Movement Patterns of Hawaiian Petrels and Newell's Sheatwaters
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Life in Mauna Kea's Alpine Desert
Life in Mauna Kea’s by Mike Richardson Alpine Desert Lycosa wolf spiders, a centipede that preys on moribund insects that are blown to the summit, and the unique, flightless wekiu bug. A candidate for federal listing as an endangered species, the wekiu bug was first discovered in 1979 by entomologists on Pu‘u Wekiu, the summit cinder cone. “Wekiu” is Hawaiian for “topmost” or “summit.” The wekiu bug belongs to the family Lygaeidae within the order of insects known as Heteroptera (true bugs). Most of the 26 endemic Hawaiian Nysius species use a tube-like beak to feed on native plant seed heads, but the wekiu bug uses its beak to suck the hemolymph (blood) from other insects. High above the sunny beaches, rocky coastline, Excluding its close relative Nysius a‘a on the nearby Mauna Loa, the wekiu bug and lush, tropical forests of the Big Island of Hawai‘i differs from all the world’s 106 Nysius lies a unique environment unknown even to many species in its predatory habits and unusual physical characteristics. The bug residents. The harsh, barren, cold alpine desert is so possesses nearly microscopically small hostile that it may appear devoid of life. However, a wings and has the longest, thinnest legs few species existing nowhere else have formed a pre- and the most elongated head of any Lygaeid bug in the world. carious ecosystem-in-miniature of insects, spiders, The wekiu bug, about the size of a other arthropods, and simple plants and lichens. Wel grain of rice, is most often found under rocks and cinders where it preys diur come to the summit of Mauna Kea! nally (during daylight) on insects and Rising 13,796 feet (4,205 meters) dependent) community of arthropods even birds that are blown up from lower above sea level, Mauna Kea is the was uncovered at the summit. -
Mauna Loa Reconnaissance 2003
“Giant of the Pacific” Mauna Loa Reconnaissance 2003 Plan of encampment on Mauna Loa summit illustrated by C. Wilkes, Engraved by N. Gimbrede (Wilkes 1845; vol. IV:155) Prepared by Dennis Dougherty B.A., Project Director Edited by J. Moniz-Nakamura, Ph. D. Principal Investigator Pacific Island Cluster Publications in Anthropology #4 National Park Service Hawai‘i Volcanoes National Park Department of the Interior 2004 “Giant of the Pacific” Mauna Loa Reconnaissance 2003 Prepared by Dennis Dougherty, B.A. Edited by J. Moniz-Nakamura, Ph.D. National Park Service Hawai‘i Volcanoes National Park P.O. Box 52 Hawaii National Park, HI 96718 November, 2004 Mauna Loa Reconnaissance 2003 Executive Summary and Acknowledgements The Mauna Loa Reconnaissance project was designed to generate archival and inventory/survey level recordation for previously known and unknown cultural resources within the high elevation zones (montane, sub-alpine, and alpine) of Mauna Loa. Field survey efforts included collecting GPS data at sites, preparing detailed site plan maps and feature descriptions, providing site assessment and National Register eligibility, and integrating the collected data into existing site data bases within the CRM Division at Hawaii Volcanoes National Park (HAVO). Project implementation included both pedestrian transects and aerial transects to accomplish field survey components and included both NPS and Research Corporation University of Hawaii (RCUH) personnel. Reconnaissance of remote alpine areas was needed to increase existing data on historic and archeological sites on Mauna Loa to allow park managers to better plan for future projects. The reconnaissance report includes a project introduction; background sections including physical descriptions, cultural setting overview, and previous archeological studies; fieldwork sections describing methods, results, and feature and site summaries; and a section on conclusions and findings that provide site significance assessments and recommendations. -
THE HAWAIIAN-EMPEROR VOLCANIC CHAIN Part I Geologic Evolution
VOLCANISM IN HAWAII Chapter 1 - .-............,. THE HAWAIIAN-EMPEROR VOLCANIC CHAIN Part I Geologic Evolution By David A. Clague and G. Brent Dalrymple ABSTRACT chain, the near-fixity of the hot spot, the chemistry and timing of The Hawaiian-Emperor volcanic chain stretches nearly the eruptions from individual volcanoes, and the detailed geom 6,000 km across the North Pacific Ocean and consists of at least etry of volcanism. None of the geophysical hypotheses pro t 07 individual volcanoes with a total volume of about 1 million posed to date are fully satisfactory. However, the existence of km3• The chain is age progressive with still-active volcanoes at the Hawaiian ewell suggests that hot spots are indeed hot. In the southeast end and 80-75-Ma volcanoes at the northwest addition, both geophysical and geochemical hypotheses suggest end. The bend between the Hawaiian and .Emperor Chains that primitive undegassed mantle material ascends beneath reflects a major change in Pacific plate motion at 43.1 ± 1.4 Ma Hawaii. Petrologic models suggest that this primitive material and probably was caused by collision of the Indian subcontinent reacts with the ocean lithosphere to produce the compositional into Eurasia and the resulting reorganization of oceanic spread range of Hawaiian lava. ing centers and initiation of subduction zones in the western Pacific. The volcanoes of the chain were erupted onto the floor of the Pacific Ocean without regard for the age or preexisting INTRODUCTION structure of the ocean crust. Hawaiian volcanoes erupt lava of distinct chemical com The Hawaiian Islands; the seamounts, hanks, and islands of positions during four major stages in their evolution and the Hawaiian Ridge; and the chain of Emperor Seamounts form an growth. -
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 -
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. -
Metadata for Hawaii Environmental Sensitivity Index (ESI)
HYDRO Hawaii ESI: HYDRO (Hydrology Polygons and Lines) Metadata: Identification_Information Data_Quality_Information Spatial_Data_Organization_Information Spatial_Reference_Information Entity_and_Attribute_Information Distribution_Information Metadata_Reference_Information Identification_Information: Citation: Citation_Information: Originator: National Oceanic and Atmospheric Administration (NOAA), National Ocean Service, Office of Response and Restoration, Hazardous Materials Response Division, Seattle, Washington Publication_Date: 200111 Title: Hawaii ESI: HYDRO (Hydrology Polygons and Lines) Edition: Second Geospatial_Data_Presentation_Form: Vector digital data Series_Information: Series_Name: None Issue_Identification: Hawaii Publication_Information: Publication_Place: Seattle, Washington Publisher: National Oceanic and Atmospheric Administration (NOAA), National Ocean Service, Office of Response and Restoration, Hazardous Materials Response Division, Seattle, Washington Other_Citation_Details: Prepared by Research Planning, Inc., Columbia, South Carolina for the National Oceanic and Atmospheric Administration (NOAA), National Ocean Service, Office of Response and Restoration, Hazardous Materials Response Division, Seattle, Washington Description: Abstract: This data set contains vector arcs and polygons representing coastal hydrography used in the creation of the Environmental Sensitivity Index (ESI) for Hawaii. The HYDRO data layer contains all annotation used in producing the atlas. The annotation features are categorized into -
Ecologically Distinct Populations of Hawaiian Petrel (Pterodroma
The University of Akron IdeaExchange@UAkron Williams Honors College, Honors Research The Dr. Gary B. and Pamela S. Williams Honors Projects College Spring 2020 Ecologically Distinct Populations of Hawaiian Petrel (Pterodroma sandwichensis): Quantitative Isotopic Analysis to Explore the Uniqueness of Foraging Habits in Kauai and Hawaii Populations Drew Casey [email protected] Follow this and additional works at: https://ideaexchange.uakron.edu/honors_research_projects Part of the Population Biology Commons Please take a moment to share how this work helps you through this survey. Your feedback will be important as we plan further development of our repository. Recommended Citation Casey, Drew, "Ecologically Distinct Populations of Hawaiian Petrel (Pterodroma sandwichensis): Quantitative Isotopic Analysis to Explore the Uniqueness of Foraging Habits in Kauai and Hawaii Populations" (2020). Williams Honors College, Honors Research Projects. 1046. https://ideaexchange.uakron.edu/honors_research_projects/1046 This Dissertation/Thesis is brought to you for free and open access by The Dr. Gary B. and Pamela S. Williams Honors College at IdeaExchange@UAkron, the institutional repository of The University of Akron in Akron, Ohio, USA. It has been accepted for inclusion in Williams Honors College, Honors Research Projects by an authorized administrator of IdeaExchange@UAkron. For more information, please contact [email protected], [email protected]. Ecologically Distinct Populations of Hawaiian Petrel (Pterodroma sandwichensis): Quantitative -
Post-Release Survival of Fallout Newell's Shearwater Fledglings From
Vol. 43: 39–50, 2020 ENDANGERED SPECIES RESEARCH Published September 3 https://doi.org/10.3354/esr01051 Endang Species Res OPEN ACCESS Post-release survival of fallout Newell’s shearwater fledglings from a rescue and rehabilitation program on Kaua‘i, Hawai‘i André F. Raine1,*, Tracy Anderson2, Megan Vynne1, Scott Driskill1, Helen Raine3, Josh Adams4 1Kaua‘i Endangered Seabird Recovery Project (KESRP), Pacific Cooperative Studies Unit (PCSU), University of Hawai‘i and Division of Forestry and Wildlife, State of Hawai‘i Department of Land and Natural Resources, Hanapepe, HI 96716, USA 2Save Our Shearwaters, Humane Society, 3-825 Kaumualii Hwy, Lihue, HI 96766, USA 3Archipelago Research and Conservation, 3861 Ulu Alii Street, Kalaheo, HI 96741, USA 4U.S. Geological Survey, Western Ecological Research Center, Santa Cruz Field Station 2885 Mission St., Santa Cruz, CA 95060, USA ABSTRACT: Light attraction impacts nocturnally active fledgling seabirds worldwide and is a par- ticularly acute problem on Kaua‘i (the northern-most island in the main Hawaiian Island archipel- ago) for the Critically Endangered Newell’s shearwater Puffinus newelli. The Save Our Shearwaters (SOS) program was created in 1979 to address this issue and to date has recovered and released to sea more than 30 500 fledglings. Although the value of the program for animal welfare is clear, as birds cannot simply be left to die, no evaluation exists to inform post-release survival. We used satellite transmitters to track 38 fledglings released by SOS and compared their survival rates (assessed by tag transmission duration) to those of 12 chicks that fledged naturally from the moun- tains of Kaua‘i. -
Chemistry of Kilauea and Mauna Loa Lava in Space and Time
"JflK 8 B72 Branch of Chemistry of Kilauea and Mauna Loa Lava in Space and Time GEOLOGICAL SURVEY PROFESSIONAL PAPER 735 Chemistry of Kilauea and Mauna Loa Lava in Space and Time By THOMAS L. WRIGHT GEOLOGICAL SURVEY PROFESSIONAL PAPER 735 An account of the chemical composition of lavas from Kilauea and Mauna Loa volcanoes. Hawaii, and an interpretation of the processes of partial melting and subsequent fractional crystallization that produced the chemical variability UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS G. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, A cting Director Library of Congress catalog-card No. 74-178247 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Price 50 cents (paper.cover) Stock number 2401-1185 CONTENTS Page Page Abstract ________________________________________ 1 Observations Continued Introduction _____________________________________ 1 Olivine-controlled lavas _________________ 16 Acknowledgments ________________________________ 2 Petrography __________ __ 16 Definitions and terminology _______________________ 2 Chemistry _______________________ 16 Tholeiite ____________________________________ 2 Differentiated lavas ______ _ ___ 23 Mineral control lines _________________________ 4 Chemical variation within Kilauea lava and differ Olivine-controlled and differentiated basalt _____ 4 ence between Kilauea and Mauna Loa lavas____ 23 Previous work ___________________________________ 5 -
Activities/Attractions Business Name Island Open/Closed Projected
Activities/Attractions Business Name Island Open/Closed Projected Reopening Air Ventures Hawaii Kaua‘i Temporarily Closed TBD Alii Kauai Air Tours & Charters Kaua‘i Open Aloha with Touch Kauai Kaua‘i Open Anaina Hou Community Park Kaua‘i Open Anara Spa Kaua‘i Open Apex Charters Kaua‘i Open Aulii Luau Kaua‘i Temporarily Closed TBD Best of Kauai Tour Kaua‘i Open Blue Dolphin Charters Kaua‘i Open Blue Hawaiian Helicopters Kaua‘i Open Blue Ocean Adventure Tours Kaua‘i Open Bubbles Below Scuba Charters Kaua‘i Open Captain Andy's Sailing Adventures Kaua‘i Open Catamaran Kahanu Kaua‘i Open CJM Country Stables, Inc. Kaua‘i Open Common Ground Kauai Kaua‘i Open CrossFit Poipu Kaua‘i Open Da Life Outdoors Kaua‘i Open Deep Sea Fishing Kauai Kaua‘i Open Dolphin Touch Wellness Center Kaua‘i Open Eco eBikes Kauai Kaua‘i Open Garden Island Chocolate Kaua‘i Open GetYourGuide Kaua‘i Open Go Fish Kauai Kaua‘i Open Grand Hyatt Kauai Luau Kaua‘i Temporarily Closed TBD Grove Farm Museum Kaua‘i Open Halele'a Spa Kaua‘i Temporarily Closed 2022 Hanalei Spirits Distillery Corp Kaua‘i Open Holo Holo Charters Kaua‘i Open Ho'opulapula Haraguchi Rice Mill Kaua‘i Temporarily Closed TBD Hunt Fish Kauai Kaua‘i Open Island Gym & Fitness Kaua‘i Open Island Helicopters Kauai, Inc. Kaua‘i Open Jack Harter Helicopters Kaua‘i Open Kauai Athletic Club-Lihue & Kapaa Kaua‘i Open Kauai ATV Kaua‘i Open Kauai Backcountry Adventures Kaua‘i Open Kauai Beach Boys Kaua‘i Open Kauai Bound Kaua‘i Open Kauai Coffee Company Visitor Center Kaua‘i Open Kauai CrossFit Kaua‘i Open Kauai Eco -
Hawaii Pacific Aviation Mauna Loa Helicopters Student Catalog
Hawaii Pacific Aviation Mauna Loa Helicopters Student Catalog Excellence In Flight Training HAWAII PACIFIC A VIATION M AUNA LOA H ELICOPTERS HAWAII Statement of Nondiscrimination The policy of Mauna Loa Helicopters assumes that no person in the United States shall be discriminated against because of race, religion, age, color, sex, disability, handicap, national origin, marital status, veteran’s status, political belief or affiliation, and that equal opportunity and access to facilities shall be available to all. MLH maintains all student records in confidentiality according to the Family Education Rights and Privacy Act of 1964. Because of the changing needs of the aviation industry, course content, material, or schedules, may occasionally change. Mauna Loa Helicopters reserves the right to make modifications and changes to the Professional Pilot Program and any individual courses offered. The changes may include staff or material and equipment used for the course. The FAA may change a regulation or standard, and MLH will maintain the necessary standards set forth by these governing powers. These changes are designed and incorporated to ensure each student receives the best training possible. This catalog, as well as other bulletins, publications or announcements, are subject to change without notice. Updates on the facts and other information in this catalog can be obtained from the President or General Manager. 73-310 U’u Street 90 Nakolo Place, Suite 2 301 Airport Boulevard maunaloahelicopters.com Kailua Kona, Hawaii 96740 Honolulu, Hawaii 96819 Troy, Alabama 36079 maunaloahelicoptertours.com 808-334-0234 808-834-6799 334-770-0359 Updated January 2015 2 HAWAII PACIFIC A VIATION M AUNA LOA H ELICOPTERS HAWAII Table of Contents Our School ............................................................................................................................................................ -
Maunaloa/Current/Longterm.Html K!Lauea – the Most Active Volcano on Earth K!Lauea Structure
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