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Chapter Three ROCKS

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Page 1: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Chapter Three

ROCKS

Page 2: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Section 3-1 Classifying Rocks

• When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral composition.– Using color and texture, geologists can classify

a rock according to its origin.– Texture is the look that results from the size,

shape, and pattern of the rocks grains.

Page 3: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-1

• Coarse-grained: the grains are large and easy to see.

• Fined-grained: the grains are small and can been seen under a microscope or hand-lens.– Some rock’s grains results from the shape of

the crystals that form the rock.– In other rocks, the grain shapes result from

fragments of other rock.

Page 4: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Texture

Page 5: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Texture

Page 6: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-1

• The three major groups of rock are:– Igneous: forms from the cooling of molten

rock.– Sedimentary: forms when particles of other

rocks of the remains of plants and animals are pressed and cemented together.

– Metamorphic: forms when an existing rock is changed by heat, pressure, or chemical reactions.

Page 7: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-2 Igneous Rock

• Igneous rock is any rock that forms from magma or lava. Most igneous rocks are made of mineral crystals. Igneous rocks are classified according to their origin, texture, and mineral composition.

Page 9: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Extrusive Rock

– Extrusive rock: is igneous rock formed from lava that erupted onto Earth’s surface.

• Basalt is the most common extrusive rock.

Page 10: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Extrusive Rock

Page 11: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-2

– Intrusive rock: Igneous rock that formed when magma hardened beneath the Earth’s surface.• Granite is the most abundant intrusive

rock.– The texture of an igneous rock depends

on the size and shape of its mineral crystals.

Page 12: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

• Texture may be fine-grained, coarse-grained, porphyritic, or glassy.

– Fined-grained: rapid cooling lava forms fined-grained.

– Coarse-grained: slow cooling lava forms coarse-grained.

– Porphyritic: large crystals scattered on top of small crystals. This occurs when magma cools in two stages, first slow, and then rapidly as magma moves near to the surface.

Page 13: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Intrusive RockGranite

Page 14: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Intrusive RockGabbros

Page 15: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Intrusive RockDiorite

Page 16: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-2

• Lava low in silica forms dark-colored rocks, such as basalt.

• Magma that is high in silica usually forms light colored rocks, such as granite.

• Many igneous rocks are hard, dense, and durable. People use igneous rock for tools and building materials.

Page 17: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-3 – Sedimentary Rock

• Sedimentary rocks form from particles deposited by water and wind. Sand, mud, and pebbles. Sediment is small, solid pieces of material that come from rocks or living things.

1. Erosion: running water or wind loosen and carry fragments of rock.

2. Deposition: the process by which sediment settles out of the water or wind.

3. Compaction: the process that presses sediments together.

4. Cementation: the process in which dissolved minerals crystallize and glue particles of sediment together.

Page 18: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-3

• There are three major groups of sedimentary rocks:

– Clastic rock: sedimentary rock that forms when rock fragments are squeezed together. Sandstone is a clastic rock formed from the compaction and cementation of sand.

– Organic Rock: forms where the remains of plants and animals are deposited in thick layers. Coal is formed from the remains of swamp plants and limestone is formed from the hard shells of living things – seashells.

– Chemical Rock: when minerals that are dissolved in a solution crystallize. Chemical rocks also form from mineral deposits left when seas or lakes evaporate.

Page 19: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Sedimentary Rock

• Sandstone

Page 20: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Sedimentary Rock

• Gypsum

Page 21: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Samples of Sedimentary Rock

• Shale

Page 22: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-4 Rocks from Reefs

• Coral animals are tiny relatives of jellyfish that live together in vast numbers. They build skeletons that grow together to form a structure called a coral reef.

• Coral reefs only form in warm, shallow tropical waters.

• When coral animals die, their skeletons remain, and new corals build on top of them.

• There are three types of coral reefs: fringing reefs, barrier reefs, and atolls.

• A coral reef is really organic limestone.

Page 24: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Barrier Reef

Page 26: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Coral Reefs

Page 27: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Coral Reefs

Page 28: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-5 Metamorphic Rock

• Every metamorphic rock is a rock that has changed its form. Heat and pressure deep beneath Earth’s surface can change any rock into metamorphic rock. Metamorphic rock can form out of igneous, sedimentary, or other metamorphic rock.– Geologists classify metamorphic rocks by the

arrangement of the grains that make up the rocks.• Metamorphic rocks that have their grains arranged in parallel

layers or bands are said to be foliated – slate is the most common.

• Metamorphic rocks that have grains arranged randomly. Marble and Quartz.

Page 29: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Metamorphic Rock Samples

Page 30: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Metamorphic Rock Samples

• Marble

Page 31: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Metamorphic Rock Sample

• Quartz

Page 32: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

3-6 Rock Cycle

• Forces inside Earth and at the surface produce a rock cycle that builds, destroys, and changes the rocks in the crust.– The rock cycle is a series of processes on and

beneath Earth’s surface that slowly change rocks from one kind to another.

Page 34: Chapter Three ROCKS. Section 3-1 Classifying Rocks When studying a rock sample, geologists observe the rock’s color and texture and determine its mineral

Rock Pictures - Lava

• http://www.hoho.co.uk/html/lanzarote_lava_and_rocks.html