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Lecture 2

 

The earth is not a static, but a dynamic system with predictable changes.

 

The major theory covering the geologic processes at the surface of the earth is summarized in the Theory of Plate Tectonics

 

         Basic Theorem: the crust is made up of individual plates which move independently of each other.  There are 8 major plates (e.g. North American Plate, Pacific Plate) and about 20 minor plates (e.g. Juan de Fuca Plate off the coast of Oregon). Fig. 1

         Consequence: Three types of boundaries between plates

        Divergent boundary: new oceanic crust is formed; basaltic volcanism; shallow earthquakes

        Convergent boundary: crust is recycled into mantle; andesitic volcanism; major earthquake zones

        Tangential boundary: crust is neither formed nor recycled; strong earthquakes

 

Observation: Histogram of altitudes has a bimodal distribution à Presence of two types of crust (Fig. 2):

         Continental Crust: Granitic, 30à100 km thick, density 2700 kg/m3

        Average height ~800 m

        Maximum height: Mt. Everest 8,800 m

         Oceanic crust: Basaltic, 6à15 km thick, density 2900 kg/m3

        Average depth ~ 3800 m

        Maximum depth Mariana Trench 11,000 m

The break in the distribution is somewhat below sealevel, indicating that part of the continental crust is flooded as this time (continental shelf).

 

Three types of converging boundaries:

Oceanic-oceanic

à    trench + island arc:

à    Marianas

Oceanic-continental

à    trench + volcanic mountain range:

à    Andes

Continental-continental

à    mountain range + plateau:

à    Himalayas + Tibet

 

Fig. 3 summarizes the processes of Plate Tectonics

 

History of the Earth system:

         Geologic times scales

         Two dating methods:

        Geologic times scale: Relative

        Radiometric time scale: Absolute

 

The Geologic time system (Fig. 4)

 

         Age of Earth: 4.56 Ga

         Turnover time for Mantle: 1 Ga

         Opening of Atlantic: 200 Ma

         Extinction of Dinosaurs: 65 Ma

         Onset of subduction off Oregon: 10 Ma

 

Focus on Metals:

         Categories:

         Iron and Ferro-alloy metals (Fe, Ni, Mn, Mo)

         Base metals: Cu, Zn, Pb and Sn

         Light metals: Al, Mg

         Noble Metals: Au, Ag, Pt

         Special use metals: Ti, Ga, Ge

         Fuels: Th, U

 

History of mine production and population (Fig. 5):

 

Observations:

Increase in mine production steeper than population increase

 

More Fe mined than other metals combined

 

Increase in production is parallel in most cases

 

Exceptions: Al, Sn, Pb

 

Large minima in all production lines