Different Types of Rocks

What is a Rock?

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

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Rocks are classified into three types:

  1. @@Igneous Rocks@@
  2. @@Sedimentary Rocks@@
  3. @@Metamorphic Rocks@@

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  1. IGNEOUS ROCKS

   It comprises 95% of the Earth’s crust.

How do igneous rocks form?

MagmaSolidificationofLavaIgneousRocksMagma - 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

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  1. 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.

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  1. SEDIMENTARY ROCKS

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

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  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.@@

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