiescence and limestone deposition before a new arc formed. This arc began erupting at around 11 Ma on Obi as a result of subduction of the Molucca Sea plate. Initiation of subduction is thought to have occurred around 15-17 Ma and may have been responsible for disturbing potassium-argon ages of pre-Neogene rocks. Dates from fresh rocks show that the volcanic front migrated northwards through Bacan and Halmahera throughout the Late Miocene to Early Pliocene. Limestone deposition was curtailed as arc activity migrated north while volcanism died out from the south. No Neogene volcanism younger than 8 Ma is observed in the Obi area while on Bacan subduction-related volcanism ceased at c. 2 Ma. Late Pliocene crustal deformation caused a 30-40 km westward shift of the volcanic front.
    [Show full text]
  • Celebes Sea by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
    An Atlas of Oceanic Internal Solitary Waves (February 2004) Celebes Sea by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Celebes Sea Overview The Celebes Sea is located in the western Pacific Ocean north of the Indonesian Island of Celebes and south of the Sulu Sea and the Philippines (Figure 1). It is a deep-water sea, roughly circular with several exits to the Sulu Sea (to the north), the Makassar Strait (to the south), and the Phillipine and Molucca Seas (to the east). Figure 1. Bathymetry of the Celebes Sea. [Smith and Sandwell, 1997] Observations Like the Sulu Sea to the north, the Celebes Sea has a depth of over 4000 meters. It is surrounded by a shallow water regime along the edges of the adjacent landmasses and islands. The water depth in the northern region changes rapidly, from over 4000 m in Sulu Sea to approximately 100 m in the area across the Sulu Archipelago, returning to over 4000 m in the Celebes Sea. These bathymetric changes take place over approximately 150-km of horizontal distance. A similar situation takes place at the eastern end among the Kepulauan Sangi Islands. Both of these areas appear to be the sources of the internal waves observed in the Celebes Sea. There has been very little scientific research on the internal waves in the Celebes Sea. Satellite imagery indicates the internal waves are similar in character to those observed in the Sulu Sea. Internal waves are expected to occur all year round in the Celebes Sea, similar to other regions of the tropical Pacific (Table 1).
    [Show full text]
  • Plate Boundary Evolution in the Halmahera Region, Indonesia
    ~ectono~h~s~c~, 144 (1987) 337-352 337 EIsevier Science Publishers B.Y., Amsterd~ - Printed in The Netberiands Plate boundary evolution in the Halmahera region, Indonesia ROBERT HALL (Received December 1.1986; revised version accepted March 10,1987) Abstract Hall, R., 1987. Plate boundaryevolution in the Halmahera region, Indonesia. ~e~~~no~~.y~jcs,144: 337-352, H&mahera is situated in eastern Indonesia at the southwest comer of the Philippine Sea PIate. Active arc-arc collision is in process in the Molucca Sea to the west of Halmahera. New stratigraphic observations from Halmahera link this island and the east P~Iippin~ and record the history of subduction of the Molucca Sea lithosphere. The HaImahera Basement Complex and the basement of east Mindanao were part of an arc and forearc of Late Cretaceous-Early Tertiary age and have formed part of a single plate since the Late Eocene-Early Oligocene. There is no evidence that HaImabera formed part of an Oligo-Miocene arc but arc volcanism, associated with eastwards subduction of the Molucca Sea beneath Halmahera, began in the Pliocene and the Pliocene arc is built on a basement of the early Tertiary arc. Arc volcanism ceased briefIy during the Pleistocene and the arc shifted westwards after an episode of deformation. The present active arc is built upon deformed rocks of the Ptiocene arc. The combination of new strati~ap~c info~ation from the genera islands and models of the present-day tectonic structure of the region deduced from seismic and other geophysicat studies is used to constrain the tectonic evolution of the region since the Miocene.
    [Show full text]
  • Celebes Sea and Sulu Sea, Leg 124, Sites 767 and 7681
    Silver, E. A., Rangin, C., von Breymann, M. T., et al., 1991 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 124 30. SUBSIDENCE AND SEDIMENTATION ANALYSIS OF MARGINAL BASINS: CELEBES SEA AND SULU SEA, LEG 124, SITES 767 AND 7681 Zehui Huang,2 Felix M. Gradstein,2 and Keith E. Louden3 ABSTRACT Based on the chronostratigraphy and porosity of the sediments recovered from ODP Sites 767 and 768 drilled in the Celebes Sea and Sulu Sea, respectively, we examine the decompacted sedimentation and basement subsidence rates using a quantitative method. The results of this study help us to recognize several important tectonic events in these two marginal basins which improve understanding of the regional tectonic development. Among the recognized events are: (1) a pronounced increase in decompacted sedimentation rate in the Celebes Sea at 23.4 Ma, indicating basin transformation from a larger, more open oceanic setting to a marginal basin; (2) an increased basement subsidence rate in both basins between 10.8 and 8.9 Ma associated with the initiation of the Sulu Trough and the Sulawesi Trough; (3) appearance of a decompacted sedimentation rate peak between 10.0 and 8.9 Ma in both basins, indicating the combined effect of tectonic uplift in the source area and a sea-level drop; (4) uplift of the basement since 2.0 Ma, first in the Celebes Sea and then in the Sulu Sea, probably occurring as the result of collision events. INTRODUCTION strike-slip fault system that cuts through Sulawesi, which is a Neogene volcanic arc. The Molucca Sea collision zone, which is The Sulu and Celebes Seas are two small marginal basins in nearing completion and features incipient thrusting on its west- the west Pacific region, a complicated geotectonic region ern boundary, lies to the southeast of the Celebes Sea (Hamilton, marked by dynamic arc-arc and arc-continent collision zones, 1977; Moore and Silver, 1982).
    [Show full text]
  • Tectonic Controls on the Distribution of Large Copper and Gold Deposits in Southeast Asia to Identify Productive and Non-Productive Structures
    Tectonic controls on the distribution of large copper and gold deposits in Southeast Asia to identify productive and non-productive structures Bert De Waele, Peter Williams, Gavin Chan SRK Consulting, 10, Richardson Street, West Perth, WA6005, Western Australia Abstract. Ore deposits occur in a wide range of tectonic the east, however, on Sumbawa, several porphyry settings, and are highly variable in their local systems are known, of which the largest is the 5 Million characteristics. In this paper, we focus on the distribution year-old Batu Hijau deposit. Tectonics in that region, of copper and gold deposits in the Southeast Asia region, east of longitude 115°E, consists of the consumption of and investigate large-scale plate-tectonic controls on the the IP below the remnants of the Molucca Sea Plate distribution and characteristics of these porphyry copper and epithermal gold deposits. We then discuss the (MSP), i.e intra-oceanic subduction and the formation of applicability of these results to exploration in older island arcs. geological terranes, and suggest clues to distinguishing In Northern Indonesia, dextral escape tectonics productive from non-productive geological structures. related to India-Asia collision resulted in the southward subduction of the proto-South China Sea Plate (PSCSP) Keywords: Porphyry Copper-Gold, Tectonics below Borneo. This subduction ceased at about 24 Ma, with continent-continent collision and accretion of the 1 Tectonics and mineralisation in SE Asia sedimentary prism to northern Borneo. The cessation of subduction changed motion of the PSP, and collision of Southeast Asia is a collage of ophiolitic, island and the AP with the Sunda Arc resulted in counter clockwise oceanic arc terranes that formed as part of a complex rotation of Borneo.
    [Show full text]
  • Water Resources in Southeast Asia
    Water Resources Locator Map 180° 120°W 30°W 30°E 90°E 150°E N ^ ep Bhutan KA al ^ THMA THIMPHU NDU S a 60°N 60°N in Southeast Asia a utr l map w rah e X B e i n J Taipei anges ia China Red Mangroves G n g BANGLADESH Taiwan ^DHAKA Red mangroves grow along the shore of Thailand’s Lipe Island, T'ainan one of many offshore islands included in the country’s Tarutao Chittagong Kaoshsiung Orissa Coµast VIETNAM Hong Kong Marine National Park, off the western coast in the Canal Macau Mouths of the MYANMAR HANOI Strait of Malacca. Mangroves are an essential part ^ 60°S 60°S Ganges µ I of the marine ecology in many tropical areas of r LAOS Haiphong r Kendrapara a w the world, providing estuaries for wildlife nesting and feeding. Canal a Gulf of 180° 120°W 30°W 30°E 90°E 150°E d Luzon Strait d VIENTIA Tonkin Bay of Bengal y NE C ^ h a Lingayen RANGOON o M Luzon µ^ P e Gulf Twante Canal h k Da Nang ra o y THAILAND n a g Mouths of the Quezon City Polillo Irrawaddy Gulf of ^ Islands MANILA Martaban ^BANGKOK PHILIPPINE CAMBODIA P H I L I P P I N E S Andaman SOUTH Albay Gulf SEA Mindoro S PHNOM a Islands CHINA SEA m Asid Mergui PENH Gu a SIMAR SEA lf r Archipelago ^ ay Gulf of an PACIFIC n P s Thailand a o ol OCEAN µµ r oh Kinh Cai San w Panay g B Xom Kinh la e a ANDAMAN µµ a Gulf N e Lianga Bay Mouths of the Mekong P o S SEA Kinh Song Trem Mind ana Mindanao S Kinh Ca Maudi Bac Lieu SULU SEA Nikobar t Palau ra Davao Islands it Pujada Bay o Moro f o Gulf M BRUNEI g Davao a la la BANDAR SERI BENGAWAN e c Gulf c ip a MALAYSIA ^ rch ulu A EA Medan S S KUALA
    [Show full text]
  • The Indonesian Throughflow in OCCAM
    Ocean Sci. Discuss., 4, 325–370, 2007 Ocean Science www.ocean-sci-discuss.net/4/325/2007/ Discussions OSD © Author(s) 2007. This work is licensed 4, 325–370, 2007 under a Creative Commons License. Papers published in Ocean Science Discussions are under The Indonesian open-access review for the journal Ocean Science throughflow in OCCAM U. W. Humphries and D. J. Webb Title Page On the Indonesian throughflow in the Abstract Introduction OCCAM 1/4 degree ocean model Conclusions References Tables Figures U. W. Humphries1 and D. J. Webb2 1 King Monghut’s Institute of Technology, Thailand J I 2National Oceanography Centre, Southampton SO14 3ZH, UK J I Received: 5 March 2007 – Accepted: 16 March 2007 – Published: 21 March 2007 Back Close Correspondence to: D. J.Webb ([email protected]) Full Screen / Esc Printer-friendly Version Interactive Discussion 325 EGU Abstract OSD The Indonesian Throughflow is analysed in two runs of the OCCAM 1/4 degree global ocean model, one using monthly climatological winds and one using ECMWF analysed 4, 325–370, 2007 six-hourly winds for the period 1993 to 1998. The long-term model throughflow agrees 5 with observations and the value predicted by Godfrey’s Island Rule. The Island Rule The Indonesian has some skill in predicting the annual signal each year but is poor at predicting year throughflow in to year and shorter term variations in the total flow especially in El Nino years. OCCAM The spectra of transports in individual passages show significant differences be- tween those connecting the region to the Pacific Ocean and those connecting with U.
    [Show full text]
  • 2020 SOUTHEAST ASIA REGIONAL ENVIRONMENTAL SECURITY FORUM Pacific Environmental Security Forum Proposal for 2020
    2020 SOUTHEAST ASIA REGIONAL ENVIRONMENTAL SECURITY FORUM Pacific Environmental Security Forum Proposal for 2020 CDR LAZARO ERNESTO VALDEZ JR PCG J.D LLM Chief of Staff, National Coast Watch Center Office of the President, Republic of the Philippines 17 Seas Andaman Sea Arafura Sea TOTAL SEA Balabac Strait SURFACE AREA: Banda Sea Celebes Sea Flores Sea Gulf of Tonkin COMBINED Gulf of Thailand COASTAL LENGTH: Java Sea Malacca Strait Makassar Strait Molucca Sea Philippine Sea SUPPORTS South China Sea Sulu Sea Timor Sea Visayan Sea 17 Seas SEA Maritime Domain Andaman Sea is recognized as: the FAUNISTIC CENTRE Arafura Sea of the entire Indo-Pacific Balabac Strait Banda Sea a GLOBAL MARINE Celebes Sea BIODIVERSITY HOTSPOT Flores Sea Gulf of Tonkin GLOBAL HOTSPOT Gulf of Thailand Java Sea for coral reefs Malacca Strait Makassar Strait Molucca Sea 80% of the world’s 50% of seagrass Philippine Sea hard corals species South China Sea Sulu Sea Timor Sea 60% of mangrove species Visayan Sea 17 Seas very rich and important Andaman Sea INCOME SOURCE and RESOURCE FOR SEAFOOD Arafura Sea e.g. South China Sea Balabac Strait Banda Sea Celebes Sea over 3 million people <> 300 million people Flores Sea per day rely on fishing for their main dependent on the SCS for nutrition income sources and socioeconomic well-being Gulf of Tonkin Gulf of Thailand Java Sea Malacca Strait Makassar Strait Molucca Sea Philippine Sea South China Sea Sulu Sea Timor Sea Visayan Sea mid-1960S RAPID ECONOMIC FAST-EXPANDING GROWTH POPULATION Major CAUSES of Marine Environmental Degradation HUMAN ACTIVITIES/ NATURAL PHENOMENON ANTHROPOGENIC 1 PRESSURES 2 CLIMATE 3 CHANGE “MARINE ENVIRONMENTAL ACTIVISM IN SOUTHEAST ASIA” Environmental Activism Marine Environmental Concerns in SEA Marine Environmental Activism in SEA Future of Marine Environmental Activism in SEA THANK YOU AND MABUHAY!!!.
    [Show full text]
  • Chapter 13 Adjacent Seas of the Indian Ocean and the Australasian
    Chapter 13 Adjacent seas of the Indian Ocean and the Australasian Mediterranean Sea (the Indonesian throughflow) Being the smallest of all oceans, the Indian Ocean does not have the large number of distinct subregions found in the Pacific and Atlantic Oceans. Regions known under their own names include the Bay of Bengal and the Arabian Sea already discussed in the previous chapter, the Mozambique Strait (mentioned in the discussion of the western boundary currents), and the Great Australian Bight, clearly the least researched part of the Indian Ocean. Malacca Strait and the Andaman Sea form the transition region between the Bay of Bengal and the adjacent seas of the Pacific Ocean in Southeast Asia. The only regional seas that have some impact on the hydrography of the Indian Ocean and therefore require separate discussion are the Red Sea and the Persian Gulf. Since that discussion will not provide sufficient material for a full-length chapter, we include here the description of the Australasian Mediterranean Sea and what is often known as the Indonesian throughflow, i.e. the exchange of water between the Pacific and Indian Oceans. The Australasian Mediterranean Sea is of course a regional sea of the Pacific Ocean; but its impact on the Indian Ocean is much bigger than its influence on Pacific hydrography, and its inclusion in this chapter is justified on that ground alone. The Red Sea The Red Sea can be considered the prototype of a concentration basin. It is a deep mediterranean sea with a relatively shallow sill in a region where evaporation vastly exceeds precipitation (evaporation 200 cm per year, rainfall 7 cm per year, giving a net annual water loss of nearly 2 m).
    [Show full text]
  • Download Pdf Chapter VI. NORTH MOLUCCAS
    BIBLIOGRAPHY OF THE GEOLOGY OF INDONESIA AND SURROUNDING AREAS Edition 7.0, July 2018 J.T. VAN GORSEL VI. NORTH MOLUCCAS (incl. Seram, Sula) www.vangorselslist.com VI. NORTH MOLUCCAS VI. NORTH MOLUCCAS ............................................................................................................................... 13 VI.1. Halmahera, Bacan, Waigeo, Molucca Sea ......................................................................................... 13 VI.2. Banggai, Sula, Taliabu, Obi ............................................................................................................... 33 VI.3. Seram, Buru, Ambon ......................................................................................................................... 43 This chapter VI of Bibliography Ed. 7.0 deals with the northernmost part of the Indonesian Archipelago. It contains 67 pages, with 423 titles, and is divided into three sub-chapters. The North Moluccas are a geologically complex region with a number of active volcanic arcs, non-volcanic 'outer arcs', fragments of remnant arcs, microcontinents, and deep basins floored by oceanic crust. VI.1. Halmahera, Bacan, Waigeo, Yapen, Molucca Sea Sub-chapter VI.1. contains 155 references on the geology of the Halmahera region. Figure VI.1.1. Early geologic map of Halmahera- Bacan- Waigeo (Verbeek 1908) Bibliography of Indonesian Geology, Ed. 7.0 1 www.vangorselslist.com July 2018 This area of N Indonesia is in the realm of the western Pacific Ocean (Philippine Sea Plate). The western part is the Molucca Sea complex, where Molucca Sea Plate oceanic crust is subducting in two directions, under Halmahera in the East and the Sangihe arc in the West. The S side is bordered by the Sorong Fault zone, a major strike slip zone separating the W-moving Pacific from a N-moving Australia- New Guinea plate. Islands are composed of fragments of Late Cretaceous- M Eocene and younger island arc volcanics, intruded into and overlying collisional complexes with Jurassic or Cretaceous-age ophiolites.
    [Show full text]
  • The Spice Islands in Prehistory Archaeology in the Northern Moluccas, Indonesia
    terra australis 50 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 1. Burrill Lake and Currarong: Coastal Sites in Southern 30. Archaeological Science Under a Microscope: Studies in Residue New South Wales. R.J. Lampert (1971) and Ancient DNA Analysis in Honour of Thomas H. Loy. 2. Ol Tumbuna: Archaeological Excavations in the Eastern M. Haslam, G. Robertson, A. Crowther, S. Nugent and Central Highlands, Papua New Guinea. J.P. White (1972) L. Kirkwood (2009) 3. New Guinea Stone Age Trade: The Geography and Ecology 31. The Early Prehistory of Fiji. G. Clark and A. Anderson of Traffic in the Interior. I. Hughes (1977) (2009) 4. Recent Prehistory in Southeast Papua. B. Egloff (1979) 32. Altered Ecologies: Fire, Climate and Human Influence on Terrestrial Landscapes. S. Haberle, J. Stevenson and 5. The Great Kartan Mystery. R. Lampert (1981) M. Prebble (2010) 6. Early Man in North Queensland: Art and Archaeology in the 33. Man Bac: The Excavation of a Neolithic Site in Northern Laura Area. A. Rosenfeld, D. Horton and J. Winter (1981) Vietnam: The Biology. M. Oxenham, H. Matsumura and 7. The Alligator Rivers: Prehistory and Ecology in Western N.
    [Show full text]