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Papua New Guinea
PAPUA NEW GUINEA EMERGENCY PREPAREDNESS OPERATIONAL LOGISTICS CONTINGENCY PLAN PART 2 –EXISTING RESPONSE CAPACITY & OVERVIEW OF LOGISTICS SITUATION GLOBAL LOGISTICS CLUSTER – WFP FEBRUARY – MARCH 2011 1 | P a g e A. Summary A. SUMMARY 2 B. EXISTING RESPONSE CAPACITIES 4 C. LOGISTICS ACTORS 6 A. THE LOGISTICS COORDINATION GROUP 6 B. PAPUA NEW GUINEAN ACTORS 6 AT NATIONAL LEVEL 6 AT PROVINCIAL LEVEL 9 C. INTERNATIONAL COORDINATION BODIES 10 DMT 10 THE INTERNATIONAL DEVELOPMENT COUNCIL 10 D. OVERVIEW OF LOGISTICS INFRASTRUCTURE, SERVICES & STOCKS 11 A. LOGISTICS INFRASTRUCTURES OF PNG 11 PORTS 11 AIRPORTS 14 ROADS 15 WATERWAYS 17 STORAGE 18 MILLING CAPACITIES 19 B. LOGISTICS SERVICES OF PNG 20 GENERAL CONSIDERATIONS 20 FUEL SUPPLY 20 TRANSPORTERS 21 HEAVY HANDLING AND POWER EQUIPMENT 21 POWER SUPPLY 21 TELECOMS 22 LOCAL SUPPLIES MARKETS 22 C. CUSTOMS CLEARANCE 23 IMPORT CLEARANCE PROCEDURES 23 TAX EXEMPTION PROCESS 24 THE IMPORTING PROCESS FOR EXEMPTIONS 25 D. REGULATORY DEPARTMENTS 26 CASA 26 DEPARTMENT OF HEALTH 26 NATIONAL INFORMATION AND COMMUNICATIONS TECHNOLOGY AUTHORITY (NICTA) 27 2 | P a g e MARITIME AUTHORITIES 28 1. NATIONAL MARITIME SAFETY AUTHORITY 28 2. TECHNICAL DEPARTMENTS DEPENDING FROM THE NATIONAL PORT CORPORATION LTD 30 E. PNG GLOBAL LOGISTICS CONCEPT OF OPERATIONS 34 A. CHALLENGES AND SOLUTIONS PROPOSED 34 MAJOR PROBLEMS/BOTTLENECKS IDENTIFIED: 34 SOLUTIONS PROPOSED 34 B. EXISTING OPERATIONAL CORRIDORS IN PNG 35 MAIN ENTRY POINTS: 35 SECONDARY ENTRY POINTS: 35 EXISTING CORRIDORS: 36 LOGISTICS HUBS: 39 C. STORAGE: 41 CURRENT SITUATION: 41 PROPOSED LONG TERM SOLUTION 41 DURING EMERGENCIES 41 D. DELIVERIES: 41 3 | P a g e B. Existing response capacities Here under is an updated list of the main response capacities currently present in the country. -
AGRICULTURAL. SYSTEMS of PAPUA NEW GUINEA Ing Paper No. 14
AUSTRALIAN AtGENCY for INTERNATIONAL DEVELOPMENT AGRICULTURAL. SYSTEMS OF PAPUA NEW GUINEA ing Paper No. 14 EAST NIEW BRITAIN PROVINCE TEXT SUMMARIES, MAPS, CODE LISTS AND VILLAGE IDENTIFICATION R.M. Bourke, B.J. Allen, R.L. Hide, D. Fritsch, T. Geob, R. Grau, 5. Heai, P. Hobsb21wn, G. Ling, S. Lyon and M. Poienou REVISED and REPRINTED 2002 THE AUSTRALIAN NATIONAL UNIVERSITY PAPUA NEW GUINEA DEPARTMENT OF AGRI LTURE AND LIVESTOCK UNIVERSITY OF PAPUA NEW GUINEA Agricultural Systems of Papua New Guinea Working Papers I. Bourke, R.M., B.J. Allen, P. Hobsbawn and J. Conway (1998) Papua New Guinea: Text Summaries (two volumes). 2. Allen, BJ., R.L. Hide. R.M. Bourke, D. Fritsch, R. Grau, E. Lowes, T. Nen, E. Nirsie, J. Risimeri and M. Woruba (2002) East Sepik. Province: Text Summaries, Maps, Code Lists and Village Identification. 3. Bourke, R.M., BJ. Allen, R.L. Hide, D. Fritsch, R. Grau, E. Lowes, T. Nen, E. Nirsie, J. Risimeri and M. Woruba (2002) West Sepik Province: Text Summaries, Maps, Code Lists and Village Identification. 4. Allen, BJ., R.L. Hide, R.M. Bourke, W. Akus, D. Fritsch, R. Grau, G. Ling and E. Lowes (2002) Western Province: Text Summaries, Maps, Code Lists and Village Identification. 5. Hide, R.L., R.M. Bourke, BJ. Allen, N. Fereday, D. Fritsch, R. Grau, E. Lowes and M. Woruba (2002) Gulf Province: Text Summaries, Maps, Code Lists and Village Identification. 6. Hide, R.L., R.M. Bourke, B.J. Allen, T. Betitis, D. Fritsch, R. Grau. L. Kurika, E. Lowes, D.K. Mitchell, S.S. -
Lombok Island, Sumbawa Island, and Samalas Volcano
ECOLE DOCTORALE DE GEOGRAPHIE DE PARIS (ED 4434) Laboratoire de Géographie Physique - UMR 8591 Doctoral Thesis in Geography Bachtiar Wahyu MUTAQIN IMPACTS GÉOMORPHIQUES DE L'ÉRUPTION DU SAMALAS EN 1257 LE LONG DU DÉTROIT D'ALAS, NUSA TENGGARA OUEST, INDONÉSIE Defense on: 11 December 2018 Supervised by : Prof. Franck LAVIGNE (Université Paris 1 – Panthhéon Sorbonne) Prof. HARTONO (Universitas Gadjah Mada) Rapporteurs : Prof. Hervé REGNAULD (Université de Rennes 2) Prof. SUWARDJI (Universitas Mataram) Examiners : Prof. Nathalie CARCAUD (AgroCampus Ouest) Dr. Danang Sri HADMOKO (Universitas Gadjah Mada) 1 Abstract As the most powerful event in Lombok’s recent eruptive history, volcanic materials that were expelled by the Samalas volcano in 1257 CE covered the entire of Lombok Island and are widespread in its eastern part. Almost 800 years after the eruption, the geomorphological impact of this eruption on the island of Lombok remains unknown, whereas its overall climatic and societal consequences are now better understood. A combination of stratigraphic information, present-day topography, geophysical measurement with two-dimensional resistivity profiling technique, local written sources, as well as laboratory and computational analysis, were used to obtain detailed information concerning geomorphic impacts of the 1257 CE eruption of Samalas volcano on the coastal area along the Alas Strait in West Nusa Tenggara Province, Indonesia. This study provides new information related to the geomorphic impact of a major eruption volcanic in coastal areas, in this case, on the eastern part of Lombok and the western coast of Sumbawa. In the first place, the study result shows that since the 1257 CE eruption, the landscape on the eastern part of Lombok is still evolved until the present time. -
Undiscovered Papua National Mask Festival
UNDISCOVERED PAPUA NATIONAL MASK FESTIVAL One of the world’s most astonishing man-made spectacles, the Papua New Guinea national mask festival celebrates the unique mask cultures of the tribes of East New Britain: the Tolai, Baining, Pomio and Sulka. The festival itself is a four day extravaganza of storytelling, music, cultural dancing, and ritual performance. On the first day at dawn, the Kinavai is held, signalling the arrival of the Tolai Tubuans who arrive on canoes amidst the chanting and beating of kundu drums. Traditional masks will be on display during the festival – some many decades old, brought over from New Ireland Province and other parts of Papua New Guinea. Many of these masks are sacred and are not meant to be viewed, and the opening ceremony acts as a cleansing or appeasement ritual for the broken taboos. The highlight of the evening performances are the spectacular fire dances in which young initiated Baining men perform exhilarating rituals through blazing fires as their elders chant in haunting tones. During our stay we will also have time to visit wartime sites and WWII relics, travel through colourful welcoming villages and tour the rim of an active volcano. Attend the astonishing Kinavai ceremony on Kokopo beach at dawn. Witness the arrival of the Tolai people on canoes with wild drum beats. See traditional masks from all over Papua New Guinea. Be immersed by the performance of the Asaro mud-men warriors from the central highlands. Climb an active volcano and visit a vulcanology research station. Travel to the landing spot of Australian forces in World War One. -
Multi-Year Satellite Observations of Sulfur Dioxide Gas Emissions and Lava Extrusion at Bagana Volcano, Papua New Guinea B.T
1 Multi-year satellite observations of sulfur dioxide gas emissions and lava extrusion at Bagana volcano, Papua New Guinea B.T. McCormick Kilbride 1;∗, K. Mulina 2, G. Wadge 3, R.W. Johnson 4, I. Itikarai 2, and M. Edmonds 1 1COMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK. 2Rabaul Volcanological Observatory, Rabaul, Papua New Guinea. 3COMET, Department of Meteorology, University of Reading, Reading, UK. 4School of Asia and the Pacific, Australian National University, Canberra, Australia. Correspondence*: Brendan T. McCormick Kilbride, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK [email protected] 2 ABSTRACT 3 Bagana, arguably the most active volcano in Papua New Guinea, has been in a state of 4 near-continuous eruption for over 150 years, with activity dominated by sluggish extrusion of 5 thick blocky lava flows. If current extrusion rates are representative, the entire edifice may have 6 been constructed in only 300-500 years. Bagana exhibits a remarkably high gas flux to the 7 atmosphere, with persistent sulfur dioxide (SO2) emissions of several thousand tonnes per day. 8 This combination of apparent youth and high outgassing fluxes is considered unusual among 9 persistently active volcanoes worldwide. We have used satellite observations of SO2 emissions 10 and thermal infrared radiant flux to explore the coupling of lava extrusion and gas emission 11 at Bagana. The highest gas emissions (up to 10 kt/day) occur during co-extrusive intervals, 12 suggesting a degree of coupling between lava and gas, but gas emissions remain relatively high 13 (∼2500 t/d) during inter-eruptive pauses. -
Geophysical and Geochemical Signals at Yellowstone and Other Large Caldera Systems
Phil. Trans. R. Soc. A (2006) 364, 2055–2072 doi:10.1098/rsta.2006.1813 Published online 27 June 2006 Monitoring super-volcanoes: geophysical and geochemical signals at Yellowstone and other large caldera systems 1, 2 1 BY JACOB B. LOWENSTERN *,ROBERT B. SMITH AND DAVID P. HILL 1US Geological Survey, Volcano Hazards Team, MS 910, 345 Middlefield Road, Menlo Park, CA 94025, USA 2Department of Geology and Geophysics, University of Utah, 135 South, 1460 East, Room 702, Salt Lake City, UT 84112, USA Earth’s largest calderas form as the ground collapses during immense volcanic eruptions, when hundreds to thousands of cubic kilometres of magma are explosively withdrawn from the Earth’s crust over a period of days to weeks. Continuing long after such great eruptions, the resulting calderas often exhibit pronounced unrest, with frequent earthquakes, alternating uplift and subsidence of the ground, and considerable heat and mass flux. Because many active and extinct calderas show evidence for repetition of large eruptions, such systems demand detailed scientific study and monitoring. Two calderas in North America, Yellowstone (Wyoming) and Long Valley (California), are in areas of youthful tectonic complexity. Scientists strive to understand the signals generated when tectonic, volcanic and hydrothermal (hot ground water) processes intersect. One obstacle to accurate forecasting of large volcanic events is humanity’s lack of familiarity with the signals leading up to the largest class of volcanic eruptions. Accordingly, it may be difficult to recognize the difference between smaller and larger eruptions. To prepare ourselves and society, scientists must scrutinize a spectrum of volcanic signals and assess the many factors contributing to unrest and toward diverse modes of eruption. -
Silicic Magma Chambers and Mafic Dikes a Dissertation Submitted to the Department Of
INVESTIGATIONS OF MAGMATIC END-MEMBERS: SILICIC MAGMA CHAMBERS AND MAFIC DIKES A DISSERTATION SUBMITTED TO THE DEPARTMENT OF GEOLOGICAL AND ENVIRONMENTAL SCIENCES AND THE COMMITTEE ON GRADUATE STUDIES OF STANFORD UNIVERSITY IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY Gwyneth Retta Hughes May 2010 © 2010 by Gwyneth Retta Hughes. All Rights Reserved. Re-distributed by Stanford University under license with the author. This work is licensed under a Creative Commons Attribution- Noncommercial 3.0 United States License. http://creativecommons.org/licenses/by-nc/3.0/us/ This dissertation is online at: http://purl.stanford.edu/cf090yt6229 Includes supplemental files: 1. Caldera references for Chapters 2 and 3 (Caldera_index_ref.pdf) 2. Bayes Classifier Code for Chapter 3 (bayes_classifier.zip) 3. Caldera data for Chapter 2 (Arc_caldera_data.csv) 4. Caldera data for Chapter 3 (All_caldera_data.csv) ii I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. Gail Mahood, Primary Adviser I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. David Pollard I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. Paul Segall Approved for the Stanford University Committee on Graduate Studies. Patricia J. Gumport, Vice Provost Graduate Education This signature page was generated electronically upon submission of this dissertation in electronic format. -
Assessing Pyroclastic Fall Hazard Through Field Data And
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Earth-prints Repository JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. B2, 2063, doi:10.1029/2001JB000642, 2003 Assessing pyroclastic fall hazard through field data and numerical simulations: Example from Vesuvius Raffaello Cioni,1 Antonella Longo,2 Giovanni Macedonio,3 Roberto Santacroce,2 Alessandro Sbrana,2 Roberto Sulpizio,2 and Daniele Andronico4 Received 12 April 2001; revised 2 April 2002; accepted 7 May 2002; published 1 Feburary 2003. [1] A general methodology of pyroclastic fall hazard assessment is proposed on the basis of integrated results of field studies and numerical simulations. These approaches result in two different methods of assessing hazard: (1) the ‘‘field frequency,’’ based on the thickness and distribution of past deposits and (2) the ‘‘simulated probability,’’ based on the numerical modeling of tephra transport and fallout. The proposed methodology mostly applies to volcanoes that, by showing a clear correlation between the repose time and the magnitude of the following eruptions, allows the definition of a reference ‘‘maximum expected event’’ (MEE). The application to Vesuvius is shown in detail. Using the field frequency method, stratigraphic data of 24 explosive events in the 3–6 volcanic explosivity index range in the last 18,000 years of activity are extrapolated to a regular grid in order to obtain the frequency of exceedance in the past of a certain threshold value of mass loading (100, 200, 300, and 400 kg/m2). Using the simulated probability method, the mass loading related to the MEE is calculated based on the expected erupted mass (5 Â 1011 kg), the wind velocity profiles recorded during 14 years, and various column heights and grain-size populations. -
12. Eruption Alert at Rabaul Caldera: 1971–1994
12. Eruption Alert at Rabaul Caldera: 1971–1994 In a statement issued in Papua New Guinea on Monday [23 January 1984], the principal volcanologist, Dr P. Lowenstein, said that ‘evidence is accumulating to suggest that the volcano has embarked on an irreversible course towards the next eruption and that it is only a matter of time before this occurs … the eruption that was previously only a possibility is now much more likely to occur within the next few months’. Peter Hastings (1984) Crisis Build-up and Stage-2 Alert Villagers living near the south-eastern end of Matupit Island, Rabaul, were by 1970–1971 aware that nearby coastal clis had encroached perilously close towards their homes as a result of sea-wave erosion. Their concerns were alleviated after 1971, however, when a new beach began to form at the foot of the pumice clis which gradually became stranded inland. The south-eastern end of the island was rising episodically, following the two, major, Solomon Sea earthquakes that had shaken Rabaul in July 1971. Rabaul Volcanological Observatory (RVO) sta led by Rob Cooke began measuring the amount of ground uplift in 1973 using a survey line that ran southwards from Rabaul town to the end of the island. About 60 centimetres of uplift had been detected by 1979, the year of Cooke’s death, and to more than a metre by 1983.1 Matupit is a low-lying island that in 1971 was already well known for its vertical oscillations, most noticeably at times of major earthquakes or tsunamis when a causeway linking the island with the shore might disappear and then reform.2 The island is made up of at-lying pumice beds, but there is no persuasive geological evidence that it is, or ever was, an eruptive centre. -
Geology and Petrology of Rabaul Caldera, Papua New Guinea
Geology and Petrology of Rabaul Caldera, Papua New Guinea R. F. HEMING* Department of Geology and Geophysics, University of California, Berkeley, California 94720 ABSTRACT parison with experimental data for high- off the north coast of New Guinea and ter- alumina basalt also suggests a shallower minates at Rabaul. Only the New Britain Rabaul caldera is unusual in that it was origin. A progressive increase in Ti02, section has the classical features of an is- formed by two episodes of construction and A1203, and alkalis along the New land arc: a deep submarine trench to the collapse on an older basalt volcano. One Britain—New Guinea arc toward Rabaul at south, an inclined seismic zone dipping collapse occurred around 3,500 yr B.P. and its eastern end cannot be explained. Key northward, and a string of volcanoes on the the latest around 1,400 yr B.P. Both were words: igneous petrology, volcanology. side of the island opposite the trench. West accompanied by the eruption of daciiic of New Britain, the trench disappears, and pumiceous ash flows. Following initial col- INTRODUCTION in the vicinity of Long Island (Fig. 1), the lapse, volcanism was confined to a large Rabaul caldera, situated at the northeast- simple Benioff zone is replaced by a north- andesite volcano in the southern part of the ern tip of the island of New Britain, is the and a south-dipping zone (Denham, 1969). caldera, but a renewal of basaltic volcanism easternmost volcano of the New West of here, the volcanic arc lies well occurred at a point on the eastern ring frac- Guinea—New Britain arc (Fig. -
13. Eruptions at Rabaul: 1994–1999
13. Eruptions at Rabaul: 1994–1999 Many of our old folk (our patuana) knew that an eruption was imminent. The strength of the earthquakes told them that an eruption was only a matter of days or hours away … . But the government authorities had not said anything about an eruption … . The Volcanological Observatory, as we have always been told, has some of the most modern and sophisticated monitoring equipment which can predict an eruption to the minute. How come these machines have not said anything about an imminent eruption? Derol Ereman, a Boisen High School student from Matupit Island (quoted by Neumann, 1995, pp. 2–3). First Three Weeks Independence Day celebrations for the 19th national birthday of Papua New Guinea were interrupted by earthquake activity over the weekend in Rabaul beginning at 2.50–2.51 am on Sunday 18 September 1994. Two earthquakes about 40 seconds apart — one near Tavurvur the other near Vulcan — were felt strongly throughout the harbour area. Aftershocks and ground shaking continued, particularly in the Vulcan area. Rabaul Volcanological Observatory (RVO) volcanologists suspected, for about 12 hours, that the earthquake activity represented another ‘seismic swarm’, similar to many of those experienced in Rabaul during the 1970s and 1980s. The ground shaking continued and, by Sunday afternoon, villagers near Tavurvur on Matupit Island had begun a spontaneous evacuation into Rabaul town, encouraged by older people who recalled the 1937 volcanic eruption. Hundreds of other Matupits, however, remained on their threatened island.1 The number of people moving along the road grew, fed by other nearby communities, and by evening thousands of evacuees had gathered at oodlit Queen Elizabeth Park, an evacuation assembly point prescribed in the Rabaul Disaster Plan. -
Near-Real-Time Thermal Monitoring of Global Volcanism
Journal of Volcanology and Geothermal Research 135 (2004) 29–49 www.elsevier.com/locate/jvolgeores MODVOLC: near-real-time thermal monitoring of global volcanism Robert Wright*, Luke P. Flynn, Harold Garbeil, Andrew J.L. Harris, Eric Pilger Hawaii Institute of Geophysics and Planetology, University of Hawaii, 1680 East-West Road, Honolulu, HI 96822, USA Accepted 5 December 2003 Abstract MODVOLC is a non-interactive algorithm developed at the Hawaii Institute of Geophysics and Planetology (HIGP) that uses low spatial resolution (1-km pixel-size) infrared satellite data acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) to map the global distribution of volcanic thermal anomalies in near-real-time. MODVOLC scans the Level-1B MODIS data stream, on a pixel-by-pixel basis, for evidence of pixel and sub-pixel-sized high-temperature radiators. Once a hot spot has been identified its details (location, emitted spectral radiance, time, satellite observation geometry) are written to ASCII text files and transferred via FTP to HIGP, from where the results are disseminated via the internet http://modis.higp.hawaii.edu). In this paper, we review the underlying principles upon which the algorithm is based before presenting some of the results and data that have been obtained since its inception. We show how MODVOLC reliably detects thermal anomalies at a large number of persistently and sporadically active volcanoes that encompass the full range of common eruptive styles including Erebus (Antarctica), Colima (Me´xico), Karymsky (Kamchatka), Popocate´petl (Me´xico), Etna (Italy), and Nyiragongo (Democratic Republic of Congo), amongst others. We also present a few cautionary notes regarding the limitations of the algorithm and interpretation of the data it provides.