earthsci 3 - minerals and rocks

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Page 1: EarthSci 3 - Minerals and Rocks
Page 2: EarthSci 3 - Minerals and Rocks
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is a solid combination of more than one mineral formations.

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is a solid formation that occurs naturally in the earth.

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Igneous Rocks• These are rocks formed by the cooling of

molten rock (magma.)

magma

volcano Magma cools and solidifies forming igneous rocks

Page 53: EarthSci 3 - Minerals and Rocks
Page 54: EarthSci 3 - Minerals and Rocks

Sedimentary Rocks• Sedimentary Rocks are rocks

formed when particles of sediment build up and are “cemented together” by the effect of pressure and minerals.

sea

Fragments washed to the sea

Sedimentary rocks

Rocks are brokenup by the actionof weather

Gettin

g o

lder

Page 55: EarthSci 3 - Minerals and Rocks
Page 56: EarthSci 3 - Minerals and Rocks

Metamorphic Rocks• Metamorphic rocks are formed by the effect

of heat and pressure on existing rocks.• This can greatly affect the hardness, texture

or layer patterns of the rocks.

Magma

metamorphic

rockforming

here

heat

Pressure from surface rocks

Page 57: EarthSci 3 - Minerals and Rocks

Igneous rock begins as magma.Magma can form:

▪ When rock is heated▪ When pressure is released▪ When rock changes composition

Magma freezes between 700 °C and 1,250 °C

Magma is a mixture of many minerals

http://www.fi.edu/fellows/payton/rocks/create/igneous.htm

Page 58: EarthSci 3 - Minerals and Rocks

Felsic: light colored rocks that are rich in elements such as aluminum, potassium, silicon, and sodium

Mafic: dark colored rocks that are rich in calcium, iron, and magnesium, poor in silicon

Coarse-grained: takes longer to cool, giving mineral crystals more time to grow

Fine-grained: cools quickly with little to no crystals

Page 59: EarthSci 3 - Minerals and Rocks

Felsic

Mafic

Coarse-Grained

Fine-Grained

Granite

Gabbro Basalt

Rhyolite

Page 60: EarthSci 3 - Minerals and Rocks

Intrusive Igneous Rocks: magma pushes into surrounding rock below the Earth’s surface

Extrusive Rocks: forms when magma erupts onto the Earth’s surface (lava), cools quickly with very small or no crystals formed

http://www.windows.ucar.edu/tour/link=/earth/geology/ig_intrusive.html&edu=high&fr=t

Page 61: EarthSci 3 - Minerals and Rocks

Obsidian

What is Obsidian?

Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.

____________ is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form. Is this rock

Felsic or Mafic?

Is it fine-grained or coarse-grained?

Is this rock Intrusive or Extrusive?

Page 62: EarthSci 3 - Minerals and Rocks
Page 63: EarthSci 3 - Minerals and Rocks

Obsidian

What is Obsidian?

Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.

Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form. Is this rock

Felsic or Mafic?

Is it fine-grained or coarse-grained?

Is this rock Intrusive or Extrusive?

Mafic, fine grained, extrusive

Page 64: EarthSci 3 - Minerals and Rocks

http://www.fi.edu/fellows/payton/rocks/create/sediment.htm

Sedimentary rock is formed by erosion

Sediments are moved from one place to another

Sediments are deposited in layers, with the older ones on the bottom

The layers become compacted and cemented together

Page 65: EarthSci 3 - Minerals and Rocks
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Sedimentary Rocks are formed at or near the Earth’s surface

No heat and pressure involved

Strata – layers of rock

Stratification – the process in which sedimentary rocks are arranged in layers

Page 69: EarthSci 3 - Minerals and Rocks
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Clastic – made of fragments of rock cemented together with calcite or quartz_________ is a term

most often used for clastic sedimentary rocks that are composed of large angular fragments (over two millimeters in diameter).

The spaces between the large angular fragments can be filled with a matrix of smaller particles or a mineral cement that binds the rock together.

Page 71: EarthSci 3 - Minerals and Rocks
Page 72: EarthSci 3 - Minerals and Rocks

Clastic – made of fragments of rock cemented together with calcite or quartzBreccia is a term most

often used for clastic sedimentary rocks that are composed of large angular fragments (over two millimeters in diameter).

The spaces between the large angular fragments can be filled with a matrix of smaller particles or a mineral cement that binds the rock together.

Page 73: EarthSci 3 - Minerals and Rocks

Chemical Sedimentary – minerals crystallize out of solution to become rock

__________is a sedimentary rock composed primarily of calcium carbonate (CaCO3) in the form of the mineral calcite. It most commonly forms in clear, warm, shallow marine waters.

It is usually an organic sedimentary rock that forms from the accumulation of shell, coral, algal and fecal debris.

Page 74: EarthSci 3 - Minerals and Rocks
Page 75: EarthSci 3 - Minerals and Rocks

Chemical Sedimentary – minerals crystallize out of solution to become rock

Limestone is a sedimentary rock composed primarily of calcium carbonate (CaCO3) in the form of the mineral calcite. It most commonly forms in clear, warm, shallow marine waters.

It is usually an organic sedimentary rock that forms from the accumulation of shell, coral, algal and fecal debris.

Page 76: EarthSci 3 - Minerals and Rocks

Organic sedimentary – remains of plants and animals

_________ is an organic sedimentary rock that forms from the accumulation and preservation of plant materials, usually in a swamp environment. 

Coal is a combustible rock and along with oil and natural gas it is one of the three most important fossil fuels. 

Page 77: EarthSci 3 - Minerals and Rocks
Page 78: EarthSci 3 - Minerals and Rocks

Organic sedimentary – remains of plants and animals

Coal is an organic sedimentary rock that forms from the accumulation and preservation of plant materials, usually in a swamp environment. 

Coal is a combustible rock and along with oil and natural gas it is one of the three most important fossil fuels. 

Page 79: EarthSci 3 - Minerals and Rocks

http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm

Meaning to change shape

Changes with temperature and pressure, but remains solid

Usually takes place deep in the Earth

Page 80: EarthSci 3 - Minerals and Rocks

Contact Metamorphism – heated by nearby magma

Increased temperature changes the composition of the rock, minerals are changed into new minerals

_________ is a fine-grained non-foliated metamorphic rock produced by contact metamorphism http://www.windows.ucar.edu/tour/link=/earth/geology/meta_contact.html&ed

u=h igh&fr=t

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Page 82: EarthSci 3 - Minerals and Rocks

Contact Metamorphism – heated by nearby magma

Increased temperature changes the composition of the rock, minerals are changed into new minerals

Hornfels is a fine-grained non-foliated metamorphic rock produced by contact metamorphism http://www.windows.ucar.edu/tour/link=/earth/geology/meta_contact.html&ed

u=h igh&fr=t

Page 83: EarthSci 3 - Minerals and Rocks

Regional Metamorphism – pressure builds up in rocks that is deep within the Earth

Large pieces of the Earth’s crust collide and the rock is deformed and chemically changed by heat and pressure

http://www.windows.ucar.edu/tour/link=/earth/geology/meta_regional.html&edu=high&fr=t

Page 84: EarthSci 3 - Minerals and Rocks

Foliated - contain aligned grains of flat minerals

________ is foliated metamorphic rock that has a banded appearance and is made up of granular mineral grains.

It typically contains abundant quartz or feldspar minerals.

Page 85: EarthSci 3 - Minerals and Rocks
Page 86: EarthSci 3 - Minerals and Rocks

Foliated - contain aligned grains of flat minerals

Gneiss is foliated metamorphic rock that has a banded appearance and is made up of granular mineral grains.

It typically contains abundant quartz or feldspar minerals.

Page 87: EarthSci 3 - Minerals and Rocks

Non-Foliated – mineral grains are not arranged in plains or bands

_________ is a non-foliated metamorphic rock that is produced from the metamorphism of limestone.

It is composed primarily of calcium carbonate.

Page 88: EarthSci 3 - Minerals and Rocks
Page 89: EarthSci 3 - Minerals and Rocks

Non-Foliated – mineral grains are not arranged in plains or bands

Marble is a non-foliated metamorphic rock that is produced from the metamorphism of limestone.

It is composed primarily of calcium carbonate.

Page 90: EarthSci 3 - Minerals and Rocks

Determine if the following rock samples are foliated or non-foliated:

Amphibolite Quartzite Phyllite

Foliated

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Igneous

metamorphic

Sedimentary

The Rock Cycle

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Felsic: light colored rocks that are rich in elements such as aluminum, potassium, silicon, and sodium

Mafic: dark colored rocks that are rich in calcium, iron, and magnesium, poor in silicon

Coarse-grained: takes longer to cool, giving mineral crystals more time to grow

Fine-grained: cools quickly with little to no crystals

Page 98: EarthSci 3 - Minerals and Rocks

Felsic

Mafic

Coarse-Grained

Fine-Grained

Granite

Gabbro Basalt

Rhyolite

Page 99: EarthSci 3 - Minerals and Rocks

Intrusive Igneous Rocks: magma pushes into surrounding rock below the Earth’s surface

Extrusive Rocks: forms when magma erupts onto the Earth’s surface (lava), cools quickly with very small or no crystals formed

http://www.windows.ucar.edu/tour/link=/earth/geology/ig_intrusive.html&edu=high&fr=t

Page 100: EarthSci 3 - Minerals and Rocks
Page 101: EarthSci 3 - Minerals and Rocks

Obsidian

What is Obsidian?

Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.

Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form. Is this rock

Felsic or Mafic?

Is it fine-grained or coarse-grained?

Is this rock Intrusive or Extrusive?

Mafic, fine grained, extrusive

Page 102: EarthSci 3 - Minerals and Rocks
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http://www.fi.edu/fellows/payton/rocks/create/sediment.htm

Sedimentary rock is formed by weathering then sedimentation

Sediments are moved from one place to another

Sediments are deposited in layers, with the older ones on the bottom

The layers become compacted and cemented together

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Clastic – made of fragments of rock cemented together with calcite or quartzBreccia is a term most

often used for clastic sedimentary rocks that are composed of large angular fragments (over two millimeters in diameter).

The spaces between the large angular fragments can be filled with a matrix of smaller particles or a mineral cement that binds the rock together.

Page 110: EarthSci 3 - Minerals and Rocks
Page 111: EarthSci 3 - Minerals and Rocks

Chemical Sedimentary – minerals crystallize out of solution to become rock

Limestone is a sedimentary rock composed primarily of calcium carbonate (CaCO3) in the form of the mineral calcite. It most commonly forms in clear, warm, shallow marine waters.

It is usually an organic sedimentary rock that forms from the accumulation of shell, coral, algal and fecal debris.

Page 112: EarthSci 3 - Minerals and Rocks
Page 113: EarthSci 3 - Minerals and Rocks

Organic sedimentary – remains of plants and animals

Coal is an organic sedimentary rock that forms from the accumulation and preservation of plant materials, usually in a swamp environment. 

Coal is a combustible rock and along with oil and natural gas it is one of the three most important fossil fuels. 

Page 114: EarthSci 3 - Minerals and Rocks
Page 115: EarthSci 3 - Minerals and Rocks

http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm

Meaning to change shape

Changes with temperature and pressure, but remains solid

Usually takes place deep in the Earth

Page 116: EarthSci 3 - Minerals and Rocks
Page 117: EarthSci 3 - Minerals and Rocks

Contact Metamorphism – heated by nearby magma

Increased temperature changes the composition of the rock, minerals are changed into new minerals

Hornfel is a fine-grained non-foliated metamorphic rock produced by contact metamorphism http://www.windows.ucar.edu/tour/link=/earth/geology/meta_contact.html&ed

u=h igh&fr=t

Page 118: EarthSci 3 - Minerals and Rocks

Regional Metamorphism – pressure builds up in rocks that is deep within the Earth

Large pieces of the Earth’s crust collide and the rock is deformed and chemically changed by heat and pressure

http://www.windows.ucar.edu/tour/link=/earth/geology/meta_regional.html&edu=high&fr=t

Page 119: EarthSci 3 - Minerals and Rocks
Page 120: EarthSci 3 - Minerals and Rocks

Foliated - contain aligned grains of flat minerals

Gneiss is foliated metamorphic rock that has a banded appearance and is made up of granular mineral grains.

It typically contains abundant quartz or feldspar minerals.

Page 121: EarthSci 3 - Minerals and Rocks
Page 122: EarthSci 3 - Minerals and Rocks

Non-Foliated – mineral grains are not arranged in plains or bands

Marble is a non-foliated metamorphic rock that is produced from the metamorphism of limestone.

It is composed primarily of calcium carbonate.

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Igneous

metamorphic

Sedimentary

The Rock Cycle

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