An assessment of the relative contribution that geoscience has made to our contemporary understanding of physical oceanography.
Written in 2004; 3,072 words; 8 sources; MLA; $ 89.95
Paper Summary:
This paper purports to investigate our greater understanding of the unified theory of plate tectonics and seafloor spreading. The structure of the earth and the traditional theory of continental drift is examined, followed by a look at the more unified theory of plate tectonics. The global ramifications of this theory is investigated by examining the damaging tectonic activity caused by seafloor spreading, specifically earthquakes as well as the hazards these earthquakes in turn generate, namely tsunamis. Case studies are provided to illustrate the damaging nature of these natural forces. Finally the paper examines whether these hazards can be predicted or prepared for given our greater understanding of their causes.
From the Paper:
"The Earth is a layered planet consisting of the crust, mantel and core as illustrated in Figure 1 below. Due to the intense heat during the formation of the planet, Earth was mostly molten. The more dense materials sank to the centre forming the core while the lighter materials floated to the surface and gradually formed a rigid layer called the lithosphere (Byatt 2001:18). The upper part of this lithosphere is called the crust, a layer about 80km to 40km thick (Strahler & Strahler 1989:254). The lithosphere also includes the upper part of the mantle called the asthenosphere, which is highly heated to a state that is semi plastic. The rigid, brittle lithosphere, which is broken into large fragments called lithospheric plates, has the capability of moving over the soft, plastic asthenosphere."
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