SURVEY in the NANDA DEVI DISTRICT. E. E. Shipton
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Design & Development Of
Design & Development Of Involving Local Communities Bilal Habib Wildlife Institute of India, Dehradun, India It’s always further than it looks. It’s always taller than it looks. And it’s always harder than it looks.” Nanda Devi Peak CONTENTS 01 Nanda Devi Biosphere Reserve 01 02 Biodiversity Features 03 03 Origin of Biosphere Reserves 05 04 UNESCO MAB Programme 06 05 Development of Monitoring Programme 07 06 Literature Review and Baseline Maps 07 07 Field Protocol (Sampling Design) 07 08 Field Protocol (Sampling Strategy) 12 09 Field Protocol (Data Collection Formats) 12 10 Data Format for Carnivore Species 13 11 Instructions for Carnivore Data Format 14 12 Data Format for Ungulate Species 18 13 Instructions for Prey Point Data Sheet 19 14 Statistical Analysis 20 15 Expected Outcomes 20 16 Recommendations and Learnings 20 17 Success of the Exercise 21 18 Key Reference 22 Design and Development of Ecological Monitoring Programme in Nanda Devi Biosphere Reserve, Uttarakhand India, Involving Local Communities Nanda Devi Biosphere Reserve: Nanda Devi Biosphere Reserve (NBR) (30°05' - 31°02' N Latitude, 79012' - 80019' E Longitude) is located in the northern part of west Himalaya in the biogeographical classification zone 2B. The Biosphere Reserve spreads over three districts of Uttarakhand - Chamoli in Garhwal and Bageshwar and Pithoragarh in Kumaun. The Nanda Devi Biosphere Reserve falls under Himalayan Highlands (2a) zone of the biogeographic zonation of India. It has wide altitudinal range (1,500 - 7,817 m). It covers 6407.03 km2 area with core zone (712.12 km2), buffer zone (5,148.57 km2) and transition zone (546.34 km2). -
National Ganga River Basin Authority (Ngrba)
NATIONAL GANGA RIVER BASIN AUTHORITY (NGRBA) Public Disclosure Authorized (Ministry of Environment and Forests, Government of India) Public Disclosure Authorized Environmental and Social Management Framework (ESMF) Public Disclosure Authorized Volume I - Environmental and Social Analysis March 2011 Prepared by Public Disclosure Authorized The Energy and Resources Institute New Delhi i Table of Contents Executive Summary List of Tables ............................................................................................................... iv Chapter 1 National Ganga River Basin Project ....................................................... 6 1.1 Introduction .................................................................................................. 6 1.2 Ganga Clean up Initiatives ........................................................................... 6 1.3 The Ganga River Basin Project.................................................................... 7 1.4 Project Components ..................................................................................... 8 1.4.1.1 Objective ...................................................................................................... 8 1.4.1.2 Sub Component A: NGRBA Operationalization & Program Management 9 1.4.1.3 Sub component B: Technical Assistance for ULB Service Provider .......... 9 1.4.1.4 Sub-component C: Technical Assistance for Environmental Regulator ... 10 1.4.2.1 Objective ................................................................................................... -
Ecosystem Function of Buffer Zone Villages of Nanda Devi Biosphere Reserve
ECOSYSTEM FUNCTION OF BUFFER ZONE VILLAGES OF NANDA DEVI BIOSPHERE RESERVE Sunil Nautiyal, PhD (1999) PhD in Botany (Specialization: Ecology) from HNB Garhwal University, Srinagar, Garhwal, Uttarakhand PhD work was carried out at GB Pant Institute of Himalayan Environment and Development (an Autonomous Institute of the Ministry of Environment, Forest & Climate Change, Govt. of India) Supervisor: Dr. R. K. Maikhuri, Scientist In-charge, Garhwal Unit, GB Pant Institute of Himalayan Environment and Development, Garhwal Unit, Srinagar, Garhwal, Uttarakhand Summary: The Nanda Devi Biosphere Reserve is situated in Himalayan highlands biogeographic province of India was established in 1988 under the UNESCO’s Man and Biosphere Programme (MAB) for the conservation of biological and cultural diversity. It consists of a central core zone (624.62 km2) surrounded by a buffer zone (1612.12 km2). In1992 it was declared as one of the world heritage site by World Heritage Committee. Legally the reserve includes the areas of reserve forests, civil forests and panchayat forests and individual farmlands. From the geomorphological point of view, the buffer zone occupies the entire Rishi Ganga catchment. A total of 17 villages are situated in the buffer zone of NDBR, of which 10 villages fall in the Garhwal (district Chamoli) and 7 villages in Kumaon (districts Pithoragarh and Almora). The present study was carried out in the 10 buffer zone villages belonging to Chamoli district of Garhwal Himalaya with a total population of 2253. The Nanda Devi Biosphere Reserve is one such protected area where local people inhabited in the buffer zone areas have been deprived of the traditional uses of the natural resources from the reserve. -
Melt Water Characteristics of Gangotri Glacier, Headwater of Ganga River Manohar Arora* & Jatin Malhotra National Institute of Hydrology, Roorkee, Uttarakhand, India
Roorkee Water Conclave 2020 Melt Water Characteristics of Gangotri Glacier, Headwater of Ganga River Manohar Arora* & Jatin Malhotra National Institute of Hydrology, Roorkee, Uttarakhand, India Abstract: Behavior of glacier plays an important role in runoff delaying characteristics of the glacier. Changes in delaying characteristics of the runoff over the melt season can be understood by studying the variation in time to peak (tp) and time-lag (t1) between melt generation and its emergence as runoff. In this study, the runoff delaying characteristics of the Gangotri Glacier in the Garhwal Himalayas (glacierized area 286 km2; drainage area 556 km2) have been studied. For this purpose, hourly discharge and temperature data were monitored near the snout of the glacier for the entire ablation period (May-October, 2010). In the early stages of the ablation period, poor drainage network and stronger storage characteristics of the glaciers due to the presence of seasonal snow cover resulted in a much delayed response of melt water, providing a higher tl and tp. In the beginning of melt season, the night time flow is almost equal to day time flow, but in the later part of the melt season, night time flow is slightly lower than the day time flow. This analysis suggests that storage characteristics are much stronger in the early part of melt season and reduce as the melt season progresses. Keywords: Gangotri Glacier, Himalayas, Melt Season, Runoff Delay Characteristics, Storage Characteristics 1. Introduction Glaciers fed rivers provide much of the water supply in some parts of the world. All the major south Asian rivers originate in the Himalayan and their upper catchments are covered with snow and glaciers. -
Volume 30 # October 2014
Summit ridge of Rassa Kangri (6250m) THE HIMALAYAN CLUB l E-LETTER l Volume 30 October 2014 CONTENTS Climbs and Explorations Climbs and Exploration in Rassa Glacier ................................................. 2 Nanda Devi East (7434m) Expedition 204 .............................................. 7 First Ascent of P6070 (L5) ....................................................................... 9 Avalanche on Shisha Pangma .................................................................. 9 First Ascent of Gashebrum V (747m) .....................................................0 First Ascent of Payu Peak (6600m) South Pillar ......................................2 Russians Climb Unclimbed 1900m Face of Thamserku .........................3 The Himalayan Club - Pune Section The story of the club’s youngest and a vibrant section. ..........................4 The Himalayan Club – Kolkata Section Commemoration of Birth Centenary of Tenzing Norgay .........................8 The Himalayan Club – Mumbai Section Journey through my Lense - Photo Exhibition by Mr. Deepak Bhimani ................................................9 News & Views The Himalayan Club Hon. Local Secretary in Kathmandu Ms. Elizabeth Hawley has a peak named after her .................................9 Climbing Fees Reduced in India ............................................................. 22 04 New Peaks open for Mountaineering in Nepal ................................ 23 Online Show on Yeti ............................................................................... -
William S. Sax
WILLIAM S. SAX The Royal Pilgrimage of the Goddess Nanda Introduction: the goddess and her pilgrimage Once every twelve years, when it is thought that some calamity has taken place because of the curse of the goddess Nanda Devi, a four-horned ram is born in the fields of the former king of Garhwal, an erstwhile Central Himalayan kingdom in north India (see map of Garhwal). This four-horned ram leads a procession of priests and pilgrims on the most dangerous and spectacular pilgrimage in all of India: a three-week, barefoot journey of one-hundred and sixty-four miles, during some of the worst weather of the year, at the end of the rainy season. The procession reaches Rupkund, a small pond located at an altitude of more than 5,000 metres, which is surrounded by human skeletons, and from there it goes yet further, to Homkund, the ‘Lake of the Fire Sacrifice’. According to the faithful, the four-horned ram leaves the procession at that point and finds its way, unaided, to the summit of Mount Trishul. As its name suggests, the Royal Procession is closely associated with the ruler of this erstwhile Himalayan kingdom: he attends its inaugural rituals, the bones that litter the shores of Rupkund are believed to be those of one of his ancestors, and the chief sponsor of the event is a local ‘Prince’ who is thought to be descended from the first kings of Garhwal. This Prince traverses the domain of his ancestors and thereby lays claim to it in the name of the goddess Nanda, who is not only his lineage goddess but was also the royal goddess of the neighbouring kingdom of Kumaon, in pre-colonial times. -
Ganga As Perceived by Some Ganga Lovers Mother Ganga's Rights Are Our Rights
Ganga as Perceived by Some Ganga Lovers Mother Ganga’s Rights Are Our Rights Pujya Swami Chidanand Saraswati Nearly 500 million people depend every day on the Ganga and Her tributaries for life itself. Like the most loving of mothers, She has served us, nourished us and enabled us to grow as a people, without hesitation, without discrimination, without vacation for millennia. Regardless of what we have done to Her, the Ganga continues in Her steady fl ow, providing the waters that offer nourishment, livelihoods, faith and hope: the waters that represents the very life-blood of our nation. If one may think of the planet Earth as a body, its trees would be its lungs, its rivers would be its veins, and the Ganga would be its very soul. For pilgrims, Her course is a lure: From Gaumukh, where she emerges like a beacon of hope from icy glaciers, to the Prayag of Allahabad, where Mother Ganga stretches out Her glorious hands to become one with the Yamuna and Saraswati Rivers, to Ganga Sagar, where She fi nally merges with the ocean in a tender embrace. As all oceans unite together, Ganga’s reach stretches far beyond national borders. All are Her children. For perhaps a billion people, Mother Ganga is a living goddess who can elevate the soul to blissful union with the Divine. She provides benediction for infants, hope for worshipful adults, and the promise of liberation for the dying and deceased. Every year, millions come to bathe in Ganga’s waters as a holy act of worship: closing their eyes in deep prayer as they reverently enter the waters equated with Divinity itself. -
Ganges Strategic Basin Assessment
Public Disclosure Authorized Report No. 67668-SAS Report No. 67668-SAS Ganges Strategic Basin Assessment A Discussion of Regional Opportunities and Risks Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized GANGES STRATEGIC BASIN ASSESSMENT: A Discussion of Regional Opportunities and Risks b Report No. 67668-SAS Ganges Strategic Basin Assessment A Discussion of Regional Opportunities and Risks Ganges Strategic Basin Assessment A Discussion of Regional Opportunities and Risks World Bank South Asia Regional Report The World Bank Washington, DC iii GANGES STRATEGIC BASIN ASSESSMENT: A Discussion of Regional Opportunities and Risks Disclaimer: © 2014 The International Bank for Reconstruction and Development / The World Bank 1818 H Street NW Washington, DC 20433 Telephone: 202-473-1000 Internet: www.worldbank.org All rights reserved 1 2 3 4 14 13 12 11 This volume is a product of the staff of the International Bank for Reconstruction and Development / The World Bank. The findings, interpretations, and conclusions expressed in this volume do not necessarily reflect the views of the Executive Directors of The World Bank or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Rights and Permissions The material in this publication is copyrighted. Copying and/or transmitting portions or all of this work without permission may be a violation of applicable law. -
Drainage System
CHAPTER DRAINAGE SYSTEM ou have observed water flowing through 2006) in this class . Can you, then, explain the the rivers, nalas and even channels reason for water flowing from one direction to Yduring rainy season which drain the the other? Why do the rivers originating from the excess water. Had these channels not been Himalayas in the northern India and the Western there, large-scale flooding would have Ghat in the southern India flow towards the east occurred. Wherever channels are ill-defined or and discharge their waters in the Bay of Bengal? choked, flooding is a common phenomenon. The flow of water through well-defined channels is known as ‘drainage’ and the network of such channels is called a ‘drainage system’. The drainage pattern of an area is the outcome of the geological time period, nature and structure of rocks, topography, slope, amount of water flowing and the periodicity of the flow. Do you have a river near your village or city? Have you ever been there for boating or bathing? Figure 3.1 : A River in the Mountainous Region Is it perennial (always with water) or ephemeral (water during rainy season, and dry, otherwise)? A river drains the water collected from a Do you know that rivers flow in the same specific area, which is called its ‘catchment area’. direction? You have studied about slopes in the An area drained by a river and its tributaries other two textbooks of geography (NCERT, is called a drainage basin. The boundary line Important Drainage Patterns (i) The drainage pattern resembling the branches of a tree is known as “dendritic” the examples of which are the rivers of northern plain. -
Regular Article Psychrophilic Microbial
REGULAR ARTICLE PSYCHROPHILIC MICROBIAL DIVERSITY AND PHYSICOCHEMICAL CHARACTERISTICS OF GLACIERS IN THE GARHWAL HIMALAYA, INDIA Rahul Kumar* and Ramesh C. Sharma Address (es): Dr. Rahul Kumar Laboratory of Environmental Microbiology and Biotechnology, Department of Environmental Sciences, H.N.B. Garhwal University (A Central University), Srinagar Garhwal- 246174, Uttarakhand, India *Corresponding author: [email protected] ABSTRACT The main objective of the current research work was to investigate the physicochemical properties of ice samples collected from the snout of three important glaciers located in the Garhwal Himalaya along with the psychrophilic microbial diversity. This study was carried out for two years from 2015 to 2016 with two sampling attempts each year. Ice samples were collected from all the pre-identified sampling sites at a depth of 5cm to observe and record the characteristics and to isolate and identify the psychrophilic diversity of microorganisms. Overall fourteen physical and chemical properties of ice samples were recorded. The psychrophilic microbial diversity was identified through the morphological, biochemical and MALDI-TOF-MS techniques. The α–diversity of microbes in the ice of Satopanth glacier was 17 with 08 bacterial species, 04 actinomycetes species and 05 fungal species. However, the α–diversity of microbes in the ice of Bhagirathi-Kharak glacier was also 17 with 06 bacterial species, 05 actinomycetes species and 06 fungal species. The α–diversity of microbes in the ice of Gangotri glacier was 19 with 09 bacterial species, 05 actinomycetes species and 05 fungal species. The present research work can be a decent reference for additional investigations in a similar discipline. The available data will also help the researchers to study the psychrophiles, their existence in glaciers and their importance to society. -
Determining the Barriers to and Opportunities for Community Involvement in the Management of the Nanda Devi Biosphere Reserve, Uttarakhand, India
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2016 Determining the barriers to and opportunities for community involvement in the management of the Nanda Devi Biosphere Reserve, Uttarakhand, India Trisha Singh Follow this and additional works at: https://scholarworks.umt.edu/etd Part of the Biodiversity Commons, and the Ecology and Evolutionary Biology Commons Let us know how access to this document benefits ou.y Recommended Citation Singh, Trisha, "Determining the barriers to and opportunities for community involvement in the management of the Nanda Devi Biosphere Reserve, Uttarakhand, India" (2016). Graduate Student Theses, Dissertations, & Professional Papers. 4574. https://scholarworks.umt.edu/etd/4574 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]. DETERMINING THE BARRIERS TO AND OPPORTUNITIES FOR COMMUNITY INVOLVEMENT IN MANAGEMENT OF THE NANDA DEVI BIOSPHERE RESERVE, UTTARAKHAND, INDIA By TRISHA SINGH B.S. Wildlife Ecology, University of Maine, Orono, Maine, 2009 Thesis Presented in partial fulfillment of the requirements for the degree of Master of Science Resource Conservation, Option (International Conservation and Development) The University -
The Nanda Devi Basin.1
58 The N anda Devi Basin. land to the sea, which, as usual, according to our experience, lay under a blanket of yellow fog. When we left the summit we descended towards the S.W. to a glacier upon which we turned theW. flank of our pealL We regained our depression of the morning, returning by the same line to the head of Eglinton Fjord. ILLUSTRATIONS. I. M. H. Ritchie. Fjord scenery to the E., from summit of Sanderson's Hope. 2. M. H. Ritchie. Devil's Thumb from the W. Climber's route by ridge facing camera. 3. M. H. Ritchie. View N. from nameless peak near head of Eglinton Fjord (climbed by Longstaff and Hanhan). 4. M. H. Ritchie. Early morning view towards glen near head of Eglinton _ Fjord (taken from a peak of 5050 ft.). 5. M. H. Ritchie. Vertical slabs on peak in Eglinton Fjord, Baffin Land. ' THE NANDA DEVI BASIN.1 BY E. E. SHIPTON. (Read before the Alpine Club, March 5, 1935.) ERHAPS one of the principal objects I had in mind when I decided to go to the Himalaya last year was to prove to my O"\vn satisfaction at least : first, that the small self-contained party is in a position to obtain far better results from the mountaineering point of vie'v than the big, unwieldy expedition which, for some obscure reason, since the war has been thought necessary for a Himalayan campaign; and, second, that the prevalent opinion regarding the cost of Himalayan expeditions is vastly exaggerated. Our party consisted of t'vo Europeans, H.