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57 Cards in this Set
- Front
- Back
Map scale equation
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map distance/ground distance
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large vs. small scale
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large= more detail, smaller area
small= less detail, larger area *the smaller the scale is, the lower the % is that it will be accurate *smaller scale means fewer features |
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Q: how many inches on a map is 20 miles on a 1:100,000 scale map?
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1/100,00=x/20
-cross multiply and get x by itself -then convert miles to inches |
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Cartographic accuracy
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what we can physically see on the map
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positional accuracy
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-tested against something
-actually going out and standing somewhere the GPS says there's a tree and seeing if there actually is and how far off it is from the map |
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MMU
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(minimum mapping unit)
-when mapping, if an area is less than MMU, it is merged into a larger unit *more detail with smaller MMU |
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Datums
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mathematical model estimating shape of spheroid
-has a set of precise control points which help define a base control system to have least amount of distortion |
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3 types of datum
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NAD27
NAD83 WGS84 |
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NAD27
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-based on clarke1866
-"middle" was meades, KS |
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NAD83
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-based on GRS spheroid
-"middle" was center of earth |
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WGS84
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-GPS is based on this type of datum
-uses GRS80 spheroid |
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types of projections
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planar
cylindrical conic |
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planar
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representation of sphere or ellipsoid on planar surface
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cylindrical
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round earth in cylinder
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conic
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round earth in cone
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round earth on flat map distorts..?
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-distance
-shape -direction -area -angles |
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planar/azimuthal
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-tangent or secant
-3 light sources |
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3 light sources of planar/azimuthal
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gnomonic
stereographic orthographic |
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gnomonic
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light source is center of earth
-least amount of distortion b/c it's a straight line -shortest distance is closest |
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stereographic
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-light source is opposite side
-preserves shape |
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orthographic
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-light source is infinite
-"truest" direction |
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standard parallel
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the lines that intersect the earth for a secant projection
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3 secant orientations
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equatorial
transverse oblique |
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equatorial standard parallels
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axis is parallel to earth's rotation
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transverse standard parallel
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axis is 90 degrees to earth's rotation
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oblique standard parallel
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axis is at any other angle than parallel or 90 degrees
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Conformal projection
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preserves shape
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equivalent projection
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preserves area
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compromise projection
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preserves neither shape nor area
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2 popular types of projection
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Albers equal area
-preserves area Lambert conformal -preserves shape |
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area on earth --> type of projection
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near equator --> cylindrical
mid-latitude --> conic polar region --> planar east/west --> conic north/south --> transverse cylindrical |
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Coordinate systems
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standardized method for assigning codes
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types of coordinate systems
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geographic (*NOT a true grid)
cartesian UTM military grid state plane *the rest of these ARE true grids |
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geographic
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- not a true grid
- latitude and longitude - uses decimal degrees |
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decimal degrees
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46 degrees 15 minutes 36 seconds
-->46 + 15/60 + 36/3600= 46+.25+.01 [46.26] |
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cartesian coordinate system
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-2 points- straight line difference
-find the distance with Pythagorean theorem (x=easting y=northing) |
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UTM
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-projection AND coordinate system
- tangent along central meridian - split into 60 sections of 6 degree widths so each section is its own coordinate system to accommodate for less distortion |
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state plane
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- each state divided into 1 or more zones
- each zone with its own coordinate system - horizontal= lambert conformal conic -vertical= transverse mercator |
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digital cartography
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presenting spatial info digitally
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map
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real world model where features are replaced by symbols
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7 map requirements
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1- title
2- map figure 3- legend 4- scale 5- north arrow 6- source block 7- neat line |
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inset and locator maps
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inset map is more detailed and zoomed in than a locator map
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types of map data
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discrete
continuous nominal ordinal ratio interval |
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discrete
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specific # of fractions at one point
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continuous
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a continuous measurement
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nominal
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-tells you A is different from B
-derived from qualitative |
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ordinal
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-differentiated by class/rank
-derived from quantitative -"small, medium, large" |
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interval
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-ordinal or rank data WITH values
-based on an arbitrary scale -0 IS arbitrary *you can have 0 for a temp value, or an elevation |
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ratio
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-based on an arbitrary scale
-ordinal or rank data with values -0 is NOT arbitrary *you can't have 0 as an age, or an area, or a precip value.... it simply doesn't exist at that point |
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natural breaks
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look for breaks in data
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manual
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you enter interval width data
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equal interval
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diff. b/w lowest and highest value (range)
pick # of classes and it interval is determined -they'll have equal widths unlike natural breaks method |
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defined interval
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pick interval and it gives you the # of classes
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quantile
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-arranges data from low to high
-equal # of observations in each interval |
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arithmetic
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class width increases at an arithmetic (additive) rate as it goes up
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geometric
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widths of classes increase in size at an exponential rate
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projection properties summary
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3 surfaces (planar, conic, cylindrical)
3 light sources (gnomonic, stereographic, orthographic) 3 orientations (equatorial, transverse, oblique) contact points (tangent, secant) distortion patterns |