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What is GIS

Course: GGS 311, Fall 2011
School: George Mason
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Information Geographic System Geographic Information System Geographic (GIS) ((GIS) (GIS) GIS) What is GIS? Think About Geography Think About Geography Think What is Geography? Association of American Geographers definition: Geography is the science of place and space Merriam-Websters definition: A science that deals with the description, distribution, and interaction of the diverse physical, biological, and...

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Information Geographic System Geographic Information System Geographic (GIS) ((GIS) (GIS) GIS) What is GIS? Think About Geography Think About Geography Think What is Geography? Association of American Geographers definition: Geography is the science of place and space Merriam-Websters definition: A science that deals with the description, distribution, and interaction of the diverse physical, biological, and cultural features of the earths surface Think About Geography Think About Geography Think Questions Geographers Ask Where is it located? Why is it located there? How and why are places different? How do people interact with their environment? The answer to these questions is spatial data History of Cartography History of Cartography History The First Maps Rock walls Clay tablets Uses of Maps Topographic Celestial Cosmographic Picture of a cuneiform tablet from http://www.crystalinks.com/cuneiformtablets.html Early Maps of the World Early Maps of the World Early Picture of a T-O map from University of Texas, Foundations of Western European Cartography Exploring the World Exploring the World Exploring Mercator map picture from Encyclopedia Britannica. Maps at War Maps at War Maps Topographic map picture of Harpers Ferry from www.DavidRumsey.com. Linked information reveals patterns Linked What is Spatial Data? What is Spatial Data? What Location Data How Many? What Kind? Where? Scale of Data Local to Global to Beyond Data Presentation Words, Charts, Graphs, Tables, or Maps Estimates are that 80% of all data has a spatial Estimates spatial 80% component component Data from most sciences can be analyzed spatially spatially Geographic Information Systems Geographic Information Systems Geographic A Definition of GIS A Definition of GIS Definition Definition A Geographic Information System (GIS) links locational and Geographic attribute information and enables a person to visualize patterns, relationships, and trends. This process gives an entirely new perspective to data analysis that cannot be easily seen in a table or list format or on a paper map. Exploring data using GIS turns data into information into knowledge Five Components of GIS Five Components of GIS Five Hardware Hardware The computer, peripherals, and sometimes servers on which the GIS operates Software Provides the functions and tools required to store, analyze, and display data Data Data is stored as vector, raster, or attribute data Methods The guidelines, specifications, standards, and procedures for collecting and analyzing data and applying GIS People GIS needs people to ask the questions; choose, collect, and analyze the data; and interpret the results A Complete GIS A Complete GIS Complete Visualization GIS as a tool to display spatial data as a map Database Management GIS as a tool to store and organize spatial data Spatial Analysis GIS as a tool to analyze and interpret spatial data GIS Combines Spatial Data From Many Sources GIS Combines Spatial Data From Many Sources GIS Sources of Spatial Data Sources of Spatial Data Sources Digitized and Scanned Maps Purchased, donated, free (Internet) Created by user Databases Tables of data GPS Global Positioning System Accurate locations Field Sampling of Attributes Remote Sensing and Aerial Photography GIS stores and organizes spatial data in databases Database Database Database Not easy to interpret Not easy to interpret Visualization Visualization Visualization Worth a Thousand Words Worth a Thousand Words Two Ways to Visualize Data Two Ways to Visualize Data Two The World in GIS The World in GIS Raster -- Grid Pixels A location and value Satellite images and aerial photos are already in this format Vector -- Linear Real world Points, lines, and polygons Features (house, lake, etc.) Attributes size, type, length, etc. Five Data Layers Five Data Layers Alike Features Alike Features Rivers Layer Rivers Roads Layer Lakes Layer Capitals Layer States Layer Turning Data Into Information Turning Data Into Information Turning SpatialAnalysisNotJustaMap Asking a Question -- Interaction Asking a -- Question Interaction Asking Maps and Databases are Interactive Maps and Databases are Interactive Maps The Goal of GIS The Goal of GIS The The goal of GIS is to help people and companies do their work better, faster, and cheaper through better faster cheaper Visualization Visualization GIS provides users with quicker, more accurate representations of spatial data Database Management GIS makes it easier to keep the spatial data accurate and up to date Spatial Analysis GIS helps users make more informed decisions *Wherever Spatial Data Analysis Is Needed* Some Ways GIS is Used Some Ways GIS is Used Some Emergency Services Fire and Police Environmental Environmental Monitoring and Modeling Business Site Location, Delivery Systems Industry Transportation, Communication, Mining, Pipelines, Healthcare Government Government Local, State, Federal, Military Education Research, Teaching Tool, Administration Defense Management Defense Management Defense Real Estate Management Real Estate Management Real Education Education Education Utility Management Utility Management Utility Transportation Management Transportation Management Transportation Public Safety Public Safety Public Government Government Government Hospital Facilities Hospital Facilities Hospital GIS on the Internet GIS on the Internet GIS National Atlas http://nationalatlas.gov National Geographic Map Machine http://www.nationalgeographic.com/mapmachine Store Locator http://www.godiva.com Wildlife Finder http://www.worldwildlife.org/wildfinder GIS Info http://www.gis.com ESRI ESRI ESRI ESRI provides our users with a complete GIS complete Visualization Database Management Spatial Analysis ESRI offers more than just GIS software. We offer solutions. Our goal is to make our users more successful ESRI ESRI ESRI 40 Years of Experience Annual Revenues of $660 Million The Fifth Largest Privately Held Software Company in the World 350,000+ Clients of ESRI Software More Than One Million Users ESRI Regional Offices and International Distributors ESRI Regional Offices and International Distributors ESRI Headquartered in Redlands, California 10 Domestic Regional Offices International Distributors in More Than 80 Countries Users in More Than 150 Countries ArcGIS Family of Products ArcGIS ArcGIS Server Platform Desktop Author/Serve/Use Maps Data Explorer Web Map Viewer Mobile Open APIs Enterprise Environment Us e Models Globes Metadata Serv e ArcGIS Server Autho r Making GIS Knowledge Available To Anyone . . . . . . Integrates With Other Systems Via Standards Integrates Sharing GIS With Others Sharing GIS With Others GIS is a new medium for communication GIS Newspapers Radio Television Internet GIS GIS helps people to Better understand and collaborate Tell stories about conditions, situations, and events Forecast the future Sharing GIS With Others GIS Day Sharing GIS With Others GIS Day What Is GIS Day? What International grassroots event to provide education about the power and functionality of GIS Builds GIS understanding and collaboration in organizations, schools, and communities When To Participate? Third Wednesday in November each year (held in conjunction with National Geographic Societys Geography Awareness Week) November 19, 2008 marks the tenth annual celebration GIS Day events are held throughout the year! GIS Day GIS Day How Do I Participate? How Host an Event (open house, workshop, demonstrations, press events) Teach a Class Solicit Proclamations Mentor Students Conduct Webcasts ...the possibilities are endless ...the GIS Day GIS Day Why Participate? Why Promote your organizations use of GIS Introduce GIS to new prospects, internal and external audiences Build community understanding of the value of GIS Participate in GIS educational initiatives and community service projects Establish mentor relationships with local youth and expose students to cutting edge technology and career options Market GIS to potential clients GIS Day GIS Day Visit www.gisday.co m for more information and to register your event!
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George Mason - GGS - 311
Final Examination Study Sheet GGS 311: Introduction to Geographic Information Systems Dr. Matt Rice, Fall 2011 Geographic Data Modeling Longley, chapter 8 GGS-311_-_Lecture6.ppt 1) Definition of a Data Model
George Mason - GGS - 311
GGS 311: Introduction toGeographic InformationSystemsChapter 5: GeoreferencingDr. Matt RiceGeorge Mason UniversityFall 2011IntroductionLongley et al., Chapter 5 Learning Objectives: Learn the requirements for an effective system ofgeoreferencin
George Mason - GGS - 311
Geographic Data ModelingLongley Chapter 8Dr. Matt RiceGeography and GeoinformationScience 311Fall 2011Outline Definitions Data models / modeling GIS data models Topology Example Water facilitiesDefinitions Data model set of constructs for r
George Mason - GGS - 311
Cartography and MapProductionLongley Chapter 12Dr. Matt RiceGeography and Geoinformation Science 311Fall 2011Outline Nature of maps and cartography Principles of map design Composition Symbolization Map series Applications ConclusionsIntrodu
George Mason - GGS - 311
Accuracy & UncertaintyMatt RiceGGS 311 - GMUFall 2011NationalMapPublished byAccuracyUSGSStandardshttp:/egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US%20NationalHorizontalaccuracyFor maps onpublicationNationalMapPublished byAccuracyU
George Mason - GGS - 311
Web GIS / Future of GISDr. Matt RiceGeography and Geoinformation Science311Fall 2011Overview:Future of GISGIS software architectureDataLegal Issues and IPPrivacyPanoramic Map of EurekaCalifornia (l890 1910) availablethrough the Library of Con
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATION SCIENCE 311 INTRODUCTION TO GEOGRAPHIC INFORMATION SYSTEMS Instructor: Dr. Matt Rice Term: Fall 2011 Classroom: Innovation Hall, room 222 Classtime: (GGS 311003: CRN 75396), Tuesday 4:30pm
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATIONSCIENCE 311INTRODUCTION TO GEOGRAPHICINFORMATION SYSTEMSInstructor: Dr. Matt RiceFaculty Office: Research Building I, Room 242Faculty Office Hours: Wednesday, 11:00am-1:00pm or by appointmentEmail: rice@gmu.eduFaculty web
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATIONSCIENCE 311INTRODUCTION TO GEOGRAPHICINFORMATION SYSTEMSInstructor: Dr. Matt RiceFaculty Office: Research Building I, Room 242Faculty Office Hours: Wednesday, 11:00am-1:00pm or by appointmentEmail: rice@gmu.eduFaculty web
George Mason - GGS - 311
GIS Data CollectionLongley, chp. 9Dr. Matt RiceGeorge Mason UniversityFall 2011OverviewIntroductionPrimary data captureSecondary data captureData transferCapturing attribute dataManaging a data capture projectData CollectionOne of most expens
George Mason - GGS - 311
Data Collection TechniquesRasterVectorSecondaryDigitalremotesensingimagesGPSmeasurementsDigitalaerialphotographsPrimarySurveymeasurementsScannedmapsTopographicsurveysDEMsfrommaps ToponymydatasetsfromatlasesPrimary Data CaptureCapture sp
George Mason - GGS - 311
GGS 311 Introduction to GIS Dr. Matt Rice Midterm Exam Study Sheet Fall 2011 1) Read Chapters 1, 7, 5, 3, 9 completely and pay attention to the bold points they are probably going to appear on the exam, p
George Mason - GGS - 311
GGS 311: Introduction to Geographic InformationSystemsChapter 3: RepresentingGeographyDr. Matt RiceGeorge Mason UniversityFall 2011QuestionWhat coordinate system are theseunits likely associated with?621,161 m E3,349,894 m NUTM?PLSS / Townshi
George Mason - GEOL - 102
2/25/11Archean Eonand the Solar System87% of the Earths history is inthe Precambrian!A little background before weget to the Earthmore background All of the planets were formed around thesame time (~4.7bya). They are formed from the same materia
George Mason - GEOL - 102
ArcheanRemember Precambrian time includes 80% of theearth's history, from 4.5 byr - 700 myr. So for the first 500 myr there is nogeologic record. Original crust was thin and composed mainlyof komatite & basalt. Granites have formed from basalts fr
George Mason - GEOL - 102
Cenozoic EventsCenozoic periodEocene and ModernCenozoic Half of the present sea floor was formedsince the end of the Cretaceous! Atlantic and Indian rifting had increased.East CoastFlorida region Erosion is still dominant. Passive margins. Carb
George Mason - GEOL - 102
4/22/11Cenozoic LifeCenozoicEVIDENCE FOR CENOZOICCLIMATE CHANGE Remember in the Cretaceous, climateswere much warmer than today. Although the oceans and atmosphereare affected by the K/T boundary theclimate soon returned to its greenhousestate i
George Mason - GEOL - 102
2/4/11EVOLUTIONLife on EarthTypes of fossilization, againPermineralizationReplacementCarbonizationMolds/casts steinkern Amber Trace fossils Tracks, trails, and burrowsPermineralization Original pore spacesare permeated withgroundwater. Min
George Mason - GEOL - 102
Geologic Time ScalePERIODEPOCHHoloceneNeogeneTertiaryPliocenePaleogenePleistoceneOligoceneMioceneEocenePaleocene0.011.65.323.736.657.8Mesozoic66.4Cretaceous144Jurassic208Triassic245CarboniferousPermianPaleozoicPhanerozoicCen
George Mason - GEOL - 102
Historical GeologyFinal ReviewSpring 2011Current eventsExtinctionKnow 5 largest extinction eventsPermian and Cretaceous extinction eventsMesozoic Tectonics Chapter 13Breakup of PangeaKnow ages of rifting eventsPalisades & Newark formationsDinos
George Mason - GEOL - 102
GeologicTime Scaleagain!Time & GeologyTime v Rock DivisionsEonEraPeriodEpochAgeRock versus TimeEonothemErathemSystemSeriesStageEvolution of geologic time scaleSedgwick and Murchison1Lithology denesComposition of mineral grainsColorTe
George Mason - GEOL - 102
HISTORICAL GEOLOGYGEOLOGY 102, section 002Spring, 2011Instructor: Dr. Stacey Verardosverardo@gmu.edu, 703-993-1045Class hours: Tuesdays and Thursdays 1:30 -2:45pmOffice: David King Hall Room 3037Office Hour: Thursdays, 11am -noonClassroom: Enterpr
George Mason - GEOL - 102
Early ManPrimate groups Prosimmii Tree shrews, lemurs, tarsiers Often nocturnal Anthropoidea Monkeys, apes, humansProsimii & AnthropoideaEarliest primates -Prosimian The earliestrelatives of theprimates werefound in theMesozoic andare simila
George Mason - GEOL - 102
IntroductionTime scaleTime scaleTaxonomicclassicationThis is theversion thatyou will bequizzed on.kingdoms1Factors for fossilization Rapid burial is the best way for successfulfossilization. Most often occur in shallow water with highenergy
George Mason - GEOL - 102
1/18/11HISTORICALGEOLOGYGeology102SowhatisthedierencebetweenGEO101andGEO102? InthisclassyouwilllearnoftheoriginoftheearthandtheevoluJonoftheland,atmosphereandallofitslife. AndthisiswhereyoullneedtolearntheGeologicTimescale. Therewillbeaquizonito
George Mason - GEOL - 102
4/10/11Mesozoic LifeAfter Permian extinction Seas were dominated by an abundance ofmollusks, sea urchins, crustaceans and sh& reptiles. On land, synapsids were replaced byreptiles. crocodiles, turtles, snakes, lizards and dinosaursMesozoicevents
George Mason - GEOL - 102
Mesozoic tectonicsMesozoic era -55-250myrThe breakup of PangaeaRepresents a change tectonically fromcompressional mountain building in theeast and northern parts of the continentto compressional forces on the westernmargin.What was happening ? La
George Mason - GEOL - 102
Rodinia was rifting apartEarly PaleozoicCambrian-SilurianLaurentiaBalticaKazakhstaniaSiberiaChinaGondwana Iapetus Ocean openthen closedRODINIA to PANNOTIANorth America & EuropeCambrianto SilurianDomes and basins1Vendian to OrdovicianCrat
George Mason - GEOL - 102
Late Paleozoic TectonicsLate Paleozoic 410-250 million years ago. Divided into Devonian, Carboniferous,Permian. By the Permian Pangea was assembled. During this time Acadian & Caladonian orogenies Alleghenian & Hercynian orogeniesLatePaleozoicP
George Mason - GEOL - 102
Paleozoic LifeEarly life Fossil record increases with increase infossil hard parts. Vertebrates evolve. Animals move onto land. Vascular plants show up. Also largest mass extinction EVER.Precambrian-Cambrian Invertebrate phylaEarly Cambrian foss
George Mason - GEOL - 102
2/11/11Plate TectonicsJOIDES resolutionP-wavesEARTHQUAKE WAVES P-waves S-waves Surface waves/Long wavesS-waves Oscillate back and forth perpendicular to the directionof wave travel. Change shape of rock. Only in solids. Cause strong movement
George Mason - GEOL - 102
PLEISTOCENE EPOCH1.7myr7 kyr agoExtent of ice during LGMevidenceAn Alps region glaciated valley In 1836 Louis Agassiz, apaleontologist, began to believe thatthe glaciers in the Alps were oncemuch more extensive than today.Glaciated EuropeChanges
George Mason - GEOL - 102
3/3/11Proterozoic2.5bya-540myaProterozoic compared to Archean. Proterozoic has a more modern type ofplate tectonics, sedimentation, and climate. First major Wilson cycle. First large ice age most of Earth cooled. Most BIFs. 42% of Earths history!
George Mason - GEOL - 102
Rocks & MineralsCriteria to be a mineral Occurs naturally as an inorganic solid. Has a specic internal structure. Has a specic chemical composition can exchange occasionally. Has specic physical properties. Minerals can be composed of one element
George Mason - GEOL - 102
Sedimentary ArchivesWhat determines which type ofsedimentary rock forms indifferent environs?Sedimentary EnvironmentsTectonic settingType of rock being weatheredType of transportClimateAmount of pressure & temperatureTimeSedimentary Environment
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam OneSpring 2011Know the TIME SCALEKnow current eventsScience of Historical GeologyChapter 1Scientific MethodUniformitarianismThe 6 KingdomsTaxonomic ClassifiicationsTypes of FossilizationPermineralization
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam TwoCURRENT EVENTSArchean and the Solar System -chapter 8Archean most of Earths History4.6 bya to 700 mya80% of Earths historySolar Nebular HypothesisKnow the planets!Terrestrial & GaseousMeteorites, Astero
George Mason - GEOL - 302
American Mineralogist, Volume 93, pages 16931720, 2008Review PaPeRMineral evolutionRobeRt M. Hazen,1,* DoMinic PaPineau,1 wouteR bleekeR,2 RobeRt t. Downs,3JoHn M. FeRRy,4 tiMotHy J. Mccoy,5 DiMitRi a. sveRJensky,4 anD Hexiong yang3Geophysical Labora
George Mason - GEOL - 306
Thevesoilformingfactors AllinteracttoformthedierenttypesofsoilThevesoilformingfactors Parentalmaterial Canberock Bedrock Residualsoils Transportedmaterialnotinplace TransportedsoilsThevesoilformingfactors LimestonesandstonebasaltThevesoilform
George Mason - GEOL - 306
CATION EXCHANGECAPACITYCLAY MINERALSAnd clay sized fractionThe very very smallveryKaolinite a clay mineral stacks ofhexagonalsheets shownhere are acharacteristicof many clayminerals. Bar is 50m1/1,000,000 m 1/1000 mmhttp:/www.reading.ac.uk
George Mason - GEOL - 306
soilorganicsSpodosolMyakka.TheOcialStateSoilofFloridaAEBhCarbon(cyclelater) dominantlyaddingCtothesoil soweretalkingmoreabouttheupperhorizonAofthesoildominantly.SOMsoilorganicmaFer OrganicmaFerisessenGaltoproducGvesoils improvesphysicala
George Mason - GEOL - 306
MacronutrientsNitrogenxingnodulesh4p:/blog.lib.umn.edu/denis036/thisweekinevoluAon/2007/08/cooperaAon_gets_complex_1.htmlESSENTIALELEMENTS Wearelearningthatsoilsareverycomplexmedium manyreacAonsoccurring thesystemasawholeinaconstantstateofux.Add
George Mason - GEOL - 306
Soil in the newsSome bad- But also some good thingsThe future rests on the soilbeneath our feet.http:/s.ngm.com/2008/09/soil/img/soil-615.jpgPopulation factsPopulationPopulation The world's population will reach 7billion people late this year, a
George Mason - GEOL - 306
SOILORGANICMATTERSOMPeatIsleofLewis,ScotlandSOM EspeciallyinOandA Nutrients Importantfor Supportmicroandmacroorganisms CEC TheyarepartofSOM Holdingwater Tilth. FormaGonofpedsstructure MostofthisnextweekCarboncycle Wewillcoverthisnextweek
George Mason - GEOL - 306
AGoodrichsoilneeds Soil acomplex,breathingen8ty Soil Plants chemistry9macronutrients Neededforplantstogrow C,H,O,N Crucial96%ofaplant K,Ca,Mg,P(phosphorus)S(sulfur)7micoelements Fe,Cl,Mn(Manganese),B(Boron),Cu,Mo(Molybdenum),Zn Lessthan0.010
George Mason - GEOL - 306
SoilPhysicalproper/es.SoilsamplingSoilsampling EarthDay2007 Sunnyside therepresenta5vesoilfortheDistrictofColumbia U.S.Na5onalArboretum.SoilsamplingSoil TextureSoil Texture = %Sand, Silt & Clay in a soil. Soil texture is the single most impor
George Mason - GEOL - 306
GEOLOGY306SOILSCIENCESPRING2011http:/mason.gmu.edu/~jnord/geol306/PREREQUISITE GEOL 101 and CHEM 103 or 211CLASS MEETS Monday 4:30 p.m. to 7:10 p.m. - Enterprise Hall 276Dr. Julia Nord, 3055 David King HallINSTRUCTOREmail Address - jnord@gmu.eduOF
George Mason - GEOL - 306
Soil Taxonomy- more detailsPurpose of Soil Taxonomy:1. Organize knowledge about soils2. Understand relationships among different soils3. Establish groups or classes for practical purposes.a. predicting behaviorb. identifying best usesc. estimating
George Mason - GEOL - 306
Soil solution- Not pure waterWater striderHydrological cycle water in living thingsImportance to plants Maintain turgidity Carry dissolved nutrients Required for Ps Lost in transpiration to cool plant and keep nutrients moving upImportance to p
George Mason - GEOL - 306
ROCKCYCLEIGNEOUSROCKGraniteh*p:/web.uct.ac.za/depts/geolsci/dlr/rocks/gran9.jpg VIOOLSDRIFBATHOLITHSAA1900Ma ADAMELLITE(TwoFeldsparGranite):Orthoclase(phenocrysHc)PlagioclaseQuartzBioHteMagneHteROCK asolidaggregateofoneormoremineralsormineralli
George Mason - GEOL - 306
SEDIMENTARYROCKSWhiteClisofDover(chalk)h5p:/cache.eb.com/eb/image?id=74594&rendTypeId=4RockcycleWEATHERING producessolidparKcles (primaryandsecondary) +ionsinsoluKonTRANSPORTATION movessolidparKcles (primaryandsecondary) +ionsinsoluKonDEPOS
George Mason - GEOL - 306
TwelveSoilordersPicturesfromNRCSNaturalResourcesConserva8onServiceh:p:/soils.usda.gov/technical/classica8on/orders/En8solrecentSoilsthathaveli:leornoevidenceofdevelopmentofpedogenichorizons.Manyaresandyorveryshallow.MountainsetcIncep8solL.Incept
George Mason - GEOL - 306
ROCKCYCLEWEATHERING thephysicalbreakdown(disintegra5on)andchemicalaltera5on(decomposi5on)ofrocksatornearEarth'ssurface Slowbutconstant Plentyof5meSURFICIALorEXTERNALPROCESSES Aectsthetop150feetjust!WEATHERINGsceneryWEATHERINGscenery TheBrides
UNC Chapel Hill - STOR - 155
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UNC Chapel Hill - STOR - 155
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UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155