The Highest and Lowest points of the Lithosphere are both found at the Earths plate boundaries, with reference to the process of plate tectonics, explain why this is so.

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Patrick Brosch

Period 8

Geography Higher IB

September 16th, 2000

IB EXAM ESSAY QUESTION

Question:

The Highest and Lowest points of the Lithosphere are both found at the Earths plate boundaries, with reference to the process of plate tectonics, explain why this is so.

The process of plate tectonics, also known as Orogenesis, has shaped Planet Earth to what it is today. The four different spheres; Lithosphere, Hydrosphere, Atmosphere, and Biosphere, have worked together to create a beautiful a gigantic Ecosystem where Fauna, Flora, Detritus Feeders (Bacteria and other Micro-organisms) and Decomposers have created a world to live in with the highest and smartest known species; the Human. Plate Tectonics has not only build our world but also helped to destroy it and to rebuild it in different shapes and forms.

The Earths Landmasses used to be joined together known under the name of Pangea. After millions of year the art of plate tectonics has moved this large landmass apart into smaller landmasses known as Continents and Islands. It is already estimated what the “Next Pangea” will look like, that would be 250 Million years from now (Figure 4.1). Through this process many new landscapes have been created. There are seven major plates that move between the earths surface and core, which is named the Asthenosphere. They are the Pacific Plate, Indo-Australian Plate, African Plate, North American Plate, South American Plate, Antarctic Plate, and the Eurasian Plate (Figure 6.1). The structure of the Earth can be easily shown in a diagram which is shown in (Figure 1.1) at the end of this document. The plates which are moved by the convection currents in different directions have therefore created and destroyed parts of the lithosphere, also known as Denudation (Process of breaking down the Lithosphere). These convection cells and their currents have moved these major plates in different directions through all this time. These movements have different names too. They are describes like this and diagrams are shown in (Figure 2.1) and

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(Figure 3.1) at the end of the Document:

Constructive Margins- is when two plates move apart and away from each other letting Magma (the molten rock which belies under the earths crust) reach the surface where its then called Lava. It cools off and created to landmasses which are very fertile because of it’s large mineral content. This process forms Mid-Ocean Ridges and is sometimes known as Sea-Floor Spreading. Example: Iceland.

Destructive Margins- is when two plates move together and one plate is pushed under the other plate. This only happens when a Continental Plate and a Oceanic ...

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