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THE ROCK CYCLE
WHAT YOU LEARN
 To distinguish between minerals and rocks
 How rocks are classified
 How rocks are constantly recycled providing raw materials for other rocks
HOW ROCKS RECYCLE
The rock cycle is a general model that describes how various geological processes create,
modify, and influence rocks.
the origin of all rocks can be ultimately traced back to the solidification of molten
magma.
Magma consists of a partially melted mixture of elements and compounds commonly
found in rocks.
Magma exists just beneath the solid crust of the Earth in an interior zone known as the
mantle. (Figure 1)
All rock types can be physically and chemically decomposed by a variety of surface processes
collectively known as weathering.
The debris that is created by weathering is often transported through the landscape by erosional
processes via streams, glaciers, wind, and gravity.
When this debris is deposited as a permanent sediment, the processes of burial,
compression, and chemical alteration over long periods of time produce sedimentary
rocks
A number of geologic processes, like tectonic folding and faulting, can exert heat and
pressure on both igneous and sedimentary rocks causing them to be altered physically or
chemically. Rocks modified in this way are termed metamorphic rocks
Composition of the Crust
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
The earth’s crust is composed of rocks
Rocks are composed of minerals
What is a mineral?
A mineral is:



A naturally occurring inorganic substance
With a definite chemical composition and
Characteristic atomic structure
Rock Classification


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Igneous Rocks form from the cooling and crystallization of magma.
Sedimentary Rocks form from lithification of sediments from other rocks.
Metamorphic Rocks form from recrystallization of other rocks due to heat,
pressure, and chemical alteration.
IGNEOUS ROCKS
Igneous Rocks Are Subdivided Into Two Classes
1. Volcanic (Extrusive) Igneous Rocks
Volcanic extrusive igneous rocks form at the earth's surface as lava cools.

Basalt



Basalt is the most widespread volcanic rock.
It is a dark, fine-grained rock.
Basalt is the rock of the sea floor.
2. Plutonic (or Intrusive) Igneous Rocks



Plutonic igneous rocks form deep underground where magma cools
slowly
Plutonic rocks have a coarse crystalline texture.
Granite
 Granite is the most widespread of plutonic igneous rocks.
 It underlies much of the continental crust.
SEDIMENTARY ROCKS
Most sedimentary rocks are formed of layers of materials that have washed into
lakes, rivers, and the ocean.



Sedimentary Rocks Form Strata
Sometimes these layers are tilted by earth movements.
Sedimentary Rocks Contain Fossils
Subclasses of Sedimentary Rocks
1.
2.
3.
Clastic: rocks form from bits and pieces of other rocks.
Chemical: rocks consist of minerals deposited from a solution.
Organic: rocks consist of organic matter such as plants and animal remains.
How do sediments turn into hard rock?
Lithification Processes:



Compaction
Cementation
Crystallization
Organically-Formed Sedimentary Rocks
Organically-formed sedimentary rocks form from the remains of plants and
animals.


Fossil limestone
Coal
METAMORPHIC ROCKS
Metamorphic rocks are rocks that have been changed in form due to heat, pressure,
and chemical alteration.
FOLIATED
NONFOLIATED
Slate
Marble
Schist
Quartzite
Gneiss
SUMMARY
Igneous Rocks
 Volcanic (Extrusive) Igneous
 Plutonic (Intrusive) Igneous
Sedimentary
 Clastic
 Chemical
 Organic
Metamorphic
 Foliated
 Nonfoliated
The Rock Cycle shows how rocks of any rock class can be recycled into rocks of any other
rock class.
of the rock types described above can be returned to the Earth's interior by tectonic forces at
areas known as subduction zones. Once in the Earth's interior, extreme pressures and
temperatures melt the rock back into magma to begin the rock cycle again.