Publications of the Volcano Hazards Program 1994 - 1998
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Expeditions & Treks 2008/2009
V4362_JG_Exped Cover_AW 1/5/08 15:44 Page 1 Jagged Globe NEW! Expeditions & Treks www.jagged-globe.co.uk Our new website contains detailed trip itineraries 2008 for the expeditions and treks contained in this brochure, photo galleries and recent trip reports. / 2009 You can also book securely online and find out about new trips and offers by subscribing to our email newsletter. Jagged Globe The Foundry Studios, 45 Mowbray Street, Sheffield S3 8EN United Kingdom Expeditions Tel: 0845 345 8848 Email: [email protected] Web: www.jagged-globe.co.uk & Treks Cover printed on Take 2 Front Cover: Offset 100% recycled fibre Mingma Temba Sherpa. sourced only from post Photo: Simon Lowe. 2008/2009 consumer waste. Inner Design by: pages printed on Take 2 www.vividcreative.com Silk 75% recycled fibre. © 2007 V4362 V4362_JG_Exped_Bro_Price_Alt 1/5/08 15:10 Page 2 Ama Dablam Welcome to ‘The Matterhorn of the Himalayas.’ Jagged Globe Ama Dablam dominates the Khumbu Valley. Whether you are trekking to Everest Base Camp, or approaching the mountain to attempt its summit, you cannot help but be astounded by its striking profile. Here members of our 2006 expedition climb the airy south Expeditions & Treks west ridge towards Camp 2. See page 28. Photo: Tom Briggs. The trips The Mountains of Asia 22 Ama Dablam: A Brief History 28 Photo: Simon Lowe Porter Aid Post Update 23 Annapurna Circuit Trek 30 Teahouses of Nepal 23 Annapurna Sanctuary Trek 30 The Seven Summits 12 Everest Base Camp Trek 24 Lhakpa Ri & The North Col 31 The Seven Summits Challenge 13 -
Crary-Henderson Collection, B1962.001
REFERENCE CODE: AkAMH REPOSITORY NAME: Anchorage Museum at Rasmuson Center Bob and Evangeline Atwood Alaska Resource Center 625 C Street Anchorage, AK99501 Phone: 907-929-9235 Fax: 907-929-9233 Email: [email protected] Guide prepared by: Mary Langdon, Volunteer, and Sara Piasecki, Archivist TITLE: Crary-Henderson Collection COLLECTION NUMBER: B1962.001, B1962.001A OVERVIEW OF THE COLLECTION Dates: circa 1885-1930 Extent: 19.25 linear feet Language and Scripts: The collection is in English. Name of creator(s): Will Crary; Nan Henderson; Phinney S. Hunt; Miles Bros.; Lyman; George C. Cantwell; Johnson; L. G. Robertson; Lillie N. Gordon; John E. Worden; W. A. Henderson; H. Schultz; Merl LaVoy; Guy F. Cameron; Eric A. Hegg Administrative/Biographical History: The Crary and Henderson Families lived and worked in the Valdez area during the boom times of the early 1900s. William Halbrook Crary was a prospector and newspaper man born in the 1870s (may be 1873 or 1876). William and his brother Carl N. Crary came to Valdez in 1898. Will was a member of the prospecting party of the Arctic Mining Company; Carl was the captain of the association. The Company staked the “California Placer Claim” on Slate Creek and worked outside of Valdez on the claim. Slate Creek is a tributary of the Chitina River, in the Chistochina District of the Copper River Basin. Will Crary was the first townsite trustee for Valdez. Carl later worked in the pharmaceutical field in Valdez and was also the postmaster. Will married schoolteacher Nan Fitch in Valdez in 1906. Carl died of cancer in 1927 in Portland, Oregon. -
Arenal Volcano Tours
TRUST THE EXPERTS Hand Crafted Itineraries Curated Hotel Collection Luxury Vehicles Experienced Travel Consultants ARENAL VOLCANO 24/7 In-Country TOURS Assistance The Arenal Volcano once erupted an average of 41 times per day. Today, the volcano is in a resting phase but still a sight to behold. The region is not only home to the volcano, it also benefits from volcano-fed thermal hot springs, plunging waterfalls, the impressive Over 50,000 Satisfied size of Lake Arenal, and a rich secondary rainforest ecosystem with Customers exotic wildlife. Now considered by many the adventure capital of Costa Rica, Arenal is a great base for adventure tours like zip-lining, whitewater rafting, COSTA RICA waterfall rappelling, and more. EXPERTS The listed tours are available from hotels in the central Arenal zone. 3166 N Lincoln Ave., Additional fees may apply for hotels outside of the central zone Suite 424 Chicago, IL. 60657 www.costaricaexperts.com Phone: 800-827-9046 Fax: 773-935-9252 Arenal Hanging Bridges Hike Hike across the Arenal Hanging Bridges with a naturalist guide for a perfect half-day Arenal tour. This ecotourism project of solid ground trails and state of the art hanging bridges was designed for the observation and conservation of Costa Rica’s incredible nature. The reserve, with nearly 370 acres of rainforest, is home to countless species of amazing birds, mammals, and lush vegetation. You will walk along the treetops with your naturalist guide, encountering 8 fixed bridges and 6 hanging bridges. These connect gaps in the reserve canyon, allowing you to walk right into the most important layers of the rainforest. -
Mejoras En El Paradigma Del Manejo De La Gestión Del Riesgo En Los Parques Nacionales Volcánicos De Costa Rica, Entre El Año 2000 Y El 2020
Revista Geológica de América Central, 64, 1-15 , 2021 doi: 10.15517/rgac.v0i64.46615 ISSN: 0256-7024 Mejoras en el paradigma del manejo de la gestión del riesgo en los parques nacionales volcánicos de Costa Rica, entre el año 2000 y el 2020 Improvements in risk management paradigm in Costa Rican volcanic national parks between 2000 and 2020 Guillermo E. Alvarado*, Lidier Esquivel y Blas Sánchez Comisión Nacional de Prevención de Riesgos y Atención de Emergencias (CNE), Unidad de Investigación y Análisis del Riesgo, San José, Costa Rica *Autor para contacto: [email protected] (Recibido: 23/08/2020; aceptado 13/01/2021) RESUMEN: Costa Rica es conocida a nivel mundial como una meca turística. A partir de 1955, casi todos los grandes volcanes comenzaron a ser declarados parques nacionales, deteniendo la ocupación y explotación humana en la cúspide de estos sectores, al tiempo que varios parques han estado expuestos a la actividad eruptiva de los cinco volcanes históricamente activos. Los parques nacionales volcánicos están sujetos al turismo y, con ello, al peligro de que se puedan generar afectación y pérdidas en vidas huma- nas. La muerte de una turista norteamericana y su guía costarricense en el año 2000, así como la repentina erupción del Poás en el año 2017, aunado a la persistente actividad eruptiva del Turrialba por más de 10 años, fueron los mecanismos disparadores de cuatro grandes cambios en el manejo y seguridad de los parques volcánicos costarricenses: a) la generación del decreto de restricción del uso de la tierra alrededor -
Discriminación De Unidades Volcánicas a Partir De Ímagenes Ópticas Y Radar: Estudio De Caso Volcán De Colima, Periodo 2004-2014.”
UNIVERSIDAD AUTÓNOMA DEL ESTADO DE MÉXICO FACULTAD DE GEOGRAFÍA “DISCRIMINACIÓN DE UNIDADES VOLCÁNICAS A PARTIR DE ÍMAGENES ÓPTICAS Y RADAR: ESTUDIO DE CASO VOLCÁN DE COLIMA, PERIODO 2004-2014.” TESIS QUE PARA OBTENER EL GRADO DE: LICENCIADO EN GEOINFORMÁTICA PRESENTA CIRINO GARCÍA MALVAÉZ DIRECTORA DRA. NORMA DÁVILA HERNÁNDEZ REVISORES MTRO. RAÚL EDUARDO MURILLO OLVERA DR. HÉCTOR CABADAS BÁEZ TOLUCA, ESTADO DE MÉXICO. DICIEMBRE DEL 2014 Agradecimientos A mi asesora Dr. Norma Dávila Hernández por el apoyo brindado durante la elaboración de este trabajo, el creer en mí y por la dedicación brindada para lograr esta gran meta en mi vida. A mis revisores Mtro. Raúl Eduardo Murillo Olvera y Dr. Héctor Cabadas Báez, en verdad no pude haber tenido mejores revisores. Mtro. Murillo a usted un agradecimiento especial ya que siempre estuvo a mi lado en el transcurso de toda la licenciatura no solo como profesor, si no como amigo. Gracias. A mis papas con la mayor gratitud por los esfuerzos realizados para que yo lograra terminar mi tesis profesional siendo para mí la mejor herencia y a ellos les dedico este trabajo ya que son mi más grande estimulo e inspiración. Gracias por guiar mi vida, esto ha hecho que sea quien soy en la vida. LOS AMO A mis hermanas porque siempre me apoyaron, me alentaron, estimularon y me alegraron en momentos difíciles. A Mary que fue mi acompañante en toda la licenciatura, que siempre me apoyo, me ayudo a dar el máximo y me oriento. 1 INDICE 1.0 INTRODUCCIÓN .............................................................................................. 3 2.0 ANTECEDENTES ............................................................................................. 5 3.0 PLANTEAMIENTO DEL PROBLEMA Y JUSTIFICACIÓN ............................. -
Glenn Highway Tok Cutoff (GJ-125 to GJ-0) to Milepost a 160
Map GLENN HIGHWAY • TOK CUTOFF Glenn Highway To Chicken and Eagle © The MILEPOST To Delta Junction (see TAYLOR HIGHWAY section) Key to mileage boxes ver (see ALASKA HIGHWAY section) Tanana Ri miles/kilometres G miles/kilometres Tanacross 5 from: la A L c A Swb T-Tok V-Valdez ia S K 2 Tok Map Location G-Glennallen ted A ® GJ-Gakona Junction A re A-Anchorage a R 2 A 1 Tetlin Junction J-Junction N HJ-Haines Junction Mount Kimball G T-0 a To Haines DJ-Delta Junction in 10,300 ft./3,139m E ch r w GJ-125/201km Junction Chisto cie G la A-328/528km (see ALASKA Principal Route Logged Key to Advertiser er HIGHWAY Services T iv DJ-108/174km C -Camping ok R section) Paved Unpaved R HJ-296/476km D -Dump Station iv ok Other Roads Logged d -Diesel er T G -Gas (reg., unld.) Tetlin I -Ice Lake Other Roads Scenic Byway L -Lodging M -Meals T Refer to Log for Visitor Facilities P -Propane Tok Cutoff ok Cu L R -Car Repair (major) na i Scale Sla R Mineral Lakes t iv t r -Car Repair (minor) e l 0 10 Miles r e S -Store (grocery) 0 10 Kilometres T -Telephone (pay) . t Cr t Bartell off (GJ-125 r Mentasta Lake e r e t T r. o v iv C i R Mentasta Lake S t ation k R Mentasta Summit n T-65/105km 2,434 ft./742m M a . i r E N d J-0 t C T A n e S I . -
Geology of Nevado De Toluca Volcano and Surrounding Areas, Central Mexico
mch089 1 of 26 Geological Society of America Map and Chart Series MCH089 2002 Geology of Nevado de Toluca Volcano and surrounding areas, central Mexico *Armando García-Palomo, José Luis Macías, José Luis Arce Instituto de Geofísica, Universidad Nacional Autónoma de México, Coyoacán 04510, México D.F., México Lucia Capra Instituto de Geografía, Universidad Nacional Autónoma de México, Coyoacán 04510, México D.F., México Victor Hugo Garduño Departamento de Geología y Mineralogía, Instituto de Investigaciones Metalúrgicas, Universidad Michoacana de San Nicolás de Hidalgo, Morelia, Michoacán, México Juan Manuel Espíndola Instituto de Geofísica, Universidad Nacional Autónoma de México, Coyoacán 04510, México D.F., México ABSTRACT Nevado de Toluca is an andesitic-dacitic stratovolcano of Pliocene-Holocene age located in central Mexico. The volcano is built on a complex sequence of metamorphic and sedimentary formations of Jurassic-Cretaceous age, rhyolitic ignimbrites of late Eocene age, and massive andesitic lava flows of late Miocene. In the northwest corner of the map area, on top of this basement sequence, a complex andesitic-dacitic strato- volcano, San Antonio, and a series of andesitic-dacitic domes and cones of Pliocene– early Pleistocene age were also built. The first andesitic-dacitic emissions of Nevado de Toluca occurred 2.6 Ma and continued during late Pleistocene–Holocene time contem- porarily with basaltic to dacitic emissions of the Chichinautzin Volcanic Field in the eastern parts of the map area. Volcanism in the area has been controlled by the interplay of three fault systems active since late Miocene. These systems, from older to younger, are the Taxco-Querétaro Fault System (NNW–SSE), the San Antonio Fault System (NE–SW), and the Tenango Fault System (E–W). -
Eruptive History of Arenal Volcano, Costa Rica, 7 Ka to Present
+ MODEL ARTICLE IN PRESS Journal of Volcanology and Geothermal Research xx (2006) xxx–xxx www.elsevier.com/locate/jvolgeores Eruptive history of Arenal Volcano, Costa Rica, 7 ka to present Gerardo J. Soto ⁎, Guillermo E. Alvarado Área de Amenazas y Auscultación Sísmica y Volcánica, Instituto Costarricense de Electricidad, Apdo 10032-1000, San José, Costa Rica Received 30 June 2005; accepted 28 March 2006 Abstract New tephra-stratigraphic studies of Arenal volcano have been used to update its volcanic history. Deposits of major eruptions are renamed AR-1 to AR-22 (from older to younger, in stratigraphic order), extending from 7 ka B.P. to 1968 A.D. Arenal tephras overlie regional tuffs that are N20,000 years old. Isopachs and characteristics of the most relevant and recognized fall deposits are presented. Among Arenal eruptions, plinian events like AR-20, AR-15, AR-12 and AR-9, were the most relevant, with tephra volumes up to 0.44 km3. These plinian eruptions are separated by periods of 750–1080 years. Also 8 subplinian, 7 violent strombolian and 2 vulcanian eruptions have been recognized and correlated in Arenal's tephra sequence. Tens of other minor explosive eruptions resembling in size to AR-22, which occurred in July 1968, have been recognized. Lava cycles have generally followed the plinian eruptions. Typical erupting volumes for these cycles have been in the order of ∼ 0.7 km3. The estimated total volume of tephra fall is ∼ 4.5 km3. The rate of total volcanics erupted is ∼ 2.7 km3 ka−1 (0.086 m3 s−1). -
Climbers As Humanitarians: Helping Injured Migrants in Mexico
Appalachia Volume 69 Number 2 Summer/Fall 2018: Role Reversal in Article 4 the Mountains 2018 Climbers as Humanitarians: Helping Injured Migrants in Mexico Lisa Densmore Ballard Follow this and additional works at: https://digitalcommons.dartmouth.edu/appalachia Part of the Nonfiction Commons Recommended Citation Ballard, Lisa Densmore (2018) "Climbers as Humanitarians: Helping Injured Migrants in Mexico," Appalachia: Vol. 69 : No. 2 , Article 4. Available at: https://digitalcommons.dartmouth.edu/appalachia/vol69/iss2/4 This In This Issue is brought to you for free and open access by Dartmouth Digital Commons. It has been accepted for inclusion in Appalachia by an authorized editor of Dartmouth Digital Commons. For more information, please contact [email protected]. Climbers as Humanitarians Helping injured migrants in Mexico Lisa Densmore Ballard 24 Appalachia Appalachia_SF2018_FINAL REV3.indd 24 5/9/18 1:36 PM ico de Orizaba called to me when I first saw it in November P 2017, while driving into Tlachichuca, Mexico. I looked up its northwestern flank and wanted to stand on top of its white cone. It beckoned, cool and refreshing, framed by an azure sky, miles from where I stood. Around me, heat waves rose from the pavement and dust devils swirled among the cornstalk pyramids by the village gate. I realized I must not underestimate this alpine goliath. Pico de Orizaba (18,491 feet) is the third highest mountain in North America, after Denali in Alaska and Mount Logan in the Canadian Yukon. Located in Mexico’s volcanic belt, on the border of the states of Veracruz and Puebla, Orizaba rises prominently from a pancake-flat patchwork of corn and cactus in central Mexico. -
R. L. Smith, H. R. Shaw, R. G. Luedke, and S. L. Russell U. S. Geological
COMPREHENSIVE TABLES GIVING PHYSICAL DATA AND THERMAL ENERGY ESTIMATES FOR YOUNG IGNEOUS SYSTEMS OF THE UNITED STATES by R. L. Smith, H. R. Shaw, R. G. Luedke, and S. L. Russell U. S. Geological Survey OPEN-FILE REPORT 78-925 This report is preliminary and has not been edited or reviewed for conformity with Geological Survey Standards and nomenclature INTRODUCTION This report presents two tables. The first is a compre hensive table of 157 young igneous systems in the western United States, giving locations, physical data, and thermal en ergy estimates, where apropriate, for each system. The second table is a list of basaltic fields probably less than 10,000 years old in the western United States. These tables are up dated and reformatted from Smith and Shaw's article "Igneous- related geothermal systems" in Assessment of geothermal re sources of the United States 1975 (USGS Circular 726, White and Williams, eds., 1975). This Open-File Report is a compan ion to Smith and Shaw's article "Igneous-related geothermal systems" in Assessment of geothermal resources in the United States 1978 (USGS Circular 790, Muffler, ed., 1979). The ar ticle in Circular 790 contains an abridged table showing only those igneous systems for which thermal estimates were made. The article also gives an extensive discussion of hydrothermal cooling effects and an explanation of the model upon which the thermal energy estimates are based. Thermal energy is calculated for those systems listed in table 1 that are thought to contribute significant thermal en ergy to the upper crust. As discussed by Smith and Shaw (1975), silicic volcanic systems are believed to be associated nearly always with high-level (<10 km) magma chambers. -
A Trip Through Lush Greenery: Costa Rica and Nicaragua Known for Its Great Wealth of Species, Costa Rica’S Beautiful Flora and Fauna Awaits You
Tour Code CRCG 2020 A trip through lush greenery: Costa Rica and Nicaragua Known for its great wealth of species, Costa Rica’s beautiful flora and fauna awaits you. One third of its area is protected. Lagoons, beaches, coastal landscapes on both the Caribbean and Pacific sides are a must as well as the dense jungle, rainforests and volcanic landscapes. On our visit to several national parks, by bike or on foot, we discover a rich world of exotic birds and butterflies. This bike tour gives a detailed overview of these two neighbouring countries and introduces you to a sea of colours. Day 10 Granada - Walking in Mombacho Day 1 Costa Rica – San José Day 6 Arenal 40 km After a short 15-minute transfer, we arrive at A short transfer brings us to the lake dam. Departure from Frankfurt to San Jose (night the foot of Mount Granada, Mombacho. A flight with a stopover in Santa Domingo, The bike trip begins here. It follows the truck takes us to the crater from which many (flight 14.5 hours) water’s edge, through the rainforest and hiking trails leave into the rainforest. You small villages, towards Tilaran. may see monkeys (you will almost certainly Day 2 San José hear them). Granada with its colonial Day 7 Around Miravalles Volcano 55 km heritage, should not to be missed. Arrival in San José the capital of Costa Rica and transfer (30 min.) to our hotel. The Gold A quiet bike ride from Bagaces to the slopes Day 11 Belan/Rivas – San Juan del Sur of the impressive Miravalles volcano which museum is one of the largest collections of 41 km gold in America and the city is also a real is the culminating point of the day, with its jewel of history and architecture. -
Nevado De Toluca: Habitat for Romerolagus Diazi? O. Monroy
Animal Biodiversity and Conservation 43.1 (2020) 115 Nevado de Toluca: habitat for Romerolagus diazi? O. Monroy–Vilchis, A. A. Luna–Gil, A. R. Endara–Agramont, M. M. Zarco–González, G. A. González–Desales Monroy–Vilchis, O., Luna–Gil, A. A., Endara–Agramont, A. R., Zarco–González, M. M., González–Desales, G. A., 2020. Nevado de Toluca: habitat for Romerolagus diazi? Animal Biodiversity and Conservation, 43.1: 115–121, Doi: https://doi.org/10.32800/abc.2020.43.0115 Abstract Nevado de Toluca: habitat for Romerolagus diazi? The volcano rabbit (Romerolagus diazi), also known as teporingo or zacatuche, is a small rabbit that is endemic to Mexico. In this study we characterized its poten- tial habitat in the Area of Protection of Flora, and Fauna Nevado de Toluca, Mexico. Between April 2016 and November 2017, we sampled 1,807 units to determine the presence of this species using indirect evidence. We found dung pellets that could be attributed to R. diazi in 41 (2.27 %) of the sampled units. In 10 % of these units, we set up camera traps to confirm the presence of the species. Sites with presumed R. diazi pellets were characterised by rocky terrain, with Pinus hartwegii as the dominant tree species, and Festuca tolucensis as the dominant grass. Overall herbaceous cover was over 70 %. Sites observed to have a negative effect on the presence of the pellets were areas with livestock grazing and induced burning. The results of camera trapping did not reveal the presence of R. diazi in Nevado de Toluca. Key words: Teporingo, Conservation, High mountain forest Resumen El Nevado de Toluca: ¿un hábitat para Romerolagus diazi? El conejo de los volcanes (Romerolagus diazi), también conocido como teporingo o zacatuche, es un pequeño conejo endémico de México.