Page 190 - NAVAL SCIENCE 3 TEXTBOOK
P. 190

196     NAVAL SK IL LS

         The Mercator projection was developed by a Dutch cartographer,   Harbor c1wrts are  large-scale  charts  that  show  harbors  and
         Gerardus Mercator, ill  the sL'Xteenth century.  It  is the most widely   their  approaches  in  detail.  Coastal  charts are  intermediate~scale
         used of all chart projections for  nm'igation. In  this projection, the   charts used to navigate a vessel whose position may be determined
         spherical globe is projected onto a cylinder-shaped piece of paper,   b)' landmarks and lights, buoys. or soundings offshore. For navi-
         wrapped  around  the  globe  at  the  equator.  Then,  the  cylindri-  gating inside olltlying reefs or shoals, or well offshore in large bays
         cal  paper is spread flat, after clltting it  at  convenient meridians.  A   of siz'lble inland waterways, a coastal or harbor chart may be used.
         Mercator projection of the world, for instance, is lIsuall)7 cut verti-  General ocean sailing charts are small-scale charts showing the
         call)' ncar the International Date Line so the continental land areas   approaches to large areas of the coast. These charts show oft-shore
         are shown almost unbroken.                            soundings, principal lights and ollter buoys, and any natural land-
            Because  of  the  method  of projection,  increasing  distortion   marks visible at a distance.
         occurs the farther the area 011  the Mercator chart is from the equa-  Scattered  all  over water areas of any nautical  chart arc many
         tor. However, this distortion is made uniform in both latitude and   tiny italicized figures called sO//Ilrlillgs, each representing the depth
         longitude.  so  the  finished  chart  is  usable  for  navigation  even  at   of water in that particular place. Depths may be given in feet, fath-
         high latitudes. The space between parallels increases with latitude,   oms (6 feet  to  1 fathom), or meters.  A not<ltion under the title of
         but  the distance  represented by 1 degree of latitude is  alwi.l)7s  the   the chart is the key;  for example. "Soundings  in feet at mean low
         same,  I n<1uticalmile.  Because of the distortion at  high latitudes.   water." Most charts also contain dotted lines called fathom curves,
         the island of Greenland appears much larger than the United States   marking the limits of areas of certain  depths.  Most newer charts
         on a .Mercator projection. In actuality the reverse is true.   will give water depth, heights of lights. and land contours in meters
            The  meridians  on  a  Mercator chart appear as  stmight  lines,   as well as in feet.
         north  and  south,  parallel  to  and  equidistant  from  one  another.   Nautical  charts  are  available  for  purchase  at  nautical  sup-
         The}'  represent  the  imaginary curved  meridian  lines  that  come   pi)' stores in  most coastal cities and towns throughout the United
         together at the poles on a globe.                     States. In addition to traditional paper charts, electrollic chnrts on
            Scale of charts. The scale of a chart refers to a measurement of   computer data storage media that can be projected onto computer
         distance.  It is a comparison of the actual dist,lI1ce or size of a fea-  screens and  various  types of electronic  plotters are  coming into
         ture with  that shown  011  the chart. The scale of a chart or map is   widespread use in marine navigation.
         normally printed  Ileal'  the legend  ill  the  form  of a  ratio, Stich  as
         I  :5,000  (meaning  that  the  feature  shown  is actually 5,000  times
                                                               Plotting
         larger than  its size 0 11  the chart). Said in  another way, an  inch or
         centimeter or other  measurement on  the chart  represents  5,000   In  order to use  the  nautical chart  for navigating, you  must know
         identical units on the real Earth's surface. The smaller the ratio, the   something about how courses, bearings, and  lines of position arc
         smaller the scale of the chart. A chart with a scalc of I :5,000 is on   plotted on it.
         a Inllch larger scale than one whose scale is 1:4.500.000. for exam-  The basic instruments lIsed ill plotting are parallel rulers, some
         ple. Small scales arc lIsed to depict large areas on a chart. and large   kind of protractor, and dividers. The parallel ruler consists of two
         scales arc lIsed to depict sl11;.111  areas.          straightedges  connected  by  pivoted  mel'al straps  Ileal'  each  end.
            Another wa)' of expressing scale, called the 1IIIIIIerimi smle.  is   The straps allow the two  straightedges  to  be opened  and closed,
         in  inches, miles, or kilometers to  the nautical  mile. This is shown   while <1lways  remaining parallel to e;.tch other.  By placing the edge
         near the legend  as a  bar scale  (linear scale)  with  both  compared   of one straightedge along a line of bearing and "walking" the ruler
         measurements shown. one on either side of the bar. By lIsing a pair   carefully across  the chart to  a compass  rose (a graphic used  as  a
         of dividers,  set  to  the linear scale desired. YOll  can  find  distances   reference for  both  true and magnetic directions 011  a chart),  the
         by "w<llking" the dividers across the chart and  lIsing simple arith-  true  bearing of the  line  may be determined. Dividers are a  plot-
         metic.  For example. if an  inch 011  the chart represents 50 miles, 5   ting instrument  used  for  measuring chart  distances along a suit-
         inches would represent 250 miles.                     able scale on a chart.
            Remember, the larger the scale, the smaller the area shown on a   A protractor docs just about the same thing as parallel  rulers.
         given chart or map. Large-scale charts show areas in greater detail.   A simple protractor consists of a gmduated arc on a piece of clear
         Features that appe.ll' on a large-sG.lle chart may not show tip at all   pl<1stic.  Another kind of protmctor has a  ruler that pivots on the
         on a small-scale chart of the same area.              center of the cun'ahlre of the arc. The protmctor's arc is graduated
           Types  of  charts.  Nautical charts, as described above, are those   like the upper half of a compass rose. Horizontal and vertical refer-
        with  the  necessary  information  for  safe  navigation.  They  have   ence lines on the pl<1stic can be lined up with the meridians or par-
         standard symbols, figures, and abbreviations that tell  the depth of   aiJels, and any course or bearing can be easily plotted by swinging
        water, type ofbottoll1, location of navigational aids. and so forth.   the ruler to the desired degree Illark on the arc.
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