Inventory of Glaciers, Glacial Lakes and the Identification of Potential
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GLACIERS of NEPAL—Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range
Glaciers of Asia— GLACIERS OF NEPAL—Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range By Keiji Higuchi, Okitsugu Watanabe, Hiroji Fushimi, Shuhei Takenaka, and Akio Nagoshi SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, JR., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–F–6 CONTENTS Glaciers of Nepal — Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range, by Keiji Higuchi, Okitsugu Watanabe, Hiroji Fushimi, Shuhei Takenaka, and Akio Nagoshi ----------------------------------------------------------293 Introduction -------------------------------------------------------------------------------293 Use of Landsat Images in Glacier Studies ----------------------------------293 Figure 1. Map showing location of the Nepal Himalaya and Karokoram Range in Southern Asia--------------------------------------------------------- 294 Figure 2. Map showing glacier distribution of the Nepal Himalaya and its surrounding regions --------------------------------------------------------- 295 Figure 3. Map showing glacier distribution of the Karakoram Range ------------- 296 A Brief History of Glacier Investigations -----------------------------------297 Procedures for Mapping Glacier Distribution from Landsat Images ---------298 Figure 4. Index map of the glaciers of Nepal showing coverage by Landsat 1, 2, and 3 MSS images ---------------------------------------------- 299 Figure 5. Index map of the glaciers of the Karakoram Range showing coverage -
Climate-Glacier Relationship in the Monsoon-Arid Transition Zone: a Case Study in Himachal Pradesh, India
Climate-Glacier relationship in the monsoon-arid transition zone : A Case study in Himachal Pradesh, India Farooq Azam Mohd To cite this version: Farooq Azam Mohd. Climate-Glacier relationship in the monsoon-arid transition zone : A Case study in Himachal Pradesh, India. Earth Sciences. Université de Grenoble, 2014. English. NNT : 2014GRENU032. tel-01230980 HAL Id: tel-01230980 https://tel.archives-ouvertes.fr/tel-01230980 Submitted on 19 Nov 2015 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. THESIS Submitted to obtain the degree of DOCTOR OF THE UNIVERSITY OF GRENOBLE Speciality : Earth Sciences, Universe and Environment Arrêté ministériel : 1 November 2011 Presented by Mohd Farooq AZAM Thesis directed by Patrick Wagnon and co-directed by Christian Vincent & Ramanathan Alagappan Prepared in the Laboratoire de Glaciologie et de Géophysique de l’Environnement/Laboratoire d'Etudes des Transferts en Hydrologie et Environnement, UJF/CNRS in Doctoral school Earth Sciences, Universe and Environment Climate-Glacier relationship in the monsoon-arid transition zone: A Case study in Himachal Pradesh, India. Defended publicly : 17 December 2014, Before the jury : Mr. Gerhard KRINNER Research Director, CNRS, LGGE (France), President Mr. Martin HOELZLE Professor, University of Fribourg (Switzerland), Reporter Mr. -
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 -
Quarrernary GEOLOGY of MINNESOTA and PARTS of ADJACENT STATES
UNITED STATES DEPARTMENT OF THE INTERIOR Ray Lyman ,Wilbur, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director P~ofessional Paper 161 . QUArrERNARY GEOLOGY OF MINNESOTA AND PARTS OF ADJACENT STATES BY FRANK LEVERETT WITH CONTRIBUTIONS BY FREDERICK w. SARDE;30N Investigations made in cooperation with the MINNESOTA GEOLOGICAL SURVEY UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1932 ·For sale by the Superintendent of Documents, Washington, D. C. CONTENTS Page Page Abstract ________________________________________ _ 1 Wisconsin red drift-Continued. Introduction _____________________________________ _ 1 Weak moraines, etc.-Continued. Scope of field work ____________________________ _ 1 Beroun moraine _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 47 Earlier reports ________________________________ _ .2 Location__________ _ __ ____ _ _ __ ___ ______ 47 Glacial gathering grounds and ice lobes _________ _ 3 Topography___________________________ 47 Outline of the Pleistocene series of glacial deposits_ 3 Constitution of the drift in relation to rock The oldest or Nebraskan drift ______________ _ 5 outcrops____________________________ 48 Aftonian soil and Nebraskan gumbotiL ______ _ 5 Striae _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 48 Kansan drift _____________________________ _ 5 Ground moraine inside of Beroun moraine_ 48 Yarmouth beds and Kansan gumbotiL ______ _ 5 Mille Lacs morainic system_____________________ 48 Pre-Illinoian loess (Loveland loess) __________ _ 6 Location__________________________________ -
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 ................................................................................................... -
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. -
Rupsiyabagar-Khasiyabara Hydroelectric Power Project
CENTREFOR WILDLIFESTUDIES August3,2012 Admln. Ofrice: # {669, 31st Cross, l6th Main, Banashankari 2nd Stage, Dr.P.J. Dilip Kumar, IFS Bengaluru - 560 070, Indla. Chair,Forest Advisory Committee Tel. : +91 80 26715364,Tele Fax : +9'l 80 26715255 DirectorGeneral of Forests WEBSITE : rrvwwwcslndia.org Regd. Oflice: 26-2,Aga Abbas Ali Road (Apt.403) Ministryof Environmentand Forests Bengaluru - 560 042, lndia. ParyavaranBhavan CGOComplex, Lodhi Road NewDelhi-1 10003 Sub:Final Report of thesub-committee of the FACon the Rupsiyabagar Khasiyabarahydroelectric project i n Munsiyari (RKH PP), Uttarakhand. Sir, This reportpertains to the site inspectionthat I had carriedout withAIGF Sri HC Choudhryon April21-22,2012. The site inspection was relatedto the 261 MW Rupsiyabagar-KhasiyabaraHydro-Power Project ("RK HPP" for short)in Pithoragarhdistrict of Uttarakhand,proposed by the NationalThermalPower CorporationLimited (henceforth NTPC). The StateGovernment of Uttarakhand videtheir letter dated 21.12.2009 submitted a proposalto obtainprior approval of CentralGovernment under the Forest(Conservation) Act, 1980 for diversionof 217.522 hectare of forestland for 30 years,in favourof the useragency. The proposalwas examinedby the ForestAdvisory Committee ('FAC", for short)on 25.05.2010and rejected. As you are aware,in responseto a representationfonryarded by the Nodal Officer,Forest (Conservation)Act, 1980 (Government of Uttarakhand)in his letterdated 15.09.2010, requesting the MoEFto re-considerits decision to declineapproval of the CentralGovernment, the ForestAdvisory Committee set- up a sub-committeeto undertakea site inspection. Accordingly,the abovesub-committee of the FAC,headed by me, inspectedthe site identifiedfor constructionof the RK HPP in orderto assessfirst-hand the floraand faunaavailable in and aroundthe forestland proposed for diversion and the ecologicalvalue of the area.The mandatedinspection was carriedon 21stand 22nd April 2012. -
Climate Vulnerability in North Western Himalayas
Climate Vulnerability in North Western Himalayas Mukesh Ray, NeerajDoshi, NishantAlag and R.Sreedhar Environics Trust, 2011 A Contribution to the Ongoing Nation-wide Climate Studies Vulnerability in Various Ecoregions of India, 2011 Indian Network on Ethics and Climate Change (INECC) CONTENTS 1.0 INTRODUCTION 2.0 THE HIMALAYAS - PHYSIOGRAPHIC FEATURES 3.0 VULNERABILITY OF THE NORTH WESTERN HIMALAYAS 4.0 ENVIRONMENTS OF CONCERN 5.0 REDUCING RISKS DUE TO CLIMATE CHANGE 1.0 INTRODUCTION Global warming induced climate change has triggered events such as melting glaciers, rising sea levels and changing weather patterns.This in turn has lead to storms, droughts, flash floods, cloudbursts, change in vegetation. Growing body of scientific evidence has established that this phenomenon is directly linked to unprecedented amount of GHG gases released in the atmosphere largely due to burning of fossil fuels since the beginning of industrialization in last century. The situation is likely to worsenas countries with low industrialization including China and India began to pursue the same path of carbon based economic growth. However, the impact of climate change is not distributed evenly across the world. Mountain eco-systems are more sensitive to the habitat and climate change due to the interaction of tectonic, geomorphic, ecological and climate agents. For instance, temperatures are rising more rapidly in the Himalayas than the global average. Over the last decade the average temperature in Nepal has risen 0.6 degrees, compared with an increase in average temperatures globally of 0.7 degrees over the last hundred years (Gravgaard, 2010). In another Himalayan region, Tibetan Plateau, temperatures have gone up over three times the global average (Schell, 2010). -
Pleistocene Geology of Eastern South Dakota
Pleistocene Geology of Eastern South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 262 Pleistocene Geology of Eastern South Dakota By RICHARD FOSTER FLINT GEOLOGICAL SURVEY PROFESSIONAL PAPER 262 Prepared as part of the program of the Department of the Interior *Jfor the development-L of*J the Missouri River basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $3 (paper cover) CONTENTS Page Page Abstract_ _ _____-_-_________________--_--____---__ 1 Pre- Wisconsin nonglacial deposits, ______________ 41 Scope and purpose of study._________________________ 2 Stratigraphic sequence in Nebraska and Iowa_ 42 Field work and acknowledgments._______-_____-_----_ 3 Stream deposits. _____________________ 42 Earlier studies____________________________________ 4 Loess sheets _ _ ______________________ 43 Geography.________________________________________ 5 Weathering profiles. __________________ 44 Topography and drainage______________________ 5 Stream deposits in South Dakota ___________ 45 Minnesota River-Red River lowland. _________ 5 Sand and gravel- _____________________ 45 Coteau des Prairies.________________________ 6 Distribution and thickness. ________ 45 Surface expression._____________________ 6 Physical character. _______________ 45 General geology._______________________ 7 Description by localities ___________ 46 Subdivisions. ________-___--_-_-_-______ 9 Conditions of deposition ___________ 50 James River lowland.__________-__-___-_--__ 9 Age and correlation_______________ 51 General features._________-____--_-__-__ 9 Clayey silt. __________________________ 52 Lake Dakota plain____________________ 10 Loveland loess in South Dakota. ___________ 52 James River highlands...-------.-.---.- 11 Weathering profiles and buried soils. ________ 53 Coteau du Missouri..___________--_-_-__-___ 12 Synthesis of pre- Wisconsin stratigraphy. -
(A) Revised Fee Structure Is Applicable for the Climbing Season 2020 Only
ANNEXURE REDUCTION/DISCOUNTS ON PEAK FEE TO OTHERS FOR LESS CLIMBED PEAKS Height of Peak Existing Peak Fee ProposeD peak Fee for the Climbing Season 2020 Below 6500 M (1) US$ 500 for party of two 1) US$ 250 for party of two members. members. (List of peaks attacheD AppenDix “A”) (2) For additional members upto (2) For additional members twelve, US$ 225 each. upto twelve, US$ 110 each. 6501 M to 7000 M (1) US$ 700 for party of two (1) US$ 350 for party of two members. members. (List of Peaks attacheD AppenDix “B”) (2) For additional members upto (2) For additional members upto twelve, US$ 325 each. twelve, US$ 165 each. 7001 M anD above (1) US$ 1000 for party of two (1) US$ 500 for party of two members. members. (List of Peaks attacheD AppenDix “C”) (2) For additional members upto (2) For additional members upto twelve, US$ 450 each. twelve, US$ 225 each. Trekking Peaks (List of (1) US$ 100 for party of two (1) US$ 100 for party of two peak AppenDix “D”) members. members. (2) For additional members upto (2) For additional members upto twelve, US$ 50 each twelve, US$ 50 each Note : (a) Revised fee structure is applicable for the climbing season 2020 only. (b) There is no change in other terms and conditions applicable. Appendix “A” PEAKS BELOW 6500 M IN OPEN AREA J&K S.NO. Name of peak Height Longitude Latitude Remarks 1. Bobang 5971 M 76° 08’ 33° 25’ Leh-Harpass-Kijai Nala- Nagdal Lake-C-I-CII Summit Attempt 2. -
Everest Base Camp Trek 12 D/11 N
Everest Base Camp Trek 12 D/11 N Pre Trek: Travel to Kathmandu (1,300m): To ensure all permit paperwork and other necessary arrangements are completed before you trip it is important that you are in Kathmandu at least 24 hours prior to the trek commencement. The local operator will contact you to collect the required documents early in the afternoon. At 5:00 pm (17:00) a rickshaw will pick you up from your hotel and bring you to the trekking offices for a safety briefing on the nature of the trek, equipment and team composition. You will meet your trek leader and other team members. You can also make your last minute purchases of personal items as you will be flying to the Himalayas tomorrow. At 6:00 pm (18:00) we will make our way to a welcome dinner and cultural show where you will learn about Nepali culture, music and dance and get to know your trekking team. Overnight in Kathmandu (self selected) Included meals: Dinner DAY 01: Kathmandu to Lukla then trek to Phakding (2,652m): 25 minute flight, plus 3 to 4 hour trek. After breakfast you will be escorted to the domestic terminal of Kathmandu airport for an early morning flight to Lukla (2,800m), the gateway destination where our trek begins. After an adventurous flight above the breathtaking Himalaya, we reach the Tenzing-Hillary Airport at Lukla. This is one of the most beautiful air routes in the world culminating in a dramatic landing on a hillside surrounded by high mountain peaks. -
Damage from the April-May 2015 Gorkha Earthquake Sequence in the Solukhumbu District (Everest Region), Nepal David R
Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard To cite this version: David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard. Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal. GSA Annual Meeting, Sep 2016, Denver, United States. hal-01373311 HAL Id: hal-01373311 https://hal.archives-ouvertes.fr/hal-01373311 Submitted on 28 Sep 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. DAMAGE FROM THE APRIL-MAY 2015 GORKHA EARTHQUAKE SEQUENCE IN THE SOLUKHUMBU DISTRICT (EVEREST REGION), NEPAL LAGESON, David R.1, FORT, Monique2, BHATTARAI, Roshan Raj3 and HUBBARD, Mary1, (1)Department of Earth Sciences, Montana State University, 226 Traphagen Hall, Bozeman, MT 59717, (2)Department of Geography, Université Paris Diderot, 75205 Paris Cedex 13, Paris, France, (3)Department of Geology, Tribhuvan University, Tri-Chandra Campus, Kathmandu, Nepal, [email protected] ABSTRACT: Rapid assessments of landslides Valley profile convexity: Earthquake-triggered mass movements (past & recent): Traditional and new construction methods: Spectrum of structural damage: (including other mass movements of rock, snow and ice) as well as human impacts were conducted by many organizations immediately following the 25 April 2015 M7.8 Gorkha earthquake and its aftershock sequence.