Assessment of Indian Pangolin in Potohar Region (2013-14)
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
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. -
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). -
Stratigraphic Analysis of Paleocene and Lower Eocene Rocks Adjacent to the Potwar Plateau, Northern Pakistan
Stratigraphic Analysis of Paleocene and Lower Eocene Rocks Adjacent to the Potwar Plateau, Northern Pakistan By Bruce R. Wardlaw, U.S. Geological Survey Wayne E. Martin, U.S. Geological Survey Iqbal Hussain Haydri, Geological Survey of Pakistan Chapter F of Regional Studies of the Potwar Plateau Area, Northern Pakistan Edited by Peter D. Warwick and Bruce R. Wardlaw Prepared in cooperation with the Geological Survey of Pakistan, under the auspices of the U.S. Agency for International Development, U.S. Department of State, and the Government of Pakistan Bulletin 2078–F U.S. Department of the Interior U.S. Geological Survey iii Contents Abstract .........................................................................................................................................................F1 Introduction.....................................................................................................................................................1 Acknowledgments ................................................................................................................................1 Section Descriptions .....................................................................................................................................2 Paleontologic Control ....................................................................................................................................9 Lithofacies .......................................................................................................................................................9 -
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, -
Conservation of Punjab Urial ( Ovis Vignei Punjabiensis ) Through Long-Term Monitoring of Marked Individuals
Conservation of Punjab urial ( Ovis vignei punjabiensis ) through long-term monitoring of marked individuals Ghulam Ali Awan 2006 A report to the The Rufford Maurice Laing Foundation, London, UK Conservation of Punjab urial ( Ovis vignei punjabiensis ) through long-term monitoring of marked individuals Ghulam Ali Awan Summary The Punjab urial ( Ovis vignei punjabiensis ) is endemic to northern Punjab, Pakistan, and is currently classified as endangered by the IUCN. The distribution of this wild sheep sub-species in Pakistan is betIen the Indus and Jhelum rivers at elevations of 250 -1,500 m primarily in the Kala Chitta and Salt Ranges. The dominant habitat type in the area is dry sub-tropical, semi- evergreen scrub forest. Punjab urial Ire once present over all northern Punjab Mountains, but in recent decades underInt a severe decline in both range and numbers, disappearing from much of their historic range. The main reasons for the rapid decline in numbers appear to be poaching, the capture of newborn lambs that are kept as pets, fragmentation of home ranges, competition with domestic livestock and habitat disturbance and destruction associated with increasing agriculture, forestry and mining. In addition, infusion of exotic but compatible mouflon sheep genes may have occurred. The recent construction of the M-2 Motorway between Islamabad and Lahore created a substantial barrier to seasonal migrations and to dispersal. Poaching can accelerate extinction processes, particularly when driven by commercial gain. The lamb capture and marking was started in 2002 in the community-managed Kalabagh Game Reserve (KGR). RSG grant was used for marking and monitoring of Punjab urial lambs for this ongoing project and particularly for the year 2005. -
Human Activity Mediates Reciprocal Distribution and Niche Separation of Two Sympatric Mongoose Species on the Pothwar Plateau, Pakistan
Turkish Journal of Zoology Turk J Zool (2017) 41: 1045-1058 http://journals.tubitak.gov.tr/zoology/ © TÜBİTAK Research Article doi:10.3906/zoo-1606-34 Human activity mediates reciprocal distribution and niche separation of two sympatric mongoose species on the Pothwar Plateau, Pakistan 1 1, 1 1 2 Riaz HUSSAIN , Tariq MAHMOOD *, Faraz AKRIM , Hira FATIMA , Muhammad Sajid NADEEM 1 Department of Wildlife Management, PMAS-Arid Agriculture University Rawalpindi, Pakistan 2 Department of Zoology, PMAS-Arid Agriculture University Rawalpindi, Pakistan Received: 20.06.2016 Accepted/Published Online: 01.06.2017 Final Version: 21.11.2017 Abstract: Ecologically and morphologically similar species living in sympatry are predicted to partition their resources, although the resources themselves may vary in time and space and in relation to extrinsic factors. We studied two sympatric species of carnivores that vary in their distribution along a gradient of human activity, and one species exploits a wider range of food sources. We recorded the distribution of the small Indian mongoose (Herpestes javanicus) and the gray mongoose (Herpestes edwardsii) through reconnaissance surveys within high, medium, and low human activity areas of the Pothwar Plateau from November 2011 to June 2013. We found that the distribution of the two mongoose species interacted significantly with human activity levels; the small Indian mongoose was highly distributed where human activity level was high and vice versa for the gray mongoose. The gray mongoose showed a wider food niche breadth compared to the small Indian mongoose, while the food niche measured by Pianka’s index overlapped between the two species at 0.95. -
Evaluation of Climate Change Impacts on Rainfall Patterns in Pothohar Region of Pakistan
Water Conservation and Management (WCM) 3(1) (2019) 01-06 Water Conservation & Management (WCM) DOI : http://doi.org/10.26480/wcm.01.2019.01.06 ISSN: 2523-5664 (Print) ISSN: 2523-5672 (Online) CODEN: WCMABD REVIEW ARTICLE EVALUATION OF CLIMATE CHANGE IMPACTS ON RAINFALL PATTERNS IN POTHOHAR REGION OF PAKISTAN Gohar Gulshan Mahmood*, Haroon Rashid, Shafiq Anwar, Abdul Nasir Department of Structures & Environmental Engineering, University of Agriculture Faisalabad, Pakistan-38000 *Corresponding Author Email: [email protected] This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited ARTICLE DETAILS ABSTRACT Article History: Pakistan is a developing country whose economy mainly depends on agriculture which is more susceptible to the effects of climate changes. Due to lack of modern technical resources, Pakistan does not have adequate monitoring Received 24 November 2018 systems for the prediction of likelihood of occurrence of extreme events, or the assessment of possible changes in Accepted 25 December 2018 weather patterns, thus making the task of developing short term response or disaster mitigation strategies Available line 2 January 2019 extremely difficult. Pothohar is a plateau in north-eastern Pakistan, forming the northern part of Punjab including On 4 Attock, Chakwal, Jhehlum, Rawalpindi districts and Islamabad Territory. Pothohar region is a prominent region in Pakistan and consists of important districts. Its agriculture is entirely based on rainfall and no canals are available for the irrigation in this area. Farmers in this area are adversely affected by the changing climate and abrupt changes in rainfall. -
Geology and Geophysics of the Foreland Fold-Thrust Belt of Northwestern Pakistan 1
AN ABSTRACT OF THE THESIS OF James W. McDougall for the degree of Doctor of Philosophy in Geology presented on September 29. 1988 Title: Geology and Geophysics of the Foreland Fold-Thrust Belt of Northwestern Pakistan 1 Abstract approved: Robert S. Yeats Himalayan collision produced frontal and lateral ramps and associated Pliocene to Quaternary tectonic geomorphic features in the foreland fold-thrust belt of northwestern Pakistan. The transpressional right-lateral Kalabagh tear fault zone displaced the emergent Surghar Range frontal thrust from the western Salt Range by 16-19 km since 1.9-2.1 Ma: the age of youngest Siwalik molasse strata erosionally truncated during the southward advance of decollement thrusting. Folds and fanglomerate deposits resulting from decollement thrusting were also cut by the Kalabagh fault. North of the eastern Surghar Range, the N15W-trending Kalabagh fault bends to the west into north-dipping thrust faults that sole out beneath the southern Kohat Plateau. Foreland subsidence associated with the southward advance of thrusting controlled the distribution of Indus River conglomerates during the late Pliocene and Quaternary. Uplift in the northern Kalabagh fault zone diverted the Indus river eastward to its present course. South of the Main Boundary thrust (MBT) and west of the Indus River, decollement thrusting dominated by layer-parallel slip of as much as 32 km on a single thrust fault emplaced blind thrust sheets and fault-bend folds. Balanced cross sections show over 50% line-length shortening in sedimentary strata between the top of the basement and the base of the elastic wedge of the Murree and Kamlial formations and the Siwalik Group. -
Pakistan Studies/Affairs: Most Important Mcqs (Set V) for CSS, PMS, PCS, NTS
Pakistan Studies/Affairs: Most Important MCQs (Set V) for CSS, PMS, PCS, NTS The length of Kala Chitta Range is: (a) 62 km (b) 72 km (c) 82 km (d) None of these Answer: b Where is Nanga Parbat situated? (a) Himalayan range (b) Hindukash range (c) Karakoram range (d) None of these Answer: a In which area the Nanga Parbat is situated? (a) Gilgit-Baltistan (b) Khyber Pakhtunkhwa (c) FATA (d) Balochistan Answer: a The Chinese province adjoining to Pakistan is: (a) Ching Chee (b) Sinkiang (c) Minking (d) None of these Answer: b Check Also: Important and Most Wanted MCQs about Current Federal Cabinet of Pakistan Which range of Pakistan is called “Roof of the World”? (a) Pamir (b) Karakoram (c) Himalayas (d) None of these Answer: a Which range links Pakistan with China? (a) Hindukush Downloaded from www.csstimes.pk | 1 Pakistan Studies/Affairs: Most Important MCQs (Set V) for CSS, PMS, PCS, NTS (b) Karakoram (c) Himalayas (d) None of these Answer: b What is the area of Potwar Plateau? (a) 600 sq km (b) 700 sq km (c) 800 sq km (d) None of these Answer: b The elevation of Potwar Plateau is: (a) 200-400 metres (b) 300-600 metres (c) 400-700 metres (d) 500-800 metres Answer: b The height of Tilla Jogian Hill is: (a) 775 metres (b) 975 metres (c) 1075 metres (d) 1275 metres Answer: b What is the average height of Salt Range? (a) 2200 ft (b) 2000 ft (c) 1800 ft (d) 1600 ft Answer: a The most complete geologic sequence in the world is: (a) Salt Range (b) Karakoram Range (c) Himalyas Range (d) None of these Answer: a Downloaded from www.csstimes.pk -
U.S. Department of the Interior U.S. Geological
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE ISLAMABAD-RAWALPINDI AREA, PUNJAB, NORTHERN PAKISTAN by Van S. Williams1 and Mustafa K. Pasha2 and Iqbal M. Sheikh2 Open-File Report 99-47 Report prepared jointly by the U.S. Geological Survey and the Geological Survey of Pakistan under the auspices of the U.S. Agency for International Development This report is preliminary and has not been reviewed for conformity with the U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. AUTHOR AFFILIATIONS 1 U.S. Geological Survey 2 Geological Survey of Pakistan Base Credit: Base from Survey of Pakistan, Islamabad and Surroundings, 1985 Place names used in this report do not necessarily conform with names approved by the U.S. Board on Geographic Names Geology credit: Geology mapped and compiled in 1988-90 by I.M. Sheikh, M.K. Pasha, and V.S. Williams; with help from S. Qamar Reza, Kanwar Sabir Ali Khan, and Akram M. Bhatti. DESCRIPTION OF MAP UNITS Qal Stream-channel alluvium (Holocene)--Unconsolidated gravel, sand, and silt that is subject to stream transport each year. Poorly to moderately sorted and low-angle crossbedding. Generally without soil or vegetation. Forms low islands and bars within braided ard meandering stream channels. Maximum thickness about 3 m Qfp Flood-plain and fan alluvium (Holocene)--Moderately bedded and sorted, sand and gravel channel and debris-flow deposits overlain by thin veneer of sandy silt and clay fro~a overbank flooding and slope-wash deposition. -
Regional Studies of the Potwar Plateau Area, Northern Pakistan
Regional Studies of the Potwar Plateau Area, Northern Pakistan Edited by Peter D. Warwick and Bruce R. Wardlaw Prepared in cooperation with the Geological Survey of Pakistan, under the auspices of the U.S. Agency for International Development, U.S. Department of State, and the Government of Pakistan This volume is published as chapters A through I. The chapters are also available separately on the World Wide Web. Bulletin 2078 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2007 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1–888–ASK–USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1–888–ASK–USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citations: Warwick, P.D., and Wardlaw, B.R., eds., 2007, Regional studies of the Potwar Plateau area, northern Pakistan: U.S. Geological Survey Bulletin 2078–A–I, chapters are separately paged, 5 oversize plates in pocket. (Also available online.) Edwards, L.E., 2007, Paleocene and Eocene dinocysts from the Salt Range, Punjab, northern Pakistan, chap. -
Department of the Interior U.S. Geological Survey Mineralogy and Thermal Properties of Clay Deposits in the Salt Range and Kala
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY MINERALOGY AND THERMAL PROPERTIES OF CLAY DEPOSITS IN THE SALT RANGE AND KALA CHITTA RANGE, PUNJAB PROVINCE, PAKISTAN Gene Whitney1, Syed Qamar Abbas2, and Kenneth Esposito 1 U.S. Geological Survey Open-File Report 90-657 Report prepared jointly by the Geological Survey of Pakistan and the U.S. Geological Survey under the auspices of the U.S. Agency for International Development. This report is preliminary and has not been reviewed for conformity with the U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1 U.S. Geological Survey, Box 25046, Denver Federal Center, Denver, Colorado 80225 2 Ministry of Petroleum and Natural Resources, Geological Survey of Pakistan, Lahore, Pakistan 54590 MINERALOGY AND THERMAL PROPERTIES OF CLAY DEPOSITS IN THE SALT RANGE AND KALA CHITTA RANGE, PUNJAB PROVINCE, PAKISTAN Gene Whitney, Syed Qamar Abbas, and Kenneth Esposito INTRODUCTION The Salt Range and Kala Chitta Range, Pakistan, contain many small deposits of laterite, bauxite, bentonite, and other economic clay deposits. Many of these deposits are located in remote and inaccessible areas and therefore have not been well studied or exploited. Others deposits have been very well characterized. The present examination of the clay deposits of the Salt Range and Kala Chitta Range was undertaken as part of a cooperative geological research program between the Geological Survey of Pakistan and the U.S. Geological Survey (Punjab Regional Framework Program), funded by the government of Pakistan and the U.S. Agency for International Development. The purpose of this study is to provide an internally consistent mineralogical and thermal data set for a broad sampling of the clay deposits in the Salt Range and Kala Chitta Range, Punjab.