Metamorphic Rock Essay
1058 WordsAug 16th, 20105 Pages
Metamorphism means to change form; this is exactly what metamorphic rocks do. This paper will take a look at the Earth’s rock cycle to examine exactly where the metamorphic rock fits into it. It will also look at how metamorphic rocks are formed and the relationship between metamorphic rocks and igneous rock and sedimentary rocks. This paper will examine the geological characteristics and materials of metamorphic rocks, and examine some examples of metamorphic rocks and will describe mineral composition of some examples and explain its economic uses.
The Rock Cycle The rock cycle helps people to understand the starting point of the igneous, sedimentary, and metamorphic rocks. In addition to explaining how each of the…show more content…
Regional metamorphism usually occurs during the formation of a mountain. Large amounts of rock are subject to extreme pressure and heat while the Earth’s crust is moving to create a mountain. Regional metamorphism also takes place when there is a collision of two continental plates. The force from the collision puts forth enough extreme pressure needed for a rock to go through a metamorphic change.
Relationship Among the Three Rock Groups
When sedimentary rock and igneous rock are exposed to extreme heat or pressure, they can change their appearance and mineral make up. The color and density of the rock can change as the mineral and density changes the structure of the rock. The rock under pressure and heat doesn't melt but the chemical or mineral structure of the rock condenses and compacts changing the rock to metamorphic rock. This chemical reaction will cause the rock to change color with the mineral grains and will give the appearance of strips. The metamorphic rock can keep changing its density and appearance when it is exposed to more heat and pressure. The rock type of granite gneiss and biotite schist that are found in the Green Mountains of Vermont are two types of metamorphic rock.
Examples of Metamorphic Rocks
There are many different types of metamorphic rocks that one can see on a regular basis; many probably do not realize they are metamorphic rocks. For example, slate
Essay/Term paper: Rock classification
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October 11, 1999
Rocks are classified to make it easier on people to identify them in the future. This can be done by a numerous amount of ways. Each rock type has their own specific ways, but there are two distinct characteristics that apply to all. These are texture and composition. These two, along with many others helps to classify igneous, sedimentary, and metamorphic rocks.
Igneous rocks are classified first by texture. This is broken down mainly into grain size. First there are intrusive, or plutonic igneous rocks. These types of rocks cool within the crust and forms large, visible crystals. The opposite would be extrusive, or volcanic rocks. These cool at the surface rapidly, forming small grains. A combination of the two would be porphyritic, large grains in an aphanitic, or extrusive matrix. Secondly, composition is used to classify igneous rocks. There are four types, ultramafic, mafic, intermediate, and felsic. Ultramafic rocks are very dark and contain and extreme amount of iron and magnesium. Mafic rocks are also dark in color; they too contain high iron and magnesium amounts. An example would be olivine, or pyroxene. Intermediate igneous rocks are made from silica and plagioclase. They tend to be grays and browns in color. Finally, felsic socks are light in color and contains high amounts of silica. Quartz and potassium feldspar are examples of felsic igneous rocks. Other types of rocks are classified similarly.
Sedimentary rocks form from the weathering of pre-existing rocks. The broken down particles are then compacted and cemented together after the sorting process is complete. Depending on what the sedimentary rock is formed by, determines whether is known as clastic or chemical. Clastic rocks are composed of particles from weathering. They are then sorted by grain size, gravel being the largest and clay being the smallest. A few examples would be sandstones and shales. Chemical sedimentary rocks are biochemical, and contain ions in the solution from weathering. These are also further classified. First you have limestone, which can be either organic or inorganic. An example would be fossiliferous or chalk. Next is dolostone, and it is formed from dolomite. Chert is next; and can be organic or inorganic also. Flint and jasper are some examples of chert. Rock salt and gypsum are what are known as evaporites. These form from the evaporation of saline waters in an arid environment. Finally there is coal, which is organic and forms from buried plant remains and carbon. There is one more type of rock that is classified the same way as the previous two.
Metamorphic rocks are pre-existing rocks that are changed by heat and pressure. The pre-existing rock is called the parent rock, or protolith. Metamorphism occurs in these rocks when the minerals become instable. There are two types of metamorphism, contact and regional. Contact is high temperature, low pressure. It is basically a massive rock that is baked. Regional is high pressure and low temperature. Strong fabric, or layering, develops from this kind of metamorphism. Along with metamorphism, you get texture changes. The first is recrystallization, which is where you get new minerals from old. Some of the new minerals that form are micas, feldspars, and garnet. You can also get foliation, which is a planar fabric in a metamorphic rock. Simply, this is the alignment of minerals within the rock that are platy. Types of foliation are slaty cleavage, schistosity, and gneissic layering. Non-foliated rocks can also form. These are massive in size, uniform, and have no planar fabric. Marble and quartzite are the two best examples of a non-foliated metamorphic rock.
In conclusion, classification of rocks is a very important and difficult process. If rocks were not classified, then no one would know what rock was what, and that would end in chaos. All three families of rocks, igneous, sedimentary, and metamorphic are all classified mainly by texture and composition. Each family has different ways and names for this process, but it basically the same thing. All in all, classification of rocks comes down to the texture is contains, whether it has large, visible grains or small grains, and what the rock itself is comprised of.
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