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National Weather Service High Wind Warning
National Weather Service Text Product Display https://forecast.weather.gov/product.php?site=HFO&issuedby=HFO&pr... National Weather Service Weather Forecast Office Honolulu, HI Non-Precipitation Warnings / Watches / Advisories Issued by NWS Honolulu, HI Home | Current Version | Previous Version | Text Only | Print | Product List | Glossary On Versions: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 000 WWHW70 PHFO 071330 NPWHFO URGENT - WEATHER MESSAGE National Weather Service Honolulu HI 330 AM HST Sat Mar 7 2020 ...HIGH WIND WARNING FOR LEEWARD WEST MAUI LANAI KAHOOLAWE AND THE LEEWARD KOHALA DISTRICT UNTIL 6 PM HST THIS EVENING... ...WIND ADVISORY FOR ALL HAWAIIAN ISLANDS UNTIL 6 PM HST THIS EVENING... .High pressure far north of the islands will support strong to locally damaging trade winds today, with winds gradually weakening tonight and Sunday. HIZ014>016-018-026-080400- /O.CON.PHFO.HW.W.0003.000000T0000Z-200308T0400Z/ Lanai Makai-Lanai Mauka-Kahoolawe-Maui Leeward West-Kohala- Including the cities of Manele, Lanai City, Lahaina, Kaanapali, and Waikoloa 330 AM HST Sat Mar 7 2020 ...HIGH WIND WARNING REMAINS IN EFFECT UNTIL 6 PM HST THIS EVENING... * WHAT...Northeast winds 30 to 40 mph with localized gusts over 60 mph. * WHERE...Leeward West Maui, Lanai, Kahoolawe and the Leeward Kohala District on the Big Island. * WHEN...Until 6 PM HST this evening. * IMPACTS...Damaging winds will blow down trees and power lines. Sporadic power outages can be expected. Travel will be difficult, especially for high profile vehicles. PRECAUTIONARY/PREPAREDNESS ACTIONS... Motorists, especially those in high profile vehicles, are urged to drive with extreme caution. -
Precontact Vegetation and Soil Nutrient Status in the Shadow of Kohala Volcano, Hawaii ⁎ Oliver A
Geomorphology 89 (2007) 70–83 www.elsevier.com/locate/geomorph Precontact vegetation and soil nutrient status in the shadow of Kohala Volcano, Hawaii ⁎ Oliver A. Chadwick a, , Eugene F. Kelly b, Sara C. Hotchkiss c, Peter M. Vitousek d a Department of Geography, University of California, Santa Barbara, CA 93106, USA b Department of Crop and Soil Science, Colorado State University, Fort Collins, CO 80523, USA c Department of Botany, University of Wisconsin, Madison, WI 53706, USA d Department of Biological Sciences, Stanford University, Stanford, CA 94305, USA Received 13 January 2005; received in revised form 25 July 2006; accepted 25 July 2006 Available online 2 October 2006 Abstract Humans colonized Hawaii about 1200 years ago and have progressively modified vegetation, particularly in mesic to dry 13 tropical forests. We use δ C to evaluate the contribution of C3 and C4 plants to deep soil organic matter to reconstruct pre-human contact vegetation patterns along a wet to dry climate transect on Kohala Mountain, Hawaii Island. Precontact vegetation assemblages fall into three distinct zones: a wet C3 dominated closed canopy forest where annual rainfall is N2000 mm, a dry C4 dominated grassland with annual rainfall b500 mm, and a broad transition zone between these communities characterized by either C3 trees with higher water-use efficiency than the rainforest trees or C3 trees with a small amount of C4 grasses intermixed. The likelihood of C4 grass understory decreases with increasing rainfall. We show that the total concentration of rock-derived nutrients in the b2-mm soil fraction differs in each of these vegetation zones. -
HAWAII National Park HAWAIIAN ISLANDS
HAWAII National Park HAWAIIAN ISLANDS UNITED STATES RAILROAD ADMINISTRATION N AT IONAL PAR.K. SERIES n A 5 o The world-famed volcano of Kilauea, eight miles in circumference An Appreciation of the Hawaii National Park By E. M. NEWMAN, Traveler and Lecturer Written Especially for the United States Railroad Administration §HE FIRES of a visible inferno burning in the midst of an earthly paradise is a striking con trast, afforded only in the Hawaii National Park. It is a combination of all that is terrify ing and all that is beautiful, a blending of the awful with the magnificent. Lava-flows of centuries are piled high about a living volcano, which is set like a ruby in an emer ald bower of tropical grandeur. Picture a perfect May day, when glorious sunshine and smiling nature combine to make the heart glad; then multiply that day by three hundred and sixty-five and the result is the climate of Hawaii. Add to this the sweet odors, the luscious fruits, the luxuriant verdure, the flowers and colorful beauty of the tropics, and the Hawaii National Park becomes a dreamland that lingers in one's memory as long as memory survives. Pa ae three To the American People: Uncle Sam asks you to be his guest. He has prepared for you the choice places of this continent—places of grandeur, beauty and of wonder. He has built roads through the deep-cut canyons and beside happy streams, which will carry you into these places in comfort, and has provided lodgings and food in the most distant and inaccessible places that you might enjoy yourself and realize as little as possible the rigors of the pioneer traveler's life. -
Geology, Geochemistry and Earthquake History of Lō`Ihi Seamount, Hawai`I
INVITED REVIEW Geology, Geochemistry and Earthquake History of Lō`ihi Seamount, Hawai`i Michael O. Garcia1*, Jackie Caplan-Auerbach2, Eric H. De Carlo3, M.D. Kurz4 and N. Becker1 1Department of Geology and Geophysics, University of Hawai`i, Honolulu, HI, USA 2U.S.G.S., Alaska Volcano Observatory, Anchorage, AK, USA 3Department of Oceanography, University of Hawai`i, Honolulu, HI, USA 4Department of Chemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, USA *Corresponding author: Tel.: 001-808-956-6641, FAX: 001-808-956-5521; email: [email protected] Key words: Loihi, seamount, Hawaii, petrology, geochemistry, earthquakes Abstract A half century of investigations are summarized here on the youngest Hawaiian volcano, Lō`ihi Seamount. It was discovered in 1952 following an earthquake swarm. Surveying in 1954 determined it has an elongate shape, which is the meaning of its Hawaiian name. Lō`ihi was mostly forgotten until two earthquake swarms in the 1970’s led to a dredging expedition in 1978, which recovered young lavas. This led to numerous expeditions to investigate the geology, geophysics, and geochemistry of this active volcano. Geophysical monitoring, including a real- time submarine observatory that continuously monitored Lō`ihi’s seismic activity for three months, captured some of the volcano’s earthquake swarms. The 1996 swarm, the largest recorded in Hawai`i, was preceded by at least one eruption and accompanied by the formation of a ~300-m deep pit crater, renewing interest in this submarine volcano. Seismic and petrologic data indicate that magma was stored in a ~8-9 km deep reservoir prior to the 1996 eruption. -
General Plan for the County of Hawai'i
COUNTY OF HAWAI‘I GENERAL PLAN February 2005 Pursuant Ord. No. 05-025 (Amended December 2006 by Ord. No. 06-153, May 2007 by Ord. No. 07-070, December 2009 by Ord. No. 09-150 and 09-161, June 2012 by Ord. No. 12-089, and June 2014 by Ord. No. 14-087) Supp. 1 (Ord. No. 06-153) CONTENTS 1: INTRODUCTION 1.1. Purpose Of The General Plan . 1-1 1.2. History Of The Plan . 1-1 1.3. General Plan Program . 1-3 1.4. The Current General Plan Comprehensive Review Program. 1-4 1.5. County Profile. 1-7 1.6. Statement Of Assumptions. 1-11 1.7. Employment And Population Projections . 1-12 1.7.1. Series A . 1-13 1.7.2. Series B . 1-14 1.7.3. Series C . 1-15 1.8. Population Distribution . 1-17 2: ECONOMIC 2.1. Introduction And Analysis. 2-1 2.2. Goals . .. 2-12 2.3. Policies . .. 2-13 2.4. Districts. 2-15 2.4.1. Puna . 2-15 2.4.2. South Hilo . 2-17 2.4.3. North Hilo. 2-19 2.4.4. Hamakua . 2-20 2.4.5. North Kohala . 2-22 2.4.6. South Kohala . 2-23 2.4.7. North Kona . 2-25 2.4.8. South Kona. 2-28 2.4.9. Ka'u. 2-29 3: ENERGY 3.1. Introduction And Analysis. 3-1 3.2. Goals . 3-8 3.3. Policies . 3-9 3.4. Standards . 3-9 4: ENVIRONMENTAL QUALITY 4.1. Introduction And Analysis. -
NKAWS Report Final Draft
Table of Contents Executive Summary ......................................................................................................................1 Section 1 Introduction ..........................................................................................................3 Section 2 Types of Agriculture ............................................................................................5 2.1 Definition of Agriculture .........................................................................5 2.2 Crop Type ..............................................................................................10 2.3 Scale of Agriculture ...............................................................................12 2.31 Large Scale Agriculture .............................................................12 2.32 Mid-Size Agriculture .................................................................12 2.33 Small/Micro Agriculture ............................................................13 2.34 Agricultural Processing ..............................................................13 Section 3 Resources ...........................................................................................................15 3.1 Historical Systems .................................................................................15 3.2 Current Ditch System Intakes ................................................................17 3.3 Springs ...................................................................................................18 3.4 -
Maunaloa/Current/Longterm.Html K!Lauea – the Most Active Volcano on Earth K!Lauea Structure
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Raw Sewage and Solid Waste Dumps in Lava Tube Caves of Hawaii Island
William R. Halliday - Raw sewarge and sold waste dumps in lave tube caves of Hawaii Island. Journal of Cave and Karst Studies, v. 65, n. 1, p. 68-75. RAW SEWAGE AND SOLID WASTE DUMPS IN LAVA TUBE CAVES OF HAWAII ISLAND WILLIAM R. HALLIDAY Hawaii Speleological Survey, 6530 Cornwall Court, Nashville, TN 37205 USA [email protected] Lava tubes on the island of Hawaii (and elsewhere) are possible subsurface point sources of contamina- tion in addition to more readily identifiable sources on the surface. Human and animal waste, and haz- ardous and toxic substances dumped into lava tube caves are subject to rapid transport during flood events, which are the dominant type of groundwater flow through Hawaiian lava tubes. Although these waste materials may not be a major source of pollution when compared with some surface sources, this potential hazard should be evaluated much as in the case of karstic floodwater conduits. This paper explores the interaction of water flow and solid waste dumps and sewage in lava tubes and lava tube caves of Hawaii Island, Hawaii - an island almost as large as the state of Connecticut (Fig. 1)-and resulting potential threats to groundwater quality. In recent years, Hawaiian cavers and speleologists have become increasingly concerned about these occurrences. Some of the solid waste dumps can be seen to contain partially empty containers of toxic and/or hazardous substances (Fig. 2), including automotive and agricultural waste. Stinking raw sewage speaks for itself (Fig. 3), and members of the Hawaii chapter of the National Speleological Society have been shown the top of a septic tank or cesspool near Keaau said to consist of an unlined segment of lava tube cave. -
Table 4. Hawaiian Newspaper Sources
OCS Study BOEM 2017-022 A ‘Ikena I Kai (Seaward Viewsheds): Inventory of Terrestrial Properties for Assessment of Marine Viewsheds on the Main Eight Hawaiian Islands U.S. Department of the Interior Bureau of Ocean Energy Management Pacific OCS Region August 18, 2017 Cover image: Viewshed among the Hawaiian Islands. (Trisha Kehaulani Watson © 2014 All rights reserved) OCS Study BOEM 2017-022 Nā ‘Ikena I Kai (Seaward Viewsheds): Inventory of Terrestrial Properties for Assessment of Marine Viewsheds on the Eight Main Hawaiian Islands Authors T. Watson K. Ho‘omanawanui R. Thurman B. Thao K. Boyne Prepared under BOEM Interagency Agreement M13PG00018 By Honua Consulting 4348 Wai‘alae Avenue #254 Honolulu, Hawai‘i 96816 U.S. Department of the Interior Bureau of Ocean Energy Management Pacific OCS Region August 18, 2016 DISCLAIMER This study was funded, in part, by the US Department of the Interior, Bureau of Ocean Energy Management, Environmental Studies Program, Washington, DC, through Interagency Agreement Number M13PG00018 with the US Department of Commerce, National Oceanic and Atmospheric Administration, Office of National Marine Sanctuaries. This report has been technically reviewed by the ONMS and the Bureau of Ocean Energy Management (BOEM) and has been approved for publication. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the US Government, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. REPORT AVAILABILITY To download a PDF file of this report, go to the US Department of the Interior, Bureau of Ocean Energy Management, Environmental Studies Program Information System website and search on OCS Study BOEM 2017-022. -
Petrology, Mineralogy, and Geochemistry of the East Molokai Volcanic Series, Hawaii
Petrology, Mineralogy, and Geochemistry of the East Molokai Volcanic Series, Hawaii GEOLOGICAL SURVEY PROFESSIONAL PAPER 961 Petrology, Mineralogy, and Geochemistry of the East Molokai Volcanic Series, Hawaii By MELVIN H. BEESON GEOLOGICAL SURVEY PROFESSIONAL PAPER 961 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 76-12795 For ~ale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02810-7 CONTENTS Page Page 1\bstract__________________________________________________ 1 Phenocryst-free compositions ------------------------------ 14 Introduction ---------------------------------------------- 1 Mineralogy ____ __ __ __ __ ______ __ ________ __ __________ ______ 21 Previous investigations------------------------------------ 3 Compositional variation of olivine______________________ 21 Purpose and scope ---------------------------------------- 4 Compositional variation of clinopyroxene ______________ 25 1\nalytical procedures ------------------------------------ 4 Compositional variation of plagioclase__________________ 27 Stratigraphy and petrology-------------------------------- 6 Compositional variation of opaque minerals ____________ 28 Whole-rock compositions ---------------------------------- 11 Summary ------------------------------------------------ 30 References________________________________________________ 33 -
Waimanu Valley Oral History Report
WAIMANU VALLEY ORAL HISTORY REPORT prepared by . Kim Des Rochers for the Natural Area Reserve System Department of Land and Natural Resources, State of Hawaii Honolulu, Hawaii and Sea Grant Extension Service, University of Hawaii at Manoa Honolulu, Hawaii August 1990 UNI H I-SEAGRANT -OT -89-02 WAIMANU VALLEY ORAL HISTORY REPORT prepared by Kim Des Rochers for the Natural Area Reserve System Department of Land and Natural Resources, State of Hawaii Honolulu, Hawaii and Sea Grant Extension Service, University of Hawaii at Manoa Honolulu, Hawaii August 1990 TABLE OF CONTENTS ACKNOWLEDGEMENTS ............................................................................ 1 PROJECT DESCRIPTION AND BACKGROUND .............................................. 2 METHODOLOGy ......................................................................................5 EARLY HISTORY OF WAIMANU VALLEy ..................................................... 7 BIBLIOGRAPHy ...................................................................................... 11 Biographical Summary for Eugene Burke .................................................... 1 6 Oral History Interviews with Eugene Burke ................................................. 17 Biographical Summary for Wilfred Mock Chew ........................................... 43 Oral History Interviews with Wilfred Mock Chew ........................................ 44 Biographical Summary for Lily Chong ........................................................ 79 Oral History Interview with Lily Chong ..................................................... -
Hawaiian Mission Children Named After Ali'ì
Hawaiian Mission Children Named After Ali‘ì “I was born in the ‘Old Mission House’ in Honolulu on the 5th day of July, 1831. When I was but a few hours old, ‘Kīna’u,’ the Premier, came into the bedroom with her crowd of ‘kahus,’ took me into her arms and said that she wanted to adopt me, as she had no girl of her own.” “My mother, in her weak state, was terribly agitated, knowing that the missionaries were unpopular and entirely dependent on the good-will of the natives, so feared the consequences of a denial. They sent for my father in haste, who took in the state of affairs at a glance.” “’We don’t give away our children,’ he said to Kīna’u. ‘But you are poor, I am rich, I give you much money,’ replied the Chiefess. ‘No, you can’t have her,’ my father answered firmly. Kīna’u tossed me angrily down on the bed and walked away, leaving my poor mother in a very anxious frame of mind.” (Wilder; Wight) “She accordingly went away in an angry and sullen mood, and was not heard from until the infant was being christened a few weeks later, when she again appeared, elbowed the father to one side, and exclaimed in the haughtiest of tones, ‘Call the little baby Kīna’u.’” “Fearing that a second refusal would result disastrously, the parents agreed, and the child was accordingly christened Elizabeth Kīna’u Judd.” (The Friend, May 1912) Kīna’u “seemed somewhat appeased after the (christening) ceremony, and, as I was the first white girl she had ever seen, deigned from that time on to show a great interest in me, either visiting me or having me visit her every day.” (Wright, Wight) Kīna’u, daughter of Kamehameha I, became a Christian in 1830.