49 Pages

Midterm Study Powerpoint

Course: GGS 311, Fall 2011
School: George Mason
Rating:
 
 
 
 
 

Word Count: 1739

Document Preview

Collection Data Techniques Raster Vector Secondary Digitalremote sensingimages GPS measurements Digitalaerial photographs Primary Survey measurements Scannedmaps Topographic surveys DEMsfrommaps Toponymydata setsfromatlases Primary Data Capture Capture specifically for GIS use Raster remote sensing e.g. SPOT and IKONOS satellites and aerial photography Passive and active sensors Resolution...

Register Now

Unformatted Document Excerpt

Coursehero >> Virginia >> George Mason >> GGS 311

Course Hero has millions of student submitted documents similar to the one
below including study guides, practice problems, reference materials, practice exams, textbook help and tutor support.

Course Hero has millions of student submitted documents similar to the one below including study guides, practice problems, reference materials, practice exams, textbook help and tutor support.
Collection Data Techniques Raster Vector Secondary Digitalremote sensingimages GPS measurements Digitalaerial photographs Primary Survey measurements Scannedmaps Topographic surveys DEMsfrommaps Toponymydata setsfromatlases Primary Data Capture Capture specifically for GIS use Raster remote sensing e.g. SPOT and IKONOS satellites and aerial photography Passive and active sensors Resolution is key consideration Three key aspects of resolution: Spatial Spectral Vector Primary Data Capture Surveying Locations of objects determines by angle and distance measurements from known locations Uses expensive field equipment and crews Most accurate method for large scale, small areas GPS Collection of satellites used to fix locations on Earths surface Differential GPS used to improve accuracy Secondary Geographic Data Data collected for apture C other purposes can be converted for use in GIS Raster conversion Scanning of maps, aerial photographs, documents, etc Important scanning parameters are spatial and spectral (bit depth) resolution Vector Secondary Data Capture Collection of vector objects from maps, photographs, plans, etc. Digitizing Manual (table) Heads-up and vectorization Photogrammetry the science and technology of making measurements from photographs, etc. COGO Coordinate Geometry Managing Data Capture P Key principles rojects Fundamental tradeoff between Clear plan, adequate resources, appropriate funding, and sufficient time Quality, speed and price Two strategies Incremental Blitzkrieg (all at once) Alternative resource options In house Specialist external agency Summary Data collection is very expensive, timeconsuming, tedious and error prone Good procedures required for large scale collection projects Main techniques Primary Raster e.g. remote sensing Vector e.g. field survey Secondary Raster e.g. scanning Vector e.g. table digitizing Addendum: Volunteered The Tea Fire Geographic Santa Information Barbara, (VGI) California, Nov. 2008 An unfortunate case study Exacerbated by sundowner VGI: An unfortunate The Tea Fire case study Official sources: Precise fire boundaries every 24-36 hours GIS and Image-based techniques PDF format, posted online and distributed at community outlets Unofficial sources Rough boundaries Real-time Volunteered Geographic Information (VGI) @ GMU 30,000+ students Majority geo-aware and with mobile computing Could they be used to augment an official information source with VGI? Goal: Capture real-time VGI- Building VGI @ GMU: GeoParsing Collect available sources of official infrastructure data building footprints building contents sidewalks, roads, parking Build a localized gazetteer Develop ability to geo- A Localized Gazetteer Purpose: . Translate between human world and GIS world provide spatial footprint for placenames in VGI Link resources by location Current problem with campus emergency alert system: Ambiguous Gazetteer Digital Representation Uses only two symbols, 0 and 1, to represent information The basis of almost all modern human communication Many standards allow various types of information to be expressed in digital form MP3 for music JPEG for images ASCII for text GIS relies on standards for geographic data Types of Attributes Nominal, e.g. land cover class Ordinal, e.g. a ranking Interval, e.g. Celsius temperature Ratio, e.g. Kelvin temperature Differences make sense Ratios make sense Cyclic, e.g. wind direction, slope Cyclic Attributes Do not behave as other attributes What is the average of two compass bearings, e.g. 350 and 10? Occur commonly in GIS Slope aspect Wind direction Flow direction Special methods are needed The Fundamental Problem Geographic information links a place, and often a time, with some property of that place (and time) The temperature at 34 N, 120 W at noon local time on 12/2/99 was 18 Celsius The potential number of properties is vast In GIS we term them attributes Attributes can be physical, social, economic, demographic, environmental, etc. The Fundamental Problem contd. The number of places and times is also vast The more closely we look at the world, the more detail it reveals Potentially infinite Potentially ad infinitum The geographic world is infinitely complex Humans have found ingenious ways of dealing with this problem Many methods are used in GIS to create representations or data models Discrete Objects Points, lines, and areas Countable Persistent through time, perhaps mobile Biological organisms Animals, trees Human-made objects Vehicles, houses, fire hydrants Continuous Fields Properties that vary continuously over space Value is a function of location Property can be of any attribute type, including direction Elevation as the archetype A single value at every point on the Earths surface The source of metaphor and language Any field can have slope, gradient, peaks, pits Characteristics of Rasters Pixel size The size of the cell or picture element, defining the level of spatial detail All variation within pixels is lost Assignment scheme The value of a cell may be an average over the cell, or a total within the cell, or the commonest value in the cell It may also be the value found at the cells central point Vector Data Used to represent points, lines, and areas All are represented using coordinates One per point Areas as polygons Straight lines between points, connecting back to the start Point locations recorded as coordinates Lines as polylines Straight lines between points Raster vs Vector Volume of data Raster becomes more voluminous as cell size decreases Source of data Remote sensing, elevation data come in raster form Vector favored for administrative data Software Some GIS better suited to raster, some to vector GIS software Chapter 7, parts of a GIS 4 technical parts: Network Hardware Software Data GIS Software: The processing of engine a complete, working, GIS Narrower view of GIS software: Systems with a range of generic capabilities to collect, store, manage, query, analyze, and present geographic information Distributed primarily as commercial-off-the-shelf Architectur e of GIS Software Fig. 7.2 Three-tier perspective on GIS software (using terminology from Information Systems) Architectur e of GIS Software Centralized desktop GIS (fig.7.5) Thin clients are used to run only a small application, that Desktop & Network Todays GIS Geographic nformation pIaradigms Systems work with software running on the desktop or on the web. GIS Software Systems & Vendors Types of GIS Software Main types of GIS software: Desktop GIS Web Mapping Server GIS Virtual Globes Developer GIS Hand-held GIS Desktop GIS: Software ported to PCs (mid-90s) Desktop GIS is now the most widely-used category of GIS software systems From Professional high-end editor-analysis systems: ESRI ArcInfo, Intergraph GeoMedia Types of GIS Software Main types of GIS software: Desktop GIS Web Mapping Server GIS Virtual Globes Developer GIS Hand-held GIS Web Mapping: 2000-2010 Integrated Web-accessible software 2-D map database and services (routing, gazetteers, etc.) Google Maps, MyMaps Types of GIS Software [p.167-174] Main types of GIS software: Desktop GIS Web Mapping Server GIS Virtual Globes Developer GIS Hand-held GIS Server GIS: Last decade 1990s dominated by desktop GIS, next decade will be dominated by Server GIS products. Server GIS runs on a computer server that can handle concurrent processing requests Types of GIS Software Main types of GIS software: Desktop GIS Web Mapping Server GIS Virtual Globes Developer GIS Hand-held GIS Virtual Globes: 3-D Web services hosted on Web-based GIS that publish global 3-D databases and associated services for use over the Web. [p.200] Global 3-D databases 3-D web services Types of GIS Software Main types of GIS software: Desktop GIS Web Mapping Server GIS Virtual Globes Developer GIS Hand-held GIS Developer GIS: GIS Vendors release collections of GIS software components for developers. Toolkits of GIS Functions for programmers to use in building GIS applications http://www.deluoelectronics.com/customer/154-Deluo_Marine_Navigation_System Examples: BlueMarble Geographics GeoObjects, ESRI ArcGIS Engine, MapInfo MapX Types of GIS Software Main types of GIS software: Desktop GIS Web Mapping Server GIS Virtual Globes Developer GIS Hand-held GIS Handheld GIS: Handheld GIS are lightweight systems designed for mobile and field use Important factors in development: Miniaturization & hardware design Introduction Atomic Element of Geographic Information Location (X , Y) , Time , Attribute Time is an optional element in geographic information, but location is essential Terms used to describe the act of assigning location to atoms of information: georeference geolocate geocode Georeferences Every georeference has an associated spatial resolution equal in size to the size of the area that is assigned that georeference. Street address assigned to a parcel by a municipality, passed on to tax assessor, EMS, schools, etc. Georeferences Metric georeferences, such as latitude and longitude are based on measurement. Advantage: infinitely fine spatial resolution with finer measurement Advantage: GIS functionality, including computing distance Metric georeferences are much more useful because they allow maps to be made and distances to be calculated Georeferen cing: Gazetteer: Placename s A geographic dictionary or index Link between a placename and a map Alexandria Digital Library Gazette Server Client UCSB Map & Imagery Library / UC Board of Regents Georeferen cing: Cadasters and the US Public Land Survey System Cadaster: A map of land ownership for taxing land and for public record Parcels of land organized in a cadaster and uniquely identified and persistent, therefore a good means of georeferencing land. US Public Land Survey System was developed during the settlement of the western US A Surveyor lays out a NorthSouth meridian, then 6 mile by 6 mile blocks referenced by township and range index numbers. Each section is divided further into 36 1 mile by 1 mile sections, and further into four Projections and A basic problem Ccoordinate aused by a round Earth: s Earth: Ellipsoid Paper: Flat Maps: Flat Photographic film: Flat Map projections Map projects always distort the Earth in some way, but some map projections are good at preserving certain characteristics or properties. Two important map properties are conformality and equivalence. Conformal projections preserve shape of small features, and preserves angles locally. The scale of the projection is the same in any direction. Because conformal projections are good at preserving angle (bearing) they are often used for navigation. Examples: Mercator Projection (1569) Lambert Conformal Conic (1772) Map projections Equal Area (Equivalent) projections preserve area. Areas measured on the map are always in the same Map projections Cylindrical projections are analogous to wrapping a cylindrical sheet of paper around Map projections Azimuthal or planar projections are analogous to touching the Earth and projecting its Map projections Conic projections are analogous to wrapping a sheet of paper in a cone shape Map Projections: Plate Care The Plate Care (or Cylindrical Equidistant) projection simply assigns X to longitude and Y to latitude Map Projections : UTM The Universal Transverse Mercator Projection (abbreviate UTM) is used in many military applications and datasets with national or Map Projections : UTM UTM coordinates are in meters, with extra decimals for sub-meter precisions: 855,000 meters east Map Projections The State : State Plane Plane Coordinate System Coordinate (SPCS) aSystem llows for (SPCS) measuremen ts that can be more accurate than with UTM.
Find millions of documents on Course Hero - Study Guides, Lecture Notes, Reference Materials, Practice Exams and more. Course Hero has millions of course specific materials providing students with the best way to expand their education.

Below is a small sample set of documents:

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
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155
UNC Chapel Hill - STOR - 155