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Impact of Climatic Change on Agro-Ecological Zones of the Suru-Zanskar Valley, Ladakh (Jammu and Kashmir), India
Journal of Ecology and the Natural Environment Vol. 3(13), pp. 424-440, 12 November, 2011 Available online at http://www.academicjournals.org/JENE ISSN 2006 - 9847©2011 Academic Journals Full Length Research Paper Impact of climatic change on agro-ecological zones of the Suru-Zanskar valley, Ladakh (Jammu and Kashmir), India R. K. Raina and M. N. Koul* Department of Geography, University of Jammu, India. Accepted 29 September, 2011 An attempt was made to divide the Suru-Zanskar Valley of Ladakh division into agro-ecological zones in order to have an understanding of the cropping system that may be suitably adopted in such a high altitude region. For delineation of the Suru-Zanskar valley into agro-ecological zones bio-physical attributes of land such as elevation, climate, moisture adequacy index, soil texture, soil temperature, soil water holding capacity, slope, vegetation and agricultural productivity have been taken into consideration. The agricultural productivity of the valley has been worked out according to Bhatia’s (1967) productivity method and moisture adequacy index has been estimated on the basis of Subrmmanyam’s (1963) model. The land use zone map has been superimposed on moisture adequacy index, soil texture and soil temperature, soil water holding capacity, slope, vegetation and agricultural productivity zones to carve out different agro-ecological boundaries. The five agro-ecological zones were obtained. Key words: Agro-ecology, Suru-Zanskar, climatic water balance, moisture index. INTRODUCTION Mountain ecosystems of the world in general and India in degree of biodiversity in the mountains. particular face a grim reality of geopolitical, biophysical Inaccessibility, fragility, diversity, niche and human and socio economic marginality. -
Figure 3. Terrace Sections
Quaternary Research (2018), 89, 281–306. Copyright © University of Washington. Published by Cambridge University Press, 2017. doi:10.1017/qua.2017.92 Quantifying episodic erosion and transient storage on the western margin of the Tibetan Plateau, upper Indus River Tara N. Jonella,b*, Lewis A. Owenc, Andrew Carterd, Jean-Luc Schwennigere, Peter D. Cliftb aSchool of Geosciences, University of Louisiana at Lafayette, Lafayette, Louisiana 70504, USA bDepartment of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA cDepartment of Geology, University of Cincinnati, Cincinnati, Ohio 45221, USA dDepartment of Earth and Planetary Sciences, Birkbeck College, London WC1E 7HX, United Kingdom eResearch Laboratory for Archaeology and the History of Art, University of Oxford, Oxford OX1 3QY, United Kingdom (RECEIVED April 13, 2017; ACCEPTED September 27, 2017) Abstract Transient storage and erosion of valley fills, or sediment buffering, is a fundamental but poorly quantified process that may significantly bias fluvial sediment budgets and marine archives used for paleoclimatic and tectonic reconstructions. Prolific sediment buffering is now recognized to occur within the mountainous upper Indus River headwaters and is quantified here for the first time using optically stimulated luminescence dating, petrography, detrital zircon U-Pb geochronology, and morphometric analysis to define the timing, provenance, and volumes of prominent valley fills. This study finds that climatically modulated sediment buffering occurs over 103–104 yr time scales and results in biases in sediment compositions and volumes. Increased sediment storage coincides with strong phases of summer monsoon and winter westerlies precipitation over the late Pleistocene (32–25 ka) and mid-Holocene (~8–6 ka), followed by incision and erosion with monsoon weakening. -
The Road to Lingshed: Manufactured Isolation and Experienced Mobility in Ladakh
HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 32 Number 1 Ladakh: Contemporary Publics and Article 14 Politics No. 1 & 2 8-2013 The Road to Lingshed: Manufactured Isolation and Experienced Mobility in Ladakh Jonathan P. Demenge Institute of Development Studies, UK, [email protected] Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Demenge, Jonathan P.. 2013. The Road to Lingshed: Manufactured Isolation and Experienced Mobility in Ladakh. HIMALAYA 32(1). Available at: https://digitalcommons.macalester.edu/himalaya/vol32/iss1/14 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]. The Road to Lingshed: Manufactured Isolation and Experienced Mobility in Ladakh Acknowledgements 1: Nyerges, Endrew (1997), The ecology of practice: studies of food crop production in Sub-Saharan West Africa (Amsterdam: Gordon and Breach). 2: Swyngedouw, Erik (2003), 'Modernity and the Production of the Spanish Waterscape, 1890-1930', in Karl S. Zimmerer and Thomas J. Bassett (eds.), Political Ecology: An Integrative Approach to Geography and Environment-Development Studies (New York: The Guilford Press). This research article is available in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies: https://digitalcommons.macalester.edu/himalaya/vol32/iss1/14 JONATHAN DEMENGE INSTITUTE OF DEVELOPMENT STUDIES, UK THE ROAD TO LINGSHED: MANUfacTURED ISOLATION AND EXPERIENCED MOBILITY IN LADAKH The article deals with the political ecology of road construction in Ladakh, North India. -
Quaternary River Erosion, Provenance, and Climate Variability
Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School 2017 Quaternary River Erosion, Provenance, and Climate Variability in the NW Himalaya and Vietnam Tara Nicole Jonell Louisiana State University and Agricultural and Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Earth Sciences Commons Recommended Citation Jonell, Tara Nicole, "Quaternary River Erosion, Provenance, and Climate Variability in the NW Himalaya and Vietnam" (2017). LSU Doctoral Dissertations. 4423. https://digitalcommons.lsu.edu/gradschool_dissertations/4423 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. QUATERNARY RIVER EROSION, PROVENANCE, AND CLIMATE VARIABILITY IN THE NW HIMALAYA AND VIETNAM A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geology and Geophysics by Tara Nicole Jonell B.S., Kent State University 2010 M.S., New Mexico State University, 2012 May 2017 ACKNOWLEDGMENTS There are so many people for which I am thankful. Words can barely express the gratitude I have for my advisor, Dr. Peter D. Clift, who has countlessly provided humor and outstanding support throughout this project. I cannot imagine completing this research without his untiring guidance both in the lab and outside in the field. I also wish to thank my advisory committee for their invaluable insight and patience: Dr. -
An Archaeological Account of the Markha Valley, Ladakh. by Quentin
An Archaeological Account of the Markha Valley, Ladakh. By Quentin Devers1 and Martin Vernier2 n this paper we intend to give a first account of the archaeological remains of Markha valley (Ladakh, state of Jammu & Kashmir, I India). In spite of its rich historical heritage, this valley has received very little to no academic attention, and, except for the temple of Skyu and the fortified village of Hankar, all the sites described here are unpublished material3. Our account will follow a geographical order, reporting the sites as one encounters them when walking the valley upstream. But, before we do so, we shall give a quick overview of the valley’s geographical setting within Ladakh. Markha valley, which is south of and parallel to the Indus [Fig. 1], has five traditional access routes [Fig. 2]. The first and easiest one is by crossing the Zanskar river near its meeting point with the Markha river. There one can cross the Zanskar by means of a rudimentary trolley (although a bridge is now under construction with the aim to link the valley to the modern road network). Until recently, the traditional spot to cross the river was further downstream, nearby the hamlet of Chilling. Once on the other bank one had to follow a path over the low Kuki pass (3420 m) before reaching the Markha valley itself. A second route leads directly from central Ladakh. It starts from the village of Spituk in the Indus valley, on the right bank of the river 7 km south of Leh town, and crosses the mountains via the Ganda pass before it reaches Skyu, the second village of the valley. -
Leh(Ladakh) District Primary
Census of India 2011 JAMMU & KASHMIR PART XII-B SERIES-02 DISTRICT CENSUS HANDBOOK LEH (LADAKH) VILLAGE AND TOWN WISE PRIMARY CENSUS ABSTRACT (PCA) DIRECTORATE OF CENSUS OPERATIONS JAMMU & KASHMIR CENSUS OF INDIA 2011 JAMMU & KASHMIR SERIES-02 PART XII - B DISTRICT CENSUS HANDBOOK LEH (LADAKH) VILLAGE AND TOWN WISE PRIMARY CENSUS ABSTRACT (PCA) Directorate of Census Operations JAMMU & KASHMIR MOTIF Pangong Lake Situated at a height of about 13,900 ft, the name Pangong is a derivative of the Tibetan word Banggong Co meaning "long, narrow, enchanted lake". One third of the lake is in India while the remaining two thirds lies in Tibet, which is controlled by China. Majority of the streams which fill the lake are located on the Tibetan side. Pangong Tso is about five hours drive from Leh in Ladakh region of Jammu & Kashmir. The route passes through beautiful Ladakh countryside, over Chang La, the third highest motorable mountain pass (5289 m) in the world. The first glimpse of the serene, bright blue waters and rocky lakeshore remains etched in the memory of tourists. There is a narrow ramp- like formation of land running into the lake which is also a favorite with tourists. During winter the lake freezes completely, despite being saline water. The salt water lake does not support vegetation or aquatic life except for some small crustaceans. However, there are lots of water birds. The lake acts as an important breeding ground for a large variety of migratory birds like Brahmani Ducks, are black necked cranes and Seagulls. One can also spot Ladakhi Marmots, the rodent-like creatures which can grow up to the size of a small dog. -
Lutra Lutra) in LADAKH, INDIAN TRANS HIMALAYAS
IUCN Otter Spec. Group Bull. 33(2) 2016 R E P O R T FIRST SYSTEMATIC SURVEY FOR OTTER (Lutra lutra) IN LADAKH, INDIAN TRANS HIMALAYAS Pushpinder Singh JAMWAL1*, Jigmit TAKPA2, Pankaj CHANDAN1, Melissa SAVAGE3 1Western Himalayas Landscape, WWF-India 2Department of Wildlife Protection, Jammu and Kashmir, India 3University of California, Los Angeles, USA * e-mail [email protected] (*corresponding author) (Received 3rd September 2016, accepted 24th October 2016) ABSTRACT: We report the findings of the first survey for Eurasian otter (Lutra lutra) from the Upper Indus River and several of its tributaries in Leh and Kargil Districts, India. The survey was conducted between 25th August to 30th October, 2015. We report the distribution of otter sign, including camera trap images, scats, tracks, and latrines, and the habitat characteristics along 50 km of riverbank. We observed indirect sign of otter presence on two of the four rivers surveyed, but otter abundance appears to be low in the area. Human disturbance, including proximity to settlements, grazing livestock, and particularly feral dogs, appears to deter otter presence. Key words: Eurasian otter, Lutra lutra, Western Himalaya landscape, Indus River, Dras River INTRODUCTION The presence of otters in the Upper Indus River Valley of Ladakh, India, has only been reported anecdotally to date. Ladakh is a region in the northernmost Indian State of Jammu and Kashmir, on the western edge of the Tibetan Plateau. The great trough of the Upper Indus River Valley runs between the Zanskar Mountains, north of the Great Himalaya Range, and south of the Ladakh Mountains, a part of the Karakoram Range. -
Ladakh, Threatened Stronghold of Rare Himalayan Mammals
Ladakh, threatened Himalayan mamma Ladakh, a remote region of India lying Ladakh covers some 100,000 sq km of the Indian between the Himalayas and Tibet, is state of Jammu and Kashmir. The region ethnically and geographically distinct stretches into the north-eastern extremity of the Karakoram and includes the western limits of the from the rest of the country. Because of Tibetan plateau. Access is forbidden beyond the its isolation, change came later to Ladakh 'Inner Line' which delineates sensitive zones near than to other parts of the Himalayas, but India's borders with Pakistan and China but most recent years have seen the familiar of Central Ladakh and Zanskar is freely acces- pattern of social change, human popu- sible. The climate is one of extremes, with con- siderable daily and seasonal variations in tem- lation increase, tourism and rural perature. Rainfall is scanty and the landscape arid development beginning to affect the and inhospitable. Winter temperatures fall to environment. The authors, jointly and —30°C and below and although heavy snowfalls individually, made a series of visits to the occur on the main Himalayan ranges, far less falls area to investigate the status of the in Ladakh. The country is extremely rugged and mountainous with peaks over 6200 m and passes wildlife and to look at conservation up to 5500 m. The vegetation is characteristic of a measures. high-altitude desert. Trees are few: Juniperus spp. grow mainly on high, inaccessible slopes or The opening of Ladakh in 1974, and popular- in remote valleys; they have been gradually isation of the area by the media, has focused reduced over the years by felling for timber and considerable attention on this remote, trans- for fuel and by the cutting of foliage for incense. -
The Geology of Western Zanskar 1-50 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1982 Band/Volume: 125 Autor(en)/Author(s): Fuchs Gerhard Artikel/Article: The geology of Western Zanskar 1-50 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jahrb. Geol. B.-A. ISSN 0016-7800 Band 125, Heft 1-2 S. 1-50 Wien, Dezember 1982 The geology of Western Zanskar By GERHARD FUCHS*) With 18 Figures and 6 Tables (= Beilagen 1-6) (Fig. 2, 4-10, 13-18 on Tables 3-5) v NW-Himalaya X Ladakh -I W-Zanskar 3 Stratigraphy 3 Tectonics 03 Evolution CONTENTS Abstract 2 Zusammenfassung 2 1. Introduction 3 2. Stratigraphy 5 2.1. Stratigraphy of the Tibetan Zone 5 2.1.1. Crystalline 5 2.1.2. Panjal Trap 6 2.1.3. Permo-Triassic 6 2.1.4. Triassic 7 2.1.5. Quartzite Series and Kioto Limestone 7 2.1.6. Upper Dogger 7 2.1.7. Spiti Shales 8 2.1.8. Giumal Sandstone 8 2.1.9. Chikkim Limestone 8 2.1.10. Kangi La Flysch 9 2.1.11. Spanboth Limestone 10 2.1.12. Chulung La Slates 12 2.2. Stratigraphy of the Northern Zanskar Unit (N.Z.U.) 13 2.2.1. Triassic-Jurassic Carbonates 13 2.2.2. Jurassic-lower Upper Cretaceous 14 2.2.3. Shillakong Formation 15 2.2.4. Lamayuru Formation (Maestrichtian portion) 16 2.2.5. Lingshet Limestone 17 2.2.6. Kong Slates 19 *) Address of the author: Dr. -
India – the Himalayas
http://juriwaro.com 1 India – The Himalayas August – September, 2005 Finally, I have reached the endless ocean, called India. But first, as an introduction to India, I am going to share my impression from the Himalayas. Here, you are not going to find anything about Hinduism, magicians, saris, elephants, the Gang River, or anything else, that is typical for the plains. That is because the mountain peoples around the Globe are rather a common group of people, than a part of any other. When I have the chance, I only pass through big cities. So, at noon, I spent only an hour at Shiliguri. It was at the end of the rainy season. Due to my laziness I did not take out my raincoat and I was drenched to the bone. Nevertheless, I managed to exchange some rupees and to buy a detailed atlas of India and the timetable of the Indian train system. I was always keeping these two books while being in India. They helped me much better than any travel guide. Travel guides inevitably put every tourist on the beaten tracks of this huge and boring industry. Several times I have overheard the almost forgotten Tibetan greeting „tashi delek“. Other mountain peoples, common for the region, started to be seen along with Indians and Tibetans: Nepali, Bhutanese, Sikkimese, and many more, all they dressed in their colourful, worn-out, and filthy costumes. I caught a bus to Darjeeling. The narrow-gage covers the same distance of 90 km for 6 hours. On top of that it is more expensive and operates once a day. -
Glacier Monitoring in Ladakh and Zanskar, Northwestern India
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2009 Glacier Monitoring in Ladakh and Zanskar, northwestern India Martin Edward Byrne The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Byrne, Martin Edward, "Glacier Monitoring in Ladakh and Zanskar, northwestern India" (2009). Graduate Student Theses, Dissertations, & Professional Papers. 493. https://scholarworks.umt.edu/etd/493 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. GLACIER MONITORING IN LADAKH AND ZANSKAR, NORTHWESTERN INDIA By MARTIN EDWARD BYRNE Bachelor of Arts, Eastern Washington University, Cheney, Washington, 2006 Thesis presented in partial fulfillment of the requirements for the degree of Master of Science in Geography, GIS and Cartography The University of Montana Missoula, MT June 2009 Approved by: Perry Brown, Associate Provost for Graduate Education Graduate School Ulrich Kamp, Chair Department of Geography Anna Klene Department of Geography Joel Harper Department of Geosciences Tobias Bolch Institute of Cartography, Dresden University of Technology, Germany Byrne, Martin, M.A, May 2009 Geography GLACIER MONITORING IN LADAKH AND ZANSKAR, NORTHWESTERN INDIA Chairman: Ulrich Kamp Abstract Glaciers in the Himalaya are often heavily covered with supraglacial debris, making them difficult to study with remotely-sensed imagery alone. -
The Geology of the Markha-Khurnak Region in Ladakh (India) 403 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1985 Band/Volume: 128 Autor(en)/Author(s): Fuchs Gerhard Artikel/Article: The Geology of the Markha-Khurnak Region in Ladakh (India) 403 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jb. Geol. B.-A. ISSN 0016-7800 Band 128 I Heft 3 + 4 1__ S_._4_0_3_-_4_3_7 W_i_e_n_,J_s_'n_n_e_r_1_9_8_6__ The Geology of the Markha-Khurnak Region in Ladakh (India) By GERHARD FUCHS') With 28 figures and 5 plates Himalaya India Ladakh Indus Suture Zone Tibetan Zone Tectonics Palaeogeography Content Zusammenfassung, Summary 403 1. Introduction 404 2. The Indus Molasse observations along the Leh - Ganda La route 404 3. The Dras Unit and overlying Ultrabasic Klippes 406 4. The Ophiolitic Melange Zones 410 5. The Lamayuru Unit ~ 416 6. The Metasedimentary Sequence of the Nimaling (Tso Morari) Dome 419 6.1. The Basal Flysch 419 6.2. The Micaschist-Dolomite Series 420 6.3. The Carbonate Series 420 6.4. The Siltite-Quartzite-Limestone Series 421 6.5. The Lamayuru Formation 421 6.6. The Age of the Metasedimentary Succession of the Nimaling Dome : 422 7. The Tibetan (Tethys) Zone of Zanskar 422 7.1. The Zanskar Carbonates 422 7.2. The Upper Dogger 423 7.3. The Giumal Sandstone and Khurnak Formation 423 7.4. The Upper Cretaceous 424 7.5. The Upper Paleocene Limestones 424 8. The Markha-Nimaling Area and the Geology of Ladakh 425 8.1. Stratigraphy and Palaeogeography 425 8.2.