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Plant Diversity and Composition Changes Along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon
diversity Article Plant Diversity and Composition Changes along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon Pablo Lozano 1,*, Omar Cabrera 2 , Gwendolyn Peyre 3 , Antoine Cleef 4 and Theofilos Toulkeridis 5 1 1 Herbario ECUAMZ, Universidad Estatal Amazónica, Km 2 2 vía Puyo Tena, Paso Lateral, 160-150 Puyo, Ecuador 2 Dpto. de Ciencias Biológicas, Universidad Técnica Particular de Loja, San Cayetano Alto s/n, 110-104 Loja, Ecuador; [email protected] 3 Dpto. de Ingeniería Civil y Ambiental, Universidad de los Andes, Cra. 1E No. 19a-40, 111711 Bogotá, Colombia; [email protected] 4 IBED, Paleoecology & Landscape ecology, University of Amsterdam, Science Park 904, 1098 HX Amsterdam, The Netherlands; [email protected] 5 Universidad de las Fuerzas Armadas ESPE, Av. General Rumiñahui s/n, P.O.Box, 171-5-231B Sangolquí, Ecuador; [email protected] * Correspondence: [email protected]; Tel.: +593-961-162-250 Received: 29 April 2020; Accepted: 29 May 2020; Published: 8 June 2020 Abstract: The paramo is a unique and severely threatened ecosystem scattered in the high northern Andes of South America. However, several further, extra-Andean paramos exist, of which a particular case is situated on the active volcano Sumaco, in the northwestern Amazon Basin of Ecuador. We have set an elevational gradient of 600 m (3200–3800 m a.s.l.) and sampled a total of 21 vegetation plots, using the phytosociological method. All vascular plants encountered were typified by their taxonomy, life form and phytogeographic origin. In order to determine if plots may be ensembled into vegetation units and understand what the main environmental factors shaping this pattern are, a non-metric multidimensional scaling (NMDS) analysis was performed. -
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. -
New Distributional Bird Records from the Eastern Andean Slopes of Ecuador Istributio D
ISSN 1809-127X (online edition) © 2010 Check List and Authors Chec List Open Access | Freely available at www.checklist.org.br Journal of species lists and distribution N New distributional bird records from the eastern Andean slopes of Ecuador ISTRIBUTIO D 1,2,3* 4 RAPHIC G Alejandro Solano-Ugalde and Galo J. Real-Jibaja EO 1 G N O Fundación Imaymana, Paltapamba 476 San Pedro del Valle, Nayón. Quito, Ecuador. 2 Neblina Forest Natural History and Birding Tours, South America, Isla Floreana e8-129. Quito, Ecuador. 3 Natural History of Ecuador’s [email protected] Avifauna Group, 721 Foch y Amazonas. Quito, Ecuador. OTES 4 Real Nature, Travel Company, Casa Upano. Macas, Morona Santiago, Ecuador. N * Corresponding author. E-mail: Abstract: Distribution of birds is dynamic. Understanding, documentation and appropriate use of new records are essential, especially when managing threatened species. Here we present novel data regarding new distributional records for 17 bird species along the Amazonian slopes of the eastern Ecuadorian Andes. The new records fill gaps on our knowledge in the distribution, both in latitude and altitude. Although knowledge on the distribution of birds on mainland Ecuador has been well studied (Fjeldså Rostrhamus sociabilis ACCIPITRIDAE during recent years an inspiring number of articles have Snail Kite Cassin, 1854 - Two beenand Krabbe published 1990; documenting Ridgely and newGreenfield discoveries 2001; on2006), the individuals in juvenile plumage were seen flying over the distribution of birds in mainland Ecuador (e.g. Freile old-Zamora Airstrip on 6 March 2008, Zamora-Chinchipe et al. province (950 m a.s.l., 03°59’ S, 78°53’ W). -
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. -
The World Heritage Convention and the National Park Service: the First Two Decades, 1972–1992 Peter H
The World Heritage Convention and the National Park Service: The First Two Decades, 1972–1992 Peter H. Stott Introduction As recounted in the first essay of this three-part series,1 the Convention Concerning the Protection of the World Cultural and Natural Heritage (the “World Heritage Conven - tion”), was adopted by the United Nations Educational, Scientific, and Cultural Organiza - tion (UNESCO) in 1972. The United States, and the National Park Service (NPS) in partic- ular, had important roles in its development and in negotiations leading to its adoption. The NPS Office of International Affairs (OIA), which celebrated its 50th anniversary last year, participated in all phases of that development. This essay, published in the 40th anniversary year of the convention, recounts the US role in the first two decades of the convention’s exis- tence, culminating in its 20th anniversary session in 1992 in Santa Fe, New Mexico. The United States was the first nation to ratify the new convention, and when it came into force in 1975, the US was on its governing body, the World Heritage Committee, for all but four of the sixteen committee sessions in the period through 1992. The US played a key role in the convention’s development: in addition to hosting the session of the committee at which the first sites were inscribed on the World Heritage List, at subsequent sessions it was a vocal advocate for the more problematic issues that began to appear almost immediately: the integrity of the list and the conservation of sites already inscribed. David Hales, the US Committee chair at that 1978 session in Washington, voiced the dominant sentiment of the period: We viewed the Convention as—in many ways—a US initiative and an initiative that we want- ed to help parent early on and bring it up the right way; that we felt it should be incredibly objective and unimpeachable in its judgements; that it needed to rely on professional expert- ise, not consensual votes as often dominated in some other international institutions... -
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. -
Caracterización De Depósitos De Corriente De Densidad Piroclástica Asociados a La Caldera De Cuicocha, Norte De Los Andes Ecuatorianos
UNIVERSIDAD DE INVESTIGACIÓN DE TECNOLOGÍA EXPERIMENTAL YACHAY Escuela de Ciencias de la Tierra, Energía y Ambiente TÍTULO: CARACTERIZACIÓN DE DEPÓSITOS DE CORRIENTE DE DENSIDAD PIROCLÁSTICA ASOCIADOS A LA CALDERA DE CUICOCHA, NORTE DE LOS ANDES ECUATORIANOS. Trabajo de integración curricular presentado como requisito para la obtención del título de Geóloga Autor: Patricia Janeth Rengel Calvopiña Tutor: Ph. D. Almeida Gonzalez Rafael Urcuquí, Julio 2020 AUTORÍA Yo, Patricia Janeth Rengel Calvopiña, con cédula de identidad 1725202830, declaro que las ideas, juicios, valoraciones, interpretaciones, consultas bibliográficas, definiciones y conceptualizaciones expuestas en el presente trabajo; así cómo, los procedimientos y herramientas utilizadas en la investigación, son de absoluta responsabilidad de el/la autora (a) del trabajo de integración curricular. Así mismo, me acojo a los reglamentos internos de la Universidad de Investigación de Tecnología Experimental Yachay. Urcuquí, Julio 2020. ___________________________ Patricia Janeth Rengel Calvopiña CI: 1725202830 AUTORIZACIÓN DE PUBLICACIÓN Yo, Patricia Janeth Rengel Calvopiña, con cédula de identidad 1725202830, cedo a la Universidad de Tecnología Experimental Yachay, los derechos de publicación de la presente obra, sin que deba haber un reconocimiento económico por este concepto. Declaro además que el texto del presente trabajo de titulación no podrá ser cedido a ninguna empresa editorial para su publicación u otros fines, sin contar previamente con la autorización escrita de la Universidad. Asimismo, autorizo a la Universidad que realice la digitalización y publicación de este trabajo de integración curricular en el repositorio virtual, de conformidad a lo dispuesto en el Art. 144 de la Ley Orgánica de Educación Superior Urcuquí, Julio 2020. ___________________________ Patricia Janeth Rengel Calvopiña CI: 1725202830 “El mayor desafío que enfrentan nuestros países de cara al futuro como naciones con doscientos años de independencia es la educación. -
Tourism Perspectives in Baños, Ecuador, a Municipality of the Tungurahua Aspiring Geopark Project
Tourism perspectives in Baños, Ecuador, a municipality of the Tungurahua Aspiring Geopark project JASMINE CARDOZO MOREIRA1 AND PATRICIA ESTÉVEZ2 - 1. Department of Tourism, Ponta Grossa State University, Ponta Grossa, Brazil <[email protected]> ¶ 2. SEDPGYM, Quito, Ecuador Baños, located in the province of Tungurahua, in the center of Ecuador, between the Andes and the Ecuadorian Amazon, has tourism as an economic base. It is one of the entrance gates to the Sangay National Park, a world heritage site, which is home to the volcano Tungurahua (Throat of Fire in Quichua, the indigenous language). The volcano has been active since 1999 and frequently spits smoke and fire. Due to its topography and natural attractions, it is a premier destination for hiking, biking, rappel, canyoning, climbing, rafting, horseback riding, bridge jumping, kayaking, among others. There are many waterfalls and deep river gorges that can be crossed with “tarabitas”. Beyond ecotourism, the area receives visitors interested in health, religious, adventure and geological tourism. With a population of 20,000 inhabitants, it has several lodging options, restaurants, 49 local tour operators, and many spa’s and public pools with the hot water from the depths of Tungurahua volcano. Many of the tour operators offer tours that are conducted on vehicles called “chiva”, a kind of truck adapted to carry passengers. The city has great accessibility and culture connected with volcanism. The Basilica of the Virgin of the Holy Water was built with volcanic rock. The Geopark Project is already being promoted in the city on the map distributed to visitors and in a specific folder about the Project, which explains what a Geopark is, and its benefits to the community. -
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. -
The First Geopark in Ecuador: Imbabura
EDITORIAL - The First Geopark in Ecuador: Imbabura. EDITORIAL The First Geopark in Ecuador: Imbabura. Yaniel Misael Vázquez Taset and Andrea Belén Tonato Ñacato DOI. 10.21931/RB/2019.04.01.1 The UNESCO Global Geoparks are created in the nineties as Geoparks composed specific geographic areas that show particular a European regional initiative to respond the increasing need for and relevant geological features of our planet’s history (UNESCO enhancing and preserving the geological heritage of our planet 1, 4). In South America, and principally in the Andean zone, the evi- based on the geological record of determined areas. These geo- dence associated to the convergence and subduction of the Nazca 830 graphic sites are part of the evidence of the 4600 Ma of Earth’s Plate and South American Plate is well preserved. For this reason, evolution. This initiative is based on three essential pillars 2: pres- there is a wide variety of natural and geological attractions (rang- ervation, education and geo – tourism designed to reach the sus- es of different ages, valleys, volcanoes, geothermal systems, sed- tainable economic development based on the harnessing of the imentary basins, faults, rocks, minerals, fossils, etc.). The beauty geological heritage. These main thrusts are the guidelines to man- and the showiness of the region have motivated the launching of age Geoparks, and give the possibility to develop economic and various Geopark proposals, for example: Napo – Sumaco in the touristic activities which increase the economic income in com- Amazon Region, Península Santa Elena and Jama – Pedernales in munities. As a consequence, the settler’s life’s quality is positively the Coast, Galápagos in the Insular Region, and Volcán Tungura- affected.