week 1 - maps, cross sections, and graphs Flashcards
equator
great circle around the earth that includes all points equally distant from the poles
what do maps do? (3 things)
- provide valuable interface to explore the geography of the world
- incorporate quantifiable units
- represents geographic information, or other things like temperature and depth
parallels of latitude
small circles that are parallel to the equator
- poles at 90 degrees north and 90 degrees south
meridians of longitude
great circles perpendicular to the equator that intersect at the poles
- measure angles east and west of the prime meridian which is at 0 degrees longitude (right in the middle)
latitude
measured from 0 to 90, north and south of the equator
longitude
start at the prime meridian and go around the globe
- 0 to 180 from east to west
how many minutes in between latitude degrees?
60
cross sections
projections that are slices perpendicular to the surface of the earth
- presents a side view of the earth
- allows for description of the interior of the earth and subsurface of the oceans
vertical exaggeration
helps maximize the utility of cross sections across large distances
- to check if something is vertically exaggerated
- check the difference in size between 0 and 1 on the x and y axis
how to find how many times something is exaggerated
- find horizontal and vertical scales
scale = distance represented on map/distance represented on earth - measure representation physically and then divide by what it tells you
ex. 4.5 cm on paper/6 km on earth - vertical/horizontal scale
graphs
something to help visualize the relationship between two variables or more
- useful for 2D representations of data
interpolation
estimating a value from within the known data plot
extrapolation
estimating a value from beyond the known data plot
contour lines (5 important things)
lines connecting data points of equal value (on maps and cross sections)
- when depth is steeper, the lines are closer together and vice versa
- contour maps go up in elevation and bathymetric maps go downward in elevation
- bigger numbers are deeper in the ocean, smaller numbers are nearer to the surface
- if contour map is going up in elevation it is a valley
- if contour map is going down in elevation it is a ridge
three rules of contour maps
- contours never cross one another
- cannot be two different elevations or depths at the same time - contours can close itself
- v’s that point uphill are troughs or valleys, and the ones that point downhill are ridges