Abbotabhad Formation, 138, 139, 140 Abruzzi Ridge, 62 Actinolite, 142

Total Page:16

File Type:pdf, Size:1020Kb

Abbotabhad Formation, 138, 139, 140 Abruzzi Ridge, 62 Actinolite, 142 Index [Italic page numbers indicate major references] Abbotabhad Formation, 138, 139, Askolc, 69 fluvial, 288 140 assemblage, heavy mineral, 131 gravel, 244, 251, 253, 255, 261 Abruzzi Ridge, 62 asthenosphere, 44 lacustrine, 288 actinolite, 142 Astor River, 25 limestone, 206, 208 Adak Island, 80 Astor Valley, 279 mudstone, 305 Afghanistan, 2, 48, 135 Attock thrust, 126, 267 sandstone, 305 age Attock-Cherat Range, 265, 266, 272, Berinag quartzite, 35 conventional, 7 273 Bering Nadi, 253 cooling, 3, 8 Aza Khel Khwar, 269 beryl, 36, 65 fission-track, 8 Besham, 138, 140, 142, 148 spectra, 6 backfolding, 146, 157 deformation, 146 Aghil Formation, 54 backthrusting, 50, 115 metamorphism, 142 Aghil Range, 51 Badrinath peak, 36 Besham antiform, 138 Alaknanda River, 34 Badrinath, 34 Besham Group, 138, 146, 151 Alaska, 80, 91 Baghanwala Formation, 102, 104, basement rocks, 151 albite, 42, 174 105 gneiss, 148 Aleutian Arc, 80, 87 Bagrot, 288 Besham nappe, 151 Aling Valley, 65 Bagrot Valley, 279 Bhaga Valley, 156 allanitc, 57 Bahadur Khcl Formation, 111 Bhagirath Kharak glacier, 34 alluvial plains, 109 Bakhor Das, 64 Bhagirathi leucogranite, 33 alluvium, 104, 109, 110, 269, 288 Baltistan, 203 geochronology, 37 almandinc, 62, 142 Baltoro Glacier, 48, 54, 57, 60, 69 isotopes, 37 Alpurai, 142 Baltoro plutonic unit (BPU), 57,58, model, 42 Alpurai Schist, 139, 140, 142, 147, 62, 69, 70 petrochemistry, 36 148, 151 geochronology, 58 Bhagirathi peak, 35, 36, 37 Altyn Tagh fault, 187 Baltoro region, 47, 69 Bhagirathi pluton, 39, 148 alumino-silicatc, 68 Baluchistan, 135 Bhagirathi River, 34, 35 Amb Formation, 101, 105 banding, 177 Bhagirathi valley, 34 Amc Ges, 284 Banna, 140 Bhaun, 124 amphibolc, 6, 78, 85, 86, 299 Banna Formation, 140 Bhaun section, 118 Bhedabari, 255 pargasitic, 87 Banna sequence, 151 Bheri River, 254,255 amphibolitc, 24, 61, 62, 64, 76, 78, Bannu Depression, 109 Bhilangana valley, 34 133, 137, 138, 142, 148, 173, Bannu Plain, 109, 110 Bhutan, 34, 256 239 Bari Gad Fault, 244, 256,260 amygdular, 65 Bari Gad River, 256, 259 Biafo Glacier region, 47, 48, 58, 69 anatexis, 42, 44 barium, 70 Biafo Gyang Glacier, 193 andalusitc, 36, 68 Baroch Group, 102 biotite, 3, 7, 26, 29, 36, 54, 57, 59, andesite, 76 Baroluma fault, 177, 178 60, 61, 62, 63, 69, 70, 142, anhydrite, 109 basalt, 65, 87 174, 206, 211 Annapurna, 157 pillow, 65 garnet, 57 Annapuma massif, 165 tholeiitic, 165 blueschist, 50, 138, 146, 149, 204, anomalies basement 206 gravity, 221, 225, 227, 239 crystalline, 39, 137, 150, 156, Border Ranges complex 80, 91 negative, 87, 90, 239 165, 173, 180, 221, 225, 226, Borit Jheel, 288 positive, 87, 91 232, 234 Borit Jheel advance, 277 anorthite, 26 granite, 140 BPU. See Baltoro plutonic unit anorthositc, 76, 77, 80 basin brachiopods, 101, 208 apatite, 36, 57, 189 intcrmontane, 183, 184, 193, 221, Brainta Lukpar Glacier, 69 aplite, 10, 57 265, 272, 305 Braldu-Askole area, 70 aplitc-pegmatiic sheets, 49 piggyback, 118, 124, 193 Braldu gorge, 64 aquamarine, 173 pull-apart, 188, 193 Braldu River, 64 arcs Batkor Gah, 288 Braldu Valley, 69, 70, 209 calc-alkaline, 2 Batura advance, 277 Bransfield Strait, 87 environmncnt, 92 Batura plutonic unit, 57 breccias, 77 island, 2 Batura Valley, 279 Broad Peak porphyry, 54 magmatism, 238 Bauma-Harel Formation, 206, 209 Broad Peak Range, 54 argillite, 266, 270 Bauma-Harel line, ¡93 bryozoans, 101, 208 argon, 9, 10 Bauma-Harel Lungma, 208, 209, 210 Budhi schist, 157 Arwa River, 34 bcdrock, 115, 269, 273 Bulache antiform, 177, 178 Arwa valley, 37 norite, 283 Buldar Glacier, 289 ash-flow tuffs, 54 plutonic, 306 Buner Limestone, 138, 140 Asian plate, 31, 76, 137, 203, 209, beds Buner outcrop, 279 213 boulder, 115, 117, 121, 244 Buner terrace, 283 Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/957397/spe232-bm.pdf by guest on 28 September 2021 312 Index Bunhar River alluvium, 104 Chinji-Upper Siwalik interval, dacites, 165 Bunji, 289 135 Dadot Formation, 104 Bunji Canyon, 175, 176, 177 Chinji Village area, 130, 131, 133, Dak Chauki, 288 Bunthang 135 Dak Chauki moraine 279 deposition duration, 304 Chisal Algad, 109 Dakhner Formation, 270 outcrop, 189, 301, 306 Chitral region, 48, 49 Daltumbore Formation, 208, 209, till, 298 chlorite, 35, 142 213 Bunthang sequence, 184, 193, 194, Choa Saidan Shar area, 104 Dang Dun, 253, 255 295,298, 307 Chogolisa Glacier, 61 Darband fault, 271 age, 303 Chogolisa Mountains, 69 Darel-Shatial demagnetization, 302 Chomolungma Thrust, 159 ice mass, 290 lower, 299, 302, 304 Chor Gali Formation, 103, 105 lake beds, 290 middle, 300, 305 chromitite, 77, 80, 85 moraines, 290 upper, 300, 303, 304 chromium, 209 Darel Valley, 283, 289 Buri Khel, 107 Chunda, 193, 299 Darjeeling Himalaya, 244, 261, 262 Burji, 206 Chung La pluton, 34 Darkot Pass plutonic unit, 49, 57 Burji Formation, 206 clastics, 115, 204, 282 Darma fault, 256 Burma arc, 218 clasts Dassu, 65, 211 glacial origin, 117 Dassu Canyon, 176 calc-alkaline, 69 granitic, 117 Dassu felsic gneiss, 65 calc-silicates, 24 limestone, 65, 266 Dassu Gneiss, 211, 214 calcite, 299 quartz, 64 Datta Formation, 99, 102, 107 calcium, 211 sandstone, 119 Daud Khel area, 109 Cambrian clay, 104, 105, 110, 271 decompression, 29 Late, 101 clay-shales, 104, 109 deformation, 68, 113, 146, 173, 177, Middle, 101 claystonc, 299 194, 241, 267, 279 Campbcllporc basin, 266, 273 clinopyroxenc, 80, 81, 84 brittle, 176 carbonate, 54, 64, 115, 142, 159, clinozoisitc, 142 Dchra Dun, 261, 263 204, 206, 283 coal, 103, 104, 110 Deosai Mountains, 184, 298 pedogcnic, 119 conglomerates, 54, 65, 103, 104, Deosai Plateau, 298 shallow-water, 115 105, 106, 107, 109, 119, 121, Deosai region, 193 Carboniferous, 101 140, 204, 206, 208, 266, 279 deposits, 125 Central Crystalline complcx, 73 basal, 101, 146 alluvial, 103, 110, 298 Central Potwar, 134 belts, 64 alluvial-fan, 273 cephalopods, 102 fluvioglacial 101 clastic, 103 Ceratitc Beds, 105 glacial, 101 flood, 270 chalcopyrite, 84 gypsiferous, 104 flood-plain, 271 Chalsa, 251 conodonts, 208 fluvial, 117, 130, 254, 260, 273 Chalsa Cliff, 251 continental shelf, 166 glacial, 176 Chalsa fault, 251 convergence, postcollision, 50 lacustrine, 273, 286, 288 Chambal area, 102 cooling ages, 3, 8 saliferous, 95, 101 Chambal ridge, 103, 104, 124 cooling histories, 9 shelf, 163 Chambal scarp, 104 corals, 101 talus, 255 Chambal structures, 121, 124, 126 cordicritc, 209 terrace, 261 Chambal thrust, 114 corrals, horn, 208 Dhariala, 103, 105 Chamon transform zone, 169 crcnulations, 146 Dhaukgiri Southwest fault, 256, 261 Chandra Valley, 156 Crctaceous, 102 Dhauli Valley, 157 Chani Khcl, 130 crinoids, 208 Dhodha Wahan gorge, 106 Chaudabisc Khola, 260, 261 cross-bcds, trough, 130 Dhodha Wahan section, 107 Chcl River, 244 crust, 2, 3, 9, 23, 30, 48, 60, 70, Dhok Pathan Formation, 120, 121, Chcnab River, 130, 135 71, 155, 165, 167, 189, 191, chert, 204 227, 228, 230, 232, 233, 130, 131, 135 241 Dhok Pathan/Socan, formational Chharat Group, 102, 103 boundary, 119 Chhidru, 101, 111 continental, 3, 8, 42, 44, 60, 70, Dhok Pathan/Tatrot, faunal boundary, Chhidru Formation, 101, 105, 110 169, 180, 204, 218, 221 119 Chhidru Hills, 106 crystalline, 231 diabase, 35 Chichali Formation, 102 foreshortening, 184 diamictite, 277, 279, 286, 290 Chikkim Formation, 166 loading, 115 basal, 298 Chilas, 77, 282, 283, 289 occanic, 10, 49 Dianyor, 288 Chilas Complex, 75, 92, 174, 204 shortening, 70, 180, 241, 262, Dianyor moraine, 288 mineral chcmistry, 78 263 diapirism, 103 origin, 89 stacking, 151 dikes, 36, 37, 54, 57, 60, 68, 69, wholc-rock geochemistry, 87 thickcning, 148, 189, 238, 241 77, 174, 206, 211, 213, Chile, southern, 87 Crystal Peak, 54 Diljabba-Karangal Thrust, 104 Chingkang-la, 62, 69 crystallization, 78 diopside, 60 Chingkang Valley, 64, 65, 68 crystals diorite, 76, 77 Chinji Formation, 109, 122, 130 muscovite, 142 hornblende, 60 Chinji-Nagri, lithostratigraphic suspensions, 77 quartz, 54 boundary, 133 cumulates, 92 Dir River, 76 Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/957397/spe232-bm.pdf by guest on 28 September 2021 Index 313 Dobang, 256 strike-slip, 48, 109, 115, 188, geobarometers, 26, 143 Doda Valley, 156 189, 221, 259 gcothermal activity, 165 Dogra Slates, 3 tear, 2, 31, 104, 109, 110, 115, geothermometer, 63 Doksam scqucncc, 54 180, 181 Ghatte Khola, 261 dolerite, 232 thrust, 24, 31, 106, 115, 146, Ghothamal Canyon, 299, 300, 301 dolomite, 102, 105 155, 185, 187, 191, 225, 238 Ghulkin ice advances, 277 Domeli ridge, 126 fauna, cephalopod, 101 Ghundi, 109 Drang, 279, 284 feldspar, 36, 61, 299 Gilgit, 211 Dras, 91 alkali, 26, 27, 36 Gilgit channel, 288 Dras Volcanics, 76, 165, 204 fibrolite, 69 Gilgit River, 10, 191, 194, 275, dropstone, 279, 300 fields, oil, 111 286, 288 Dubhair, 141 flexure modeling, 228, 232, 234 Gilgit-Skardu line, 191 Dudishal till, 279 flora, 101 Gilgit Valley, 279, 282, 286, 288 Dumordo unit, 64 flow Ginne, 289 dunite, 77 glacial, 194 Ginne Valley, 279 Duns, 253 heat, 165 Giumal Formation, 166 paths, 196 glacial chronology, 291 earthquakes, 186, 188, 189, 262, plastic, 103 glacial erosion, 184, 194, 198, 276, 305 263, 290 fluoritc, 62 eclogite, 30 flux, heat, 149 glacial flow, 194 Eocambrian, 101 flysch, 156, 159, 265 glacial ice, 297 Eocene, 102 folds, 35, 107, 124, 138, 146, 147, glaciation, 184, 194, 196, 276, 305, late, 103 150, 175, 190, 214 307 epidoto, 174, 206 thrust, 114 mountain, 275 equilibrium, hctcrogcneorus, 27 foliation, 61, 68, 70, 176, 177, 211 glaciers, 288, 301, 306 erosion, 3, 30, 102, 103, 104, 106, cross-cut, 174 boulders, 65 110, 113,
Recommended publications
  • 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.
    [Show full text]
  • Habitat Suitability Index (Hsi) Model of Punjab Urial (Ovis Vegnei Punjabiensis) in Pakistan Abstract Introduction
    Suleman et al., The J. Anim. Plant Sci. 30(1):2020 HABITAT SUITABILITY INDEX (HSI) MODEL OF PUNJAB URIAL (OVIS VEGNEI PUNJABIENSIS) IN PAKISTAN S. Suleman*1, W. A. Khan1, K. M. Anjum1, W. Shehzad2 and S. G. M. Hashmi1 1 Department of Wildlife & Ecology, University of Veterinary & Animal Sciences, Lahore, Pakistan. 2 Institute of Biochemistry & Biotechnology, University of Veterinary & Animal Sciences, Lahore, Pakistan. Corresponding author’s email: [email protected] ABSTRACT Unprecedented losses in biodiversity due to habitat loss and fragmentations in the current era have not only alarmed the scientists worldwide but also urged the need to devise suitable conservation strategies which are impossible without understanding the habitat requirements of the concerned species. Among many conservational methods Habitat suitability models are effective for identification of potential habitat and its relationship with the species. Punjab Urial is an endangered mammalian species of Kala Chitta Range and Salt Range in the Punjab, Pakistan. Maxent model was applied to identify the potential habitat by applying 120 sighting point, topographical and current bioclimatic variables. Possible area under receiver operating characteristics curves (AUC) test for current prediction is 0.988 that shows significant correlation between testing points and variables. In Pakistan total 3477 km2 area is suitable for Punjab Urial and potential habitats lie in limited areas in Rawalpindi, Sargodha, Gujrat, Mardan, Swabi, Nowshera, North Wziristan, Bannu, Dera Ismail Khan, Laki-Marwat and some area in Azad Jammu & Kashmir. Habitat of Punjab Urial is shrinking due to certain reasons including habitat fragmentation. In-situ and Ex-situ techniques are the major recommendation for species conservation in suitable and potential habitat of Punjab Urial.
    [Show full text]
  • The Geographic, Geological and Oceanographic Setting of the Indus River
    16 The Geographic, Geological and Oceanographic Setting of the Indus River Asif Inam1, Peter D. Clift2, Liviu Giosan3, Ali Rashid Tabrez1, Muhammad Tahir4, Muhammad Moazam Rabbani1 and Muhammad Danish1 1National Institute of Oceanography, ST. 47 Clifton Block 1, Karachi, Pakistan 2School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 4Fugro Geodetic Limited, 28-B, KDA Scheme #1, Karachi 75350, Pakistan 16.1 INTRODUCTION glaciers (Tarar, 1982). The Indus, Jhelum and Chenab Rivers are the major sources of water for the Indus Basin The 3000 km long Indus is one of the world’s larger rivers Irrigation System (IBIS). that has exerted a long lasting fascination on scholars Seasonal and annual river fl ows both are highly variable since Alexander the Great’s expedition in the region in (Ahmad, 1993; Asianics, 2000). Annual peak fl ow occurs 325 BC. The discovery of an early advanced civilization between June and late September, during the southwest in the Indus Valley (Meadows and Meadows, 1999 and monsoon. The high fl ows of the summer monsoon are references therein) further increased this interest in the augmented by snowmelt in the north that also conveys a history of the river. Its source lies in Tibet, close to sacred large volume of sediment from the mountains. Mount Kailas and part of its upper course runs through The 970 000 km2 drainage basin of the Indus ranks the India, but its channel and drainage basin are mostly in twelfth largest in the world. Its 30 000 km2 delta ranks Pakiistan.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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).
    [Show full text]
  • Asian Journal of Biological and Life Sciences Original Research
    Asian Journal of Biological and Life Sciences Original Research Conserving wildlife, not their clinics: A case study of wild herbal clinic (Berberis) across alpine pastures in Karakoram Mountain Ranges Tika Khan1*, Imtiaz Ahmed Khan2, Abdul Rehman2, Rehmat Karim1 1Integrated Mountain Area Research Centre, Karakoram International University, Pakistan 2Department of Biological Sciences, Karakoram International University, Pakistan E-mail : [email protected] Submitted : 12.10.2014 Accepted : 19.12.2014 Published : 31.12.2014 Abstract Shepherds take care of their livestock but who cares wildlife? Conservation agencies flag certain species which become threatened. Many single- species oriented conservation programmes have negatively impacted, become self-annihilating and causing threats to the concerned species or the others. Ignorance towards wildlife-human synergy level and symbiotic relationship is the core source of ecological imbalance and failure. Several mountain ungulates and carnivores are in conservation list in the area. Almost all of them directly or indirectly rely on Berberis species for their healthcare but none of the conservationist so far thinks of its conservation, which, itself has become critically endangered. It is highly medicinal and serves a wild herbal clinic for wildlife, livestock and humans equally. Berberis pseudumbellata subsp. gilgitica grows above 2500 masl and climbing into the alpine pastures (3500 m). EOO and AOO are less than 100 km2 and 10 km2 respectively. Overgrazing and habitat loss are principal degenerative agents. Besides, long-term conservation of Berberis pseudumbellata subsp. gilgitica, comprehensive studies of these fragile ecosystems are important to make conservation effort more fruitful. Present research will improve knowledge gap to improve overall biodiversity conservation paradigm.
    [Show full text]
  • Geology of the Southern Gandghar Range and Kherimar Hills, Northern Pakistan
    AN ABSTRACT OF THE THESIS OF Michael D. Hylland for the degree of Master of Science in Geology presented on May 3. 1990 Title: Geology of the Southern Gandghar Range and Kherimar Hills. Northern Pakistan Abstract approved: RobeS. Yeats The Gandghar Range and Kherimar Hills, located in the Hill Ranges of northern Pakistan, contain rocks that are transitional between unmetarnorphosed foreland-basin strata to the south and high-grade metamorphic and plutonic rocks to the north. The southern Gandghar Range is composed of a succession of marine strata of probable Proterozoic age, consisting of a thick basal argillaceous sequence (Manki Formation) overlain by algal limestone and shale (Shahkot, Utch Khattak, and Shekhai formations). These strata are intruded by diabase dikes and sills that may correlate with the Panjal Volcanics. Southern Gandghar Range strata occur in two structural blocks juxtaposed along the Baghdarra fault. The hanging wall consists entirely of isoclinally-folded Manki Formation, whereas the footwall consists of the complete Manki-Shekhai succession which has been deformed into tight, northeast-plunging, generally southeast (foreland) verging disharmonic folds. Phyllite near the Baghdarra fault displays kink bands, a poorly-developed S-C fabric, and asymmetric deformation of foliation around garnet porphyroblasts. These features are consistent with conditions of dextral shear, indicating reverse-slip displacement along the fault. South of the Gandghar Range, the Panjal fault brings the Gandghar Range succession over the Kherimar Hills succession, which is composed of a basal Precambrian arenaceous sequence (Hazara Formation) unconformably overlain by Jurassic limestone (Samana Suk Formation) which in turn is unconformably overlain by Paleogene marine strata (Lockhart Limestone and Patala Formation).
    [Show full text]
  • 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
    [Show full text]
  • Concordia & K2
    Tel : +47 22413030 | Epost :[email protected]| Web :www.reisebazaar.no Karl Johans gt. 23, 0159 Oslo, Norway Concordia & K2 Turkode Destinasjoner Turen starter THC Pakistan Islamabad Turen destinasjon Reisen er levert av 21 dager Islamabad Fra : NOK 44 036 Oversikt Unrivalled high mountain scenery and breathtaking views of Pakistan's K2 Reiserute Day 1 Start Islamabad The group flight arrives in Islamabad very early in the morning and we transfer straight to our hotel where rooms will be waiting for you; the rest of the day is free to recover from your journey. Those not flying with the group from London will join us at the hotel in Islamabad during the day. Later in the day, when everyone has arrived, we will have a group briefing. We may also have to visit the Ministry of Tourism for an official briefing.Standard Hotel Day 2 Spectacular flight to Skardu This morning we travel to the airport and take the spectacular flight (weather permitting) across the mountains to Skardu. The rest of the day is free.Standard Hotel Day 3 Free day in Skardu In the morning we will have a walk up to the remains of Skardu fort, which overlooks the town and has great views of the Indus Valley. We will then walk to a small village, which grows all its crops organically. The afternoon is free to explore. You may like to take an optional jeep tour to Satpara Lake (US$65 per person) or explore the bazaar. We may have to visit the Ministry of Tourism for an official briefing later in the day and to have our official documents cleared to start the trek.Standard Hotel Day 4 Drive through spectacular mountain scenery to Askole We set off northwards by jeep up the Shigar valley to Dassu, which used to be the end of the road.
    [Show full text]
  • Part-I: Post Code Directory of Delivery Post Offices
    PART-I POST CODE DIRECTORY OF DELIVERY POST OFFICES POST CODE OF NAME OF DELIVERY POST OFFICE POST CODE ACCOUNT OFFICE PROVINCE ATTACHED BRANCH OFFICES ABAZAI 24550 Charsadda GPO Khyber Pakhtunkhwa 24551 ABBA KHEL 28440 Lakki Marwat GPO Khyber Pakhtunkhwa 28441 ABBAS PUR 12200 Rawalakot GPO Azad Kashmir 12201 ABBOTTABAD GPO 22010 Abbottabad GPO Khyber Pakhtunkhwa 22011 ABBOTTABAD PUBLIC SCHOOL 22030 Abbottabad GPO Khyber Pakhtunkhwa 22031 ABDUL GHAFOOR LEHRI 80820 Sibi GPO Balochistan 80821 ABDUL HAKIM 58180 Khanewal GPO Punjab 58181 ACHORI 16320 Skardu GPO Gilgit Baltistan 16321 ADAMJEE PAPER BOARD MILLS NOWSHERA 24170 Nowshera GPO Khyber Pakhtunkhwa 24171 ADDA GAMBEER 57460 Sahiwal GPO Punjab 57461 ADDA MIR ABBAS 28300 Bannu GPO Khyber Pakhtunkhwa 28301 ADHI KOT 41260 Khushab GPO Punjab 41261 ADHIAN 39060 Qila Sheikhupura GPO Punjab 39061 ADIL PUR 65080 Sukkur GPO Sindh 65081 ADOWAL 50730 Gujrat GPO Punjab 50731 ADRANA 49304 Jhelum GPO Punjab 49305 AFZAL PUR 10360 Mirpur GPO Azad Kashmir 10361 AGRA 66074 Khairpur GPO Sindh 66075 AGRICULTUR INSTITUTE NAWABSHAH 67230 Nawabshah GPO Sindh 67231 AHAMED PUR SIAL 35090 Jhang GPO Punjab 35091 AHATA FAROOQIA 47066 Wah Cantt. GPO Punjab 47067 AHDI 47750 Gujar Khan GPO Punjab 47751 AHMAD NAGAR 52070 Gujranwala GPO Punjab 52071 AHMAD PUR EAST 63350 Bahawalpur GPO Punjab 63351 AHMADOON 96100 Quetta GPO Balochistan 96101 AHMADPUR LAMA 64380 Rahimyar Khan GPO Punjab 64381 AHMED PUR 66040 Khairpur GPO Sindh 66041 AHMED PUR 40120 Sargodha GPO Punjab 40121 AHMEDWAL 95150 Quetta GPO Balochistan 95151
    [Show full text]