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Mr Parkes
   Earth Sciences
   4. The properties of rocks and minerals reflect the
    processes that formed them.
    As a basis for understanding this concept, students know:
    a. how to differentiate among igneous, sedimentary, and
    metamorphic rocks by their properties and methods of
    formation (the rock cycle).
    b. how to identify common rock-forming minerals (including
    quartz, calcite, feldspar, mica, and hornblende) and ore
    minerals using a table of diagnostic properties.
Crystals        Fossils        Gas bubbles      Glassy          Ribbonlike      Sand or
Small, flat     Imprints of    "Holes," like    surface         layers          pebbles
surfaces that   leaves,        Swiss            A shiny and     Straight or     Individual
are shiny or
                shells,        cheese, in the   smooth          wavy stripes    stones,
sparkly, like
tiny mirrors.   insects, or    rock.            surface, like   of different    pebbles, or
                other items                     colored         colors in the   sand grains
                                                glass           rock.           visible in the
                in the rock.
                                                                                rock.
Igneous-”Firemade” from
   cooled lava

Metamorphic-created from
 heat and pressure

Sedimentary-pebbles and
  gravel form layers
  sometimes with fossils
All rocks on earth were
originally igneous as
that's the only method
entirely new rock can
be formed. Basalt
Crystallize from molten material




                                                                      Rhyolite


 Quick cooling = fine grains
Slow cooling = coarse grains

      Magma - below the Earth's surface
     Lava - erupts onto the Earth's surface

                                                 Obsidian = volcanic glass
   Igneous rocks are                 Lava Erupting
    recognized by:
   the interlocking texture of
    the grains
   the presence of vesicles
    (holes) in extrusive igneous
    rocks
   may be dark-colored and
    heavy
   may display two grain
    sizes, one much larger
    than the other
Animations
 Sedimentary rocks are
  recognized by:
 grains cemented
  together
 the presence of fossils
 light-colored and light
  weight
 may display interlocking
  grains but is very light
  weight
 Igneous Rock Formation

 Metamorphic rocks            Gneiss Rocks

  are recognized by:
 the interlocking
  texture of large grains
 foliation (layering)
                                      •Schist Rocks
 banded light and dark
  colors
 "ching" sound instead
  of a "chunk" sound
  when tapped
Mylonite –forms along
      fault zones




                        Heat & Pressure
 Define the rock cycle. Use a simple diagram
 with lables


 http://www.minsocam.org/MSA/K12/rkcycle/
 rkcycleindex.html
   5. Waves, wind, water, and ice shape and reshape the Earth's land
    surface.
    As a basis for understanding this concept, students know:
    a. some changes in the Earth are due to slow processes, such as erosion,
    and some changes are due to rapid processes, such as landslides,
    volcanic eruptions, and earthquakes.
    b. natural processes, including freezing/thawing and growth of roots,
    cause rocks to break down into smaller pieces.
    c. moving water erodes landforms, reshaping the land by taking it away
    from some places and depositing it as pebbles, sand, silt, and mud in
    other places (weathering, transport, and deposition).

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Rock cycle 2

  • 2. Earth Sciences  4. The properties of rocks and minerals reflect the processes that formed them. As a basis for understanding this concept, students know: a. how to differentiate among igneous, sedimentary, and metamorphic rocks by their properties and methods of formation (the rock cycle). b. how to identify common rock-forming minerals (including quartz, calcite, feldspar, mica, and hornblende) and ore minerals using a table of diagnostic properties.
  • 3. Crystals Fossils Gas bubbles Glassy Ribbonlike Sand or Small, flat Imprints of "Holes," like surface layers pebbles surfaces that leaves, Swiss A shiny and Straight or Individual are shiny or shells, cheese, in the smooth wavy stripes stones, sparkly, like tiny mirrors. insects, or rock. surface, like of different pebbles, or other items colored colors in the sand grains glass rock. visible in the in the rock. rock.
  • 4. Igneous-”Firemade” from cooled lava Metamorphic-created from heat and pressure Sedimentary-pebbles and gravel form layers sometimes with fossils
  • 5. All rocks on earth were originally igneous as that's the only method entirely new rock can be formed. Basalt
  • 6. Crystallize from molten material Rhyolite Quick cooling = fine grains Slow cooling = coarse grains Magma - below the Earth's surface Lava - erupts onto the Earth's surface Obsidian = volcanic glass
  • 7. Igneous rocks are  Lava Erupting recognized by:  the interlocking texture of the grains  the presence of vesicles (holes) in extrusive igneous rocks  may be dark-colored and heavy  may display two grain sizes, one much larger than the other
  • 9.  Sedimentary rocks are recognized by:  grains cemented together  the presence of fossils  light-colored and light weight  may display interlocking grains but is very light weight
  • 10.
  • 11.  Igneous Rock Formation 
  • 12.  Metamorphic rocks  Gneiss Rocks are recognized by:  the interlocking texture of large grains  foliation (layering) •Schist Rocks  banded light and dark colors  "ching" sound instead of a "chunk" sound when tapped
  • 13. Mylonite –forms along fault zones Heat & Pressure
  • 14.  Define the rock cycle. Use a simple diagram with lables  http://www.minsocam.org/MSA/K12/rkcycle/ rkcycleindex.html
  • 15. 5. Waves, wind, water, and ice shape and reshape the Earth's land surface. As a basis for understanding this concept, students know: a. some changes in the Earth are due to slow processes, such as erosion, and some changes are due to rapid processes, such as landslides, volcanic eruptions, and earthquakes. b. natural processes, including freezing/thawing and growth of roots, cause rocks to break down into smaller pieces. c. moving water erodes landforms, reshaping the land by taking it away from some places and depositing it as pebbles, sand, silt, and mud in other places (weathering, transport, and deposition).