In Shimshal Valley Gilgit-Baltistan Pakistan
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Khunjerab National Park
Khunjerab National Park General features vegetation, with Juniper spp., Rosa webbiana, and Polygonum spp. occurring on dry slopes, and Myricaria germanica and Country: Pakistan, Hunza-Nagar District Hippophae rhamnoides along stream beds. Broadleaf species Date of establishment: 1975 mainly consist of Salix sp. and Betula utilis. 2 Area: 4,455 km Fauna Geographic location: Latitude: 36°30’N; Fourteen mammalian species have been recorded in the Longitude: 75°30’E park, of which three are critically endangered and two IUCN category: IV are endangered. Marco Polo sheep (Ovis ammon polii), Overview cape hare (Lepus capensis), common pipistrelle (Pipistrellus pipistrellus), grey long-eared bat (Plecotus austriacus), common Khunjerab National Park (KNP) is located in the extreme red fox (Vulpes vulpes), field mouse Apodemus( sylvaticus), north of Pakistan. The high-altitude park covers about 4,445 Himalayan ibex (Capra sibirica), long-tailed marmot (Marmota km2, making it Pakistan’s third largest national park. It was caudata), large-eared pika (Ochotona macrotis), migratory set up to protect rare and unique species of the Pamir and hamster (Cricetulus migratorius), blue sheep (Pseudois nayaur), Tibetan Plateau. The elevation within the park ranges from brown bear (Ursus arctos), snow leopard (Panthera uncia), 3,200 to 7,700 masl. Khunjerab Pass, the gateway to China and Indian wolf (Canis lupus pallipes). The park has some of via the Karakoram Highway, lies at 4,934 masl. the most diverse avifauna in mountain regions, with 48 avian People species having been recorded in the park. Tajik and Brushu Threats Flora Decline of Marco Polo sheep population, largely as a result of hunting and general disturbance from the Due to the protected area’s high elevation, floral species Karakoram Highway which runs through the park. -
Glaciers in Xinjiang, China: Past Changes and Current Status
water Article Glaciers in Xinjiang, China: Past Changes and Current Status Puyu Wang 1,2,3,*, Zhongqin Li 1,3,4, Hongliang Li 1,2, Zhengyong Zhang 3, Liping Xu 3 and Xiaoying Yue 1 1 State Key Laboratory of Cryosphere Science/Tianshan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; [email protected] (Z.L.); [email protected] (H.L.); [email protected] (X.Y.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 College of Sciences, Shihezi University, Shihezi 832000, China; [email protected] (Z.Z.); [email protected] (L.X.) 4 College of Geography and Environment Sciences, Northwest Normal University, Lanzhou 730070, China * Correspondence: [email protected] Received: 18 June 2020; Accepted: 11 August 2020; Published: 24 August 2020 Abstract: The Xinjiang Uyghur Autonomous Region of China is the largest arid region in Central Asia, and is heavily dependent on glacier melt in high mountains for water supplies. In this paper, glacier and climate changes in Xinjiang during the past decades were comprehensively discussed based on glacier inventory data, individual monitored glacier observations, recent publications, as well as meteorological records. The results show that glaciers have been in continuous mass loss and dimensional shrinkage since the 1960s, although there are spatial differences between mountains and sub-regions, and the significant temperature increase is the dominant controlling factor of glacier change. The mass loss of monitored glaciers in the Tien Shan has accelerated since the late 1990s, but has a slight slowing after 2010. Remote sensing results also show a more negative mass balance in the 2000s and mass loss slowing in the latest decade (2010s) in most regions. -
Wildlife Protection Along the Karakorum Highway in Khunjerab
Pakistan J. Zool., vol. 44(5), pp. 1452-1457, 2012. occurred, causing severe destruction along the KKH. In February 2006, Pakistan and China signed Wildlife Protection Along the a Memorandum of Understanding which initiated Karakorum Highway in Khunjerab the improvement of the highway between Raikot Bridge and Khunjerab Pass during first phase of National Park project (Tao et al., 2010). The section of the KKH from K753+800 to Yun Wang,1 * Jiding Chen,1 Shuangcheng Tao,1 1 1 K811+343 (kilometer markers) bisects Khunjerab Mengmeng Wang, Xuanya Wang and Asif National Park (KNP). The KNP was built in 1975 Shah2 1 with the primary objective of protecting the China Academy of Transportation Sciences, threatened species Marco Polo sheep (Ovis ammon Beijing, 100029, China 2 polii) and its natural habitat. Other protected species China Agricultural University, Beijing, 100193, found in the KNP include: the snow leopard (Uncia China uncia) and the brown bear (Ursus arctos). These species of wildlife make the KNP one of the most Abstract.- The Karakorum Highway (KKH) which connects Pakistan and China passes through important centers for biodiversity in Pakistan Khunjerab National Park in Pakistan. The park has (Qureshi et al., 2011). extremely rich wildlife diversity. The potential The impact of highway construction on adverse impacts of KKH improvement project on wildlife and the need to protect wildlife are wildlife were analyzed with field surveys, becoming critical issues for zoologists throughout interviews and secondary data for the period from 2009 to 2011. Protective measures were developed the world (Forman and Alexander, 1998). The and used to guide highway construction. -
Tntroduction to the Geological Map of the North Karakorum Terrain from the Chapursan Valley to the Shimshal Pass 1:150.000 Scale
Riv. It. Paleont. Strat. v. 100 n. 1 pp. 725-736 Giugno 1994 TNTRODUCTION TO THE GEOLOGICAL MAP OF THE NORTH KARAKORUM TERRAIN FROM THE CHAPURSAN VALLEY TO THE SHIMSHAL PASS 1:150.000 SCALE ANDREA ZANCHI * & MAURZIO GAETANI * *, + * with contributioru from Lucia Angiolini Frangois Debon ", Flavio Jadoul & Alda Nicora Key-zoords: Geological map, Karakorum, Pakistan. Riass*nto. Questa nota introduce una nuova carta geologica a scala 1:150.000, allegata al presente articolo. L'area cartografata include un vasto settore dell'alta valle di Hunza (Karakorum, Pakistan), situato a N del Batolite Assiale del Karakorum e comprendente la copertura sedimentaria del Karakorum, l'età della quale è compresa tra il Permiano e il Cretacico superiore. Sono state riconosciute 4 grandi unità strutturali, che risultano dislocate in modo complesso durante eventi orogenetici polifasici, anivi dal Cretaceo sino a tutto il Cenozoico, in conseguenza delle successive collisioni contro il margine asiatico dell'Arco del Kohistan prima e della Placca Indiana poi. La cartografia presentata, pur avendo un marcato carattere stratigrafico-strut- turale, tiene conto, a grandi linee, anche della distribuzione dei depositi quaternari. Abstract. These notes introduce a new geological map at 1:150,000 scale of a large part of the Upper Hunza valley (Karakorum, Pakistan). The mapped area includes the Permian to Cretaceous sedimentary cover of the Karakorum, which is located north of the Karakorum Axial Batholith. The rnapped sedimentary and intrusive complexes form four major tectonic units, stacked in a very complex system, due to polyphase events, spanning from Cretaceous to Cenozoic. These even6 are linked to repeated collisions against the Asian margin of the Kohistan Arc during the Cretaceous and of the Indian Plate during the Cenozoic. -
A Global Overview of Protected Areas on the World Heritage List of Particular Importance for Biodiversity
A GLOBAL OVERVIEW OF PROTECTED AREAS ON THE WORLD HERITAGE LIST OF PARTICULAR IMPORTANCE FOR BIODIVERSITY A contribution to the Global Theme Study of World Heritage Natural Sites Text and Tables compiled by Gemma Smith and Janina Jakubowska Maps compiled by Ian May UNEP World Conservation Monitoring Centre Cambridge, UK November 2000 Disclaimer: The contents of this report and associated maps do not necessarily reflect the views or policies of UNEP-WCMC or contributory organisations. The designations employed and the presentations do not imply the expressions of any opinion whatsoever on the part of UNEP-WCMC or contributory organisations concerning the legal status of any country, territory, city or area or its authority, or concerning the delimitation of its frontiers or boundaries. TABLE OF CONTENTS EXECUTIVE SUMMARY INTRODUCTION 1.0 OVERVIEW......................................................................................................................................................1 2.0 ISSUES TO CONSIDER....................................................................................................................................1 3.0 WHAT IS BIODIVERSITY?..............................................................................................................................2 4.0 ASSESSMENT METHODOLOGY......................................................................................................................3 5.0 CURRENT WORLD HERITAGE SITES............................................................................................................4 -
Collaborative Management of Protected Areas First Asia Parks Congress, Sendai, Japan, 13-17 November, 2012
Islamic Republic of Pakistan Collaborative Management of Protected Areas First Asia Parks Congress, Sendai, Japan, 13-17 November, 2012 By: Muhammad Samar Hussain Khan Assistant Secretary (Wildlife) Forestry Wing, Climate Change Division, (Cabinet Secretariat) Government of Pakistan, Islamabad Email: samar [email protected] [email protected] K2 About 1,000 miles Arabian Sea Pakistan is an oblong stretch of land between the Arabian sea and Karakoram mountains. Lying diagonally 24˚ N and 37˚ N latitudes and 61˚ E and 75˚ E longitudes, and covering an area of 87.98 million hectares. Topographically, the country has a continuous massive mountainous tract in the north, the west and south-west and large fertile plain, the Indus plain. The northern mountain system, comprising the Karakoram, the Himalays, and the Hindu-Kush, has enormous mass of snow and glaciers and 100 peaks of over 5400m in elevation. From Arabian Sea to the second highest peak in the world, K-2 (8,563m), it is the greatest change in elevation within any sovereign state on earth. More than 80% of the country is arid or semiarid. Due to this extensive aridity, the natural forest area is very small (about 5% of the total area) Pakistan’s Ecological Zones WWF- Global 200 Ecoregions Pakistan has five diverse and representative ecoregions included in Global 200 Ecoregions, identified by WWF. That are: The North Arabian Sea The Indus Ecoregion Rann of Kutch Tibetan plateau Western Himalayan Temperate Forests BIODIVERSITY OF PAKISTAN Biodiversity of Pakistan is blend of Palaearctic, Indo-Malayan and Ethiopian forms. Species belonging to Palaearctic realm occur in the Himalayan and Balochistan uplands; those belonging to Indo-Malayan realm occur in the Indus plains including Thar Desert and the Himalayan foothills. -
Brief Description of the Northern Areas
he designation of geographical entities in this book, and the presentation of the material, do T not imply the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN. Published by: IUCN Pakistan. Copyright: ©2003 Government of Pakistan, Northern Areas Administration and IUCN–The World Conservation Union. Reproduction of this publication for educational and other non-commercial purposes is authorised without prior permission from the copyright holders, providing the source is fully acknowledged. Reproduction of the publication for resale or for other commercial purposes is prohibited without prior written permission from the copyright holders. Citation: Government of Pakistan and IUCN, 2003. Northern Areas State of Environment and Development. IUCN Pakistan, Karachi. xlvii+301 pp. Compiled by: Scott Perkin Resource person: Hamid Sarfraz ISBN: 969-8141-60-X Cover & layout design: Creative Unit (Pvt.) Ltd. Cover photographs: Gilgit Colour Lab, Hamid Sarfraz, Khushal Habibi, Serendip and WWF-Pakistan. Printed by: Yaqeen Art Press Available from: IUCN–The World Conservation Union 1 Bath Island Road, Karachi Tel.: 92 21 - 5861540/41/42 Fax: 92 21 - 5861448, 5835760 Website: www.northernareas.gov.pk/nassd N O RT H E R N A R E A S State of Environment & Development Co n t e n t s Acronyms and Abbreviations vi Glossary -
A Late Quaternary Catastrophic Flood in the Lahul Himalayas
JOURNAL OF QUATERNARY SCIENCE (1996) 11 (6)495-510 CCC 0267-8179/96/060495-16 0 1996 by John Wiley & Sons, Ltd. A Late Quaternary catastrophic flood in the Lahul Himalayas PETER COXON Department of Geography, Trinity College, Dublin, Ireland LEWIS A. OWEN Department of Geography, Royal Holloway, University of London, Egham TW20 OEX, England WISHART A. MITCHELL School of Geological and Environmental Sciences, University of Luton, Luton LU1 3JU, England Coxon, P., Owen, L.A. and Mitchell, W.A. 1996. A Late Quaternary catastrophic flood in the Lahul Himalayas. Journal of Quaternary Science, Vol. 11, pp. 495-51 0. ISSN 0267-8179 Received 6 March 1996 Accepted 8 May 1996 ABSTRACT: Impressive flood deposits are described resulting from a catastrophic lake outburst in the Upper Chandra valley in the Lahul Himalaya, northern India. Reconstructions of the former glacial lake, Glacial Lake Batal, and the discharges were undertaken using landforms and sediment data. The glacial dam burst released 1.496 km3 of water in 0.72 days, with peak discharges of between 21 000 and 27000 m3 s-' at Batal. Dating by OSL suggests the flood occurred ca. 36.9 If: 8.4 to 43.4 2 10.3 ka ago. This cataclysmic flood was responsible for major resedimentation and landscape modification within the Chandra valley. Journal of Quaternary Suence KEYWORDS: Himalayas; high-magnitude flood event; northern India; glacial lake outburst; glacial geomorphology. Introduction The study area The flood deposits occur as extensive but discontinuous Catastrophic outbursts of glacial lakes in the Himalayas have sheets of bouldery diamicton between Batal and Chhatiru been described by several authors (Mason 1929, 1930; in the upper Chandra valley (Fig. -
Glaciers in Pakistan | World General Knowledge
Glaciers in Pakistan | World General Knowledge With 7,253 known glaciers, including 543 in the Chitral Valley, there is more glacial ice in Pakistan than anywhere on Earth outside the polar regions, according to various studies. Those glaciers feed rivers that account for about 75 percent of the stored-water supply in the country of at least 200 million. But as in many other parts of the world, researchers say, Pakistan’s glaciers are receding, especially those at lower elevations, including here in the Hindu Kush mountain range in northern Khyber Pakhtunkhwa province. Among the causes cited by scientists: diminished snowfall, higher temperatures, heavier summer rainstorms and rampant deforestation. 1) Baltoro Glacier The glacier at 63km in length is one of the largest land glaciers on Earth. It can be accessed through Gilgit-Baltistan region. The glacier gives rise to the Shigar River. 2) Batura Glacier At 53 km in length, the Batura Glacier is up there with the biggest in the world. It lies in the Batura Valley in the Gojal region of Gilgit Baltistan. 3) Biafo Glacier The Biago Glacier is 67kms long and the third biggest land glacier in the entire world. Mango, Baintha and Namla are campsites set up near the glacier and can be accessed through the Askole Village of Gilgit-Baltistan. 4) Panmah Glacier Located in the Central Karakoram National Park, Gilgit-Baltistan, 5) Rupal Glacier It is the source of the Rupal River and lies in the Great Himalayas. It is South of the Nanga Parbat and North of Laila Peak. Downloaded from www.csstimes.pk | 1 Glaciers in Pakistan | World General Knowledge 6) Sarpo Laggo The glacier flows from Pakistan to China just north of the Baltoro Muztagh Range. -
Status and Red List of Pakistan's Mammals
SSttaattuuss aanndd RReedd LLiisstt ooff PPaakkiissttaann’’ss MMaammmmaallss based on the Pakistan Mammal Conservation Assessment & Management Plan Workshop 18-22 August 2003 Authors, Participants of the C.A.M.P. Workshop Edited and Compiled by, Kashif M. Sheikh PhD and Sanjay Molur 1 Published by: IUCN- Pakistan Copyright: © IUCN Pakistan’s Biodiversity Programme This publication can be reproduced for educational and non-commercial purposes without prior permission from the copyright holder, provided the source is fully acknowledged. Reproduction of this publication for resale or other commercial purposes is prohibited without prior permission (in writing) of the copyright holder. Citation: Sheikh, K. M. & Molur, S. 2004. (Eds.) Status and Red List of Pakistan’s Mammals. Based on the Conservation Assessment and Management Plan. 312pp. IUCN Pakistan Photo Credits: Z.B. Mirza, Kashif M. Sheikh, Arnab Roy, IUCN-MACP, WWF-Pakistan and www.wildlife.com Illustrations: Arnab Roy Official Correspondence Address: Biodiversity Programme IUCN- The World Conservation Union Pakistan 38, Street 86, G-6⁄3, Islamabad Pakistan Tel: 0092-51-2270686 Fax: 0092-51-2270688 Email: [email protected] URL: www.biodiversity.iucnp.org or http://202.38.53.58/biodiversity/redlist/mammals/index.htm 2 Status and Red List of Pakistan Mammals CONTENTS Contributors 05 Host, Organizers, Collaborators and Sponsors 06 List of Pakistan Mammals CAMP Participants 07 List of Contributors (with inputs on Biological Information Sheets only) 09 Participating Institutions -
Pakistan Protected Areas M E E T I
Pakistan Protected Areas Me e t i n g Pr o c e e d i n g s Islamabad, Pakistan September 24 – 25, 1994 This workshop was funded by United States National Park Service The views expressed in this publication are not necessarily those of IUCN Cover photo: IUCN Editors: Naziha Ghazali, Umber Khairi and the Communications Unit, IUCN IUCN–The World Conservation Union, Pakistan 1, Bath Island Road, Karachi 75530 © 1995 by IUCN–The World Conservation Union, Pakistan All rights reserved ISBN 969-8141-15-4 Formatted by the Communications Unit, IUCN Printed by Rosette Contents List of Abbreviations and Acronyms iii Objectives of the Meeting 1 Being Systematic: Introducing National Systems Planning for Protected Areas 3 Laos PDR: Protected Areas Systems Planning 7 Overview of Protected Areas Systems Planning: Focus on Pakistan 9 International Experiences in Protected Areas Systems Plans 11 Protected Areas Systems Plans: Principles, Process and Structure 15 The Sarhad Provincial Conservation Strategy, Biodiversity and Protected Areas 17 IUCN's Role in Conservation in Pakistan 21 The Role and Contribution of WWF Pakistan to Conservation 25 Working Group Discussions 27 Annexures 29 1. IUCN Protected Area Categories 31 2. Agenda 35 3. List of Participants 37 PAKISTAN PROTECTED AREAS MEETING i ii PAKISTAN PROTECTED AREAS MEETING List of Abbreviations and Acronyms CNPPA Commission on National Parks and Protected Areas IUCN IUCN–The World Conservation Union NCS National Conservation Strategy NWFP North West Frontier Province PA Protected Area UNDP United Nations Development Programme UNEP United Nations Environment Programme WCMC World Conservation Monitoring Centre WWF World Wide Fund for Nature PAKISTAN PROTECTED AREAS MEETING iii iv PAKISTAN PROTECTED AREAS MEETING Objectives of the Meeting Abdul Latif Rao Programme Director, Strategies Support Unit, IUCN Pakistan boasts an impressive network of 14 ● Conservation values of PAs are not fully National Parks, 84 Wildlife Sanctuaries and 76 known. -
Ground Water Scenario of Himalaya Region, India
Hkkjr ds fgeky;h {ks=k dk Hkwty ifjn`'; Ground Water Scenario of Himalayan Region, India laiknu@Edited By: lq'khy xqIrk v/;{k Sushil Gupta Chairman Central Ground Water Board dsanzh; Hkwfe tycksMZ Ministry of Water Resources ty lalk/ku ea=kky; Government of India Hkkjr ljdkj 2014 Hkkjr ds fgeky;h {ks=k dk Hkwty ifjn`'; vuqØef.kdk dk;Zdkjh lkjka'k i`"B 1- ifjp; 1 2- ty ekSle foKku 23 3- Hkw&vkd`fr foKku 34 4- ty foKku vkSj lrgh ty mi;kst~;rk 50 5- HkwfoKku vkSj foorZfudh 58 6- Hkwty foKku 73 7- ty jlk;u foKku 116 8- Hkwty lalk/ku laHkko~;rk 152 9- Hkkjr ds fgeky;h {ks=k esa Hkwty fodkl ds laca/k esa vfHktkr fo"k; vkSj leL;k,a 161 10- Hkkjr ds fgeky;h {ks=k ds Hkwty fodkl gsrq dk;Zuhfr 164 lanHkZ lwph 179 Ground Water Scenario of Himalayan Region of India CONTENTS Executive Summary i Pages 1. Introduction 1 2. Hydrometeorology 23 3. Geomorphology 34 4. Hydrology and Surface Water Utilisation 50 5. Geology and Tectonics 58 6. Hydrogeology 73 7. Hydrochemistry 116 8. Ground Water Resource Potential 152 9. Issues and problems identified in respect of Ground Water Development 161 in Himalayan Region of India 10. Strategies and plan for Ground Water Development in Himalayan Region of India 164 Bibliography 179 ifêdkvks dh lwph I. iz'kklfud ekufp=k II. Hkw vkd`fr ekufp=k III. HkwoSKkfud ekufp=k d- fgeky; ds mRrjh vkSj if'peh [kaM [k- fgeky; ds iwohZ vkSj mRrj iwohZ [kaM rFkk iwoksZRrj jkT; IV.