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(A). Mention Important Features of the Indian Monsoon. Ans. 1
ACADEMIC YEAR 2020-21 REVISION WORK CLASS - X GEOGRAPHY Question 1. (a). Mention important features of the Indian Monsoon. Ans. 1. Seasonal 2. Erratic and Unpredictable 3. Unevenly distributed. 4. Mainly orographic in nature. 5. It affects the economy.Some of the rain occurs due to tropical depressions. (b). What are the causes of Winter rain? Ans. 1. In Tamil Nadu, the north-east monsoon winds pick up moisture from the Bay of Bengal and bring rain. 2. The cause of the rain in all the northern states are the Western disturbances that originate in the Mediterranean Sea. (c). State the benefits that are derived from the local winds that blow in summer in the following states - i. Kerala ii. West Bengal Ans. i. Kerala - Mango showers are good for tea, coffee and mangoes. ii. West Bengal - Kalbaisakhi is good for rice, jute & tea. (d). Name two types of cyclonic systems that affect India and two areas that receive rainfall from these systems. Ans. (i) Western Disturbances : During winter there is an inflow of low pressure depressions called Western Disturbances in North West India. These originate in the Mediterannean Sea and enter India after crossing Iraq, Afghanistan and Pakistan. They intensify over North West India and move eastward causing rain in Punjab, Haryana and Western Uttar Pradesh. (ii). Tropical Cyclones : During the summer, the whole east coast of India comes under the influence of tropical depressions that are low pressure systems originating at the head of Bay of Bengal. Give reasons for the following: (e). Chennai has a lower annual range of temperature than Lucknow. -
Center 1 Ectonic Evolution of the Cocos-Nazca Spreading
,, s11bs1i11ae the.se pages for pages J.10../-/../(}(¡ 111 tÍle Ocwber 1977 Bulletin. 1•. 88. 110. JO. Giorgio DE LA TORRE Mora1e~ Teniente de Fragata-SU 1 ectonic evolution of the Cocos-Nazca spreading center RICHARD HEY ''· Department of Geolog1cal and Geophysical Sciences, Prmceton Unwersity, Prmceto11, New }asey 08 5-1 11 ABSTRACT zone of compression suggesr~(ferron and Heirrzler ( 1967) an( Raff (1968) is ºAAfecSbl quirement rhat rwo or pos_sibh Magnetic and bathymetric data from the easrern Pacific have three of rhe rirn'~u s r sprea o liquely, because "ar triple 1unc been analyzed and a model for the evolution of the Galapagos re tions, slafloor spreading cannot be perpendicular to al i rhree of th1 gion developed. The Farallon piare appears to have broken apart rifts" ( to~~:o . ;ipd Dietz, 1972, p. 267). Jn' fact. spreading may b, along a pre-existing Pacific-Farallon fracture zone, possibly the perpen ifulaF· tb-'a~l ·~ r!fts wirhour resulting zones of compres- Marquesas fracture zone, ar about 25 m.y. B.P. to fonn the Cocos sion an · ho.uwcio!a~ 0Í-ffte-rig;d-plate hypothesis. and Nazca plates. This break is marked on the Nazca piare topo Van Andel and others (197 1) proposed rhar the aseismic Coco~ graphically by the Grij alva scarp and magnetically by a rough and Carnegie Ridges were formed by rifring apart of a pre-exisrint smooth boundary coincident with the scarp. The oldest Cocos ancestral ridge. This hypothesis has since undergone severa! mod Nazca magnetic anomalies parallel this boundary, implying that ificarions (Malfair and Dinkelman, 1972; Heath and van Andel. -
Current Affairs Magazine May
2 INDEX 1.GEOGRAPHY………………………………4 9.3 Tax Revenue - Record GST Collections ...... 29 1.1 Cyclone Fani - An Unusual Storm ............... 4 9.4 SEBI's Order on NSE ................................... 30 2.POLITY……………………………………6 9.5 New Income Tax Rule for Senior Citizens . 31 2.1 L-G Role in Puducherry Administration ..... 6 9.6 RBI Draft Rules for NBFCs ......................... 32 2.2 Concerns over Judicial Appointments ......... 7 9.7 Tariff Issues in Indo-US Trade ................... 33 2.3 SC Order on Karnataka Reservation .......... 8 9.8 Assessing India's Trade Policy ................... 34 2.4 Recording Dissenting Opinion in EC ........... 9 9.9 Crisis in WTO's Appellate Body.................. 36 3.GOVERNMENT ACTS & POLICIES.10 9.10 Boosting Private Investments .................... 37 3.1 Issues with Universal Debt Relief 10.AGRICULTURE……………………….39 Programme .............................................................. 11 10.1 PepsiCo and Potato Farmers Case ............. 39 4.SOCIAL JUSTICE……………………….12 11.SCIENCE & TECHNOLOGY……….40 4.1 Women Workforce Participation ................ 12 11.1 Blockchains for Internet of Things ............. 40 5.HEALTH…………………………………..13 11.2 RISAT-2B Launch ........................................ 42 5.1 Report on Economic Impacts of 12.ENVIRONMENT…………………….43 Antimicrobial Resistance ........................................ 13 12.1 IPBES Report ............................................... 43 5.2 Under-Five Mortality and Low Birth Weight - Lancet Global Health ............................................ 14 12.2 Global Concentration of Atmospheric CO246 12.3 CEA’s Plan on Renewable Energy .............. 47 6.INDIA & ITS NEIGHBORHOOD…..16 6.1 Masood Azhar as Global Terrorist ............. 16 12.4 India and Arctic Council ............................. 48 6.2 Indian Ocean Region - China's Strategy and 13.DISASTER MANAGEMENT………..49 India's Response ...................................................... 17 13.1 Lessons from Fani Cyclone ........................ -
INP-10 (Catalogue of Indian Charts, Encs & Publications)
INP - 10 ROGR D A Y P H H I L C A O N F O F I I C T A E N INDIAN I N DIA Nautical Publications CATALOGUE OF INDIAN PAPER CHARTS ELECTRONIC NAVIGATIONAL CHARTS AND PUBLICATIONS Published by National Hydrographic Office, Dehradun Edition - 2021 INP 10 ROGR D A Y P H H I L C A O N F O F I I C T A E N I N DIA CATALOGUE OF PAPER CHARTS, ELECTRONICS NAVIGATIONAL CHARTS AND PUBLICATIONS NATIONAL HYDROGRAPHIC OFFICE DEHRADUN INDIA Jan 2021 CONTENTS INDEX PAGE Indian Ocean (Small Scale Charts) 1-2 Pakistan and West Coast of India (Sir Creek to Diu Head) 3-4 West Coast of India (Diu Head to Betul) 5-6 West Coast of India (Betul to Quilon and Lakshadweep) 7-8 South Coast of India and Sri Lanka 9-10 East Coast of India 11-12 Andaman and Nicobar Islands 13-14 Maldives, Mauritius and Seychelles Groups 15-16 Kenya, Tanzania and Mozambique 17-18 Myanmar, Thailand, Malaysia and Malacca Strait 19-20 Folios of IN Charts & Prices of Indian Hydrographic Charts and 21-22 Publications INDIAN OCEAN (SMALL SCALE CHARTS) Chart No. INT No. Chart Title Scale 1: Date of ENC Publication/ Released New Edition 21 Muscat to Mumbai 1 500000 1 5-A pr-201 8 Yes 22 752 Mumbai to Cape Comorin 1 500000 3 1 - J u l - 2 0 1 9 Yes 31 756 Bay of Bengal - Northern Portion (Krishnapatnam 1 500000 1 5-A pr-201 7 No to Bassein River) 32 754 Kochi (Cochin) to Visakhapatnam 1 500000 3 1 - J u l - 2 0 1 9 Yes 33 755 Bay of Bengal - Southern Portion 1 500000 31 -M ay-201 6 Yes 41 757 Andaman Sea 1 500000 1 5-D ec-201 0 Yes 7070 70 Indian Ocean Southern Part 10000000 1 5-M ar-201 9 No -
The Madras Presidency, with Mysore, Coorg and the Associated States
: TheMADRAS PRESIDENG 'ff^^^^I^t p WithMysore, CooRGAND the Associated States byB. THURSTON -...—.— .^ — finr i Tin- PROVINCIAL GEOGRAPHIES Of IN QJofttell HttinerHitg Blibracg CHARLES WILLIAM WASON COLLECTION CHINA AND THE CHINESE THE GIFT OF CHARLES WILLIAM WASON CLASS OF 1876 1918 Digitized by Microsoft® Cornell University Library DS 485.M27T54 The Madras presidencypresidenc; with MysorMysore, Coor iliiiiliiiiiiilii 3 1924 021 471 002 Digitized by Microsoft® This book was digitized by Microsoft Corporation in cooperation witli Cornell University Libraries, 2007. You may use and print this copy in limited quantity for your personal purposes, but may not distribute or provide access to it (or modified or partial versions of it) for revenue-generating or other commercial purposes. Digitized by Microsoft® Provincial Geographies of India General Editor Sir T. H. HOLLAND, K.C.LE., D.Sc, F.R.S. THE MADRAS PRESIDENCY WITH MYSORE, COORG AND THE ASSOCIATED STATES Digitized by Microsoft® CAMBRIDGE UNIVERSITY PRESS HonBnn: FETTER LANE, E.G. C. F. CLAY, Man^gek (EBiniurBi) : loo, PRINCES STREET Berlin: A. ASHER AND CO. Ji-tipjifl: F. A. BROCKHAUS i^cto Sotfe: G. P. PUTNAM'S SONS iBomlaj sriB Calcutta: MACMILLAN AND CO., Ltd. All rights reserved Digitized by Microsoft® THE MADRAS PRESIDENCY WITH MYSORE, COORG AND THE ASSOCIATED STATES BY EDGAR THURSTON, CLE. SOMETIME SUPERINTENDENT OF THE MADRAS GOVERNMENT MUSEUM Cambridge : at the University Press 1913 Digitized by Microsoft® ffiambttige: PRINTED BY JOHN CLAY, M.A. AT THE UNIVERSITY PRESS. Digitized by Microsoft® EDITOR'S PREFACE "HE casual visitor to India, who limits his observations I of the country to the all-too-short cool season, is so impressed by the contrast between Indian life and that with which he has been previously acquainted that he seldom realises the great local diversity of language and ethnology. -
Himalaya - Southern-Tibet: the Typical Continent-Continent Collision Orogen
237 Himalaya - Southern-Tibet: the typical continent-continent collision orogen When an oceanic plate is subducted beneath a continental lithosphere, an Andean mountain range develops on the edge of the continent. If the subducting plate also contains some continental lithosphere, plate convergence eventually brings both continents into juxtaposition. While the oceanic lithosphere is relatively dense and sinks into the asthenosphere, the greater sialic content of the continental lithosphere ascribes positive buoyancy in the asthenosphere, which hinders the continental lithosphere to be subducted any great distance. Consequently, a continental lithosphere arriving at a trench will confront the overriding continent. Rapid relative convergence is halted and crustal shortening forms a collision mountain range. The plane marking the locus of collision is a suture, which usually preserves slivers of the oceanic lithosphere that formerly separated the continents, known as ophiolites. The collision between the Indian subcontinent and what is now Tibet began in the Eocene. It involved and still involves north-south convergence throughout southern Tibet and the Himalayas. This youthful mountain area is the type example for studies of continental collision processes. The Himalayas Location The Himalayas form a nearly 3000 km long, 250-350 km wide range between India to the south and the huge Tibetan plateau, with a mean elevation of 5000 m, to the north. The Himalayan mountain belt has a relatively simple, arcuate, and cylindrical geometry over most of its length and terminates at both ends in nearly transverse syntaxes, i.e. areas where orogenic structures turn sharply about a vertical axis. Both syntaxes are named after the main peaks that tower above them, the Namche Barwa (7756 m) to the east and the Nanga Parbat (8138 m) to the west, in Pakistan. -
Andaman Islands, India
Journal of Global Change Data & Discovery. 2019, 3(4): 398-405 © 2019 GCdataPR DOI:10.3974/geodp.2019.04.15 Global Change Research Data Publishing & Repository www.geodoi.ac.cn Global Change Data Encyclopedia Andaman Islands, India Shen, Y.1 Liu, C.1* Shi, R. X.1 Chen, L. J.2 1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. National Geomatics Center of China, Beijing 100830, China Keywords: Andaman Islands; Andaman and Nicobar Islands; Bay of Bengal; Indian Ocean; India; data encyclopedia Andaman Islands is the main part of the An- daman and Nicobar Islands. It belongs to the Indian Union Territory of Andaman and Nicobar Islands, and its geo-location is 10°30′39″N–13°40′36″N, 92°11′55″E–94°16′ 38″E[1]. It is located between the Bay of Bengal and the Andaman Sea (Figure 1). It is separated from Coco Islands[2] by Coco Chanel at its north, and from Nicobar Islands[3] by Ten De- gree Chanel at its south. The Andaman Islands consists of Great Andaman Archipelago[4], Lit- tle Andaman Group[5], Ritchie’s Archipelago[6], [7] [8] East Volcano Islands and Sentinel Islands Figure 1 Map of Andaman Islands (Figure 2), with a total of 211 islands (islets, [1] (.kmz format) rocks) . The total area of the Andaman Islands is 5,787.79 km2, and the coastline is 2,878.77 km. Great Andaman Archipelago is the main part of Andaman Islands, and is the largest Ar- chipelago in Andaman Islands. -
Shankar Ias Academy Test 8 – Geography - Ii - Answer Key
SHANKAR IAS ACADEMY TEST 8 – GEOGRAPHY - II - ANSWER KEY 1. Ans (c) Explanation: http://www.iasparliament.com/article/prelim-bits-18-07-2017?q=national%20park 2. Ans (d) Explanation: Sl. No. Integrated check post State Border 1. Petrapole West Bengal India-B’desh 2. Moreh Manipur India-Myanmar 3. Raxaul Bihar India-Nepal 4. Attari (Wagah) Punjab India-Pakistan 5. Dawki Meghalaya India-B’desh 6. Akhaura Tripura India-B’desh 7. Jogbani Bihar India-Nepal 8. Hili West Bengal India-B’desh 9. Chandrabangha West Bengal India-B’desh 10. Sutarkhandi Assam India-B’desh 11. Kawarpuchiah Mizoram India-B’desh 12. Sunauli Uttar Pradesh India-Nepal 13. Rupaidiha Uttar Pradesh India-Nepal 3. Ans (b) Explanation: Devprayag: where river Alaknanda meet river Bhagirathi Rudraprayag: where river Alaknanda meet river Mandakini Karnaprayag: where river Alaknanda meet river Pinder Nandprayag: where river Alaknanda meet river Nandakini Vishnuprayag: where river Alaknanda meet river Dhauli Ganga 4. Ans (c) Explanation: The Haryana government launched Asia's First 'Gyps Vulture Reintroduction Programme' at Jatayu Conservation Breeding Centre, Pinjore. SHANKAR IAS ACADEMY The Centre has become prominent vulture breeding and conservation centre in the country-after successfully breeding Himalayan Griffon Vultures-an old world vulture in the family of Accipitridae-in captivity. The government had released two Himalayan Griffon Vultures The Himalayan Griffon is closely related to the critically endangered resident Gyps species of vultures but is not endangered. Two Himalayan Griffons have been in captivity for over a decade and have been in the aviary with resident Gyps vultures. These birds were wing-tagged and were leg-ringed for identification. -
Geography Model Test Questions 2 in English with Answers 1
Indian Geography Prepared By www.winmeen.com Geography Model Test Questions 2 in English With Answers 1. Match list I correctly with list II and select your answer using the codes given below: List I List II a) Punjab 1) Jute b) Maharashtra 2) Paddy c) West Bengal 3) Tobacco d) Andhra Pradesh 4) Sugarcane e) Tamil Nadu 5)Wheat Codes: a b c d e (A) 3 1 2 4 5 (B) 5 4 1 3 2 (C) 4 5 3 2 1 (D) 2 3 4 1 5 2. Consider the statements: I. India is a monsoon oriented country. II. South – West monsoon generally brings more rain to India III. North – east monsoon rains are mainly confined to eastern and southern India IV. Monsoon is always a gamble in India Of the statements: (A) I alone is correct (B) I and II are correct (C) I, II and III are correct (D) All the statements are correct 3. The following part of India is closet to equator? (A) Minicoy island (B) Nicobar island (C) Cape comorin (D) Lakshadweep 4. The total area from which all surface run-off is drained by a river is called its (A) water shed (B) flood plain (C) catchment area (D) interfluvial area 5. The longest coastal line is situated in one of the which Indian states? Learning Leads To Ruling Page 1 of 13 Indian Geography Prepared By www.winmeen.com (A) Tamil Nadu (B) Kerala (C) Andhra Pradesh (D) West Bengal 6. Dandakaranya forest is located in (A) Southern India (B) North – Eastern India (C) Central India (D) Western India 7. -
Holocene Erosion of the Lesser Himalaya Triggered by Intensified
Holocene erosion of the Lesser Himalaya triggered by intensifi ed summer monsoon Peter D. Clift School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK Liviu Giosan Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Jerzy Blusztajn Ian H. Campbell Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia Charlotte Allen Malcolm Pringle Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Ali R. Tabrez Mohammed Danish National Institute for Oceanography, Clifton, Karachi 75600, Pakistan M.M. Rabbani Anwar Alizai Geological Survey of Pakistan, Block 2, Gulistan e Jauhar, Karachi, Pakistan Andrew Carter School of Earth Sciences, University and Birkbeck College London, Gower Street, London WC1E 6BT, UK Andreas Lückge Bundesanstalt für Geowissenschaften und Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany ABSTRACT We study the erosional response of the Indus drainage basin, encom- Climate is one of the principal controls setting rates of conti- passing a number of ranges located in the western Himalaya (Fig. 1). The nental erosion. Here we present the results of a provenance analysis vast majority of the sediment eroded in this region is delivered to the delta of Holocene sediments from the Indus delta in order to assess climatic via the Indus River and its tributaries. Consequently changes in the prov- controls on erosion over millennial time scales. Bulk sediment Nd iso- enance of sediment reaching the delta can be used to understand how cli- tope analysis reveals a number of changes during the late Pleistocene mate change since the last deglaciation has infl uenced Himalayan erosion. -
Prelim Bits 01-05-2019
Prelim Bits 01-05-2019 BCIM Economic Corridor The Bangladesh China India Myanmar (BCIM) economic corridor aims to connect Kolkata with Kunming, capital of the Yunnan province of China. It envisages the formation of a thriving economic belt, focusing on cross- border transport, energy and telecommunication networks. India will benefit in terms of the development of the Kolkata port and the opening up of the economic potential of the northeast states. Earlier BCIM was part of China’s BRI initiative, recently the project has been delisted from the BRI umbrella. Projects under Belt and Road Initiative of China Belt and Road Initiative (BRI) is a giant connectivity initiative speared by China to revive the ancient Silk Road across Eurasia and Africa. Under the project South Asia is covered by three major undertakings 1. China-Myanmar Economic Corridor (CMEC). 2. Nepal-China Trans-Himalayan Multi-dimensional Connectivity Network, including Nepal-China cross-border railway. 3. China Pakistan Economic Corridor (CPEC) – India opposes this project as it passes through Pakistan occupied Kashmir. Other projects in which India is a member IMT trilateral Highway - India-Myanmar-Thailand Trilateral Highway will join India’s Northeast with Thailand and other ASEAN members through Myanmar. Kaladan Multimodal Project - The Kaladan Multimodal Transit Transport Project will help connect the Northeast with Myanmar as well as with West Bengal. BBIN - Bangladesh, Bhutan, India, and Nepal (BBIN) needs to be accorded the highest priority as it has great potential to deliver rich dividends quickly. Global Food Policy Report International Food Policy Research Institute (IFPRI) releases Global Food Policy Report annually. -
Quaternary River Erosion, Provenance, and Climate Variability
Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School 2017 Quaternary River Erosion, Provenance, and Climate Variability in the NW Himalaya and Vietnam Tara Nicole Jonell Louisiana State University and Agricultural and Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Earth Sciences Commons Recommended Citation Jonell, Tara Nicole, "Quaternary River Erosion, Provenance, and Climate Variability in the NW Himalaya and Vietnam" (2017). LSU Doctoral Dissertations. 4423. https://digitalcommons.lsu.edu/gradschool_dissertations/4423 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. QUATERNARY RIVER EROSION, PROVENANCE, AND CLIMATE VARIABILITY IN THE NW HIMALAYA AND VIETNAM A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geology and Geophysics by Tara Nicole Jonell B.S., Kent State University 2010 M.S., New Mexico State University, 2012 May 2017 ACKNOWLEDGMENTS There are so many people for which I am thankful. Words can barely express the gratitude I have for my advisor, Dr. Peter D. Clift, who has countlessly provided humor and outstanding support throughout this project. I cannot imagine completing this research without his untiring guidance both in the lab and outside in the field. I also wish to thank my advisory committee for their invaluable insight and patience: Dr.