IOC Workshop on the Technical Aspects of Tsunami Warning Systems, Tsunami Analysis, Preparedness, Observation and Instrumentatio
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Geology of Hawaii Reefs
11 Geology of Hawaii Reefs Charles H. Fletcher, Chris Bochicchio, Chris L. Conger, Mary S. Engels, Eden J. Feirstein, Neil Frazer, Craig R. Glenn, Richard W. Grigg, Eric E. Grossman, Jodi N. Harney, Ebitari Isoun, Colin V. Murray-Wallace, John J. Rooney, Ken H. Rubin, Clark E. Sherman, and Sean Vitousek 11.1 Geologic Framework The eight main islands in the state: Hawaii, Maui, Kahoolawe , Lanai , Molokai , Oahu , Kauai , of the Hawaii Islands and Niihau , make up 99% of the land area of the Hawaii Archipelago. The remainder comprises 11.1.1 Introduction 124 small volcanic and carbonate islets offshore The Hawaii hot spot lies in the mantle under, or of the main islands, and to the northwest. Each just to the south of, the Big Island of Hawaii. Two main island is the top of one or more massive active subaerial volcanoes and one active submarine shield volcanoes (named after their long low pro- volcano reveal its productivity. Centrally located on file like a warriors shield) extending thousands of the Pacific Plate, the hot spot is the source of the meters to the seafloor below. Mauna Kea , on the Hawaii Island Archipelago and its northern arm, the island of Hawaii, stands 4,200 m above sea level Emperor Seamount Chain (Fig. 11.1). and 9,450 m from seafloor to summit, taller than This system of high volcanic islands and asso- any other mountain on Earth from base to peak. ciated reefs, banks, atolls, sandy shoals, and Mauna Loa , the “long” mountain, is the most seamounts spans over 30° of latitude across the massive single topographic feature on the planet. -
The Achievements of Captain George Vancouver on The
THE ACHIEVEMENTS OF CAPTAIN GEORGE VANCOUVER ON THE BRITISH COLUMBIA COAST. by William J. Roper A Thesis submitted in partial fulfilment of the requirements for the degree of MASTER OF ARTS in the Department of HISTORY The University of British Columbia October, 1941 THE ACHIEVEMENTS OF CAPTAIN GEORGE VANCOUVER ON THE BRITISH COLUMBIA COAST TABLE Off CONTENTS TABLE OF CONTENTS Introduction Chapter I. Apprenticeship. Page 1 Chapter II. The Nootka Sound Controversy. Page 7 Chapter III. Passage to the Northwest Coast. Page 15 Chapter IV. Survey—Cape Mendocino to Admiralty Inlet. Page 21 Chapter V. Gulf of Georgia—Johnstone Straits^-Nootka. Page 30 Chapter VI. Quadra and Vancouver at Nootka. Page 47 Chapter VII. Columbia River, Monterey, Second Northward Survey, Sandwich Islands. Page 57 Chapter VIII. Third Northern Survey. Page 70 Chapter IX. Return to England. Page 84 Chapter X. Summary of Vancouver's Ac hi evement s. Page 88 Appendix I. Letter of Vancouver to Evan Nepean. ' Page 105 Appendix II. Controversy between Vancouver and Menzies. Page 110 Appendix III. Comments on.Hewett's Notes. Page 113 Appendix IV. Hydrographic Surveys of the Northwest Coast. Page 115 Bibliography- Page I* INTRODUCTION INTRODUCTION I wish to take this opportunity to express my thanks to Dr. W. N. Sage, Head of the Department of History of the University of British Columbia for his helpful suggestions and aid in the preparation of this thesis. CHAPTER I. APPRENTICESHIP THE ACHIEVEMENTS OF CAPTAIN GEORGE VANCOUVER ON THE BRITISH COLUMBIA COAST CHAPTER I. APPRENTICESHIP What were the achievements of Captain Vancouver on the British Columbia coast? How do his achievements compare with those of Captain Cook and the Spanish explorers? Why was an expedition sent to the northwest coast at this time? What qualifications did Vancouver have for the position of commander of the expedition? These and other pertinent questions will receive consideration in this thesis. -
Another Clue for Fast Motion of the Hawaiian Hotspot 27 February 2018
Another clue for fast motion of the Hawaiian hotspot 27 February 2018 Northwest Pacific. But soon there was doubt over whether hotspots are truly stationary. The biggest contradiction was a striking bend of about 60 degrees in this volcanic chain, which originated 47 million years ago. "If you try to explain this bend with just a sudden change in the movement of the Pacific Plate, you would expect a significantly different direction of motion at that time relative to adjacent tectonic plates," says Bernhard Steinberger of the GFZ German Research Center for Geosciences. "But we have not found any evidence for that." Recent studies have suggested that apparently two processes were effective: On the one hand, the Pacific Plate has changed its direction of motion. On the other hand, the Hawaiian hotspot moved relatively quickly southward in the period from 60 to about 50 million years ago - and then stopped. If this hotspot motion is considered, only a smaller change of Pacific plate motions is needed to explain the volcano chain. Graph shows the dates of volcanoes of the three volcanic chains in the Pacific and their relative movement over time (left). The location of the three This hypothesis is now supported by work in which volcanic chains shown in the map (right). The stars mark Steinberger is also involved. First author Kevin the youngest end or the active volcanoes today. Credit: Konrad, Oregon State University in Corvallis, Nature Communications, Kevin Konrad et al. Oregon, and his team have evaluated new rock dating of volcanoes in the Rurutu volcanic chain, including, for example, the Tuvalu volcanic islands in the Western Pacific. -
Data Summary Report for Chum Salmon Escapement Surveys in the Nass Area in 2015
Data Summary Report for Chum Salmon Escapement Surveys in the Nass Area in 2015 Prepared by: LGL Limited environmental research associates 9768 Second Street Sidney, BC V8L 3Y8 Prepared for: Pacific Salmon Commission 600 - 1155 Robson Street Vancouver, BC V6E 1B5 and Nisga’a Lisims Government Fisheries & Wildlife Department P.O. Box 228 Gitlaxt’aamiks, BC V0J 1A0 Nisga’a Fisheries Report #15-26 31 December 2016 Data Summary Report for Chum Salmon Escapement Surveys in the Nass Area in 2015 Prepared by: LGL Limited environmental research associates 9768 Second Street Sidney, BC V8L 3Y8 Prepared for: Pacific Salmon Commission 600 - 1155 Robson Street Vancouver, BC V6E 1B5 and Nisga’a Lisims Government Fisheries & Wildlife Department P.O. Box 228 Gitlaxt’aamiks, BC V0J 1A0 Nisga’a Fisheries Report #15-26 31 December 2016 EA3624 DATA SUMMARY REPORT FOR CHUM SALMON ESCAPEMENT SURVEYS IN THE NASS AREA IN 2015 Prepared by: I. A. Beveridge, R. F. Alexander, S. C. Kingshott, C. A. J. Noble, and C. Braam LGL Limited environmental research associates 9768 Second Street Sidney, BC V8L 3Y8 Prepared for: Pacific Salmon Commission #600 - 1155 Robson Street Vancouver, BC V6E 1B5 and Nisga’a Lisims Government Fisheries & Wildlife Department P.O. Box 228 Gitlaxt’aamiks, BC V0J 1A0 Nisga’a Fisheries Report #15-26 31 December 2016 i TABLE OF CONTENTS LIST OF TABLES .................................................................................................................................ii LIST OF FIGURES ...............................................................................................................................ii -
Hawaii Hotspot (Crustal Plate Movement)
Earth Science Name: Dynamic Crust Laboratory # 13 Hawaii Hotspot (Crustal Plate Movement) Introduction: Plate tectonics has been an accepted theory since the 1960’s. According to this theory, the crust of the Earth is composed of plates that move over the asthenosphere. There are two basic types of plates: heavy, thin and dense oceanic plates, which are primarily composed of basalt; and thick, lighter continental plates, which are comprised of silicate rocks (granite). Movement of the Pacific plate over the Hawaiian Hot Spot: The idea behind plate tectonics is that the crustal plates are moving with respect to one another over geologic time. The rates of movement of crustal plates can be determined by using data from the plate margins along the mid-ocean ridges, or at regions known as “HOTSPOTS” where the distance and age can be measured. The Hawaiian Islands are volcanic islands that are produced as superheated molten material rises upward from deep within the mantle. As the molten material breaks through weak places in the crustal plate a new “island” will form. Hawaii Crustal Plate Lab.doc 10/6/2013 1 Procedures: 1. Using Map 1 on this page and the absolute dates of lava in bold black numbers that represent millions of years before the present. Calculate the age difference between the islands and enter the data in the table on page 3. When there is more than one age on an island use an average! 2. Make distance measurements between the “dots” of each circle using the scale on the diagram. 3. Convert the distance from kilometers to “land” or “real” centimeters (NOT cm on the map!) by multiplying the distance in KM by 100,000 (which is the number of cm in 1 km). -
Hawaiian Hotspot
V51B-0546 (AGU Fall Meeting) High precision Pb, Sr, and Nd isotope geochemistry of alkalic early Kilauea magmas from the submarine Hilina bench region, and the nature of the Hilina/Kea mantle component J-I Kimura*, TW Sisson**, N Nakano*, ML Coombs**, PW Lipman** *Department of Geoscience, Shimane University **Volcano Hazard Team, USGS JAMSTEC Shinkai 6500 81 65 Emperor Seamounts 56 42 38 27 20 12 5 0 Ma Hawaii Islands Ready to go! Hawaiian Hotspot N ' 0 3 ° 9 Haleakala 1 Kea trend Kohala Loa 5t0r6 end Mauna Kea te eii 95 ol Hualalai Th l 504 na io sit Mauna Loa Kilauea an 509 Tr Papau 208 Hilina Seamont Loihi lic ka 209 Al 505 N 98 ' 207 0 0 508 ° 93 91 9 1 98 KAIKO 99 SHINKAI 02 KAIKO Loa-type tholeiite basalt 209 Transitional basalt 95 504 208 Alkalic basalt 91 508 0 50 km 155°00'W 154°30'W Fig. 1: Samples obtained by Shinkai 6500 and Kaiko dives in 1998-2002 10 T-Alk Mauna Kea 8 Kilauea Basanite Mauna Loa -K M Hilina (low-Si tholeiite) 6 Hilina (transitional) Hilina (alkali) Kea Hilina (basanite) 4 Loa Hilina (nephelinite) Papau (Loa type tholeiite) primary 2 Nep Basaltic Basalt andesite (a) 0 35 40 45 50 55 60 SiO2 Fig. 2: TAS classification and comparison of the early Kilauea lavas to representative lavas from Hawaii Big Island. Kea-type tholeiite through transitional, alkali, basanite to nephelinite lavas were collected from Hilina bench. Loa-type tholeiite from Papau seamount 100 (a) (b) (c) OIB OIB OIB M P / e l p 10 m a S E-MORB E-MORB E-MORB Loa type tholeiite Low Si tholeiite Transitional 1 f f r r r r r r r f d y r r d b b -
New Available LNG Sites on Canada's West Coast
New Available LNG Sites on Canada’s West Coast Disclaimer This presentation contains information that is preliminary in nature and may be subject to change in the future. Forward looking statements involve risks and uncertainties because they relate to events and depend upon circumstances that will or may vary in the future. Actual outcomes may differ. Any party interested in pursuing the opportunities presented here should undertake its own research and due diligence to satisfy itself of the quality of the information presented within. 2 Contents Page Introduction 4 Welcome 5 The Nisga’a Nation – An Overview 6 Natural Gas Supply in Western Canada 11 Nisga’a Nation Sites for a Floating or Land-Based LNG Facility 15 Regional Infrastructure 28 Next Steps 37 Contacts 39 3 Introduction • The Nisga’a Nation wishes to attract sustainable economic development, including LNG projects, to our area. • Canada’s vast resources of natural gas are ideal as a new LNG supply source for global markets. • Suitable sites for LNG development along the west coast of Canada are limited due to the mountainous terrain and restricted access. • Some perceive that most, if not all, sites have already been selected by various parties for their LNG projects. • The Nisga’a Nation owns all or part of four first rate sites for development that have not previously been identified for LNG projects. • These sites offer unique opportunities as a result of the Nisga’a Treaty, our Nisga’a Government, our property interests and our unique environmental assessment rights. • This package is a preliminary description of available LNG sites on the Portland Inlet waterway, near the Nass River, on Canada’s west coast, north of Prince Rupert. -
Neon, Helium and Argon Isotope Systematics of the Hawaiian Hotspot
Universität Potsdam Institut für Geowissenschaften Neon, Helium and Argon Isotope Systematics of the Hawaiian Hotspot Dissertation zur Erlangung des akademischen Grades "doctor rerum naturalium" (Dr. rer. nat.) in der Wissenschaftsdisziplin Geowissenschaften eingereicht an der Mathematisch-Naturwissenschaftlichen Fakultät der Universität Potsdam von Tina Mailer, geb. Krüsmann Potsdam, Juni 2009 This work is licensed under a Creative Commons License: Attribution - Noncommercial - Share Alike 3.0 Germany To view a copy of this license visit http://creativecommons.org/licenses/by-nc-sa/3.0/de/deed.en Published online at the Institutional Repository of the University of Potsdam: URL http://opus.kobv.de/ubp/volltexte/2009/3963/ URN urn:nbn:de:kobv:517-opus-39633 http://nbn-resolving.org/urn:nbn:de:kobv:517-opus-39633 Fire and Ice Some say the world will end in fire, Some say in ice. From what I've tasted of desire I hold with those who favor fire. But if it had to perish twice, I think I know enough of hate To say that for destruction ice Is also great And would suffice. Robert Frost, 1923 Table of Contents Abstract ...................................................................................................................................... 1 Zusammmenfassung................................................................................................................... 2 Motivation and goals of this study ............................................................................................. 3 1 Noble Gas Geochemistry ....................................................................................................... -
Non-Hawaiian Lithostratigraphy of Louisville Seamounts and the Formation of High-Latitude Oceanic Islands and Guyots
Non-Hawaiian lithostratigraphy of Louisville seamounts and the formation of high-latitude oceanic islands and guyots David M. Buchsa,⁎, Rebecca Williamsb, Shin-ichi Sanoc, V. Paul Wrightd a Cardiff University, UK b University of Hull, UK c Fukui Prefectural Dinosaur Museum, Japan d National Museum of Wales, UK This is an author accepted manuscript for an article published in Journal of Volcanology and Geothermal Research, doi: 10.1016/j.jvolgeores.2017.12.019. ABSTRACT Guyots are large seamounts with a flat summit that is generally believed to form due to constructional biogenic and/or erosional processes during the formation of volcanic islands. However, despite their large abundance in the oceans, there are still very few direct constraints on the nature and formation of guyots, in particular those formed at high latitude that lack a thick cap of shallow-marine carbonate rocks. It is largely accepted based on geophysical constraints and surficial observations/sampling that the summit platform of these guyots is shaped by wave abrasion during post-volcanic subsidence of volcanic islands. Here we provide novel constraints on this hypothesis and the summit geology of guyots with a lithostratigraphic analysis of cores from three Louisville seamounts (South Pacific) collected during Expedition 330 of the Integrated Ocean Drilling Program (IODP). Thirteen lithofacies of sedimentary and volcanic deposits are described, which include facies not previously recognized on the top of guyots, and offer a new insight into the formation of high-latitude oceanic islands on a fast- moving plate. Our results reveal that the lithostratigraphy of Louisville seamounts preserves a very consistent record of the formation and drowning of volcanic islands, with from bottom to top: (i) volcaniclastic sequences with abundant lava-fed delta deposits, (ii) submarine to subaerial shield lava flows, (iii) post-volcanic shallow to deeper marine sedimentary rocks lacking thick reef deposits, (iv) post-erosional rejuvenated volcanic rocks, and (v) pelagic sediments. -
Hawaii Hotspot
Name ______________ Date _________ Per ______ Mini-Lesson 1) On which tectonic plate is the Hawaii hot spot? A) North American Plate B) African Plate C) Antarctic Plate D) Pacific Plate 2) Approximately what are the coordinates of the Hawaii Hot Spot? A) 50° N, 120° W C) 25° N, 158° W B) 25° N, 158° E D) 25° S, 158° E 3) The cross section below shows the direction of movement of an oceanic plate over a mantle hot spot, resulting in the formation of a chain of volcanoes labeled A, B, C, and D. The geologic age of volcano C is shown. What are the most likely geologic ages of volcanoes B and D? A) B is 5 million years old and D is 12 million years old. B) B is 2 million years old and D is 6 million years old. C) B is 9 million years old and D is 9 million years old. D) B is 10 million years old and D is 4 million years old. Page 1 4) Base your answer to the following question on the world map in your answer booklet and on your knowledge of Earth science. The map shows major earthquakes and volcanic activity occurring from 1996 through 2000. Letter A represents a volcano on a crustal plate boundary. The source of the magma for the volcanic activity in Hawaii is A) a magma plume originating in the mantle B) heat from the atmosphere C) radiation from nuclear facilities D) sedimentary rocks found on North America Page 2 5) Base your answer to the following question on the map and passage below. -
SCIENCE of TSUNAMI HAZARDS the Internationaljournal of the Tsunami Society
ISSN 0736-5306 SCIENCE OF TSUNAMI HAZARDS The InternationalJournal of The Tsunami Society Volume 7 Number 1 1989 MAXIMUM TSUNAMI AMPLITUDES ANI) ASSOCIATED CURRENTS 3 ON THE COAST OF BRITISH COLUMBIA D. Dunbar Seaconsult Marine F!esearch Ltd., Vancouver, Canada P. H. LeBlond University of British Columbia, Vancouver, Canada T. S. Murt Institute o{ Ocean Sciences, Sidney, Canada THE LARGEST HISTORICAL TSUNAMIS IN THE NORTHERN 45 ADRIATIC SEA: A CRITICAL REVIEW E. Guidoboni tind S. Tinti University of Bologlna, Bologna, Italy MEMORIUM TO SERGEI SERGEEVICH VOIT (1920-1987) 55 S.L. Soloviev, V. D. Larichev, B. 1. Sebekin and V. V. Zmur copyright@ 1989 THE TSUNAMI SOCIETY OBJECTIVE: The Tsunami Society publishes this journal to increase and disseminate knowlsdge about tsunamis and their hazards. DISCLAIMER: The Tsunami Society publishes this journal to disseminate information relating to tsunamis. Although these articles have been technically reviewed by peers, The Tsunami Society is not responsible for the veracity of any statement, opinion, or consequences. EDITORIAL STAFF T. S. Murty Technical Editor Charles L. Mader - Production Editor Institute of Ocean Sciences Joint Institute for Marine and Atmospheric Research Department of Fisheries and Oceans University of Hawaii Sidney, B. C., Canada Honolulu, HI, U.S.A. George Pararas-Carayannis - Circulation George D. Curtis - President/Publisher International Tsunami Information Center Joint Institute for Marine aqi Atmospheric Research Honolulu, HI, U.S.A. University of Hawaii Honolulu, HI, U.S.A. T. S. Murty Technical Editor Submit manuscripts of articles, notes, or letters to: Institute of Ocean Sciences Department of Fisheries and Oceans Sidney, B. C., Canada V8L 4B2 If article is accepted for publication the author(s) must submit a camera ready manuscript. -
Anyox Dominion Day Celebration Was Big Affair Conservative Meetings
S S S S S I •'* sf $2.50 a Year A little paper Alice Arm and with all the { Anyox. $2.75 to news and a big all other points. circulation THE HERALD •4*4*4 I1H1HH1H Si SiHH •' S H •"> Published in the interests of Alice Arm and Anyox, B. C. 5 cents each. VOL. 7, NO. 52 ALICE ARM, B. C, FRIDAY, JULY 6,1928 Anyox Dominion Day Conservative Meetings Tampering With Water Honor Rolls Presented Development Work On Celebration Was Held This Week Barrels Dangerous At Entertainment Musketeer Proves Rich Big Affair A Publio meeting of the support The water barrels in Anyox that The entertainment given at the Property ers of the Conservative party was are placed at convenient points for closing of the Alice Arm school on Thursday evening last was attended Close prospecting and surface The celebration of 61st. anniver held on Tuesday last July 3rd. at the quenching of a fire in its early by a large number of adults. development work of the Musketeer sary of the Confederation ot Cana the Mine Hall at 8 p.m. when T- stages have recently been the scene of serious depredations on the part Honor rolls were presented to Group in the Upper Kitsault da went over with a bang at Any F. Baxter of Vancouver gave an of the juveniles. In several cases the pupils which are as follows: country has produoed some re ox on Monday. Sports of all kinds address on behalf of T. W. Fal the water has been emptied out and Proficiency—Lillian Moss.