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The Rock Cycle
Thinking about relationships among
       the major rock groups
Major Rock Groups
• Igneous
     – Formed from molten rock (magma/lava) that has cooled
     – Literally means “from fire”
1. Extrusive igneous rock is formed from lava (on earth’s
 surface) and tends to solidify quickly.
2. Intrusive igneous rock is formed from magma (inside the
 earth) and tends to take a long time to solidify into rock.




                                                               2
Major Rock Groups
• Sedimentary
  – All types of rock are continuously being broken down into
    small fragments called sediment.
  – This sediment can be compressed or cemented together
    to form sedimentary rock
Major Rock Groups
• Metamorphic
• Processes such as extreme heat/pressure can
  alter the chemical composition of the original
  rock to form a new rock.
Rock Cycle
• Geologic forces cause rock to constantly
  change from one type to another
• Complete the rock cycle diagram by adding
  the appropriate processes that connect each
  rock type to the others
SEDIMENT      Erosion
          Weathering

                                                           Transport



                                                                  Deposition
                                                   SEDIMENTARY
IGNEOUS

                                                                 Increased P&T

                                                METAMORPHIC
                   Crystallization
                                                 Melting
                                                                         Burial
 Uplift                              MAGMA



                                                                           6
Crystal Formation
• As magma cools, minerals that have been
  melted tend to solidify into specific shapes
  called crystals. Since extrusive igneous tend
  to solidify more quickly, the crystals tend to be
  small or fine grained.
• Examples: Basalt and Rhyolite
Crystal Formation
• Some extrusive igneous rocks cool so quickly
  that crystals are not formed at all.
• If this happens and the lava has very little
  dissolved gasses, the rock will be a glassy rock
  called obsidian.


• If there are a lot of dissolved gasses the rock
  will be very porous or vesicular and be called
  pumice.
Crystal Formation
• Intrusive igneous rock that cools slowly can
  form a mixture of large crystals and are said
  to be coarse grained.
• Example: Granite
Bowens Reaction
• N. L. Bowen studied mineral crystallization
  and found out that minerals form at specific
  times during that solidification process and
  they generally form in the same order.
Composition of Igneous Rock
• Felsic rock: generally light colored and
  contains a high concentration of silica
• Mafic rock: generally dark colored and
  contains a low concentration of silica
Intrusive Rock Structures
•Volcanic Neck: Magma that solidifies in the
main vent of a volcano is much harder than the
surrounding rock.
•Eventually the surrounding rock is eroded
leaving the harder intrusive igneous rock
exposed.
Devils Tower (Wyoming)
Intrusive Rock Structures
•A sill forms when magma flows between
layers of existing rock and forms a new layer
parallel to the existing layers (even if the
existing layers are tilted).
Intrusive Rock Structures
•A dike forms when magma forces its way
through rock by following an existing fracture or
making new ones. The layer made by a dike is
NOT parallel to the existing rock layers.
Formation of Sedimentary Rock
•Compaction: is when pieces of sediment are
squeezed together by the weight of overlying
layers (including water)
•Cementation of sediment occurs when minerals
are deposited in a bed of sediment and as the
water evaporates the dissolved minerals form
crystals that “glue” the sediment particles to
each other.
Three Types of Sedimentary Rock

• Chemical Sedimentary Rock: Formed by
  minerals that were once dissolved in water
  but as the water evaporated the minerals
  formed rocks called evaporates.
• Examples include gypsum (drywall) or halite
  (rock salt). The Bonneville salt flats were
  formed this way.
Three Types of Sedimentary Rock

• Organic Sedimentary Rock: The remains of
  living organisms can sometimes form rocks
  such as coal or limestone.
• Coal is partially decayed plant and animal
  material while limestone is made entirely of
  CaCO3 (Calcium Carbonate) shells from dead
  organisms.
Three Types of Sedimentary Rock

• Clastic Sedimentary Rock: Made of rock
  fragments that are carried away from their
  source by water wind or ice and left as
  deposits. Over time these fragments become
  cemented/compacted together.
Conglomerate
• A clastic rock that contains rounded
  fragments that are cemented together by
  smaller sand sized sediment.
Breccia
• A clastic rock that contains angular fragments
  that are cemented together by smaller
  pieces.
Sandstone
• Contains uniformly small pieces of mineral
  grains that are cemented together.
Shale
• Composed of clay sized (smaller than sand
  grains) particles that are compressed into flat
  layers
Metamorphic Rocks
• Metamorphic rocks are formed from existing
  rock that is subjected to pressure and heat
  (but not melted) into a new type of rock.
Marble
• Marble is formed when limestone is subjected
  to heat and pressure.
Slate
• Slate is formed from shale.
Quartzite
• Quartzite is formed from sandstone.
Diamonds
• Diamonds are formed from Coal

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Rock Cycle PowerPoint

  • 1. The Rock Cycle Thinking about relationships among the major rock groups
  • 2. Major Rock Groups • Igneous – Formed from molten rock (magma/lava) that has cooled – Literally means “from fire” 1. Extrusive igneous rock is formed from lava (on earth’s surface) and tends to solidify quickly. 2. Intrusive igneous rock is formed from magma (inside the earth) and tends to take a long time to solidify into rock. 2
  • 3. Major Rock Groups • Sedimentary – All types of rock are continuously being broken down into small fragments called sediment. – This sediment can be compressed or cemented together to form sedimentary rock
  • 4. Major Rock Groups • Metamorphic • Processes such as extreme heat/pressure can alter the chemical composition of the original rock to form a new rock.
  • 5. Rock Cycle • Geologic forces cause rock to constantly change from one type to another • Complete the rock cycle diagram by adding the appropriate processes that connect each rock type to the others
  • 6. SEDIMENT Erosion Weathering Transport Deposition SEDIMENTARY IGNEOUS Increased P&T METAMORPHIC Crystallization Melting Burial Uplift MAGMA 6
  • 7. Crystal Formation • As magma cools, minerals that have been melted tend to solidify into specific shapes called crystals. Since extrusive igneous tend to solidify more quickly, the crystals tend to be small or fine grained. • Examples: Basalt and Rhyolite
  • 8. Crystal Formation • Some extrusive igneous rocks cool so quickly that crystals are not formed at all. • If this happens and the lava has very little dissolved gasses, the rock will be a glassy rock called obsidian. • If there are a lot of dissolved gasses the rock will be very porous or vesicular and be called pumice.
  • 9. Crystal Formation • Intrusive igneous rock that cools slowly can form a mixture of large crystals and are said to be coarse grained. • Example: Granite
  • 10. Bowens Reaction • N. L. Bowen studied mineral crystallization and found out that minerals form at specific times during that solidification process and they generally form in the same order.
  • 11. Composition of Igneous Rock • Felsic rock: generally light colored and contains a high concentration of silica • Mafic rock: generally dark colored and contains a low concentration of silica
  • 12. Intrusive Rock Structures •Volcanic Neck: Magma that solidifies in the main vent of a volcano is much harder than the surrounding rock. •Eventually the surrounding rock is eroded leaving the harder intrusive igneous rock exposed.
  • 14.
  • 15. Intrusive Rock Structures •A sill forms when magma flows between layers of existing rock and forms a new layer parallel to the existing layers (even if the existing layers are tilted).
  • 16. Intrusive Rock Structures •A dike forms when magma forces its way through rock by following an existing fracture or making new ones. The layer made by a dike is NOT parallel to the existing rock layers.
  • 17. Formation of Sedimentary Rock •Compaction: is when pieces of sediment are squeezed together by the weight of overlying layers (including water) •Cementation of sediment occurs when minerals are deposited in a bed of sediment and as the water evaporates the dissolved minerals form crystals that “glue” the sediment particles to each other.
  • 18. Three Types of Sedimentary Rock • Chemical Sedimentary Rock: Formed by minerals that were once dissolved in water but as the water evaporated the minerals formed rocks called evaporates. • Examples include gypsum (drywall) or halite (rock salt). The Bonneville salt flats were formed this way.
  • 19.
  • 20. Three Types of Sedimentary Rock • Organic Sedimentary Rock: The remains of living organisms can sometimes form rocks such as coal or limestone. • Coal is partially decayed plant and animal material while limestone is made entirely of CaCO3 (Calcium Carbonate) shells from dead organisms.
  • 21. Three Types of Sedimentary Rock • Clastic Sedimentary Rock: Made of rock fragments that are carried away from their source by water wind or ice and left as deposits. Over time these fragments become cemented/compacted together.
  • 22. Conglomerate • A clastic rock that contains rounded fragments that are cemented together by smaller sand sized sediment.
  • 23. Breccia • A clastic rock that contains angular fragments that are cemented together by smaller pieces.
  • 24. Sandstone • Contains uniformly small pieces of mineral grains that are cemented together.
  • 25. Shale • Composed of clay sized (smaller than sand grains) particles that are compressed into flat layers
  • 26. Metamorphic Rocks • Metamorphic rocks are formed from existing rock that is subjected to pressure and heat (but not melted) into a new type of rock.
  • 27. Marble • Marble is formed when limestone is subjected to heat and pressure.
  • 28. Slate • Slate is formed from shale.
  • 29. Quartzite • Quartzite is formed from sandstone.
  • 30. Diamonds • Diamonds are formed from Coal