DOCSLIB.ORG

Hotel Rio Serrano Excursions

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Hotel Rio Serrano Excursions Aonikenk The Aonikenks or Tehuelches were expert nomads and hunters who inhabited Patagonia. They hunted mainly the guanaco and the ñandu using the bow, the arrow and the spear. Come and discover ancient vestiges of the first humans that challenged the inclement patagonia. Initial altitude: 70 m.a.s.l Maximum altitude: 350 m.a.s.l Duration Difficulty 2,5 hrs. Medium Once we depart from the hotel it will take us about an We will continue the walk, this time with a view of hour to get to the beginning of the trail, which does not Sarmiento Lake, the trail will end at Portería Sarmiento represent a major difficulty, or large slopes, it is highly and then we'll return to the hotel. During the walk it is recommended if you are looking for a quiet walk. possible to observe guanacos, foxes and various species We will be reaching the highest point of the trail which of birds as well as typical landscapes of the Patagonian is at the base of conglomerate rocks. Here we will find pampas. some cave paintings that are more than 4,000 years old, made by the natives who inhabited the area. The place invites us to imagine what life was like for these men and women in the past and how they lived in Includes: perfect harmony with the environment. Snacks (Cereal bar, dried fruits, chocolate) Beverages ALTITUDE N 800 A 600 400 B 200 A Start / Finish B Portería Sarmiento 0 0 km 1,57 km 3,15 km 4,75 km 6,3 km DISTANCE [email protected] - www.rioserrano.com (+56 61) 224 05 28 / (+56 61) 222 08 78 / (+56 61) 222 41 81 Base of the Torres One of the most demanding excursions and part of the famous W circuit of the Paine massif. We move towards the northeast of the Torres del Paine National Park until we reach Estancia Cerro Paine. Initial altitude: 120 m.a.s.l Maximum altitude: 875 m.a.s.l Duration Difficulty 9-12 hrs. High We will start walking slowly and after crossing the stretch of the day as we will ascend 300 meters in the last Ascencio River, we’ll ascent continuously for about 2.5 kilometer of the trail, in a land dominated by loose stones Km by one of the shoulders from Monte Almirante and rock steps. Nieto (2,600 masl) until reaching the pass of the winds After an hour walking, the effort is rewarded with the (at 480 masl) from where we will enjoy a beautiful pano- most famous postcard of the Park: The Torres del Paine ramic view of the valley, then descend through the and its peri-glacial lagoon of spectacular turquoise color; Ascencio Valley until we reach our first stop at Refugio scene that makes Torres del Paine Park worthy of the title el Chileno, once we’re there, we’ll have already com- "Eighth Wonder of the World". pleted half of the trail. Throughout the trail it is possible to observe local fauna, From this point, we’ll gradually continue ascending, mainly birds such as the condor, eagles and carancho and this time surrounded by an incredible Lenga forest and if we are lucky, we will also see mammals such as the glacier slopes, until we reach the last flat sector, where Huemul, which makes this excursion an unique and unfor- we will find ourselves above 550 masl, before starting gettable experience when visiting the park. the ascent through the Torres Glacier moraine, which is perhaps the most demanding Includes: Snacks (Cereal bar, dried fruits, chocolate) Beverages Box Lunch ALTITUDE N 800 B 600 400 A 200 A Welcome center B Base of the Torres 0 0 km 5,5 km 11 km 16,5 km 22 km DISTANCE [email protected] - www.rioserrano.com (+56 61) 224 05 28 / (+56 61) 222 08 78 / (+56 61) 222 41 81 Cordon Chacabuco Patagonia is synonymous with peace and immensity in all its territory and this mountain range represents an unbeatable option to experience both sensations in this remote land. Initial altitude: 30 m.a.s.l Maximum altitude: 700 m.a.s.l Duration Difficulty 9-10 hrs. High When leaving from our hotel we will go to the This is probably one of the most interesting trails we offer, south-west of Villa Serrano to enter the first section of and although physically demanding because of the the path, surrounded by the Magellanic forest while the distance traveled, it is an excellent option to enjoy a day ascent begins slowly. From the height we will have a in the forests of Patagonia. panoramic view of the village and the magallanic steppe that is at the base of the Paine massif, after this view we will enter again in the forest to only leave the vegetation once near the end of our activity, when we are 500 meters above sea level we will be above the Includes: treetops and here us where we’ll appreciate the snowy Snacks (Cereal bar, dried fruits, chocolate) peaks and glaciers of the area that surround this Beverages unknown but impressive place, as well as the great Box Lunch fjord of Ultima Esperanza, which is lost behind the mountains. ALTITUDE N 800 A 600 400 B 200 A Rio Serrano Hotel B Chacabuco outlook 0 0 km 6,35 km 12,7 km 19,05 km 25,4 km DISTANCE [email protected] - www.rioserrano.com (+56 61) 224 05 28 / (+56 61) 222 08 78 / (+56 61) 222 41 81 Chorillo Pingo Walking through the edge of Pingo River, this valley will offer us in all its extension multiple attractions, new views of the Paine Massif and one of the most humid and green areas of the park, surrounded by interesting flora where we will distinguish the characteristic forests of Nothofagus. Initial altitude: 50 m.a.s.l Maximum altitude: 120 m.a.s.l Duration Difficulty 4 hrs. Low The trek starts at Guardería Grey, from where we will During the walk we will be able to spot the massif, specifi- slowly enter the Pingo Valley walking through the cly the Paine Grande, and the Cuernos del Paine, from edge of Pingo River; After crossing the valley, we will its west side. We will see a variety of birds and vegetation go into one of the oldest forests in the Park, where no typical of the western sector and if we are lucky enough fire has been present. we might even spot the king mammal of the park: the We'll walk through Magellanic forest, surrounded by its huemul. colors and aromas that will accompany us during our journey. Most of the trail is flat, with small slopes and is known to be one of the most humid places in the park, so do not be surprised if we walk on muddy terrain. We will finish the hike after two and a half hours, once we Includes: reach a small stream of water known as "Chorrillo de Snacks (Cereal bar, dried fruits, chocolate) los Salmones" located in the middle of large trees and Beverages rocks. For the return, we'll use the same path. ALTITUDE N 800 600 B 400 A 200 A Guardería Grey B Chorillo Pingo 0 0 km 2,25 km 4,45 km 6,7 km 8,9 km DISTANCE [email protected] - www.rioserrano.com (+56 61) 224 05 28 / (+56 61) 222 08 78 / (+56 61) 222 41 81 Condor Viewpoint An unforgettable walk inside the park, takes us to one of the best viewpoints of Pehoe Lake and the Paine Massif. Initial altitude: 70 m.a.s.l Maximum altitude: 350 m.a.s.l Duration Difficulty 2,5 hrs. Medium To reach this viewpoint we must face a short but com- From here we will have a panoramic view of Pehoe Lake plicated climb of 250 meters and be prepared to hike with its memorable waters and also the Paine Massif. uphill on stony terrain and experience the strong winds During the tour, it is possible to spot birds such as the of Patagonia. condor and the eagles. Without doubt an unforgettable We will start the trail for two kilometers ascending from experience. Camping Pehoe located on the shores of the Lake until we reach the first flat terrain located about 100 meters above the beginning of the day, here we can take a short break while admiring the view of the place . This colorfull lake reveals to us in its full extension, then Includes: we will pass through a wind channel since it is the low Snacks (Cereal bar, dried fruits, chocolate) point between two mountains, which generates that Beverages the winds increase when being under pressure by space reduction, after this part we’ll be reaching the summit of the viewpoint. ALTITUDE N B 800 600 400 A 200 A Pehoe Camping B Finish 0 0 km 1,12 km 2,25 km 3,37 km 4,5 km DISTANCE [email protected] - www.rioserrano.com (+56 61) 224 05 28 / (+56 61) 222 08 78 / (+56 61) 222 41 81 Pingo Waterfall The trail begins at 60 m.a.s.l. in the Guarderia Grey. Through a flat trail and an open landscape we will travel along the Pingo River where we’ll find the greenest forest of the region. Initial altitude: 60 m.a.s.l Maximum altitude: 191 m.a.s.l Duration Difficulty 8 hrs. High This excursion is highly recommended for those who From this point, we will walk towards Pingo Waterfall, love the forests and the nature in its purest state, Pingo going through valleys and some areas with steep slopes is one of the places inside the Park that have few or non and mud, which will make this full-day excursion a physi- human intervation, becouse of that the entrance to the cally demanding challenge, so it is important to have the trail is restricted to visitors, except for those who are right equipment to face this trek.
Load more

Recommended publications
  • Ecoadventures Patagonia Tours Paine National Park Hosteria Las
    EcoAdventures Patagonia Tours Paine National Park Hosteria Las Torres 2018-2019 For booking and more information call toll free: 1-800-325-5026 email: [email protected] or visit: www.ecoadventures.com/hotels/torresdelpainehotel.php www.ecoadventures.com | 1 Torres del Paine National Park Región de Magallanes y la Antártica Chilena Phone: +56(61)2617450 - +56(61)2360280 Las Torres Patagonia it´s found in the heart of Torres del Paine National Park. With 85 charmed rooms, restaurant, bar-lounge, conference center, spa-boutique, agro-tourism, 150 horses and Hotel Las Torres invites you to enjoy an unforgettable experience national park Torres del Paine. untamed Patagonia without any concerns just to enjoy the freedom of our pampas and observe the beauty of the mountains www.ecoadventures.com | 2 PROGRAM RATES USD Validity: September 15th, 2018 until April 30th, 2019 Low Season High Season Sept. - Oct. 2018 / Apr. 2019 Nov. Dec. 2018/ Jan. Feb.- Mar 2019 Noches Nights View Sgl Dbl Tpl Chd Sgl Dbl Tpl Chd Mountain 1.940 1.430 1.240 710 2.120 1.550 1.370 780 2 noches 2 Garden 1.815 1.300 1.110 650 1.920 1.410 1.230 710 Montaña 2.650 1.940 1.690 970 2.890 2.180 1.920 1.090 3 noches 3 Jardín 2.470 1.770 1.510 885 2.695 1.980 1.730 990 Montaña 3.220 2.370 1.920 1.185 3.520 2.660 2.200 1.330 4 noches 4 Jardín 2.990 2.140 1.690 1.070 3.260 2.400 1.940 1.200 Montaña 4.030 2.960 2.400 1.480 4.400 3.320 2.760 1.660 5 noches 5 Jardín 3.740 2.670 2.110 1.340 4.080 3.000 2.430 1.500 Montaña 4.590 3.375 2.730 1.690 5..020 3.790 3.140 1.895 6 noches 6 Jardín 4.260 3.045 2.400 1.520 4.650 3.420 2.770 1.710 Montaña 5.360 3.935 3.190 1.970 5.850 4.420 3.660 2.210 7 noches 7 Jardín 4.970 3.550 2.800 1.780 5.420 3.990 3.230 1.990 *Rack rate per person in US dollar* PROGRAM INCLUDES • Transfer IN/OUT from Punta Arenas, Puerto Natales and Calafate.
    [Show full text]
  • Variations of Patagonian Glaciers, South America, Utilizing RADARSAT Images
    Variations of Patagonian Glaciers, South America, utilizing RADARSAT Images Masamu Aniya Institute of Geoscience, University of Tsukuba, Ibaraki, 305-8571 Japan Phone: +81-298-53-4309, Fax: +81-298-53-4746, e-mail: [email protected] Renji Naruse Institute of Low Temperature Sciences, Hokkaido University, Sapporo, 060-0819 Japan, Phone: +81-11-706-5486, Fax: +81-11-706-7142, e-mail: [email protected] Gino Casassa Institute of Patagonia, University of Magallanes, Avenida Bulness 01855, Casilla 113-D, Punta Arenas, Chile, Phone: +56-61-207179, Fax: +56-61-219276, e-mail: [email protected] and Andres Rivera Department of Geography, University of Chile, Marcoleta 250, Casilla 338, Santiago, Chile, Phone: +56-2-6783032, Fax: +56-2-2229522, e-mail: [email protected] Abstract Combining RADARSAT images (1997) with either Landsat MSS (1987 for NPI) or TM (1986 for SPI), variations of major glaciers of the Northern Patagonia Icefield (NPI, 4200 km2) and of the Southern Patagonia Icefield (SPI, 13,000 km2) were studied. Of the five NPI glaciers studied, San Rafael Glacier showed a net advance, while other glaciers, San Quintin, Steffen, Colonia and Nef retreated during the same period. With additional data of JERS-1 images (1994), different patterns of variations for periods of 1986-94 and 1994-97 are recognized. Of the seven SPI glaciers studied, Pio XI Glacier, the largest in South America, showed a net advance, gaining a total area of 5.66 km2. Two RADARSAT images taken in January and April 1997 revealed a surge-like very rapid glacier advance.
    [Show full text]
  • Remote Sensing Study of Glacial Change in the Northern Patagonian Icefield
    Advances in Remote Sensing, 2015, 4, 270-279 Published Online December 2015 in SciRes. http://www.scirp.org/journal/ars http://dx.doi.org/10.4236/ars.2015.44022 Remote Sensing Study of Glacial Change in the Northern Patagonian Icefield Lucy Dixon, Shrinidhi Ambinakudige Department of Geosciences, Mississippi State University, Starkville, MS, USA Received 23 October 2015; accepted 27 November 2015; published 30 November 2015 Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract The Patagonian Icefield has the largest temperate ice mass in the southern hemisphere. Using re- mote sensing techniques, this study analyzed multi-decadal glacial retreat and expansion of glaci- er lakes in Northern Patagonia. Glacial boundaries and glacier lake boundaries for 1979, 1985, 2000, and 2013 were delineated from Chilean topographic maps and Landsat satellite images. As- ter stereo images were used to measure mass balance from 2007 to 2012. The highest retreat was observed in San Quintin glacier. The area of glacier lakes increased from 13.49 km2 in 1979 to 65.06 km2 in 2013. Four new glacier lakes formed between 1979 and 2013. Between 2007 and 2012, significant glacial thinning was observed in major glaciers, including HPN1, Pared Norte, Strindberg, Acodado, Nef, San Quintin, Colonia, HPN4, and Benito glaciers. Generally, ablation zones lost more mass than accumulation zones. Keywords Patagonia, Glaciers, South America, ASTER 1. Introduction Glaciers are key indicators for assessing climate change [1]-[3]. Beginning in the nineteenth century, glaciers in many parts of the world retreated significantly, which was a clear indicator of climate warming [3]-[7].
    [Show full text]
  • 168 2Nd Issue 2015
    ISSN 0019–1043 Ice News Bulletin of the International Glaciological Society Number 168 2nd Issue 2015 Contents 2 From the Editor 25 Annals of Glaciology 56(70) 5 Recent work 25 Annals of Glaciology 57(71) 5 Chile 26 Annals of Glaciology 57(72) 5 National projects 27 Report from the New Zealand Branch 9 Northern Chile Annual Workshop, July 2015 11 Central Chile 29 Report from the Kathmandu Symposium, 13 Lake district (37–41° S) March 2015 14 Patagonia and Tierra del Fuego (41–56° S) 43 News 20 Antarctica International Glaciological Society seeks a 22 Abbreviations new Chief Editor and three new Associate 23 International Glaciological Society Chief Editors 23 Journal of Glaciology 45 Glaciological diary 25 Annals of Glaciology 56(69) 48 New members Cover picture: Khumbu Glacier, Nepal. Photograph by Morgan Gibson. EXCLUSION CLAUSE. While care is taken to provide accurate accounts and information in this Newsletter, neither the editor nor the International Glaciological Society undertakes any liability for omissions or errors. 1 From the Editor Dear IGS member It is now confirmed. The International Glacio­ be moving from using the EJ Press system to logical Society and Cambridge University a ScholarOne system (which is the one CUP Press (CUP) have joined in a partnership in uses). For a transition period, both online which CUP will take over the production and submission/review systems will run in parallel. publication of our two journals, the Journal Submissions will be two­tiered – of Glaciology and the Annals of Glaciology. ‘Papers’ and ‘Letters’. There will no longer This coincides with our journals becoming be a distinction made between ‘General’ fully Gold Open Access on 1 January 2016.
    [Show full text]
  • Torres Del Paine National Park R Biosphere Reserve (UNESCO, 1978) 2
    73°20' 73°10' 73°0' 72°50' A 615,000 B 620,000 C 625,000 D 630,000 E 635,000 F 640,000 G 645,000 H 650,000 I 655,000 J 660,000 D e la s C h in as R i ve 4,380,000 4,380,000 Torres del Paine National Park r Biosphere Reserve (UNESCO, 1978) 2 KEY Cubo Glacier A R G E N T I N A SERVICES Station or Gatehouse 4,375,000 4,375,000 Tourist Information Health Center (high season) Police (high season) 3 Bus Stop Dickson Glacier Restrooms 2 de Enero Ranch Radio Phone Hotel 1,000 4,370,000 4,370,000 During low season, Jara trekking is only allowed between Escondida Pond Pond Lodge 4 campsites Serón and Pass, . 3 with an authorized guide 500 k Camping area 1,000 m - 500 1,500 2 h Campsite 556 4 500 50°50' Restaurant Cafeteria Stokes Pond 6 .5 Store 271 k m 5 h Dickson 3. - - Paine Lake 2 km 50°50' ATTRACTIONS 4 2 h h 4.5 Lake k 1 3 SOUTHERN ICE FIELDS ICE SOUTHERN - 1005 Olvidado Glacier Quemado m km Las Chinas - DE LA PALOMA .5 Lake 2 8 From Cebolla Lake to the west, the trail Waterfalls Viewpoint h WETLANDS Ohnet Glacier 358 is only authorized for horseback rides 4,365,000 4,365,000 Waterfalls er Pa iv 1645 ine R Cebolla 9 D Trekking k e m l Lake - 4 a Coirón Station h s h C Trekking on ice 1 Azul Pond h - i m Serón 5 h n k h a Escondido 3 6 s Horseback rides Co.
    [Show full text]
  • Surface Energy Fluxes on Chilean Glaciers
    The Cryosphere, 14, 2545–2565, 2020 https://doi.org/10.5194/tc-14-2545-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Surface energy fluxes on Chilean glaciers: measurements and models Marius Schaefer1, Duilio Fonseca-Gallardo1, David Farías-Barahona2, and Gino Casassa3,4 1Instituto de Ciencias Físicas y Matemáticas, Facultad de Ciencias, Austral University of Chile, Valdivia, Chile 2Institut für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, Germany 3Dirección General de Aguas, Ministerio de Obras Públicas, Santiago, Chile 4Centro de Investigación Gaia Antártica, Universidad de Magallanes, Punta Arenas, Chile Correspondence: Marius Schaefer ([email protected]) Received: 12 March 2019 – Discussion started: 13 June 2019 Revised: 15 May 2020 – Accepted: 14 June 2020 – Published: 10 August 2020 Abstract. The surface energy fluxes of glaciers determine 1 Introduction surface melt, and their adequate parametrization is one of the keys to a successful prediction of future glacier mass balance Glaciers are retreating and thinning in nearly all parts of and freshwater discharge. Chile hosts glaciers in a large range the planet, and it is expected that these processes are go- of latitudes under contrasting climatic settings: from 18◦ S ing to continue under the projections of global warming in the Atacama Desert to 55◦ S on Tierra del Fuego. Using (IPCC, 2019). For mountain glaciers melt is mostly deter- three different methods, we computed surface energy fluxes mined by the energy exchange with the atmosphere at their for five glaciers which represent the main glaciological zones surfaces. The processes leading to this exchange of energy of Chile.
    [Show full text]
  • Ecoadventures Patagonia Tours Paine National Park Tierra
    EcoAdventures Patagonia Tours Paine National Park Tierra Patagonia Hotel 2018-2019 For booking and more information call toll free: 1-800-325-5026 email: [email protected] or visit: www.ecoadventures.com/hotels/tierrapatagoniahotel.php www.ecoadventures.com | 1 Tierra Patagonia is brother hotel to Tierra Atacama and Ski Portillo and its opening was late 2011. Located by the shore of Lake Sarmiento in the north-east border of Torres del Paine National Park, in southern Chile. The hotel boasts a privileged sight to the Paine Massif, its characteristic Horns and its granite towers www.ecoadventures.com | 2 DESIGN AND INSTALLATIONS The architecture and design of the hotel shows the warm and comfortable ambiance of Patagonia. Large Windows give an excellent view from every corner of the common areas and the 40 rooms. The hotel facilities includes living room, bar, dining room, excursions room, library, TV room, indoor pool, outdoor Jacuzzi and Uma Spa. ROOMS Tierra Patagonia has 3 suites, 37 double rooms and 6 family apartments, each one with a wonderful sight of Lake Sarmiento and the mountains of the Paine Massif. The suites have a living room on the upper part and down the stairs you will find the bedroom with restroom, which measures 51 m2. The size of the double rooms is of 36 m2. The apartments measures 72 m2, each has 2 rooms and 2 restrooms and has room for 4 to 6 guests. Every room has a hair dryer, safe and heating. MEALS AND WINES The Chef at Tierra Patagonia makes the most of the local products; seafood from the Magellan Strait, lamb and meats from the neighbouring ranches and Calafate for making hearty delicious meals.
    [Show full text]
  • Brochure, and to Bring This Equipment to the Trip
    Index Our Company Kayak en Patagonia was born more than a decade ago, originally conceived by a group of friends and guides that were born and raised on the shores of the Señoret Channel. Their dream was to explore and navigate the hidden secrets that only locals knew and to show their beauty and wonders to the people that visit this region. Today, after the many unforgettable experiences that we have shared paddling with people from all over the world, we want to welcome you to Patagonia, a true paradise for Kayaking adventures. In Kayak en Patagonia, we want to give you a “Travel experience”. We work with the best quality of gear, equipment and food on each of our trips. Our certified guides have the knowledge and qualification that is needed to provide you a safe, fun and unique experience. 3 Grey Our Icebergs & River (1 day) Trips RiverSerrano & Glacier (2 days) Grey & Serrano Icebergs, Rivers & Glaciers (3 days) 4 Physical Levels: Easy Moderate Challenging Accessible to all people in good Accessible to all those in good Suites those that are physically health, paddle from 1 -2 hours health, who are doing some sport active and have some background per day. regularly, 3-5 hours of paddling in sea kayak. 6-8 hours of per day. paddling per day. 5 Level 1 Kayaking Location: semi-protected waterway with access to shore. (Lakes and rivers with moderate current) Distance per day: 10 to 20 miles Levels: Wind: 10 to 25 knots Recommended Paddle Skills: Previous kayaking experience, forward stroke, reverse stroke Level 2 Location: semi-protected waterway with access to shore.
    [Show full text]
  • Landscapes of Torres Del Paine Park and Surrounding Area
    Landscapes of Torres del Paine Park and surrounding area PATAGONIA Luis Bertea Rojas EXPLORATION CRUISE TO THE REMOTE REGIONS OF TIERRA DEL FUEGO AND STRAIT OF MAGELLAN EXCLUSIVE PHOTO EXPEDITION AND NATURE CRUISE A BOARD THE M/V FORREST [email protected] EXPEDITION CRUISE www.patagoniaphotosafaris.com PHOTOGRAPHY, CIENce & EDUCATION www.expedicionfitzroy.com PATAGONIA Landscapes of Torres del Paine Park and surrounding area Editor / Publisher - Luis Bertea Fotografías y diseño / Photographs & design - Luis Bertea Textos / Text - Andrea Espinoza Traducción / Translation - Sara Anderson Impresión / Printed by - B&B Impresores Editorial Patagonia Interactiva Chiloe 1667 Punta Arenas, Chile - Fono / Phone 56-61 226653 www.patagoniainteractiva.com - [email protected] Primera Edición bilingue, Español - Inglés de 5000 ejemplares - Punta Arenas, Patagonia, Chile, Noviembre de 2006 First bilingual edition, Spanish - English, 5000 copies - Punta Arenas, Patagonia, Chile, November 2006 ISBN 956-7820-08-2 Inscripción Nº / Registration Nº 157.726 - © 2006 Luis Bertea Rojas Derechos reservados de los textos y fotografías - All rights reserved for text and photographs Prohibida su Total o Parcial Reproducción - Partial or Total Reproduction is Prohibited Landscapes of Torres del Paine Park and surrounding area PATAGONIA Luis Bertea Rojas Rutas, Huellas y Recuerdos de la Patagonia Trails, Tracks and Memories of Patagonia Todo lo que rodea a La Patagonia tiene un toque misterioso, tanto Everything surrounding Patagonia has a touch of mystery, so much so es así, que hasta el origen de su nombre se ha relacionado durante that even the origin of its name is considered an enigma. For centuries siglos al gran tamaño que –supuestamente- caracterizaba los pies de the origin was allegedly related to the great size of the feet of the los indígenas que habitaban la zona.
    [Show full text]
  • Glacier Clusters Identification Across Chilean Andes Using Topo-Climatic
    119 Glacier Clusters identification across Chilean Andes using Topo-Climatic variables Identificación de clústeres glaciares a lo largo de los Andes chilenos usando variables topoclimáticas Historial del artículo Alexis Caroa; Fernando Gimenob; Antoine Rabatela; Thomas Condoma; Recibido: Jean Carlos Ruizc 15 de octubre de 2020 Revisado a Université Grenoble Alpes, CNRS, IRD, Grenoble-INP, Institut des Géosciences de l’Environnement (UMR 5001), 30 de octubre de 2020 Grenoble, France. Aceptado: b Department of Environmental Science and Renewable Natural Resources, University of Chile, Santiago, Chile. 05 de noviembre de 2020 c Sorbonne Université, Paris, France. Keywords Abstract Chilean Andes, climatology, Using topographic and climatic variables, we present glacier clusters in the Chilean Andes (17.6-55.4°S), where the glacier clusters, topography Partitioning Around Medoids (PAM) unsupervised machine learning algorithm was utilized. The results classified 23,974 glaciers inside thirteen clusters, which show specific conditions in terms of annual and monthly amounts of precipitation, temperature, and solar radiation. In the Dry Andes, the mean annual values of the five glacier clusters (C1-C5) display precipitation and temperature difference until 400 mm (29 and 33°S) and 8°C (33°S), with mean elevation contrast of 1800 m between glaciers in C1 and C5 clusters (18 to 34°S). While in the Wet Andes the highest differences were observed at the Southern Patagonia Icefield latitude (50°S), were the mean annual values for precipitation and temperature show maritime precipitation above 3700 mm/yr (C12), where the wet Western air plays a key role, and below 1000 mm/yr in the east of Southern Patagonia Icefield (C10), with differences temperature near of 4°C and mean elevation contrast of 500 m.
    [Show full text]
  • Currentknowledgeofthe
    CURRENTKNOWLEDGEOFTHESOUTHERN PATAGONIA ICEFIELD Gino Casassa':", Andrés Rivera':', Masamu Aniya', and Renji Naruse" 1. ABSTRACT We present here a review of the current glaciological knowledge of the Southern Patagonia Icefield (SPI). With an area of 13,000 km2 and 48 major glaciers, the SPI is the largest ice mass in the Southern Hemisphere outside of Antarctica. The glacier inventory and recent glacier variations are presented, as well as ice thickness data and its variations, ice velocity, ablation, accumulation, hydrological characteristics, climate changes and implications for sea level rise. Most ofthe glaciers have been retreating, with a few in a state of equilibrium and advance. Glacier retreat is interpreted primarily as a response to regional atmospheric warrning and to a lesser extent, to precipitation decrease observed during the last century in this region. The general retreat of SPI has resulted in an estimated contribution of 6% to the global rise in sea level due to melting of small glaciers and ice caps. Many glaciological characteristics of the SPI, in particular its mass balance, need to be determined more precisely. 2. INTRODUCTION The Southern Patagonia Icefield (SPI) extends north-south for 370 km, between 48°15' S and 51°35' S, at an average longitude of73°30' W (Figure 1). Its mean width is 35 km, and the minimum width is 9 km. The first detailed glacier inventory was compiled by Aniya el al. (1996), who showed that the SPI is composed of 48 major outlet glaciers and over 100 small cirque and valley glaciers. These glaciers flow frorn the Patagonian Andes to the east and west, generally terminating with calving fronts in freshwater lakes (east) and Pacific Ocean fjords (west).
    [Show full text]
  • Universidad De Chile Facultad De Ciencias Físicas Y Matemáticas Departamento De Geología
    UNIVERSIDAD DE CHILE FACULTAD DE CIENCIAS FÍSICAS Y MATEMÁTICAS DEPARTAMENTO DE GEOLOGÍA PALEO-TERMOMETRÍA Y EVOLUCIÓN DEL SISTEMA HIDROLÓGICO DEL PARQUE NACIONAL TORRES DEL PAINE, PATAGONIA. TESIS PARA OPTAR AL GRADO DE DOCTOR EN CIENCIAS MENCIÓN GEOLOGÍA MARCELO ALBERTO SOLARI CORVALAN PROFESOR GUÍA: FRANCISCO HERVE ALLAMAND MIEMBROS DE LA COMISION: GABRIEL VARGAS EASTON JACOBUS LE ROUX ALCIDES NOBREGA SIAL CLAUDIO LATORRE HIDALGO SANTIAGO DE CHILE NOVIEMBRE 2010 Resumen de la Tesis para optar al grado de Doctor en Ciencias Mención Geología. Por: Marcelo Alberto Solari Corvalán. Fecha de Examen: 05-11-2010 Prof. Guía Sr. Francisco Herve PALEO-TERMOMETRÍA Y EVOLUCIÓN DEL SISTEMA HIDROLÓGICO DEL PARQUE NACIONAL TORRES DEL PAINE, PATAGONIA Un conjunto de complejos morrénicos se distribuyen desde el margen este de la Cuenca de Drenaje de Torres del Paine hasta las cercanías del margen actual de los Campos de Hielo Patagónicos. Regionalmente se reconocen en el paisaje un conjunto de terrazas lacustres vinculadas a las fluctuaciones glaciares. Las evidencias geomorfológicas y sedimentarias lacustres encontradas apoyan la existencia de un único lago proglacial denominado en el presente estudio como Gran Paleo-Lago Tehuelche (GPT), mejoran la cronología de los eventos glaciales y permiten una comprensión de la evolución del sistema hidrológico de Torres del Paine. Los avances glaciares previamente denominados por Marden (1993) como A, B y C, se desarrollaron durante el Último Máximo Glacial y alimentaron al GPT con aguas de fusión, permitiéndole al lago alcanzar su mayor extensión y altitud. El hallazgo de trombolitos en Laguna Amarga fue clave para determinar que el desagüe del GPT hacia el Seno de Última Esperanza se produjo hace 7110 años calibrados antes del presente (años cal AP) producto de la fusión de una gran barrera glacial existente durante el avance E, que posteriormente dio paso al complejo sistema hidrológico de ríos y lagos existente.
    [Show full text]