Climb Cotopaxi, Ecuador, South America
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UNIVERSIDAD CENTRAL DEL ECUADOR FACULTAD DE CIENCIAS AGRÍCOLAS Carrera De Turismo Ecológico
UNIVERSIDAD CENTRAL DEL ECUADOR FACULTAD DE CIENCIAS AGRÍCOLAS Carrera de Turismo Ecológico PROPUESTA DE UN MODELO DE GESTIÓN TURÍSTICA SOSTENIBLE PARA LA CONSOLIDACIÓN DEL ECOTURISMO EN LA CABECERA CANTONAL MACHACHI DEL CANTÓN MEJÍA TESIS DE GRADO PREVIO A LA OBTENCIÓN DEL TÍTULO EN LICENCIATURA EN TURISMO ECOLÓGICO ADRIÁN STALIN MOREJÓN LÓPEZ QUITO – ECUADOR 2015 DEDICATORIA A Dios en primer lugar por ser mi luz y guía, y haberme concedido la bendición de ser llamado su Hijo. A mis padres y mejores amigos Stalin Morejón y Jenny López, por todo su apoyo y esfuerzo durante mi vida estudiantil, por enseñarme a salir siempre adelante, a no bajar los brazos y luchar por conquistar mis miedos y cumplir mis sueños. A mi papi Telmo Egas, por estar a mi lado y ser una bendición enorme en mi vida. A mis hermanos Esthefanía, María Rosa, Telmo Alfonso y Julio por ser mi alegría y compañeros de aventuras. A mis familias Morejón, López, Egas y Rivadeneira por el apoyo constante, la preocupación y las palabras de aliento. A mi novia y futura esposa Anita Rivadeneira por presionarme a ser mejor de lo que los demás me limitan, y no soltar mi mano en los malos tiempos y en los buenos. A mis abuelitos Vicente y Carmen desde el cielo, y Aidita desde mi lado que cuidan mi camino y guían mis pasos. A la ciudad de Machachi, tierra del Chagra, valle de los 9 volcanes, gente amable y trabajadora. ii AGRADECIMIENTOS A Dios por darme la vida y permitirme esta oportunidad en mi carrera profesional. -
Tungurahua Volcano, Ecuador: Structure, Eruptive History and Hazards
Journal of Volcanology and Geothermal Research 91Ž. 1999 1±21 www.elsevier.comrlocaterjvolgeores Tungurahua Volcano, Ecuador: structure, eruptive history and hazards Minard L. Hall a,1, Claude Robin b,), Bernardo Beate c, Patricia Mothes a,1, Michel Monzier a,d,2 a Instituto Geofõsico,ÂÂ Escuela Politecnica Nacional, P.O. Box 1701-2759, Quito, Ecuador b Institut de Recherches Pour le DeÂÕeloppement() IRD, ex-ORSTOM , UR 6, OPGC, 5 Rue Kessler, 63038, Clermont-Ferrand, France c Departamento de Geologõa,ÂÂÂ Facultad de Geologõa, Minas y Petroleos, Escuela Politecnica Nacional, P.O. Box 1701-2759, Quito, Ecuador d Institut de Recherches pour le DeÂÕeloppement() IRD, ex-ORSTOM , UR 6, A.P. 17-11-6596, Quito, Ecuador Accepted 25 March 1999 Abstract Tungurahua, one of Ecuador's most active volcanoes, is made up of three volcanic edifices. Tungurahua I was a 14-km-wide andesitic stratocone which experienced at least one sector collapse followed by the extrusion of a dacite lava series. Tungurahua II, mainly composed of acid andesite lava flows younger than 14,000 years BP, was partly destroyed by the last collapse event, 2955"90 years ago, which left a large amphitheater and produced a ;8-km3 debris deposit. The avalanche collided with the high ridge immediately to the west of the cone and was diverted to the northwest and southwest for ;15 km. A large lahar formed during this event, which was followed in turn by dacite extrusion. Southwestward, the damming of the Chambo valley by the avalanche deposit resulted in a ;10-km-long lake, which was subsequently breached, generating another catastrophic debris flow. -
Determinación Del Volumen Del Casquete De Hielo Del Volcán Cotopaxi
DETERMINACIÓN DEL VOLUMEN DEL CASQUETE DE HIELO DEL VOLCÁN COTOPAXI M. Hall – P. Mothes INAMHI Instituto Nacional de Meteorología e Hidrología IRD Institut de Recherche pour le Développement IG-EPN Instituto de Geofísica de la Escuela Politécnica Nacional INGEOMINAS Instituto Colombiano de Geología y Minería Por Bolívar Cáceres, Jair Ramírez, Bernard Francou, Jean-Philippe Eissen, Jean-Denis Taupin, Ekkehard Jordan, Lars Ungerechts, Luis Maisincho, Diego Barba, Eric Cadier, Rodolphe Bucher, Arturo Peñafiel, Pablo Samaniego, Patricia Mothes 2 “Un nevado de los alrededores, que se llama Cotopaxi, se había despertado después de 200 años, después de tantos años de silencio, para recomenzar a echar fuego y llamas y una gran cantidad de polvo sulfuroso que se iba disipando hasta perderse en las inmediaciones: la hierba y las praderas se ahogaron. La mayor parte del ganado, que no encontró nada que pastar en los campos, murió de hambre y necesidad, y este polvo se extendió más de 60 leguas a la redonda. El año pasado, desde el mes de noviembre hasta ahora, hubo los daños más terribles; el fuego interno, que fundió la nieve de la cual estaba cubierta la cima de la montaña, formó un torrente tan terrible que se llevó consigo casas, terrenos, hombres, mujeres, manufacturas de textiles de las comarcas, echó abajo la mayoría de los puentes que desde las calles del poblado cruzan las diferentes corrientes de agua que descienden de esta montaña y nos causaron además, por infección del aire, una enfermedad también llamada Cotopaxi, que no era otra cosa que la parodititis conglomerada”. Joseph de Jussieu, 16 de marzo, 1745, Lettre à son frère. -
ECUADOR's FORGOTTEN VOLCANO the Eruption
Desastes en la Región ECUADOR’S FORGOTTEN VOLCANO The Eruption of Reventador Ecuador, one of the countries with the largest number of active volcanoes in the world, awoke on Sunday 3 November to a volcanic emergency. Since not enough funds are available to monitor all volcanoes, the Geophysical Institute of the National Polytechnic School— the body in charge of such surveillance— had not been paying too much attention to Reventador volcano, located 95 Km East of Quito, in the province of Napo, which had lain dormant for 26 years. Such was not the case that morning, though, as violent explosions flung gases, pyroclastic flows and large amounts of ash that reached an altitude of 16 Km. Residents of nearby communities in Napo and Sucumbíos provinces, frightened by the magnitude of the eruption, fled the area. “On Sunday we left in a hurry as soon as we saw that the mountain was starting to spit fire,” said a cattleman from the Chaco, the area nearest the volcano. The lava flows followed the course of Maker River, on the volcano’s slopes, and caused several landslides that cut off the main highway between Quito and Lago Agrio, the capital of Sucumbíos. Easterly winds blowing in the direction of Quito covered everything in their path—fields, rivers, houses, cattle, reservoirs—with dense ash. The population of Oyacachi, one of the most severely affected towns, reported that by 11 in the morning darkness was almost total. The ash reached Quito by 1:30 in the afternoon, wrapping the city in a grey cloud that made it almost impossible to breathe. -
Parroquia De Machachi.Pdf
PORTADA INSTITUTO TECNOLÓGICO SUPERIOR DE TURISMO Y HOTELERÍA CARRERA: GUÍA NACIONAL DE TURISMO TEMA: DIAGNÓSTICO DEL POTENCIAL TURÍSTICO DE LA PARROQUIA DE MACHACHI CANTÓN MEJÍA PROVINCIA DE PICHINCHA Trabajo de investigación previo a la obtención del título de Técnico en Guía Nacional de Turismo Autora: Grace Viviana Arias Cabrera Director: Ing. Wilson Villavicencio Vivar QUITO – ECUADOR 2014 DEDICATORIA A Dios por haberme permitido llegar hasta este punto y haberme dado salud, ser el motor de mi vida y darme lo necesario para seguir adelante cada día logrando culminar mis objetivos. A mis padres José Gabriel y Sandra Edith porque estuvieron animándome y apoyándome en los momentos más difíciles de mi vida y además por haberme dado toda la educación que desde mis primeros pasos han sembrado y que ahora pueden cosechar como mayor satisfacción a una profesional capaz de enfrentarse a la vida laboral con los conocimientos necesarios y los valores aprendidos en el núcleo familiar. A mi hermana Sandra Gabriela quien es mi mayor apoyo y la fuente de mi alegría para poder seguir cumpliendo mis anhelados sueños. A toda la población a nivel nacional e internacional para que puedan conocer una pequeña parte del Ecuador pero que a su vez es grande en los corazones de sus pobladores. Grace Viviana Arias Cabrera ii AGRADECIMIENTO En primer lugar a Dios por ser la guía y sustento durante mis años de formación como profesional y que gracias a Él he logrado culminar uno de mis mayores éxitos. A mis padres por todos sus esfuerzos, consideraciones y apoyo durante cada momento de mi vida y que han sido la base de mis esfuerzos estando a mi lado en mis mayores alegrías y también las tristezas. -
Cayambeantisana Skills Expedition
The Spirit of Alpinism www.AlpineInstitute.com [email protected] Administrative Office: 360-671-1505 Equipment Shop: 360-671-1570 CayambeAntisana Skills Expedition Program Itinerary Copyright 2015, American Alpine Institute Day 1: Arrive Quito (9500 ft / 2895 m) – Start of Part 1 This is the first scheduled day of the program. Arrive in Quito and meet your guide and other members of the expedition at Hotel Reina Isabel. The first day is designated for travel to Ecuador and becoming situated in country. For those who arrive early, we will provide you with a variety of sight seeing options including a tour of the historic colonial sector of Quito and El Panecillo overlooking the city. We will spend the night at Hotel Reina Isabel. Day 2: Acclimatize Otavalo Market After meeting the rest of your group for breakfast, we will drive north, crossing the line of the Equator on our way to the Otavalo market. We begin our acclimatization by exploring the market which is filled with indigenous crafts and food. For lunch, we will take a leisurely walk to Lago de San Pablo and dine on the lake shore across from the dormant Imbabura Volcano (15,255ft). We will return to Hotel Reina Isabel for the evening. Day 3: Acclimatize Cerro Pasochoa (13,776 ft / 4199 m) Today we will go on our first acclimatization hike on Cerro Pasochoa. The Pasochoa Wildlife Refuge has been protected since 1982, and exists as it did in preColombian times. In the forest below Cerro Pasochoa we will hike among stands of pumamaqui, polyapis, podocarpus, and sandlewood trees as we watch for some of the more than one hundred species of native birds. -
Area Changes of Glaciers on Active Volcanoes in Latin America Between 1986 and 2015 Observed from Multi-Temporal Satellite Imagery
Journal of Glaciology (2019), 65(252) 542–556 doi: 10.1017/jog.2019.30 © The Author(s) 2019. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Area changes of glaciers on active volcanoes in Latin America between 1986 and 2015 observed from multi-temporal satellite imagery JOHANNES REINTHALER,1,2 FRANK PAUL,1 HUGO DELGADO GRANADOS,3 ANDRÉS RIVERA,2,4 CHRISTIAN HUGGEL1 1Department of Geography, University of Zurich, Zurich, Switzerland 2Centro de Estudios Científicos, Valdivia, Chile 3Instituto de Geofisica, Universidad Nacional Autónoma de México, Mexico City, Mexico 4Departamento de Geografía, Universidad de Chile, Chile Correspondence: Johannes Reinthaler <[email protected]> ABSTRACT. Glaciers on active volcanoes are subject to changes in both climate fluctuations and vol- canic activity. Whereas many studies analysed changes on individual volcanoes, this study presents for the first time a comparison of glacier changes on active volcanoes on a continental scale. Glacier areas were mapped for 59 volcanoes across Latin America around 1986, 1999 and 2015 using a semi- automated band ratio method combined with manual editing using satellite images from Landsat 4/5/ 7/8 and Sentinel-2. Area changes were compared with the Smithsonian volcano database to analyse pos- sible glacier–volcano interactions. Over the full period, the mapped area changed from 1399.3 ± 80 km2 − to 1016.1 ± 34 km2 (−383.2 km2)or−27.4% (−0.92% a 1) in relative terms. -
Park Guards in the Conservation of Protected Areas Angela Martin
park guards in the conservation of protected areas Angela Martin Parks in Peril, Innovations in Conservation Series, 2007 Park guards are the field staff in charge of the protection and security of natural resources in a protected area (Núñez, 2005). Depending on the specific character- istics of the protected area, they are also in charge of safeguarding cultural resources (PROARCA/APM, 2004). Without their presence, protected areas are more vul- nerable to the factors threatening their integrity. Park guards may be employed by government or civil society institutions, (using their own or donors’ resources), or work as volunteers. Support for park guards and their work is considered a key component for the Hugo Arnal strengthening of protected areas. This includes the provision of essential equipment for their operations, such as vehicles, radios and uniforms, as well as training. Accord- ing to a 1998 study done for the Parks in Peril (PiP) program, the most effective way to engage communities in management activities was to hire them as guards for the areas (Brandon et al, 1998). PiP has consequently promoted participatory processes in this issue... as a way of involving the community and encouraging local residents to become guides • General characteristics of park or park guards, on a paid or volunteer basis. Also, PiP encouraged government agen- guards cies to facilitate patrolling and training for park guards and transfer authority to local actors (Martin and Rieger, 2003). • Innovative strategies with park guards The purpose of this bulletin is to present general elements about the characteristics, - Community, indigenous and roles and responsibilities of the park guards in the protected areas, emphasizing some volunteer park guards innovative strategies from which lessons can be derived. -
Landing Helicoptero
New Helicopter Tours Watch Video GENERAL DESCRIPTION Flying over the Avenue of the Volcanoes from the comfort and vantage point of a state-of-the-art helicopter is a once in a lifetime experience for all those seeking a luxurious rush. You’ll have the city of Quito under your feet and impressive views all around that showcase the wide variety of Ecuadorian landscapes. Mountains, rivers and waterfalls all come into view for excellent photo opportunities and an unforgettable memory, creating an experience that can only be compared to the wonder seen in epic movies. Ask about prices, additional fees, medical restrictions and the best times to make this exclusive activity a reality. And don’t forget to bring your camera and adventurous spirit along! SEAT CONFIGURATION ROUTES Route 1 Route 2 Route 3 Route 4 Quito ROUTE 1: TAMBILLO, WATERFALLS, COTOPAXI, RUMIÑAHUI Get familiar with some of Ecuador’s most beautiful views while flying up high on this brief but wholly satisfying ride. Flight time: 35 minutes Flight distance: ≈ 71 km (44 mi) ROUTE 2: TAMBILLO, WATERFALLS, COTOPAXI, RUMIÑAHUI, MACHACHI Fly over the outskirts of Quito and admire its fertile farmlands surrounded by rocky mountains gorgeous waterfalls, and majestic volcanoes. Flight time: 39 minutes Flight distance: ≈ 82 km (50 mi) ROUTE 3: TAMBILLO, ANTISANA, COTOPAXI, RUMIÑAHUI, MACHACHI A flight along Quito’s perimeter brings us face-to-face with the Andes’ most impressive features, from snow-capped volcanoes to gigantic mountains that many adventurers explore on weekends. Flight time: 56 minutes Flight distance: ≈ 123 km (76 mi) ROUTE 4: TAMBILLO, MACHACHI, RUMIÑAHUI, COTOPAXI, ANTISANA, CAYAMBE, QUITO An expansive journey that goes as far as the Middle of the World allows us to experience a wide variety of spectacular landscapes and scenery that surround the capital. -
Ccotopaxi & Chimborazo
Ccotopaxi & chimborazo - the ring of fire trek 13 days of pure adventure which includes reaching the summits of 4 of Ecuador’s highest volcanoes. Your go to high altitude experts from Everest to Kili and all the adventures inbetween What's inside? About the Ring of Fire Expedition 3 Why trek with EverTrek? 4 What’s included? 7 What to expect on the trek 8 Best time to go 9 How fit do I need to be? 10 Your itinerary 11 Equipment list 23 Chat to our Yetis 25 2 about cotopaxi and chimbarazo The Cotopaxi and Chimbarazo - Ring of Fire trek takes you through the ‘Avenue of Volcanoes’ as it’s called locally. It’s 13 days of awesome adventure which includes reaching the summits of 4 of Ecuador’s highest volcanoes, Imbabura (4560m), Cayambe (5790m) Cotopaxi (5897m) and finally the mighty Chimborazo (6268m). This is a true South American adventure offering you full immersion into the sights and sounds of Ecuador as well as experiencing altitude in one of the world’s most beautiful mountain ranges. 3 Why trek with eveRtrek? Are the mountains calling you again? EverTrek are the UK’s leading specialists in hardcore high altitude trekking. Why our customers think we’re awesome? We spend more time on preparing our EverTrekkers and truly believe they are the best prepared trekkers on the mountain with a success rate of over 95% (industry standard 65%). You get a personalised trip planner which will be your trekking bible for both before and during the trek to help prepare you practically, mentally & physically. -
Ecuador, Costa: Guayaquil Tour PE Guayaquil Airport
Mary Murphy Slide Collection Slide Continent Country, State: Locale Collection Description Date Number Editor's Note South America Ecuador, Costa: Guayaquil Tour PE Guayaquil airport. Nov. 15, 1996 PE-541 South America Ecuador, Costa: Guayaquil Tour PE Guayaquil from the plane. Nov. 15, 1996 PE-542 South America Ecuador, Costa: Guayaquil Tour PE Guayaquil from the plane. Nov. 18, 1996 PE-715 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-722 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-725 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-726 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-727 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-728 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-729 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-730 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-731 South America Ecuador, Costa: Guayaquil Tour PE Cathedral from the hotel. Nov. 20, 1996 PE-732 South America Ecuador, Costa: Guayaquil Tour PE Guayaquil from the plane. Nov. 20, 1996 PE-733 South America Ecuador, Insular: Galápagos Islands Tour PE [Map of Galápagos Islands.] No date. PE-0b No provenance. Copyright Restricted. South America Ecuador, Insular: Galápagos Islands Tour PE Galápagos Islands from the plane. Nov. 15, 1996 PE-543 South America Ecuador, Insular: Galápagos Islands Tour PE Galápagos Islands from the boat. -
089 Sarmiento 2002 Treeline.Pdf
ANTHROPOGENIC CHANGE IN THE LANDSCAPES OF HIGHLAND ECUADOR* FAUSTO 0. SARMIENTO ABSTRACT. The anthropogenii nature of Andean ecosystems is discussed in the framework of tree-line dynamics in selected sites in Ecuador. Indicators of human impact are evidence of the need for a scientific understanding of neotropical mountains that is better in tune with the special conditions of tropical Andean environments. Tropandean systems are neither tropical ecosystems nor midlatitude regions, and lessons from ecologically damaging activi- ties in those ecosystems cannot be transferred readily to Tropandean systems. Better research from the ethnobiological and ecological fronts is needed if we are to comprehend the intri- cate functions of neotropical mountains, particularly the cloud-forest belt, which is regarded as the most threatened ecosystem when considering sustainability scenarios. Keywords: Andes Mountains, Ecuador, geoecology, paramos, tree-line change, tropical montane cloudforest. %istory-geological, archaeological, and agricultural-is a necessary main frame- work when delimiting the edge of the Tropandean ecoregion, or tropical montane cloud forest ( TMCF). Landscape-level conservation planning must then acknowl- edge humans as the catalyst of landscape change. Today’s TMCF landscape in fact reflects two tree lines: an upper one that correlates with the extension of grazing into the colder, higher reaches, which reduces the area of TMCFS from above; and a lower one that correlates with the ascending intensification of cropland agriculture