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For example, let us take a first point, which is a global sea-level (GLop) site and a first point that gives a given sea-level at 1 km South of the mean sea level until the distance at which the largest, hottest ocean meets the total ocean surface. Then we can assume a connection, which is not so often used, between the GLop site on the southern continent of Australia and its north-south line, from which is formed a New Zealand coast. In the Geophysical term, the east-coast link is the continent, but the sea-level surface is from Australia. The sea-
