NATIONAL GEOPHYSICAL RESEARCH INSTITUTE, HYDERABAD, INDIA. Induction Workshop: (18-23 October, 2004)
|
|
|
- Cameron Bailey
- 5 years ago
- Views:
Transcription
1 NATIONAL GEOPHYSICAL RESEARCH INSTITUTE, HYDERABAD, INDIA. Induction Workshop: (18-23 October, 2004) Venue for 17th workshop (18th to 23rd OCTOBER2004) NATIONAL GEOPHYSICAL RESEARCH INSTITUTE, HYDERABAD, INDIA.
2 Welcome to India! 5000 Years of civilisation Assimilation of technology Economic travel and living costs Improved communications to global centres India is well-connected by the global network of airlines. Mumbai and New Delhi are major international gateways. Hyderabad is connected to most cities in India and Singapore, Malayasia and Middle East. Mumbai - The Gateway to India : A major metropolis on the West Coast and financial capital of the country having a year-round mild climate, with temperatures 30ºc. Hyderabad years of heritage : A city situated on the Deccan Plateau at 500m elevation, with dry climate and mean temperatures around 25ºc, reinventing itself as one of the IT centres of the country
3 International bodies: The Workshop is supported by: International Union of Geodesy and Geophysics International Assembly of Geomagnetism and Aeronomy Working Group 1.2 National Science Foundation, U.S.A National Agencies: Indian National Science Academy Department of Science & Technology National Geophysical Research Institute Indian Institute of Geomagnetism Council of Scientific & Industrial Research Department of Ocean Development Oil Industry Development Board Oil & Natural Gas Commission Limited Directorate General of Hydrocarbons Oil India Limited THEME Induction Workshop: (18-23 October, 2004) The International Workshop on Electromagnetic (EM) Induction in the Earth is the premier venue for EM researchers around the world to exchange research results and new developments. EM measurements provide a unique view of the Earth because of the range of variations in electrical conductivity encountered in the Earth's sub-surface. Scientific sessions will primary focus on
4 1. Local and regional studies 2. 3D modelling and inversion from theory to application 3. Environmental studies 4. Application to Oil industry, geothermal activity and resources 5. Ocean studies 6. Anisotropy versus heterogeneity from lab to in-situ 7. The electrical lithosphere and asthenosphere 8. Seismic and volcanic imaging studies 9. Electromagnetic contribution to multi technique geophysical studies 10. EM studies of fossil and active continent-continent collision zones (1/2 day - end of the workshop just prior to the tacked-on Himalaya-Tibet workshop) 11. Deep EM studies of the continental lithosphere (for diamond industry interest) 12. Estimation of the response function, including removal of distortion using tensor decomposition. 13. Open session Venue:: National Geophysical Research Institute (An ISO 9001 Organisation) Hyderabad, India's principal Institution for R&D in earth science. Pre-Workshop (13-16 October 2004) MT Data Interpretation Workshop (MTDIW) will be tailor made for developing Human resource for EM research and investigations in developing countries. This would be in liaison with Interdivision Commission for Developing Countries - ICDC (IAGA). The MTDIW shall specially focus on the recent advances in data processing analysis, numerical modelling and interpretation of the results in the light of collateral data. Venue: Indian Institute of Geomagnetism, Navi Mumbai. A premier Institution for Geomagnetism, since Post-Workshop (24-25 October 2004) Multi-disciplinary studies of the Himalaya. A number of groups from all over the world have been involved in Geo-scientific investigations in Tibet and Himalaya. In 1997, Department of Science & Technology, Govt. of India has also launched a multi-disciplinary programme in NW Himalaya. A 2-days Workshop meeting will be organised to discuss the data and results emerging from all disciplines in different sectors of the Himalaya.
5 Venue:: National Geophysical Research Institute (An ISO 9001 Organisation) Hyderabad, India's principal Institution for R&D in earth science. For further details: Convener Prof. Baldev Arora Indian Institute of Geomagnetism Navi Mumbai, Presently at Wadia Institute of Himalayan Geology 33, Gen. Mahadeo Singh Road, Dehradun wihg@emindia2004.org Voice: +91-(0) Fax :+91-(0) Co-Convener Dr. T. Harinarayana National Geophysical Research Institute Uppal Road, Hyderabad , A.P.,India tharinarayana@emindia2004.org Voice: Fax:
LECTURE 1 - Introduction Hrvoje Tkalčić
LECTURE 1 - Introduction Hrvoje Tkalčić *** N.B. The material presented in these lectures is from the principal textbooks, other books on similar subject, the research and lectures of my colleagues from
International Union of Geodesy and Geophysics. Resolutions
International Union of Geodesy and Geophysics Resolutions ADOPTED BY THE COUNCIL AT THE XXVI GENERAL ASSEMBLY PRAGUE, CZECH REPUBLIC (22 JUNE 2 JULY 2015) 0 Page Resolution 1: Role of Ocean in Climate
New Progress of SinoProbe:
New Progress of SinoProbe: Deep Exploration in China, 2008-2012 Shuwen DONG, Tingdong LI, et al. Chinese Academy of Geological Sciences Beijing 100037 China Background of Deep Exploration in World USA
Dr. Yildirim Dilek Department of Earth Sciences Miami University, USA
Dr. Yildirim Dilek Department of Earth Sciences Miami University, USA 40 years of successful, field-based, inter-disciplinary exploration of the Earth processes and training of the future generations of
ANNOUNCEMENT WMO/ESCAP PANEL ON TROPICAL CYCLONES THIRTY-EIGHTH SESSION NEW DELHI, INDIA
WMO IMD ESCAP ANNOUNCEMENT THIRTY-EIGHTH SESSION NEW DELHI, INDIA (21-25 February 2011) HISTORICAL BACKGROUND The tropical cyclones are particularly severe in the north Indian Ocean region. The northern
Grand Unifying Theory of everything... for the Geosciences, at least!
Plate Tectonics: Grand Unifying Theory of everything... for the Geosciences, at least! The Earth s lithosphere, composed of Oceanic and continental crust, is broken up into pieces that move and interact
Plate Tectonics Lab II: Background Information
Plate Tectonics Lab II: Background Information This lab is based on a UW ESS101 Lab. Note: Hand in only the Answer Sheet at the back of this guide to your Instructor Introduction One of the more fundamental
Sub-basalt exploration in the Kutch-Saurashtra basin using EM
Sub-basalt exploration in the Kutch-Saurashtra basin using EM Paper ID: 2003081 Deepankar Borgohain 1, Krishna Kumar 2, U G Marathe 3, Pradipta Mishra 3, Deepak Kumar 1 1.EMGS Asia Pacific Sdn Bhd, 1009
Global Challenges And Indian Initiatives *
HIGH LEVEL FORUM ON GLOBAL GEOSPATIAL MANAGEMENT INFORMATION WORKING PAPER No. 15 First Forum Seoul, Republic of Korea, 24-26 October 2011 Global Challenges And Indian Initiatives * * Submitted by: Mr.
Welcome to GEO 101 Introduction to Geology
Welcome to GEO 101 Introduction to Geology so what is Geology? not just rocks! Geology is... study of Earth and planetary bodies processes responsible for formation processes that modify all areas of geology
Mapping of Mesozoic Sediments below Deccan trap using Magnetotelluric Method.
P - 364 Mapping of Mesozoic s below Deccan trap using Magnetotelluric Method. Surajit Gorain*(sgorain@gmail.com), Puja Prakash, Dr. Prabhakar Thakur Hindustan Petroleum Corporation Limited Summary Magnetotelluric
Multi-Hazard Mitigation of Risks to Cultural Heritage
Indo-Italian Joint Workshop on: Multi-Hazard Mitigation of Risks to Cultural Heritage 4-5 December 2017, Senate Hall, IIT Delhi Organised by: Indian Institute of Technology, Jodhpur Embassy of Italy, New
GOVERNMENT OF INDIA MINISTRY OF EARTH SCIENCES
GOVERNMENT OF INDIA MINISTRY OF EARTH SCIENCES MINUTES OF THE MEETING HELD ON 14th DECEMBER 2010 AT SCOPE CONVENTION CENTRE, NEW DELHI TO DISCUSS PROPOSAL FOR DEEP DRILLING IN KOYNA REGION. A meeting was
UNCLOS Article 76- Formulae and constraint lines
UNCLOS Article 76- Formulae and constraint lines Dr Lindsay Parson (UNCLOS Group, National Oceanography Centre, UK) ABLOS TUTORIAL SESSION - Article 76 of UNCLOS 10th October 2005 IHO/IAG/IOC Advisory
Specific gravity field and deep crustal structure of the Himalayas east structural knot
49 4 2006 7 CHINESE JOURNAL OF GEOPHYSICS Vol. 49, No. 4 Jul., 2006,,.., 2006, 49 (4) :1045 1052 Teng J W, Wang Q S, Wang GJ, et al. Specific gravity field and deep crustal structure of the Himalayas east
12/3/2014. Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7. Continental drift: an idea before its time
Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7 Stanley C. Hatfield Southwestern Illinois College Continental drift: an idea before its time Alfred Wegener First proposed
GEO-DEEP9300 Lithosphere and Asthenosphere: Composition and Evolution
GEO-DEEP9300 Lithosphere and Asthenosphere: Composition and Evolution Summary Presentation The Structural Evolution of the Deep Continental Lithosphere Focused on the Junction of Arabian, Eurasian and
FORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.
FORCES ON EARTH An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. GEOLOGY Geologists scientists who study the forces that make and shape the Earth Geologists
The continental lithosphere
Simplicity to complexity: The continental lithosphere Reading: Fowler p350-377 Sampling techniques Seismic refraction Bulk crustal properties, thickness velocity profiles Seismic reflection To image specific
FINLAND, A COOL ARCTIC COUNTRY WITH SNOW-HOW
FINLAND, A COOL ARCTIC COUNTRY WITH SNOW-HOW To succeed in a constantly changing world, you have to change as well. Finland has reinvented itself in just one short century and we re still at it. Our national
Introduction To Plate Tectonics Evolution. (Continents, Ocean Basins, Mountains and Continental Margins)
Introduction To Plate Tectonics Evolution (Continents, Ocean Basins, Mountains and Continental Margins) Geo 386 (Arabian Shield Course) Dr. Bassam A. A. Abuamarah Mohanna G E O 3 8 6 A R A B I A N G E
Dar es Salaam - Reality Check Workshop
Dar es Salaam - Reality Check Workshop hosted by GIZ and Dar es Salaam City Council Introduction: Key Urban Characteristics of Dar es Salaam Challenges and Opportunities for Resilient Development in the
v Hypothesis: The uplift of the Tibetan Plateau is an active driver for global cooling of the Cenozoic period By Roslyn Gober 11 February 2015
Objective Uplift of Tibetan Plateau as Active Driver for Cenozoic Climate Change v Use Paleoarchives from the Tibetan Plateau to support the uplift weathering hypothesis for global cooling over the last
OCN 201 Physiography of the Seafloor
OCN 201 Physiography of the Seafloor Hypsometric Curve for Earth s solid surface Note histogram Hypsometric curve of Earth shows two modes. Hypsometric curve of Venus shows only one! Why? Ocean Depth vs.
Coastal Zones & Ocean Science
4 th International Conference on Coastal Zones & Ocean Science Theme: Discovering the Innovative methods for the betterment of Coastal and Ocean science Dates: May 15-16, 2019 Venue: https://coastalzonemanagement.conferenceseries.com/
USU 1360 TECTONICS / PROCESSES
USU 1360 TECTONICS / PROCESSES Observe the world map and each enlargement Pacific Northwest Tibet South America Japan 03.00.a1 South Atlantic Arabian Peninsula Observe features near the Pacific Northwest
Global Chemistry Congress. June 10-12, 2019 Rome, Italy
June 10-12, 2019 Rome, Italy Global Chemistry Congress Phronesis, LLC, 919 North Market Street, Suite 950 Wilmington, Delaware 19801 USA Email: gcc@phronesisonline.net, gcc@phronesisonline.us Tel: +1 (302)
Cooperating Organization Report of Circum Pacific Council for Energy and Mineral Resources (CPC)
CCOP-41AS/6.2-29 Coordinating Committee for Geoscience Programmes in East and Southeast Asia (CCOP) 41 st CCOP Annual Session 15 18 November 2004 Tsukuba, Japan Cooperating Organization Report of Circum
Geology 101 Lab 7: Isostasy Laboratory
Name TA Name Geology 101 Lab 7: Isostasy Laboratory To what thickness can sediments accumulate on the earth s surface, and what controls this thickness? How deeply can the continents be eroded? These are
Refer to the map on page 173 to answer the following questions.
Chapter 8-1 Plate Tectonics 1. Brainstorm the type of evidence that would indicate a climate change and how this evidence supports the theory of continental drift. Tropical fossils in cold regions Evidence
SEISMIC VELOCITY STRUCTURE OF THE NORTHWESTERN & NORTHEASTERN HIMALAYA AND ITS IMPLICATIONS FOR EARTHQUAKE HAZARD ASSESSMENT
SEISMIC VELOCITY STRUCTURE OF THE NORTHWESTERN & NORTHEASTERN HIMALAYA AND ITS IMPLICATIONS FOR EARTHQUAKE HAZARD ASSESSMENT UKIERI Thematic Partnership Supriyo Mitra Keith Priestley Motivation ~50 Ma
Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.
Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.
OCN 201 Physiography of the Seafloor
OCN 201 Physiography of the Seafloor 1 Ocean Depth versus Continental Height Why do we have dry land? Solid surface of Earth is dominated by two levels: Land with a mean elevation of +840 m (29% of Earth
Deformation of the Crust
Deformation of the Crust Review Choose the best response. Write the letter of that choice in the space provided. 1. The state of balance between the thickness of the crust and the depth at which it rides
DR. PRASANTA K. PATRO CSIR-NGRI, HYDERABAD, INDIA http://scholar.google.co.in/citations?hl=en&user=bzevoe8aaaaj NGRI RESEARCH GROUP: Magnetotellurics FIELD OF SPECIALIZATION: Passive Electromagnetics,
RCOF Review [Regional Climate Outlook Forum for the Gulf of Guinea region of Africa - PRESAGG] Status Report
![RCOF Review [Regional Climate Outlook Forum for the Gulf of Guinea region of Africa - PRESAGG] Status Report](/thumbs/78/77466191.jpg "RCOF Review [Regional Climate Outlook Forum for the Gulf of Guinea region of Africa - PRESAGG] Status Report")
RCOF Review 2017 [Regional Climate Outlook Forum for the Gulf of Guinea region of Africa - PRESAGG] Status Report Specific Climate features of concerned region This region typically covers the area below
34 th IGC, AUSTRALIA 2012 Brisbane Convention and Exhibition Centre (BCEC) Opening 5 August 2012 Closing 10 August 2012 Pre-congress training workshop
34th International Geological Congress Brisbane, Australia: 5-10 August, 2012 www.34igc.org 03/153-22 34 th IGC, AUSTRALIA 2012 Brisbane Convention and Exhibition Centre (BCEC) Opening 5 August 2012 Closing
SUMMARY. Executive Summary: NAVAREA VIII provides the paper of MSI Self Assessment for CPRNW 10
CPRNW Meeting 10 Agenda Item 3.2.1 CPRNW10/3/2/VIII MSI Self Assessment - NAVAREA VIII Submitted by INDIA SUMMARY Executive Summary: NAVAREA VIII provides the paper of MSI Self Assessment for CPRNW 10
The Third International Congress on Geology, Resources, Geo-hazards of Myanmar and surrounding regions
The Third International Congress on Geology, Resources, Geo-hazards of Myanmar and surrounding regions 31 st January, 1 st & 2 nd February, 2018, Sedona Hotel, Yangon, Myanmar Congress Patron The Honorable
SEISMIC HAZARD ASSESSMENT - PRACTICAL CONSIDERATIONS
SEISMIC HAZARD ASSESSMENT - PRACTICAL CONSIDERATIONS Richard D SHARPE 1 And Robert D JURY 2 SUMMARY Most national seismic design codes are developed over a considerable period of time by interested parties
Areas Beyond National Jurisdiction (ABNJ) 2016 Regional Leaders Program. March 22 to April 1, 2016 United Nations, New York
Areas Beyond National Jurisdiction (ABNJ) 2016 Regional Leaders Program March 22 to April 1, 2016 United Nations, New York Welcome and Introductions Biliana Cicin-Sain President, Global Ocean Forum Vladimir
Earth s Interior: Big Ideas. Structure of the Earth
Earth s Interior: Big Ideas Earth science investigations take many different forms. Earth scientists do reproducible experiments and collect multiple lines of evidence. Our understanding of Earth is continuously
The Junior College Multi-Disciplinary Conference: Research, Practice and Collaboration
The Junior College Multi-Disciplinary Conference: Research, Practice and Collaboration Pre-Conference Physics Workshop Monday, 17 September 2018 1 Programme NB The programme may be subject to changes Monday
Continental Drift. & Plate Tectonics
Continental Drift & Plate Tectonics Alfred Wegener, a German scientist, proposed the hypothesis of CONTINENTAL DRIFT, in 1912. Hypothesis stated: All Earth s continents were once a single landmass (Pangaea)
Earth s Tectonic Plates
MASTER 49 6.2 3.7 5.4 Philippine Pacific 5.4 North American Juan de Fuca Caribbean Cocos 10.0 9.2 2.3 2.5 2.3 1.8 3.0 Indian-Australian 10.5 7.1 17.2 16.8 6.0 Nazca South American 11.1 10.3 7.3 3.7 7.5
Five Themes of Geography Project Ms. Kiesel, Per 5. The United States of America
Five Themes of Geography Project Ms. Kiesel, Per 5 The United States of America Location Absolute Location : The USA is located in the continent of North America in the northern and western hemispheres.
Sub-regional Training on development of Geo-referenced Disaster Risk Management Information Systems for SAARC countries
Sub-regional Training on development of Geo-referenced Disaster Risk Management Information Systems for SAARC countries Jointly organized by Economic and Social Commission for Asia and the Pacific and
FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.
FORCES ON EARTH UNIT 3.2 An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. USE THESE NOTES: OUR HOME PLANET EARTH: What do you know about our planet? SO.HOW
Chapter 21 Southwest Asia: Harsh & Arid Lands
Name Hour Chapter 21 Southwest Asia: Harsh & Arid Lands Essential Question: How has the physical geography of Asia influenced the development of these regions (i.e. history, population distribution, &
HYDERABAD STUDY CIRCLE CIVILS PRELIMS (GS) - TEST SERIES SCHEDULE Ancient India I
HYDERABAD STUDY CIRCLE CIVILS PRELIMS (GS) - TEST SERIES SCHEDULE 2018 Date No. 24-02-2018-1 Geography - I India location, Size Structure and Physiography Drainage system + map Pointing (India) Ancient
Annexure I. SCIENTIFIC AND LOGISTICS OBJECTIVES OF THE 30 th INDIAN SCIENTIFIC ANTARCTIC EXPEDITION
Annexure I SCIENTIFIC AND LOGISTICS OBJECTIVES OF THE 30 th INDIAN SCIENTIFIC ANTARCTIC EXPEDITION Investigation of magnetospheric-ionospheric coupling between high and low latitudes related to space weather
TRAINING ON GLACIER STUDIES AND REMOTE SENSING
TRAINING ON GLACIER STUDIES AND REMOTE SENSING Divecha Centre for Climate Change Bengaluru Indian Institute of Science June 19-30, 2017 Bengaluru- 560012 Sponsored by Divecha Centre for Climate Change
UNIVERSITY OF NAIROBI
UNIVERSITY OF NAIROBI SPEECH DELIVERED BY THE VICE-CHANCELLOR PROF. G.A.O. MAGOHA DURING THE KENYA JAPAN EXCHANGE SEMINAR ON OCEAN SCIENCE COOPERATING TOWARDS A BETTER PLANET EARTH ON 16 TH JANUARY 2006
NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2
NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2 Assignment is due the beginning of the class period on December 14, 2004. Mark answers on a scantron sheet, which will be provided.
Vision: The National Oceanography Centre will, by 2015, be recognised as the world-leading Centre for integrated ocean sciences and technology".
National Oceanography Centre from coast to deep ocean Waterfront Campus, Southampton Vision: Joseph Proudman Building, Liverpool The National Oceanography Centre will, by 2015, be recognised as the world-leading
August 8-10, 2016 Lhasa, China
International Workshop on Land Surface Multi-spheres Processes of Tibetan Plateau and their Environmental and Climate Effects Assessment First Circular August 8-10, 2016 Lhasa, China Organized and Sponsored
The Nansen-Zhu International Research Centre: Beijing, China
The Nansen-Zhu International Research Centre: Beijing, China Vision To become an internationally acknowledged climate research and training centre with emphasis on tropical and highlatitude regions, and
12. The diagram below shows the collision of an oceanic plate and a continental plate.
Review 1. Base your answer to the following question on the cross section below, which shows the boundary between two lithospheric plates. Point X is a location in the continental lithosphere. The depth
LAB J - WORLD CLIMATE ZONES
Introduction LAB J - WORLD CLIMATE ZONES The objective of this lab is to familiarize the student with the various climates around the world and the climate controls that influence these climates. Students
Capacity Building Programme
Capacity Building Programme 14-17 August 2012 Space Technology for improving Hazard Mapping in Sri Lanka An event organised as a follow up of the UN-SPIDER Technical Advisory Mission to Sri Lanka - 17-21
Earth s Interior StudyGuide
Name Date Period Earth s Interior StudyGuide 1. The two main elements that make up the Earth s crust are and. 2. The Earth s inner core is made of solid and. 3. When one plates slides under another plate
International Geomagnetic Reference Field the eighth generation
Earth Planets Space, 52, 1119 1124, 2000 International Geomagnetic Reference Field the eighth generation Mioara Mandea 1 and Susan Macmillan 2 1 Institut de Physique du Globe de Paris, B.P. 89, 4 Place
Plates Moving Apart Types of Boundaries
Plates Moving Apart Types of Boundaries PLATE TECTONICS IS The theory that the Earth s crust is broken into slabs of rock that move around on top of the asthenosphere. How fast are plates moving? The Arctic
BELLRINGER How close a group of measurements are to each other is called. 1. estimation 2. accuracy 3. precision. 0% 0% 0% 0% 4.
BELLRINGER How close a group of measurements are to each other is called 1. estimation 2. accuracy 3. precision 0% 0% 0% 0% 4. percent error estimation accuracy precision percent error Inside Earth Chapter
Learning Objectives (LO)! Lecture 11: Plate Tectonics II! No Homework!! ** Chapter 3 **! What we ll learn today:!
Learning Objectives (LO)! Lecture 11: Plate Tectonics II! No Homework!! ** Chapter 3 **! What we ll learn today:! 1. List the three types of tectonic plate boundaries! 2. Describe the processes occurring
Iceland. 1. Warm up. A. Talk about the picture and read the essay. B. Discuss the questions about the essay.
1. Warm up A. Talk about the picture and read the essay. Iceland My country, Iceland, is one of the most beautiful countries on Earth. It is an island country. It is located in Europe, in the North Atlantic
Nanotechnology: Energy & Health
\ Indian Academy of Sciences, Bangalore Indian National Science Academy, New Delhi The National Academy of Sciences, Allahabad Fergusson College, Pune Sponsored by Science Academies Lecture Workshop on
The thermal and density structure of passive margins
The thermal and density structure of passive margins Magdalena Scheck-Wenderoth, Yuriy Maystrenko, Julia Autin, Hans Jürgen Götze, Sabine Schmidt, Christian Reichert basins in their plate-tectonic setting
Warm Episode over Indian Sub-continent March 2010 By Richard Grumm National Weather Service State College Contributions by Lance Bosart SUNY Albany
Warm Episode over Indian Sub-continent March 2010 By Richard Grumm National Weather Service State College Contributions by Lance Bosart SUNY Albany 1. INTRODUCTION A massive subtropical ridge formed over
Prentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined
Prentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined
United Nations, UNGEGN, and support for national geographical names standardization programmes
Philippines, 2018 United Nations, UNGEGN, and support for national geographical names standardization programmes Helen Kerfoot, UNGEGN Cecille Blake, UNGEGN Secretariat What is important to know? Background
Name Class Date. 1. What is the outermost layer of the Earth called?. a. core b. lithosphere c. asthenosphere d. mesosphere
Name Class Date Assessment Geology Plate Tectonics MULTIPLE CHOICE Write the letter of the correct answer in the space provided. 1. What is the outermost layer of the Earth called?. a. core b. lithosphere
The Theory of Continental Drift. Continental Drift Discovery
The Theory of Continental Drift Continental Drift Discovery The World ALFRED WEGENER THEORY OF CONTINENTAL DRIFT Found evidence for PANGAEA and proposed the theory of continental drift. Continental Drift
Land Board, NW Services and SDI Tambet Tiits, FRICS
Land Board, NW Services and SDI Tambet Tiits, FRICS 07.09.2016 200th anniversary of the Struve Geodetic Arc Friedrich Georg Wilhelm Struve and Carl Friedrich Tenner Struve Geodetic Arc The Struve Geodetic
Visiting Faculty at Amity University, Haryana for the Course Engineering Geology for B.Tech (Civil Engineering).
Dr. PANKAJ MEHTA Ph: 91 9868447103 (M) Email: - drpankajmehta79@gmail.com CURRENT POSITION & ASSIGNMENT Assistant Professor Environmental Sciences September 2010 till Date Working as Assistant Professor
TOPIC 8: POPULATION DISTRIBUTION AND URBANIZATION
TOPIC 8: POPULATION DISTRIBUTION AND URBANIZATION Concept of population distribution Factors affecting population distribution and density Urbanization: Concept and issues associated Introduction WORLD
Indian Ocean Forecast System (INDOFOS) Abhisek Chatterjee
Indian Ocean Forecast System (INDOFOS) Abhisek Chatterjee Earth System Sciences Organisation (ESSO) Indian National Centre for Ocean Information Services (INCOIS) Ministry of Earth Sciences, Government
Post Independence Trends of Urbanization and Role of Small and Medium Towns in Maharashtra- A Geographical Analysis
Post Independence Trends of Urbanization and Role of Small and Medium Towns in Maharashtra- A Geographical Analysis A careful and systematic study of the process of urbanization and related factors is
PLATE TECTONICS. Continental Drift. Continental Drift. Continental Drift. Continental Drift- Wegener s Evidence
Continental Drift PLATE TECTONICS E.B. Taylor (1910) and Alfred Wegener (1915) published on Continental Drift. Continental Drift Wegener s evidence 1. Fit of the Continents 2. Fossil Evidence 3. Rock Type
Canadian Mapping Big Book
Canadian Mapping Big Book Grades 4-6 Written by Lynda Golletz Illustrated by S&S Learning Materials About the Author: Lynda Golletz was an elementary school teacher for thirty-three years. She is the author
GD3.3/GM3.3/GMPV16/TS4.7
GD Geodynamics Orals and PICOs MO1, 08:30 10:00 MO2, 10:30 12:00 MO3, 13:30 15:00 MO4, 15:30 17:00 TU1, 08:30 10:00 TU2, 10:30 12:00 TU3, 13:30 15:00 Monday, 08 April Medal Lecture) (co-organized), 08:30
INFLUENCE OF LOCAL PERTURBATION ON REGIONAL STRESS AND ITS IMPACT ON THE DESIGN OF MAJOR UNDERGROUND STRUCTURE IN HYDROELECTRIC PROJECT
INFLUENCE OF LOCAL PERTURBATION ON REGIONAL STRESS AND ITS IMPACT ON THE DESIGN OF MAJOR UNDERGROUND STRUCTURE IN HYDROELECTRIC PROJECT *D.S. Subrahmanyam National Institute of Rock Mechanics, Bangalore
Chapter. Graphics by Tasa Graphic Arts. Inc.
Earth Chapter Plate Science 9 Tectonics Graphics by Tasa Graphic Arts. Inc. 1 I. Earth s surface is made up of lithospheric plates. A. Lithospheric plates are composed of the crust and part of the upper
Continental Drift Discussion Questions:
Continental Drift Discussion Questions: 1) What are tectonic plates? 2) What happens at the boundaries between these plates? 3) What are fault lines? 4) What effect has Continental Drift had on the shape
Tropical Moist Rainforest
Tropical or Lowlatitude Climates: Controlled by equatorial tropical air masses Tropical Moist Rainforest Rainfall is heavy in all months - more than 250 cm. (100 in.). Common temperatures of 27 C (80 F)
Effects of galvanic distortions on magnetotelluric data: Interpretation and its correction using deep electrical data
Effects of galvanic distortions on magnetotelluric data: Interpretation and its correction using deep electrical data Jimmy Stephen 1, S G Gokarn 2, C Manoj 1 and S B Singh 1 1 National Geophysical Research
Rising from the Depths Utilising Marine Cultural Heritage in East Africa to help develop sustainable social, economic and cultural benefits
KENYA MEETING, 23 rd FEBRUARY 2018 1 Rising from the Depths Utilising Marine Cultural Heritage in East Africa to help develop sustainable social, economic and cultural benefits 1. Introduction The Rising
In order to study Plate Tectonics, we must first
TB Chapter 13 In order to study Plate Tectonics, we must first reorganize our layering system for the Earth: Old System 4 layers Crust (rigid) id) (rigid) Mantle (putty like) (semi rigid) Outer core (liquid)
Survey Of India. Route Map For The Western Himalayas, Kashmir, Punjab And Northern India, With Portions Of Afghanistan, Baluchistan &c (including The
Survey Of India. Route Map For The Western Himalayas, Kashmir, Punjab And Northern India, With Portions Of Afghanistan, Baluchistan &c (including The Former Kashmir Route Map). Compiled Originally By Major
Map Skills Test. 1. What do we call a person who makes maps? a. mapographer b. cartographer c. geologist d. archaeologist
Map Skills Test 1. What do we call a person who makes maps? a. mapographer b. cartographer c. geologist d. archaeologist 2. What is the name of the 0 latitude line? a. Equator b. Arctic Circle c. First
Blocks offered in Sri Lanka s Second Licensing Round
Blocks offered in Sri Lanka s Second Licensing Round Sri Lankan Main Basins Cauvery Basin Cauvery Deep Water sub-basin Mannar Basin 2 Structural Framework Sri Lanka Basins Cauvery & Mannar Basins were
Untapped Vast Hydrocarbon Resource Potential of Deep Water basins in India
Untapped Vast Hydrocarbon Resource Potential of Deep Water basins in India Dev Dutt Sharma, Principal Geologist, Oilex Limited, Australia ABSTRACT India is the fourth largest consumer of hydrocarbons and
TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April
TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April MO1, 08:30 10:00 MO2, 10:30 12:00 MOL, 12:15 13:15 MO3, 13:30 15:00 MO4, 15:30 17:00 GD3.3/GM3.3/GMPV16/TS4.7, The evolution of plate
ICTP (International Centre for Theoretical Physics) representative, Director, School of Computing and Informatics,
DVC(RPE) s Speech at The Opening Ceremony of the Workshop on Applications of Wireless Sensor Networks for Weather Monitoring in East Africa Protocol: Thursday, 7 th July 2011 The Radio Communications Unit
Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor
Earth s Continents and Seafloors GEOL100 Physical Geology Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types of crust Dense, thin,
Aerosol Optical Depth Variation over European Region during the Last Fourteen Years
Aerosol Optical Depth Variation over European Region during the Last Fourteen Years Shefali Singh M.Tech. Student in Computer Science and Engineering at Meerut Institute of Engineering and Technology,
Dynamic Earth Quiz. 4. The accompanying diagram shows some features of Earth s crust and upper mantle.
DO NOT WRITE ON THIS Dynamic Earth Quiz DO NOT WRITE ON THIS 1. Base your answer(s) to the following question(s) on the diagram below. The diagram shows a model of the relationship between Earth s surface
The Structure of the Earth and Plate Tectonics
The Structure of the Earth and Plate Tectonics Agree or Disagree? 1. The Earth if made up of 4 different layers. 2. The crust (where we live) can be made of either less dense continental crust or the more
About places and/or important events Landmarks Maps How the land is, hills or flat or mountain range Connected to maps World Different countries
What do you think you know about geography? About places and/or important events Landmarks Maps How the land is, hills or flat or mountain range Connected to maps World Different countries What do you