Atoll Research Bulletin No. 342 Notes on the Birds Of
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Traditional Leadership in the Constitution of the Marshall Islands
TRADITIONAL LEADERSHIP IN THE CONSTITUTION OF THE MARSHALL ISLANDS by C. J. LYNCH Working Papers Series Pacific Islands Studies Center for Asian and Pacific Studies in collaboration with the Social Science Research Institute University of Hawaii at Manoa Honolulu, Hawaii Joe Lynch is a consultant on legislation and constitutional drafting whose long experience in the Pacific encompasses island areas in Micronesia, Melanesia, and Polynesia. Robert C. Kiste, Director Pacific Islands Studies Program Center for Asian and Pacific Studies University of Hawaii at Manoa Honolulu, Hawaii 96822 TRADITIONAL LEADERSHIP IN THE CONSTITUTION OF THE MARSHALL ISLANDS (With Comparative Notes) C. J. Lynch 1984 TABLE OF CONTENTS Preface v Introductory 1 Part I. THE COUNCIL OF IROIJ l. The precursors 3 2. Functions of the Council 4 (a) General 4 (b) Relations with the Nitijela 6 ( c) The Council in action 9 3. Composition of the Council 10 4. Procedures of the Council 13 5. Miscellaneous matters 14 6. Comparisons 16 (a) Palau 16 (b) The Federated States of Micronesia 17 (c) Yap 18 (d) Vanuatu 21 (e) Western Samoa 22 (f) The Cook Islands 22 (g) Comment 24 Part II. THE TRADITIONAL RIGHTS COURT 7. The Traditional Rights Court and the judicial system 27 ADDENDUM: Two problems of interpretation 8. Comparisons and comment 34 Part III. CONCLUSION 9. General comments 35 10. Is a traditional input desirable? 37 APPENDIX 42 NOTES 43 iii PREFACE It hardly needs to be said that this paper is written by a lawyer and from a lawyer's point of view. This fact, however , necessarily means that it is selective, firstly in the aspects of its subject that are considered and secondly in the detail (especially on non-legal aspects) into which it goes. -
Indigenous Encounters
From Islands to Atoll: Relating Reefs of History at Kwajalein Greg Dvorak 1. Atollism Islands of starvation, islands of abundance, islands of connectedness: the nearly one hundred flat coral islets that form Kwajalein in the Marshall Islands, the largest atoll on earth, are a gigantic ring on the water, strung together by a dynamic reef. The lagoon it encloses—indeed the entire atoll—is a microcosm of Oceania, a metaphor for the contradictory and interconnected histories of the contemporary world. I choose Kwajalein to explore the idea of “encounter” not only because it was the site of a major battle of the Pacific War and a place of unfathomable change throughout the twentieth century between Marshall Islanders, Japanese, and Americans; I focus on Kwajalein also because it was my childhood hometown, where I spent the first decade of my life. Because the main island of the atoll is leased to the US Army as a missile-testing base, my early years in American suburbia there provided my first taste of the ways in which huge nations and small localities intersect. Haunted by the ghosts of Japanese soldiers and the lullabies of our Marshallese housekeeper, I knew that this atoll had been home to many others before me, yet I felt linked to those other people through the common idea of home, and through the genealogy of the atoll itself. Coral colonizes: Polyps voyage in the ocean currents, joining with other coral communities atop subaquatic volcanoes that rise miles from the sea floor to break the surface. Their migrations are based on the flows of the sea, and their settlements are serendipitous. -
United States Army Garrison- Kwajalein Atoll Information Handbook
United States Army Garrison- Kwajalein Atoll Information Handbook Produced by DYNCORP INTERNATIONAL LLC Last updated: 4 September 2019 U.S. ARMY GARRISON KWAJALEIN ATOLL/ REAGAN TEST SITE U.S. ARMY INSTALLATION MANAGEMENT COMMAND KWAJALEIN ATOLL, MARSHALL ISLANDS I. INSTALLATION DATA Name of Site: The installation is currently called “United States Army Garrison - Kwajalein Atoll/ Ronald Reagan Ballistic Missile Defense Test Site” (USAG-KA/RTS) effective 01 October 2013. The installation has undergone multiple name changes since its inception: U.S. Army Kwajalein Atoll/ Ronald Reagan Ballistic Missile Defense Test Site (USAKA/RTS) from 15 June 2001 to 01 October 2013; U.S. Army Kwajalein Atoll/ Kwajalein Missile Range (USAKA/KMR) from 01 March 1998 to 15 June 2001; U.S. Army Kwajalein Atoll (USAKA) from 14 November 1986 to 30 September 1997; Kwajalein Missile Range (KMR) from 15 April 1968 to 13 November 1986; Kwajalein Test Site from 1 July 1964 to 14 April 1968. Between 1945 and 30 June 1964, while under the command of the United States Navy, the installation was referred to at various times as the Navy Operating Base Kwajalein, Naval Air Station Kwajalein, Naval Station Kwajalein and Pacific Missile Range Facility (PMRF) Kwajalein. Site Number: NQ100 [for Military Real Property Inventory purposes, assigned by the U.S. Army Chief of Engineers per paragraph 2.2.1 (3) of AR 405-45] U.S. Mail Address: PSC 701-PO Box 26, APO AP 96555-0001 Status: USAG-KA/RTS is a Class II site (Active) of the United States Army and is designated a subordinate activity of the U.S. -
Feasibility Study GREEN CLIMATE FUND FUNDING PROPOSAL I
Annex II – Feasibility Study GREEN CLIMATE FUND FUNDING PROPOSAL I FEASIBILITY STUDY Addressing Climate Vulnerability In the Water Sector (ACWA) United Nations Development Programme UNDP On behalf of Government of the Republic of the Marshall Islands RMI March 2018 For Submission to the Green Climate Fund EXECUTIVE SUMMARY The Republic of the Marshall Islands (RMI) is a small island developing states (SIDS) consisting of 29 coral atolls and 5 single islands. The nation is a large-ocean state, with approximately 1,225 islands and islets with a total land area of only 182 km2, spread across over 2 million km2 of vast ocean space. Most of the 24 inhabited local government jurisdictions (atolls and islands) are remote and lie merely 2 meters above sea level on average, posing various challenges and risks to sustainable development in face of climate change. RMI’s population in 2017 is estimated as 55,5621, most of which is concentrated in urban atolls of Majuro and Kwajalein (Ebeye)2. Context Climate Change: It is predicted, that RMI will face increasing sea level rise, increasing rainfall variability with potential for extended drought periods and increasing storm surges with climate change3, further aggravating RMI’s vulnerability and more specifically sustainable water supply. These climate change impacts are likely to exacerbate the risks of water shortages in RMI, by further challenging the ability of the Marshallese people to have access to safe freshwater resources year-round. Droughts and storm waves are some of the key climate based events that impact RMI. Climate projections show that in the next twenty-five years, rainfall and drought scenarios in RMI will continue and may increase in the short term4. -
TROPICAL STORM TALAS FORMATION and IMPACTS at KWAJALEIN ATOLL Tom Wright * 3D Research Corporation, Kwajalein, Marshall Islands
J16A.3 TROPICAL STORM TALAS FORMATION AND IMPACTS AT KWAJALEIN ATOLL Tom Wright * 3D Research Corporation, Kwajalein, Marshall Islands 1. INTRODUCTION 4,000 km southwest of Hawaii, 1,350 km north of the equator, or almost exactly halfway Tropical Storm (TS) 31W (later named Talas) between Hawaii and Australia. Kwajalein is the developed rapidly and passed just to the south of largest of the approximately 100 islands that Kwajalein Island (hereafter referred to as comprise Kwajalein Atoll and is located at 8.7° “Kwajalein”), on 10 December 2004 UTC. north and 167.7° east. Kwajalein is the southern-most island of Kwajalein Atoll in the Marshall Islands (see figure 2.2 Topography/Bathymetry 1). Despite having been a minimal tropical storm as it passed, TS Talas had a significant impact The islands that make up Kwajalein Atoll all lie not only on the residents of Kwajalein Atoll, but very near sea level with an average elevation of on mission operations at United States Army approximately 1.5 m above mean sea level. The Kwajalein Atoll (USAKA)/Ronald Reagan Test Site highest elevations are man-made hills which top (RTS). out at approximately 6 m above mean sea level. This paper will describe the development and evolution of TS Talas and its impacts on Kwajalein Atoll and USAKA/RTS. Storm data, including radar, satellite, and surface and upper air observations, and a summary of impacts will be presented. A strong correlation between Tropical Cyclone (TC) frequency and the phase of the El Niño Southern Oscillation (ENSO) has been observed for the Northern Marshall Islands. -
The Shallow-Water Crinoid Fauna of Kwajalein Atoll, Marshall Islands: Ecological Observations, Interatoll Comparisons, and Zoogeographic Affinities!
Pacific Science (1985), vol. 39, no. 4 © 1987 by the Univers ity of Hawaii Press. All rights reserved The Shallow-Water Crinoid Fauna of Kwajalein Atoll, Marshall Islands: Ecological Observations, Interatoll Comparisons, and Zoogeographic Affinities! D. L. ZMARZLy 2 ABSTRACT: Twelve species ofcomatulid crinoids in three families were found to inhabit reefs at Kwajalein Atoll during surveys conducted both day and night by divers using scuba gear. Eleven of the species represent new records for the atoll, and five are new for the Marshall Islands. A systematic resume of each species is presented, including observations on die! activity patterns, degree of exposure when active, and current requirements deduced from local distri butions. More than half of the species were strictly nocturnal. Densities of nocturnal populations were much higher than those typically observed during the day . Occurrence and distribution ofcrinoids about the atoll appeared to be influenced by prevailing currents. Some species, of predominantly cryptic and semicryptic habit by day, occurred at sites both with and without strong currents. While these species were able to survive in habitats where currents prevailed, they appeared not to require strong current flow. In contrast, the remaining species, predominantly large, fully exposed comasterids, were true rheophiles; these were found on seaward reefs and only on lagoon reefs in close proximity to tidal passes. Comparison of crinoid records between atolls in the Marshall Islands shows Kwajalein to have the highest diversity, although current disparities between atolls in the number of species recorded undoubtedly reflect to some extent differences in sampling effort and methods. Based on pooled records, a total of 14 shallow-water crinoid species is known for the Marshall Islands, compared with 21 for the Palau Archipelago and 55 for the Philippines. -
KW 15, 1955 Northern Marshall Islands Lkpedition, 1951-1952
ATOLL RLSZiRCkI BULLSTIN Northern Marshall Islands Expedition, 1951-1952. Land biota: Vascular plants. by F, R. F'osberg Issued by THE PACIFIC SCILiVCE BOliHD National Academy of Sciences-National Research Council :lashington, D. C. KW 15, 1955 Northern Marshall Islands lkpedition, 1951-1952. Land biota: Vascular plants .ly2 by F. 8. Fosberg 3 1/ Publication authorized by the Di.rector, U. S. Geological Survey Preli!ninary results of the lkpedition to the Northern Elarshall Islands, 1951-1352, 110.2. Botanist, U. S, Geological Survey . Northern Narshall Islands Zxpedition; 1951-1952. Land biota: Vascular plants. by F. 3. Fosberg , . Following the nhrrative of the expedi-tion to the northern Karshalls made in 1951 and 1952, it seems north whi1.e to present the raw dsta collected in a series of: prel3minary papers, to make them available for general use and reference xitilout waiting urlbil tLey are cc:npletely studied and interpreted. Formal pubiicri.tion of a more parmanent charactsr is planned as detailed .studies are co;u$eted. This paper presents distribu- tional and ecological records, as aell as r~iitiverimes, of the vascular plants coliected on the expedition.. TQ these have beer1 added recorus from the author% 1946 and. 1950 coLlections, a few Wake &lad collections made in 1953, a~cja few miscell.acileo;ls collections by others. Other signi- ficant collections fromthe nort,%ern Marsilr:lis, not included here, are those of NU. Randolph Taylor, pubiished by hiin iri his MI'lants of Bikini," ttiose , made by Adelbert de . Ct~aniissowkii,.e on the Zotzebue ikpeditionJ and those made on several [email protected] . -
BORA BORA Bora Borabora 156 © Lonelyplanetpublications (Guesthouses), Often Situated Onsomeofthebestreal Estate, Inwhichtorest Yourhead
© Lonely Planet Publications 156 www.lonelyplanet.com BORA BORA •• History 157 HISTORY deterring visitors because of overdevelop- In ancient times, the island was known as ment, while at the same time its major Vava’u, perhaps supporting the theory that it drawcard – marine life – is seriously under Bora Bora was colonised by inhabitants from the Ton- threat. Let’s hope the juggling act can be gan island of the same name. ‘Bora Bora’ managed, because this is a truly beautiful roughly translates as ‘first-born’, indicating part of the world. that this may have been the most impor- tant island after Ra’iatea. According to local ORIENTATION Bora Bora will seduce you into buying the Cadillac of paradises, the one loaded with all myth, the legendary Hiro, the first king of Bora Bora was created by volcanic activity the luxury trappings you know you don’t need but just can’t live without. Legendary not Ra’iatea, sent his son Ohatatama to rule Bora around three or four million years ago. The only for its lush beauty but also its hedonistic decadence, this island is a fairy-tale creation Bora. rim of the ancient volcano can be easily of jagged volcanic peaks juxtaposed against crystal-clear aqua lagoons. One of the world’s Due to the shortage of level ground on traced; the sea has broken into the crater to Bora Bora, land pressures created an unusu- form Povai Bay at the southern tip of the is- most famous dream destinations, Bora Bora lures honeymooners, heiresses and movie stars ally defensive population of fierce warriors. -
The State of Coral Reef Ecosystems of the United States
STATUSSTATUS OFOF THETHE CORALCORAL REEFSREEFS ININ THETHE PACIFICPACIFIC FREELYFREELY ASSOCIATEDASSOCIATED STATESSTATES CharlesCharles Birkeland,Birkeland, AhserAhser Edward,Edward, YimnangYimnang Golbuu,Golbuu, JayJay Gutierrez,Gutierrez, NoahNoah Idechong,Idechong, JamesJames Maragos,Maragos, GustavGustav Paulay,Paulay, RobertRobert Richmond,Richmond, AndrewAndrew Tafileichig,Tafileichig, andand NancyNancy VanderVander VeldeVelde From east to west, the Freely Associated States 14o N, the Marshalls have a total dry land area of include the Republic of the Marshall Islands (the only about 181.3 km2. However, when the Exclu Marshalls or the RMI), the Federated States of sive Economic Zone (by statute, from the shoreline Micronesia (FSM), and the Republic of Palau. The to 200 miles offshore) is figured in, the Republic Federated States of Micronesia – Kosrae, Pohnpei, covers 1,942,000 km2 of ocean within the larger Chuuk, and Yap – along with Palau, are known as Micronesia region. There are 11,670 km2 of sea FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES the Caroline Islands, which are among the longest within the lagoons of the atolls. FREELY ASSOCIATED STATES FREELY ASSOCIATED STATES island chains in the world at 2,500 km. Land only makes up less than 0.01% of the area of All of these Micronesian islands were formerly a the Marshall Islands. Most of the country is the part of the Trust Territory of the Pacific Islands broad open ocean with a seafloor that reaches 4.6 administered by the United States after World War km (15,000 ft). Scattered throughout are nearly a II. -
Survival of Rats at Eniwetok Atolli WILLIAM B
Survival of Rats at Eniwetok AtollI WILLIAM B. JACKSON2 THE STORY of rats at Eniwetok Atoll (Marshall While proof is lacking, I believe that the only Islands) and their apparently uncanny ability to rodent at Eniwetok Atoll prior to the initiation survive atomic detonations and inhabit areas of the AEC program in 1946 was the Polynesian with high levels of radiation has been referred rat (Rattus exulans). This is the common rat of to in various documents (Berrill, 1966; Hines, the Pacific islands, having moved with the 1962 and 1966; French, 1965; Woodbury, Micronesians from island to island. Probably 1962); all are to some degree incomplete or in only the larger islets of the atoll (those with error. The purpose of this paper is to pull to coconut plantings) were infested. gether the fragments of data that are available Although the Germans, and later the Japa and, at this late date, attempt to piece together nese, were active in the Marshall Islands in the the story of the survival of rat populations at first half of the twentieth century, no specific Eniwetok. records of rodents for Eniwetok Atoll seem to exist. St. John (1960) indicated that no botan HISTORICAL BACKGROUND ical accounts existed from German (or the Eniwetok and Bikini atolls in the northern earlier Spanish) explorations. While botanical Marshall Islands were involved in the United collections were made by the Japanese, I can States nuclear testing program between 1946 find no descriptions of rats, and no rodent and 1958. During this period six major opera specimens from Eniwetok Atoll were present whe~ exa~ined tions were carried out at Eniwetok Atoll and I the collection in the Japanese involved some 40 detonations. -
Terminal Evaluation: Undp Gef Project (Id 2568) Renewable Energies (Admire)” 12 May 2016
TERMINAL EVALUATION: UNDP GEF PROJECT (ID 2568) “ACTION FOR THE DEVELOPMENT OF MARSHALL ISLANDS RENEWABLE ENERGIES (ADMIRE)” 12 MAY 2016 AMITAV RATH i Acknowledgements I am grateful to many people for their cooperation and assistance during the conduct of this evaluation and wish to thank them for providing time for meetings, interviews and for answering many questions in person and by email and phone. Special thanks are due to all the persons (listed in the third annex) who provided time and valuable insights and information and contributed to this evaluation. Special thanks are due to the staff of the Ministry of Resources and Development, Republic of the Marshall Islands for their support during the evaluation mission and to the staff of UNDP in Fiji and Bangkok, who provided many documents, shared their insights and provided full assistance. Individual mention and acknowledgement are due to ‐ Walter Myazoe at MRD, who provided a very wide set of documents on the many different energy related cooperation activities in RMI, without which my understanding of the situation would have been very inadequate; Dolores deBrum Kattil, the Project Manager who provided me with the considerable documentation on the project and made all arrangements for the meetings in RMI; Ned Lobwij at MRD who stepped in to make many interviews and meetings actually happen, as Annex 3. Special acknowledgements are due to Emma Mario, the Environment Programme Analyst at the UNDP Fiji MCO for discussions and additional documents; Thomas Jensen, Energy Programme Specialist at the UNDP Pacific Centre, Fiji, for extensive comments to the first draft; and to Manuel L. -
University of California, Berkeley of These Two Populations and Will Attempt to Discuss the Causes of Some Of
A STUDY OF THE RELOCATION OF TWO MARSHALLESE ATOLL COMMUNITES Anne Chambers University of California, Berkeley The effects of forced relocation on Bikini and Enewetak populations of the Marshall Islands are compared. The problems of adaptation to different environmental conditions are discussed. Administrative insistence on speedy resettlement and its failure to realize aspects of the relocated peoples' ecological, political, and social relationships are seen as contributing to the failure of the Bikinians to make a successful adaptation. (Bikini, culture change, ecology, Enewetak, Marshall Islands, Micronesia, relocation) Early in 1946, the Atomic Energy Commission decided to use Bikini Atoll in the Marshall Islands as the site of controlled atomic bomb explosions and the U.S. Navy, administrator of the area, was given the responsibility of relocating the atoll's 167 residents. The decision to use Bikini was based on the atoll's distance from heavily populated areas, air routes, and sea routes; its small population; and the predictability of winds in the area (Kiste 1968:1). About a year later, it was decided that the residents of neighboring Enewetak Atoll would also have to be relocated. This paper will compare and contrast the processes and effects of the relocation of these two populations and will attempt to discuss the causes of some of the problems encountered. Bikini Atoll is the northernmost atoll in the western chain of the Marshall Islands. Enewetak Atoll lies about 150 miles almost due west of Bikini (see map). Three other atolls or islands are significant in the relocation story of the people of Bikini and Enewetak.