Geodesy and Great Earthquakes in the Himalaya, by Roger Bilham a New Quaternary Strand of the Karakoram Fault System, Ladakh Himalayas, by Wendy M

Total Page:16

File Type:pdf, Size:1020Kb

Geodesy and Great Earthquakes in the Himalaya, by Roger Bilham a New Quaternary Strand of the Karakoram Fault System, Ladakh Himalayas, by Wendy M In Cooperation with the National Science Foundation, San Francisco State University and Stanford University, the California Academy of Sciences, and University of California Santa Cruz Proceedings of the 25th Himalaya- Karakoram-Tibet Workshop Edited by Mary L. Leech, Simon L. Klemperer, and Walter D. Mooney Open-File Report 2010-1099 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia 2010 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 Suggested citation: Leech, Mary L., Klemperer, Simon L., and Mooney, Walter D., eds., 2010, Proceedings of the 25th Himalaya- Karakoram-Tibet Workshop: U.S. Geological Survey Open-File Report 2010-1099 [http://pubs.usgs.gov/of/2010/1099/]. 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 material contained within this report. Cover: Everest from base camp in Tibet. Photograph by Mary Leech Contents Preface to Proceedings of the 25th Himalaya-Karakoram-Tibet Workshop, by Mary L. Leech, Simon L. Klemperer, and Walter D. Mooney Historical (<2000 B.P.) and Recent Glacier Fluctuations in the Inner Himalaya (North of the Annapurna and Dhaulagiri Himalaya), by Hermann Achenbach Landscape Evolution of the Bhutan Himalaya — Insights from Tectonic Geomorphology and Low- Temperature Thermochronology, by Byron A. Adams, Matthijs C. van Soest, Kip V. Hodges, Kelin X. Whipple, and Arjun Heimsath Testing Earthquake Nucleation Models from the Response of Himalayan Seismicity to Secular and Periodic Stress Variations, by Thomas Ader, Jean-Philippe Avouac, and Sachiko Tanaka Shear-Velocity Profiles Across the Tibetan Plateau from Broadband, Surface-Wave, Phase- Velocity Measurements, by Matthew R. Agius, and Sergei Lebedev Geochemical and Isotopic Constraints on the Nature of the Indus and Shyok Suture Zones, Remnants of the Neo-Tethyan Ocean in the Trans-Himalayan Region, by Talat Ahmad Structural Analysis of Swat and the Surrounding Peshawar Basin, North Pakistan: Application of GIS and Remote Sensing, by Irshad Ahmad, Joseph A. DiPietro, Shuhab D. Khan, and Noor Jehan Clockwise Rotation and Tilting in the Tethyan Himalaya of SE Tibet Deduced from Paleomagnetic data: Implications for the Miocene Tectonic Evolution of the NE Himalaya, by Borja Antolín, Erwin Appel, Richard Gloaguen, István Dunkl, Chiara Montomoli, Lin Ding, Ursina Liebke, and Qiang Xu Organic Matter Studies for Hydrocarbon Generation in the Argillaceous Sediments of the Ladakh Himalaya, India, by A.K.Awasthi, M.K.Moezabadi, A.K.Jain, and S.Singh Timing of Earliest India-Asia Contact: Evidence of Terrestrial Vertebrates from Cambay Shale, Gujarat, Western Peninsular India, by Sunil Bajpai Thinning of Glaciers in the Khumbu Himal from 1955 to 2008, by Adam D. Barker and Bernard Hallet Himalayan-Tibetan Orogeny: Channel Flow versus (Critical) Wedge Models, a False Dichotomy?, by Christopher Beaumont and Rebecca Jamieson Petrology and geochemistry of the Xiugugabu ophiolitic massif, western Yarlung Zangbo Suture Zone, Tibet, by Rachel Bezard, Réjean Hébert, Chengshan Wang, Jaroslav Dostal, and Jingen Dai Geodesy and Great Earthquakes in the Himalaya, by Roger Bilham A New Quaternary Strand of the Karakoram Fault System, Ladakh Himalayas, by Wendy M. Bohon, Kip V. Hodges, J Ramon Arrowsmith, and Alka K. Tripathy Simultaneous Earthquake Pulses along the Main Himalayan Thrust, by Laurent Bollinger, Dili Ram Tiwari, Sudhir Rajaure, Soma Nath Sapkota, and Jean-Phillipe Avouac The INDEPTH Transect: Looking Back from Golmud to Yadong, by Larry D. Brown, Wenjin Zhao, and the Project INDEPTH Team iii Receiver Function Imaging in the Western Himalaya, by Warren B. Caldwell, Simon L. Klemperer, Jesse F. Lawrence, and Shyam S. Rai Seasonal Variations in Geodetic Strain Induced by Hydrological Surface Loading in the Himalaya and Implications for Shallow Elastic Structure of the Earth, by Kristel Chanard, Jean-Philippe Avouac, Takeo Ito, Jeff Genrich, John Galetzka, Mireille Flouzat, Som Nath Sapkota, and Bharat Koirala The Golmud Step: New Details of the 15 km Moho Offset Between the Tibet Plateau and Qaidam Basin from INDEPTH IV Seismic Results, by Chen Chen, Larry Brown, Marianne Karplus, and Simon Klemperer The Determination of Anisotropic Parameters from Wide-Angle Seismic Reflection Polarizations: A Model Study, by Jingyi Chen, Zhongjie Zhang, and José Badal Fault Histories of the Northeastern Tibetan Plateau Margin: Geodynamic Implications of Far- Field Deformation During Continental Collision, by Marin K. Clark, Alison R. Duvall, Nora Lewandowski, Eric A. Hetland, Dewen Zheng, Richard O. Lease, William Craddock, Eric Kirby,and Zhicai Wang Metamorphic History of the South Tibetan Detachment System, Mt. Everest Region, Revealed by RSCM Thermometry and Phase Equilibria Modeling, by John M. Cottle, David J. Waters, Olivier Beyssac, and Micah J. Jessup Quaternary Slip History for the Central Altyn Tagh Fault Reveals Time-Varying Slip Rate, by Eric Cowgill, Ryan D. Gold, J. Ramon Arrowsmith, Xuanhua Chen, and Xiao-Feng Wang Oligo-Miocene Basins in Central Tibet and Along the Indus Suture: Records of Plateau Evolution and Dynamics of Subducting Indian Continental Crust, by P.G. DeCelles, P. Kapp, J. Quade, G.E. Gehrels, and M. Murphy Was There Pre-Collisional Metamorphism in Swat Pakistan?, by Joseph A. DiPietro and Alex Pullen Muscovite, by Michael Doon, Djordje Grujic, Isabelle Coutand, and Nicholas Whynot Superposed Folds in the Himalaya Indicating Late Stages of the Himalayan Orogeny: Implications for Seismicity, by Ashok Kumar Dubey Tectono-Geomorphic and Climatic Controls on Landscape Development in the Lesser Himalaya, by C.S. Dubey, M. Tajbaksh, R. Marston, E.J. Catlos, Sandeep Singh, and M. Rogibala Pleistocene-Holocene Climate Fluctuations and Fluvial Response in the Tectonically Active Yamuna Valley, North-Western Himalaya: Timescales and Source-to-Sink Interlinkage, by Sharat Dutta, N. Suresh, and Rohtash Kumar Eocene Faulting in Northeastern Tibet: Insights from Coupled Low-Temperature Thermochronometry and Ar Dating of Fault Gouge along the West Qinling Fault, by Alison R. Duvall, Marin K. Clark, Ben van der Pluijm, and Chuanyou Li Centrifuge Modelling Study of Contrasting Structural Styles in Salt Range and Potwar Plateau, Northern Pakistan, by Shah Faisal and John M. Dixon Mid-Miocene Climate-Driven Rapid Erosion of the Northern Tibetan Plateau, by Xiaomin Fang, Chunhui Song, Weilin Zhang, Erwin Appel, Junping Gao, and Maodu Yan iv Can Detrital Tourmaline Provide Stratigraphic Fingerprints? Initial Tests in the Western Himalaya, by Xuan Feng, A. Alexander G. Webb, and Darrell J. Henry Present-Day Vertical Motion of the Tibetan Plateau and Surrounding Area, by Jeffrey T. Freymueller, Yuning Fu, Wang Qi, and Xu Caijun Geometry and Slip Patterns of the Main Himalaya Thrust Fault in the India-Eurasia Collistion Zone Constrained by Geodetic Observations, by Yuning Fu, Jeffrey T. Freymueller, Caijun Xu, and Qi Wang SINOPROBE Deep Seismic Reflection Profiling across the Bangong-Nujiang Suture, Central Tibet, by Rui Gao, Zhanwu Lu, Xiong Xiaosong, Lingsen Zeng, Wenhui Li, Gong Deng, and Simon L. Klemperer Construction of the Tibetan Plateau by Distributed Lithospheric-Scale Shortening: Evidence from Deep Seismic-Reflection Profiling across Northeastern Tibet, by Rui Gao, Cheng-Shan Wang, An Yin, Haiyan Wang, and Yuxiu Zhang Tertiary Eclogite Facies Metamorphism in the Greater Himalayan Sequence: Evidence from Zircon U-Pb Geochronology and Trace Element Geochemistry, by Djordje Grujic, Clare Warren, and Joseph L. Wooden Erosion Rates at the Crest of the Himalaya: Slow or Fast?, by Bernard Hallet, Peter K. Zeitler, Peter O. Koons, Noah J. Finnegan, and Adam D. Barker An Integrated Approach to Determining the Crustal Thickness History of Southern Tibet, by T.M. Harrison, D.J. DePaolo, X. Mo, Z. Zhao, and A. Yin Geochemical Comparison of North Himalayan Gneiss Domes, by William C. Hassett, John W. Sommerfeld, Forrest M. Horton, and Mary L. Leech Uplift and Exhumation along the Arun River (Eastern Nepal): Implications for the Mechanism of Uplift of the High Himalaya and the Coupling between Erosion and Tectonics, by Itai Haviv, Jean-Philippe Avouac, Kenneth A. Farley, Mark T. Harrison, Matthew T. Heizler, Neupane C. Prabhat, and Gweltaz Mahéo Ophiolites Associated with Suture Zones of the Collisional System between India and Eurasia: a Synthesis, by Réjean Hébert, Carl Guilmette, Rachel Bezard, Jarosalv Dostal, Chengshan Wang, and Jingen Dai Towards Defining the Transition in Style and Timing of Quaternary Glaciation between the Monsoon-Influenced Greater Himalaya and the Semi-Arid Transhimalaya of Northern India, by Kathryn A. Hedrick, Yeong Bae Seong, Lewis A. Owen, Marc W. Caffee, and Craig Dietsch The Tibet-Himalaya Accommodation Zone and the Nature of Orogenic Plateau Margins, by K.V. Hodges and K.X. Whipple Preliminary Fault Slip-Rate Estimate for the Right-Lateral Beng Co Strike-Slip Fault, based on Quaternary
Recommended publications
  • Not Eligible) - General
    LIST OF STUDENTS UNDER SPECIAL SCHOLARSHIP SCHEME FOR J&K 2013-14 (NOT ELIGIBLE) - GENERAL DATE S.N CA FIRST MIDDLE LAST CATEG COLLEGE FATHER’S OF COURSE NAME REASON O. NID NAME NAME NAME NAME ORY NAME BIRTH ABHILASHI SHAKEEL 13-11- ORIGINAL DOMICILE, INCOME CERTIFICATE 1 SHADAB AHMAD MANHAS SEBC GROUP OF B PHARMA MANHAS 1996 NOT PRODUCED INSTITUTE ABHILASHI GH MOHD. 01/01/19 ORIGINAL INCOME CERTIFICATE NOT 2 ABID HUSSAIN RATHER OPEN GROUP OF B.PHARMA RATHER 95 PRODUCED INSTITUTE ADESH 455 SH. CHUNI 7-FEB- B.SC MRI CT 3 VISHALI . SHARMA OPEN UNIVERSITY,B INCOME CERTIFICATE NOT PRODUCED 58 LAL 1995 TECHNOLOGY ATHINDA MANZOOR ADESH 459 MEHWIS MANZOO 31-MAR- BACHELOR 4 KHAN AHMAD OPEN UNIVERSITY,B INCOME CERTIFICATE NOT PRODUCED 15 H R 1993 PHYSIOTHERAPY(BPT) KHAN ATHINDA ADHUNIK MOHD INSTITUTE OF 385 8-MAR- 5 AZAD ASHRAF KAWA ASHRAF OPEN EDUCATION & BCA DOMICILE CERTIFICATE NOT PRODUCED 41 1994 KAWA RESEARCH, GHAZIABAD SH. ALWAR 405 BURHA IRSHAD 6-AUG- 6 IRSHAD DEV OPEN PHARMACY B.PHARMACY MANAGEMENT QUOTA 82 N AHMAD 1994 COLLEGE DEV ALWAR 405 MUZAMI SH. MOHD 28-SEP- 7 AYOOB AYOOB SEBC PHARMACY B.PHARMACY MANAGEMENT QUOTA 97 L AYOOB 1996 COLLEGE MUNEER AMAR JYOTI 399 MEHREE 1-JUL- BACHLOR IN 8 SYED MUNEER AHMAD OPEN CHARITABLE PROOF OF ADMISSION IS NOT SUBMITTED 84 N 1991 PHYSIOTHERAPY NAQASH TRUST AMITY LAW 474 MOHAN 18-JUL- 9 TARUN MOHAN SHARMA OPEN SCHOOL BA LLB 12TH FROM OUTSIDE J&K 34 LAL 1994 NOIDA AMRITSAR COLLEGE OF AB 427 16-FEB- HOTEL 10 AABID QAYOOM QAYOOM OPEN B.SC INCOME CERTIFICATE NOT PRODUCED 53 1995 MANAGEMENT WANI AND
    [Show full text]
  • Ecosystem Services Changes Between 2000 and 2015 in the Loess Plateau, China: a Response to Ecological Restoration
    RESEARCH ARTICLE Ecosystem services changes between 2000 and 2015 in the Loess Plateau, China: A response to ecological restoration Dan Wu1, Changxin Zou1, Wei Cao2*, Tong Xiao3, Guoli Gong4 1 Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing, China, 2 Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, China, 3 Satellite Environment Center, Ministry of Environmental Protection, Beijing, China, 4 Shanxi Academy of Environmental Planning, Taiyuan, China a1111111111 a1111111111 * [email protected] a1111111111 a1111111111 a1111111111 Abstract The Loess Plateau of China is one of the most severe soil and water loss areas in the world. Since 1999, the Grain to Green Program (GTGP) has been implemented in the region. This OPEN ACCESS study aimed to analyze spatial and temporal variations of ecosystem services from 2000 to Citation: Wu D, Zou C, Cao W, Xiao T, Gong G 2015 to assess the effects of the GTGP, including carbon sequestration, water regulation, (2019) Ecosystem services changes between 2000 soil conservation and sand fixation. During the study period, the area of forest land and and 2015 in the Loess Plateau, China: A response grassland significantly expanded, while the area of farmland decreased sharply. Ecosystem to ecological restoration. PLoS ONE 14(1): services showed an overall improvement with localized deterioration. Carbon sequestration, e0209483. https://doi.org/10.1371/journal. pone.0209483 water regulation and soil conservation increased substantially. Sand fixation showed a decreasing trend mainly because of decreased wind speeds. There were synergies Editor: Debjani Sihi, Oak Ridge National Laboratory, UNITED STATES between carbon sequestration and water regulation, and tradeoffs between soil conserva- tion and sand fixation.
    [Show full text]
  • Optical and Physical Characteristics of the Lowest Aerosol Layers Over the Yellow River Basin
    atmosphere Article Optical and Physical Characteristics of the Lowest Aerosol Layers over the Yellow River Basin Miao Zhang 1,*, Jing Liu 2, Muhammad Bilal 3,* , Chun Zhang 1, Feifei Zhao 1, Xiaoyan Xie 4,5 and Khaled Mohamed Khedher 6,7 1 School of Environmental Science and Tourism, Nanyang Normal University, Wolong Road No.1638, Nan Yang 473061, China; [email protected] (C.Z.); zff@nynu.edu.cn (F.Z.) 2 Lingnan College, Sun Yat-sen University, Guangzhou 510275, China; [email protected] 3 School of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 2100444, China 4 South China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Guangzhou 510300, China; [email protected] 5 College of Marine Science, Shanghai Ocean University, Shanghai 201306, China 6 Department of Civil Engineering, College of Engineering, King Khalid University, Abha 61421, Saudi Arabia; [email protected] 7 Department of Civil Engineering, Institut Superieur des Etudes Technologiques, Campus Universitaire Mrezgua, Nabeul 8000, Tunisia * Correspondence: [email protected] (M.Z.); [email protected] (M.B.) Received: 17 September 2019; Accepted: 19 October 2019; Published: 22 October 2019 Abstract: Studying the presence of aerosols in different atmospheric layers helps researchers understand their impacts on climate change, air quality, and human health. Therefore, in the present study, the optical and physical properties of aerosol layers over the Yellow River Basin (YERB) were investigated using the CALIPSO Level 2 aerosol layer products from January 2007 to December 2014. The Yellow River Basin was divided into three sub-regions i.e., YERB1 (the plain region downstream of the YERB), YERB2 (the Loess Plateau region in the middle reaches of the YERB), and YERB3 (the mountainous terrain in the upper reaches of the YERB).
    [Show full text]
  • Preliminary Assessment of Large Mammals in the Namcha Barwa Region of South-Eastern Tibet
    ORYX VOL 30 NO 1 JANUARY 1996 Preliminary assessment of large mammals in the Namcha Barwa region of south-eastern Tibet Qiu Ming Jiang and William V. Bleisch In 1994 the authors made two rapid assessments of wildlife in the remote Namcha Barwa region, south-eastern Tibet, China. They conducted interviews, examined and recorded trophies in the possession of local Menba, Luoba and Kangba Tibetans and made opportunistic field observations. Despite the extensive forests in this extremely remote region, wildlife populations appeared to be low except in inaccessible areas along county borders. Frequent reports of tiger predation on cattle, horses and mules in glaciated valleys on the south slope of the Himalayas may indicate a shortage of natural prey. Uncontrolled hunting, human population growth and expedient economic development threaten the survival of large mammals in the region. Habitat ized by Terminalia myriocarpa, Lagerstroemia minuticarpa, Garcinia morella, Sloanea sinensis, The Namcha Barwa region lies within the Fissistigma oldhamii and other broadleaved Linzhi District in the south-east of the Xizang evergreen species. The trees Alingia sp., (Tibetan) Autonomous Region in China Actinodaphne lancifolia and Cryptocarya chinen- (Figure 1). Zoogeographically, it lies at the sis form an understorey. Between 1100 and junction of the Eastern Himalayas, the 2500 m there are well-developed subtropical, Qinghai-Xizang Plateau, the Hengduan montane, broadleaved forests, containing oak Mountains and the Assam Region (Zhang et Quercus tungmaiensis and evergreen chinkap- ah, 1982). The Yarlung Tsangpo River (the ins Castanopsis xizangensis and C. lamellosa. Brahmaputra in India) runs from west to east, Alder Alnus nepalensis and birch Betula utilis cutting through a range of high mountains dominate the lower slopes and valley bottoms.
    [Show full text]
  • On Bhutanese and Tibetan Dzongs **
    ON BHUTANESE AND TIBETAN DZONGS ** Ingun Bruskeland Amundsen** “Seen from without, it´s a rocky escarpment! Seen from within, it´s all gold and treasure!”1 There used to be impressive dzong complexes in Tibet and areas of the Himalayas with Tibetan influence. Today most of them are lost or in ruins, a few are restored as museums, and it is only in Bhutan that we find the dzongs still alive today as administration centers and monasteries. This paper reviews some of what is known about the historical developments of the dzong type of buildings in Tibet and Bhutan, and I shall thus discuss towers, khars (mkhar) and dzongs (rdzong). The first two are included in this context as they are important in the broad picture of understanding the historical background and typological developments of the later dzongs. The etymological background for the term dzong is also to be elaborated. Backdrop What we call dzongs today have a long history of development through centuries of varying religious and socio-economic conditions. Bhutanese and Tibetan histories describe periods verging on civil and religious war while others were more peaceful. The living conditions were tough, even in peaceful times. Whatever wealth one possessed had to be very well protected, whether one was a layman or a lama, since warfare and strife appear to have been endemic. Security measures * Paper presented at the workshop "The Lhasa valley: History, Conservation and Modernisation of Tibetan Architecture" at CNRS in Paris Nov. 1997, and submitted for publication in 1999. ** Ingun B. Amundsen, architect MNAL, lived and worked in Bhutan from 1987 until 1998.
    [Show full text]
  • Late Cenozoic-Recent Tectonics of the Southwestern Margin of the Tibetan Plateau, Ladakh, Northwest India
    Late Cenozoic-recent tectonics of the southwestern margin of the Tibetan Plateau, Ladakh, northwest India by Wendy Bohon A Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy Approved April 2014 by the Graduate Supervisory Committee: Kip Hodges Ramon Arrowsmith Arjun Heimsath Kelin Whipple Stephen Reynolds ARIZONA STATE UNIVERSITY May 2014 DEDICATION This work is dedicated to my grandmother, Eunice Waterfield Boyette, who was a model of perseverance and dedication, and to my parents, Dean and Linda Bohon, who always believed I could do anything. i ACKNOWLEDGMENTS First, I need to give a sincere and hearty thank you to my advisors, Ramon Arrowsmith and Kip Hodges. You have both been incredible sources of inspiration and support, and I am grateful for your guidance during this processes. I would also like to thank my committee, Kelin Whipple, Arjun Heimsath, and Steve Reynolds for providing mentorship and support for the last several (or more!) years. I must also give a special acknowledgement to Matthijs van Soest and Jo-Anne Wartho for their patience and mentorship in the laboratory. I would also like to thank Thijs for many informative and helpful discussions about my data. I must also thank the JMARS team, especially Chris Edwards and Scott Dickenshied, for their help with all aspects of the ASTER remote sensing. My advisors and other mentors have been amazing, but my fellow graduate students also deserve special recognition for the integral part they have played in my educational journey. Many thanks to all of the students in the Hodges and Arrowsmith research groups- and to the larger surfaces processes crew- especially the folks in Room 603.
    [Show full text]
  • VIII. Arbitrary Arrest and Detention
    HUMAN RIGHTS UNDER CHINA’S SHADOW Mistreatment of Tibetans in Nepal WATCH Under China’s Shadow Mistreatment of Tibetans in Nepal Copyright © 2014 Human Rights Watch All rights reserved. Printed in the United States of America ISBN: 978-1-62313-1135 Cover design by Rafael Jimenez Human Rights Watch is dedicated to protecting the human rights of people around the world. We stand with victims and activists to prevent discrimination, to uphold political freedom, to protect people from inhumane conduct in wartime, and to bring offenders to justice. We investigate and expose human rights violations and hold abusers accountable. We challenge governments and those who hold power to end abusive practices and respect international human rights law. We enlist the public and the international community to support the cause of human rights for all. Human Rights Watch is an international organization with staff in more than 40 countries, and offices in Amsterdam, Beirut, Berlin, Brussels, Chicago, Geneva, Goma, Johannesburg, London, Los Angeles, Moscow, Nairobi, New York, Paris, San Francisco, Tokyo, Toronto, Tunis, Washington DC, and Zurich. For more information, please visit our website: http://www.hrw.org MARCH 2014 978-1-62313-1135 Under China’s Shadow Mistreatment of Tibetans in Nepal Map of Nepal .................................................................................................................... i Summary ......................................................................................................................... 1
    [Show full text]
  • OU1901 092-099 Feature Cycling Ladakh
    Cycling Ladakh Catching breath on the road to Rangdum monastery PICTURE CREDIT: Stanzin Jigmet/Pixel Challenger Breaking the There's much more to Kate Leeming's pre- Antarctic expeditions than preparation. Her journey in the Indian Himalaya was equally about changing peoples' lives. WORDS Kate Leeming 92 93 Cycling Ladakh A spectacular stream that eventually flows into the Suru River, on the 4,000m plains near Rangdum nergy was draining from my legs. My heart pounded hard and fast, trying to replenish my oxygen deficit. I gulped as much of the rarified air as I could, without great success; at 4,100m, the atmospheric oxygen is at just 11.5 per cent, compared to 20.9 per cent at sea level. As I continued to ascend towards the snow-capped peaks around Sirsir La pass, the temperature plummeted and my body, drenched in a lather of perspiration, Estarted to get cold, further sapping my energy stores. Sirsir La, at 4,828m, is a few metres higher than Europe’s Mont Blanc, and I was just over half way up the continuous 1,670m ascent to get there. This physiological response may have been a reality check, but it was no surprise. The ride to the remote village of Photoksar on the third day of my altitude cycling expedition in the Indian Himalaya had always loomed as an enormous challenge, and I was not yet fully acclimatised. I drew on experience to pace myself: keeping the pedals spinning in a low gear, trying to relax as much as possible and avoiding unnecessary exertion.
    [Show full text]
  • LIST of INDIAN CITIES on RIVERS (India)
    List of important cities on river (India) The following is a list of the cities in India through which major rivers flow. S.No. City River State 1 Gangakhed Godavari Maharashtra 2 Agra Yamuna Uttar Pradesh 3 Ahmedabad Sabarmati Gujarat 4 At the confluence of Ganga, Yamuna and Allahabad Uttar Pradesh Saraswati 5 Ayodhya Sarayu Uttar Pradesh 6 Badrinath Alaknanda Uttarakhand 7 Banki Mahanadi Odisha 8 Cuttack Mahanadi Odisha 9 Baranagar Ganges West Bengal 10 Brahmapur Rushikulya Odisha 11 Chhatrapur Rushikulya Odisha 12 Bhagalpur Ganges Bihar 13 Kolkata Hooghly West Bengal 14 Cuttack Mahanadi Odisha 15 New Delhi Yamuna Delhi 16 Dibrugarh Brahmaputra Assam 17 Deesa Banas Gujarat 18 Ferozpur Sutlej Punjab 19 Guwahati Brahmaputra Assam 20 Haridwar Ganges Uttarakhand 21 Hyderabad Musi Telangana 22 Jabalpur Narmada Madhya Pradesh 23 Kanpur Ganges Uttar Pradesh 24 Kota Chambal Rajasthan 25 Jammu Tawi Jammu & Kashmir 26 Jaunpur Gomti Uttar Pradesh 27 Patna Ganges Bihar 28 Rajahmundry Godavari Andhra Pradesh 29 Srinagar Jhelum Jammu & Kashmir 30 Surat Tapi Gujarat 31 Varanasi Ganges Uttar Pradesh 32 Vijayawada Krishna Andhra Pradesh 33 Vadodara Vishwamitri Gujarat 1 Source – Wikipedia S.No. City River State 34 Mathura Yamuna Uttar Pradesh 35 Modasa Mazum Gujarat 36 Mirzapur Ganga Uttar Pradesh 37 Morbi Machchu Gujarat 38 Auraiya Yamuna Uttar Pradesh 39 Etawah Yamuna Uttar Pradesh 40 Bangalore Vrishabhavathi Karnataka 41 Farrukhabad Ganges Uttar Pradesh 42 Rangpo Teesta Sikkim 43 Rajkot Aji Gujarat 44 Gaya Falgu (Neeranjana) Bihar 45 Fatehgarh Ganges
    [Show full text]
  • A Study on Tectonic and Sedimentology in Order to Fault Rupture Potential in Coasts the Makran Sea
    Open Journal of Geology, 2017, 7, 1269-1286 http://www.scirp.org/journal/ojg ISSN Online: 2161-7589 ISSN Print: 2161-7570 A Study on Tectonic and Sedimentology in Order to Fault Rupture Potential in Coasts the Makran Sea Mohyeddin Ahrari-Roudi Oceanography Department, Marine Sciences Faculty, Chabahar Maritime University, Chabahar, Iran How to cite this paper: Ahrari-Roudi, M. Abstract (2017) A Study on Tectonic and Sedimen- tology in Order to Fault Rupture Potential Makran zone is one of the largest accretionary wedges in the world. This re- in Coasts the Makran Sea. Open Journal of search had used methods such as studies of Office and library, field observa- Geology, 7, 1269-1286. tion and surveying that several field visits, sampling, registered structural evi- https://doi.org/10.4236/ojg.2017.79084 dence, Laboratory studies, Data analysis, interpretation and conclusions. The Received: July 29, 2017 most important objective of this study is assessment of Tectonics and hazard Accepted: August 29, 2017 Potential in Coasts the Oman Sea based on tectonics and sedimentology. The Published: September 1, 2017 northward movement and subduction of Oman oceanic lithosphere beneath Iranian micro-plate at a very shallow angle and at high rate is responsible for Copyright © 2017 by author and Scientific Research Publishing Inc. active orogenesis and uplift. Detailed seismological and geological informa- This work is licensed under the Creative tion in planning is extremely essential to avoid any disaster. It is to be re- Commons Attribution International membered that seismicity does not remain fixed in an area but migrates slow- License (CC BY 4.0).
    [Show full text]
  • Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal
    HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 17 Number 2 Himalayan Research Bulletin: Article 16 Solukhumbu and the Sherpa 1997 Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal Alton C. Byers Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Byers, Alton C.. 1997. Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal. HIMALAYA 17(2). Available at: https://digitalcommons.macalester.edu/himalaya/vol17/iss2/16 This Research Article is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal Alton C. Byers The Mountain Institute This study uses repeat photography as the primary Introduction research tool to analyze processes of physical and Repeat photography, or precise replication and cultural landscape change in the Khumbu (M!. Everest) interpretation of historic landscape scenes, is an region over a 40-year period (1955-1995). The study is analytical tool capable of broadly clarifying the patterns a continuation of an on-going project begun by Byers in and possible causes of contemporary landscapellanduse 1984 that involves replication of photographs originally changes within a given region (see: Byers 1987a1996; taken between 1955-62 from the same five photo 1997). As a research tool, it has enjoyed some utility points. The 1995 investigation reported here provided in the United States during the past thirty years (see: the opportunity to expand the photographic data base Byers 1987b; Walker 1968; Heady and Zinke 1978; from five to 26 photo points between Lukla (2,743 m) Gruell 1980; Vale, 1982; Rogers et al.
    [Show full text]
  • Review of Human-Elephant FINAL Reduced 01.Cdr
    Prithiviraj Fernando, M. Ananda Kumar, A. Christy Williams, Eric Wikramanayake, Tariq Aziz, Sameer M. Singh WORLD BANK-WWF ALLIANCE FOR FOREST CONSERVATION & SUSTAINABLE USE Review of Human-Elephant Conflict Mitigation Measures Practiced in South Asia (AREAS Technical Support Document Submitted to World Bank) Prithiviraj Fernando, M. Ananda Kumar, A. Christy Williams, Eric Wikramanayake, Tariq Aziz, Sameer M. Singh Published in 2008 by WWF - World Wide Fund for Nature. Any reproduction in full or in part of this publication must mention the title and credit the above mentioned publisher as the copyright owner. © text and graphics: 2008 WWF. All rights reserved. Photographs by authors as credited. CONTENTS Preamble 1-2 LIST OF TECHNIQUES Problem Animal Removal 28-33 Traditional Crop Protection 3-7 Capture and domestication Capture and semi-wild management Crop guarding Elimination Noise and Throwing Things Fire Compensation & Insurance 34-35 Supplements to traditional crop protection Land-Use Planning 36-38 Alarms Providing benefits from conservation to Repellants Local communities Organized Crop Protection 8-11 Recommendations 39 Guard teams, 40-43 Vehicle patrols, References Cited Koonkies Literature Cited 44-45 Elephant Barriers 12-18 Physical FORMAT FOR Wire fences EACH TECHNIQUE Log and stone fences Technique Ditches Applicable scale Biological fences Objective Psychological Description of technique Electric fences Positive effects Cleared boundaries and simple demarcation of fields People Elephants Buffer Crops & Unpalatable Crops 19-20 Negative effects People Supplementary Feeding 21-22 Elephants Translocation 23-27 Future needs Chemical immobilization and transport In-country applications Elephant drives Sri Lanka PREAMBLE ew wild species evoke as much attention and varied emotions from humans as elephants.
    [Show full text]