Rocks & Minerals
Chapter 8 Study Guide
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Earth’s crust is made up of rocks
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Rocks are made up of natural, nonliving solid crystals that are called minerals.
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All minerals are made of crystals that have certain physical properties. Minerals are a repeated crystal pattern.
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Mica is a common mineral that forms rocks.
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Rocks differ from each other. They are made up of different combinations of minerals.
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Minerals are identified by their physical properties such as color, luster, hardness, streak, and cleavage.
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Mohr’s scale for hardness ranks minerals from 1 to 10. The greater the Mohr’s ranking the harder the mineral is. Quartz has a hardness of 7 on the Mohr’s scale.
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Talc is a very soft mineral.
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Metamorphic rocks are formed when rocks are changed by great heat and pressure.
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Igneous rocks are formed when magma or lava cools and gardens.
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Halite is another term for salt.
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Some rocks are more compact, such as obsidian, so they will weigh more. While porous rocks, such as pumice, are lighter.
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Sedimentary rocks are formed when layers of sediment are weighed down and harden.
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Scientist can tell many things form a fossil. They can tell what ancient plant or animal life was like, what the animal looked like, what the environment was like, and how the environment has changed since then.
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Fossils are formed in sedimentary rocks; the heat and pressure required to form either metamorphic or igneous rock would destroy a fossil.
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Soil forms when weathering causes rocks to break apart, such as with water and plant roots. Soil contains small bits of rock, decaying plants and animals, and tiny life forms.