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The vertical datum is a collection of specific points on the Earth with known heights either above or below mean sea level. Near coastal areas, mean sea level is determined with a tide gauge. In areas far away from the shore, mean sea level is determined by the shape of the geoid.
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Elements of precise surveying and geodesy. avity,as indicated by the plumb line at that point; from the lawsof hydrostatics it is evident that the free surface of all waters 85. THE
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