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Earth Science Chapter 4 1 Rocks Chapter 4

Rocks

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Rocks. Chapter 4. Rock. Material that makes up solid parts of Earth Can be made of one or more minerals Solid organic matter Noncrystalline matter, such as glass. Rock-forming minerals. About twenty minerals that make up most rocks on Earth’s crust. Granite. - PowerPoint PPT Presentation

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Page 1: Rocks

Earth Science Chapter 4 1

Rocks

Chapter 4

Page 2: Rocks

Earth Science Chapter 4 2

Rock• Material that makes up solid parts of Earth• Can be made of

• one or more minerals• Solid organic matter• Noncrystalline matter, such as glass

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Earth Science Chapter 4 3

Rock-forming minerals

• About twenty minerals that make up most rocks on Earth’s crust

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Earth Science Chapter 4 4

Granite

• Made of quartz, feldspar, hornblende, and mica

• May also contain other minerals• Generally light-colored• High silica content

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Earth Science Chapter 4 5

Basalt

• Dark-colored• Low in silica• Very small mineral crystals

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Earth Science Chapter 4 6

Grains

• Small particles of minerals or other rocks that make up a rock

• Grain size• Coarse, fine, or not visible

• Grain shape• Rounded or jagged

• Grain pattern• Nonbanded or banded

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Earth Science Chapter 4 7

Texture

• The look and feel of a rock’s surface

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Earth Science Chapter 4 8

Igneous rock

• From Latin term meaning “from fire”• Hardened magma or lava

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Sedimentary rock

• Compressed or cemented sediment• Sediment – rocks, minerals, and organic

matter that has been broken into fragments

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Metamorphic rock

• Means “changed form”• Existing rock is altered by tremendous

pressure, extreme heat, or chemical processes

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Earth Science Chapter 4 11

Discuss

• What three characteristics do geologists use to identify rocks?

• What are the grains of a rock?• What are the three main groups of rocks?• Gneiss is a kind of rock that forms when

heat and pressure inside Earth change granite. To what group of rocks does gneiss belong?

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Earth Science Chapter 4 12

Igneous rock

• Formed from lava or magma• Classified by origin, texture, and mineral

composition

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Origin

• Extrusive rock• From lava• Basalt is most common

• Intrusive rock• From magma• Granite is most common

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Texture

• Depends on size and shape of mineral crystals• Some igneous rocks cool so quickly that they

lack crystal structure• Intrusive rocks have larger crystals

• Cooled more slowly

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Earth Science Chapter 4 15

Silica

• Material formed form oxygen and silicon

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Earth Science Chapter 4 16

Mineral composition• Lava low in silica forms dark-colored rocks

• Basalt has feldspar and dark-colored minerals, but no quartz

• Magma high in silica forms light-colored rocks• Granite rich in feldspar is speckled pink• Granite rich in hornblende and mica is light gray with

dark specks• Quartz crystals add gray or smoky specks to granite

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Earth Science Chapter 4 17

Building materials from igneous rocks

• Granite is used for• Statues (over 3,500 years ago)• Fortresses (about 600 years ago)• Bridges, public buildings, and cobblestones

(1800s and 1900s)• Curbstones, floors, and countertops (today)

• Basalt is crushed and used in construction

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Earth Science Chapter 4 18

Other uses of igneous rocks

• Pumice’s rough surface makes it a good abrasive for cleaning and polishing.

• Obsidian was used by ancient peoples to make sharp tools.

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Earth Science Chapter 4 19

Discuss

• How are igneous rocks classified?• Compare and contrast granite and basalt in

terms of their origin and texture. Which is extrusive? Which is intrusive?

• Would pumice be a good material to use to make a floor? Explain.

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Earth Science Chapter 4 20

Sediment

• Small, solid pieces• Come from rock, shells, bones, leaves, etc.

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Earth Science Chapter 4 21

Sedimentary rock formation

• Sediment is deposited by water and wind.• Most sedimentary rocks are formed by

erosion, deposition, compaction, and cementation.

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Erosion

• Running water, wind, or ice loosen and carry away fragments of rock

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Earth Science Chapter 4 23

Deposition

• Sediment settles out of the water or wind carrying it

• Sinks to the bottom of the water

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Earth Science Chapter 4 24

Compaction

• Sediments are pressed together by weight of layers above

• Minerals dissolve in the water

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Cementation

• Dissolved minerals crystallize and glue particles together

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Earth Science Chapter 4 26

Discuss

• What is sediment?• In layers of sedimentary rock, where would

you expect to find the oldest layers? Explain.

• Place these steps in the formation of sedimentary rock in the proper sequence: compaction, erosion, cementation, deposition.

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Earth Science Chapter 4 27

Major groups of sedimentary rocks

• Clastic rocks• Organic rocks• Chemical rocks

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Earth Science Chapter 4 28

Clastic Rocks• Formed when rock fragments are squeezed

together• Shale

• Clay particles in thin, flat layers• Sandstone

• Forms from sand• Mostly quartz

• Conglomorate• Rounded rock fragments

• Breccia• Jagged rock fragments

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Earth Science Chapter 4 29

Organic Rocks

• Remains of plants and animals in thick layers• Coal

• Remains of swamp plants (takes millions of years to form)

• Limestone• Shells from coral, clams, and oysters (millions of

years to form)

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Earth Science Chapter 4 30

Chemical Rocks

• When minerals dissolved in solution crystallize• Limestone

• When dissolved calcite comes out of solution• Rock salt

• When seas or lakes evaporate

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Uses

• Flint arrowheads• Hard, yet can be shaped• Formed when silica settles out of water

• Sandstone and limestone building materials• Soft enough to be easily cut

• Limestone used in making cement and steel

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Earth Science Chapter 4 32

Discuss• What are the three main types of

sedimentary rock?• What process causes deposits of rock salt to

form? What type of sedimentary rock is rock salt?

• The particles of sediment that make up shale are not usually well cemented. Would shale be a good choice of building material in a wet climate?

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Earth Science Chapter 4 33

Metamorphic rock

• Can be made from any other rock being changed by heat and/or pressure

• May become smoother• Minerals in the rock may change into other

minerals• Classified according to the arrangement of

the grains that make up the rocks

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Earth Science Chapter 4 34

Foliated rocks

• Grains arranged in parallel layers or bands• May split apart along these bands

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Earth Science Chapter 4 35

Nonfoliated rocks

• Mineral grains arranged randomly

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Uses

• Marble• Limestone subjected to heat and pressure• Has fine, even grain• Can be cut thin or carved into shapes• Easy to polish• Flooring, statues, buildings

• Slate• Foliated – splits easily into flat pieces• Flooring, roofing, sidewalks, chalkboards

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Earth Science Chapter 4 37

Discuss

• What does metamorphic mean?• How do geologists classify metamorphic

rocks?• Describe foliated and nonfoliated rocks.• Which might be more useful for carving

chess pieces, marble or slate?

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Earth Science Chapter 4 38

Rock cycle

• Series of processes on Earth’s surface and in the crust and mantle that slowly change rocks from one kind to another

• Any of the three major types of rock can be changed into another of the three types

• There are many possible pathways a rock can follow

• See diagram on page 115

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Earth Science Chapter 4 39

Discuss

• Website• Define the rock cycle in your own words.• What must happen in order for any rock in

the rock cycle to become a sedimentary rock?