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for the remaining portion of the earth. While the observational
requirements for these computations appear enormous, the results well
justify the necessary survey work.
Figure 13.4 Products of the gravimetric method
Figure 13.4. shows how the mass surplus of the mountains and
the mass deficiency of the oceans cause the deflections of the vertical
and the undulations of the geoid. A mountain mass attracts the plumb
line from the normal of the ellipsoid. Likewise the mass deficiency of
the ocean does not attract the plumb line. These effects of the mass
anomalies contribute to the deflection of the vertical. However, both
deflections of the vertical and undulation values result from density
variations throughout the earth. In the area of mass surplus, the
observed gravity (reduced to sea level considering only the elevation)
is generally greater than the theoretical value, and the anomalies are
positive. In the areas of mass deficiency, the observed (reduced in the
same manner) is generally smaller than the theoretical value and the
anomalies are negative. Figure 13.5.
The deflections and undulations computed with sufficient gravity
information are considered absolue values referred to an earth-
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