Lulc Classifications Using Gis and Remote Sensing Techniques in Gori Ganga Watershed of Kumaun Himalaya, Uttarakhand
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Gori River Basin Substate BSAP
A BIODIVERSITY LOG AND STRATEGY INPUT DOCUMENT FOR THE GORI RIVER BASIN WESTERN HIMALAYA ECOREGION DISTRICT PITHORAGARH, UTTARANCHAL A SUB-STATE PROCESS UNDER THE NATIONAL BIODIVERSITY STRATEGY AND ACTION PLAN INDIA BY FOUNDATION FOR ECOLOGICAL SECURITY MUNSIARI, DISTRICT PITHORAGARH, UTTARANCHAL 2003 SUBMITTED TO THE MINISTRY OF ENVIRONMENT AND FORESTS GOVERNMENT OF INDIA NEW DELHI CONTENTS FOREWORD ............................................................................................................ 4 The authoring institution. ........................................................................................................... 4 The scope. .................................................................................................................................. 5 A DESCRIPTION OF THE AREA ............................................................................... 9 The landscape............................................................................................................................. 9 The People ............................................................................................................................... 10 THE BIODIVERSITY OF THE GORI RIVER BASIN. ................................................ 15 A brief description of the biodiversity values. ......................................................................... 15 Habitat and community representation in flora. .......................................................................... 15 Species richness and life-form -
Timber Line Delineations Using NDVI Techniques in the Gori Ganga Watershed of Kumaun Himalaya, Uttarakhand
Quest Journals Journal of Research in Environmental and Earth Sciences Volume 7 ~ Issue 4 (2021) pp: 40-45 ISSN(Online) :2348-2532 www.questjournals.org Research Paper Timber Line Delineations Using NDVI Techniques in the Gori Ganga Watershed of Kumaun Himalaya, Uttarakhand D. S. Parihar Department of Geography, Kumaun University, S.S.J Campus, Almora (Uttarakhand), India-263601 ABSTRACT Present research paper is an attempt to delineations the timber line by using Normalized Difference Vegetation Index (NDVI) in the Gori Ganga watershed, Kumaun Himalaya, Uttarakhand (India). The objective of the present study is delineation of vegetation lines of the Gori Ganga watershed in time space. For the study of detect timber line used of Landsat-5, 8 and Cartosat-1 satellite imageries of three different time periods like Landsat-5 Thematic Mapper (TM) of 1990, Landsat-5 (TM) of 1999 and Landsat-8 Operational Land Imager and Thermal Infrared Sensor (OLI and TIRS) of 2016 and Cartosat-1 of 2008. Geographical distribution of timber line average height reveals that in 1990 was about 3516.11 m (± 369 m) which varies between 1729 m to 4560 m, in 1999 was about 3680.69 m (± 362 m) which varies between 2654 m to 6093 m and in 2016 was about 4060.58 m (± 619 m) which varies between 3125 m to 5185 m. KEY WORDS: NDVI Techniques, Timber line, Remote Sensing and GIS Received 25 April, 2021; Revised: 06 May, 2021; Accepted 08 May, 2021 © The author(s) 2021. Published with open access at www.questjournals.org I. INTRODUCTION Ecosystem provides various forms of services through payment mechanism which contributes surplus money to national income and supports to improve the local livelihoods (Khanal et al., 2014). -
India L M S Palni, Director, GBPIHED
Lead Coordinator - India L M S Palni, Director, GBPIHED Nodal Person(s) – India R S Rawal, Scientist, GBPIHED Wildlife Institute of India (WII) G S Rawat, Scientist Uttarakhand Forest Department (UKFD) Nishant Verma, IFS Manoj Chandran, IFS Investigators GBPIHED Resource Persons K Kumar D S Rawat GBPIHED Ravindra Joshi S Sharma Balwant Rawat S C R Vishvakarma Lalit Giri G C S Negi Arun Jugran I D Bhatt Sandeep Rawat A K Sahani Lavkush Patel K Chandra Sekar Rajesh Joshi WII S Airi Amit Kotia Gajendra Singh Ishwari Rai WII Merwyn Fernandes B S Adhikari Pankaj Kumar G S Bhardwaj Rhea Ganguli S Sathyakumar Rupesh Bharathi Shazia Quasin V K Melkani V P Uniyal Umesh Tiwari CONTRIBUTORS Y P S Pangtey, Kumaun University, Nainital; D K Upreti, NBRI, Lucknow; S D Tiwari, Girls Degree College, Haldwani; Girija Pande, Kumaun University, Nainital; C S Negi & Kumkum Shah, Govt. P G College, Pithoragarh; Ruchi Pant and Ajay Rastogi, ECOSERVE, Majkhali; E Theophillous and Mallika Virdhi, Himprkrthi, Munsyari; G S Satyal, Govt. P G College Haldwani; Anil Bisht, Govt. P G College Narayan Nagar CONTENTS Preface i-ii Acknowledgements iii-iv 1. Task and the Approach 1-10 1.1 Background 1.2 Feasibility Study 1.3 The Approach 2. Description of Target Landscape 11-32 2.1 Background 2.2 Administrative 2.3 Physiography and Climate 2.4 River and Glaciers 2.5 Major Life zones 2.6 Human settlements 2.7 Connectivity and remoteness 2.8 Major Land Cover / Land use 2.9 Vulnerability 3. Land Use and Land Cover 33-40 3.1 Background 3.2 Land use 4. -
Nanda Devi – Milam Valley, India
NANDA DEVI – MILAM VALLEY, INDIA Land-only duration: 22 days Grade: Moderate Trekking days: 15 days Max altitude: 3835m (option to 4500m) 2015 price: contact us We can run this on dates to suit you for a minimum group size of 1. Dates: The 2 main trekking seasons are Spring and Autumn. Contact us at [email protected] with your preferred dates tel (within UK: 01244 940 940 tel (outside UK): +44 1244 940 940 email: [email protected] web: www.trekmountains.com skype ID: trekMountains The twin peaks of 7818m Nanda Devi form India’s second highest mountain, situated in a remote region bordering Nepal and Tibet. The alpine glaciers, high valleys and flower- strewn meadows on the eastern approach to this magnificent mountain are an enticing world apart, and ideal for trekking. The area remains one of the lesser trod regions of the Indian Himalaya, - welcome news for the connoisseur trekker. A fascinating drive from Delhi across the northern plains of India brings us to the foothills of the Himalaya and border region of Kumaon. Our trek begins at the quiet hill town of Munsiari where we descend to the lush Milam Valley, whose semi-tropical rainforests are alive with huge butterflies, exotic birds and large lizards. Once an important trade route, the broad trail was built by the British and is still used by local people to travel from village to village. Following the gorge of the Gori Ganga, we weave high above its foaming waters, climbing steadily among rhododendron forests, which support a botanist’s paradise of ferns orchids, peonies and hydrangea. -
Nanda Devi : the 'Bliss Giving' Goddess of Kumaun
1 NANDA DEVI : THE ‘BLISS GIVING’ GODDESS OF KUMAUN Mountains, like men, have their history. They too are born, grow, decay and die. One cannot claim that, like men, they love, but it is true - and how true – that they are loved. Felice Benuzzi, No Picnic on Mount Kenya The twin peaks of Nanda Devi (7,816 m) and Nanda Devi East (7,434 m) of Kumaun stand majestically in the centre of a ring of mountains, distinct and beautiful, particularly as the first and the last rays of the sun caress their summits. Hugh Ruttledge, a British explorer, after his attempt to find a route to these peaks in 1932, described the Nanda Devi Sanctuary in a letter to The Times, London: “A seventy- mile barrier ring on which stand twelve measured peaks of over 21,000 ft, which has no depression lower than 17,000 ft except in the west where the Rishi Ganga rising at the foot of Nanda Devi draining the area of some 250 square miles (800 square kilometres) of snow and ice has earned for itself what must be one of the most terrific gorges in the world.” Without the Sanctuary and its wall of high peaks to absorb the main thrust of the icy Tibetan winds, the Gangetic plains, the granary of India, would have been stripped barren. History In 1883, in one of the first attempts to reach the inner sanctuary, W W Graham, a British traveller, tried to forge a way through the Rishi Ganga gorge, failing to make much headway. -
Adverse Anthropogenic Impacts in Yarsa-Gambu and Alpine Region in the Gori Ganga Watershed Kumaun Himalaya
SSRG International Journal of Geo-informatics and Geological Science Volume 8 Issue 2, 26-36, May-Aug, 2021 ISSN: 2393 – 9206 /doi:10.14445/23939206/IJGGS-V8I2P103 © 2021 Seventh Sense Research Group® Adverse Anthropogenic Impacts in Yarsa-Gambu and Alpine Region in the Gori Ganga Watershed Kumaun Himalaya D. S.Parihar1, J. S. Rawat2 and Deepak3 Department of Geography, Kumaun University, S.S.J. Campus, Almora, India- 263601 Received Date: 22 May 2021 Revised Date: 26 June 2021 Accepted Date: 09 July 2021 ABSTRACT playsaprominentrolein the Himalayan region, in the socio- Caterpillar Fungus is an endemic herb of economy of rural people (Shrestha et al., the higher Himalayan regions. It has become the very 2014,Pantetal2017). Various parts of the Tibet region show important source of cash income in whole areas of that soaring prices of caterpillar fungus have to increases Kumaun Himalaya, where it is known as Yarsa-Gambu, in annual cash income for certain households. In some ‘summer-grass-winter-worm’, this new occupation of the locations, caterpillar fungus accounts for 50-80% of total local inhabitant arisen out of extraction of Yarsa-Gambu rural income, making it one of the most common profitable in the higher Himalayan areas is now struggling for its local sources of income (Winkler 2008; Woodhouse et al., survival due to various anthropogenic activities. The 2013).Pandey andPokhrel, 2020 presented opportunities adverse anthropogenic activities are (i) increase human and challenges in Yarsagumba collection and onsite pressure in the caterpillar growing areas is steadily trading in district Darchula (Nepal) and district increasing the atmospheric temperature in the region, Pithoragadh (India) from an institutional perspective. -
Uttarakhand State Perspective and Strategic Plan 2009-2027 Watershed Directorate, Management Dehradun
Uttarakhand State Perspective and Strategic Plan 2009-2027 Watershed Management Directorate, Watershed Dehradun TABLE OF CONTENTS Executive Summary List of Abbreviations Chapter-1 – Introduction 1-5 Chapter-2 - About the State 6-39 General State Profile Physiographic Zones of Uttarakhand Land use Natural Resource Base of Uttarakhand Forest Cover Water Regime Development Indicators of the State Operational and Livelihood Status Irrigation Status Drought and Floods Agricultural Growth and Development Inputs in Agriculture Status of Forests Livestock Fisheries Agriculture Marketing, Credit and Processing Chapter-3 - Status of Rainfed Areas in the State 40-82 Position of Rainfed Area in the State Livelihood Analysis in Rainfed Areas Major Problems and Constraints of Agriculture Production in Uttarakhand Yield Gaps of Major Crops Yield Gaps in Horticulture Crops Yield Gaps in Fisheries Inputs, Credits, Processing and Marketing Gaps Technology/Extension/ Adoption Gaps Infrastructural and Institutional Gaps Chapter-4 - Major Programs / Schemes and Impacts 83-98 Major Programs/Schemes/Projects Operational In the State Analysis of Various Programs/ Schemes Chapter – 5 - Issues and Challenges 99-110 Challenges for Food Security Challenges for Water Security Challenges for Feed and Fodder Security Challenges for Environmental Security Challenges for Livelihood Security Chapter – 6 - Vision and Mission 111-112 Vision of Watershed Management Directorate Mission Statement Chapter -7 – Perspective 113-143 Need for Perspective Plan Project Area Soil -
Morphotectonic Indices of Drainage And
Aligarh Muslim University Department of Geology December 16, 2016 Dr. S. Farooq Professor CERTIFICATE This is to certify that Mr. Mohd. Nazish Khan has carried out the investigation on Morphotectonic indices of drainage and landscape and their bearing on active tectonics in the Goriganga River Basin, eastern Kumaon Himalaya under my supervision for award of the degree of Doctor of Philosophy of the Aligarh Muslim University, Aligarh. The work is an original contribution to the existing knowledge of the subject. He is allowed to submit the work for award of the Ph.D. degree of the Aligarh Muslim University, Aligarh. Dr. S. Farooq (Supervisor) Acknowledgement I wish to thank Prof. S. Farooq for creating in me an interest in the lofty Himalaya, and processes of active tectonics that perpetually change the shape of this orogen, and for encouraging, helping and guiding me through the years that I’ve been engaged in the investigation of the active tectonic processes in the eastern Kumaon Himalaya. I would like to extend my appreciation to the Aligarh Muslim University for the academic and technical assistance provided to me for the conduct of my research work. Thanks are due to the Chairman Department of Geology for providing institutional facilities necessary for this work. I am also thankful to the University Grants Commission for financial support in the form of a fellowship for the pursuit of this research work. A research grant NRDMS/11/1669/10/Pr:9 by the Department of Science & Technology, Government of India to my research guide, which helped procure data for this study and facilitated field work is gratefully acknowledged. -
ISSN: 2320-5407 Int. J. Adv. Res. 9(03), 30-34
ISSN: 2320-5407 Int. J. Adv. Res. 9(03), 30-34 Journal Homepage: - www.journalijar.com Article DOI: 10.21474/IJAR01/12550 DOI URL: http://dx.doi.org/10.21474/IJAR01/12550 RESEARCH ARTICLE SPATIO-TEMPORAL CHANGE IN SNOW COVER AREA USING RS & GIS IN THE GORI GANGA WATERSHED, KUMAUN HIGHER HIMALAYA D.S. Parihar and J.S. Rawat Department of Geography, Kumaun University, S.S.J. Campus, Almora, Uttarakhand (India). …………………………………………………………………………………………………….... Manuscript Info Abstract ……………………. ……………………………………………………………… Manuscript History Present research paper is an attempt to examine the dynamics of snow Received: 05 January 2021 cover by using Normalized Difference Snow Index (NDSI) in Gori Final Accepted: 09 February 2021 Ganga watershed, Kumaun Himalaya, Uttarakhand (India). For the Published: March 2021 study of snow cover of Landsat satellite imageries of three different time periods like Landsat TM of 1990, Landsat TM of 1999 and Key words: NDSI, Snow Cover Dynamics, Kumaun Landsat TM 2016 were used. Geographical distribution of snow cover 2 Himalaya, Remote Sensing and GIS, reveals that in 1990 about 30.97% (678.87 km ), in 1999 about 25.77% Gori Ganga Watershed (564.92 km2) area of the Gori Ganga watershed was under snow cover while in 2016 the snow cover was found only 15.08% (330.44 km2). These data suggest that due to global warming about 348.43 km2 snow cover of Gori Ganga watershed has been converted into non-snow cover area at an average rate 13.40 km2/year during the last 26 years. Copy Right, IJAR, 2021,. All rights reserved. …………………………………………………………………………………………………….... Introduction:- Snow is a key component for energy balance of the earth’s i.e. -
Geology and Mining Unit Directorate of Industries,Uttarakhand, Bhopalpani, P O Badasi, Raipur –Thano Road, Dehradun -248001
GEOLOGY AND MINING UNIT DIRECTORATE OF INDUSTRIES,UTTARAKHAND, BHOPALPANI, P O BADASI, RAIPUR –THANO ROAD, DEHRADUN -248001 Ref. No. 01 Date: 04/02/2013 Tender Notice For engaging consultants to obtain Environmental Clearance in terms of EIA Notification, 2006 and directions issued by Hon'ble Supreme Court of India vide its orders dated 27.02.2012 in SLP 19628-19629 of 2009, titled Deepak Kumar etc. V/s State of Haryana and others etc. for the quarries of minor minerals namely ordinary sand, gravel/Bajri and boulders in the state of Uttarakhand as given below: Scope of work Pre-Feasibility- 1. Topographical map of core zone and buffer zone in 1:25000 scale if not available then in 1:50000 scale to be prepared. 2. Map (1:25,000) of core zone and 10 km area of buffer zone from boundary of core zone to be prepared from interpretation of satellite imagery of 5.6 m or higher resolution of multi spectral sensor procured from NRSA have to be submitted depicting the following: • Recent land use features in the region. • Other proposed or working mines in the region. • Map Depictions: Colored maps depicting land- use of the region showing sensitive/fragile features and detailed lay-out of the site clearly showing green-belt (existing & planned). • Location with khasra no is also to be shown in Tehsil map procured from revenue department indicating the boundary of each quarry to ensure that the boundary is not touching with the boundary of other quarry. 3. (i) The EIA should be prepared based on model TOR for appraisal of mining projects issued by MoEF, New Delhi/State Environmental Impact Assessment Authority (ii) Data in the EIA should be given for the entire mine life. -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on 30 July 2009 Geological Society of America Bulletin The Kumaun and Garwhal Lesser Himalaya, India: Part 1. Structure and stratigraphy Julien Célérier, T. Mark Harrison, Andrew Alexander G. Webb and An Yin Geological Society of America Bulletin 2009;121;1262-1280 doi: 10.1130/B26344.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes © 2009 Geological Society of America Downloaded from gsabulletin.gsapubs.org on 30 July 2009 The Kumaun and Garwhal Lesser Himalaya, India: Part 1. -
''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.