Mauna Ulu Eruption Guide
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Lava Lake Eruptive Processes Quantified with Infrasound and Video at Mount Erebus, Antarctica
LAVA LAKE ERUPTIVE PROCESSES QUANTIFIED WITH INFRASOUND AND VIDEO AT MOUNT EREBUS, ANTARCTICA by Alexander Miller A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geophysics Boise State University August 2016 © 2016 Alexander Miller ALL RIGHTS RESERVED BOISE STATE UNIVERSITY GRADUATE COLLEGE DEFENSE COMMITTEE AND FINAL READING APPROVALS of the thesis submitted by Alexander Miller Thesis Title: Lava Lake Eruptive Processes Quantified with Infrasound and Video at Mount Erebus, Antarctica Date of Final Oral Examination: 04 March 2016 The following individuals read and discussed the thesis submitted by student Alexander Miller, and they evaluated the presentation and response to questions during the final oral examination. They found that the student passed the final oral examination. Jeffrey B. Johnson, Ph.D. Chair, Supervisory Committee Brittany Brand, Ph.D. Member, Supervisory Committee Paul Michaels, Ph.D. Member, Supervisory Committee The final reading approval of the thesis was granted by Jeffrey B. Johnson, Ph.D., Chair of the Supervisory Committee. The thesis was approved for the Graduate College by Jodi Chilson, M.F.A., Coordinator of Theses and Dissertations. The truth is out there. iv ACKNOWLEDGMENTS The author wishes to express gratitude to the Mount Erebus Volcano Observa- tory, efforts of Dr. Philip Kyle, Dr. Richard Aster, Dr. William McIntosh, Jake Anderson, Hugo Ortiz, and the McMurdo personnel. v ABSTRACT A natural laboratory exists at Mount Erebus where strombolian activity from the lava lake is directly observed from the crater rim. Lava lake eruptions occur when pressurized bubble slugs distend the lake surface before bursting within a few tenths of a second. -
Survey of Roadside Alien Plants in Hawai`I Volcanoes National Park and Adjacent Residential Areas 2001–2005
Technical Report HCSU-032 SURVEY OF ROADSIDE ALIEN PLANts IN HAWAI`I VOLCANOES NATIONAL PARK AND ADJACENT RESIDENTIAL AREAS 2001–2005 Linda W. Pratt1 Keali`i F. Bio2 James D. Jacobi1 1 U.S. Geological Survey, Pacific Island Ecosystems Research Center, Kilauea Field Station, P.O. Box 44, Hawaii National Park, HI 96718 2 Hawai‘i Cooperative Studies Unit, University of Hawai‘i at Hilo, P.O. Box 44, Hawai‘i National Park, HI 96718 Hawai‘i Cooperative Studies Unit University of Hawai‘i at Hilo 200 W. Kawili St. Hilo, HI 96720 (808) 933-0706 September 2012 This product was prepared under Cooperative Agreement CA03WRAG0036 for the Pacific Island Ecosystems Research Center of the U.S. Geological Survey. Technical Report HCSU-032 SURVEY OF ROADSIDE ALIEN PLANTS IN HAWAI`I VOLCANOES NATIONAL PARK AND ADJACENT RESIDENTIAL AREAS 2001–2005 1 2 1 LINDA W. PRATT , KEALI`I F. BIO , AND JAMES D. JACOBI 1 U.S. Geological Survey, Pacific Island Ecosystems Research Center, Kīlauea Field Station, P.O. Box 44, Hawai`i Volcanoes National Park, HI 96718 2 Hawaii Cooperative Studies Unit, University of Hawai`i at Hilo, Hilo, HI 96720 Hawai`i Cooperative Studies Unit University of Hawai`i at Hilo 200 W. Kawili St. Hilo, HI 96720 (808) 933-0706 September 2012 This article has been peer reviewed and approved for publication consistent with USGS Fundamental Science Practices ( http://pubs.usgs.gov/circ/1367/ ). Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. -
Volcanic Eruption Impacts Student Worksheet
Volcanic Eruption Impacts Student Worksheet Explosive and Effusive Volcanoes The type of volcanic eruption is largely determined by magma composition. Flux-mediated melting at subduction zones creates a felsic magma with high levels of carbon dioxide and water. These dissolved gases explode during eruption. Effusive volcanoes have a hotter, more mafic magma with lower levels of dissolved gas, allowing them to erupt more calmly (effusive eruption). Sinabung (Indonesia) Mount Sinabung is a stratovolcano located 40 km from the Lake Toba supervolcano in North Sumatra. It lies along the Sunda Arc, where the Indo-Australian plate subducts beneath the Sunda and Burma plates. After 1200 years of dormancy, Sinabung began erupting intermittently in 2010. Major eruptions have occurred regularly since November 2013. In November and December 2015, ash plumes reached 6 – 11 km in height on multiple occasions. Pyroclastic flows and ashfall blanketed the region in January 2014 and lava flows travelled down the south flank, advancing 2.5 km by April 2014. Pyroclastic flows in February 2014 killed 17 people in a town 3 km from the vent. In June 2015, ash falls affected areas 10 – 15 km from the summit on many occasions. A lahar in May 2016, caused fatalities in a village 20 km from Sinabung. Pyroclastic flows occurred frequently throughout 2016 and 2017 Eruption of Sinabung 6 October 2016 Major eruptions occurred in 2018 and 2019. In (Y Ginsu, public domain) February 2018, an eruption destroyed a lava dome of 1.6 million cubic metres. At least 10 pyroclastic flows extended up to 4.9 km and an ash plume rose more than 16 km in altitude. -
Hawaiian Volcanoes: from Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012
AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012 Conveners Michael Poland, USGS – Hawaiian Volcano Observatory, USA Paul Okubo, USGS – Hawaiian Volcano Observatory, USA Ken Hon, University of Hawai'i at Hilo, USA Program Committee Rebecca Carey, University of California, Berkeley, USA Simon Carn, Michigan Technological University, USA Valerie Cayol, Obs. de Physique du Globe de Clermont-Ferrand Helge Gonnermann, Rice University, USA Scott Rowland, SOEST, University of Hawai'i at M noa, USA Financial Support 2 AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Meeting At A Glance Sunday, 19 August 2012 1600h – 1700h Welcome Reception 1700h – 1800h Introduction and Highlights of Kilauea’s Recent Eruption Activity Monday, 20 August 2012 0830h – 0900h Welcome and Logistics 0900h – 0945h Introduction – Hawaiian Volcano Observatory: Its First 100 Years of Advancing Volcanism 0945h – 1215h Magma Origin and Ascent I 1030h – 1045h Coffee Break 1215h – 1330h Lunch on Your Own 1330h – 1430h Magma Origin and Ascent II 1430h – 1445h Coffee Break 1445h – 1600h Magma Origin and Ascent Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Origin and Ascent III 1645h – 1900h Poster Session Tuesday, 21 August 2012 0900h – 1215h Magma Storage and Island Evolution I 1215h – 1330h Lunch on Your Own 1330h – 1445h Magma Storage and Island Evolution II 1445h – 1600h Magma Storage and Island Evolution Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Storage -
Chapter 2 the Evolution of Seismic Monitoring Systems at the Hawaiian Volcano Observatory
Characteristics of Hawaiian Volcanoes Editors: Michael P. Poland, Taeko Jane Takahashi, and Claire M. Landowski U.S. Geological Survey Professional Paper 1801, 2014 Chapter 2 The Evolution of Seismic Monitoring Systems at the Hawaiian Volcano Observatory By Paul G. Okubo1, Jennifer S. Nakata1, and Robert Y. Koyanagi1 Abstract the Island of Hawai‘i. Over the past century, thousands of sci- entific reports and articles have been published in connection In the century since the Hawaiian Volcano Observatory with Hawaiian volcanism, and an extensive bibliography has (HVO) put its first seismographs into operation at the edge of accumulated, including numerous discussions of the history of Kīlauea Volcano’s summit caldera, seismic monitoring at HVO HVO and its seismic monitoring operations, as well as research (now administered by the U.S. Geological Survey [USGS]) has results. From among these references, we point to Klein and evolved considerably. The HVO seismic network extends across Koyanagi (1980), Apple (1987), Eaton (1996), and Klein and the entire Island of Hawai‘i and is complemented by stations Wright (2000) for details of the early growth of HVO’s seismic installed and operated by monitoring partners in both the USGS network. In particular, the work of Klein and Wright stands and the National Oceanic and Atmospheric Administration. The out because their compilation uses newspaper accounts and seismic data stream that is available to HVO for its monitoring other reports of the effects of historical earthquakes to extend of volcanic and seismic activity in Hawai‘i, therefore, is built Hawai‘i’s detailed seismic history to nearly a century before from hundreds of data channels from a diverse collection of instrumental monitoring began at HVO. -
Hawaii Volcanoes National Park Cycle 5 Report
Road Inventory and Condition Assessment Hawaii Volcanoes National Park HAVO Cycle 5 Report Prepared By: Federal Highway Administration Road Inventory Program (RIP) Data Collected: 04/2014 Report Date: 11/2014 Hawaii Volcanoes National Park in Hawaii HAWAIIKAUAI OAHU MOLOKAI LANAI HAWAIIMAUI HAWAII Hawaii Volcanoes National Park Sources: Esri, HERE, DeLorme, TomTom, Intermap, increment P Corp., GEBCO, USGS, FAO, NPS, NRCAN, GeoBase, IGN, Kadaster NL, Ordnance Survey, Esri Japan, METI, Esri China (Hong Kong), Sources: Esri, GEBCO, NOAA, National Geographic, DeLorme, HERE, Geonames.org, and other contributors DCV = Data Collection Vehicle TABLE OF CONTENTS SECTION PAGE 1 INTRODUCTION 1-1 2 PARK ROUTE INVENTORY Route ID, Subcomponent, and Changes Reports 2-1 3 PARK SUMMARY INFORMATION Paved Route Miles and Percentages by Functional Class and PCR 3-1 DCV Road Condition Summary 3-3 Parkwide DCV Condition Summary 3-7 4 PARK ROUTE LOCATION MAPS Route Location Key Map 4-1 Route Location Area Map 4-2 Route Condition Key Map – PCR Mile by Mile 4-9 Route Condition Area Map – PCR Mile by Mile 4-10 5 PAVED ROUTE CONDITION RATING SHEETS 5-1 6 MANUALLY RATED PAVED ROUTE CONDITION RATING SHEETS 6-1 6A: Condition Rating Sheets from April 2014 6-2 6B: Condition Rating Sheets from January 2012 6-21 7 PARKING AREA CONDITION RATING SHEETS 7-1 7A: Condition Rating Sheets from April 2014 7-2 7B: Condition Rating Sheets from January 2012 7-69 8 PARKWIDE / ROUTE MAINTENANCE FEATURES SUMMARIES Parkwide Maintenance Features Summary 8-1 Route Maintenance Features -
The Tragedy of Goma Most Spectacular Manifestation of This Process Is Africa’S Lori Dengler/For the Times-Standard Great Rift Valley
concentrate heat flowing from deeper parts of the earth like a thicK BlanKet. The heat eventually causes the plate to bulge and stretch. As the plate thins, fissures form allowing vents for hydrothermal and volcanic activity. The Not My Fault: The tragedy of Goma most spectacular manifestation of this process is Africa’s Lori Dengler/For the Times-Standard Great Rift Valley. Posted June 6, 2021 https://www.times-standard.com/2021/06/06/lori- In Africa, we are witnessing the Birth of a new plate dengler-the-tragedy-of-goma/ boundary. Extensional stresses from the thinning crust aren’t uniform. The result is a number of fissures and tears On May 22nd Mount Nyiragongo in the Democratic oriented roughly north south. The rifting began in the Afar RepuBlic of the Congo (DRC) erupted. Lava flowed towards region of northern Ethiopia around 30 million years ago the city of Goma, nine miles to the south. Goma, a city of and has slowly propagated to the south at a rate of a few 670,000 people, is located on the north shore of Lake Kivu inches per year and has now reached MozamBique. In the and adjacent to the Rwanda border. Not all of the details coming millennia, the rifts will continue to grow, eventually are completely clear, but the current damage tally is 32 splitting Ethiopia, Kenya, Tanzania and much of deaths, 1000 homes destroyed, and nearly 500,000 people Mozambique into a new small continent, much liKe how displaced. Madagascar Began to Be detached from the main African continent roughly 160 million years ago. -
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. -
Hawaiʻi Board on Geographic Names Correction of Diacritical Marks in Hawaiian Names Project - Hawaiʻi Island
Hawaiʻi Board on Geographic Names Correction of Diacritical Marks in Hawaiian Names Project - Hawaiʻi Island Status Key: 1 = Not Hawaiian; 2 = Not Reviewed; 3 = More Research Needed; 4 = HBGN Corrected; 5 = Already Correct in GNIS; 6 = Name Change Status Feat ID Feature Name Feature Class Corrected Name Source Notes USGS Quad Name 1 365008 1940 Cone Summit Mauna Loa 1 365009 1949 Cone Summit Mauna Loa 3 358404 Aa Falls Falls PNH: not listed Kukuihaele 5 358406 ʻAʻahuwela Summit ‘A‘ahuwela PNH Puaakala 3 358412 Aale Stream Stream PNH: not listed Piihonua 4 358413 Aamakao Civil ‘A‘amakāō PNH HBGN: associative Hawi 4 358414 Aamakao Gulch Valley ‘A‘amakāō Gulch PNH Hawi 5 358415 ʻĀʻāmanu Civil ‘Ā‘āmanu PNH Kukaiau 5 358416 ʻĀʻāmanu Gulch Valley ‘Ā‘āmanu Gulch PNH HBGN: associative Kukaiau PNH: Ahalanui, not listed, Laepao‘o; Oneloa, 3 358430 Ahalanui Laepaoo Oneloa Civil Maui Kapoho 4 358433 Ahinahena Summit ‘Āhinahina PNH Puuanahulu 5 1905282 ʻĀhinahina Point Cape ‘Āhinahina Point PNH Honaunau 3 365044 Ahiu Valley PNH: not listed; HBGN: ‘Āhiu in HD Kau Desert 3 358434 Ahoa Stream Stream PNH: not listed Papaaloa 3 365063 Ahole Heiau Locale PNH: Āhole, Maui Pahala 3 1905283 Ahole Heiau Locale PNH: Āhole, Maui Milolii PNH: not listed; HBGN: Āholehōlua if it is the 3 1905284 ʻĀhole Holua Locale slide, Āholeholua if not the slide Milolii 3 358436 Āhole Stream Stream PNH: Āhole, Maui Papaaloa 4 358438 Ahu Noa Summit Ahumoa PNH Hawi 4 358442 Ahualoa Civil Āhualoa PNH Honokaa 4 358443 Ahualoa Gulch Valley Āhualoa Gulch PNH HBGN: associative Honokaa -
' Hawaiian Volcanoes . During 1950
' Hawaiian Volcanoes . During 1950 GEOLOGICAL SURVEY BULLETIN 996-B A CONTRIBUTION TO GENERAL GEOLOGY HAWAIIAN VOLCANOES DURING 1950 By R. H. FINCH and GORDON A. MACDONALD ABSTRACT The activities of the Hawaiian Volcano Observatory during the calendar year 1950 are briefly described. Statistics on local and distant earthquakes recorded during the year, tilting of the ground surface, crack measurements, monthly rainfall statistics, and temperature measurements are presented and briefly dis cussed. Occurrences of warm water at several localities on the rift zones of Kilauea volcano are described. The warm water apparently results from heating of ground water by either contact with hot intrusive rock or rising hot gases. An eruption of Mauna Loa began on the evening of June 1, and continued until June 23. Fissures opened along the southwest rift zone of Mauna Loa for a distance of more than 12 miles. At 9:04 p. in. a fissure 1.5 miles long opened between 11,000 and 12,000 feet altitude. Floods of very liquid lava poured out, and a cloud of fume rose two .miles in the air, brightly illuminated by the red glare of the liquid lava beneath. This activity lasted only about four hours. At 10:15 p. in. a new series of fissures started to open lower on the rift, .between 8,500 and 10,500 feet altitude. Activity along the upper portion of the lower group of fissures lasted about a week, but the*lower portion remained active for more than three weeks. A total of seven large lava flows poured out, both south eastward and westward. -
Features of Lava Lake Filling and Draining and Their Implications for Eruption Dynamics
Bull Volcanol (2009) 71:767–780 DOI 10.1007/s00445-009-0263-0 RESEARCH ARTICLE Features of lava lake filling and draining and their implications for eruption dynamics W. K. Stovall & Bruce F. Houghton & Andrew J. L. Harris & Donald A. Swanson Received: 13 March 2008 /Accepted: 7 January 2009 /Published online: 13 February 2009 # Springer-Verlag 2009 Abstract Lava lakes experience filling, circulation, and roughly horizontal lava shelves on the lakeward edge of the often drainage depending upon the style of activity and vertical rinds; the shelves correlate with stable, staggered lake location of the vent. Features formed by these processes stands. Shelves either formed as broken relict slabs of lake have proved difficult to document due to dangerous crust that solidified in contact with the wall or by accumula- conditions during the eruption, inaccessibility, and destruction tion, accretion, and widening at the lake surface in a dynamic of features during lake drainage. Kīlauea Iki lava lake, lateral flow regime. Thin, upper lava shelves reflect an Kīlauea, Hawai‘i, preserves many such features, because lava initially dynamic environment, in which rapid lake lowering ponded in a pre-existing crater adjacent to the vent and was replaced by slower and more staggered drainage with the eventually filled to the level of, and interacted with, the vent formation of thicker, more laterally continuous shelves. At all and lava fountains. During repeated episodes, a cyclic pattern lava lakes experiencing stages of filling and draining these of lake filling to above vent level, followed by draining back processes may occur and result in the formation of similar sets to vent level, preserved features associated with both filling of features. -
Explore Crater Rim Drive and Chain of Craters Road VISITOR ALERT High Amounts of Dangerous Sulfur Dioxide Gas Are Present at the Volcano”S Summit
National Park Service Hawai‘i Volcanoes National Park U.S. Department of the Interior Explore Crater Rim Drive and Chain of Craters Road VISITOR ALERT High amounts of dangerous sulfur dioxide gas are present at the volcano”s summit. Personal Safety When driving along Crater Rim Drive, keep your windows closed when visible. Volcanic gas conditions (visually similar to smog) exist along Chain of Craters Road— keep your windows closed when visible. If the air irritates, smells bad, or you have difficulty breathing, return to your vehicle and leave the area. If open, the Kīlauea Visitor Center is a clean air environment. Please be flexible in your travel plans. Some areas may be closed for your safety. Points of Interest Automated Cell Phone Tour 0 Dial 1-808-217-9285 to learn more about the numbered stops listed below. Kīpukapuaulu Nāmakanipaio For emergencies call Mauna Loa Road (13.5-miles one way) Kīlauea Military Camp Campground 808-985-6170 or 911 11 9 Steam Vents 1 To Kailua- Sulphur Banks 4 Kona Crater Rim Drive Jaggar Kīlauea Overlook Museum and Picnic Area Kïlauea Visitor Center 0 Volcano Village 2 7 Volcano House (Gas and Food) closed for renovations Park Entrance 11 KĪLAUEA CALDERA To Hilo 6 Halema‘uma‘u Kīlauea Iki Crater Crater Overlook Thurston Lava Tube (Nāhuku) 3 Road Closed Pu‘u Pua‘i Due to high amounts of sulphur dioxide gas. Pit Devastation Trail 5 Craters Hilina Pali Road (9 miles / 14.5 km one-way) Pu‘u Huluhulu Cinder Cone Hilina Pali Mauna Ulu Shield Overlook Kulanaokuaiki Mau Loa o Campground Mauna Ulu Pu‘u