By Louella Oettinger Parsons
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Extra resources for How to Write for the "Movies"
But as their uppermost parts sink slowly below sea level, they are flattened by marine erosion to create a distinctive type of drowned island called a guyot. 54 It is also worth mentioning at this point that sometimes even within the coral seas, islands do sink without trace. Much clearly depends on the rate at which the subsidence occurs; rapid subsidence, perhaps coseismic, may drop an island coast below the photic zone in a matter of seconds. 6. The Subsidence Theory of Atoll Formation. a. The process of atoll formation begins when a volcanic island in the coral seas, surrounded by a fringing reef growing upward from shallow foundations, begins to sink.
Around that time, most of the continental crust of the earth had aggregated into the supercontinent Rodinia. 23 The edge of the nascent Pacific Ocean is likely to have been a good place to live because, as Rodinia broke up, in perhaps a mere 180 million years, the accompanying increase in continental coastline produced an unparalleled diversification of climates. 24 The disaggregation of Rodinia created a huge diversity of environments for occupation by specially adapted life-forms, and the increase in atmospheric oxygen provided the important impetus for their evolution.
As is seen in chapter 5, certain aspects of the human history of the Pacific during the period of postglacial sea-level rise are explainable by the effects of catastrophic sea-level rise events (CREs). These CREs resulted from the rupture of natural dams that held back huge lakes of meltwater on the continents. The water poured down valleys and into the ocean, raising its level comparatively rapidly. 1. a. Echo-sounding trace by RV Horizon across the top of Alexa Bank, one of the first submerged islands to be mapped and examined.