Hawaiian Volcanoes and Your Knowledge of Science to Answer Questions 1–4
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Summary of 2016 Reef Fish Surveys Around Kahoolawe Island 1
doi:10.7289/V5/DR-PIFSC-17-011 Summary of 2016 Reef Fish Surveys around Kahoolawe Island 1 Results and information presented here summarize data gathered by the Coral Reef Ecosystem Program (CREP) of NOAA’s Pacific Islands Fisheries Science Center and partners during 2 days of reef fish and habitat surveys around Kahoolawe Island in July/August 2016. Surveys were conducted as part of the NOAA National Coral Reef Monitoring Program. Surveys were conducted using a standard sampling design and method implemented by NOAA’s Pacific Reef Assessment and Monitoring Program (Pacific RAMP) since 2009. In brief, pairs of divers record numbers, sizes, and species of fishes inside adjacent 15m-diameter ‘point- count’ cylinders and estimate benthic cover by functional groups (e.g. ‘coral’, ‘sand’). Because it is unpopulated and protected, Kahoolawe is an important reference location in in the main Hawaiian Islands and may also be a significant source of larvae and fish recruits for other parts of Maui-nui and perhaps beyond. Therefore, CREP hopes to routinely survey Kahoolawe reefs during future monitoring efforts. However, as 2016 was the first year for Kahoolawe surveys, we have a relatively small sample size there - 24 sites - in comparison to other Main Hawaiian Islands (MHI: between 107 and 257 survey sites per island). Main conclusions and observations: • Reef fish biomass was high at most sites we visited in Kahoolawe, with mean island-wide biomass higher than at any other of the MHI, although only marginally higher than at Niihau. Biomass tended to be slightly higher at sites along the southern section of the island. -
Demartini NWHI Overview for CRSAW (Feb 1
NOWRAMP Overview Ed DeMartini NOAA Fisheries, PIFSC • Objectives • Design & Status of Surveys • Major Patterns Northwestern Hawaiian Islands 99 9 9 99 9 9 9 9 NWHI Survey Objectives • Qualitative reconnaissance of ichthyofauna; describe relative abundance, assemblage structure • Initial quantitative assessment of both economic and ecologically interacting resources (corals, algae, macrobenthos as well as fishes); to provide baseline characterization of biota • Subsequent monitoring of target taxa at select representative stations; to enable detection of major changes over decadal time frame Summary of Design Elements • Develop sampling and analysis designs; standardize data collection protocols – size- and species/taxon- specific tallies per unit area • graded bins: by cm (< 5 cm), by 5 cm (6-50 cm), …by 25 cm (> 100 cm TL) – station(=dive): 3, 25-m long x 4- or 8- m wide belt transects, plus 4, 10- m radius (5-min) SPCs, apportioned among 3 divers • belts: total 600 m2 area for “large” (> 20 cm Total Length, TL) fishes • belts: total 300 m2 area for “small” (< 20 cm TL) fishes • SPCs: total @ 1257 m2 area (fish > 25 cm TL only) – followed by @ 3,000 m2 Roving Diver Survey • Analysis Design – abundance (N, biomass) for baseline assessment – density for monitoring temporal change – stratified by major habitat within reef (eg, fore-, back-reef, lagoonal patch at atolls) Sampling & Analysis Design Summary (cont’d) – at least 50% hard substrate – number of stations proportional to reef-area (and variance of stratum) – all sampleable reef quadrants (emphasis on leeward for monitoring) – distribute among-observer bias (< 15%) across stations and tasks – control for seasonality (eg, in recruitment) by design • differs among NWHI and other reef-systems NOWRAMP Cruise-Effort • 5-cruise baseline assessment • 25-mo period from Sep 00 to Oct 02 – Sep-Oct 00: NOAA’s Townsend Cromwell (TC00-10) & R/V Rapture – Sep 01: Cromwell (TC01-11); FFS, Maro Reef – Sep-Oct 02: Cromwell (TC02-07) & Rapture • Single monitoring cruise thus far – Jul-Aug 03: Oscar E. -
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. -
Spiders of the Hawaiian Islands: Catalog and Bibliography1
Pacific Insects 6 (4) : 665-687 December 30, 1964 SPIDERS OF THE HAWAIIAN ISLANDS: CATALOG AND BIBLIOGRAPHY1 By Theodore W. Suman BISHOP MUSEUM, HONOLULU, HAWAII Abstract: This paper contains a systematic list of species, and the literature references, of the spiders occurring in the Hawaiian Islands. The species total 149 of which 17 are record ed here for the first time. This paper lists the records and literature of the spiders in the Hawaiian Islands. The islands included are Kure, Midway, Laysan, French Frigate Shoal, Kauai, Oahu, Molokai, Lanai, Maui and Hawaii. The only major work dealing with the spiders in the Hawaiian Is. was published 60 years ago in " Fauna Hawaiiensis " by Simon (1900 & 1904). All of the endemic spiders known today, except Pseudanapis aloha Forster, are described in that work which also in cludes a listing of several introduced species. The spider collection available to Simon re presented only a small part of the entire Hawaiian fauna. In all probability, the endemic species are only partly known. Since the appearance of Simon's work, there have been many new records and lists of introduced spiders. The known Hawaiian spider fauna now totals 149 species and 4 subspecies belonging to 21 families and 66 genera. Of this total, 82 species (5596) are believed to be endemic and belong to 10 families and 27 genera including 7 endemic genera. The introduced spe cies total 65 (44^). Two unidentified species placed in indigenous genera comprise the remaining \%. Seventeen species are recorded here for the first time. In the catalog section of this paper, families, genera and species are listed alphabetical ly for convenience. -
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. -
Hawaii's , Kaho`Olawe Island Section 319 Success Story
Section 319 NONPOINT SOURCE PROGRAM SUCCESS STORY Restoring Native Vegetation Reduces SedimentHawaii Entering Coastal Waters Dry environmental conditions combined with a long history of human Waterbody Improved land use have resulted in severe erosion on Kaho`olawe. Much of the island has been reduced to barren hardpan, and sediment-laden runoff affects nearshore water quality and threatens the coral reef ecosystem. Efforts to minimize erosion and restore native vegetation in two watersheds on Kaho`olawe (Hakioawa and Kaulana) have reduced the amount of sediment entering the stream/gulch systems and coastal waters and have improved the quality of coastal waters, coral reef ecosystems and native wildlife habitat. Problem The island of Kaho`olawe, the smallest of the eight main Hawaiian Islands, is approximately 7 miles southwest of Maui. Kaho`olawe lies within the rain shadow of the volcanic summit of Maui. The island has a unique history. Evidence sug- gests that Hawaiians arrived as early as 1000 A.D. Kaho`olawe served as a navigational center for voyaging, an agricultural center, the site of an adze quarry, and a site for religious and cultural ceremo- nies. More recently, Kaho`olawe was used as a penal colony, a ranch (1858–1941), and a bombing range Figure 1. A lack of vegetation leads to excessive erosion by the U.S. Navy (1938–1990). The island was also on Kaho’olawe, which in turn home to as many as 50,000 goats during a 200-year causes sediment loading into period (1793–1993). Throughout the ranching period, adjacent marine waters. uncontrolled cattle and sheep grazing caused a substantial loss of soil through accelerated erosion. -
Numerical Model 39 4.2 Results of the Hawaiian Islands Response to Generalized Input Approaching from Alaska 41
NOAA-JTRE-167 .. ,. HIG-76-6 · A NUMERICAl STUDY OF .THE TSU.NAMI RESPONSE OF THE HAWAIIAN ISLANDS By EDDIE N. BERNARD MAY 1976 HAWAII INSTITUTE OF GEOPHYSICS UNIVERSITY OF HAWAII, HONOLULU and JOINT TSUNAMI RESEARCH EFFORT PACIFIC MARINE ENVIRONMENTAL LABORATORY ENVIRONMENTAL RESEARCH LABORATORY, NOAA HAWAII INSTITUTE OF GEOPHYSICS UNIVERSITY OF HAWAII NOAA-JTRE-167 HIG-76-6 A NUMERICAL STUDY OF THE TSUNAMI RESPONSE OF THE HAWAIIAN ISLANDS* By Eddie N. Bernard May 1976 Hawaii Institute of Geophysics University of Hawaii, Honolulu and Joint Tsunami Research Effort Pacific Marine Environmental Laboratory Environmental Research Laboratories. NOAA * A D I SS ERTATION SUBMITTE D TO THE GRADUATE DIVISION OF TEXA S A&M 11 NIV £RS ITY IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGR E E OF DOCTOR OF PHILOSOPHY IN OCEANOGRAPH~ AUGU S T 1 876 . ) u~:~~~~ Di recUr Di r<ector' Joint Tsunami Research Effort Hawaii Institute of Geophysics ABSTRACT The response of linearized long waves to the eight major Hawaiian Islands is investigated numerically using a mathematical model of the island system. A spline interpolation scheme ~s utilized to convert the actual soundings of the island bathymetry to a 5.5 km square grid closely approximating the topography of the islands. A time-marching, central difference, explicit scheme is used to evaluate the wave field by the linear, long wave, Eulerian equations of motion and continuity ~n Cartesian coordinates for a frictionless, homogeneous fluid. The condition of no normal flow is employed at the island shorelines and a localized interpolation technique is utilized at the outer boundary to simulate a free-flow boundary. -
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. -
KM Tours Hawaiian Paradise
KM Tours Presents Hawaiian Paradise February 1 - 11, 2019 From $4,495 per person from Hartford Featuring Maui, the Big Island of Hawaii, Kauai and Waikiki Tour Highlights • 11 Days, 13 Meals • 3 nights on Maui’s Kaanapali Beach • Tour the beautiful Iao Valley • 2 nights in Kona on the Big Island of Hawaii • Tour Volcano’s National Park • 2 nights on the Garden Isle of Kauai • Cruise the Wailua River and visit the Fern Grotto • Relax at our resort hotel on Coconut Beach • 2 nights in the heart of Honolulu • Honolulu City Tour • Tour Pearl Harbor and the USS Missouri • Famous Waikiki Beach • Traditional Hawaiian Luau • Full escorted from Hartford This is an exclusive travel program presented by InterTrav Corporation Fri., Feb. 1 – HARTFORD/MAUI We depart Hartford by motor coach to Chicago’s O’Hare International Airport for our transpacific flight traveling to Kahului, Maui. We are greeted by the warm trade winds and a traditional Hawaiian “lei” and “aloha”! A short drive remains to our resort on fabulous Ka’anapali Beach. This evening dinner is included at our hotel. (D) Sat., Feb. 2 – MAUI (Iao Valley) Maui’s rich cultural history and natural beauty come alive on our adventure to the Iao Valley State Park and Lahaina Town, where you will explore everything from lava formations to the island’s vibrant art scene. At Iao Valley State Park, which served as a burial ground for Hawaiian royalty, we see where King Kamehameha defeated Maui’s army to unite the Hawaiian Islands. The lush park is also home to the famous Iao Needle, a heavily eroded peak that rises sharply 2,500 feet above sea level to form a dramatic centerpiece in the valley. -
USGS Geologic Investigations Series I-2761, Molokai and Lanai
Molokai and Lanai Molokai and Lanai are the least populated and smallest of the main Hawaiian Islands. Both are relatively arid, except for the central mountains of each island and northeast corner of Molokai, so flooding are not as common hazards as on other islands. Lying in the center of the main Hawaiian Islands, Molokai and Lanai are largely sheltered from high annual north and northwest swell and much of south-central Molokai is further sheltered from south swell by Lanai. On the islands of Molokai and Lanai, seismicity is a concern due to their proximity to the Molokai 71 Seismic Zone and the active volcano on the Big Island. Storms and high waves associated with storms pose a threat to the low-lying coastal terraces of south Molokai and northeast Lanai. Molokai and Lanai Index to Technical Hazard Maps 72 Tsunamis tsunami is a series of great waves most commonly caused by violent Amovement of the sea floor. It is characterized by speed (up to 590 mph), long wave length (up to 120 mi), long period between successive crests (varying from 5 min to a few hours,generally 10 to 60 min),and low height in the open ocean. However, on the coast, a tsunami can flood inland 100’s of feet or more and cause much damage and loss of life.Their impact is governed by the magnitude of seafloor displacement related to faulting, landslides, and/or volcanism. Other important factors influenc- ing tsunami behavior are the distance over which they travel, the depth, topography, and morphology of the offshore region, and the aspect, slope, geology, and morphology of the shoreline they inundate. -
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.