PACIFIC REGIONAL NAVIGATION INITIATIVE SAMOA Hydrographic
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High-Resolution Bathymetric Survey of Samoa
EU-SOPAC Project Report 112 Reducing Vulnerability of Pacific ACP States SAMOA TECHNICAL REPORT High-Resolution Bathymetric Survey Fieldwork Undertaken from 27 January to 1 March 2004 October 2008 Western Samoa three-dimensional Digital Elevation Model Prepared by: Jens Krüger and Salesh Kumar SOPAC Secretariat May 2008 PACIFIC ISLANDS APPLIED GEOSCIENCE COMMISSION c/o SOPAC Secretariat Private Mail Bag GPO, Suva FIJI ISLANDS http://www.sopac.org Phone: +679 338 1377 Fax: +679 337 0040 www.sopac.org [email protected] Important Notice This report has been produced with the financial assistance of the European Community; however, the views expressed herein must never be taken to reflect the official opinion of the European Community. Samoa: High-Resolution Bathymetry EU EDF-SOPAC Reducing Vulnerability of Pacific ACP States – iii TABLE OF CONTENTS EXECUTIVE SUMMARY ......................................................................................................... 1 1. INTRODUCTION ........................................................................................................ 2 1.1 Background ................................................................................................................ 2 1.2 Geographic Situation .................................................................................................. 2 1.3 Geological Setting ...................................................................................................... 3 1.4 Previous Bathymetry Compilations............................................................................ -
Solar Power Development Project
DRAFT Initial Environmental Examination Project Number: 49339-001 June 2017 SAM: Solar Power Development Project Prepared by Sun Pacific Energy Ltd This initial environmental is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. Your attention is directed to the “terms of use” section on ADB’s website. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. CONTENTS I. INTRODUCTION ............................................................................................................... 4 II. POLICY AND LEGAL FRAMEWORK ................................................................................ 4 III. PROJECT DESCRIPTION ................................................................................................. 5 A. Project Significance ........................................................................................................... 5 B. Site Description .................................................................................................................. 6 C. Project Schedule ................................................................................................................ 7 D. Project Components ......................................................................................................... -
Apolima Strait −13˚12' Samoa
Apolima Strait −13˚12' Samoa −13˚24' Fagamalo Asau Harbour Entrance Cape Mulinu’u −13˚36' Faga Sala’ilua Salelologa Passage Satupaitea Aganoa −13˚48' Apolima Strait Apia Harbour Entrance Mulifanua Warf Fugro Wave Buoy 1 −14˚00' Safata Bay Salani Fugro Wave Buoy 2 Nu’usafe’e Bay Cape Tapaga −14˚12' −173˚00' −172˚48' −172˚36' −172˚24' −172˚12' −172˚00' −171˚48' −171˚36' −171˚24' −171˚12' Figure 1. Location maps of the site. The map on the left shows the region. The map on the right shows the island and its surroundings. The red point shows to the actual site and green points (if present) indicate other available wave climate reports in the region. A copy of this report is available at http://gsd.spc.int/wacop/ I. General Wave Climate I.1 General Introduction This wave climate report presents wave information for Apolima Strait in Samoa. This report contains information about wind−generated surface gravity waves, often called wind waves and swell. The wave climate is defined here as the statistics of waves conditions over a 30 year period. The report details the average wave condition (page 2 and 3), the variability of wave conditions (page 4 and 5), severe and extreme waves (page 6 to 9) and characterises the wave energy resource(Page 10). Similar wave climate reports are available for more than 80 locations around the Pacific, near important ports, large settlements, tide gauge locations and areas where the wave climate is of particular interest. Other locations in Samoa are shown in Figure 1 (Previous page). -
2.1.4 Samoa Port of Mulifanua
2.1.4 Samoa Port of Mulifanua Port Overview Mulifanua is a village on the north-western tip of the island of Upolu. Mulifanua wharf is the main ferry terminal for inter-island vehicle and passenger travel across the Apolima Strait between Upolu and the island of Savai'i. The government's joint venture company Samoa Shipping Corporation (SSC) operates the ferry service, seven days a week, between Mulifanua and Salelologa at the east end of Savai'i Island. A one-way trip between the two islands takes about 90 minutes. The ferry usually runs every two hours during the day. SSC is also responsible for management of the port . The port is utilised solely as a ferry terminal, and as such there are no facilities at the port other than a passenger terminal, ticket office and roll on roll off wharf. In 2018 Mulifanau had an upgrade completed on the passenger and bus terminal. As a result of drifting sand, dredging operation is being planned to maintain channel width and depth. Port website: http://www.samoashipping.com/destinations/mulifanua Key port information may also be found at: http://www.maritime-database.com Port Location and Contact Country Samoa Province or District Upolu Island, Aiga-i-le-Tai district Nearest Town or City Mulifanau with Distance from Port (Village at the port) Port's Complete Name Port of Mulifanau Latitude -13.830154 Longitude -172.036398 Managing Company or Port Authority Samoa Shipping Company Management Contact Person Pipi Ioane Fomai ([email protected]) Nearest Airport and Airlines with Frequent International Arrivals/Departures Faleolo International Airport Air NZ, Virgin Australia, Samoa Airlines. -
SAMOA AVIATION INVESTMENT PROJECT Public Disclosure Authorized
GOVERNMENT OF SAMOA SAMOA AIRPORT AUTHORITY Public Disclosure Authorized SAMOA AVIATION INVESTMENT PROJECT Public Disclosure Authorized PACIFIC AVIATION INVESTMENT PROGRAMME FINAL REPORT Public Disclosure Authorized Report Prepared for: World Bank Samoa Airport Authority Report Prepared by: Public Disclosure Authorized On Behalf of: Chief Executive Officer Samoa Airport Authority Date Issued: OCTOBER 2013 Samoa Aviation Investment Project/EMP/SA October 2013 PACIFIC AVIATION INVESTMENT PROGRAMME, FALEOLO, UPOLU ISLAND, SAMOA FINAL DRAFT REPORT Acknowledgment The team wishes to formally acknowledge all those interviewed and consulted and especially the support of the following organisations Land Transport Authority Ministry of Women Community and Social Development Ministry of Natural Resources and Environment Ministry of Works Transport and Infrastructure Nuanua O le Alofa Samoa Bureau of Statistics Samoa Land Corporation Samoa Trust Estates Corporation Samoa Water Authority Village mayors and communities of Satapuala, Satui and Mulifanua Samoa Airport Authority ii Samoa Aviation Investment Project/EMP/SA October 2013 PACIFIC AVIATION INVESTMENT PROGRAMME, FALEOLO, UPOLU ISLAND, SAMOA FINAL DRAFT REPORT TABLE OF CONTENTS Preface ………………………..……………………………………………………………………. iv 1 The Team 2 Approach/Methodology 3 EMP and SA 4 Overall Findings 5 Priority Consideration 6 Final Remarks A Annexes as per Terms of Reference………………………………………………………………..vii 1 Terms of Reference...................................................................................................................vii -
Geological Subsidence and Sinking Islands: The
1 Symposium for W. Dickinson – SAA 2015 “Geological subsidence and sinking Islands: the case of Manono (Samoa)” Christophe Sand1, Jacques Bolé1, David Baret1, André-John Ouetcho1, Fiona Petchey2, Alan Hogg2 Tautala Asaua3 Abstract W. Dickinson, as part of his wide study of the geological history of the Pacific islands, has proposed in a series of papers to explainlinked the unique case of the deeply submerged Lapita site of Mulifanua in Western Upolu (Samoa), as linked to the slow subsidence of Upolu Island. Recent archaeological research on the neighbouring small island of Manono, has brought new and detailed data on this geological process. A series of new dates has allowed us to define chronologically the speed of the subsidence and demonstrateas well as the massive environmental changes that the local population had to adapt to over the past 2500 years. 1. Institute of Archaeology of New Caledonia and the Pacific (IANCP) 2. Radiocarbon Dating Laboratory, University of Waikato 3. Center for Samoan Studies, National University of Samoa 2 Introduction The geological diversity of the Pacific region defies any simple categorization. The region is, divided between different tectonic plates and, cut in two on its western side by the active “belt of fire”, with iIslands ranking being derived from continental fragments to old eroding or still active volcanic summits to simple coral aAtolls, defies any simple categorization. Volcanic activity, earthquakes and possible tsunami-related events, associated to episodes of extreme weather devastation through cyclones/typhoons or prolonged droughts make Oceania a region that often defies the idyllic image built by Western imagination. -
Climate of Samoa
DaDatata CCoollecllectiotionn aanndd mmodeodellillinnggffoor ar adadaptaptationtion Nusipepa Lepale Samoa Presentation OutlinePresentation Outline Background info Geography Climate of Samoa Impacts of Climate Change (CC) in Samoa CC Adaptation in Samoa Data Observation Network (Data collection) Modeling used in Samoa Responses to Climate Change in Samoa Samoa Climate Early Warning System (CLEWS) Background InformationBackground Information Samoa, officially the Independent State of Samoa (formerly known as Western Samoa and German Samoa), is a country governing the western part of the Samoan Islands in the South Pacific Ocean. It became independent from New Zealand in 1962. The two main islands of Samoa are Upolu and one of the biggest islands in Polynesia Savai'i. The capital city Apia and Faleolo International Airport are situated on the island of Upolu. The 1960 Constitution, which formally came into force with independence from New Zealand in 1962, is based on the British pattern of parliamentary democracy, modified to take account of Samoan customs The unicameral legislature (Fono) consists of 49 members serving 5-year terms. Forty-seven are elected from territorial districts by ethnic Samoans; the other two are chosen by non-Samoans with no chiefly affiliation on separate electoral rolls GeographyGeography The country is located east of the international date line and south of the equator, about halfway between Hawai‘i and New Zealand in the Polynesian region of the Pacific Ocean. The total land area is 2934 km² -
Report on Samoa
South Pacific Geoscience Commission (SOPAC) SAMOA COUNTRY REPORT National Consultant Report on: OCTOBER 2005 Promotion of Environmentally Sustainable Transportation in the Pacific Islands SOUTH PACIFIC GEOSCIENCE COMMISSION (SOPAC) NATIONAL CONSULTANT REPORT ON PROMOTION OF ENVIRONMENTALLY SUSTAINABLE TRANSPORTATION IN THE PACIFIC ISLANDS REPORT ON SAMOA TABLE OF CONTENTS GLOSSARY ..................................................................................................................... I EXECUTIVE SUMMARY ................................................................................................ 1 REPORT ON METHODOLOGY ..................................................................................... 3 1.0 INTRODUCTION .................................................................................................. 4 1.1 Environmentally Sustainable Transport.....................................................................................................4 1.2 Towards Achieving Environmental Sustainable Transport ......................................................................6 1.3 Sustainable Transport - Changing Our Way of Thinking.........................................................................9 1.4 Global Warming, Greenhouse Gases and Pollution.................................................................................12 1.5 The Pacific Context .....................................................................................................................................15 1.6 Samoa – A -
Samoa— Polynesian Diving in Upolu Text and Photos by Brandi Mueller
Samoa— Polynesian Diving in Upolu Text and photos by Brandi Mueller 22 X-RAY MAG : 98 : 2020 EDITORIAL FEATURES TRAVEL NEWS WRECKS EQUIPMENT BOOKS SCIENCE & ECOLOGY TECH EDUCATION PROFILES PHOTO & VIDEO PORTFOLIO travel Samoa Looking out from the shore past To-Sua Ocean Trench on Upolu Island in Samoa. PREVIOUS PAGE: Seafan and soft coral in Samoa Located in the Polynesian region The small, nine-passenger, turboprop Apia of the South Pacific Ocean, the airplane violently shook us up and down Our destination was Apia, Samoa, and like an amusement park ride. Out of the I was three days late coming in from idyllic paradise of Samoa, which windows, all I could see were the gray Pago Pago, American Samoa because comprises the two main islands clouds of the seemingly endless succes- the airport had been closed due to a of Savai'i and Upolu and sev- sion of storms that had been ravaging line of tropical storms and cyclones that eral smaller islands, is part of the area. just did not seem to stop. Several days Those of us in the back of the small earlier, my original flight from Honolulu the Commonwealth of Nations. plane could see into the cockpit and to Pago Pago had also been delayed Brandi Mueller managed to past the single pilot’s vision and his view for 24 hours due to unsafe weather venture to Upolu Island before was just as impenetrable with thick, dark conditions, and when it was time to the coronavirus pandemic clouds as what we saw through our win- make this short hop, the storms just kept dows. -
The Rare Plants of Samoa JANUARY 2011
The Rare Plants of Samoa JANUARY 2011 BIODIVERSITY CONSERVATION LESSONS LEARNED TECHNICAL SERIES 2 BIODIVERSITY CONSERVATION LESSONS LEARNED TECHNICAL SERIES 2 The Rare Plants of Samoa Biodiversity Conservation Lessons Learned Technical Series is published by: Critical Ecosystem Partnership Fund (CEPF) and Conservation International Pacific Islands Program (CI-Pacific) PO Box 2035, Apia, Samoa T: + 685 21593 E: [email protected] W: www.conservation.org Conservation International Pacific Islands Program. 2011. Biodiversity Conservation Lessons Learned Technical Series 2: The Rare Plants of Samoa. Conservation International, Apia, Samoa Author: Art Whistler, Isle Botanica, Honolulu, Hawai’i Design/Production: Joanne Aitken, The Little Design Company, www.thelittledesigncompany.com Series Editors: James Atherton and Leilani Duffy, Conservation International Pacific Islands Program Conservation International is a private, non-profit organization exempt from federal income tax under section 501c(3) of the Internal Revenue Code. ISBN 978-982-9130-02-0 © 2011 Conservation International All rights reserved. OUR MISSION Building upon a strong foundation of science, partnership and field demonstration, CI empowers societies to responsibly and sustainably care for nature for the well-being of humanity This publication is available electronically from Conservation International’s website: www.conservation.org ABOUT THE BIODIVERSITY CONSERVATION LESSONS LEARNED TECHNICAL SERIES This document is part of a technical report series on conservation projects funded by the Critical Ecosystem Partnership Fund (CEPF) and the Conservation International Pacific Islands Program (CI-Pacific). The main purpose of this series is to disseminate project findings and successes to a broader audience of conservation professionals in the Pacific, along with interested members of the public and students. -
Change in the Agricultural Land Use in West Upolu
UNIVERSITY OF HAWAII LIBRARY CHANGE IN THE AGRICULTURAL LAND USE IN WEST UPOLU WESTERN SAMOA THESIS SUBMITTED TO THE GRADUATE DIVISION OP UNIVERSITY OP HAWAII IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OP MASTER OF ARTS IN GEOGRAPHY SEPTEMBER 1967 By Nevin A. Bryant Thesis Committee: Peter N. D. Pirie, Chairman Robert M. Warner Forrest R. Pitts H^unA 635223 1 We certify that we have read this thesis and that in our opinion it is satisfactory in scope and quality as a thesis for the degree of Master of Arts in Geography. THESIS COMMITTEE TABLE OP CONTENTS Page LIST OP TABLES.................................... lv LIST OP F I G U R E S .................................. vi GLOSSARY OP SAMOAN TERMS ........................ Viii CHAPTER I. INTRODUCTION................. 1 CHAPTER II. THE PATTERN OP VILLAGE AGRICULTURE TODAY................ 8 The Land Tenure S y s t e m .... 8 The Pattern of Land Use ...... 16 CHAPTER III. SAMOAN AGRICULTURE PRIOR TO FOREIGN ADMINISTRATION.......... 28 The Pre-Contact Period .......... 28 Missionaries, Traders, and Wars . 31 CHAPTER IV. ADMINISTRATION RULE PRIOR TO WORLD WAR I I .................... 39 Stability Under German Rule 1900-1914 39 The New Zealand Occupation and Mandate until 1926 ....... 43 The Mau and the Depression 195^1936 ...................... 53 The Period Prior to World War II (1936-1942)............ 57 CHAPTER V. WORLD WAR II AND POSTWAR CHANGE . 60 The United States Armed Forces Occupation .............. 60 Postwar Agricultural Change .... 62 CHAPTER VI. THE PHYSICAL GEOGRAPHY AND CROP ECOLOGY OP WEST UPOLU ............ 75 Climate.......................... 75 So l i s........... 81 Crop Requirements................ 85 The Yearly Cycle of Planting and H a r v e s t i n g .............. -
Geoarchaeological Context of Holocene Subsidence at the Ferry Berth Lapita Site, Mulifanua, Upolu, Samoa
GEA(Wiley) INTERACTIVE Geoarchaeological Context of Holocene Subsidence at the Ferry Berth Lapita Site, Mulifanua, Upolu, Samoa William R. Dickinson Department of Geosciences, University of Arizona, Tucson, Arizona 85721 Roger C. Green Department of Anthropology, University of Auckland, Private Bag 92019, Auckland 1, New Zealand The 1973 discovery of an underwater archaeological site during dredging for a ferry landing at Mulifanua on Upolu raised important unanswered questions about the prehistory of Samoa, particularly the evolution of Holocene shorelines and relative local sea levels. A cultural horizon yielding Lapita potsherds, the only decorated Lapita assemblage yet found in Samoa and dating to ca. 2.8 ka, lies at a depth of 2.25 m below modern sea level beneath a capping of cemented paleobeachrock. With ¯uctuating hydro-isostatic sea level taken into account, the sherd occurrence implies subsidence of a former coastline by ca. 4 m at a mean rate of 1.4 mm/yr. Shoreline features on both Upolu and nearby Savai'i are fully compatible with bulk Holocene subsidence. We attribute the observed subsidence to down¯exure of the lithosphere from volcano loading centered on the Savai'i locus of historic volcanism, and conclude that any other Lapita sites that may exist in Samoa have subsided by a comparable amount. Al- though the Samoan linear volcanic chain resembles other Paci®c hotspot tracks where active volcano loading is con®ned to their southeastern ends, the most voluminous Holocene erup- tions in Samoa have occurred on Savai'i at the northwestern end of the exposed island chain. Samoan volcanism has evidently been in¯uenced by lateral ¯exure of the Paci®c plate as it moves past the northern extension of the Tonga subduction zone, and the active volcanism is apparently controlled by a longitudinal rift, which transects both Upolu and Savai'i and is superimposed upon older volcanic edi®ces that may record earlier hotspot volcanism.