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50 Cards in this Set

  • Front
  • Back
Globe's Limitations

1) can only see half of Earth at one time


2) cannot show great detail


3) cumbersome (not easy to carry)


4) cannot include in a book, newspaper, etc.

Characteristics of Ideal Map

1) show true relative area


2) shows true shape


3) shows true direction


4) shows true distance


5) shows true position or location


Impossible (position/location should always be correct)

Cartography
science of map making
Map Essentials

1) Title


2) Author or Data Source


3) Date


4) Legend or Key


5) Orientation and Direction


6) Scale: Horizontal and vertical


7) Map Projection



Horizontal Scale Types

1) Representative Fraction


2) Bar Scale


3) Verbal Scale

Representative Fraction

1 mile = 63,360 inches


1: 63,360

Bar Scale (linear, graphic)

Verbal Scale (written)
one inch equals five miles
small scale map

- shows very large area (world map)


-shows little detail


-rep. fractions in millions

Large scale map

-shows very small area (city map)


- shows great detail


- rep. fractions in thousands


(the larger the scale the greater the detail)

Vertical Scale

4 types of info vertically on map


1) Elevation of ground


2) shape of Landform


3) size of landform


4) slope of the ground

topographic map
show vertical scale, elevation and relief
elevation
distance above or below the datum plane ( sea level)
relief
difference between highest and lowest elevation in a given area
Spot Heights
(way to show elevation and relief) exact elevations for specific points on the map
Shaded relief map
uses shadows to give a 3 dimensional effect to show landforms (relief)
Hyposometric (layered) map
uses colors to show elevation
Hachure Map
uses tiny short lines ( hash marks or tick marks) to draw a picture of landforms
Raised Relief map
is 3 dimensional

Contour Map

uses contour lines to show relief


(contour line: line on a map that connect points of equal elevation)

Contour Line Characteristics

1) never end


2) never cross


3) never split (fork)


4) generally form smooth curves


5) tend to parallel eachother


6) parallel streams


7) crossing a stream, form a "V" that points upstream


8) lines close together = steep slope, far apart = gentle slope

contour interval
vertical difference between contour lines (5', 20', 100' etc)
Index contour
thicker, numbered contour lines
depression contours (hachured)
used for a depression (hole) - elevation gets lower
Map Projections

-attempt to duplicate the round earth on a flat plane (map)


-A system of lines drawn on a flat surface, representing a chosen number of parallels and meridians in harmonic arrangement


- true position or location must be correct

Direct projections
can be demonstrated using a light transparent globe and geometric figures
Cylindrical projection

- type of direct projection


-cylinder placed over globe

Mercator Projection

-type of cylindrical projection


-used for navigation


-combination of gnomic projection and great circle route

Rhumb line
line of true compass projection
Conic Projections

-type of direct map projections


-cone placed over globe


- most useful for land in middle latitudes (U.S.)


- used for Geological U.S. maps

Polyconic Projection
many cones, not a direct projection
Plane Projections

flat plane is placed on the globe


(polar plane: centered over one of the poles, equatorial plane: centered over equator)

Indirect Projections

cannot be demonstrated with light and globe


(most are oval projections and most are equal area)

Goode's Interrupted Equal Area Homolosine Projection
popular indirect projection
Aerial Photographs
recording images from above the earth (may be taken in stereo pairs)
Stereoscope
used to view two photos 3 - dimensionally
Hydrosphere
the water world (3/4 water)
Hydrologic Cycle
the balance and recycling of Earth's fresh water supply
Continental Shelf
shallow area around continents (sea level to 600 ft in depth)
Tides

-periodic rise and fall of sea level


- caused by gravitational pull of the moon and the sun


-moon has greater effect because it is closer


-tides rise and fall twice daily (takes 12 hrs and 25 min to complete cycle) ( 24 hrs and 50 min to complete two tidal cycles)

Tidal Range

- difference between the high tide and the low tide (averages 6 to 8 feet)


- Bay of Fundy (Canada) - world's highest tidal ranges

Tidal Bore
tide comes in as a wall of water
Spring tides

-unusually high tides that occur twice each month (new and full moon)



Neap Tides
-lower than normal tidal variations (1st and third quarter)

Waves

- generally caused by wind


-wind may be caused by storm thousands of miles away

Ocean Currents and drifts

- "rivers" of water that circulate around in the oceans


- caused by drag exerted by prevailing winds and the Earth's rotation


-location of continents also affects their movements

Movement of Currents

-clockwise in Northern Hemisphere


-counterclockwise in Southern Hemisphere

Coriolis Effect

-all objects in motion in N Hemisphere tend to turn to the right of their original direction (clockwise)


-left (counterclockwise) in S Hemisphere


- caused by Earth's rotation (no deflection at equator, max deflection at poles)

Currents (need to know)

1) Gulf Stream (warm) - Eastern U.S.


2) Brazil (warm) - Eastern South America


3) Peru or Humboldt (cold) - Western South America


4) Japan (warm) - Eastern Asia


5) California (cold) - Western U.S.

Tsunamis
- seismic waves or "tidal waves"-huge waves caused by submarine earthquakes or volcanic eruptions or submarine landslides- tsunamis travel at 500 mph