Day 6 Geography Qa Civil Service Corner

Total Page:16

File Type:pdf, Size:1020Kb

Day 6 Geography Qa Civil Service Corner TARGET OCS 2020 DAILY QUIZ DAY – 6 DATE : 29-09-2020 GEOGRAPHY Q Questions Answers Q1 Which of the following is the type of Correct Option: (d) plate Explanation: Option (d) is correct: ContinentContinent boundary of the Indian plate along the convergence is the type of Himalayan Mountains? plate boundary of the Indian plate along (a) Ocean-Continent Convergence the Himalayan mountains. (b) Divergent Boundary Supplementary notes: (c) Transform Boundary Movement of the Indian Plate The Indian plate includes (d) Continent-Continent Convergence Peninsular India and the Australian continental portions. The subduction zone along the Himalayas forms the northern plate boundary in the form of Continent-Continent convergence. In the east, it extends through the Rakinyoma Mountains of Myanmar towards the island arc along the Java Trench. The Western margin follows the Kirthar Mountain of Pakistan. It further extends along the Makrana coast and joins the spreading site from the Red Sea rift southeastward along the Chagos Archipelago. India was a large island situated off the Australian coast, in a vast ocean. The Tethys Sea separated it from the Asian continent until about 225 million years ago. India is supposed to have started her northward journey about 200 million years ago at the time when Pangaea broke. India collided with Asia about 40-50 million years ago causing rapid uplift of the Himalayas. About 140 million years before the present, the subcontinent was located as south as 50 degrees south latitude. The two major plates were separated by the Tethys Sea and the Tibetan block was closer to the Asiatic landmass. During the movement of the Indian plate towards the Asiatic plate, a major event that occurred was the outpouring of lava and formation of CIVIL SERVICE CORNER civilservicecorner.in https://t.me/CSCODISHA1 WHATSAPP- 7682092884 the Deccan Traps. Q2 Peninsular Rivers are characterised by: Correct Option: (d) (a) Fixed course of flow Explanation: Option (d) is correct: Peninsular (b) Absence of meanders Rivers are characterised by fixed (c) Non-perennial flow of water course, absence of meanders and nonperennial flow of (d) All of the above water. Supplementary notes: The Peninsular Drainage System The Peninsular drainage system is older than the Himalayan one. This is evident from the broad, largely-graded shallow valleys, and the maturity of the rivers. The Western Ghats running close to the western coast act as the water divide between the major Peninsular Rivers , discharging their water in the Bay of Bengal and as small rivulets joining the Arabian Sea. Most of the major Peninsular Rivers except Narmada and Tapi flow from west to east. The Chambal, the Sind, the Betwa, the Ken, the Son, originating in the northern part of the Peninsula belong to the Ganga river system. The other major river systems of the peninsular drainage are – the Mahanadi the Godavari, the Krishna and the Kaveri. Peninsular rivers are characterised by fixed course, absence of meanders and non-perennial flow of water. The Narmada and the Tapi, which flow through the rift valley, are exceptions. Q3 Which of the following rivers are the Correct Option: (d) right Explanation: Statements 3 and 4 are incorrect: bank tributaries of Indus? Chenab and Jhelum are left bank tributaries 1. Khurram of River Indus. 2. Tochi Supplementary notes: 3. Chenab Tributaries of Indus River System The Indus receives a 4. Jhelum number of Himalayan 5. Gomal tributaries such as the Shyok, the Gilgit, the Select the correct answer using the code Zaskar, the Hunza, the Nubra, the Shigar, given the Gasting and the Dras. below: It finally emerges out of the hills near (a) 1, 3 and 4 only Attock where it receives the Kabul river on (b) 2 and 4 only its right bank. (c) 2, 3 and 5 only The other important tributaries (d) 1, 2, and 5 only joining the right bank of the Indus are the Khurram, the Tochi, the Gomal, the Viboa and the Sangar. They all originate in the Sulaiman ranges. The river flows southward and receives ‘Panjnad’ a little above Mithankot. The Panjnad is the name given to the five CIVIL SERVICE CORNER civilservicecorner.in https://t.me/CSCODISHA1 WHATSAPP- 7682092884 rivers of Punjab, namely the Satluj, the Beas, the Ravi, the Chenab and the Jhelum. It finally discharges into the Arabian Sea, east of Karachi. The Indus flows in India only through Jammu and Kashmir Q4 “The higher reaches of this region are Correct Option: (b) inhabited Explanation: Option (b) is correct: The Himalaya by Lepcha tribes while the southern part region in this quotation is Darjiling and has Sikkim Himalayas. a mixed population of Nepalis, Supplementary notes: Bengalis, and The Darjiling and Sikkim Himalayas They are flanked tribals from Central India”. The by Nepal Himalayas in the Himalaya west and Bhutan Himalayas in the east. It region in this quotation is: is relatively small but is the most significant (a) Himachal and Uttarakhand part of the Himalayas. Himalayas Known for its fast-flowing rivers such as (b) Darjiling and Sikkim Himalayas Tista, it is a region of high mountain peaks (c) Arunachal Himalayas like Kanchenjunga (Kanchengiri) and deep (d) Kashmir or Northwestern Himalayas valleys. The higher reaches of this region are inhabited by Lepcha tribes while the southern part, particularly the Darjiling Himalayas, has a mixed population of Nepalis, Bengalis and tribals from Central India. Q5 In the Continental Drift Theory, Correct Option: (a) Wegener Explanation: Option (a) is correct: The pole-fleeing suggested that the movement force is created by the centrifugal force from responsible for the Earth’s rotation and by the buldge at the drifting of the continents was caused the slightly flattened Earth’s Equator. by Supplementary notes: pole-fleeing force and tidal force. What Force for Continental Drift The drift was in two is polefleeing force? directions- Equator wards due to the interaction (a) The force created by centrifugal of forces of gravity, pole-fleeing force from force and buoyancy (ship floats in the Earth’s rotation and by the bulge at water due to buoyant force offered by the slightly flattened Earth’s equator. water), and (b) The force created by centripetal Westwards due to tidal force from currents because of the earth’s motion the Earth’s rotation and by the bulge at (earth rotates form west to east, so tidal the slightly flattened Earth’s equator. currents act from east to west). (c) The force created by centrifugal Wegener suggested that tidal force also force played a major role. from the Earth’s rotation and attraction The polar-fleeing force relates to the between Sun and Earth. rotation of the earth. The earth is not (d) The force created by centrifugal a perfect sphere; it has a bulge at the force equator. This bulge is due to the rotation from the Earth’s rotation and attraction of the earth. [Greater Centrifugal force at between Moon and Earth. the equator]. Centrifugal force increases as we move from poles towards equator. This increase in centrifugal force has led to pole fleeing. Tidal force is due to the attraction of CIVIL SERVICE CORNER civilservicecorner.in https://t.me/CSCODISHA1 WHATSAPP- 7682092884 the moon and the sun that develops tides in oceanic waters. Wegener believed that these forces would become effective when applied over many million years. According to Wegener, the drift is still continuing. Causes of Drift are: Gravity of the earth, buoyancy of the seas and the tidal currents were given as the main factors causing the drift, by Wegener. Q6 Match the following: Correct Option: (a) Passes States Explanation: Option (a) is correct: A. Chang La Pass 1. Arunachal Pradesh Passes States B. Kunzum Pass 2. Sikkim A. Chang La Pass 3. Jammu and Kashmir C. Jelep La Pass 3. Jammu & Kashmir B. Kunzum Pass 4. Himachal Pradesh D. Sela Pass 4. Himachal Pradesh C. Jelep La Pass 2. Sikkim Select the correct answer using the code D. Sela Pass 1. Arunachal Pradesh given Supplementary notes: below: Important Passes in India Jelep La Pass - This pass A B C D passes through (a) 3 4 2 1 the Chumbi valley. It connects Sikkim (b) 1 4 2 3 with Lhasa, the capital of Tibet. (c) 3 4 1 2 Chang-La - It is a high mountain pass (d) 2 1 3 4 in the Greater Himalayas. It connects Ladakh with Tibet. Sela Pass – It is in Arunachal Pradesh Kunzum Pass – It is in Himachal Pradesh Bara-La/ Bara- Lacha La - It is situated in the state of Jammu and Kashmir. It connects Manali and Leh. Traill’s Pass - It is located in Uttarakhand. Lipu Lekh - It connects Uttarakhand with Tibet. Mana Pass - It is located in the Greater Himalayas and connects Tibet with Uttarakhand. Debsa Pass - It joins Spiti Valley and Parvati Valley. It is a high mountain pass in between the Kullu and Spiti of Himachal Pradesh. It is a bypass route of Pin-Parvati Pass. Rohtang Pass - This is located in the state of Himachal Pradesh. This pass connects Kullu, Spiti, and Lahul. Khardung La - It is the highest motorable pass in the country. It connects Leh and Siachen glaciers. Nathu La Pass - Sikkim. It forms a part of an offshoot of the ancient silk route. Shipki La Pass - It is located through Sutlej Gorge. It connects Himachal Pradesh with Tibet. CIVIL SERVICE CORNER civilservicecorner.in https://t.me/CSCODISHA1 WHATSAPP- 7682092884 Thang La - It is located in Ladakh. It is the second-highest motorable mountain pass in India. Arunachal Pradesh (India), China, and Myanmar. It lies on the McMahon Line. Banihal Pass (Jawahar Tunnel) - It is situated in the Pir Panjal Range.
Recommended publications
  • Burlington House
    Sutainable Resource Development in the Himalaya Contents Pages 2-5 Oral Programme Pages 6-7 Poster programme Pages 8-33 Oral presentation abstracts (in programme order) Pages 34-63 Poster presentations abstracts (in programme order) Pages 64-65 Conference sponsor information Pages 65-68 Notes 24-26 June 2014 Page 1 Sutainable Resource Development in the Himalaya Oral Programme Tuesday 24 June 2014 09.00 Welcome 11.30 Student presentation from Leh School 11.45 A life in Ladakh Professor (ambassador) Phunchok Stobdan, Institute for Defence Studies and Analyses 12.30 Lunch and posters 14.00 Mountaineering in the Himalaya Ang Rita Sherpa, Mountain Institute, Kathmandu, Nepal Session theme: The geological framework of the Himalaya 14.30 Geochemical and isotopic constraints on magmatic rocks – some constraints on collision based on new SHRIMP data Professor Talat Ahmed, University of Kashmir 15.15 Short subject presentations and panel discussion Moderators: Director, Geology & Mining, Jammu & Kashmir State & Director, Geological Survey of India Structural framework of the Himalayas with emphasis on balanced cross sections Professor Dilip Mukhopadhyay, IIT Roorkee Sedimentology Professor S. K. Tandon, Delhi University Petrogenesis and economic potential of the Early Permian Panjal Traps, Kashmir, India Mr Greg Shellnut, National Taiwan Normal University Precambrian Professor D. M. Banerjee, Delhi University 16.00 Tea and posters 16.40 Short subject presentations continued & panel discussion 18.00 Close of day 24-26 June 2014 Page 2 Sutainable Resource Development in the Himalaya Wednesday 25 June 2014 Session theme: Climate, Landscape Evolution & Environment 09.00 Climate Professor Harjeet Singh, JNU, New Delhi 09.30 Earth surface processes and landscape evolution in the Himalaya Professor Lewis Owen, Cincinnati University 10.00 Landscape & Vegetation Dr P.
    [Show full text]
  • 2014), Latitudinal Variation of Aerosol Where Absorbing Aerosols Are Dominant
    PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Latitudinal variation of aerosol properties from Indo- 10.1002/2013JD021040 Gangetic Plain to central Himalayan foothills Key Points: during TIGERZ campaign • First latitudinal variation of aerosols from IGP to Himalayas U. C. Dumka1, S. N. Tripathi2, Amit Misra2, D. M. Giles3,4, T. F. Eck5,4, Ram Sagar1, and B. N. Holben4 • First comprehensive calculations of heating rate 1Aryabhatta Research Institute of Observational Sciences, Nainital, India, 2Department of Civil Engineering, Indian Institute • Large gradient in heating rates seen 3 4 from IGP to Himalayas of Technology, Kanpur, India, Sigma Space Corporation, Lanham, Maryland, USA, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA, 5Universities Space Research Association, Columbia, Maryland, USA Correspondence to: Abstract As part of TIGERZ campaign, latitudinal variation of aerosol optical properties was analyzed over U. C. Dumka, Indo-Gangetic Plains (IGP) to central Himalayas during premonsoon of 2008 and 2009. Measurements of [email protected]; [email protected] aerosol optical depth (AOD) were performed using Aerosol Robotic Network Sun photometer at four sites with different aerosol environments. The AOD increases from Nainital located in central Himalayas to Kanpur located in IGP region. Further, aerosol size varies spatially with dominance of coarse-mode aerosols at Kanpur Citation: fi Dumka, U. C., S. N. Tripathi, A. Misra, D. M. compared to ne-mode aerosols dominated at Nainital. Spectral variation of single-scattering albedo Giles, T. F. Eck, R. Sagar, and B. N. Holben suggests that during premonsoon, dust is the dominant species in the IGP with exception of Pantnagar, (2014), Latitudinal variation of aerosol where absorbing aerosols are dominant.
    [Show full text]
  • Himalayan Geography: History, Society, and Culture
    Himalayan Geography: History, Society, and Culture Spring 2021, ANTH 0730 WEB Synchronous/Asynchronous T, 8 – 9 am EST via Zoom General Education Requirements: Social Science Specific Geographical Region Mr. Akshay Shah [email protected] Hanifl Center for Outdoor Education, Landour, India 1 COURSE DESCRIPTION The Himalayan region is characterized by a tremendous range of social and cultural diversity that corresponds to climatic, ecological and geographical variation, as well as local and regional geopolitical factors. Historical change from the emergence of early forms of social complexity centered on chiefs and their forts – from which the regional designation of “Garhwal” takes its name – through the development of kingdoms and larger polities, shows the intimate link between geography, environment and socio-political transformation. Similarly, local language patterns, regional religious practices, musical styles, mythology, food culture, sartorial fashion, architectural design, agricultural and transportation technologies and engineering and trade networks have all been shaped by the structure of mountain barriers, bounded valley communities and bracketed lines of communication that follow river systems. Whereas the political economy of the Himalayas has been structured around agricultural production, and the development of elaborate field terrace systems, there have also been subsidiary economies centered on trans-Himalayan trade and pilgrimage as well as pastoral nomadism and transhumance. Since the colonial period, the Himalayas have increasingly become a place for rest, relaxation, tourism and adventure, and this – along with further political transformations since Indian independence -- has led to the rapid development of urban areas. This course will provide a survey of Himalayan history, society and culture with a focus on the relationship between nature, the environment and geography.
    [Show full text]
  • HIMALAYAN WILDLIFE.Pdf
    HIMALAYAN m WILDLIFE pit; Himalayan Wildlife Habitat and Conservation t/ ^ 5 / S.S. NEGI CI N D U E INDUS PUBLISHING COMPANY NEW DELHI Preface The Himalaya are the most prominent feature on the face of the earth. They extend in an arcuate shape from the Indus gap in the north west to the Brahmaputra gap in the east. Jammu & Kashmir, Himachal Pradesh. Garhwal, Kumaun, Nepal, Darjeeling hills, Sikkim, Bhutan and most of Arunachal Pradesh lie in the Himalaya. Natural vegetation of this mountain chain is varied, both in compo sition and distribution. The principal forest types found in this mountain chain range from the wet evergreen forests in the eastern Himalayan foothills to the tropical dry forests ofJammu, the alpine meadows near the snowline and the open, stunted forests of the cold deserts. These forests and their adjoining tracts are the home of a large number of animals including tiger, leopard, snow leopard, clouded leopard, ele phant, rhinoceros, gaur, yak, Tibetan wild ass, sambhar, cheetal, musk deer, hog deer, barking deer, wild boar, brown and black bears, pheas ants, vultures, eagles, tits, warblers, snakes, crocodiles and jackals. This book discusses in briefthe mammals, birds, reptiles, fishes and amphibians found in different parts of the Hinrialaya. Importantnational parks,sanctuariesandbiosphere reservesset-uptoconserveandmanage the unique flora and fauna of this mountain chain havealso beendealt with in this book. It is hoped that this book will serve as a handy reference work on these topics for the foresters, wildlifers, naturalists, environmentalists and even the layman interested in knowing about the Himalayan wildlife and its management I am grateful to ShriA.K.
    [Show full text]
  • Mining Plan and Progressive Mine Closure Plan for Boulder, Graval & Sand Mine (Minor Mineral)
    MINING PLAN AND PROGRESSIVE MINE CLOSURE PLAN FOR BOULDER, GRAVAL & SAND MINE (MINOR MINERAL) DEVDHAR BLOCK (YNR B-24) Lease area : 31.87 ha, Lease Period- 8 years; Production –0.573 Million T/Annum) SUBMITTED TO THE DIRECTOR GENERAL, MINES & GEOLOGY HARYANA APPLICANT PREPARED BY M/s Northern Royalty Co., S.N. SHARMA 603-604, Santpura Road, RQP/DDN/0135/2001-A Model Town, yamunanagar House No. 282, sector 11-D, Faridabad (Haryana) Sector-23, Rohini, Delhi CONTENTS S.NO DESCRIPTION PAGE NO Introduction 1-4 1.0 General 5 2.0 Details of the Mining lease area 6 3.0 Details of Existing Mining pits, their dimensions etc 8 3.1 Physiography, Drainage and Climate 10-15 3.2 Geology of the Area 15 3.2.1 Regional Geology 16 3.2.2 Local Geology 16 3.2.3 Description of formation 17 3.2.4 Boulder,Graval & Sand 17-19 3.2.5 Physical & Chemical Characteristics of mineral 20 3.2.6 Original & control of mineralisation ( Annual replenishment of 21-26 mineral in river bed area vis-a-vis-sedimentation 3.2.7 Grade and use of Boulder,Graval & Sand 26 3.3 Reserves 27 3.3.1 Method of estimation of reserves 27-30 4.0 Details of production & dispatches of five years 30 5.0 Physical and Geological Characters of the deposit 32 6.0 Details of Mining Machinery Deployed/ to be deployed 32 6.1 Fuel consumption Per Day 32 7.0 Method of mining 33 7.1 Proposed year wise development for five years 33 7.2 Proposed rate of production when the mine is fully developed 34 7.3 Mineable reserves and anticipated life of the mine 34 7.4 Proposed method of mining 34-40 7.5 Conceptual Mining Plan 40-42 7.7 Mine Drainage 43 7.8 Water requirement 43 7.9 Site services 44 8.0 Year wise Annual Program me of mining for the next 5 years 46 9.0 Details of Employment 47 Environment Management Plan 48-60 10.0 MEASURES TAKEN AND TO BE TAKEN FOR LAND RESTORATION, 48-50 RECLAMATION AND PLANTATION IN/ OR NEARBY LEASE AREA 11.0 Measures taken/ to be taken for protection of Environment in 51 and around mining areal 12.0 Measures taken/ to be taken for dumping overburden, stacking of 52 top soil.
    [Show full text]
  • Jal Vikas January 2018
    An Overview of NWDA Presence in India Water Week-2017 An Overview of NWDA Involvement in Trade Fair-2017 2 From Director General’s Desk It gives me immense pleasure to present the Annual Jal Vikas-2018 issue of NWDA. The in-house bulletin of NWDA gives an overview of the main functions and objectives of NWDA in the field of Water Resources Planning and Development, particularly with respect to Inter Basin Water Transfer (IBWT) as well as Intra-State Water Transfer Projects commonly known as the Programme on Interlinking of Rivers (ILR), Government of India, under the Ministry of Water Resources, River Development and Ganga Rejuvenation (MoWR,RD&GR). It is pertinent to mention that the NWDA, with the support and guidance of Hon’ble Minister (WR, RD & GR) and Secretary (WR, RD &GR), has accomplished all its assigned functions in an efficient and effective manner during the year 2017, in spite of many hurdles and constraints especially relating to the shortage of Technical Officers. The main works dealt and completed by NWDA during the period of 1st January, 2017 to 31st December, 2017 and that indicated in the annual issue are related with the Techno-Economic Clearance and Water Sharing Issues of Ken-Betwa (Phase-I/II), Par- Tapi-Narmada and Damanganga-Pinjal Link Projects along with their Clearances from Wild Life, Environment, Forest Land Diversion, Ministry of Tribal Affairs (MoTA), Investment, Funding Pattern and Implementation Mechanism Departments. All the Clearances could be obtained mainly because of the concerted efforts taken by NWDA. In addition to these activities, NWDA also organized India Water Week-2017- the fifth event in the series during 10-14 October, 2017 by concurrently conducting the International Conference and Water Expo-2017; 3rd and 4th Jal Manthan respectively on 13.01.2017 and 27-28.07.2017; 64th Meeting of the Governing Body of NWDA on 27.03.2017; and 31st Annual General Meeting of NWDA on 12.09.2017.
    [Show full text]
  • The Saraswatī and the Lost River of the Indian Desert
    Journal of the Royal Asiatic Society http://journals.cambridge.org/JRA Additional services for Journal of the Royal Asiatic Society: Email alerts: Click here Subscriptions: Click here Commercial reprints: Click here Terms of use : Click here Art. III.—The Saraswatī and the Lost River of the Indian Desert C. F. Oldham Journal of the Royal Asiatic Society / Volume 25 / Issue 01 / January 1893, pp 49 - 76 DOI: 10.1017/S0035869X00022176, Published online: 15 March 2011 Link to this article: http://journals.cambridge.org/abstract_S0035869X00022176 How to cite this article: C. F. Oldham (1893). Art. III.—The Saraswatī and the Lost River of the Indian Desert. Journal of the Royal Asiatic Society, 25, pp 49-76 doi:10.1017/S0035869X00022176 Request Permissions : Click here Downloaded from http://journals.cambridge.org/JRA, IP address: 139.184.14.159 on 26 Mar 2015 49 ART. III.—The Saraswatl and the Lost River of the Indian Desert. By Surgeon-Major 0. F. OLDHAM. As is well known, the description of the Saraswatl river, given in the Veda, differs much from that met with in the Hahabharata and other ancient but later authorities, while neither agrees with the present condition of that sacred stream. In the Rig Yeda we are told of a large and rapid river flowing from the mountains to the sea. The Mahabharata describes the same stream as losing itself in the sands. At the present day we find a river, wide and rapid during floods, but containing little water at other times, joining another stream of similar character, and thereupon losing its name; the river below the confluence being now called Gaggar.
    [Show full text]
  • Social Studies Date: 15/04/2020
    ZEE HIGH SCHOOL HAYATHNAGAR CLASS : IV SUB: SOCIAL STUDIES DATE: 15/04/2020 TOPIC: PHYSICAL DIVISIONS OF INDIA WORKSHEET-3 __________________________________________________________________ Hi children, earlier in two worksheets you came to know about our India, its states, Union Territories and its capitals. And even you have learnt about our Indian culture and heritage. Now let us know about the Physical divisions of India. India is a land with beautiful landforms such as snow-covered mountains, valleys, rivers, hills, plateaus, plains, deserts, coastal plains and islands. The important physical features of India are: 1 1. The Northern mountains 2. The Northern Plains 3. The Great Indian Desert or the Thar Desert. 4. The Southern Plateau or Deccan plateau 5. The Eastern and Western Coastal Plains 6. The Islands 1 The Northern Mountains: The Northern Mountains stretch across the boundary of India. They consist of the Himalayas and the Karakoram ranges. The Himalayas stretch from Jammu and Kashmir in the North to Arunachal Pradesh in the east. They are the highest mountain ranges in the world. The Indian states that are part of Himalayan region are- Himachal Pradesh, Jammu and Kashmir [Unionteritory] Uttarakhand, Sikkim, Arunachal Pradesh, and parts of Nagaland, Manipur, Mizoram, Tripura, Meghalaya, The Himalayas: The word Himalayas means abode of snow, as a large part of these mountains is covered with snow throughout the year. The Himalayas are divided in to three parallel rows of mountains or hills called ranges. HIMALAYAS ___________________________________________________________________ ↓ ↓ ↓ The Greater Himalayas The Middle Himalayas The lower Himalayas OR OR OR (Himadri) (Himachal) (Shiwalik) 2 1. The Greater Himalayas: It is the highest of the three Himalayan ranges.
    [Show full text]
  • Contact December 2016.Cdr
    catio Edu n . R e g 1966 - 2016 s e in a n i r Hkkjrh; lqnwj laosnu laLFkku c a r h T Indian Institute of Remote Sensing Indian Institute of Remote Sensing 5Golden Jubilee iirs dkWUVSDV Contact vad 18 la[;k 2@ Volume 18 No. 2 fnlEcj 2016@December 2016 ...on a mission for transferring technology through education, research and capacity building CONTENTS TECHNICAL COMMUNICATIONS Ÿ Numerical Simulation and Modeling of Debris flow at Tangni (Pagal Nala), Joshimath, 2 EDITORIAL Uttarakhand using Earth Observation Data Ÿ Landslide characterization using Remote Sensing and advanced Geophysical techniques at 2 An efficient and effective disaster management Kunjethi village, Kalimath, Garhwal Himalaya requires infusion of space technology, which is Ÿ Avalanche Hazard Site Mapping for Alaknanda Basin 3 Ÿ Aerosol distribution over Uttarakhand during intense forest fire episode in April-May 2016 4 developing at a rapid pace due to both technological Ÿ Flood Early Warning System for North West Himalayan region using geospatial inputs and 5 advancements and greater demand caused by modelling approach emerging business opportunities and security Ÿ Flood plain delineation using Height above Nearest Drainage 6 Ÿ Ionospheric TEC modelling for earthquake precursor studies in Himalaya 8 concerns. The global community has experienced the Ÿ Analysis of Crustal deformation and seismic assessment using ground-based GNSS 9 benefit of space technology in disaster management observation data in North Western Himalaya support through various national, regional and global Ÿ Space-borne Differential Interferometric SAR Observation of Nepal Earthquake (2015) 10 Ÿ Liquefaction Hazard Assessment In and Around Lucknow Due to 2015 Nepal Earthquake 11 efforts including International Charter for Space and Ÿ A Comparison of VIIRS and MODIS Active Fire Products for Uttarakhand Episodic Forest 12 Major Disasters.
    [Show full text]
  • West Bengal Action Plan on Climate Change 1
    WEST BENGAL ACTION PLAN ON CLIMATE CHANGE 1 West Bengal State Action Plan on Climate Change April, 2012 WEST BENGAL ACTION PLAN ON CLIMATE CHANGE 2 Table of Contents Message Preface Executive Summary..........................................................................................................................................12 Chapter 1 – Intoduction ..................................................................................................................................................38 Chapter 2 - Process of Preparation ............................................................................................................................40 Chapter 3- West Bengal State Profile........................................................................................................................43 Physiography Climate Demography Water resources Biodiversity and Forests Economy Chapter 4 - Observed Climate and Climate Projections ....................................................................................47 Observed Climate, Extreme events and Sea Level Rise Projections of Climate, Extreme events and Sea level Rise Chapter 5 – Water Resources ........................................................................................................................................52 Introduction Water Availability and Demand Existing Water Related Concerns in West Bengal Institutions Involved in Water Sector Service Delivery Current Policies, Programmes and Projects of the Government Impacts of Climate Change
    [Show full text]
  • Pollution Aspects
    National Mission for Clean Ganga Ministry of Jal Shakti Department of Water Resources, River Development Public Disclosure Authorized & Ganga Rejuvenation, Government of India Public Disclosure Authorized Environmental and Social Management Framework (ESMF) Public Disclosure Authorized Annex-I - Environmental and Social Baseline Public Disclosure Authorized Prepared by The Energy and Resources Institute (January 2011) Updated by Lea Associates South Asia Pvt. Ltd (16 March 2020) CONTENTS 1. NATIONAL GANGA RIVER BASIN PROJECT ..................................................................... 1 1.1. INTRODUCTION ................................................................................................................................... 1 1.2. Ganga River Basin Management: Initiatives ....................................................................................... 1 1.3. NMCG: An Evolutionary Journey ......................................................................................................... 2 1.3.1. National Ganga River Basin Authority (NGRBA) ................................................................... 2 1.3.2. National Mission for Clean Ganga (NMCG) .......................................................................... 2 1.4. NMCG Projects .................................................................................................................................... 3 1.4.1. Short-term Action Plan ........................................................................................................
    [Show full text]
  • Edible Mushrooms of the Northwestern Himalaya, India: a Study of Indigenous Knowledge, Distribution and Diversity
    Mycosphere 5(3): 440–461 (2014) ISSN 2077 7019 www.mycosphere.org Article Mycosphere Copyright © 2014 Online Edition Doi 10.5943/mycosphere/5/3/7 Edible mushrooms of the Northwestern Himalaya, India: a study of indigenous knowledge, distribution and diversity Semwal KC1, Stephenson SL2, Bhatt VK3, Bhatt RP4 1 College of Natural and Computational Sciences, Department of Biology, Mekelle University, 3033, Mekelle, Tigray, Ethiopia (East Africa) 2 Department of Biological Sciences, University of Arkansas, Fayetteville, Arkansas, 7270, USA 3Navdanya, 105, Rajpur Road, Dehradun, Uttarakhand, India 4Department of Botany, Hemwati Nandan Bahuguna Garhwal Central Universtiy, Sringagar, Garhwal, Uttarakhand, India Semwal KC, Stephenson SL, Bhatt VK, Bhatt RP 2014 – Edible mushrooms of the Northwestern Himalaya, India: a study of indigenous knowledge, distribution and diversity. Mycosphere 5(3), 440-461, Doi 10.5943/mycosphere/5/3/7 Abstract In the present study, the diversity, edibility, indigenous knowledge and distribution of wild edible mushrooms in the Northwestern Himalaya are discussed. The information provided herein was derived from a study carried out in the states of Uttarakhand and Himachal Pradesh during the period of 2000-2013. A total of 23 species of mushrooms considered as edible or used for trade were recorded. Twenty-one of these are basidiomycetes and two are ascomycetes. Certain species of Amanita, Agaricus, Astraeus, Hericium, Macrolepiota, Morchella, Pleurotus and Termitomyces are very commonly collected and consumed by the local people, whereas species of Auricularia, Cantharellus, Sparassis, Lactarius, Ramaria and Russula are less commonly collected and consumed. Cordyceps sinensis and several species of Morchella are collected specifically for trade purposes in the spring season in high elevation areas of the Himalaya.
    [Show full text]