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Metamorphism – transformation of one rock type into another ,[object Object]
 Parent rock – origin of a metamorphic rockSee next slides for samples of metamorphic rocks
Norway
China
Lake Huron, Ontario, Canada
Michigan, North America
California, North America
California, North America
Metamorphism leads to changes in: ,[object Object]
 Texture
 Chemical compositionMetamorphic agents are: ,[object Object]
 Pressure
 Chemically active fluids,[object Object]
Degrees of metamorphism ,[object Object]
 High-grade metamorphism : identity of parent rock becomes hard to distinguish
 Remember : parent rock should not melt, if it does, then igneous processes (not metamorphic) become involved,[object Object]
Example of high-grade metamorphism: from shale (top) to slate (top right) to gneiss (right)
Degrees of metamorphism Agents of metamorphism Time low-grade LOW SHORT Heat Pressure Chemical activity HIGH high-grade LONG
Heat as an agent of metamorphism Heat provides the energy of activation for the chemical transformation in metamorphic rocks. Chemical reactions result in: ,[object Object]
formation of new minerals Chemical changes are all based on the increased kinetic energies of the ions.
Heat as an agent of metamorphism Temperatures increase with depth at a rate known as the geothermal gradient. Hence, degree of metamorphism increases as depth increases.
The deepest mine in the world The Western Deep Levels Mine in South Africa at 4 km is the deepest in the world. At these depths, the rock is actually hot enough to burn human skin.  Miners work in pairs- one digging, the other operating a large fan to keep cool.
What heats up the Earth? ,[object Object]
 Radioactivity – energy released when subatomic particles are spontaneously emitted by radioactive elements
 Solar radiation – absorbed and converted to thermal energy by the Earth’s surface,[object Object]
Solar radiation – the Earth’s crust absorbs about 50% of the Sun’s energy
The absorbed solar radiation is distributed unevenly.  The greatest concentration occurs in the tropical belt (red zone).
Radioactivity Radioactive elements contribute to Earth’s internal heat.  Background radiation (not enough to harm) exists all around us.  Shown at right is a geologist measuring background radiation with a portable Geiger counter.
Pressure as an agent of metamorphism Two types of pressure: ,[object Object]
 Differential stress – forces are unequal in different directions,[object Object]
 produces a more compact, denser rock,[object Object]
Directonial stress deforms rock layers as shown in C.  (the series shows the deformation of sediments deposited in a river flood plain)
The layers of rock shown below have been deformed by directional stress.  Such pressure is most active in convergent plate boundaries.
Rocks in shallow depths are pulverized when subjected to differential stress. At greater depths, on the other hand, rocks are more ductile and are compressed and elongated rather than crushed. A sample of conglomerate becomes metaconglomerate when subjected to differential stress at depth (note the elongated rock fragments).
Heat and pressure Heat increases with increasing pressure.  This means that areas of mountain building (continental vs continental convergent plates) are hotter due to greater pressure.
METAMORPHIC ROCKS ,[object Object]
 degrees of metamorphism
 agents of metamorphism,[object Object]
 regional metamorphism
 dynamic metamorphism,[object Object]
Contact metamorphism
Contact metamorphism
Contact metamorphism
Contact metamorphism Granite Gneiss
From limestone to marble
From igneous rocks to marble Syenite (igneous) marble
From sediments to metamorphic rocks
Regional metamorphism Mountain-building: ,[object Object]
 directional stresses are involved
 greatest volume of metamorphic rocks are produced in this way,[object Object]
Regional metamorphism
Regional vs contact metamorphism
Textural changes Texture – size, shape, and distribution of particles that constitute a rock ,[object Object]
 non-foliated,[object Object]
Types of foliation: ,[object Object]
 schistosity – larger crystals
 gneissic texture – segregation of minerals,[object Object]
Rock or  Slaty cleavage
Rock or Slaty cleavage
Schistocity mica schist – most abundant schist type
Schistocity mica schist
Schistocity
Schistocity
Schistocity
Schistocity
Schistocity talc schist
Schistocity talc schist

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Metamorphism