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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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Earth Science Chapter 4 1
Rocks
Chapter 4
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
Earth Science Chapter 4 3
Rock-forming minerals
• About twenty minerals that make up most rocks on Earth’s crust
Earth Science Chapter 4 4
Granite
• Made of quartz, feldspar, hornblende, and mica
• May also contain other minerals• Generally light-colored• High silica content
Earth Science Chapter 4 5
Basalt
• Dark-colored• Low in silica• Very small mineral crystals
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
Earth Science Chapter 4 7
Texture
• The look and feel of a rock’s surface
Earth Science Chapter 4 8
Igneous rock
• From Latin term meaning “from fire”• Hardened magma or lava
Earth Science Chapter 4 9
Sedimentary rock
• Compressed or cemented sediment• Sediment – rocks, minerals, and organic
matter that has been broken into fragments
Earth Science Chapter 4 10
Metamorphic rock
• Means “changed form”• Existing rock is altered by tremendous
pressure, extreme heat, or chemical processes
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?
Earth Science Chapter 4 12
Igneous rock
• Formed from lava or magma• Classified by origin, texture, and mineral
composition
Earth Science Chapter 4 13
Origin
• Extrusive rock• From lava• Basalt is most common
• Intrusive rock• From magma• Granite is most common
Earth Science Chapter 4 14
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
Earth Science Chapter 4 15
Silica
• Material formed form oxygen and silicon
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
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
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.
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.
Earth Science Chapter 4 20
Sediment
• Small, solid pieces• Come from rock, shells, bones, leaves, etc.
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.
Earth Science Chapter 4 22
Erosion
• Running water, wind, or ice loosen and carry away fragments of rock
Earth Science Chapter 4 23
Deposition
• Sediment settles out of the water or wind carrying it
• Sinks to the bottom of the water
Earth Science Chapter 4 24
Compaction
• Sediments are pressed together by weight of layers above
• Minerals dissolve in the water
Earth Science Chapter 4 25
Cementation
• Dissolved minerals crystallize and glue particles together
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.
Earth Science Chapter 4 27
Major groups of sedimentary rocks
• Clastic rocks• Organic rocks• Chemical rocks
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
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)
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
Earth Science Chapter 4 31
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
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?
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
Earth Science Chapter 4 34
Foliated rocks
• Grains arranged in parallel layers or bands• May split apart along these bands
Earth Science Chapter 4 35
Nonfoliated rocks
• Mineral grains arranged randomly
Earth Science Chapter 4 36
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
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?
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
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?