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57 Cards in this Set

  • Front
  • Back
Map scale equation
map distance/ground distance
large vs. small scale
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
Q: how many inches on a map is 20 miles on a 1:100,000 scale map?
1/100,00=x/20

-cross multiply and get x by itself
-then convert miles to inches
Cartographic accuracy
what we can physically see on the map
positional accuracy
-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
MMU
(minimum mapping unit)
-when mapping, if an area is less than MMU, it is merged into a larger unit

*more detail with smaller MMU
Datums
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
3 types of datum
NAD27
NAD83
WGS84
NAD27
-based on clarke1866
-"middle" was meades, KS
NAD83
-based on GRS spheroid
-"middle" was center of earth
WGS84
-GPS is based on this type of datum
-uses GRS80 spheroid
types of projections
planar
cylindrical
conic
planar
representation of sphere or ellipsoid on planar surface
cylindrical
round earth in cylinder
conic
round earth in cone
round earth on flat map distorts..?
-distance
-shape
-direction
-area
-angles
planar/azimuthal
-tangent or secant
-3 light sources
3 light sources of planar/azimuthal
gnomonic
stereographic
orthographic
gnomonic
light source is center of earth

-least amount of distortion b/c it's a straight line
-shortest distance is closest
stereographic
-light source is opposite side
-preserves shape
orthographic
-light source is infinite
-"truest" direction
standard parallel
the lines that intersect the earth for a secant projection
3 secant orientations
equatorial
transverse
oblique
equatorial standard parallels
axis is parallel to earth's rotation
transverse standard parallel
axis is 90 degrees to earth's rotation
oblique standard parallel
axis is at any other angle than parallel or 90 degrees
Conformal projection
preserves shape
equivalent projection
preserves area
compromise projection
preserves neither shape nor area
2 popular types of projection
Albers equal area
-preserves area

Lambert conformal
-preserves shape
area on earth --> type of projection
near equator --> cylindrical
mid-latitude --> conic
polar region --> planar
east/west --> conic
north/south --> transverse cylindrical
Coordinate systems
standardized method for assigning codes
types of coordinate systems
geographic (*NOT a true grid)
cartesian
UTM
military grid
state plane

*the rest of these ARE true grids
geographic
- not a true grid
- latitude and longitude
- uses decimal degrees
decimal degrees
46 degrees 15 minutes 36 seconds
-->46 + 15/60 + 36/3600= 46+.25+.01

[46.26]
cartesian coordinate system
-2 points- straight line difference
-find the distance with Pythagorean theorem (x=easting y=northing)
UTM
-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
state plane
- each state divided into 1 or more zones
- each zone with its own coordinate system
- horizontal= lambert conformal conic
-vertical= transverse mercator
digital cartography
presenting spatial info digitally
map
real world model where features are replaced by symbols
7 map requirements
1- title
2- map figure
3- legend
4- scale
5- north arrow
6- source block
7- neat line
inset and locator maps
inset map is more detailed and zoomed in than a locator map
types of map data
discrete
continuous
nominal
ordinal
ratio
interval
discrete
specific # of fractions at one point
continuous
a continuous measurement
nominal
-tells you A is different from B
-derived from qualitative
ordinal
-differentiated by class/rank
-derived from quantitative
-"small, medium, large"
interval
-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
ratio
-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
natural breaks
look for breaks in data
manual
you enter interval width data
equal interval
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
defined interval
pick interval and it gives you the # of classes
quantile
-arranges data from low to high
-equal # of observations in each interval
arithmetic
class width increases at an arithmetic (additive) rate as it goes up
geometric
widths of classes increase in size at an exponential rate
projection properties summary
3 surfaces (planar, conic, cylindrical)
3 light sources (gnomonic, stereographic, orthographic)
3 orientations (equatorial, transverse, oblique)
contact points (tangent, secant)
distortion patterns