Chapter 7 Earth's Rocks

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Created by:

jlevan Plus on March 22, 2012

Subjects:

Science 6 Chapter 7

Description:

Earth's Rocks

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Chapter 7 Earth's Rocks

Mineral

A natural, solid substance that has a definite chemical composition and physical structure.
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Terms

Definitions

Mineral
A natural, solid substance that has a definite chemical composition and physical structure.
Igneous rock
Rock that forms when melted rock cools and hardens.
lava
Magma that is exposed at Earth's Surface
sedimentary rock
Rock that forms when layers of sediment settle and are cemented together
magma
Melted rock within Earth
metamorphic rock
Rock that forms when igneous, sedimentary, or metamorphic rock is changed by pressure, high temperature, very hot water, or a combination of these factors
metamorphism
The process by which metamorphic rock forms.
rock cycle processes that change rock from one type to another type
bedrock
The bottom layer of soil, made mostly of solid rock
topsoil
The top layer of soil, made in part from broken pieces of lower layers of rock
Cave Crystals
Minerals grow as crystals. If there is enough space they can grow to be as large as 3ft. in diameter and about 50 ft. long.
Rock layers The Grand Canyons dramatic drop provides a cutaway view of this.
Carved by Water ...Over thousand of years, erosion of the rock by the Potomas River has caused the Great Falls to move 9 miles upstream.
Ancient Secrets In the 1400's the Inca people of the Andes Mountains used terraces to grow 20 varieties of corn and more than 240 varieties of potato. The terraces prevented rain from eroding what little good soil there was in the high mountains.
What effect do high temperature and pressure have on igneous rock? They change igneous rock to metamorphic rock.
What characteristic of soil might be most important to farmers? the amount of water it can retain
What best explains the glassy look of obsidian? It cooled very quickly
A way that layers of sedimentary rock bind together? by pressure
a cause of regional metamorphism mountain building


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