Blue-Sky Eruptions, Do They Exist? Implications for Monitoring New

Total Page:16

File Type:pdf, Size:1020Kb

Blue-Sky Eruptions, Do They Exist? Implications for Monitoring New Blue‐sky eruptions, do they exist? Implications for monitoring New Zealand’s volcanoes. A thesis submitted in partial fulfilment of the requirements for the Degree of Master of Science in Disaster and Hazard Management at the University of Canterbury by Angela Louise Doherty University of Canterbury 2009 Frontispiece “What are the odds, right?” “Before it happened it would have said slim, but since it did happen I would say 100%...” Dr Ray Langston replying to Catherine Willows (played by Lawrence Fishburne and Marg Helgenberger – CSI: Crime Scene Investigation). Lahar following the September 2007 eruption of Ruapehu (photo: GNS Science). Abstract The term “blue‐sky eruption” (BSE) can be used to describe eruptions which are unexpected or have no detected precursory activity. Case study analyses indicate that they have a diverse range of characteristics and magnitudes, providing both direct and indirect hazards and occur in both under‐developed and developed countries. BSEs can be a result of physical triggers (e.g. the lack of physically detectable precursors or a lack of understanding of the eruption model of the volcano), social triggers (such as an inadequate monitoring network), or a combination of the two. As the science of eruption forecasting is still relatively young, and the variations between individual volcanoes and individual eruptions are so great, there is no effective general model and none should be applied in the absence of a site‐specific model. Similarly, as methods vary between monitoring agencies, there are no monitoring benchmarks for effective BSE forecasting. However a combination of seismic and gas emission monitoring may be the most effective. The United States began a hazard and monitoring review of their volcanoes in 2005. While the general principles of their review would be beneficial in a monitoring review of New Zealand’s volcanoes, differences in styles of volcanism, geographic setting and activity levels mean changes would need to be review to fully appreciate the risk posed by New Zealand’s volcanoes. Similarly, the monitoring benchmarks provided in the U.S. review may not be fully applicable in New Zealand. While advances in technology may ultimately allow the effective forecasting of some BSEs, the immediate threat posed by unexpected eruptions means that effective management and mitigation measures may be the only tools currently at our disposal to reduce the risks from BSEs. Acknowledgements It takes a village to raise a baby, and apparently, to complete a Master’s thesis. Firstly I would like to acknowledge all the support and guidance I received from my super‐visory team, Tim Davies, Jim Cole and Gill Jolly. You were a dream team and I thank you for helping steer me in the right direction and not laughing too much at my penchant for 5 line sentences. I’d also like to sincerely thank the crew at GNS Science in Wairakei for their assistance and advice, especially Brad Scott and Craig Miller. Thank you my friends and ex‐colleagues at the Hawaii Volcano Observatory, especially Kelly, Jeff and Jim for the email research and to Florian Schwandner for your insights into the principles of volcano monitoring. I’d also like to thank William Pike for taking the time to give me a phone interview which gave a valuable insight into the 2007 eruption of Ruapehu and made the dangers of this style of eruption tangible. Thanks go to the Mason Trust for their financial support and to the entire UoC Geology Department for their expertise and assistance. To my fellow students, especially Elke, Hanna and Danni, thank you for your positivity, support and listening to my occasional rants. Thank you to those who read over things, gave advice, support and made me laugh (there are so many of you but especially Cooksey and the Facebook editorial squad). And finally, thank you my parents, Terry and Heather. Thank you for always believing in me and knowing it was worth a second shot. I could not have done this without you. ‐ v ‐ Table of Contents Frontispiece ........................................................................................................................... ii Abstract ................................................................................................................................ iii Acknowledgements .............................................................................................................. iv Table of Contents .................................................................................................................. v List of Figures.......................................................................................................................viii List of Tables ......................................................................................................................... ix Abbreviations......................................................................................................................... x Chapter 1. Introduction..................................................................................................... 1 1.1 Blue‐Sky Eruptions .................................................................................................. 2 1.2 Issues Surrounding Blue‐Sky Eruptions .................................................................. 2 1.3 The Importance of Blue‐Sky and Retrospectively‐Explained Eruptions ................. 3 1.4 Thesis Outline ......................................................................................................... 5 Chapter 2. Blue‐Sky Eruptions and Events ........................................................................ 7 2.1 Definition ................................................................................................................ 7 2.1.1 Blue‐Sky Eruption ............................................................................................ 7 2.1.2 Blue‐Sky Events................................................................................................ 8 2.2 The New Zealand Volcanic Alert Level system ....................................................... 9 2.3 Worldwide Alert Level Systems ............................................................................ 11 2.3.1 United States Geological Survey (USGS), U.S.A............................................. 11 2.3.2 Montserrat Volcano Observatory (MVO), Montserrat, West Indies ............ 13 2.4 Eruption Styles ...................................................................................................... 15 2.4.1 Magmatic Eruptions ...................................................................................... 15 2.4.2 Phreatic and Hydrothermal Eruptions........................................................... 19 2.5 Volcanic Hazards................................................................................................... 19 2.5.1 Lava Flows...................................................................................................... 20 2.5.2 Air‐fall Tephra................................................................................................ 23 2.5.3 Pyroclastic Flows, Surges and Block and Ash Flows ...................................... 25 2.5.4 Lahars and Mudflows .................................................................................... 27 2.5.5 Explosions and Directed (Lateral) Blasts ....................................................... 29 2.5.6 Volcanic Gases and Limnic Eruptions ............................................................ 30 Chapter 3. Blue‐Sky Eruptions and Blue‐Sky Events: Case Studies ................................ 33 3.1 Blue‐Sky Eruptions – Magmatic ............................................................................ 33 3.1.1 Okmok Volcano, Alaska U.S.A – 12 July 2008................................................ 33 3.1.2 Raoul Island, Kermadec Arc – 17 March 2006............................................... 35 3.1.3 Nyiragongo Volcano, Democratic Republic of Congo – 1997 & 2002........... 38 3.1.4 Galeras Volcano, Columbia – 14 January 1993 ............................................. 43 3.1.5 El Chichón Volcano, Mexico – March to April 1982 ...................................... 46 3.1.6 Historic Magmatic Blue‐Sky Eruptions: Tarawera, New Zealand – 1886...... 51 ‐ vi ‐ 3.2 Blue‐Sky Eruptions – Hydrothermal...................................................................... 54 3.2.1 Kuirau Park, Rotorua, New Zealand – 2001, 2006......................................... 54 3.2.2 Agua Shuca, Ahuachapán Geothermal Field, El Salvador – 13 October 1990............................................................................................ 56 3.3 Blue‐Sky Events..................................................................................................... 57 3.3.1 Mount St. Helens, Washington State, USA – 18 May 1980........................... 57 3.4 “Loss‐of‐Life” Events............................................................................................. 61 3.4.1 Nevado del Ruiz, Columbia – 13 November 1985......................................... 61 3.5 Conclusions ........................................................................................................... 66 Chapter 4. Monitoring Volcanoes and Forecasting Volcanic Eruptions......................... 70 4.1 Monitoring Volcanoes........................................................................................... 70 4.1.1 Effective Monitoring and Forecasting ..........................................................
Recommended publications
  • In Memoriam I Met Ralph in 1989 When I Moved to Wolverhampton, Through Our Involvement with the Wolverhampton Mountain- Eering Club
    Obituaries Matterhorn. Edward Theodore Compton. 1880. Watercolour. 43 x 68cm. (Alpine Club Collection HE118P) 399 I N M E M ORI am 401 Ralph Atkinson 1952 - 2014 In Memoriam I met Ralph in 1989 when I moved to Wolverhampton, through our involvement with the Wolverhampton Mountain- eering Club. Weekends in Wales The Alpine Club Obituary Year of Election and day trips to Matlock and the (including to ACG) Roaches became the foundation for extended expeditions to the Ralph Atkinson 1997 Alps including, in 1991, a fine Una Bishop 1982 six-day ski traverse of the Haute John Chadwick 1978 Route, Argentière to Zermatt, John Clegg 1955 and ascents in 1993 of the Mönch Dennis Davis 1977 and Jungfrau. Descending the Gordon Gadsby 1985 Jungfrau in a storm, we could Johannes Villiers de Graaff 1953 barely see each other. I slipped David Jamieson 1999 in the new snow and had to self- Emlyn Jones 1944 arrest, aided by the tension in the Brian ‘Ned’ Kelly 1968 rope to Ralph. It worked, and I Neil Mackenzie Asp.2011, 2015 Ralph Atkinson climbing on the slabs of Fournel, was soon back on the ridge, but Richard Morgan 1960 near Argentière, Ecrins. (Andy Clarke) when we dropped below the John Peacock 1966 Rottalsattel and could speak to Bill Putnam 1972 each other again, he had no idea that anything untoward had happened. Stephanie Roberts 2011 I recall long journeys by car enlivened by his wide-ranging taste in music. Les Swindin 1979 The keynote of many outings was his sense of fun. There were long stories, John Tyson 1952 jokes or pithy one-liners.
    [Show full text]
  • Source to Surface Model of Monogenetic Volcanism: a Critical Review
    Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Source to surface model of monogenetic volcanism: a critical review I. E. M. SMITH1 &K.NE´ METH2* 1School of Environment, University of Auckland, Auckland, New Zealand 2Volcanic Risk Solutions, Massey University, Palmerston North 4442, New Zealand *Correspondence: [email protected] Abstract: Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas within a wide compositional range from strongly silica undersaturated to saturated and oversatu- rated; less commonly, the spectrum includes more siliceous compositions. Small-scale volcanic systems are commonly monogenetic in the sense that they are represented at the Earth’s surface by fields of small volcanoes, each the product of a temporally restricted eruption of a composition- ally distinct batch of magma, and this is in contrast to polygenetic systems characterized by rela- tively large edifices built by multiple eruptions over longer periods of time involving magmas with diverse origins. Eruption styles of small-scale volcanoes range from pyroclastic to effusive, and are strongly controlled by the relative influence of the characteristics of the magmatic system and the surface environment. Gold Open Access: This article is published under the terms of the CC-BY 3.0 license. Small-scale basaltic magmatic systems characteris- hazards associated with eruptions, and this is tically occur at the Earth’s surface as fields of small particularly true where volcanic fields are in close monogenetic volcanoes. These volcanoes are the proximity to population centres.
    [Show full text]
  • Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens
    Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens Materials Included in this Box: • Teacher Background Information • 3-D models of Mt. St. Helens (before and after eruption) • Examples of stratovolcano rock products: Tuff (pyroclastic flow), pumice, rhyolite/dacite, ash • Sandbox crater formation exercise • Laminated photos/diagrams Teacher Background There are several shapes and types of volcanoes around the world. Some volcanoes occur on the edges of tectonic plates, such as those along the ‘ring of fire’. But there are also volcanoes that occur in the middle of tectonic plates like the Yellowstone volcano and Kilauea volcano in Hawaii. When asked to draw a volcano most people will draw a steeply sided, conical mountain that has a depression (crater) at the top. This image of a 'typical' volcano is called a stratovolcano (a.k.a. composite volcano). While this is the often visualized image of a volcano, there are actually many different shapes volcanoes can be. A volcano's shape is mostly determined by the type of magma/lava that is created underneath it. Stratovolcanoes get their shape because of the thick, sticky (viscous) magma that forms at subduction zones. This magma/lava is layered between ash, pumice, and rock fragments. These layers of ash and magma will build into high elevation, steeply sided, conical shaped mountains and form a 'typical' volcano shape. Stratovolcanoes are also known for their explosive and destructive eruptions. Eruptions can cause clouds of gas, ash, dust, and rock fragments to eject into the atmosphere. These clouds of ash can become so dense and heavy that they quickly fall down the side of the volcanoes as a pyroclastic flow.
    [Show full text]
  • Pyroclastic Flow Hazards
    Pyroclastic Flow Hazards Lecture Objectives -definition and characteristics -generation of pyroclastic flows -impacts and hazards What are pyroclastic flows? Pyroclastic flows are high- density mixtures of hot, dry rock fragments and hot gases that move away from the vent that erupted them at high speeds. Generation Mechanisms: -explosive eruption of molten or solid rock fragments, or both. -non-explosive eruption of lava when parts of dome or a thick lava flow collapses down a steep slope. Most pyroclastic flows consist of two parts: a basal flow of coarse fragments that moves along the ground, and a turbulent cloud of ash that rises above the basal flow. Ash may fall from this cloud over a wide area downwind from the pyroclastic flow. Mt. St. Helens Effects of pyroclastic flows A pyroclastic flow will destroy nearly everything in its path. With rock fragments ranging in size from ash to boulders traveling across the ground at speeds typically greater than 80 km per hour, pyroclastic flows knock down, shatter, bury or carry away nearly all objects and structures in their way. The extreme temperatures of rocks and gas inside pyroclastic flows, generally between 200°C and 700°C, can cause combustible material to burn, especially petroleum products, wood, vegetation, and houses. Pyroclastic flows vary considerably in size and speed, but even relatively small flows that move <5 km from a volcano can destroy buildings, forests, and farmland. On the margins of pyroclastic flows, death and serious injury to people and animals may result from burns and inhalation of hot ash and gases. Pyroclastic flows generally follow valleys or other low-lying areas and, depending on the volume of rock debris carried by the flow, they can deposit layers of loose rock fragments to depths ranging from less than one meter to more than 200 m.
    [Show full text]
  • DNPA's Detailed Responses to Comments
    Dartmoor National Park Authority Local Plan Review 2018 - 2036 Full report on Regulation 19 representations (by respondent) Respondent Number: 0002 Name: John Penny Organisation: Devon Stone Federation On behalf of: Rep Number: 7 Local Plan Section: 1 Paragraph / Policy: Strategy Is the Local Plan sound?: Yes Is the Local Plan legally compliant?: No Is the Local Plan compliant with the duty to co-operate?: Yes Hearing session(s)?: Yes, I wish to participate in hearing session(s) Why?: to ensure the Plan is consistent with national policy Did respondent comment on Reg 18 Local Plan?: Yes Detail of Representation: plan needs to be consistent with national policy Modifications necessary: The paragraph states "Major development will not take place in the National Park other than in exceptional circumstances". The use of the word 'will' is not appropriate and does not reflect the definition given on page 9 under "Understanding the Local Plan". The sentence about Major development is supposed to reflect para 172 of the NPPF 2018. This uses the word 'should', as in "Planning permission should be refused for major development other than in exceptional circumstances". Therefore, the sentence in the Local Plan should be changed to: "Major development should not take place in the National Park other than in exceptional circumstances". We suggest that the use of the word 'will' is reviewed elsewhere in the Draft Local Plan. Authority response: The wording is considered consistent with the NPPF, ‘should’ in the NPPF allows local policy a degree of flexibility in the application of the policy and the possibility of introducing other criteria which could allow major development to occur in a National Park, other than the exceptional circumstances stated in NPPF para 172.
    [Show full text]
  • The Science Behind Volcanoes
    The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere.
    [Show full text]
  • Annual Report 2019
    Annual Report 2019 - 2020 I te wā i tuhia ai te pūrongo ā-tau At the time of writing the 2019 | 2020 Annual 2019/2020, e tāmia ana a Aotearoa Report, Aotearoa is still whānui i te mate urutā, arā i te Korona. weathering the storm of the COVID-19 global Nā konā i raru ai ngā huinga raraunga pandemic. While not me ngā kaupapa e whakaaturia ana i relevant to the data sets and kaupapa presented tēnei pūrongo, ka mutu, e mārama ana in this report, we are mātau kua horapa āna kawenga ki tēnā cognisant of the impact this event has had on iwi, ki tēnā hapū huri noa i te ao. our iwi, hapū and every E mihi ana ngā tarahitī o TTA ki te person on our planet. The Tūhourangi Tribal manawaroa o Tūhourangi whānui, te Authority Trustees would āhei ki te papare ā-iwi, te tiaki pai i ō like to acknowledge the resilience of our tātau kōeke, te aha, te aha. Tēnei te mihi Tūhourangi whānau – o te ngākau māhaki ki a koutou katoa. our ability to collectively respond and look after He mea tuku iho ki a Tūhourangi tōna our koeke and most aumangea – ka mutu, ehara tātau i te vulnerable has been humbling. tauhou ki ngā piki me ngā heke o tēnei Tūhourangi has a legacy ao matemate, ko te hū o Tarawera of resilience – our history tērā, ko ngā pakanga o mua tērā. E is steeped in overcoming adversity, from the whakapono ana ka puta te ihu, kia Tarawera eruption in whakahōnoretia ō tātau tūpuna, kia 1886 to times of hardship before.
    [Show full text]
  • MTSC 2007-07July**
    beechleaves Newsletter of the Manawatu Tramping and Skiing Club July 2007 Issue 6 mail: MTSC P.O. Box 245 Palmerston North web: www.mtsc.org.nz Carrying out the sofa’s from our Lodge at Whakapapa. Photo by Mike Sampson. ..! Upcoming club nights ..! Looking After Your Feet ! 7.30 pm, 1st and 3rd Tuesdays of the month at the Manawatu Aero Club Rooms, Airport Drive 3rd July - Looking after your Feet! Do you suffer from sore feet after several hours tramping? The solution could be as easy as the way you tie your boot laces! Murray McDonald from the Shoe Clinic will talk about foot care, tying of shoe/boot laces and answer all your questions. 17th July- Gliding in New Zealand John Brooks, a local glider pilot, will be giving us a look at our back country from a totally different perspective, including some spectacular south island scenery. 7th August- “Birds in Arabia” by John Cockrem 21st August- Photographic competition Time to dust off those slides and prints or go through that collection of digital photos on your computer as the annual club photo competition is coming. Photos can be entered in one of the following 5 categories with the one condition that photos shouldn’t have been entered in a previous photo competition. Alpine (NZ) Predominantly alpine scenery in NZ (i.e. above the bushline). Scenic (NZ) Pictorial interest in NZ hills etc (i.e. predominantly below the bushline). Natural History (NZ) NZ flora and fauna or detail (e.g. geology, ice formations etc). Topical (NZ) Peo- ple or detail related to tramping, climbing, or skiing related activities in NZ Overseas: Open From: Map 260-U22 (LINZ) 1 President’s Report by Howard Nicholson email [email protected] or phone (06) 357 6325 July 2007 Winter is starting with a bang this year!! As I was being snowed on at the Alice Nash Memorial Heri- VES tage Lodge carpark recently, I started thinking about the awesome tramping and skiing trips that are coming up on the trip card.
    [Show full text]
  • Conditioning: Why Go to the to Pack Light, Gym When You Just Pack Right Can Go Outdoors?
    WWW.MOUNTAINEERS.ORG MARCH/APRIL 2011 • VOLUME 105 • NO. 2 MountaineerE X P L O R E • L E A R N • C O N S E R V E Conditioning: Why go to the To pack light, gym when you just pack right can go outdoors? Take your spring skiing to British Columbia’s backcountry inside Mar/Apr 2011 » Volume 105 » Number 2 9 How to best lighten your pack Enriching the community by helping people explore, conserve, learn about, and enjoy the 11 Sailing? Mountaineers? lands and waters of the Pacific Northwest. A carload of climbers said, why not? 18 B.C.’s best for spring skiing 11 Heading north? Check these lodges and huts 21 Train outdoors to get ready Why go to the gym when you can go to the beach? 24 Doing the PCT piece by piece This Foothills course is all about logistics 6 reaching OUT Mountaineers with sea legs Connecting the community to the outdoors 7 conservation currents 18 News about conservation and recreational access 14 OUR fRIENdS Goings on in the broader outdoor community 16 GEAR grist Making the turn from downhill to backcountry skiing 17 stepping UP Help prepare Kitsap Cabin for Earth Day! Best of British Columbia’s backcountry 26 bookMARkS Tasty trail food you don’t need to pack 24 27 PLAyGROUNd A place for kids to solve the puzzles of nature 28 CLIff notes New column looks at what’s up in the alpine 37 GO GUIdE Trips, outings, events, courses, seminars Taking on Washington’s Pacific Crest Trail DISCOVER THE MOUntaINEERS If you are thinking of joining — or have joined and aren’t sure where to The Mountaineer uses .
    [Show full text]
  • Lake Ōkareka 21
    Contents Purpose 1 Overview 1 Lake Rotorua 2016-2017 1 Lake Rotoehu 2016-2017 3 Lake Rotoiti 2016-2017 3 Lake Ōkāreka 2016-2017 3 Key achievements 5 Rotorua Te Arawa Lakes Annual Water Quality Results 10 Lake Rotorua 13 Lake Rotoehu 17 Lake Rotoiti 19 Lake Ōkareka 21 Actions and Outcomes for Non Deed Lakes 23 Communications and stakeholder engagement update 26 Science update 27 Land Technical Advisory Group 27 Water Quality Technical Advisory Group 27 Rotorua Te Arawa Lakes Programme – DRAFT Annual Report 2016-2017 i Environmental modelling 28 Action Plans and sewage reticulation 28 Financials 29 Rotorua Te Arawa Lakes Programme – DRAFT Annual Report 2016-2017 ii Purpose The purpose of this document is to report progress against the 2016-2017 Annual Work Programme of the Rotorua Te Arawa Lakes Programme (the Programme), for the year ending 30 June 2017. This report is in accordance with Clause 5.1 and 5.2 of Deed of Funding with the Crown, for the Programme. In this report, progress made on individual interventions is reported against the Annual Work Programme commitments. The overarching goal of the Deed of Funding Agreement is to meet community aspirations for water quality in the four Deed Funded lakes: Rotoiti, Rotorua, Ōkāreka and Rotoehu. Each of these lakes has a target water quality set by the community in the Bay of Plenty Regional Water and Land Plan. This target water quality is set by Trophic Level Index (TLI) and this report provides an update on the status of water quality across the Rotorua Te Arawa Lakes, against the targets set for all lakes, Deed and non-Deed funded.
    [Show full text]
  • GNS Science Consultancy Report 2013/155
    DISCLAIMER This report has been prepared by the Institute of Geological and Nuclear Sciences Limited (GNS Science) exclusively for and under contract to Bay of Plenty Regional Council. Unless otherwise agreed in writing by GNS Science, GNS Science accepts no responsibility for any use of, or reliance on any contents of this Report by any person other than Bay of Plenty Regional Council and shall not be liable to any person other than Bay of Plenty Regional Council, on any ground, for any loss, damage or expense arising from such use or reliance. The data presented in this Report are available to GNS Science for other use from January 2015. BIBLIOGRAPHIC REFERENCE Tschritter, C.; White, P. 2014. Three-dimensional geological model of the greater Lake Tarawera catchment. GNS Science Consultancy Report 2013/155. 42 p. Project number 631W1026 Confidential 2013 CONTENTS EXECUTIVE SUMMARY ....................................................................................................... III 1.0 INTRODUCTION ........................................................................................................ 1 2.0 REVIEW OF GEOLOGY AND HHYDROGEOLOGY IN THE GREATER LAKE TARAWERA CATCHMENT ............................................................................. 2 2.1 History and Structure ..................................................................................................... 2 2.2 Major Geological Units in the Study Area ..................................................................... 2 2.2.1 Okataina Rhyolites ..........................................................................................
    [Show full text]
  • Caving in Haiti
    Caving in Haiti Learn what it takes to rescue someone from USA a cave through lots of hands-on training and FOREIGN M —16th International January 4th, 2014—Central Indiana Grotto a full-day mock rescue. Become a safer caver arch 15-22, 2014 Vertical Training, Open Training Session, 10am- and more able to perform small party rescue! Symposium on Vulcanospeleology, Galápagos 4pm, Indianapolis, Indiana Contact: Ron Adams Course is Thursday through Sunday, with the Islands. Pre-symposium caving or scuba diving [email protected] (317) 490-7727 optional certification test on Monday, August March 10-15, 2014; Post-symposium caving March 22-29, 2014 February 22, 2014—The SERA Winter Business 25. All registration is handled by the Alabama meeting, hosted by the Pigeon Mountain Grotto, Fire College. To register, please CALL them at will be held in LaFayette, GA at the LaFayette (866) 984-3545. For more information see the Community Center. For additional information Huntsville Cave Rescue Unit website http://www. contact Diane Cousineau at dcousineau@ hcru.org/rescueclass earthlink.net May 23-26, 2014—Memorial Day Weekend: 43rd Kentucky Speleofest hosted by The Louisville Grotto at the Lone Star Preserve, Bonnieville, KY... We will have a food vendor, On Rope 1, camping, warm showers, howdy party with DJ, banquet, band, kayaking, hiking, cave social. More info: contact [email protected] July 14-18, 2014—NSS Convention, NSS Headquarters & Conference Center, Huntsville, AL. Visit our website: http://nss2014.caves. org or contact Julie Schenck-Brown, Chair, at [email protected] or (256) 599-2211 or Jeff Martin, Vice-Chair, at [email protected] or (770) 653-4435.
    [Show full text]