353 a AAR. See Accumulation-Area Ratios (Aars) Ablation Losses
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Snowlake & Biafo Hispar La Trek
Snowlake & Biafo Hispar La Trek Trip Highlights Traverse of the Biafo & Hispar Glaciers in the Karakoram Mountains Walking on world’s longest Glacier Crossing of Hispar la 5000m Pass Beautiful Hunza Valley TRIP AT GLANCE 5-6 NIGHTS HOTELS , 14 NIGHTS CAMPING, 13-14 DAYS STRENUOUS TREKKING MAX. ALTITUDE – 5150M / 16,400FT Key Destinations:Islamabad-Skardu-Shigar-Braldu-Baltoro Glacier-Biafo Glacier-K2-Hispar Glacier- Hunza -Karakoram Highway TREK BACKGROUND The interconnected Biafo and Hispar glaciers, with a combined length of 120 kilometres, provide an unlikely natural highway that cuts through the heart of the Karakoram Range. Starting out from Askole on the approach to the Baltoro and K2, this long and relatively committing glacial traverse is undertaken annually by just a handful of expeditions. This trekking holiday does just that in a 3 week experience for budding explorers. Walking either on the glaciers themselves, or through flower-carpeted ablation valleys, we encounter challenging as well as more straightforward trekking conditions. A highlight of the trip is the camp on the Hispar La (5151m), where we can watch the afternoon shadow creeping across Snow Lake to the mighty Ogre (7285m) and turn to see the sun setting over the mountains of Hunza and the distant Hindu Kush to the west. Stunning scenery and a genuine sense of adventure in a high mountain wilderness are key attractions of this magnificent trekking holiday inh the karakoram. TREK OVERVIEW BEST TIME : MID-JUNE - MID-SEPTEMBER 2018 Date Day Activity Mode Time Height -
Identification of Glacial Flood Hazards in Karakoram Range Using Remote Sensing Technique and Risk Analysis
IDENTIFICATION OF GLACIAL FLOOD HAZARDS IN Arshad Ashraf*† , Rakhshan Roohi*, Rozina Naz* KARAKORAM RANGE USING REMOTE SENSING and Naveed Mustafa* TECHNIQUEAND RISK ANALYSIS ABSTRACT importance of this situation has magnified over the past decades due to increase in numbers of glacial Glacial Lake Outburst Floods (GLOFs) are great lakes that are formed at the glacier terminus. Thirty- hazard for the downstream communities in context of five destructive out-burst floods have been recorded changing climatic conditions in the glaciated region of for the Karakoram Range during the past two hundred Pakistan. The remote sensing data of Landsat ETM+ years (Hewitt, 1982). Some of the ice dams may have was utilized for the identification of glacial lakes been the result of glacier surges. There is susceptible to posing GLOF hazard in Karakoram unambiguous evidence of large reservoirs ponded by Range. Overall, 887 glacial lakes are identified in 18 glaciers. Kelly (1988) outlines the historical different river-basins of Karakoram Range, out of development and disappearance of Virjerab lake in which 16 lakes are characterized as potentially Hunza due to glacial motion. There occurred a series dangerous in terms of GLOF. The analysis of of GLOF events in upper Hunza valley, central community’s response to GLOF events of 2008 in the Karakoram Range, within short time periods during central Karakoram Range indicated gaps in 2008 that had a devastating effect on the nearby coordination and capacity of the local communities to communities (Roohi, Ashraf, Mustafa and Mustafa, cope with such natural hazards. A regular monitoring 2008). The people residing at considerable distances of hot spots and potential GLOF lakes along with downstream from the unstable lakes are facing a capacity-building of local communities and institutions serious threat to their lives and property. -
Local Topography Increasingly Influences the Mass Balance of A
Local topography increasingly influences the mass balance of a retreating cirque glacier Caitlyn Florentine1, 2, Joel Harper2, Daniel Fagre1, Johnnie Moore2, Erich Peitzsch1 1U.S. Geological Survey, Northern Rocky Mountain Science Center, West Glacier, Montana, 59936, USA 5 2Department of Geosciences, University of Montana, Missoula, Montana, 59801, USA Correspondence to: Caitlyn Florentine ([email protected]) Abstract. Local topographically driven processes, such as wind drifting, avalanching, and shading, are known to alter the relationship between the mass balance of small cirque glaciers and regional climate. Yet partitioning such local effects from regional climate influence has proven difficult, creating uncertainty in the climate representativeness of some glaciers. We 10 address this problem for Sperry Glacier in Glacier National Park, USA using field-measured surface mass balance, geodetic constraints on mass balance, and regional climate data recorded at a network of meteorological and snow stations. Geodetically derived mass changes between 1950-1960, 1960-2005, and 2005-2014 document average mass change rates during each period at -0.22±0.12 m w.e. yr-1, -0.18±0.05 m w.e. yr-1, and -0.10±0.03 m w.e. yr-1. A correlation of field- measured mass balance and regional climate variables closely (i.e. within 0.08 m w.e. yr-1) predicts the geodetically 15 measured mass loss from 2005-2014. However, this correlation overestimates glacier mass balance for 1950-1960 by +1.18±0.92 m w.e. yr-1. Our analysis suggests that local effects, not represented in regional climate variables, have become a more dominant driver of the net mass balance as the glacier lost 0.50 km2 and retreated further into its cirque. -
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 -
Characteristics of the Bergschrund of an Avalanche-Cone Glacier in the Canadian Rocky Mountains
JOlIl"lla/ o/G/aci%gl'. VoL 29. No. 10 1. 1983 CHARACTERISTICS OF THE BERGSCHRUND OF AN AVALANCHE-CONE GLACIER IN THE CANADIAN ROCKY MOUNTAINS By G ERALD OSBORN (Department of Geology and Geophysics, Uni versity o f Calgary, Calgary, Alberta T2N I N4, Canada) ABSTRACT. Fi eld study of th e bergschrund of a small avalanche-cone glacier at the base of Mt Chephren, in Banff Nati onal Park , has been ca rried out as part of a general ex pl oratory study of glacier-head crevasses in th e Canadi an Roc ki es. The bergsc hrun d consists of a wide. shall ow. partl y bedrock-fl oored gap, und erneath whi ch ex tends a nearl y vertical Ralldklu!I, and a small , offset, subsidi ary crevasse (or crevasses). The fo ll owin g observations rega rdin g the behavior of th e bergsc hruncl and ice adjacent to it are of parti cul ar interest: ( I) topograph y of the subglaeial bedrock is a control on the location of the main bergschrund and subsidi a ry crevasses. (2) th e main bergschrund and subsid ia ry crevasse(s) are conn ected by subglacial gaps betwee n bedrock and ice; th e gaps are part of th e "bergschrund system" , (3) snow/ ice immedi ately down-glacier of the bergschrund system moves nea rl y verticall y dow nwa rd in response to rotational fl ow of the glacier. a ll owin g the bergschrund components to keep the same location and size fro m year to year, (4) an inde pend ent accumul ati on, fl ow. -
Geomorphic Character, Age and Distribution of Rock Glaciers in the Olympic Mountains, Washington
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1987 Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington Steven Paul Welter Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Welter, Steven Paul, "Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington" (1987). Dissertations and Theses. Paper 3558. https://doi.org/10.15760/etd.5440 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. For more information, please contact [email protected]. AN ABSTRACT OF THE THESIS OF Steven Paul Welter for the Master of Science in Geography presented August 7, 1987. Title: The Geomorphic Character, Age, and Distribution of Rock Glaciers in the Olympic Mountains, Washington APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Rock glaciers are tongue-shaped or lobate masses of rock debris which occur below cliffs and talus in many alpine regions. They are best developed in continental alpine climates where it is cold enough to preserve a core or matrix of ice within the rock mass but insufficiently snowy to produce true glaciers. Previous reports have identified and briefly described several rock glaciers in the Olympic Mountains, Washington {Long 1975a, pp. 39-41; Nebert 1984), but no detailed integrative study has been made regarding the geomorphic character, age, 2 and distribution of these features. -
Passupassu Passu
NWFP Wildlife Department Government of NWFP NA Forestry, Parks and Wildlife Department NA Administration PASSUPASSUPASSUPASSU MagnificentPASSU Glaciers & Mighty Peaks Rock flutes near Fatima Hil © all photographs Matthieu Paley p12 PASSU IS MAGNIFICENTLY SITUATED, IN A COUNTRY WHERE NATURE HAS DESIGNED EVERYTHING ON A NOBLE AND LAVISH SCALE. “Col. R. C. F. Schomberg, “Between the Oxus and the Indus” ” all maps by Mareile Paley. Created with the help of WWF GIS-Lab, ESRI and ERDAS imagine all maps by Mareile Paley. PASSU FACTS location Gojal, Upper Hunza, on the Karakoram Highway main settlements Passu, Janabad public transport any transport on Karakoram Highway going between Aliabad and Sost accommodation several small guesthouses in Passu, guesthouses and hotels in Janabad supplies best to buy all your trekking food in Sost, Aliabad or Gilgit population 98 households, 880 people indigenous language Wakhi indigenous wildlife snow leopard, Himalayan ibex, red fox, wolf, Himalayan snow cock, rock partridge common plant species juniper, willow, poplar, wild roses, seabuckthorn View of Passu from Avdegar INTRODUCTION INTRODUCTIONINTRODUCTIONINTRODUCTIONINTRODUCTION With the completion of the Karakoram Highway (KKH) in 1978, the previously inaccessible maze of high mountains, glaciers and hidden valleys which make up the Karakoram Range, suddenly opened its doors to the world. An area of unspoiled mountain beauty with rugged glaciers, unclimbed peaks and pristine wildlife, Gojal, the region north of Hunza, has since become a popular spot for ecotourism. The sun-drenched summits Passu village with its small rural Wakhi community lays in the heart of Gojal. Passu’s idyllic Despite its popularity as a opposite Passu are commonly trekking destination, Passu known as the Cathedral Peaks. -
Geology of Hyder and Vicinity Southeastern Alaska
DEPARTMENT OF THE INTERIOR Roy O. West, Secretary U. S. GEOLOGICAL SURVEY George Otis Smith, Director Bulletin 807 GEOLOGY OF HYDER AND VICINITY SOUTHEASTERN ALASKA WITH A RECONNAISSANCE OF CHICKAMIN RIVER BY A. F. RUDDINGTON UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1&29 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS TJ.S.OOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 35 CENTS PER COPY CONTENTS Page Foreword, by Philip S. Smith._________________________ vn Introduction...____________________________________________________ 1 Field work_.._.___._.______..____...____. -_-__-. .. 1 Acknowledgments. _-_-________-_-___-___-__--_____-__-- -____-_ 2 History._________________________________________________________ 2 Bibliography ________-______ _____________._-__.-___-__--__--_--_-_ 3 Alaska.__-___-__---______-_-____-_-___--____-___-_-___-__-___ & British Columbia____-_____-___-___________-_-___--___.._____- 4 Geography_______________________________________-____--___-__--_ 4 Location and transportation facilities.___________________________ 4 Climate. __--______-______.____--__---____-_______--._--.--__- 5 Vegetation ___________________________________________________ 6 Water power._--___._____.________.______-_.._____-___.-_____ 7 Topography-___________--____-_-___--____.___-___-----__--_-- 7 General features of the relief----______-_---___-__------_-_-_ 7 Streams.._ _______________________________________________ 9 Glaciation.. _ __-_____-__--__--_____-__---_____-__--_----__ 10 Geology.... __----_-._ -._---_--__-.- _-_____-_____-___-_ 13 General features___-_-____-__-__-___-..____--___-_-____--__-._ 13 Hazelton group._....._.._>___-_-.__-______----_-----'_-__-..-- 17 General character.-----.-------.-------------------------- 17 Greenstone and associated rocks.._______.__.-.--__--_--_--_ 18 Graywacke-slate division.._________-_-__--_-_-----_--_----_ 19 Coast.Range intrusives__________-__-__--___-----------_-----_- 22 Texas Creek batholith and associated dikes..__--__.__-__-__-. -
K2 Base Camp and Gondogoro La Trek
K2 And Gondogoro La Trek, Pakistan This is a trekking holiday to K2 and Concordia in the Karakoram Mountains of Pakistan followed by crossing the Gondogoro La to Hushe Valley to complete a superb mountaineering journey. Group departures See trip’s date & cost section Holiday overview Style Trek Accommodation Hotels, Camping Grade Strenuous Duration 23 days from Islamabad to Islamabad Trekking / Walking days On Trek: 15 days Min/Max group size 1 / 8. Guaranteed to run Meeting point Joining in Islamabad, Pakistan Max altitude 5,600m, Gondogoro Pass Private Departures & Tailor Made itineraries available Departures Group departures 2021 Dates: 20 Jun - 12 Jul 27 Jun - 19 Jul 01 Jul - 23 Jul 04 Jul - 26 Jul 11 Jul - 02 Aug 18 Jul - 09 Aug 25 Jul - 16 Aug 01 Aug - 23 Aug 08 Aug - 30 Aug 15 Aug - 06 Sep 22 Aug - 13 Sep 29 Aug - 20 Sep Will these trips run? All our k2 and Gondogoro la treks are guaranteed to run as schedule. Unlike some other companies, our trips will take place with a minimum of 1 person and maximum of 8. Best time to do this Trek Pakistan is blessed with four season weather, spring, summer, autumn and winter. This tour itinerary is involved visiting places where winter is quite harsh yet spring, summer and autumns are very pleasant. We recommend to do this Trek between June and September. Group Prices & discounts We have great range of Couple, Family and Group discounts available, contact us before booking. K2 and Gondogoro trek prices are for the itinerary starting from Islamabad to Skardu K2 - Gondogoro Pass - Hushe Valley and back to Islamabad. -
A Case Study of Gilgit-Baltistan
The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan PhD Thesis Submitted by Ehsan Mehmood Khan, PhD Scholar Regn. No. NDU-PCS/PhD-13/F-017 Supervisor Dr Muhammad Khan Department of Peace and Conflict Studies (PCS) Faculties of Contemporary Studies (FCS) National Defence University (NDU) Islamabad 2017 ii The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan PhD Thesis Submitted by Ehsan Mehmood Khan, PhD Scholar Regn. No. NDU-PCS/PhD-13/F-017 Supervisor Dr Muhammad Khan This Dissertation is submitted to National Defence University, Islamabad in fulfilment for the degree of Doctor of Philosophy in Peace and Conflict Studies Department of Peace and Conflict Studies (PCS) Faculties of Contemporary Studies (FCS) National Defence University (NDU) Islamabad 2017 iii Thesis submitted in fulfilment of the requirement for Doctor of Philosophy in Peace and Conflict Studies (PCS) Peace and Conflict Studies (PCS) Department NATIONAL DEFENCE UNIVERSITY Islamabad- Pakistan 2017 iv CERTIFICATE OF COMPLETION It is certified that the dissertation titled “The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan” written by Ehsan Mehmood Khan is based on original research and may be accepted towards the fulfilment of PhD Degree in Peace and Conflict Studies (PCS). ____________________ (Supervisor) ____________________ (External Examiner) Countersigned By ______________________ ____________________ (Controller of Examinations) (Head of the Department) v AUTHOR’S DECLARATION I hereby declare that this thesis titled “The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan” is based on my own research work. Sources of information have been acknowledged and a reference list has been appended. -
Survey of Ecotourism Potential in Pakistan's Biodiversity Project Area (Chitral and Northern Areas): Consultancy Report for IU
Survey of ecotourism potential in Pakistan’s biodiversity project area (Chitral and northern areas): Consultancy report for IUCN Pakistan John Mock and Kimberley O'Neil 1996 Keywords: conservation, development, biodiversity, ecotourism, trekking, environmental impacts, environmental degradation, deforestation, code of conduct, policies, Chitral, Pakistan. 1.0.0. Introduction In Pakistan, the National Tourism Policy and the National Conservation Strategy emphasize the crucial interdependence between tourism and the environment. Tourism has a significant impact upon the physical and social environment, while, at the same time, tourism's success depends on the continued well-being of the environment. Because the physical and social environment constitutes the resource base for tourism, tourism has a vested interest in conserving and strengthening this resource base. Hence, conserving and strengthening biodiversity can be said to hold the key to tourism's success. The interdependence between tourism and the environment is recognized worldwide. A recent survey by the Industry and Environment Office of the United Nations Environment Programme (UNEP/IE) shows that the resource most essential for the growth of tourism is the environment (UNEP 1995:7). Tourism is an environmentally-sensitive industry whose growth is dependent upon the quality of the environment. Tourism growth will cease when negative environmental effects diminish the tourism experience. By providing rural communities with the skills to manage the environment, the GEF/UNDP funded project "Maintaining Biodiversity in Pakistan with Rural Community Development" (Biodiversity Project), intends to involve local communities in tourism development. The Biodiversity Project also recognizes the potential need to involve private companies in the implementation of tourism plans (PC II:9). -
Glacier Velocities Across the Central Karakoram
Annals of Glaciology 50(52) 2009 1 Glacier velocities across the central Karakoram Luke COPLAND,1 Sierra POPE,1 Michael P. BISHOP,2 John F. SHRODER, Jr,2 Penelope CLENDON,3 Andrew BUSH,4 Ulrich KAMP,5 Yeong Bae SEONG,6 Lewis A. OWEN7 1Department of Geography, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada E-mail: [email protected] 2Department of Geography and Geology, University of Nebraska at Omaha, Omaha, Nebraska 68182, USA 3Department of Geography, University of Canterbury, Canterbury, New Zealand 4Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada 5Department of Geography, University of Montana, Missoula, Montana 59812, USA 6Department of Geography Education, Korea University, Seoul 136-701, Korea 7Department of Geology, University of Cincinnati, Cincinnati, Ohio 45221, USA ABSTRACT. Optical matching of ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) satellite image pairs is used to determine the surface velocities of major glaciers across the central Karakoram. The ASTER images were acquired in 2006 and 2007, and cover a 60 120 km region  over the Baltoro glacier and areas to the north and west. The surface velocities were compared with differential global position system (GPS) data collected on the Baltoro glacier in summer 2005. The ASTER measurements reveal fine details about ice dynamics in this region. For example, glaciers are found to be active over their termini even where they are very heavily debris covered. The characteristics of several surge-type glaciers were measured, with terminus advances of several hundred meters per year and the displacement of trunk glaciers as surge glaciers pushed into them.