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is a solid combination of
more than one mineral
formations.
is a solid formation
that occurs naturally
in the earth.
Igneous Rocks
•   These are rocks formed by the cooling of
    molten rock (magma.)


       volcano                           Magma
                                         cools and
                                         solidifies
                                         forming
                                         igneous
                                         rocks



                 magma
Sedimentary Rocks
•   Sedimentary Rocks are rocks
    formed when particles of
    sediment build up and are




                                                           Getting older
    “cemented together” by the
    effect of pressure and minerals.

                       Fragments washed to the sea



    Rocks are broken
    up by the action
    of weather                                       sea

                               Sedimentary
                               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.


                    Pressure from surface
                    rocks


      metamorphic
                       rock
                              forming
                                            here

     Magma            heat
 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
 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
Coarse-Grained   Fine-Grained




Felsic


           Granite          Rhyolite

Mafic




            Gabbro          Basalt
 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
____________ 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?
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
 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
                           http://www.fi.edu/fellows/payton/rocks/create/sediment.htm

  compacted and cemented
   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
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.
Clastic – made of fragments of rock
    cemented together with calcite or quartz
Breccia 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.
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.
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.
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.
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.
 Meaning to change shape

 Changes with temperature
  and pressure, but remains
  solid

 Usually takes place deep in

 the Earth                 http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm
 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&edu=h igh&fr=t
 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&edu=h igh&fr=t
     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
 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.
 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.
 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.
 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.
 Determine if the following rock samples are
 foliated or non-foliated:




  Amphibolite      Quartzite       Phyllite


                                  Foliated
The Rock Cycle
  Igneous


            metamorphic


   Sedimentary
 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
Coarse-Grained   Fine-Grained




Felsic


           Granite          Rhyolite

Mafic




            Gabbro          Basalt
 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
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
 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
                           http://www.fi.edu/fellows/payton/rocks/create/sediment.htm
Clastic – made of fragments of rock
    cemented together with calcite or quartz
Breccia 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.
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.
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.
 Meaning to change shape

 Changes with temperature
  and pressure, but remains
  solid

 Usually takes place deep in

 the Earth                 http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm
 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&edu=h igh&fr=t
     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
 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.
 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.
The Rock Cycle
  Igneous


            metamorphic


   Sedimentary
EarthSci 3 - Minerals and Rocks
EarthSci 3 - Minerals and Rocks
EarthSci 3 - Minerals and Rocks
EarthSci 3 - Minerals and Rocks
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EarthSci 3 - Minerals and Rocks

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  • 22.
  • 23. is a solid combination of more than one mineral formations.
  • 24.
  • 25.
  • 26. is a solid formation that occurs naturally in the earth.
  • 27.
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  • 48.
  • 49.
  • 50.
  • 51.
  • 52. Igneous Rocks • These are rocks formed by the cooling of molten rock (magma.) volcano Magma cools and solidifies forming igneous rocks magma
  • 53.
  • 54. Sedimentary Rocks • Sedimentary Rocks are rocks formed when particles of sediment build up and are Getting older “cemented together” by the effect of pressure and minerals. Fragments washed to the sea Rocks are broken up by the action of weather sea Sedimentary rocks
  • 55.
  • 56. 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. Pressure from surface rocks metamorphic rock forming here Magma heat
  • 57.  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
  • 58.  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
  • 59. Coarse-Grained Fine-Grained Felsic Granite Rhyolite Mafic Gabbro Basalt
  • 60.  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
  • 61. ____________ 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?
  • 62.
  • 63. 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
  • 64.  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 http://www.fi.edu/fellows/payton/rocks/create/sediment.htm compacted and cemented
  • 65.
  • 66.
  • 67.
  • 68. 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
  • 69.
  • 70. 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.
  • 71.
  • 72. Clastic – made of fragments of rock cemented together with calcite or quartz Breccia 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.
  • 73. 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.
  • 74.
  • 75. 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.
  • 76. 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.
  • 77.
  • 78. 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.
  • 79.  Meaning to change shape  Changes with temperature and pressure, but remains solid  Usually takes place deep in the Earth http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm
  • 80.  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&edu=h igh&fr=t
  • 81.
  • 82.  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&edu=h igh&fr=t
  • 83. 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
  • 84.  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.
  • 85.
  • 86.  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.
  • 87.  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.
  • 88.
  • 89.  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.
  • 90.  Determine if the following rock samples are foliated or non-foliated: Amphibolite Quartzite Phyllite Foliated
  • 91.
  • 92.
  • 93. The Rock Cycle Igneous metamorphic Sedimentary
  • 94.
  • 95.
  • 96.
  • 97.  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
  • 98. Coarse-Grained Fine-Grained Felsic Granite Rhyolite Mafic Gabbro Basalt
  • 99.  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
  • 100.
  • 101. 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
  • 102.
  • 103.  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 http://www.fi.edu/fellows/payton/rocks/create/sediment.htm
  • 104.
  • 105.
  • 106.
  • 107.
  • 108.
  • 109. Clastic – made of fragments of rock cemented together with calcite or quartz Breccia 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.
  • 110.
  • 111. 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.
  • 112.
  • 113. 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.
  • 114.
  • 115.  Meaning to change shape  Changes with temperature and pressure, but remains solid  Usually takes place deep in the Earth http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm
  • 116.
  • 117.  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&edu=h igh&fr=t
  • 118. 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
  • 119.
  • 120.  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.
  • 121.
  • 122.  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.
  • 123.
  • 124.
  • 125. The Rock Cycle Igneous metamorphic Sedimentary

Notes de l'éditeur

  1. Convergent boundaries are where the plates move towards each other. There are three types of convergent boundary, each defined by what type of crust (continental or oceanic) is coming together. Therefore we can have: continent-continent collision, continent-oceanic crust collision or ocean-ocean collision….