Abstract Micronesia Received Several Human Dispersals in the Prehistoric Period
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Ecology in Palau Chapter 1
ECOLOGY IN PALAU CHAPTER 1 CHAPTER 1 also has the largest tract of tropical lowland Ecology in Palau forest in the Pacific (Kitalong, 2014). In 1979, nearly 218 km2 or 52% of Palau’s land was The landscape of Palau is one of a medium to covered with lowland forests. Yet, slowly, forests low volcanic island chain with large fringing ECOLOGY IN PALAU are being cut for homesteads, development and/or barrier reefs. The Palauan island chain and roads. Forest trees and plants are valued as has all three-island types: volcanic, limestone Christopher Kitalong, David Mason sources of timber, food, medicine, habitat for and atolls. Palau’s proximity to the Asian other species, and for their cultural and aesthetic continent, Philippines, and Indonesia results Settings value (Kitalong, 2008). in increased radiation of plant taxa compared The archipelago of Palau was formed during to other islands in Micronesia. Despite being the Eocene epoch, 40 million years ago by the closest Micronesian island to larger land the subduction of the Pacific Plate beneath masses, Palau is still relatively isolated. Due the Philippine Plate along the Kyushu-Palau to these factors, Palau has the greatest number Ridge (PALARIS, 2009). Palau lies on the of endemics and highest species richness in east edge of the Andesite Line, which divides the Micronesian island chain (Canfield, 1981). the deeper basalts of the Central Pacific Basin However, the amount of arable soil is very from the partially submerged continental areas limited and very prone to erosion. As suggested of andesite. Volcanism ceased 20 million years by the USDA report deposited at Forestry ago and was succeeded by submergence of Service in Palau, islands and formation of the barrier reef began. -
Provenance Studies of Polynesian Basalt Adze Material: a Review and Suggestions for Improving Regional Data Bases
Provenance Studies of Polynesian Basalt Adze Material: A Review and Suggestions for Improving Regional Data Bases MARSHALL 1. WEISLER PACIFIC ARCHAEOLOGISTS have long been interested in the settlement of Polyne sia, the origin of colonizing groups at distant archipelagoes, and subsequent social interaction between island societies (see, for example, Howard 1967; Irwin 1990; Kirch and Green 1987). Early material studies in Polynesia inferred migration routes and social interaction from the distribution of similar architecture, especially marae (Emory 1943; also R. Green 1970), adzes (Emory 1961), and fishhooks (Sinoto 1967). The identification of exotic raw materials and finished artifacts throughout Polynesia eliminates the ambiguity often presented by linking stylistic similarities across space and through time. In relation to the long history of identifying exotic lithic materials from archaeological sites (see, for example, Grimes 1979), the compositional analysis of oceanic obsidians was begun quite recently (Key 1968). The efficacy of chemical characterization of artifacts and quarry material in New Zealand provided the in centive to apply similar techniques to obsidian of the southwest Pacific, where several large sources were known and where the archaeological distribution of this material was tl)ought to be widespread (Ambrose 1976). Although it has been possible to define the spread and interaction of human groups in the southwest Pacific by determining the spatial and temporal distribution of obsidian and pot tery, these materials are restricted to a few areas in Polynesia. Consequently, the effort to document prehistoric interaction throughout Polynesia must proceed without using obsidian or pottery. This leaves only basalt (debitage, formed arti facts, and oven stones), pearlshell, and volcanic glass as material for distributional studies (Best et al. -
The Cultural Landscapes of the Pacific Islands Anita Smith 17
World Heritage Convention Cultural Landscapes of the Pacific Islands ICOMOS Thematic study Anita Smith and Kevin L. Jones December 2007 ICOMOS 49-51 rue de la Fédération – 75015 Paris Tel +33 (0)1 45 67 67 70 – Fax +33 (0)1 45 66 06 22 www.icomos.org – [email protected] Contents Part 1: Foreword Susan Denyer 3 Part 2: Context for the Thematic Study Anita Smith 5 - Purpose of the thematic study 5 - Background to the thematic study 6 - ICOMOS 2005 “Filling the Gaps - An Action Plan for the Future” 10 - Pacific Island Cultural Landscapes: making use of this study 13 Part 3: Thematic Essay: The Cultural Landscapes of the Pacific Islands Anita Smith 17 The Pacific Islands: a Geo-Cultural Region 17 - The environments and sub-regions of the Pacific 18 - Colonization of the Pacific Islands and the development of Pacific Island societies 22 - European contact, the colonial era and decolonisation 25 - The “transported landscapes” of the Pacific 28 - Principle factors contributing to the diversity of cultural Landscapes in the Pacific Islands 30 Organically Evolved Cultural Landscapes of the Pacific 31 - Pacific systems of horticulture – continuing cultural landscapes 32 - Change through time in horticultural systems - relict horticultural and agricultural cultural landscapes 37 - Arboriculture in the Pacific Islands 40 - Land tenure and settlement patterns 40 - Social systems and village structures 45 - Social, ceremonial and burial places 47 - Relict landscapes of war in the Pacific Islands 51 - Organically evolved cultural landscapes in the Pacific Islands: in conclusion 54 Cultural Landscapes of the Colonial Era 54 Associative Cultural Landscapes and Seascapes 57 - Storied landscapes and seascapes 58 - Traditional knowledge: associations with the land and sea 60 1 Part 4: Cultural Landscape Portfolio Kevin L. -
[.35 **Natural Language Processing Class Here Computational Linguistics See Manual at 006.35 Vs
006 006 006 DeweyiDecimaliClassification006 006 [.35 **Natural language processing Class here computational linguistics See Manual at 006.35 vs. 410.285 *Use notation 019 from Table 1 as modified at 004.019 400 DeweyiDecimaliClassification 400 400 DeweyiDecimali400Classification Language 400 [400 [400 *‡Language Class here interdisciplinary works on language and literature For literature, see 800; for rhetoric, see 808. For the language of a specific discipline or subject, see the discipline or subject, plus notation 014 from Table 1, e.g., language of science 501.4 (Option A: To give local emphasis or a shorter number to a specific language, class in 410, where full instructions appear (Option B: To give local emphasis or a shorter number to a specific language, place before 420 through use of a letter or other symbol. Full instructions appear under 420–490) 400 DeweyiDecimali400Classification Language 400 SUMMARY [401–409 Standard subdivisions and bilingualism [410 Linguistics [420 English and Old English (Anglo-Saxon) [430 German and related languages [440 French and related Romance languages [450 Italian, Dalmatian, Romanian, Rhaetian, Sardinian, Corsican [460 Spanish, Portuguese, Galician [470 Latin and related Italic languages [480 Classical Greek and related Hellenic languages [490 Other languages 401 DeweyiDecimali401Classification Language 401 [401 *‡Philosophy and theory See Manual at 401 vs. 121.68, 149.94, 410.1 401 DeweyiDecimali401Classification Language 401 [.3 *‡International languages Class here universal languages; general -
Final Yap Report2
The Integration of Traditional and Modern Systems of Environmental Management and the Use of Public-Private Partnerships in Natural Resource Management and Tourism Development in the State of Yap, Federated States of Micronesia A Field Study with Observations and Recommendations Asian Development Bank TA No. 6039 – REG Formulating a Pacific Region Environmental Strategy (PRES) Contract No. COCS/03-139 Richard S. Stevenson Mantaray Management LLC 15 April 2003 The views expressed in this book are those of the authors and do not necessarily reflect the views and policies of the Asian development Bank, or its Board of Governors or the governments they represent. The Asian Development Bank does not guarantee the accuracy of the data included in this publication and accepts no responsibility for any consequences of their use. Use of the term “country” does not imply any judgment by the authors or the Asian Development Bank as to the legal or other status of any territorial entity. Acknowledgements Many gracious and knowledgeable people of Yap contributed generously of their time and their thoughts to the research for this paper. They welcomed enquiry into sometimes-difficult subjects and were patient and candid in their responses to endless questions. Busy leaders from the state and FSM government, the traditional leadership system, the private sector and the non- governmental organizations were always able and willing to find time to talk. Without them the study would not have been possible. Their names are listed in Appendix 1 of the paper. Special thanks are offered to John Wayaan, owner and manager of the Pathways Hotel who provided critical assistance in suggesting whom to interview and in making the needed introductions. -
EVIDENCE for the ORIGINS of the CHAMORRO PEOPLE of the MARIANA ISLANDS a Paper Presented to Dr. Douglas Oliver Dr. Donald Toppin
..;:, EVIDENCE FOR THE ORIGINS OF THE CHAMORRO PEOPLE OF THE MARIANA ISLANDS A Paper Presented to Dr. Douglas Oliver Dr. Donald Topping Dr. Timothy Macnaught In Partial Fulfillment Of the Requirements for the Degree M.A. in Pacific Island Studies by Robert Graham University of Hawaii November, 1977 '1'l1e Pacific Islands Program, Plan B, requires: "The student's demonstration of research capacity by the submission a major paper prepared for a 600 or 700 numbered research course." (1977-1979 Graduate Information Bulletin, University of Hawaii, ~anoa, p.B7) The submission of this paper to Drs. Oliver, Topping and Macnaught represents the fulfillemnt of that requirement. The paper was researched and written in the Gprin~ semester of 1977 for a course in the ESL department (ESL 660, Sociolinguistics). Since that time I have submitted this manuscript to a number of people to read and comment on. In rewriting this paper in Oct:>ber, 1977, I have made use of their comments and suggestions. Those who have commented on the paper include Dr. Richard Schmidt, to whom the paper was originally submitted, Dr. Donald Topping (SSLI and authority on Chamorro language), Dan Koch (Chamorro languaGe teacher) and Lolita Huxel (Chamorro language teacher). To them go my thanks for advice. Of course all responsibility remains my own. Robert Graham October, 1977 TABLE OF CONTENTS Table of Contents •...•...•. · . .. • 1 The Setting .......•..... ...• ii Map of Oceania ..••. .. · .... ·. iii Map of Marianas ..•...••... · . .. i v Chapter I The Evidence Through Language Splitting ...• 1 Dyen's Work.. .•.•......• . 4 Conclusions .. •• ••••.•••• • 7 Chapter II Ethnographic Evidence for Early Origins • • 7 Conclusions . -
Geology of Saipan Mariana Islands Part 2
Geology of Saipan Mariana Islands Part 2. Petrology and Soils GEOLOGICAL SURVEY PROFESSIONAL PAPER 280-B-D Geology of Saipan Mariana Islands Part 2. Petrology and Soils GEOLOGICAL SURVEY PROFESSIONAL PAPER 280-B-D Chapter B. Petrology of the Volcanic Rocks By ROBERT GEORGE SCHMIDT Chapter C. Petrography of the Limestones By J. HARLAN JOHNSON Chapter D. Soils By RALPH J. McCRACKEN UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR Fred A. Seaton, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS OF PART 2 Page Chapter B. Petrology of the Volcanic Rocks .... 127 Chapter C. Petrography of the Limestones ...... 177 Chapter D. Soils ................................ 189 m GEOLOGICAL SURVEY PROFESSIONAL PAPER 280 Geology of Saipan, Mariana Islands Part 1. General Geology Chapter A. General Geology By PRESTON E. CLOUD, JR., ROBERT GEORGE SCHMIDT, and HAROLD W. BURKE Part 2. Petrology and Soils Chapter B. Petrology of the Volcanic Rocks By ROBERT GEORGE SCHMIDT Chapter C. Petrography of the Limestones By J. HARLAN JOHNSON Chapter D. Soils By RALPH J. McCRACKEN Part 3. Paleontology Chapter E. Calcareous Algae By J. HARLAN JOHNSON Chapter F. Discoaster and Some Related Microfossils By M. N. BRAMLETTE Chapter G. Eocene Radiolaria By WILLIAM RIEDEL Chapter H. Smaller Foraminifera By RUTH TODD dhapter I. Larger Foraminifera By W. STORRS COLE ^Chapter J. Echinoids By C. WYTHE COOKE ~Part 4. Submarine Topography and Shoal-Water Ecology ^Chapter K. Submarine Topography and Shoal-Water Ecology By PRESTON E. CLOUD, JR. -
Stone Tools from the Ancient Tongan State Reveal Prehistoric Interaction Centers in the Central Pacific
Stone tools from the ancient Tongan state reveal prehistoric interaction centers in the Central Pacific Geoffrey R. Clarka,1, Christian Reepmeyera, Nivaleti Melekiolab, Jon Woodheadc, William R. Dickinsond, and Helene Martinsson-Walline aArchaeology and Natural History, College of Asia and the Pacific, Australian National University, Canberra, ACT 0200, Australia; bLapaha Town Council, Lapaha Village, Tongatapu, Kingdom of Tonga; cSchool of Earth Sciences, The University of Melbourne, Parkville, VIC 3010, Australia; dDepartment of Geoscience, University of Arizona, Tucson, AZ 85721; and eDepartment of Archaeology and Ancient History, Gotland Campus, Uppsala University, 75105 Uppsala, Sweden Edited by Patrick V. Kirch, University of California, Berkeley, CA, and approved June 10, 2014 (received for review April 2, 2014) Tonga was unique in the prehistoric Pacific for developing a mari- involved control and distribution of prestige exotic goods by elites time state that integrated the archipelago under a centralized and whether the polity’s interaction sphere was only one of several authority and for undertaking long-distance economic and political prehistoric networks responsible for the movement of people, exchanges in the second millennium A.D. To establish the extent goods, and ideas in the Central Pacific. of Tonga’s maritime polity, we geochemically analyzed stone tools This article reports the analysis of a significant lithic artifact excavated from the central places of the ruling paramounts, par- assemblage recovered during recent excavations of sites of the ticularly lithic artifacts associated with stone-faced chiefly tombs. Tongan polity, which was manifested by the construction of The lithic networks of the Tongan state focused on Samoa and Fiji, religo-political centers containing monumental architecture on with one adze sourced to the Society Islands 2,500 km from Ton- the island of Tongatapu (297 km2), where the political hier- gatapu. -
Locating Proto Oceanic
2 Locating Proto Oceanic _________________________________________________________________________ ANDREW PAWLEY 1 Introduction This chapter briefly describes the major biogeographical regions of Oceania and Island Southeast Asia, summarises the evidence for locating the Proto Oceanic speech community in the Bismarck Archipelago, and refers to the range of environments and environmental features to be encountered there.1 2 The major biogeographic regions of Oceania Oceania is often divided into three main geographic regions: Melanesia, Polynesia and Micronesia. However, a more useful primary division for understanding the history of plants and animals, and, particularly, of humans in the Pacific is between Near Oceania and Remote Oceania.2 Modern Near Oceania consists of Australia and that part of the Pacific Islands whose chief land masses are New Guinea, the Bismarck archipelago and the Solomons archipelago, extending as far east as Makira (formerly known as San Cristobal). Some of the islands in Near Oceania are formidable in their size and rugged terrain. New Guinea is 2300 km long and has a mountainous interior that extends the length of the island, with peaks reaching 4500 m. New Britain is 480 km long and from 50 to 80 km across, mountainous and actively volcanic. New Ireland is 350 km long though never more than 50 km across. Bougainville is more compact but has a landmass similar to New Ireland. The islands of Near Oceania for the most part form an intervisible series of landmasses which served as stepping-stones for the dispersion of plants, animals and people, enhanced at times by lower sea levels during the late Pleistocene. 1 I am indebted to Roger Green, Meredith Osmond, Malcolm Ross and Christophe Sand for helpful comments on a draft of this chapter. -
The Lexicon of Proto Oceanic the Culture and Environment of Ancestral Oceanic Society
The lexicon of Proto Oceanic The culture and environment of ancestral Oceanic society 2 The physical environment Pacific Linguistics 545 Pacific Linguistics is a publisher specialising in grammars and linguistic descriptions, dictionaries and other materials on languages of the Pacific, Taiwan, the Philippines, Indonesia, East Timor, southeast and south Asia, and Australia. Pacific Linguistics, established in 1963 through an initial grant from the Hunter Douglas Fund, is associated with the Research School of Pacific and Asian Studies at The Australian National University. The authors and editors of Pacific Linguistics publications are drawn from a wide range of institutions around the world. Publications are refereed by scholars with relevant expertise, who are usually not members of the editorial board. FOUNDING EDITOR: Stephen A. Wurm EDITORIAL BOARD: John Bowden, Malcolm Ross and Darrell Tryon (Managing Editors), I Wayan Arka, David Nash, Andrew Pawley, Paul Sidwell, Jane Simpson EDITORIAL ADVISORY BOARD: Karen Adams, Arizona State University Lillian Huang, National Taiwan Normal Alexander Adelaar, University of Melbourne University Peter Austin, School of Oriental and African Bambang Kaswanti Purwo, Universitas Atma Studies Jaya Byron Bender, University of Hawai‘i Marian Klamer, Universiteit Leiden Walter Bisang, Johannes Gutenberg- Harold Koch, The Australian National Universität Mainz University Robert Blust, University of Hawai‘i Frantisek Lichtenberk, University of David Bradley, La Trobe University Auckland Lyle Campbell, University of Utah John Lynch, University of the South Pacific James Collins, Universiti Kebangsaan Patrick McConvell, Australian Institute of Malaysia Aboriginal and Torres Strait Islander Bernard Comrie, Max Planck Institute for Studies Evolutionary Anthropology William McGregor, Aarhus Universitet Soenjono Dardjowidjojo, Universitas Atma Ulrike Mosel, Christian-Albrechts- Jaya Universität zu Kiel Matthew Dryer, State University of New York Claire Moyse-Faurie, Centre National de la at Buffalo Recherche Scientifique Jerold A. -
Volcanoes Flying Through Volcanic Ash Can Be
Volcanoes Flying through volcanic ash can be hazardous to your plane! ⇒ 1982 British Airways ⇒ 1989 KLM Boeing 247 from Alaskan Volcano ⇒ 1991 Mount Pinatubo ⇒ Since 1990 damage to at least 15 aircraft Volcanoes are not all bad: 1) Esthetic beauty 2) Skiing and hiking 3) Soils can be productive However, of course they can kill. Who Should Worry? In short – People who live on plate boundaries. ⇒ Most dangerous, convergent plate boundaries with subduction zones ⇒ 900/1350 volcanoes that have erupted are on the Pacific ring of fire (N.Z., Japan, Alaska, Mexico, C.A., Chile) Mt. Erebus of Antarctica is the farthest south ⇒ Other famous: Mediterranean – Vesuvius, Etna, Stromboli Stromboli - “Lighthouse of the Mediterranean” ⇒ Most active – mild eruption of fluid lava, typically at Divergent Plate Boundaries ⇒ 2x more volcanoes north of the equator Can affect world climate Examples: Tamboru (1815), El Chichon (1982), Mt. Pinatubo (1991) ⇒ Us- no one east of New Mexico (Figure 5.2 &5.3) – tectonics Main mainland U.S. zone – Cascadia Subduction Zone ⇒ WA, OR, CA “Alaska is the second most active volcanic region in the world, and Hawaii is not far behind.” Nature of the Problem VEI – Volcanic Explosivity Index (Figures 5.4 & 5.5) ⇒ Related to volume of stuff erupted, height it rises, and duration of eruption ⇒ Mount St. Helens (1980) – Explosive to Cataclysmic – 4 ⇒ VEI can increase with time ⇒ Magnitude and frequency – Yellowstone (cataclysmic book) ⇒ Magma’s viscosity is important T↑, V↓ or T↓, V↑ Silica: the more siliceous, the more viscous Felsic vs. Mafic and the Andesite Line Andesite Line: From Alaska to east of N.Z. -
The Geology of Tofua Island, Tonga!
The Geology of Tofua Island, Tonga! GLENN R. BAUER2 ABSTRACT: Tofua Island is an oval, steep-sided composite volcano, 5 miles by 6 miles in diameter, the summit of which has collapsed to form a caldera. Within the caldera, Lofia cone is still active. Four units have been mapped: (1) the Hamatua Formation, of precaldera age, includes basaltic andesites, pyroxene andesites, and pyroxene dacites; (2 ) the Hokula Froth Lava, a microvesiculated lava flow of andesite; ( 3) the Kolo Formation, composed of air-laid lapilli tuff-breccia, tuff, unconsolidated ash and cinder, small basaltic andesite lava flows, and one thick pyroxene andesite lava flow; and (4) the Lofia Formation, composed of air-laid tuff, ash, basaltic andesite lava flows, and andesite lava flows. An erosional unconformity separates the Hamatua Formation from the Hokula Froth Lava, and another lies between the froth lava and the Kolo Formation. The rocks are typical orogenic andesites and related types, unusually high in CaO, which is reflected in the calcic nature of the plagioclase. The pyroxenes of the groundmass are usually pigeonite and pigeonitic augite, whereas the phenocrysts are augite. Hypersthene is less common and occurs only as phenocrysts surrounded by reaction rims of pigeonite and/or pigeonitic augite. Concentric normal faults associated with caldera collapse are common on the northern, eastern, and southern rims of the caldera. Some of the faults have served as conduits for rising magma of the Kolo Formation; others, on which caldera collapse is continuing, do not exhibit .associared volcanism. Tensional cracks are abundant along the southern rim. THE GEOLOGICAL INVESTIGATION of Tofua foot contour intervals was drawn up primarily Island is part of a larger study of the Tonga and for the gravimetric work, but it was also used as the Lau islands by the Hawaii Institute of Geo a base for the geologic mapping (Fig.