Some Lava Show Caves of Hawaii & Iceland
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Pu'u Wa'awa'a Management Plan
Management Plan for the Ahupua‘a of Pu‘u Wa‘awa‘a and the Makai Lands of Pu‘u Anahulu July 15, 2003 State of Hawaii Department of Land and Natural Resources Division of Forestry and Wildlife Division of State Parks Acknowledgements In June 2002, the Pu‘u Wa‘awa‘a Advisory Council (PAC) was formed to function in a consultative capacity with Department of Land and Natural Resources (DLNR) staff involved in planning efforts for Pu‘u Wa‘awa‘a. The PAC is comprised of the following community members, who represent a wide range of expertise and interests in the various components and actions proposed in this plan: Corky Bryan Mick Castillo Dick Hoeflinger Ku‘ulei Keakealani Kepa Maly Bob Okawa Rob Pacheco Jon Sabati Michael Tomich Peter Vitousek Through a series of meetings, the PAC has reviewed several drafts of the plan and provided considerable feedback and input to DLNR staff. Many of the PAC’s suggestions have been incorporated or are now represented in this plan. The dedication, candor, and cooperation displayed by the PAC is graciously acknowledged by the DLNR. Components of this Plan relating to trails, access, ecotourism, cultural considerations, archeological resources and environmental education include modified text originally presented in a proposal by Ka ‘Ahahui o Pu‘u Wa‘awa‘a, or the “Hui”. The DLNR Management Team wishes to acknowledge and thank the Hui for permission to use these materials. Editorial Note The management objectives proposed in this management plan are not presented in a prioritized or sequential format. They are grouped by category. -
Hawaii Volcanoes National Park Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 THIS PAGE: Geologists have lloongng been monimonittoorriing the volcanoes of Hawai‘i Volcanoes National Park. Here lalava cascades durduriingng the 1969-1971 Mauna Ulu eruption of Kīlauea VolVolcano. NotNotee the Mauna Ulu fountountaiain in the background. U.S. Geologiogicalcal SurSurvveyey PhotPhotoo by J. B. Judd (12/30/1969). ON THE COVER: ContContiinuouslnuouslyy eruptuptiingng since 1983, Kīllaueaauea Volcano contcontiinues to shapshapee Hawai‘Hawai‘i VoVollccanoes NatiNationalonal ParkPark.. Photo courtesy Lisa Venture/UniversiUniversitty of Cincinnati. Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 December 2009 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
The Cavernicolous Fauna of Hawaiian Lava Tubes, 1
Pacific Insects 15 (1): 139-151 20 May 1973 THE CAVERNICOLOUS FAUNA OF HAWAIIAN LAVA TUBES, 1. INTRODUCTION By Francis G. Howarth2 Abstract: The Hawaiian Islands offer great potential for evolutionary research. The discovery of specialized cavernicoles among the adaptively radiating fauna adds to that potential. About 50 lava tubes and a few other types of caves on 4 islands have been investigated. Tree roots, both living and dead, are the main energy source in the caves. Some organic material percolates into the cave through cracks associated with the roots. Cave slimes and accidentals also supply some nutrients. Lava tubes form almost exclusively in pahoehoe basalt, usually by the crusting over of lava rivers. However, the formation can be quite complex. Young basalt has numerous avenues such as vesicles, fissures, layers, and smaller tubes which allow some intercave and interlava flow dispersal of cavernicoles. In older flows these avenues are plugged by siltation or blocked or cut by erosion. The Hawaiian Islands are a string of oceanic volcanic islands stretching more than 2500 km across the mid-Pacific. The western islands are old eroded mountains which are now raised coral reefs and shoals. The eight main eastern islands total 16,667 km2 and are relatively young in geologic age. Ages range from 5+ million years for the island of Kauai to 1 million years for the largest island, Hawaii (Macdonald & Abbott, 1970). The native fauna and flora are composed of those groups which dis persed across upwards of 4000 km of open ocean or island hopped and became successfully established. -
Ecological Studies on Hawaiian Lava Tubes
Technical Report No. 16 ECOLOGICAL STUDIES ON HAWAIIAN LAVA TUBES Francis G. Howarth Department of Entooology Bernice P. Bishop Museum Honolulu, Hawaii ISLAND ECOSYSTEMS IRP U. S. International Biological Program Decemb~r 1972 ABSTRACT The Hawaiian Islands offer great potential for evolutionary research. The discovery of specialized cavernicoles among the adaptively radiating fauna adds to that potential. About 50 lava tubes and a few other types of caves on 4 islands have been investigated. Tree roots, both living and dead, are the main energy source in the caves. Some organic material percolates into the cave through cracks associated with the roots. Cave slimes and accidentals also supply some nutrients. Lava tubes form almost exclusively in pahoehoe basalt, usually by the crusting over of lava rivers. However, the formation can be quite complex. Young basalt has numerous avenues such as vesicles, fissures, layers, and smaller tubes which allow some intercave and interlava flow dispersal of cavernicoles. In older flows these avenues are plugged by siltation or blocked or cut by erosion. -~- 2 TABLE 1. Caves Investit~ted in this Survey. Lava Tubes on Hawaii (J.:auna Loa rassif) No. Name of Cave Locality Elevation Len[th Dark Zone1 (approx.) 1. i<aurnana Cave Kaumana 290 m 1500 m + 2. Bird Park Cave #1 Hawaii Volcanoes National Park 1250 m 100 m + 3. Bird Park Cave #2 Hawaii Volcanoes National Park 1250 m 20 m 0 4. Bird Park Cave #3+4 Hawaii Volcanoes National Park 1250 m 400 m + 5. Bird Park Cave #5 Hawaii Vol canoe:!! National Park 1250 m 20 m? 0 6. -
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. -
America's Natural Nuclear Bunkers
America’s Natural Nuclear Bunkers 1 America’s Natural Nuclear Bunkers Table of Contents Introduction ......................................................................................................... 10 Alabama .............................................................................................................. 12 Alabama Caves .................................................................................................. 13 Alabama Mines ................................................................................................. 16 Alabama Tunnels .............................................................................................. 16 Alaska ................................................................................................................. 18 Alaska Caves ..................................................................................................... 19 Alaska Mines ............................................................................................... 19 Arizona ............................................................................................................... 24 Arizona Caves ................................................................................................... 25 Arizona Mines ................................................................................................... 26 Arkansas ............................................................................................................ 28 Arkansas Caves ................................................................................................ -
Cave Science News
CAV E SCIENCE NEWS CAVE SCIENCE NEWS KARST MEETING PLANNED AT MAMMOTH CAVE Kempe, S. (1996) Enlargement of lava tubes by downcutting and breakdown. Abstracts and Proceedings of the National A joint meeting of the International Geological Correlation Speleological Society Convention 58(3): 203. Program, Project 379: “Karst Processes and the Global Kempe, S. (1996). Neue Rekorde in Lavahohlen auf Hawaii, Carbon Cycle” along with Friends of Karst will take place on ein Statusbericht. Mitt. Arge f. Karstkunde Harz e.V. September 23, 24, and 25, 1998, at Mammoth Cave, Kentucky, 1996(3): 46-49 und (mit gleichem Text) Lavahohlen auf USA. The meeting will be hosted by the Center for Cave and Hawaii ein Statusbericht. Mitt.Verb. Dt. Hohlen- u. Karst Studies at Western Kentucky University, Mammoth Cave Karstforscher 42 (2): 27-29. (German) National Park, and the Cave Research Foundation. Kempe, S. (in press). Lava Falls: a major factor for the Preliminary plans are to have two days of scientific pre- enlargement of lava tube of the Ai-laau shield phase, sentations on various aspects of karst science, with particular Kilauea, Hawaii. Proceedings of the 10th International sessions so far anticipated on progress in understanding the Congress of Speleology. Switzerland. impact of karst processes on carbon cycling at a variety of Kempe, S., Buchas, H., Hartmann, J., Oberwinder, M., scales, and on recent work in the Central Kentucky Karst. A Strassenburg, J. & Wolniewicz, K. (in press). Mapping third day will be planned for a variety of surface and subsur- lava flows by following their tubes: The Keauhou face field trips in and around the Mammoth Cave System, Trail/Ainahou Ranch Flow Field, Kilauea, Hawaii. -
NEWSLETTERS NUMBER 01 to 06 (5.7
REDUCED-SIZE PHOTOCOPIES of: Newsletter # 1 .... 6 _,_--~~ ... ... "" "- ~ ,___,. ..\ ..' . 4 .. ~ COMMISSION on VOLCANIC CAVES . COMM I SSION ON VOLCANIC CAVES International Union of Speleology Newsletter #l December 22, 199~ STATUS OF IUS WORKING GROUP ON VOLCANIC CAVES RAISED TO COMMISSION The Working Group on Volcanic Caves of the International Union of Speleology h as been elevated to full Comm ission s tatus. By letter of 13 December 1993, new IUS President Paulo Forti confirmed that the IUS Bureau took the necessary action during the international congress of speleology in Beijing earlier this year. The membership of t he new commission is the same as the membership of the old working group, with one notable recent appointment, a nnounce d on this page. Names and addresses of t h e members a r e elsewhere in this issue. Because of t he change in name and status , this is Newsletter #1 of t he new commission, rather t han Newsletter #6 . Th e next issue is expected to be in Spring, 1994. Items for publication in it should be sent to the chairman at h is Hawaii address before March 1. DR. YURII B. SLEZ IN APPOINTED TO COMMISSION Yuri i B. Slezin h as accepted sppointment to t he commission. He has studied l ava flows in tubes of the 1975-1976 Tolbachic eruption on Kamchatka and the structure of a similar o l d lava field nea rby. In this lava field he mapped a cave which is a fragment of a great lava tube system. Other fragments of the system, inc l uding caves about 100-150 meters long, are present, and other tube systems in a dditidn~ This is the only known published map of a lava t ube cave i n Russia. -
Meteorological Comparison of Three Cave Systems
Western Kentucky University TopSCHOLAR® Honors College Capstone Experience/Thesis Projects Honors College at WKU 2019 Meteorological Comparison of Three Cave Systems Matthew Wine Western Kentucky University, [email protected] Follow this and additional works at: https://digitalcommons.wku.edu/stu_hon_theses Part of the Geology Commons, and the Meteorology Commons Recommended Citation Wine, Matthew, "Meteorological Comparison of Three Cave Systems" (2019). Honors College Capstone Experience/Thesis Projects. Paper 835. https://digitalcommons.wku.edu/stu_hon_theses/835 This Thesis is brought to you for free and open access by TopSCHOLAR®. It has been accepted for inclusion in Honors College Capstone Experience/Thesis Projects by an authorized administrator of TopSCHOLAR®. For more information, please contact [email protected]. METEOROLOGICAL COMPARISON OF THREE CAVE SYSTEMS A Capstone Experience/Thesis Project Presented in Partial Fulfillment of the Requirements of the Degree Bachelor of Science with Honors College Graduate Distinction at Western Kentucky University By: Matthew Wine ***** Western Kentucky University 2019 CE/T Committee: Approved by: Dr. Patricia Kambesis, Advisor Dr. Greg Goodrich __________________________________ Dr. Dennis Wilson Advisor Department of Geography & Geology Copyright by: Matthew Wine 2019 ABSTRACT Cave systems are home to delicate underground ecosystems that can be affected by changes in surface atmospheric conditions which in turn affect underground meteorology. Modern human use of caves is typically for tourism, so understanding surface-underground weather-climate interactions is important when caves carry streams that are prone to flooding in response to surface precipitation. The purpose of this research is to document the effects of surface weather conditions on cave meteorology in three different cave system types located in different geographic locations including an island, the central USA, and at high elevations in British Columbia. -
The Cavernicolous Fauna of Hawaiian Lava Tubes, Part Vi
Technical Report No. 40 THE CAVERNICOLOUS FAUNA OF HAWAIIAN LAVA TUBES, PART VI. MESOVELIIDAE OR WATER TREADERS (HETEROPTERA) , Wayne c. Gagne and Francis G. Howarth Department of Entomology Bernice P. Bishop Museum Honolulu, Hawaii 96818 ISLAND ECOSYSTEMS IRP U. s. International Biological Program May• 1974 ABSTRACT This paper is a systematic report and a biological analysis of the Mesoveliidae from Hawaiian caves. Most important is a new species of Speovelia Esaki, ~. sp. (Hawaii I.), described from material collected on moist walls in lava tubes. This apparently represents the world's first troglobitic heteropteran. Morphologically, all instars show lack of pigmentation, functionless eyes and prolongation of the appendages and head. Biologically, it is restricted to the dark zone of lava tubes. Notes on its biology are given. It also represents the first known endemic species of the family for the Hawaiian Islands. Another species, Mesovelia amoena Uhler, is troglophilic. This is the first record of this immigrant American species in the Hawaiian Islands. The remaining species in Hawaii, the immigrant'M· mulsanti White, has only been found in epigean situations. A key to the species is also presented. - i - TABLE OF CONTENTS Page ABSTRACT i INTRODUCTION 1 KEY TO HAWAIIAN MESOVELIIDAE 2 S PEOVELIA SP. 3 Taxonomic description 3 Distribution 5 Etymology and Remarks 6 Biology 7 Habitat 7 Food web 9 Associated biota 9 Distribution within caves 10 Population 10 Behavior 11 Food habits • 11 Comparative feeding and reproductive habits 12 SPEOVELIA MARITIMA ESAKI 13 MESOVELIA AMOENA UHLER 13 Taxonomic description • 13 Material examined 15 Remarks 15 MESOVELIA MULSANTI WHITE • 16 MESOVELIA SP. -
Towards Understanding the Structure of Kaumana Cave, Hawaii
TOWARDS UNDERSTANDING THE STRUCTURE OF KAUMANA CAVE, HAWAII Stephan Kempe Inst. Applied Geosciences, Techn. Univ. Darmstadt and Hawaii Speleological Survey Schnittspahnstr. 9 Darmstadt, D-64827, Germany, [email protected] Christhild Ketz-Kempe Am Schloss Stockau 2 Dieburg, D64807, Germany, [email protected] Abstract its lower entrance at Edita Street, with bolt-marks documenting the stations. W.R. Halliday published Kaumana Cave is one of the youngest lava caves on 2003 another map, showing some of the salient cave Hawaii, formed during a few weeks at the end of the features. The cave is listed with a length of 2197 m 1880/81 Mauna Loa eruption that stopped short of according to W.R. Halliday with no vertical data given downtown Hilo. We surveyed a small section of the (Gulden, 2015). This figure represents, however, not cave above and below the Kaumana County Park the entire length of the cave. A further survey entrance in order to document the stratigraphy and conducted by D. Coons and P. Kambysis, has not yet development stages of the cave. Results show that the been published. So far, no longitudinal profile, nor roof is composed of a >10 m thick sequence of lavas cross-sections nor any detailed geological information layers, with a >3 m thick primary roof formed by five were published. to six inflationary lava sheets. The initial pyroduct had a cross-section of about 3 m2. After the placement of Kaumana Cave is part of the pyroduct that was the roof a cave developed upward by collapse of wall responsible for the advance of the 1880/1881 Mauna and roof sections. -
Journal of Cave and Karst Studies Editor Louise D
December 1998 JOURNAL OF Volume 60 Number 3 ISSN 1090-6924 CAVE AND KARST STUDIES Journal of Cave and Karst Studies Editor Louise D. Hose Volume 60 Number 3 December 1998 Environmental Studies Program Westminster College CONTENTS Fulton, MO 65251-1299 (573) 573-5303 Voice (573) 592-2217 FAX Articles [email protected] Tubular Lava Stalactites and Other Related Segregations Production Editor Kevin Allred and Carlene Allred 131 James A. Pisarowicz Wind Cave National Park Hot Springs, SD 57747 History and Status of the Moiliili Karst, Hawaii (605) 673-5582 William R. Halliday 141 [email protected] Gypsum Speleothems of Freezing Origin BOARD OF EDITORS Victor V. Korshunov and Elena V. Shavrina 146 Earth Sciences-Journal Index Ira D. Sasowsky Geochemistry of Fluorite and Related Features of the Department of Geology University of Akron Kugitangtou Ridge Caves, Turkmenistan Akron, OH 44325-4101 Vladimar Maltsev and Viktor Korshunov 151 (330) 972-5389 [email protected] The Cave-inhabiting Beetles of Cuba (Insecta: Coleoptera): Diversity, Distribution and Ecology Conservation Stewart B. Peck, Amador E. Ruiz-Baliú and George Huppert Department of Geography Gabriel F. Garcés González 156 University of Wisconsin, LaCrosse LaCrosse, WI 54601 Spatial and Temporal Variations in the Dissolved Organic [email protected] Carbon Concentrations in the Vadose Karst Waters of Marengo Cave, Indiana Life Sciences Veronica A. Toth 167 David Ashley Department of Biology Missouri Western State College The Current Status and Habitats of the Illinois Cave St. Joseph, MO 64507 Amphipod, Gammarus acherondytes Hubricht and (816) 271-4334 Mackin (Crustacea: Amphipoda) [email protected] D.W.