OSDS) to Human Health and Critical Ecosystems on the Islands of Hawaii, Kauai, Maui, and Molokai
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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. -
Photographing the Islands of Hawaii
Molokai Sea Cliffs - Molokai, Hawaii Photographing the Islands of Hawaii by E.J. Peiker Introduction to the Hawaiian Islands The Hawaiian Islands are an archipelago of eight primary islands and many atolls that extend for 1600 miles in the central Pacific Ocean. The larger and inhabited islands are what we commonly refer to as Hawaii, the 50 th State of the United States of America. The main islands, from east to west, are comprised of the Island of Hawaii (also known as the Big Island), Maui, Kahoolawe, Molokai, Lanai, Oahu, Kauai, and Niihau. Beyond Niihau to the west lie the atolls beginning with Kaula and extending to Kure Atoll in the west. Kure Atoll is the last place on Earth to change days and the last place on Earth to ring in the new year. The islands of Oahu, Maui, Kauai and Hawaii (Big Island) are the most visited and developed with infrastructure equivalent to much of the civilized world. Molokai and Lanai have very limited accommodation options and infrastructure and have far fewer people. All six of these islands offer an abundance of photographic possibilities. Kahoolawe and Niihau are essentially off-limits. Kahoolawe was a Navy bombing range until recent years and has lots of unexploded ordinance. It is possible to go there as part of a restoration mission but one cannot go there as a photo destination. Niihau is reserved for the very few people of 100% Hawaiian origin and cannot be visited for photography if at all. Neither have any infrastructure. Kahoolawe is photographable from a distance from the southern shores of Maui and Niihau can be seen from the southwestern part of Kauai. -
Nihoa Manawai Holoikauaua Pearl & Hermes Atoll Kapou Papa'āpoho Lisianski Island Kamole Kauō Laysan Island Kamokuokamohoali'i Ko'anako'a Maro Reef
175°E 180° 175°W 170°W 165°W 160°W 155°W 150°W 35°N 35°N North America Japan Map Area Photo by Dan Clark/USFWS Hawaiian Islands Photo by Na‘alehu Anthony P a c i f i c Seabird Refuge A Living Hawaiian Culture O c e a n The monument is home to over 14 million seabirds 30°N Hiryū USS Yorktown Equator representing 23 species. This includes the world's Traditional Hawaiian accounts describe largest colonies of Laysan and black-footed Papahānaumokuākea as a sacred area from which Rapa Sōryū albatross. Pictured above is the world's oldest life first emerged and to which spirits return after Nui Australia known bird in the wild – a Laysan albatross named 30°N death. Akagi Wisdom! Banded in 1956 when she was at least five Kaga years old, Wisdom may have hatched more than 36 New Zealand chicks in her lifetime. Hōlanikū Manawai Unnamed Holoikauaua Mokupāpapa Seamount Kure Atoll Pearl & Hermes Atoll 582,578 square miles, only six square miles of land Helsley Seamount Ladd Seamount Kamole Kauō ‘Ōnūnui, ‘Ōnūiki Photo by Mark Sullivan/NOAA Laysan Island Photo by NOAA/OER Endemic Sanctuary Pūhāhonu New Discoveries The monument is home to many species found Kuaihelani Gardner Pinnacles The majority of the seafloor in the Northwestern nowhere else on Earth and is a critically important Pihemanu Salmon Hawaiian Islands lies at depths below 10,000 feet nesting ground for green sea turtles and breeding Bank (3,000 meters). Using advanced technologies like ground for Hawaiian monk seals. -
Albatross Or Mōlī (Phoebastria Immutabilis) Black-Footed Albatross Or Ka’Upu (Phoebastria Nigripes) Short-Tailed Albatross (Phoebastria Albatrus)
Hawaiian Bird Conservation Action Plan Focal Species: Laysan Albatross or Mōlī (Phoebastria immutabilis) Black-footed Albatross or Ka’upu (Phoebastria nigripes) Short-tailed Albatross (Phoebastria albatrus) Synopsis: These three North Pacific albatrosses are demographically similar, share vast oceanic ranges, and face similar threats. Laysan and Black-footed Albatrosses nest primarily in the Northwestern Hawaiian Islands, while the Short-tailed Albatross nests mainly on islands near Japan but forages extensively in U.S. waters. The Short-tailed Albatross was once thought to be extinct but its population has been growing steadily since it was rediscovered in 1951 and now numbers over 3,000 birds. The Laysan is the most numerous albatross species in the world with a population over 1.5 million, but its trend has been hard to determine because of fluctuations in number of breeding pairs. The Black-footed Albatross is one-tenth as numerous as the Laysan and its trend also has been difficult to determine. Fisheries bycatch caused unsustainable mortality of adults in all three species but has been greatly reduced in the past 10-20 years. Climate change and sea level rise are perhaps the greatest long-term threat to Laysan and Black-footed Albatrosses because their largest colonies are on low-lying atolls. Protecting and creating colonies on higher islands and managing non-native predators and human conflicts may become keys to their survival. Laysan, Black-footed, and Short-tailed Albatrosses (left to right), Midway. Photos Eric VanderWerf Status -
APRIL 8, 2020 Featuring Oahu, Kauai & Maui
featuring Oahu, Kauai & Maui MARCH 30 - APRIL 8, 2020 with Host JOJO TURNBEAUGH, Co-Host of Big Al & JoJo on KOA the Valley Isle for the valleys carved YOUR EXPERIENCE INCLUDES into its mountains. Lunch at the Maui • All airfare Ocean Center offers stunning views • All inter-island flights & baggage fees, of Ma’alaea Bay Harbor. After lunch, fuel surcharges, government fees, airport there’s time to browse the center’s & departure taxes (minimum value of unique collection of marine life and $250 per person) their 3D Humpbacks of Hawaii expe- rience. Next, we drive to Lahaina, an • Guaranteed prices & low deposit old whaling port dotted with historical • Holiday Tour Director & local guides landmarks, shops, and galleries. • Baggage handling at hotels The town is especially known for its • $100 travel voucher for a future tour gigantic Banyan tree whose branches JOJO TURNBEAUGH reach out over an acre. Later we 10 Excellent Meals Featuring arrive at the Hyatt Regency Maui • KOA Radio Welcome Lunch in JoJo joins Alfred “Big Al” Williams Resort & Spa for three nights to Honolulu enjoy 40 oceanfront acres of lavish every weekday from 3 p.m. until 7 • Lunch at Kilohana Plantation p.m. for Big Al & JoJo — a show that swimming pools, tropical plants, • Full breakfast buffet at Swan Court combines exclusive Broncos news, the shopping, and multiple dining Hyatt Regency Maui day’s top sports stories, and fun topics options. We have easy access to that make your drive home stress-free. long beach strolls from here and • Holiday Vacations Farewell Lunch a private balcony off your room. -
RECORDS of the HAWAII BIOLOGICAL SURVEY for 1994 Part 2: Notes1
1 RECORDS OF THE HAWAII BIOLOGICAL SURVEY FOR 1994 Part 2: Notes1 This is the second of two parts to the Records of the Hawaii Biological Survey for 1994 and contains the notes on Hawaiian species of plants and animals including new state and island records, range extensions, and other information. Larger, more comprehensive treatments and papers describing new taxa are treated in the first part of this volume [Bishop Museum Occasional Papers 41]. New Hawaiian Plant Records. I BARBARA M. HAWLEY & B. LEILANI PYLE (Herbarium Pacificum, Department of Natural Sciences, Bishop Museum, P.O. Box 19000A, Honolulu, Hawaii 96817, USA) Amaranthaceae Achyranthes mutica A. Gray Significance. Considered extinct and previously known from only 2 collections: sup- posedly from Hawaii Island 1779, D. Nelson s.n.; and from Kauai between 1851 and 1855, J. Remy 208 (Wagner et al., 1990, Manual of the Flowering Plants of Hawai‘i, p. 181). Material examined. HAWAII: South Kohala, Keawewai Gulch, 975 m, gulch with pasture and relict Koaie, 10 Nov 1991, T.K. Pratt s.n.; W of Kilohana fork, 1000 m, on sides of dry gulch ca. 20 plants seen above and below falls, 350 °N aspect, 16 Dec 1992, K.R. Wood & S. Perlman 2177 (BISH). Caryophyllaceae Silene lanceolata A. Gray Significance. New island record for Oahu. Distribution in Wagner et al. (1990: 523, loc. cit.) limited to Kauai, Molokai, Hawaii, and Lanai. Several plants were later noted by Steve Perlman and Ken Wood from Makua, Oahu in 1993. Material examined. OAHU: Waianae Range, Ohikilolo Ridge at ca. 700 m elevation, off ridge crest, growing on a vertical rock face, facing northward and generally shaded most of the day but in an open, exposed face, only 1 plant noted, 25 Sep 1992, J. -
A Summary of Historical Shoreline Changes on Beaches of Kauai, Oahu, and Maui, Hawaii Bradley M
Journal of Coastal Research 00 0 000–000 West Palm Beach, Florida Month 0000 A Summary of Historical Shoreline Changes on Beaches of Kauai, Oahu, and Maui, Hawaii Bradley M. Romine and Charles H. Fletcher* Department of Geology and Geophysics www.cerf-jcr.org School of Ocean and Earth Science and Technology University of Hawaii at Manoa POST Building, Suite 701, 1680 East–West Road Honolulu, HI 96822, USA [email protected], [email protected] ABSTRACT ROMINE, B.M. and FLETCHER, C.H., 2012. A summary of historical shoreline changes on beaches of Kauai, Oahu, and Maui; Hawaii. Journal of Coastal Research, 00(0), 000–000. West Palm Beach (Florida), ISSN 0749-0208. Shoreline change was measured along the beaches of Kauai, Oahu, and Maui (Hawaii) using historical shorelines digitized from aerial photographs and survey charts for the U.S. Geological Survey’s National Assessment of Shoreline Change. To our knowledge, this is the most comprehensive report on shoreline change throughout Hawaii and supplements the limited data on beach changes in carbonate reef–dominated systems. Trends in long-term (early 1900s– present) and short-term (mid-1940s–present) shoreline change were calculated at regular intervals (20 m) along the shore using weighted linear regression. Erosion dominated the shoreline change in Hawaii, with 70% of beaches being erosional (long-term), including 9% (21 km) that was completely lost to erosion (e.g., seawalls), and an average shoreline change rate of 20.11 6 0.01 m/y. Short-term results were somewhat less erosional (63% erosional, average change rate of 20.06 6 0.01 m/y). -
New Plant Records from the Hawaiian Archipelago
Records of the Hawaii Biological Survey for 2001–2002—Part II: Notes 23 11 (BISH); Kaplama Heights, Kamehameha Girls School, 6 Jun 1932, A. F. Judd, E. H. Bryan Jr., & M. Neal s.n. (BISH 42874); Ko‘olau Loa Distr., Sunset Beach, common ornamental or pot flower, elev. 5 m, 25 Mar 1975, D. Afualo s.n. (BISH 580134). Acknowledgments Jan Doorenbos (WAG) identified numerous voucher specimens of cultivated Begonia from BISH, which provided an excellent reference base for ongoing identification of new specimens received by Herbarium Pacificum. Literature Cited Burt-Utley, K. 1985. A revision of Central American species of Begonia sect. Gireoudia (Begoniaceae). Tulane Stud. Zool. Bot. 25(1): 1–131. de Lange, A. & F. Bouman. 1999. Seed micromorphology of Neotropical begonias. Smithson. Contrib. Bot. 90: 1–49. Staples, G. W., D. Herbst & C. T. Imada. 2000. Survey of invasive or potentially inva- sive cultivated plants in Hawai‘i. Bishop Mus. Occas. Pap. 65: 1–35. New plant records from the Hawaiian Archipelago FOREST STARR, KIM STARR, & LLOYD L. LOOPE (United States Geological Survey, Biological Resources Division, P.O. Box 369, Makawao, Hawai‘i 96768, USA; email: [email protected]). The following contributions include new island records, new state records, and range extensions of plants located on Kure Atoll, Midway Atoll, Maui, and Hawai‘i. Voucher specimens are housed in the Bishop Museum’s Herbarium Pacificum, Honolulu. Agavaceae Sanseviera trifasciata Prain New island record Previously known to be naturalized on O‘ahu where several extensive roadside popula- tions were found (Imada et al., 2000), S. trifasciata (mother-in-law’s tongue) is now also known to be naturalized on Maui where it is similarly distributed. -
A Progressive, Ealanced Coastal Construction Seteack Ordinance on the Island of Kauai, Hawaii: Implementation and Lessons Learned
Proceedingsof CoastalZone 09 Boston,Massachusetts July J9 to 23, 2009 A PROGRESSIVE, EALANCED COASTAL CONSTRUCTION SETEACK ORDINANCE ON THE ISLAND OF KAUAI, HAWAII: IMPLEMENTATION AND LESSONS LEARNED James F. O' Connell, University of Hawaii Sea Grant College Program, Kauai, HI Dolan Eversole, University of Hawaii Sea Grant College Program, Oahu, HI Zoe Norcross-Nu'u, University of Hawaii Sea Grant College Program, Maui, HI KEYWORDS: shoreline setback, ordinance, erosion, coastal zone management, Kauai County, Hawaii, shoreline change In terms of private property use and coastal resource protection, in January 2008 Kauai County, Hawaii, passed one the most balanced coastal construction setback ordinances in the Country: 'The Shoreline Setback and Coastal Protection Ordinance ¹863.' To protect life, property, and preserve coastal resources the Ordinance sets procedures establishing minimum construction setbacksbased on average lot depth and long-term shoreline erosion rates being generatedby the University of Hawaii. Furthermore, the Ordinance intent is to safely site structures away from hazards, such as coastal erosion, so shoreline hardening will not be required to protect the property during its useful life. Specific listed activities are also permitted or prohibited without a variance within the setback area. The Ordinance applies to all lands that abut or are within 500 feet of the shore. To ensure broad support, variance procedures allow variations in zoning setbacks, minimum allowable buildable footprint, and shoreline setbacks,providing that under no circumstance shall the shoreline setback be less than forty feet for new dwellings, and twenty feet for rebuilding existing dwellings. Any structure approved within the setback area by variance shall not be eligible for protection by shoreline hardening during the life of the structure. -
Northwestern Hawaiian Islands/Kure Atoll Assessment and Monitoring Program
Northwestern Hawaiian Islands/Kure Atoll Assessment and Monitoring Program Final Report March 2002 Grant Number NA070A0457 William j. Walsh1, Ryan Okano2, Robert Nishimoto1, Brent Carman1. 1 Division of Aquatic Resources 1151 Punchbowl Street Rm. 330 Honolulu, HI 96813 2 Botany Department University of Hawai`i Mānoa Honolulu, HI 96822 2 INTRODUCTION The Northwest Hawaiian Islands (NWHI) consist of 9,124 km2 of land and approximately 13,000 km2 of coral reef habitat. They comprise 70% of all coral reef areas under U.S. jurisdiction. This isolated archipelago of small islands, atolls, reefs and banks represent a unique and largely pristine coral reef ecosystem. The islands support millions of nesting seabirds and are breeding grounds for the critically endangered Hawaiian monk seal and threatened green sea turtle. The reefs include a wide range of habitats and support a diverse assemblage of indigenous and endemic reef species, many of which have yet to be described. Kure Atoll, located at the northwestern end of the NWHI chain (approximately 28º 25’ N latitude and 178º 20’ W longitude) is the northernmost atoll in the world. The atoll is located 91 km northwest of Midway Islands and nearly 1,958 km northwest of Honolulu. It is a nearly circular atoll with a diameter of 10 km (6mi). The outer reef is continuous Figure 1. IKONOS satellite image of Kure Atoll 3 and almost encircles the atoll’s lagoon except for passages to the southwest (Fig. 1). An emergent rock ledge consisting primarily of coralline algae and algally bound and encrusted coral is present along some sections of the reef crest. -
The Hawaiian Islands –Tectonic Plate Movement
Plate Tectonics Worksheet 2 L3 MiSP Plate Tectonics Worksheet #2 L3 Name _____________________________ Date_____________ THE HAWAIIAN ISLANDS – TECTONIC PLATE MOVEMENT Introduction: (excerpts from Wikipedia and http://pubs.usgs.gov/publications/text/Hawaiian.html) The Hawaiian Islands represent the last and youngest part of a long chain of volcanoes extending some 6000 km across the Pacific Ocean and ending in the Aleutian Trench off the coast of Alaska. This volcanic chain consists of the small section Hawaiian archipelago (Windward Isles, and the U.S. State of Hawaii), the much longer Northwestern Hawaiian Islands (Leeward Isles), and finally the long Emperor Seamounts. The Leeward Isles consist mostly of atolls, atoll islands and extinct islands, while the Emperor Seamounts are extinct volcanoes that have been eroded well beneath sea level. This long volcanic chain was created over some 70 million years by a hot spot that supplied magma, formed deep in the earth’s interior (mantle), that pushed its way through the earth’s surface and ocean cover forming volcanic islands. As the Pacific Plate was moved by tectonic forces within the Earth, the hot spot continually formed new volcanoes on the Pacific Plate, producing the volcanic chain. The direction and rate of movement for the Pacific Plate will be determined with the help of the approximate age of some of the Hawaiian volcanoes and distances between them. Procedure 1: 1. Using the data provided in Table 1 , plot a graph on the next page that compares the age of the Hawaiian Islands and reefs to their longitude. 2. Label the island (reef) name next to each plotted point. -
The Russian Forts on Kauai, Hawaiian Islands: a Brief Synthesis
19005 Coast Highway One, Jenner, CA 95450 ■ 707.847.3437 ■ [email protected] ■ www.fortross.org Title: The Russian Forts on Kauai, Hawaiian Islands: a Brief Synthesis Author (s): William K. Kikuchi and Delores L. Kikuchi Source: Fort Ross Conservancy Library URL: http://www.fortross.org/lib.html Unless otherwise noted in the manuscript, each author maintains copyright of his or her written material. Fort Ross Conservancy (FRC) asks that you acknowledge FRC as the distributor of the content; if you use material from FRC’s online library, we request that you link directly to the URL provided. If you use the content offline, we ask that you credit the source as follows: “Digital content courtesy of Fort Ross Conservancy, www.fortross.org; author maintains copyright of his or her written material.” Also please consider becoming a member of Fort Ross Conservancy to ensure our work of promoting and protecting Fort Ross continues: http://www.fortross.org/join.htm. This online repository, funded by Renova Fort Ross Foundation, is brought to you by Fort Ross Conservancy, a 501(c)(3) and California State Park cooperating association. FRC’s mission is to connect people to the history and beauty of Fort Ross and Salt Point State Parks. 1. · THE RUSSIAN FORTS ON YJ~UAI, HAWAIIAN ISLfu.~DS: A BRIEF SYNTHESIS by William K. Kikuchi and Delores L. Kikuchi PREFACE This report was written in partial fulfillment of Contract Number 11755 between the author and the State of Hawaii, Department of Land and Natural Resources, Division of State Parks. The contract originally called for the archaeological survey of .