The German Garhwal-Himalaya Expedition, 1938
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Table of Contents
Table of Contents Acknowledgements xi Foreword xii I. EXECUTIVE SUMMARY XIV II. INTRODUCTION 20 A. The Context of the SoE Process 20 B. Objectives of an SoE 21 C. The SoE for Uttaranchal 22 D. Developing the framework for the SoE reporting 22 Identification of priorities 24 Data collection Process 24 Organization of themes 25 III. FROM ENVIRONMENTAL ASSESSMENT TO SUSTAINABLE DEVELOPMENT 34 A. Introduction 34 B. Driving forces and pressures 35 Liberalization 35 The 1962 War with China 39 Political and administrative convenience 40 C. Millennium Eco System Assessment 42 D. Overall Status 44 E. State 44 F. Environments of Concern 45 Land and the People 45 Forests and biodiversity 45 Agriculture 46 Water 46 Energy 46 Urbanization 46 Disasters 47 Industry 47 Transport 47 Tourism 47 G. Significant Environmental Issues 47 Nature Determined Environmental Fragility 48 Inappropriate Development Regimes 49 Lack of Mainstream Concern as Perceived by Communities 49 Uttaranchal SoE November 2004 Responses: Which Way Ahead? 50 H. State Environment Policy 51 Institutional arrangements 51 Issues in present arrangements 53 Clean Production & development 54 Decentralization 63 IV. LAND AND PEOPLE 65 A. Introduction 65 B. Geological Setting and Physiography 65 C. Drainage 69 D. Land Resources 72 E. Soils 73 F. Demographical details 74 Decadal Population growth 75 Sex Ratio 75 Population Density 76 Literacy 77 Remoteness and Isolation 77 G. Rural & Urban Population 77 H. Caste Stratification of Garhwalis and Kumaonis 78 Tribal communities 79 I. Localities in Uttaranchal 79 J. Livelihoods 82 K. Women of Uttaranchal 84 Increased workload on women – Case Study from Pindar Valley 84 L. -
Shivling Trek in Garhwal Himalaya 2013
Shivling Trek in Garhwal Himalaya 2013 Area: Garhwal Himalayas Duration: 13 Days Altitude: 5263 mts/17263 ft Grade: Moderate – Challenging Season: May - June & Aug end – early Oct Day 01: Delhi – Haridwar (By AC Train) - Rishikesh (25 kms/45 mins approx) In the morning take AC Train from Delhi to Haridwar at 06:50 hrs. Arrival at Haridwar by 11:25 hrs, meet our guide and transfer to Rishikesh by road. On arrival check in to hotel. Evening free to explore the area. Dinner and overnight stay at the hotel. Day 02: Rishikesh - Uttarkashi (1150 mts/3772 ft) In the morning after breakfast drive to Uttarkashi via Chamba. One can see a panoramic view of the high mountain peaks of Garhwal. Upon arrival at Uttarkashi check in to hotel. Evening free to explore the surroundings. Dinner and overnight stay at the hotel. Day 03: Uttarkashi - Gangotri (3048 mts/9998 ft) In the morning drive to Gangotri via a beautiful Harsil valley. Enroute take a holy dip in hot sulphur springs at Gangnani. Upon arrival at Gangotri check in to hotel. Evening free to explore the beautiful surroundings. Dinner and overnight stay in hotel/TRH. Harsil: Harsil is a beautiful spot to see the colors of the nature. The walks, picnics and trek lead one to undiscovered stretches of green, grassy land. Harsil is a perfect place to relax and enjoy the surroundings. Sighting here includes the Wilson Cottage, built in 1864 and Sat Tal (seven Lakes). The adventurous tourists have the choice to set off on various treks that introduces them to beautiful meadows, waterfalls and valleys. -
Ten Days on Vasuki Parbat
MALCOLM BASS Ten Days on Vasuki Parbat s the rock flew past me I knew it was going to hit Paul. I’d heard it Acome banging and whirring down the gully, bigger and noisier than the others. I’d screamed ‘rock!’ but Paul, tethered on the open icefield below, had nowhere to hide. It smashed into the ice a metre out from my stance beneath a roof, and then spun out, arcing towards its target. The impact was a muffled thud. Paul crumpled onto the anchors. It was 3pm on day 3 and the sun was beating full onto Vasuki Parbat’s west face. Suddenly it was very quiet and I felt acutely alone. But then Paul began to move. Moans drifted up as he righted himself, then stood back up to the stance. ‘Paul, Paul … are you OK?’ ‘I think so.’ ‘Can you climb?’ ‘Give me a minute.’ I was desperate for Paul to start moving. I wanted to shout at him to get a move on (or words to that effect). We were at the bottom of a gully overhung by a 700m leaning wall of variable quality rock. For the last hour rockfall had been steadily increasing. The objective danger meter was swinging between ‘Unjustifiable’ and ‘Suicidal’. But Paul knew all that: any delay on his part could more reasonably be ascribed to having just been hit by a 3kg boulder that had fallen several hundred metres than to a lack of appreciation of the urgency of the situation. So I shut up. Paul collected himself, took out the ice screws, and began to climb towards me, slowly and stiffly at first. -
Annex A: Study Summary Details
Annex A: Study summary details Reference Location & Period Project details Methodology Summary of findings Ageta, Y., Naito, N., Nakawo, M., Fujita, K., Shankar, K., Glaciological method Pokhrel, A.P. and employed for MB measures Wangda, D., (2001). in Nepal, area and terminus Study project on the Mass balance, terminus and area measure less clear on recent rapid retreat compared across method, but consistent team shrinkage of regions/countries. Nepal data approach. Bhutan data summer- Nepal - (Hidden valley, collected during 1997-99, collected same season two Nepal - mass accumulation type Langtang, Shorong, Khumbu following on from Nakawo consecutive years - method balances negative, glaciers in the Himal),- AX010 (1997) studies 1994 + 1996. Ice only notes’ field terminus retreating - Himalayas, 1997- (Shorong)(1997,98,99), thickness data was collected but observations’ and baselines both AX010 and 1999. Bulletin of Rikha Samba (Hidden not detailed in results for use in from photo, maps and Rikha samba Glaciological Valley), , Khumbu (Khumbu this review. Bhutan data 98-99. satellite images. No error or accelerating retreat. Research 18: pp 45- Himal); Bhutan - (many, No retreat data available in accuracy noted. Medium Bhutan - no data on 49. with ref to Jichu Dramo) report however for this region. confidence in data. shrinkage. India data inconclusive as Compiling available mapping, unable to confirm Study collating as much mapping aerial photo and inventory baseline period. data as possible from all regions data to develop a picture of Narrative of findings plus more modern data analysed glacier distribution and that is set out by by team. India mapping of derive some idea of region the overall glaciers from inventory GSI 1999 retreat/change from trend is retreat of Ageta, K.Y. -
To Download Document
Apex Indian Mountaineering Foundation Newsletter * Volume 11 * October 2020 Climb of Chau Chau Kang Nilda (6,303m), Spiti, Himachal Himalaya. Image Courtesy: Naoko Ootake. Early morning view of a nomadic settlement of Changpas in Changthang - Ladakh Himalaya. Image Courtesy: Manish Lakhani Inside Apex Volume 11 Expedition Reports Shivling - Alpine ascent, Uttarakhand Himalaya : Nihar Soley President Chau Chau Kang Nilda, Ladakh Himalaya : Naoko Ootake Brig. Ashok Abbey Bhagirathi II, Uttarakhand Himalaya : Subodh Chandola Vice Presidents Rita Gombu Marwah Treks and Explorations Prof. Harshwanti Bisht Charang La - Kinner Kailash, Himachal Himalaya : Anshul Soni Honorary Secretary Col. S. P. Malik Mountain Life The Pashmina People of Changthang : Manish Lakhani Honorary Treasurer S. Bhattacharjee Chi Lupo - The Shertukpen Honey Hunters of Arunachal : Kezong D. Thongdok Governing Council Members Planning an Expedition in the Indian Himalaya Reena Kaushal Dharamshaktu Col. Vijay Singh Why Climb in the Indian Himalaya? M R Vijayaraghavan Here’s Five Reasons : Mayank Vyas Singh Dhruv Joshi Wallambok Lyngdoh Prem Singh At the IMF Wg. Cdr. T Sridharan Deepu Sharma Mountain Film Festival 2020 Col. J S Dhillon Risk Management Meet 2020 Debraj Dutta Online Initiatives : Webinar Series & Workshops Lt. Col. M S Chauhan Sport Climbing Championships Ex-Officio Members Joint Secretary, In the Indian Himalaya Ministry of Youth Affairs & Sports, Govt. of India News and events in the Indian Himalaya Joint Secretary, Book Releases Ministry of Finance, Govt. of India Recent books released on the Indian Himalaya IMF in te Times of COVID Dear Reader, As the Corona Virus pandemic continues, I take this opportunity to wish all our readers good health and well being ! These are unprecedented times for the human race world over, and India is no exception as we fight this deadly onslaught on humanity, For us to reach the new normal, we have to remain steadfast in our resolve to follow the laid down protocols scrupulously. -
Witnessing Change
WWF-India WWF-India is one of India’s largest conservation organization. Its mission is to stop the degradation of the planet’s natural environment, which it addresses through its work in biodiversity conservation and reduction of humanity’s ecological footprint. WWF-India engages multiple stakeholders in an inter-disciplinary approach to address the issues pertaining to mitigation of, and adaptation to, climate change. The focus of the Climate Change and Energy programme is to contextualize climate change in the framework of inclusive development, incorporating the climate resilience built within it. WITNESSING CHANGE: Birla Institute of Technology (BIT), Mesra, Ranchi BIT, Mesra, Ranchi is a "Deemed University" offering programmes and undertaking GLACIERS IN THE INDIAN HIMALAYAS research in diverse fields including Engineering & Technology, Applied Sciences (Environmental Sciences and Glaciology etc.), Remote Sensing, Computer Applications, and Biotechnology. The Jaipur Extension Centre of BIT, Mesra has Remote Sensing Division which has been involved since 2006, in studying and monitoring few Himalayan glaciers to understand the climate change impact on the glacier fluctuations as well on the fresh water reserve in the Himalayas. The contents of this report may be used by any one providing proper acknowledgement to WWF and BIT. The information contained herein has been obtained from sources and from analysis, which the authors believe to be reliable. All opinions expressed herein are those of the authors and are based on the author’s judgment at the time of publishing this report. The authors and any one associated with the report are not liable for any unintended errors or omissions, opinions expressed herein. -
Shivling Trek in Garhwal Himalaya 2015
Shivling Trek in Garhwal Himalaya 2015 Area: Garhwal Himalayas Duration: 13 Days Altitude: 5263 mts/17263 ft Grade: Moderate – Challenging Season: May - June & Aug end – early Oct Day 01: Delhi – Haridwar (By AC Train) - Rishikesh (25 kms/45 mins approx) In the morning take AC Train/Volvo Coach from Delhi to Haridwar at 06:50 hrs. Arrival at Haridwar by 11:25 hrs, meet our guide and transfer to Rishikesh by road. On arrival check in to hotel. Evening free to explore the area. Dinner and overnight stay at the hotel. Day 02: Rishikesh - Uttarkashi (1150 mts/3772 ft) In the morning after breakfast drive to Uttarkashi via Chamba. One can see a panoramic view of the high mountain peaks of Garhwal. Upon arrival at Uttarkashi check in to hotel. Evening free to explore the surroundings. Dinner and overnight stay at the hotel. Day 03: Uttarkashi - Gangotri (3048 mts/9998 ft) In the morning drive to Gangotri via a beautiful Harsil valley. Enroute take a holy dip in hot sulphur springs at Gangnani. Upon arrival at Gangotri check in to hotel. Evening free to explore the beautiful surroundings. Dinner and overnight stay in hotel/TRH. Harsil: Harsil is a beautiful spot to see the colors of the nature. The walks, picnics and trek lead one to undiscovered stretches of green, grassy land. Harsil is a perfect place to relax and enjoy the surroundings. Sighting here includes the Wilson Cottage, built in 1864 and Sat Tal (seven Lakes). The adventurous tourists have the choice to set off on various treks that introduces them to beautiful meadows, waterfalls and valleys. -
Glacier Changes in the Garhwal Himalaya, India, from 1968 to 2006 Based on Remote Sensing
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2011 Glacier changes in the Garhwal Himalaya, India, from 1968 to 2006 based on remote sensing Bhambri, R ; Bolch, T ; Chaujar, R K ; Kulshreshtha, S C Abstract: Glacier outlines are mapped for the upper Bhagirathi and Saraswati/Alaknanda basins of the Garhwal Himalaya using Corona and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) satellite images acquired in 1968 and 2006, respectively. A subset of glaciers was also mapped using Landsat TM images acquired in 1990. Glacier area decreased from 599.9 ± 15.6 km2 (1968) to 572.5 ± 18.0 km2 (2006), a loss of 4.6 ± 2.8%. Glaciers in the Saraswati/Alaknanda basin and upper Bhagirathi basin lost 18.4 ± 9.0km2 (5.7±2.7%) and 9.0 ± 7.7km2 (3.3±2.8%), respectively, from 1968 to 2006. Garhwal Himalayan glacier retreat rates are lower than previously reported. More recently (1990–2006), recession rates have increased. The number of glaciers in the study region increased from 82 in 1968 to 88 in 2006 due to fragmentation of glaciers. Smaller glaciers (<1 km2) lost 19.4 ± 2.5% (0.51 ± 0.07% a–1) of their ice, significantly more than for larger glaciers (>50 km2) which lost2.8± 2.7% (0.074 ± 0.071% a–1). From 1968 to 2006, the debris-covered glacier area increased by 17.8 ± 3.1% (0.46 ± 0.08% a–1) in the Saraswati/Alaknanda basin and 11.8 ± 3.0% (0.31 ± 0.08% a–1) in the upper Bhagirathi basin. -
A71prelims 1..6
Annals of Glaciology 57(71) 2016 doi: 10.3189/2016AoG71A015 131 © The Author(s) 2016. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Shrinkage of Satopanth and Bhagirath Kharak Glaciers, India, from 1936 to 2013 H.C. NAINWAL,1 Argha BANERJEE,2� R. SHANKAR,3 Prabhat SEMWAL,1 Tushar SHARMA1 1HNB Garhwal Central University, Srinagar (Garhwal), Uttarakhand, India 2Indian Institute of Science Education and Research Kolkata, Mohanpur, India 3The Institute of Mathematical Sciences, Chennai, India Correspondence: H.C. Nainwal <[email protected]> ABSTRACT. We have compiled and analysed available records and data on the shrinkage of Satopanth (SPG) and Bhagirath Kharak (BKG) Glaciers, Uttarakhand, India, during the period 1936–2013. We estimate the mean retreat rates of the snouts of SPG and BKG for this period at 9.7 � 0.8 m a–1 and 7.0 � 0.6 m a–1 respectively. We have also revised the estimates of the area vacated during the period 1956–2013 to be 0.27 � 0.05 km2 and 0.17 � 0.04 km2 for SPG and BKG respectively, corresponding to front-averaged retreat rates of 5.7 � 0.6 m a–1 and 6.0 � 0.9 m a–1. The study revealed an average thinning of glacial ice in the lower ablation zone of SPG of 9 � 11 m in the past 51 years. We observed that while the fronts of SPG and BKG depicted in the Survey of India topographic map published in 1962 are inconsistent with other available records, the elevation contours are consistent with them. -
''Deciphering Tectonic and Climatic Controls on Erosion and Sediment
Deciphering tectonic and climatic controls on erosion and sediment transfer in the NW Himalaya A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in the Department of Geology of the McMicken College of Arts and Sciences by Elizabeth N. Orr MSc., Royal Holloway, University of London BSc., University of Glasgow 19th of April 2019 Dissertation Committee Dr. Lewis A. Owen Dr. Dylan Ward Dr. Craig Dietsch Dr. Richard Beck Abstract Central to examining orogenic belt formation and evolution are efforts to define the relative roles of tectonics and climate in landscape denudation, and the complex feedbacks that exist between them. Studies in high altitude, high relief mountain settings such as the Himalayan-Tibetan orogen show that these relationships are not completely straightforward and that denudation can scale with tectonics, precipitation and/or topography. Steep north-south trending gradients in elevation, relief, rock uplift and precipitation make the NW Himalaya an excellent location to examine these controls of landscape denudation. As a first step to help elucidate the erosional processes involved in sediment mobilization from primary sources at catchment headwaters, rates of lateral rockwall slope erosion are defined for a suite of 12 catchments between the Baltistan region of Pakistan and Garhwal, northern India. These rates are derived from 10Be cosmogenic nuclide concentrations in medial moraine sediment, and affirm that between ~0.02 and 7 m of lateral slope erosion through periglacial processes can be achieved across a single millennium in this setting, and >2 km when extrapolated for the whole Quaternary. -
Classification of the Himalaya
Classification of the Himalaya COMPILED BY H. ADAMS CARTER This study aims to classify the different groups of the Himalaya from its eastern end westward through the peaks of Garhwal (Uttar Pradesh) in India. Wherever data have been available, it gives a listing of all peaks above 6500 meters (21,326 feet) and all officially named peaks between 6000 meters (19,685 feet) and 6500 meters with altitudes and coordinates. In some ranges, where peaks are lower, some unnamed peaks in the second category have been included. The Nepalese section depends almost entirely on the outstanding work done by Dr. Harka Gurung and Dr. Ram Krishna Shrestha. These two Nepalese scholars put together an inventory of all Nepalese peaks above 6000 meters with the latest altitudes, corrected names and coordinates. They used primarily the Survey of India topographic sheets at a scale of an inch to a mile (1:63,360). They also used maps ar 1:50,000 prepared for the Sino-Nepalese Boundary Agreement of 1979. For the Indian regions, extensive use was made of three maps published by the Schweizerische Stiftung fur Alpine Forschungen (Swiss Foundation for Al- pine Research) of Sikkim, Garhwal East and Garhwal West. Harish Kapadia and Dhiran Toolsides in particular gave great assistance by checking Indian data against further information available to them. Colonel Lakshmi Pati Shanna made valuable suggestions. Dr. Shi Yafeng also helped by providing an excel- lent Chinese map of the Everest region. In all sections, the Japanese Mountain- eering Maps of the World proved indispensable. Dr. Zbigniew Kowalewski had made fine studies, which are reflected here. -
Mountaineering Tourism Prospects and Trends: a Case of Uttarakhand Himalaya
International Journal of Information Movement Vol.2 Issue VII (November 2017) Website: www.ijim.in ISSN: 2456-0553 (online) Pages 226-238 MOUNTAINEERING TOURISM PROSPECTS AND TRENDS: A CASE OF UTTARAKHAND HIMALAYA Vikram Vir Bharti Assistant Professor, Research Scholar & Adventure Outdoor Professional, Department of Tourism, Kumaun University, Nainital, UTTARAKHAND. Email:[email protected] Abstract: Uttarakhand Himalayas cradles some of the richest assets of nature in terms of its vivid geodiversity and biodiversity. Uttarakhand abounds, some of the best and the richest Himalayan resources in it, as snow bound peaks, glaciers, rivers, valleys, alpine pasture, high mountain passes etc. which serves as a playground for the game called mountaineering. Mountaineering tourism among the varied types of tourism offerings in the state of Uttarakhand, in class of adventure tourism is key driver, which magnetizes adventure enthusiasts to visit Uttarakhand Himalayas. The very paper focuses on mountaineering tourism trends in Uttarakhand and further prospects and potential areas in Uttarakhand for mountaineering tourism operation and development. Keywords: Uttarakhand Himalayas, Mountaineering Tourism, Trends, Prospects. “Why do people climb mountains? Because they are there” Answered G.L Mallory 226 | P a g e Vikram Vir Bharti: Mountaineering Tourism Prospects and Trends:A case of Uttarakhand Himalaya International Journal of Information Movement Vol.2 Issue VII (November 2017) Website: www.ijim.in ISSN: 2456-0553 (online) Pages 226-238 1.0 Uttarakhand: An Introduction (Background And Physical Setup) The Central Himalaya, popularly known as Uttarakhand (Khanduri & Saklani, 2003), carved off from Uttar Pradesh. Uttarakhand as a state, came into existence on 9 Nov, 2000 as the 27th state of India.