This document provides an overview of plate tectonic theory, which unified and improved upon earlier continental drift and sea-floor spreading theories. It discusses key evidence for plate tectonics from ocean floor mapping and paleomagnetism studies. Mapping revealed the global mid-ocean ridge system and age dating showed sea floors are younger further from ridges, supporting the idea of sea floor spreading. Paleomagnetism data also indicated periodic reversals of the Earth's magnetic field and allowed calculation of spreading rates.
GEOSPATIAL TECHNOLOGY, CONCEPT, TECHNIQUES AND ITS COMPONENTS. pptxMalothSuresh2
Geospatial technology involves three major components: Geographic Information Systems (GIS), Global Positioning Systems (GPS), and Remote Sensing (RS). GIS is used for geospatial analysis and mapping across many industries. GPS uses satellites to determine location on Earth. Remote sensing collects imagery from space and aircraft. Together these tools capture spatial data to analyze resources and make informed decisions.
This document is a thesis submitted by Gagandeep Singh for his M.Tech degree in RS & GIS from NIT Warangal in 2013-2015. It discusses various topics related to digital terrain modeling including contour lines, grid DTMs, TINs, the differences between DSMs and DEMs, data acquisition methods, processing techniques, and applications of digital terrain data. It also evaluates different data sources for terrain modeling like SRTM, topographic maps, and Google Earth imagery and assesses their accuracy through statistical analysis and visual inspection.
This document provides an overview of a course on applying remote sensing and geographical information systems in civil engineering. The course consists of lectures and seminars covering topics in remote sensing and GIS. For remote sensing, lectures will discuss principles, sensors, data processing, platforms, image processing software, and microwave sensing. For GIS, lectures will cover concepts, data structures, software tools like ArcGIS, spatial queries, and applications in hydrological modeling. The goal of the course is to provide students with an understanding of remote sensing and GIS and their integration, and to learn basic skills in working with related data and software.
Galileo is the European GNSS constellation and it contributes to the user positioning adding more satellites, which number directly impacts on the Dilution of precision (DOP), or geometric dilution of precision (GDOP). It is a term used in satellite navigation and geomatics engineering to specify the additional multiplicative effect of navigation satellite geometry on positional measurement precision.
UN-GGIM is a United Nations initiative that aims to coordinate global geospatial information management. It was established in 2011 to address issues such as improving policy and legal frameworks, addressing global challenges, and building geospatial capacity. The document discusses UN-GGIM's history, mandates, regional entities, and a report on future trends. It also covers topics like how GIS is used by national statistical offices and for sustainable development goals monitoring through case studies. The role of governments in providing geospatial data and engaging citizens is examined, as well as challenges and recommendations for reaching developing countries.
GPS uses a constellation of 24 satellites orbiting Earth to enable GPS receivers to determine their precise location. The system works by using triangulation based on distance measurements from at least three satellites. The GPS segments include the space segment (satellites), control segment (ground stations that monitor satellites), and user segment (GPS receivers). GPS has both military and civilian applications including navigation, mapping, vehicle tracking, and monitoring fishing fleets.
This document summarizes a seminar on remote sensing technologies guided by Mr. B. S. Manjare from the P.G. Department of Geology at Rashtrasant Tukadoji Maharaj Nagpur University. The seminar covered the history and objectives of India's space program, types of satellites and launch vehicles used, characteristics of the Indian Remote Sensing satellite series, applications of remote sensing in geology, and India's roadmap for future space missions. Key topics discussed included the various generations of IRS satellites with improving sensors, applications of remote sensing for natural resource management and disaster monitoring, and India's goals of developing reusable launch vehicles and satellites with advanced capabilities.
GEOSPATIAL TECHNOLOGY, CONCEPT, TECHNIQUES AND ITS COMPONENTS. pptxMalothSuresh2
Geospatial technology involves three major components: Geographic Information Systems (GIS), Global Positioning Systems (GPS), and Remote Sensing (RS). GIS is used for geospatial analysis and mapping across many industries. GPS uses satellites to determine location on Earth. Remote sensing collects imagery from space and aircraft. Together these tools capture spatial data to analyze resources and make informed decisions.
This document is a thesis submitted by Gagandeep Singh for his M.Tech degree in RS & GIS from NIT Warangal in 2013-2015. It discusses various topics related to digital terrain modeling including contour lines, grid DTMs, TINs, the differences between DSMs and DEMs, data acquisition methods, processing techniques, and applications of digital terrain data. It also evaluates different data sources for terrain modeling like SRTM, topographic maps, and Google Earth imagery and assesses their accuracy through statistical analysis and visual inspection.
This document provides an overview of a course on applying remote sensing and geographical information systems in civil engineering. The course consists of lectures and seminars covering topics in remote sensing and GIS. For remote sensing, lectures will discuss principles, sensors, data processing, platforms, image processing software, and microwave sensing. For GIS, lectures will cover concepts, data structures, software tools like ArcGIS, spatial queries, and applications in hydrological modeling. The goal of the course is to provide students with an understanding of remote sensing and GIS and their integration, and to learn basic skills in working with related data and software.
Galileo is the European GNSS constellation and it contributes to the user positioning adding more satellites, which number directly impacts on the Dilution of precision (DOP), or geometric dilution of precision (GDOP). It is a term used in satellite navigation and geomatics engineering to specify the additional multiplicative effect of navigation satellite geometry on positional measurement precision.
UN-GGIM is a United Nations initiative that aims to coordinate global geospatial information management. It was established in 2011 to address issues such as improving policy and legal frameworks, addressing global challenges, and building geospatial capacity. The document discusses UN-GGIM's history, mandates, regional entities, and a report on future trends. It also covers topics like how GIS is used by national statistical offices and for sustainable development goals monitoring through case studies. The role of governments in providing geospatial data and engaging citizens is examined, as well as challenges and recommendations for reaching developing countries.
GPS uses a constellation of 24 satellites orbiting Earth to enable GPS receivers to determine their precise location. The system works by using triangulation based on distance measurements from at least three satellites. The GPS segments include the space segment (satellites), control segment (ground stations that monitor satellites), and user segment (GPS receivers). GPS has both military and civilian applications including navigation, mapping, vehicle tracking, and monitoring fishing fleets.
This document summarizes a seminar on remote sensing technologies guided by Mr. B. S. Manjare from the P.G. Department of Geology at Rashtrasant Tukadoji Maharaj Nagpur University. The seminar covered the history and objectives of India's space program, types of satellites and launch vehicles used, characteristics of the Indian Remote Sensing satellite series, applications of remote sensing in geology, and India's roadmap for future space missions. Key topics discussed included the various generations of IRS satellites with improving sensors, applications of remote sensing for natural resource management and disaster monitoring, and India's goals of developing reusable launch vehicles and satellites with advanced capabilities.
Thermal infrared remote sensing involves observing electromagnetic radiation emitted from objects in the thermal infrared wavelength range of 3-14 micrometers. In this range, sensors can detect the thermal radiative properties of ground materials. Thermal infrared imagery captures relative differences in surface temperature or radiance. Interpreting thermal images requires understanding factors like the time of day the image was taken, whether it is a positive or negative image, and how emissivity and other surface characteristics impact observed radiation and temperature values.
This document provides an introduction to Landsat and Google Earth Engine. It discusses what remote sensing is and gives an overview of Landsat, including its history, sensors, data access and applications. It also introduces Google Earth Engine, describing what it is, how it can be used to analyze large geospatial datasets, and provides some examples of analyses that can be done with it, including monitoring land use change.
This document discusses differential GPS (DGPS), which improves the accuracy of GPS positioning. It works by using a stationary GPS receiver at a known location to calculate error corrections, which are transmitted to a roving receiver to improve its position accuracy. DGPS can reduce GPS errors from sources like atmospheric delays, satellite orbit issues, and multipath effects, providing sub-meter accuracy compared to the 5-10 meter accuracy of standard GPS. It allows real-time position correction or post-processed correction through data from a fixed base station.
The basic intention of this presentation is to help the beginners in GIS to understand what GIS is? It is a simple presentation about GIS, i mean an introductory one. Hope anyone finds it useful.
Global mapper tutorial Jimma University Ethiopiachala hailu
This document discusses using Global Mapper software to delineate watersheds and calculate peak runoff for flood analysis. It provides an overview of common hydrological analysis methods for estimating maximum flood levels, and describes using the SCS unit hydrograph method within Global Mapper. It also outlines the basic steps and tools in Global Mapper for watershed delineation and peak runoff calculation.
Ground Penetrating Radar, also known as GPR, is a tool that is used to find Underground Utilities, Underground Storage Tanks (USTs), and in some cases, Graves. The depth and accuracy are dependent on a number of variables, such as soil density, moisture content, and antenna frequency. We use a 350 MHz antenna, which has the potential to reach depths of up to 35 ft (in perfect situations).
Geodesy is the science of measuring and representing the Earth, including its gravity field. It has applications in monitoring climate change, natural hazards, volcanoes, water resources, soil moisture, glaciers, and landslides using space-based technologies like GNSS, altimetry, and gravity missions. Some key technologies are GPS, GLONASS, altimetry missions like TOPEX and JASON-1, and gravity missions like GRACE and CHAMP. Geodesy has its origins in ancient Greece and has evolved into a modern discipline using satellites to study Earth systems and processes.
This document summarizes the advantages and disadvantages of raster data. Raster data represents geographic information in a grid of cells, with each cell containing a value. The main advantages are simple data structure, easy overlay of maps and images, simple simulation, and ability to represent continuous surfaces. However, disadvantages include crude appearance, difficulty representing linear features, spatial inaccuracies due to cell size, large file sizes, and loss of precision from restricting data to grid cells.
Galileo used early optical enhancements in the 1600s to observe celestial bodies and merchant ships arriving in harbor. In the 1880s, Arthur Batut affixed cameras to kites, including an altimeter to determine the scale of images, making him the father of kite aerial photography. By 1903, camera miniaturization allowed cameras to be attached to pigeons for aerial photography, though images were limited. During the Cuban Missile Crisis in 1962, U-2 spy planes detected Soviet nuclear missiles in Cuba using remote sensing, changing the course of history.
Advantages and disadvantages of Remote SensingEr Abhi Vashi
This document discusses the advantages and disadvantages of remote sensing. Some key advantages include large area coverage allowing regional surveys, repetitive coverage enabling monitoring of dynamic themes, and data being acquired at different scales and resolutions. Disadvantages include remote sensing being expensive for small areas, requiring specialized training, and human errors potentially being introduced. The document provides 15 advantages and 9 disadvantages of remote sensing in detail.
Role of electromagnetic Radiation in Remote SensingNzar Braim
This document provides an overview of electromagnetic radiation and its role in remote sensing. It defines key characteristics of electromagnetic waves like amplitude, wavelength, frequency, and speed. It describes the electromagnetic spectrum and different radiation types. Laws governing radiation like Kirchhoff's law, Stefan-Boltzmann law, and Wien's displacement law are covered. The document also discusses how radiation interacts with the atmosphere through scattering, absorption, and refraction.
This document discusses remote sensing and geographic information systems (GIS). Remote sensing involves collecting data about objects from a distance using electromagnetic energy and sensors. It works through various stages including energy source, interaction with the target, sensor recording, processing, and interpretation. Remote sensing has applications in resource exploration, environmental monitoring, and land use analysis. GIS integrates spatial data using computer hardware, software, and trained personnel. It has advantages like visualization and modeling capabilities, and disadvantages like high costs and data errors. The future of remote sensing and GIS is promising as more industries adopt these technologies.
This document discusses types of errors that can occur during spatial data editing and digitizing, including location errors, mechanical errors, human errors, and topological errors. It describes tools and processes for correcting errors such as CLEAN, nodesnap, editdistance, EXTEND, SPLIT, and edgematching. Both topological and non-topological editing approaches are covered.
1) Geodesy is the science of measuring and mapping the Earth's surface, including determining its shape, size, and gravity field.
2) Early Greek scholar Eratosthenes used simple observations and geometry to estimate the circumference of Earth to within 1% accuracy over 2000 years ago.
3) While the Earth is approximated as an oblate spheroid, its true shape, called the geoid, is irregular due to density variations underground. Precise positioning and heights require accounting for geoid undulations.
This document provides an overview of a seminar on remote sensing, GIS and their application for soil fertility mapping. It introduces remote sensing concepts like passive and active sensing, platforms like aircraft and satellites, and multispectral sensors. It discusses how GIS organizes geographic data and examples of data sources. The document presents a case study that mapped soil properties in Mathura District, India using remote sensing and GIS techniques. It describes the digitizing process in ArcGIS and studies on mapping clay minerals and soil contamination with spectroscopy. The document concludes that remote sensing and GIS can efficiently map large areas to aid in crop selection and productivity.
This document provides an introduction to Geographic Information Systems (GIS). It defines GIS as a system designed to store, manipulate, analyze and display spatially referenced data. The key components of a GIS are hardware, software and data. Common GIS software includes desktop programs like ArcGIS and open-source options like QGIS. GIS can incorporate different types of spatial data like raster, vector and remote sensing data along with associated attribute tables. Example applications discussed are in hydrology, including watershed analysis and flood modeling.
Remote sensing and GIS can be applied in civil engineering for spatial analysis and to answer geographic queries. Spatial analysis examines how the locations of objects impact analysis results and can reveal patterns. GIS uses methods like overlay, proximity, density, and network analysis to study spatial relationships. Common analyses include measuring distances, areas and shapes, transforming datasets, descriptive summaries of data, and optimizing locations.
Presentation: This presentation gives a brief introduction to tools in ArcGIS and was designed for the Surface Water Quality Monitoring (SWQM) GIS training hosted by Texas Commission on Environmental Quality (TCEQ) staff.
Training: The goal of the SWQM GIS training course is to introduce beginner and intermediate GIS users within the TCEQ surface water monitoring network to the geospatial software, skills, analyses, and data most often used by water resource professionals. The training features presentations from a range of GIS experts from TCEQ, TPWD, and other organizations.
More information on the training: https://www.tceq.texas.gov/waterquality/monitoring/training
Digitizing in GIS is the process of converting geographic data either from a hardcopy or a scanned image into vector data by tracing the features. During the digitzing process, features from the traced map or image are captured as coordinates in either point, line, or polygon format.
GIS is a system for managing and analyzing geographic data. It uses two main data models: vector, representing points, lines and polygons; and raster, representing data as a grid of cells. Common file formats include shapefiles for vector data and GeoTIFF and MrSID for raster. GIS data is referenced using coordinate systems like WGS84 for global latitude/longitude or HK80Grid for Hong Kong. ESRI's ArcGIS software allows viewing, editing, and publishing this geospatial data for mapping and analysis.
1. The document discusses various theories related to geomorphology including the Nebular theory of Laplace regarding the origin of Earth, continental drift theory, sea-floor spreading theory and plate tectonic theory.
2. It describes evidence for continental drift including matching coastlines, similarity of rock ages, fossil evidence, and paleoclimatic evidence.
3. Sea-floor spreading theory helped explain mysteries of mid-ocean ridges and trenches observed in sea-floor mapping from the 1940s-1950s through concepts of new crust formation at ridges and destruction of old crust at trenches.
1) The document discusses key concepts in geography including physical geography, human geography, latitudes, longitudes, seasons on Earth, and time zones.
2) It provides summaries of different theories related to the structure and composition of the Earth's interior including the nebular theory of Laplace and evidence from seismic wave studies.
3) The document also summarizes different theories of geomorphology like the continental drift theory, sea-floor spreading theory, and the plate tectonic theory which together explain plate tectonics and the evolution of Earth's surface.
Thermal infrared remote sensing involves observing electromagnetic radiation emitted from objects in the thermal infrared wavelength range of 3-14 micrometers. In this range, sensors can detect the thermal radiative properties of ground materials. Thermal infrared imagery captures relative differences in surface temperature or radiance. Interpreting thermal images requires understanding factors like the time of day the image was taken, whether it is a positive or negative image, and how emissivity and other surface characteristics impact observed radiation and temperature values.
This document provides an introduction to Landsat and Google Earth Engine. It discusses what remote sensing is and gives an overview of Landsat, including its history, sensors, data access and applications. It also introduces Google Earth Engine, describing what it is, how it can be used to analyze large geospatial datasets, and provides some examples of analyses that can be done with it, including monitoring land use change.
This document discusses differential GPS (DGPS), which improves the accuracy of GPS positioning. It works by using a stationary GPS receiver at a known location to calculate error corrections, which are transmitted to a roving receiver to improve its position accuracy. DGPS can reduce GPS errors from sources like atmospheric delays, satellite orbit issues, and multipath effects, providing sub-meter accuracy compared to the 5-10 meter accuracy of standard GPS. It allows real-time position correction or post-processed correction through data from a fixed base station.
The basic intention of this presentation is to help the beginners in GIS to understand what GIS is? It is a simple presentation about GIS, i mean an introductory one. Hope anyone finds it useful.
Global mapper tutorial Jimma University Ethiopiachala hailu
This document discusses using Global Mapper software to delineate watersheds and calculate peak runoff for flood analysis. It provides an overview of common hydrological analysis methods for estimating maximum flood levels, and describes using the SCS unit hydrograph method within Global Mapper. It also outlines the basic steps and tools in Global Mapper for watershed delineation and peak runoff calculation.
Ground Penetrating Radar, also known as GPR, is a tool that is used to find Underground Utilities, Underground Storage Tanks (USTs), and in some cases, Graves. The depth and accuracy are dependent on a number of variables, such as soil density, moisture content, and antenna frequency. We use a 350 MHz antenna, which has the potential to reach depths of up to 35 ft (in perfect situations).
Geodesy is the science of measuring and representing the Earth, including its gravity field. It has applications in monitoring climate change, natural hazards, volcanoes, water resources, soil moisture, glaciers, and landslides using space-based technologies like GNSS, altimetry, and gravity missions. Some key technologies are GPS, GLONASS, altimetry missions like TOPEX and JASON-1, and gravity missions like GRACE and CHAMP. Geodesy has its origins in ancient Greece and has evolved into a modern discipline using satellites to study Earth systems and processes.
This document summarizes the advantages and disadvantages of raster data. Raster data represents geographic information in a grid of cells, with each cell containing a value. The main advantages are simple data structure, easy overlay of maps and images, simple simulation, and ability to represent continuous surfaces. However, disadvantages include crude appearance, difficulty representing linear features, spatial inaccuracies due to cell size, large file sizes, and loss of precision from restricting data to grid cells.
Galileo used early optical enhancements in the 1600s to observe celestial bodies and merchant ships arriving in harbor. In the 1880s, Arthur Batut affixed cameras to kites, including an altimeter to determine the scale of images, making him the father of kite aerial photography. By 1903, camera miniaturization allowed cameras to be attached to pigeons for aerial photography, though images were limited. During the Cuban Missile Crisis in 1962, U-2 spy planes detected Soviet nuclear missiles in Cuba using remote sensing, changing the course of history.
Advantages and disadvantages of Remote SensingEr Abhi Vashi
This document discusses the advantages and disadvantages of remote sensing. Some key advantages include large area coverage allowing regional surveys, repetitive coverage enabling monitoring of dynamic themes, and data being acquired at different scales and resolutions. Disadvantages include remote sensing being expensive for small areas, requiring specialized training, and human errors potentially being introduced. The document provides 15 advantages and 9 disadvantages of remote sensing in detail.
Role of electromagnetic Radiation in Remote SensingNzar Braim
This document provides an overview of electromagnetic radiation and its role in remote sensing. It defines key characteristics of electromagnetic waves like amplitude, wavelength, frequency, and speed. It describes the electromagnetic spectrum and different radiation types. Laws governing radiation like Kirchhoff's law, Stefan-Boltzmann law, and Wien's displacement law are covered. The document also discusses how radiation interacts with the atmosphere through scattering, absorption, and refraction.
This document discusses remote sensing and geographic information systems (GIS). Remote sensing involves collecting data about objects from a distance using electromagnetic energy and sensors. It works through various stages including energy source, interaction with the target, sensor recording, processing, and interpretation. Remote sensing has applications in resource exploration, environmental monitoring, and land use analysis. GIS integrates spatial data using computer hardware, software, and trained personnel. It has advantages like visualization and modeling capabilities, and disadvantages like high costs and data errors. The future of remote sensing and GIS is promising as more industries adopt these technologies.
This document discusses types of errors that can occur during spatial data editing and digitizing, including location errors, mechanical errors, human errors, and topological errors. It describes tools and processes for correcting errors such as CLEAN, nodesnap, editdistance, EXTEND, SPLIT, and edgematching. Both topological and non-topological editing approaches are covered.
1) Geodesy is the science of measuring and mapping the Earth's surface, including determining its shape, size, and gravity field.
2) Early Greek scholar Eratosthenes used simple observations and geometry to estimate the circumference of Earth to within 1% accuracy over 2000 years ago.
3) While the Earth is approximated as an oblate spheroid, its true shape, called the geoid, is irregular due to density variations underground. Precise positioning and heights require accounting for geoid undulations.
This document provides an overview of a seminar on remote sensing, GIS and their application for soil fertility mapping. It introduces remote sensing concepts like passive and active sensing, platforms like aircraft and satellites, and multispectral sensors. It discusses how GIS organizes geographic data and examples of data sources. The document presents a case study that mapped soil properties in Mathura District, India using remote sensing and GIS techniques. It describes the digitizing process in ArcGIS and studies on mapping clay minerals and soil contamination with spectroscopy. The document concludes that remote sensing and GIS can efficiently map large areas to aid in crop selection and productivity.
This document provides an introduction to Geographic Information Systems (GIS). It defines GIS as a system designed to store, manipulate, analyze and display spatially referenced data. The key components of a GIS are hardware, software and data. Common GIS software includes desktop programs like ArcGIS and open-source options like QGIS. GIS can incorporate different types of spatial data like raster, vector and remote sensing data along with associated attribute tables. Example applications discussed are in hydrology, including watershed analysis and flood modeling.
Remote sensing and GIS can be applied in civil engineering for spatial analysis and to answer geographic queries. Spatial analysis examines how the locations of objects impact analysis results and can reveal patterns. GIS uses methods like overlay, proximity, density, and network analysis to study spatial relationships. Common analyses include measuring distances, areas and shapes, transforming datasets, descriptive summaries of data, and optimizing locations.
Presentation: This presentation gives a brief introduction to tools in ArcGIS and was designed for the Surface Water Quality Monitoring (SWQM) GIS training hosted by Texas Commission on Environmental Quality (TCEQ) staff.
Training: The goal of the SWQM GIS training course is to introduce beginner and intermediate GIS users within the TCEQ surface water monitoring network to the geospatial software, skills, analyses, and data most often used by water resource professionals. The training features presentations from a range of GIS experts from TCEQ, TPWD, and other organizations.
More information on the training: https://www.tceq.texas.gov/waterquality/monitoring/training
Digitizing in GIS is the process of converting geographic data either from a hardcopy or a scanned image into vector data by tracing the features. During the digitzing process, features from the traced map or image are captured as coordinates in either point, line, or polygon format.
GIS is a system for managing and analyzing geographic data. It uses two main data models: vector, representing points, lines and polygons; and raster, representing data as a grid of cells. Common file formats include shapefiles for vector data and GeoTIFF and MrSID for raster. GIS data is referenced using coordinate systems like WGS84 for global latitude/longitude or HK80Grid for Hong Kong. ESRI's ArcGIS software allows viewing, editing, and publishing this geospatial data for mapping and analysis.
1. The document discusses various theories related to geomorphology including the Nebular theory of Laplace regarding the origin of Earth, continental drift theory, sea-floor spreading theory and plate tectonic theory.
2. It describes evidence for continental drift including matching coastlines, similarity of rock ages, fossil evidence, and paleoclimatic evidence.
3. Sea-floor spreading theory helped explain mysteries of mid-ocean ridges and trenches observed in sea-floor mapping from the 1940s-1950s through concepts of new crust formation at ridges and destruction of old crust at trenches.
1) The document discusses key concepts in geography including physical geography, human geography, latitudes, longitudes, seasons on Earth, and time zones.
2) It provides summaries of different theories related to the structure and composition of the Earth's interior including the nebular theory of Laplace and evidence from seismic wave studies.
3) The document also summarizes different theories of geomorphology like the continental drift theory, sea-floor spreading theory, and the plate tectonic theory which together explain plate tectonics and the evolution of Earth's surface.
This document provides an introduction to physical geology and important geological concepts. It discusses how geology involves the scientific study of the Earth, including its composition and the forces that cause changes over time. Key topics covered include natural resources, geological hazards, plate tectonics, the layers of Earth's interior, and geological timescales. The theory of plate tectonics explains how the lithosphere is broken into plates that move over Earth's surface and interact at boundaries.
This document provides an introduction to physical geology and important geological concepts. It discusses how geology involves the scientific study of the Earth, including its composition and the forces that cause changes over time. Key topics covered include natural resources, geological hazards, plate tectonics, the layers of Earth's interior, and geological timescales. The theory of plate tectonics postulates that Earth's outer layer is broken into plates that move over time, interacting at boundaries where new crust is formed or plates converge.
The document discusses evidence that supports the theory of plate tectonics and continental drift. It describes how early in Earth's formation, chemical segregation resulted in layers forming within the planet. Later, the nebular hypothesis proposed that planets accreted from a disk of dust and gases orbiting the sun. Evidence like matching fossil distributions, rock formations, and paleoclimate patterns across separated continents supported Alfred Wegener's idea that continents had drifted apart from an original supercontinent. This helped establish the modern theory of plate tectonics.
This document provides an overview of important concepts in geology. It introduces geology as the scientific study of the Earth, including its physical materials and forces that cause changes to its surface and interior. Key practical aspects of geology discussed are natural resources, geological hazards, and environmental protection related to resource extraction. The document also summarizes concepts of Earth's interior structure and heat engines, plate tectonics theory including different plate boundary types, and geological timescales.
This document provides information about plate tectonics and related geological concepts. It begins with an overview of plate tectonics theory, including the three main types of plate boundaries (transform, convergent, and divergent). It then discusses early evidence that supported continental drift, including matching coastlines and shared fossil distributions. Additional sections cover paleomagnetism data, seafloor spreading evidence, characteristics of different plate boundary types, and potential driving forces of plate tectonics like mantle convection. The document concludes by discussing mountain building at plate boundaries and ways plate tectonics may operate on other celestial bodies.
The document discusses the geological time scale and plate tectonics. It describes how the geological time scale is divided into eons, eras, periods, and epochs based on fossil evidence. It then outlines the early development of the continental drift theory and its shortcomings. Finally, it summarizes the current model of plate tectonics, where the lithosphere is divided into plates that move via spreading at mid-ocean ridges, collision at plate boundaries, and sliding at transform faults.
Earth science studies the planet Earth and its place in the universe. It is divided into four categories: geology, oceanography, meteorology, and astronomy. Earth consists of four major spheres: the hydrosphere, atmosphere, geosphere, and biosphere. The geosphere is divided into the core, mantle, and crust. Maps represent Earth's surface and help scientists locate areas using grids of latitude and longitude. Scientists use the scientific method, making hypotheses and analyzing data to understand the natural world.
The document summarizes the theory of plate tectonics. It discusses how early scientists like Wegener proposed the idea of continental drift and Pangaea. Later evidence from mapping ocean floors and magnetic stripes on ocean crust supported sea floor spreading and plate tectonics. The theory states the earth's outer layer is divided into plates that constantly move via three types of boundaries: divergent where plates move apart, convergent where they push together, and transform where they slide past each other. The movement of plates like India colliding with Asia helped form features like the Himalayas.
AS Level Physical Geography - Rocks and WeatheringArm Punyathorn
The earth's surface is an ever-changing entity. With the forces of weather and climate and tectonic variability, the rocks and minerals that make up the earth are always changing in size, shape and forms - a fascinating, ancient, never-ending process.
The document provides an overview of key concepts in geology, including:
1) The Earth is composed of spheres (atmosphere, hydrosphere, biosphere, lithosphere, interior) that interact and influence each other through geological processes over time.
2) Plate tectonics theory revolutionized geology by providing a framework for understanding phenomena on a global scale and interpreting Earth's history.
3) The rock cycle and geological forces transform rocks from one type to another, with igneous, sedimentary, and metamorphic rocks forming through melting, deposition, and changes wrought by heat and pressure.
The presentation contains basic terms of Physical Geology which is related to Geology. It is a gross presentation including images and animated gif's for better understanding.
1. The document outlines an Earth and Life Science curriculum for Grade 11 covering topics in Earth Science, Geology, Meteorology, and Astronomy.
2. It includes pre-tests on the solar system, planets, and the Big Bang theory. Activities include a jumbled words exercise and an origins of the universe quiz.
3. The curriculum will examine theories on the origins of the solar system and universe such as the nebular hypothesis and provide assignments on the fate of the universe and possibility of finding Earth-like exoplanets.
This document provides information about plate tectonics and the dynamics of the Earth. It discusses key topics such as continental drift, Earth's layered structure, types of plate boundaries including convergent, divergent and transform boundaries, seafloor spreading, plate motions, and forces driving plate tectonics. The objectives are to understand concepts like continental drift, Earth's structure, plate margins, seafloor spreading, how plates move on the surface of the sphere, and driving forces. Diagrams and figures are included to illustrate these topics.
1. Plate tectonics theory explains that the Earth's lithosphere is divided into tectonic plates that move over the asthenosphere due to convection currents in the upper mantle.
2. Rates of plate movement can be measured using techniques like analyzing magnetic anomalies in seafloor crust or dating rocks near hotspots.
3. Plate tectonics is responsible for phenomena like volcanism, earthquakes, and mountain building and has influenced the global distribution of life and natural resources over geological time.
Geologists have learned about Earth's interior through examining rock samples and studying seismic waves. Temperature and pressure both increase with depth inside Earth. The crust and mantle are divided into layers with different physical properties. Convection currents in the mantle are driven by heat from the core and cause the tectonic plates to slowly move over time. The theory of plate tectonics explains how new crust forms at mid-ocean ridges and old crust is recycled into the mantle at subduction zones, causing the plates to drift apart or collide together over hundreds of millions of years.
The document discusses plate tectonics and the evidence that supports the theory. It describes how Alfred Wegener first proposed continental drift in 1912 and how scientists later discovered seafloor spreading at mid-ocean ridges. The theory of plate tectonics emerged, stating that the Earth's lithosphere is broken into plates that move over the asthenosphere. The boundaries between plates can be divergent, convergent, or transform. Plate motions are driven by convection currents in the Earth's mantle.
This document provides an overview of plate tectonics and the key individuals and discoveries that led to the development of the theory. It discusses Alfred Wegener's idea of continental drift in the early 20th century, which was initially rejected. It then covers the discoveries of the mid-ocean ridge system and magnetic striping of the ocean floor in the 1950s-60s, which provided evidence that the continents are moving and new crust is generated at ocean ridges through seafloor spreading. This led to the acceptance of plate tectonics as a scientific theory to explain geological phenomena.
How to Make a Field Mandatory in Odoo 17Celine George
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
LAND USE LAND COVER AND NDVI OF MIRZAPUR DISTRICT, UPRAHUL
This Dissertation explores the particular circumstances of Mirzapur, a region located in the
core of India. Mirzapur, with its varied terrains and abundant biodiversity, offers an optimal
environment for investigating the changes in vegetation cover dynamics. Our study utilizes
advanced technologies such as GIS (Geographic Information Systems) and Remote sensing to
analyze the transformations that have taken place over the course of a decade.
The complex relationship between human activities and the environment has been the focus
of extensive research and worry. As the global community grapples with swift urbanization,
population expansion, and economic progress, the effects on natural ecosystems are becoming
more evident. A crucial element of this impact is the alteration of vegetation cover, which plays a
significant role in maintaining the ecological equilibrium of our planet.Land serves as the foundation for all human activities and provides the necessary materials for
these activities. As the most crucial natural resource, its utilization by humans results in different
'Land uses,' which are determined by both human activities and the physical characteristics of the
land.
The utilization of land is impacted by human needs and environmental factors. In countries
like India, rapid population growth and the emphasis on extensive resource exploitation can lead
to significant land degradation, adversely affecting the region's land cover.
Therefore, human intervention has significantly influenced land use patterns over many
centuries, evolving its structure over time and space. In the present era, these changes have
accelerated due to factors such as agriculture and urbanization. Information regarding land use and
cover is essential for various planning and management tasks related to the Earth's surface,
providing crucial environmental data for scientific, resource management, policy purposes, and
diverse human activities.
Accurate understanding of land use and cover is imperative for the development planning
of any area. Consequently, a wide range of professionals, including earth system scientists, land
and water managers, and urban planners, are interested in obtaining data on land use and cover
changes, conversion trends, and other related patterns. The spatial dimensions of land use and
cover support policymakers and scientists in making well-informed decisions, as alterations in
these patterns indicate shifts in economic and social conditions. Monitoring such changes with the
help of Advanced technologies like Remote Sensing and Geographic Information Systems is
crucial for coordinated efforts across different administrative levels. Advanced technologies like
Remote Sensing and Geographic Information Systems
9
Changes in vegetation cover refer to variations in the distribution, composition, and overall
structure of plant communities across different temporal and spatial scales. These changes can
occur natural.
How to Build a Module in Odoo 17 Using the Scaffold MethodCeline George
Odoo provides an option for creating a module by using a single line command. By using this command the user can make a whole structure of a module. It is very easy for a beginner to make a module. There is no need to make each file manually. This slide will show how to create a module using the scaffold method.
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How to Add Chatter in the odoo 17 ERP ModuleCeline George
In Odoo, the chatter is like a chat tool that helps you work together on records. You can leave notes and track things, making it easier to talk with your team and partners. Inside chatter, all communication history, activity, and changes will be displayed.
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
2. Study material
ATLAS
• Orient Longman
• Study publication – India
and world
• Oxford publication
Book list
• Goh Cheng Leong
• Physical Geography – by
Savinder singh
• India: comprehensive
geography by D.R. Khullar
4. Meaning and span of Geography
• Geo= earth and Graphy = study,
which means study of earth
• Geography can be divided into two
parts:
• Physical geography and Human
geography
5. Two Parts of Geography
Physical
• Landforms
• Atmosphere
• Hydrosphere
• Biosphere
Human
• Habitation
• Population
• Agriculture
• Industries-
resources
8. Latitudes
• Largest latitude –
equator
• Tropics – heat
surplus
• Temperate, polar
regions – heat
deficit
• Responsible for
pressure system
and planetary
wind system
10. Q. Who among the following was
first to state that Earth was
spherical?
A. Aristotle
B.Copernicus
C.Ptolemy
D.Strabo
UPSC Prelims 2001
Correct Answer is A
13. Prelims
2013
Q. Variations in length of
daytime and night-time from
season to season are due to
a) Earth’s rotation on its
axis
b) Earth’s revolution
around the sun in an
elliptical manner
c) Latitudinal position of
the place
d) Revolution of earth on a
tilted axis
UPSC
Question
14. Prelims
2013
Variations in length of
daytime and night-time from
season to season are due to
a) Earth’s rotation on its
axis
b) Earth’s revolution
around the sun in an
elliptical manner
c) Latitudinal position of
the place
d) Revolution of earth on a
tilted axis
UPSC
Question
16. Longitudes
• Angular distance of
a place from prime
meridian
• Also called
meridians
• 0 degree =
Greenwich in UK
• 180 degree =
International date
line
21. Standard time
1) Every country selects its standard
meridian.
2) Angular distance between standard
meridian of a nation to Greenwich
meridian time (GMT)
23. British launched
Chaibagaan time (1 hr
ahead of IST) 150 years
ago in Assam
After independence –
rejected
2007 DST study –
rejected – admin
challenges
Jan 2014 CM of Assam –
declare to apply
Chaibagaan time
Chaibagaa
n time zone
IST
25. If 12 noon at GMT what
is the time at 75 °E?
• Difference = 75 °
• 15 ° => 1 hour
• 75 ° => 5 hours
• East (means add) 12
+5 = 5 pm
Time
zones
Question
26. If 12 noon at GMT what
is the time at 30 °W?
• Difference = 30 °
• 15 ° => 1 hour
• 30 ° => 2 hours
• East (means minus)
12 - 2 = 10 am
Time
zones
Question
27. Prelims
1999
Q. If it is 10.00 am IST,
then what would be the
local time at Shillong on
92 deg E Longitude?
a) 9.38 am
b) 10.38 am
c) 10.22 am
d) 9.22 am
Ans. B)
UPSC
Exercise
28. Prelim
s
2006
Q. Through which one of the
following groups of countries
does equator pass?
a) Brazil, Zambia and
Malaysia
b) Columbia, Kenya and
Indonesia
c) Brazil, Sudan and
Malaysia
d) Venezuela, Ethiopia and
Indonesia
UPSC
Exercise
29. Prelims
2008
Q. Which of the
following cities is
nearest to the equator ?
a) Colombo
b) Jakarta
c) Manila
d) Singapore
UPSC
Exercise
30. Prelims
2008
Q. Which one of the
following straits is
nearest to the
International Date Line?
a) Malacca Strait
b) Bering strait
c) Strait of Florida
d) Strait of Gibraltar
UPSC
Exercise
34. Prelims
2009
Q. Consider the
following countries:
1. Australia
2. Namibia
3. Brazil
4. Chile
Through which of the
above does the Tropic of
Capricorn pass?
UPSC
Exercise
38. Origin of the Earth
Nebula Theory
Theory of Laplace
Overview
Geomorpholo
gy
39. Origin of earth – Nebular theory of
Laplace
Gaseous cloud
of H, He –
radiation –
cooling-
Contracting
• Separation of
outer ring – 9
parts => 9
planets
40. Nebular Theory of Laplace
• Heavier
elements near
the core and
lighter at the
surface
• Layered
structure of
earth’s
interior
41. 1. Density study:
2. Temperature study
3. Structural study
- Direct evidences
- Indirect evidences
Interior of
the Earth
Geomorpholog
y
42. Edward Suess
• Outer layer
(continents)– SIAL
• Mantle and oceanic
crust – SIMA
• Core – Ni +Fe
43. Seismic wave studies
• Seismic waves = mechanical waves =
require medium for propagation
• Their behaviour changes with changes of
medium
• 2 imp waves: primary P and secondary S
waves
• S waves can travel into only S and G
medium
• P can travel in all 3 mediums
• But speed is highest in S>L>G
50. formed due to
solidification of magma
(Interior) or lava
(Exterior)
They don’t have strata or
layers
Because entire lava is
solidified
They are crystalline
They don’t have fossils
Igneous
Rocks
Rock
Types
51. formed due to
lithification of soil
erosion of rocks =>
deposition of granules
=> compaction =>
lithification
Always stratified
They may have fossils
Sedimentary
rocks
Rock Types
52. Metamorphosed rocks
• both igneous and sedimentary rocks
changed under heat or pressure or
both
• No fossils
• No stratification
53. Examples of metamorphosed rocks
gneiss
Granite
Marble
Limestone
quartzite
Sandstone
Slate/ schist
Clay/muds
tone
54. Prelims
2001
Consider the following
statements made about
sedimentary rocks:
1. Sedimentary rocks are
formed at earth’s surface by
hydrological system
2. Formation of sedimentary
rocks involves the
weathering of pre-existing
rocks
3. Sedimentary rocks contains
fossils
4. Sedimentary rocks occur in
layers
UPSC
Question
56. Interior of the earth
Different layers – structure and
composition
Rocks
Properties of rocks
57. Geological time scale of Earth
years Eon Era Importanc
e
4.6 -3.5
billion
Pre-
Cambrian
Proterozoic No Life
3.5 -2.5
billion
Archean 1st life form
2.5 to 545
million
Hadean 1st fish
eveloved
58. Geological time scale of the Earth
Years Eon Era Period Epoch Importan
ce
545 ml –
245 ml
Phaneroz
oic
Paleozoic Carbonife
rous
Coal
245 ml-65
ml
Mesozoic Triassic,
Jurassic,
Cretaceou
s
Reptiles
=>
Dinosaur
s =>
extinct
65 ml –
present
Cenozoic tertiary Oiligocene
,
Pliocene
Birds and
mammals
65000
years
quaternar
y
Holocene Human
74. Main
s
2013
What do you understand
by theory of continental
drift? Discuss the
prominent evidences in its
support. (5)
UPSC
Question
75. Preli
ms
2014
Q. Which of the following
phenomena might have
influenced the evolution
of organisms?
1. Continental drift
2. Glacial cycles
Ans. Both
UPSC
Question
76. Arthur Holmes
• Arthur Holmes:
• Convection current
theory
• Convection cells – force
behind drifting of
continents
78. Sea-floor mapping
• During 1940s
and 1950s
• Diversity of
ocean-floor
• Submarine hills
– guoyts – MOR
–Trench
79. Ocean floor mapping
Questions:
1) Ocean crust
not older than
mid-Mesozoic
2) Age increase
away from MOR
3) Sea-mounts
deformed at
trenches
80. Sea floor spreading Theory
• 1960s Harry Hass and Dietz answered
question regarding ocean mapping using
convection theory
• revealed mystery of mid-oceanic ridge and
trenches
83. MOR
• Rising limb of current breaks the Ocean crust
• Basaltic eruption
• Accumulation of lava – ridge => MOR
• New Oceanic crust
• Divergent limb – expansion of ocean crust
85. MOR - Trench
• At trench Ocean floor
destroyed – melted in
mantle
• Oceanic crust heavier
than continental crust
• Ocean floor act like
conveyor belt
• Ocean floor – cyclic
process – 300 ml yrs
87. Prelims
2006
Q. In which one of the
following oceans the
Diamantina Trench is
located?
a) Pacific Ocean
b) Atlantic Ocean
c) Indian Ocean
d) Arctic Ocean
Ans. C)
UPSC
Question
89. Palaeo-magentism
• Magnetism of rocks
along MOR
• Magnetometer -
Magnetic parallel
stripes– normal and
reverse magnetic
profile
• 1st Carlsberg ridge –
Indian ocean
90. Palaeo-magentism
• Vine and mattheus
• Molten lava get polarity
geomagnetic field of
that period -Solidify
• Ocean floor – magnetic
tape
91. Palaeo-magnetism
conclusion
1) Periodic reversal of magnetic field of the
earth
2) Rate of sea-floor spreading decided by age +
distance between two equal magnetic stripes
• Atlantic – 1.0 cm/ year
• Indian – 1.5 cm/year
• Pacific – 6.0 cm/year
92. Prelims
2011
Q. Between India and East
Asia, the navigation time
and distance can be greatly
reduced by which of the
following?
a) Deepening Malacca strait
between Indonesia and
Malaysia
b) Opening a new canal
across Kra Isthmus
between gulf of Siam and
Andaman sea
UPSC
Question
World Geography:
Asia= China, Japan, South East Asia, West Asia
Europe = UK, Russia, Germany-France, Eastern Europe
North America = USA, Canada
South America and Africa