Kīlauea Recovery and Resilience Plan
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Hawaii Volcanoes National Park Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 THIS PAGE: Geologists have lloongng been monimonittoorriing the volcanoes of Hawai‘i Volcanoes National Park. Here lalava cascades durduriingng the 1969-1971 Mauna Ulu eruption of Kīlauea VolVolcano. NotNotee the Mauna Ulu fountountaiain in the background. U.S. Geologiogicalcal SurSurvveyey PhotPhotoo by J. B. Judd (12/30/1969). ON THE COVER: ContContiinuouslnuouslyy eruptuptiingng since 1983, Kīllaueaauea Volcano contcontiinues to shapshapee Hawai‘Hawai‘i VoVollccanoes NatiNationalonal ParkPark.. Photo courtesy Lisa Venture/UniversiUniversitty of Cincinnati. Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 December 2009 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
Vog: Using Volcanic Eruptions to Estimate the Health Costs Of
Vog: Using Volcanic Eruptions to Estimate the Health Costs of Particulates and SO2 by Timothy Halliday, John Lynham and Áureo de Paula Working Paper No. 2015-2 April 2, 2015 UNIVERSITY OF HAWAI‘I AT MANOA 2424 MAILE WAY, ROOM 540 • HONOLULU, HAWAI‘I 96822 WWW.UHERO.HAWAII.EDU WORKING PAPERS ARE PRELIMINARY MATERIALS CIRCULATED TO STIMULATE DISCUSSION AND CRITICAL COMMENT. THE VIEWS EXPRESSED ARE THOSE OF THE INDIVIDUAL AUTHORS. Vog: Using Volcanic Eruptions to Estimate the Health Costs of Particulates and SO2∗ Timothy J. Halliday† John Lynham UH - M¯anoa and IZA UH - M¯anoa Áureo de Paula UCL, São Paulo School of Economics, IFS, CeMMAP April 2, 2015 Abstract K¯ılauea volcano is the largest stationary source of SO2 pollutioninthe United States of America. Moreover, the SO2 that the volcano emits eventu- ally forms particulate matter, another major pollutant. We use this exogenous ∗We thank Jill Miyamura of Hawai‘i Health Information Corporation for the data. Chaning Jang and Jonathan Sweeney provided expert research assistance. We also thank participants at the University of Hawai Applied Micro Group for useful comments. †Corresponding Author. Address: 2424 Maile Way; 533 Saunders Hall; Honolulu, HI 96822. Tele: (808) 956 -8615. E-mail: [email protected]. 1 source of pollution variation to estimate the impact of particulate matter and SO2 on emergency room admissions and costs in the state of Hawai‘i. Impor- tantly, our data on costs is more accurate than the measures used in much of the literature. We find strong evidence that particulate pollution increases pulmonary-related hospitalization. Specifically, a one standard deviation in- crease in particulate pollution leads to a 2-3% increase in expenditures on emergency room visits for pulmonary-related outcomes. -
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. -
Vog: Using Volcanic Eruptions to Estimate the Health Costs of Particulates
IZA DP No. 9398 Vog: Using Volcanic Eruptions to Estimate the Health Costs of Particulates Timothy J. Halliday John Lynham Áureo de Paula October 2015 DISCUSSION PAPER SERIES Forschungsinstitut zur Zukunft der Arbeit Institute for the Study of Labor Vog: Using Volcanic Eruptions to Estimate the Health Costs of Particulates Timothy J. Halliday University of Hawai’i at Mānoa and IZA John Lynham University of Hawai’i at Mānoa Áureo de Paula UCL, São Paulo School of Economics, IFS and CeMMAP Discussion Paper No. 9398 October 2015 IZA P.O. Box 7240 53072 Bonn Germany Phone: +49-228-3894-0 Fax: +49-228-3894-180 E-mail: [email protected] Any opinions expressed here are those of the author(s) and not those of IZA. Research published in this series may include views on policy, but the institute itself takes no institutional policy positions. The IZA research network is committed to the IZA Guiding Principles of Research Integrity. The Institute for the Study of Labor (IZA) in Bonn is a local and virtual international research center and a place of communication between science, politics and business. IZA is an independent nonprofit organization supported by Deutsche Post Foundation. The center is associated with the University of Bonn and offers a stimulating research environment through its international network, workshops and conferences, data service, project support, research visits and doctoral program. IZA engages in (i) original and internationally competitive research in all fields of labor economics, (ii) development of policy concepts, and (iii) dissemination of research results and concepts to the interested public. -
Pu'u Wa'awa'a Biological Assessment
PU‘U WA‘AWA‘A BIOLOGICAL ASSESSMENT PU‘U WA‘AWA‘A, NORTH KONA, HAWAII Prepared by: Jon G. Giffin Forestry & Wildlife Manager August 2003 STATE OF HAWAII DEPARTMENT OF LAND AND NATURAL RESOURCES DIVISION OF FORESTRY AND WILDLIFE TABLE OF CONTENTS TITLE PAGE ................................................................................................................................. i TABLE OF CONTENTS ............................................................................................................. ii GENERAL SETTING...................................................................................................................1 Introduction..........................................................................................................................1 Land Use Practices...............................................................................................................1 Geology..................................................................................................................................3 Lava Flows............................................................................................................................5 Lava Tubes ...........................................................................................................................5 Cinder Cones ........................................................................................................................7 Soils .......................................................................................................................................9 -
Survey of Roadside Alien Plants in Hawai`I Volcanoes National Park and Adjacent Residential Areas 2001–2005
Technical Report HCSU-032 SURVEY OF ROADSIDE ALIEN PLANts IN HAWAI`I VOLCANOES NATIONAL PARK AND ADJACENT RESIDENTIAL AREAS 2001–2005 Linda W. Pratt1 Keali`i F. Bio2 James D. Jacobi1 1 U.S. Geological Survey, Pacific Island Ecosystems Research Center, Kilauea Field Station, P.O. Box 44, Hawaii National Park, HI 96718 2 Hawai‘i Cooperative Studies Unit, University of Hawai‘i at Hilo, P.O. Box 44, Hawai‘i National Park, HI 96718 Hawai‘i Cooperative Studies Unit University of Hawai‘i at Hilo 200 W. Kawili St. Hilo, HI 96720 (808) 933-0706 September 2012 This product was prepared under Cooperative Agreement CA03WRAG0036 for the Pacific Island Ecosystems Research Center of the U.S. Geological Survey. Technical Report HCSU-032 SURVEY OF ROADSIDE ALIEN PLANTS IN HAWAI`I VOLCANOES NATIONAL PARK AND ADJACENT RESIDENTIAL AREAS 2001–2005 1 2 1 LINDA W. PRATT , KEALI`I F. BIO , AND JAMES D. JACOBI 1 U.S. Geological Survey, Pacific Island Ecosystems Research Center, Kīlauea Field Station, P.O. Box 44, Hawai`i Volcanoes National Park, HI 96718 2 Hawaii Cooperative Studies Unit, University of Hawai`i at Hilo, Hilo, HI 96720 Hawai`i Cooperative Studies Unit University of Hawai`i at Hilo 200 W. Kawili St. Hilo, HI 96720 (808) 933-0706 September 2012 This article has been peer reviewed and approved for publication consistent with USGS Fundamental Science Practices ( http://pubs.usgs.gov/circ/1367/ ). Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. -
Hawaiian Volcanoes: from Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012
AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012 Conveners Michael Poland, USGS – Hawaiian Volcano Observatory, USA Paul Okubo, USGS – Hawaiian Volcano Observatory, USA Ken Hon, University of Hawai'i at Hilo, USA Program Committee Rebecca Carey, University of California, Berkeley, USA Simon Carn, Michigan Technological University, USA Valerie Cayol, Obs. de Physique du Globe de Clermont-Ferrand Helge Gonnermann, Rice University, USA Scott Rowland, SOEST, University of Hawai'i at M noa, USA Financial Support 2 AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Meeting At A Glance Sunday, 19 August 2012 1600h – 1700h Welcome Reception 1700h – 1800h Introduction and Highlights of Kilauea’s Recent Eruption Activity Monday, 20 August 2012 0830h – 0900h Welcome and Logistics 0900h – 0945h Introduction – Hawaiian Volcano Observatory: Its First 100 Years of Advancing Volcanism 0945h – 1215h Magma Origin and Ascent I 1030h – 1045h Coffee Break 1215h – 1330h Lunch on Your Own 1330h – 1430h Magma Origin and Ascent II 1430h – 1445h Coffee Break 1445h – 1600h Magma Origin and Ascent Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Origin and Ascent III 1645h – 1900h Poster Session Tuesday, 21 August 2012 0900h – 1215h Magma Storage and Island Evolution I 1215h – 1330h Lunch on Your Own 1330h – 1445h Magma Storage and Island Evolution II 1445h – 1600h Magma Storage and Island Evolution Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Storage -
Molokai Hawaii Forgotten
Molokai -Forgotten By ETHEL A. STARBIRD NATIONAL GEOGRAPHic sENIOR STAFF Photographs by RICHARD Casting away care, Sister Richard Marie takes a day off near Molokai's leprosy hospital, where she has worked Hawaii since 1960. Independent, resourceful, generous, she shares the best qualities A. COOKE III of Hawaii's most unspoiled major island. 189 Like thirsty giants, the volcanic peaks of Molokai's eastern end steal rainfall from its flat, dry western end. Polynesians from the Marquesas Islands came to Hawaii about 1,200 years ago. They eventually settled on this island in numbers National Geographic, August 1981 far greater than today'll 6,000 population. The semicircular walls of coral and basalt seen in the shallow waters in the foreground enclose fishponds once used to capture and fatten mullet and other saltwater species for island royalty. Molokai-Forgotten Hawaii 191 Beyond the farthest road a primeval world unfolds in the lush valleys of the northeastern coast. The chill waters of Kahiwa Falls (left) drop 1,750 feet to the sea in Hawaii's longest cascade. Deep in the island's forest reserve, spray from another waterfall (above) mingles with the scent of eucalyptus and wild ginger. Amaumau ferns (right, center) stand as tall as six feet. For centuries, Molokai was revered as a place where religious rituals were performed by powerful kahuna, or priests. One of the most famous, Lanikaula, is said to be buried in a grove of kukui trees near the island's eastern tip (below right). To make lamp oil, Hawaiians traditionally took nuts from the kukui, now a symbol of Molokai. -
Chapter 2 the Evolution of Seismic Monitoring Systems at the Hawaiian Volcano Observatory
Characteristics of Hawaiian Volcanoes Editors: Michael P. Poland, Taeko Jane Takahashi, and Claire M. Landowski U.S. Geological Survey Professional Paper 1801, 2014 Chapter 2 The Evolution of Seismic Monitoring Systems at the Hawaiian Volcano Observatory By Paul G. Okubo1, Jennifer S. Nakata1, and Robert Y. Koyanagi1 Abstract the Island of Hawai‘i. Over the past century, thousands of sci- entific reports and articles have been published in connection In the century since the Hawaiian Volcano Observatory with Hawaiian volcanism, and an extensive bibliography has (HVO) put its first seismographs into operation at the edge of accumulated, including numerous discussions of the history of Kīlauea Volcano’s summit caldera, seismic monitoring at HVO HVO and its seismic monitoring operations, as well as research (now administered by the U.S. Geological Survey [USGS]) has results. From among these references, we point to Klein and evolved considerably. The HVO seismic network extends across Koyanagi (1980), Apple (1987), Eaton (1996), and Klein and the entire Island of Hawai‘i and is complemented by stations Wright (2000) for details of the early growth of HVO’s seismic installed and operated by monitoring partners in both the USGS network. In particular, the work of Klein and Wright stands and the National Oceanic and Atmospheric Administration. The out because their compilation uses newspaper accounts and seismic data stream that is available to HVO for its monitoring other reports of the effects of historical earthquakes to extend of volcanic and seismic activity in Hawai‘i, therefore, is built Hawai‘i’s detailed seismic history to nearly a century before from hundreds of data channels from a diverse collection of instrumental monitoring began at HVO. -
Large-Scale Weather Patterns Favorable for Volcanic Smog Occurrences on O’Ahu, Hawai’I
Air Qual Atmos Health DOI 10.1007/s11869-017-0502-z Large-scale weather patterns favorable for volcanic smog occurrences on O’ahu, Hawai’i Kristine Tofte1 & Pao-Shin Chu1 & Gary M. Barnes1 Received: 2 April 2017 /Accepted: 6 August 2017 # Springer Science+Business Media B.V. 2017 Abstract Kīlauea Volcano, located on the Island of Hawai’i, Keywords Atmospheric science . Synoptic patterns . Air released approximately 3700 t of sulfur dioxide (SO2) per day quality . Pollution . Volcanic smog . Volcanic activity . Health from April 2009 through 2014. Within the atmosphere, SO2 is oxidized and converted to sulfuric-acid aerosols, and this vol- canic smog is commonly referred to as vog. This study focus- Introduction es on large-scale weather patterns that bring vog to O’ahu. The Hawai’i State Department of Health PM2.5 measurements The Hawaiian archipelago should have some of the cleanest were used to identify elevated vog conditions, and a total of air in the world because of its location in the mid-ocean. 101 vog days were found. European Centre for Medium- However, the air quality is occasionally poor because of vol- Range Weather Forecasts ERA-Interim reanalysis data were canic smog (vog) emanating from Kīlauea Volcano which is used to determine weather patterns. These 101 vog days were located on the southeast corner of the Island of Hawai’i, also the result of 57 distinct vog events lasting from 3 h up to known as the Big Island (Fig. 1). 4 days. The 57 events were further categorized into three Kīlauea Volcano started erupting continuously in 1983, large-scale weather patterns: pre-cold fronts (37 cases), mainly from the Pu u Ōō vent located on the East Rift upper-level disturbances (17 cases), and Kona lows (3 cases). -
Ethnohistory of Puna
Research in Action: Ethnohistory of Puna: Davianna Pōmaikaʻi McGregor Praxis: exercise or practice of an art, science or skill. Praxis distinguishes Ethnic Studies from the long-established disciplines of the social sciences. Ethnic Studies faculty are committed to placing research at the service of the community and challenging students to examine and analyze contemporary issues of concern to Hawaiʻi’s ethnic communities from diverse perspectives. The clash between the beliefs, customs, and practices of Hawaiian descendants of Pele (Hawaiian goddess of the volcano) and the developers of geothermal energy is one of the issues which drew upon the resources of Ethnic Studies faculty and students.1 The issue evolved as the federal and state governments partnered with private corporations to clear the largest remaining lowland rainforest in Hawaiʻi for geothermal wells and power plants. In response, Hawaiians filed several civil suits, organized religious ceremonies in the volcanic rainforest, produced documentary films and joined with environmentalists in public protests. A key turning point in the struggle was a ruling by the US federal court that an Environmental Impact Study (EIS) was required for the project to proceed. Where proposed development projects funded by the federal government affect native peoples, new historic preservation laws mandated the inclusion of a cultural impact study in the EIS. Thus, for the first time since the passage of the new laws, a cultural impact study was conducted for native Hawaiians in Hawaiʻi. The First Cultural Impact Study on Native Hawaiians University of Hawaiʻi faculty from the Ethnic Studies Department, the Department of Urban and Regional Planning and the School of Social Work were contracted to conduct the study.2 The team drew upon the individual skills and experiences of their faculty and developed a multi-method approach for the study. -
Volcanic and Seismic Hazards on the Island of Hawaii
U.S. Department of the Interior / U.S. Geological Survey Volcanic and Seismic Hazards on the Island of Hawaii Volcanic and Seismic Hazards on the Island of Hawaii Lava flows entered Kalapana Gardens in December 1986. Front Cover: View of Kapoho village during the 1960 eruption before it was entirely destroyed. (Photographer unknown) Inside Front Cover (Photograph by J.D. Griggs) For sale by the U.S. Government Printing Office Superintendent of Documents, Mail Stop: SSOP, Washington, DC 20402-9328 ISBN 0-16-038200-9 Preface he eruptions of volcanoes often have direct, dramatic effects on the lives of people and Ton their property. People who live on or near active volcanoes can benefit greatly from clear, scientific information about the volcanic and seismic hazards of the area. This booklet provides such information for the residents of Hawaii so they may effectively deal with the special geologic hazards of the island. Identifying and evaluating possible geologic hazards is one of the principal roles of the U.S. Geological Survey (USGS) and its Hawaiian Volcano Observatory. When USGS scientists recognize a potential hazard, such as an impend ing eruption, they notify the appropriate govern ment officials, who in turn are responsible for advising the public to evacuate certain areas or to take other actions to insure their safety. This booklet was prepared in cooperation with the Hawaii County Civil Defense Agency. Volcanic and Seismic Hazards: Interagency Responsibilities Hawaii County National Park } Civil Defense C Service ./ Short-term hazard evaluation for the agencies responsible for public safety. Information on volcanic U.S.