Karakorum – Virjerab Glacier Almost 90 Years After the First Explorers
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Cro Ssro Ads Asia
11 How migrants made their way: The role of pioneering migrants and solidarity networks of the Wakhi of Gojal (Northern Pakistan) in shaping the dynamics of rural-urban migration Andreas Benz Working Paper Series Paper Working crossroads asia crossroads ISSN 2192-6034 Bonn, July 2013 Crossroads Asia Working Papers Competence Network Crossroads Asia: Conflict – Migration – Development Editors: Ingeborg Baldauf, Stephan Conermann, Anna-Katharina Hornidge, Hermann Kreutzmann, Shahnaz Nadjmabadi, Dietrich Reetz, Conrad Schetter and Martin Sökefeld. How to cite this paper: Benz, Andreas (2013): How migrants made their way: The role of pioneering migrants and solidarity networks of the Wakhi of Gojal (Northern Pakistan) in shaping the dynamics of rural-urban migration. In: Crossroads Asia Working Paper Series, No. 11. Partners of the Network: Imprint Competence Network Crossroads Asia: Conflict – Migration – Development Project Office Center for Development Research/ZEFa Department of Political and Cultural Change University of Bonn Walter-Flex Str. 3 D-53113 Bonn Tel: + 49-228-731722 Fax: + 49-228-731972 Email: [email protected] Homepage: www.crossroads-asia.de i How migrants made their way: The role of pioneering migrants and solidarity networks of the Wakhi of Gojal (Northern Pakistan) in shaping the dynamics of rural-urban migration Andreas Benz Table of Contents 1. Introduction ..................................................................................................................................... 1 2. The current state -
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. -
Gilgit- Baltistan)
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Florence Research Naveiñ Reet: Nordic Journal of Law and Social Research (NNJLSR) No.8 2018, pp. 77-100 Civil Society and Governance in Gojal (Gilgit- Baltistan) Fazal Amin Beg 1 and Zoran Lapov 2 Abstract Focusing on both soft and hard development, Aga Khan Rural Support Programme (AKRSP) reached Gilgit-Baltistan and neighbouring Chitral (northern Pakistan) in 1982. In a short span of time, more than 4,500 community associations, namely village and women’s organisations (VWOs), were formed throughout the Region, introducing the local population to democratic governance grounded in civil society-based system. The phenomenon brought about producing significant public and agricultural infrastructures in less than 15 years. As a result, AKRSP turned into a laboratory and model of rural development for many South Asian realities. Underpinned by a qualitative case study and relevant literature review, the present research addresses the process of civil society construction in Gojal (sub-district of Hunza, Gilgit-Baltistan), including the role and engagement of AKRSP: introduced by depicting the scheme of traditional social institutions in front of novel patterns of social organisation, the paper delves into the emergence of – formal and informal – civil society organisations (CSOs) in the form of local support organisations (LSOs) as federations of VWOs and related networks, whose establishment in Gilgit-Baltistan (as well as in Chitral) is a recent phenomenon dating back to the mid-2000s. 1 Fazal Amin Beg, the main author of the paper, has academic background in Sociocultural anthropology, and Farsi literature. -
Open Access Journal Home Page: ISSN: 2223-957X
Int. J. Econ. Environ. Geol. Vol. Alam10 (4 et) 25al.- 29 /Int.J.Econ.Environ.Geol.Vol., 2019 10(4) 25-29, 2019 Open Access Journal home page: www.econ-environ-geol.org ISSN: 2223-957X c The Process Designing of Gold Extraction from Placers of Passu to Shimshal (Hunza Valley) Gilgit-Baltistan by Mercury Amalgamation and Cyanidation Leached Method Muhammad Alam1, Javed Akhter Qureshi2*, Garee Khan2, Manzoor Ali3, Naeem Abbas4, Sher Sultan2, Asghar Khan,2 Yasmeen Bano5 Government Degree College Gilgit,1 Department of Earth Sciences,2 Department of Physics,3 Department of Mining Engineering,4 Department of Mathematical Sciences,5 Karakoram International University, Gilgit, Pakistan *E mail: [email protected] Received: 22 October, 2019 Accepted: 03 January, 2020 Abstract: Gold wash through panning or washing in the fluvial sediments or sands is done on the river banks in Skardu, Hunza and other places. The method of gold washing is very crude, primitive and most of the gold is washed away back into the river. The current study mainly focused on extraction of placer gold deposits. Pneumatic machines from Passu to Shimshal (Hunza valley) Gilgit-Baltistan. The mercury amalgamation and cyanide leached methods have been used for placer gold deposits extraction from the concentrate obtained from shaking table. The amount of gold recovered from amalgamation method with mercury was 30.9%. The alloyed gold with other metals, gold dust, and fine gold was recovered by chemical process. The reagent consumption, i.e. 1.4 kg/ton of NACN and 6 Kg / ton of CaO were used for extraction of placer gold deposits. -
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. -
WAP +92 346 2324819 Email [email protected] Rest of Pakistan: WAP +92 300 8567321 Email [email protected]
Rs 54,100 per person* Sindh: WAP +92 346 2324819 email [email protected] Rest of Pakistan: WAP +92 300 8567321 email [email protected] 9 DAYS SWAT, GILGIT-HUNZA AND KAGHAN – MOUNTAIN VALLEY HIGHLIGHTS Day 1 Rawalpindi-Islamabad– Takht-i-Bahi – Mingora/Saidu Sharif, Swat: Depart early on the M-1 motorway and then on to the Swat Express way. Stop on the way to visit Takht-i-Bahi composed of the ruins of Buddhist monasteries and listed as a UNESCO World Heritage Site. After visiting the site continue to Swat. On arrival, check-in to the hotel for overnight. Day 2 Swat: Begin the sightseeing tour of Swat with the Swat Museum, established in 1959 by the Wali-e-Swat. After the museum, visit the Saidu Baba Mosque, built in memory of the former King of Swat, the archaeological sites of Butkara I, and Saidu Stupa. Another 4 km away one reaches Ghaligai Rock Buddhas, facing the river Swat. In the afternoon we will visit Murghazar, the old white palace, then continue to Mingora Bazaar before returning to the hotel. Day 3 Swat –Gilgit: Today will be an exciting but long 12 to 13-hour drive on the Karakoram Highway (KKH), also known as the Sharah-e-Resham (Silk Road). On the way we will pass the famous Nanga Parbat (at 8126m the 9th highest peak in the world), the confluence of the Indus and Gilgit Rivers, as well as see the point where the 3 highest mountain ranges in the world (Himalayas, Karakoram and Hindu Kush) meet. -
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. -
Discover Hunza Itinerary and Information Pack
THE NORTHBOUND COLLECTIVE 13 MARCH 2018 HunzaOnFoot Your Travel Itinerary and Information Pack Day 4 GOJAL Transfer to Misgar Khunjerab National Park Day 5 GOJAL Sost Discover Hunza Khunjerab Pass Hunza - Gojal - Khunjerab National Park Day Six night all inclusive tour 6 Day 1 – Group leaves Islamabad for Hunza valley at approximately 6am (approximate drive time 45 minutes), transfer to Passu via Karakoram HUNZA Highway (drive time 2 to 3 hours, depending upon number and duration of stops) and checks into the Serena Hotel in Karimabad, Hunza. Transfer to Hunza Ganish Fort Today, participants will have some spare time to themselves in order to Duikar Sunset Hike acclimate to the higher altitudes. Group leader will be available to walk them Day 7 Day Day Day 1 2 3 GILGIT Hunza Hunza Gojal Transfer to Gilgit Transfer to Hunza Nature Walk Explore Gulmit Acclimate Baltit Fort Hike Borith Lake Return to Explore Karimabad Transfer to Passu Hike to Passu Glacier Islamabad 1 DISCOVER HUNZA 13 MARCH 2018 through Karimabad to soak in the sights in this vibrant mountain community. Day 2 – After breakfast, group explores Hunza valley on foot all the way to the serene Hyderabad village (excellent nature photography here) and then heads back to Karimabad through the downtown area which is when they get their chance to do some good souvenir shopping and a fresh cup of coffee at Café de Hunza. Once group has had some time to themselves, we hike up to the Baltit Fort for a guided tour through history followed by lunch in a beautiful garden restaurant next to the fort. -
THE KARAKORAM EXPEDITION, 1939. R. Scott Russell
THE KARAKORAM EXPEDITION, 1939 195 . THE KARAKORAM EXPEDITION, 1939 BY R. SCOTT RUSSELL Read before the Alpine Club, March 5, 1940. N 1937 Eric Shipton took his first expedition to the Karakoram and his party succeeded in mapping nearly 2000 square miles of country lying chiefly on the northern side of the main Asiatic watershed from the neighbourhood of K 2 to the Shimshal Pass. The attractive word ' unexplored ' was, however, still written in quite large letters on several parts of the Karakoram map, and in 1939 Shipton organised another expedition. The Survey of India offered the fullest cooperation, placing two Indian surveyors at his disposal for the summer and bearing part of the cost of the expedition. Generous grants were also received from the Royal Society, the Royal Geographical Society, the British Museum (Natural History), the Percy Sladen Fund and the Royal Botanic Gardens, Kew. In addition, Mr. R. W. Lloyd and Mr. A. Courtauld contributed most kindly to our funds. .We were a party of four for the greater part of the time : Shipton, Peter Mott our chief su~eyor, E. C. Fountaine as medical officer and myself. With the exception of Shipton none of us had. been in the Himalaya before. A. F. Betterton of Srinagar and Campbell Secord joined us for short periods. The programme of the expedition was divided into three sec tions. The summer of 1939 was to be spent making detailed maps of the .Hispar and Biafo Glaciers as well as the country adjacent to them. In the winter of 1939-:-1940 we planned to work from a base at Shimshal, and in the spring we would com plete the survey of the Aghil Range eventually reaching Leh in the upper Indus. -
Community Initiated Water Project for Irrigation and Drinking Yaz Sam Hussaini Gojal (2010-2011)
Community Initiated Water Project for Irrigation and Drinking Yaz sam Hussaini Gojal (2010-2011) ALI REHMAT Hussaini Organization for Local Development (HOLD) Hussaini Gojal, Hunza, Gilgit-Baltistan Total Population 639 Male 333 Female 306 Household 89 Altitude 2556m Source: Field Survey 2007 Gilgit-Baltistan Hussaini Village is situated in Hunza valley, 145 km North of Gilgit and 45 km from Ali Abad in Central Hunza. Hunza River flows in to the east while the Karakoram Highway (KKH) passes to its west. Hussaini Village is situated on 74°52'23.42" East longitude and 36°25'29.14" North latitude at an altitude of 2,556 meters above sea level. South of Hussaini is Gulmit (the headquarters of Gojal magistracy - tehsil), Ghulkin is to the southwest, while Passu is in the north with famous Batura glacier. Hussaini glacier is located to the west with famous Shisper peak, 7611meters. Hussaini is a small village of Gojal (Upper Hunza) in tGilgit-Baltistan. It is situated on the both banks of Hunza River. The old main village is on the western-bank and at the lateral moraine of Hussaini glacier and below Borith Lake. The newly irrigated land, called Zarabod, is on the left bank. The total population is 649 souls, living in 87 households. (2008) Hussaini is located in the center of the Karakoram Range, surrounded by high mountains having the heights of more than 7000 meters. Most of the peaks, remain snow covered throughout the year. Shishper (7611 m) is the highest peak of the study area. The rock exposed in the area is mainly Slate i.e. -
From Glacierized Basins in the Karakoram Mountains
Erosion and Sediment Yield: Global and Regional Perspectives (Proceedings of the Exeter Symposium, July 1996). IAHS Publ. no. 236, 1996. 85 Sediment transport from glacierized basins in the Karakoram mountains DAVID N. COLLINS Alpine Glacier Project, Department of Geography, University of Manchester, Manchester M13 9PL, UK Abstract Detailed measurements of temporal variations of suspended sediment flux in meltwaters draining from Batura glacier, Hunza basin, Karakoram mountains throughout an ablation season indicate an annual sediment yield of 6086 t km-2 year“1, or 10 144 t km"2 year“1 from the glacier sub-sole, assuming all the sediment is derived from glacial erosion. The seasonal pattern of sediment transport from Batura glacier results from the interaction of the sequence of hydrometeorologically- determined discharge events with the store of products of glacial abrasion beneath the ice. Glacier contributions to sediment flux downstream in the Indus basin are assessed in a framework of nested sub-basins. Sixty per cent of the annual sediment yield of the Hunza (47701 km“2 year“1) and more than 40% of that of the Indus leaving the Karakoram (12281 km“2 year“1) are glacier-derived, in basins in which precipitation increases markedly with elevation above arid valley bottoms. Much sediment is deposited on the plain, reducing sediment delivery to the Arabian Sea to about 2301 km“2 year“1, which masks high sediment fluxes in the small sub-basins within the Himalaya-Karakoram tectonic zone. INTRODUCTION According to Milliman & Syvitski (1992), a third of the estimated contemporary global flux of about 20 Gt year“1 of fluvial suspended sediment from the continents to the oceans is transported by the rivers of southern Asia.