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Positioning | ![]() |
By: Lindsay Craig
Objective: You will also be able to plot latitude and longitude positioning grids and locate specific localities.
Reason: Latitude and longitude positioning grids are the most common positioning grids in use worldwide; everywhere on the Earth's surface can be defined by latitude and longitude.
The adjacent
image shows the view from the top of Mt. Davidson looking down on a portion
of Virginia City (lower left). Four of the five authors of this web
site are shown. Imagine that you were at the top of Mt. Davidson hiking and
taking in the spectacular view with your best friend and a thunderstorm rumbles
in. Lightning bolts start cracking all around you, and your friend takes
a bolt. You grab your cell phone and call for help. The dispatcher needs
your position in order to send help. Instantly with a topographic map
or a Global Positioning System (GPS) receiver you would be able to give the
dispatcher exact and certain latitude and longitude coordinates; help's
on the way. This is just one example of how positioning can be
important. Global positioning helps people get jobs done, and some of
these people are navigators and Virginia City surveyors. Who else uses
positioning and maps?
People have created numerous systems for describing exact positions for anywhere
on the Earth's surface. The United States Geological Survey (USGS)
developed different topographic maps that utilize numerous useful
positioning grids including Latitude and Longitude, Universal Transverse
Mercator, Township and Range and Nevada Coordinate System (Nevada only).
All of these are useful, but for our purpose only Latitude and Longitude
will be discussed because it is the most widely used system of positioning
worldwide.
Slice an apple in half through its stem and you have created an east half and west half along a longitude cut. Put the apple back together and slice it in half perpendicular to the longitude cut. You have now created an equator or latitude line that separates the apple into north and south halves. With these two cuts have you created halves, quarters or thirds? By convention these sections are referred to as the NE, NW, SE and SW sections.
Longitude lines projected onto the Earth trace a straight line from the North
Pole to South Pole. Longitude lines are based on degrees where there are
360 degrees to a full circle. There are 180 longitude lines on each half
of the Earth. The zero degree longitude line is called the Prime Meridian
and it was randomly chosen to pass through Greenwich, England. At this place
you can put one foot on the east half of the Earth and one foot on the west
half of the
Earth.
Latitude lines, on the other hand, measure from zero degrees at the equator and are evenly spaced both in the north and south hemisphere to 90 degrees at the poles. From the equator, each equally spaced slice gets smaller as the latitude lines get shorter. This is similar to the slicing of a beet as shown in the sketch to the right; the smallest slices are at the ends.
Shown
in the adjacent image are the major continents and oceans in a worldwide
view displaying the relationship of longitude to latitude. In this
sketching, the Earth's surface has been "peeled off a globe like an onion
skin and pasted to a flat surface." Slices of longitude have been distorted
into curves while lines of latitude remain as straight lines. Lines of latitude
are greatest in length at the equator and progressively get shorter towards
the poles. To keep the terms latitude and longitude straight it helps to
remember that longitude lines are always "long" and latitude lines are always
"lateral." Lateral means "sideways." On the sketching both longitude
and latitude lines are drawn every 15 degrees. If this image were pasted
back to the globe the longitude line on the right side would be the same
line as the one on the left side.
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