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Formation of Igneous Rock
Formation of Igneous Rock
• When lava cools and hardens it forms
  igneous rock.

• The rock has two categories and is based on
  how the lava cools.
 – Intrusive igneous rock
 – Extrusive igneous rock
Intrusive Igneous
• The cooling of magma deep below the
  earth’s surface.

• Called intrusive because the lava that
  forms them intrudes other rocks.

• The magma then slowly cools to form
  rock.

• The slow cooling allows minerals to
  collect and form large crystals.
Extrusive Igneous
• Formed when there is a rapid cooling
  of lava or melting of rocks on the
  earth’s surface.

• The rapid cooling does not give
  crystals time to form.

• The main difference between the two
  types of igneous rock is the size of
  the crystal when the rock is forming.
Texture of the Rocks
• The larger the crystals, the more rough the
  rock will be.

• When rapid cooling occurs and crystal are
  not allowed the opportunity to form, the rock
  will appear extremely smooth.

• Crystal formation will be so small that they
  are not seen by the unaided eye.
Texture of the Rocks
• An igneous rock with both large and small
  crystals is called porphyritic.

• The porphyritic texture is created when lava
  cools slowly and is then sped up.
Texture of Rock
• When thick lava cools rapidly no crystals
  form at all.

• Usually thicker lava has an increased
  amount of trapped gases and this will cause
  the igneous rock to become full of holes.
Composition of Rock
• The mineral make of the lava determines the
  chemical make-up of the rock.

• There are 3 different types of families:
 – Felsic
 – Mafic
 – Intermediate

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5.3 igneous rocks

  • 2. Formation of Igneous Rock • When lava cools and hardens it forms igneous rock. • The rock has two categories and is based on how the lava cools. – Intrusive igneous rock – Extrusive igneous rock
  • 3. Intrusive Igneous • The cooling of magma deep below the earth’s surface. • Called intrusive because the lava that forms them intrudes other rocks. • The magma then slowly cools to form rock. • The slow cooling allows minerals to collect and form large crystals.
  • 4. Extrusive Igneous • Formed when there is a rapid cooling of lava or melting of rocks on the earth’s surface. • The rapid cooling does not give crystals time to form. • The main difference between the two types of igneous rock is the size of the crystal when the rock is forming.
  • 5. Texture of the Rocks • The larger the crystals, the more rough the rock will be. • When rapid cooling occurs and crystal are not allowed the opportunity to form, the rock will appear extremely smooth. • Crystal formation will be so small that they are not seen by the unaided eye.
  • 6. Texture of the Rocks • An igneous rock with both large and small crystals is called porphyritic. • The porphyritic texture is created when lava cools slowly and is then sped up.
  • 7. Texture of Rock • When thick lava cools rapidly no crystals form at all. • Usually thicker lava has an increased amount of trapped gases and this will cause the igneous rock to become full of holes.
  • 8. Composition of Rock • The mineral make of the lava determines the chemical make-up of the rock. • There are 3 different types of families: – Felsic – Mafic – Intermediate