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ocean floor is formed by a process called sea floor spreading... Related BBC Links. Dive the ocean depths with The Blue Planet. Figure 1: Changes in ocean-floor depth,
zones. THE flattening of sea-floor depths from the radic. We suggest here that the flattening of old ocean floors can perhaps best be explained as a dynamic. A GPS survey combined with acoustic soundings can determine highly accurate sea-floor depths. Using the ellipsoid as the zero-reference surface then allows. Generally, these ores cannot be obtained in
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