KM Tours Hawaiian Paradise
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Hawaii Been Researched for You Rect Violation of Copyright Already and Collected Into Laws
COPYRIGHT 2003/2ND EDITON 2012 H A W A I I I N C Historically Speaking Patch Program ABOUT THIS ‘HISTORICALLY SPEAKING’ MANUAL PATCHWORK DESIGNS, This manual was created Included are maps, crafts, please feel free to contact TABLE OF CONTENTS to assist you or your group games, stories, recipes, Patchwork Designs, Inc. us- in completing the ‘The Ha- coloring sheets, songs, ing any of the methods listed Requirements and 2-6 waii Patch Program.’ language sheets, and other below. Answers educational information. Manuals are books written These materials can be Festivals and Holidays 7-10 to specifically meet each reproduced and distributed 11-16 requirement in a country’s Games to the individuals complet- patch program and help ing the program. Crafts 17-23 individuals earn the associ- Recipes 24-27 ated patch. Any other use of these pro- grams and the materials Create a Book about 28-43 All of the information has contained in them is in di- Hawaii been researched for you rect violation of copyright already and collected into laws. Resources 44 one place. Order Form and Ship- 45-46 If you have any questions, ping Chart Written By: Cheryle Oandasan Copyright 2003/2012 ORDERING AND CONTACT INFORMATION SPECIAL POINTS OF INTEREST: After completing the ‘The Patchwork Designs, Inc. Using these same card types, • Celebrate Festivals Hawaii Patch Program’, 8421 Churchside Drive you may also fax your order to Gainesville, VA 20155 (703) 743-9942. • Color maps and play you may order the patch games through Patchwork De- Online Store signs, Incorporated. You • Create an African Credit Card Customers may also order beaded necklace. -
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 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. -
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. -
Rolling Stones: Haleakalā National Park Rocks!
Geology Unit Haleakalā National Park Rolling Stones: Haleakalā National Park Rocks! Next Generation Science Standards: 4-ESS1-1 Identify evidence from patterns in rock formations and fossils in rock layers to support an explanation for changes in a landscape over time. 4-ESS2-1 Make observations and/or measurements to provide evidence of the effects of weathering or the rate of erosion by water, ice, wind, or vegetation. 4-ESS2-2 Analyze and interpret data from maps to describe patterns of Earth’s features. 5-ESS2-1 Develop a model using an example to describe ways the geosphere, biosphere, hydrosphere, and/or atmosphere interact. Hawaiʻi Content and Performance Standards III: SC.4.8.1 Describe how slow processes sometimes shape and reshape the surface of the Earth. SC.5.2.1 Use models and/or simulations to represent and investigate features of objects, events, and processes in the real world. Description: This lesson explores the forces of weathering and erosion that shape our island home. It recounts volcanic creation, and then delves into the gradual destruction caused by the forces of wind, water, ice and waves. Duration: 60 minutes Objectives: At the end of this lesson, the students will be able to: Describe the impacts of deposition, weathering, and erosion on landforms. Background: The Earth is undergoing continuous change by weathering and erosion. As rocks are weathered (broken down into smaller pieces) and eroded (moved to new locations) the landscape is gradually transformed. The Hawaiian Islands are on a journey as they travel along toward the northwest on the pacific plate. -
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 Entomology Branch of the Hawaii Department of Agriculture Has Maintained a Continuous Program of Beneficial Organism Introductions for Many Years
Vol. XXII, No. 1, August, 1975 109 Introductions for Biological Control in Hawaii, 1973 H. K. Nakao, G. Y. Funasaki and C. J. Davis STATE DEPARTMENT OF AGRICULTURE HONOLULU, HAWAII The Entomology Branch of the Hawaii Department of Agriculture has maintained a continuous program of beneficial organism introductions for many years. This paper includes a list of beneficial insects introduced for biological control during 1973, and gives notes on the status of some pests and their purposely introduced enemies. Snail Pest Control Achatina fulica Bowdich (giant African snail). Giant African snail populations remained at low levels in former high density localities on Oahu and Maui. Efforts to eradicate or contain the snail continued on the islands of Kauai and Hawaii. On Kauai, metal- dehyde bait applications were made throughout the year in localized infestations at Poipu and Wahiawa. On Hawaii, a shipment of Gonaxis quadrilateralis (Preston) from Oahu was released along the perimeter of the snail infestation in Kahaluu (Kona) in January, and an aerial bait application was made covering 65 to 70 acres, in August. Galba viridis (Quoy & Gaimard) (liverfluke snail). No recoveries have been made of Sepedon plumbella Wiedemann, S. senex Wiedemann and S. n. sp., sciomyzids introduced from Southeast Asia in 1971 to aid in the control of Galba viridis, the intermediate host of cattle liverfluke. Populations of G. viridis, however, were reported at low levels on Oahu, Maui and Hawaii and this may, in part, be attributed to the predation of Sepedon sauteri Hendel and S. macropus Walker. Weed Pest Control Lantana camara var. aculeata L. -
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. -
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. -
Hawaii National Park
UNITED STATES DEPARTMENT OF THE INTERIOR HUBERT WORK, SECRETARY NATIONAL PARK SERVICE STEPHEN T. MATHER, DIRECTOR RULES AND REGULATIONS HAWAII NATIONAL PARK Photo © Tal Sing Loo GREAT SMOKING PIT OF KILAUEA VOLCANO AS IT APPEARS AT THE PRESENT TIME OPEN ALL THE YEAR U. S. GOVERNMENT PRINTING OFFICE : 1827 Photo © Tai Sinj; Loo DUST CLOUD, KILAUEA VOLCANO, DURING 1924 ACTIVITY Photograph by Baker THE "DEVIL'S THROAT," A VOLCANIC CHASM ON THE COCKETT TRAIL C O 1\T T E 1\T T S Page General description 1 Luxuriant tropical foliage 1 Kilauoa section 1 Common trees and shrubs 2 Bird Park 4 Volcano Observatory and Museum 4 Roads and trails 5 Mauna I.oa section 5 Kilauea-Mauna Loa trip 8 Ilaleakala section G Rase silversword plant T Summit rest house 7 Administration 7 Accommodations for visitors 7 Volcano House 7 Army and Navy recreation camps 10 Free public automobile camp 10 How to reach the park 10 A tropical gateway 10 Overnight voyage to the park 10 Transportation 11 Trip to Haleakala section 11 General information 11 Outdoor life in Hawaiian Islands 12 Rules and regulations 13 Literature 16 Authorized rates for public utilities, season of 1027 17 ILLUSTRATIONS COVER Great smoking pit of Kilauea Volcano as it appears at the present time Front. Dust cloud, Kilauea Volcano, during 1021 activity Inside front. The "Devil's Throat." a volcanic chasm on Cockett Trail Inside front. Fern Tree Drive to Kilauea Volcano Inside hack. The great crater of Ilaleakala Inside hack. City of Hilo and snow-capped Mauna Kea Back.