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Different Types of Rocks

What is a Rock?

  • According to National Geographic, rock is a Natural substance composed of solid crystals of %%different minerals%% that have been fused together into a solid lump.
  • According to Brittanica Encylopedia, it is naturally occurring and a coherent aggregate of %%one or more minerals.%%

Rocks are classified into three types:

  1. @@Igneous Rocks@@

  2. @@Sedimentary Rocks@@

  3. @@Metamorphic Rocks@@

  4. IGNEOUS ROCKS

    It comprises 95% of the Earth’s crust.

How do igneous rocks form?

Magma - Solidification of Lava - Igneous Rocks

There are two types of Igneous Rocks

  1. Intrusive Igneous Rocks (PLUTONIC)

    • Magma cools down and solidifies inside the earth’s surface.

    • %%Slow cooling = Large crystals%%

      Examples of Intrusive Igneous Rocks:

      Diorite: It is a mixture of feldspar, pyroxene, hornblende, and sometimes quartz.

      Gabbro: It contains feldspar, pyroxene, and sometimes olivine.

      Granite: it contains mainly quartz, feldspar, and mica minerals

  2. Extrusive Igneous Rocks (VOLCANIC)

    • Magma cools down and solidifies above the Earth’s surface

    • %%Fast cooling = small crystals%%

      Examples of Extrusive Igneous Rocks:

      Andesite: It is composed mainly of plagioclase with other minerals such as hornblende, pyroxene, and biotite.

      Basalt: it is composed mainly of plagioclase and pyroxene.

      Obsidian: forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.

  3. SEDIMENTARY ROCKS

    Comprised of Sediments

    Lithification: it is a %%complex process%% whereby freshly deposited loose grains of sediment are converted into rock.

How do Sedimentary rocks form?

Lithification processes:

  • Compaction: Reduces pore space due to the weight of sediments above.
  • Cementation: Dissolved substances precipitate out and act as glue.
  • Recrystallization: Form new crystalline mineral grains from the old ones.
  • Diagenesis: the cycle repeats.

3 CLASSIFICATIONS OF SEDIMENTARY ROCKS:

  • CLASTIC ROCKS: formed when individual sediment made by fragments of rocks, minerals, or shells are cemented together.
  • CRYSTALLINE ROCKS: Chemical sedimentary rocks. It is formed by the crystallization of chemical precipitates.
  • BIOCLASTIC ROCKS: organic sedimentary rocks. Formed mostly by the remains of organisms.

  1. METAMORPHIC ROCKS

    When igneous rocks and sedimentary rocks are %%exposed to high temperature and pressure.%%

    Metamorphism: change from one rock formation to another.

  • FOLIATED METAMORPHIC ROCKS: Have layered or branded appearance. It is %%produced by exposure to heat and directed pressure.%%
  • NON-FOLIATED METAMORPHIC ROCKS: Doesn’t have a layered or branded appearance. It formed around igneous intrusions where @@temperatures are high but the pressures are relatively slow.@@