Rocks are made of minerals. Minerals can break
down and form new minerals. Three types of rocks are: igneous, sedimentary,
and metamorphic. Igneous rocks are made when molten magma solidifies.
Sedimentary rocks form when rock debris becomes cemented. Metamorphic
rocks form when rocks melt again and change form.
Granitic
rocks are a type of igneous
rock. Igneous rock is formed by the cooling and solidification of
molten material (magma).
There are two types of igneous rock: volcanic
and plutonic. Yosemite was formed from plutonic rock that cooled
deep beneath the surface of the Earth. The bedrock of much of the
Sierra Nevada range is part of a vast field of rock that extends
downward many miles.
This field of rock is called a batholith
(from the Greek word bathos, meaning deep, and lithos, meaning rock).
The batholith is not one uniform mass of granite.
It is made up of a group of individual masses of rock called plutons
(named for Pluto, god of the underworld). Plutons can vary in size
from 1.6 kilometers (1 mile) to many kilometers in extent. Some
plutons are next to each other. Other plutons are separated by areas
of metamorphic
rock. The Sierra Nevada batholith is a collection of granite plutons.
The image above contains an animation depicting
this process. Click the right arrow to begin the animation. When
the right arrow reappears, click it again to see the next step.
(You can also download the Flash
Player if you need it to play the animation.)
The plutons formed during separate episodes of
magma intrusion. Molten rock, lighter than the older host rock surrounding
it, rose slowly and intruded into these host rocks. As the magma
came within a few kilometers of the surface, it began to cool. After
a long time the magma cooled completely. The minerals
in the magma crystallized and solidified to form the igneous granitic
rock of the Sierra Nevada.
Yosemite National Park
Home Page
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Last modified
Wednesday, 22-Dec-2004 10:14:49 Eastern Standard Time
Yosemite National Park Web
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