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1.IGNEOUS ROCKS
 Some were once liquid magma that
erupted from volcanoes. They cooled up
very quickly (extrusive)
 Others were once liquid magma but they
did not erupt from volcanoes. Instead,
they cooled slowly underground
EXAMPLES OF IGNEOUS ROCKS
2.SEDIMENTARY ROCKS
 Clastic sedimentary rocks are made up of
pieces (clasts) of pre-existing rocks loosened
by weathering. These rocks have particles
ranging in size from microscopic clay to huge
boulders; their names are determined by the
clast or grain size. The smallest grains are
called clay, then silt, then sand. Grains larger
than 2 millimeters are called pebbles.
EXAMPLES OF SEDIMENTARY
ROCKS:
3.METAMORPHIC ROCKS
 Metamorphic rocks arise from the
transformation of existing rock to new
types of rock, in a process called
metamorphism. The original rock is
subjected to temperatures greater than
150 to 200 °C and, often, elevated
pressure of 100 megapascals or more,
causing profound physical or chemical
change.
Types of rocks
Types of rocks
Types of rocks

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Types of rocks

  • 1.
  • 2.
  • 3. 1.IGNEOUS ROCKS  Some were once liquid magma that erupted from volcanoes. They cooled up very quickly (extrusive)  Others were once liquid magma but they did not erupt from volcanoes. Instead, they cooled slowly underground
  • 4.
  • 6. 2.SEDIMENTARY ROCKS  Clastic sedimentary rocks are made up of pieces (clasts) of pre-existing rocks loosened by weathering. These rocks have particles ranging in size from microscopic clay to huge boulders; their names are determined by the clast or grain size. The smallest grains are called clay, then silt, then sand. Grains larger than 2 millimeters are called pebbles.
  • 7.
  • 9. 3.METAMORPHIC ROCKS  Metamorphic rocks arise from the transformation of existing rock to new types of rock, in a process called metamorphism. The original rock is subjected to temperatures greater than 150 to 200 °C and, often, elevated pressure of 100 megapascals or more, causing profound physical or chemical change.