Igneous Rocks Flashcards
Igneous Rocks
Formed by minerals crystallising from a melt known as magma (or, when extruded at the Earth’s surface)
There are two types of igneous rock types, Intrusive/Plutonic and Extrusive/Volcanic.
Intrusive/Plutonic
- Formed when magma solidifies deep underground.
- Includes granites, the main rock of continents.
- Intrusive/plutonic rocks cooled slowly deep within the Earth and are coarse-grained or phaneritic (most crystals > 1mm -bigger than 1mm)
Extrusive/Volcanic
- Formed when magma solidifies at the Earth’s surface as lava
- Includes basalts, the main rock in the ocean floor
- Extrusive/volcanic rocks cooled quickly at or near Earth’s surface, giving crystals little time to grow. These rocks tend to be fine-grained or aphanitic (most crystals <1mm- smaller than 1mm)
Name/describe 2 igneous rock textures (of igneous rock)
-Phaneritic (coarse) Texture
Large Crystals
Magma cooled & crystallised slowly
-Aphanitic
Small Crystals
Magma cooled & crystallised more quickly
Extrusive rock examples
Volcanic (fine grained)
- Rhyolite (Acid- >65% Sio2)
- Andesite (Intermediate- 52-65% SiO2)
- Basalt (Basic- 45-52% SiO2)
Intrusive rock examples
Hypabyssal (med. grained)
- Porphyry (Acid- >65% SiO2)
- Porphyrite (Intermediate- 52-65% SiO2)
- Dolerite (Basic- 45-52% SiO2)
Plutonic (coarse grained)
- Granite (Acid- >65% SiO2)
- Diorite (Intermediate- 52-65% SiO2)
- Gabbro (Basic- 45-52% SiO2)
- Peridotite (Ultra Basic- <45% SiO2)
Sills and Dykes
(within the earth’s crust)
Sill- horizontal (or sub-horizontal) layer of solidified lava
Dyke- when injected vertically
Identification Summary (examples)
Light coloured (Acid): Coarse texture = Granite Medium texture = Micro-granite Fine texture = Rhyolite
Dark Colour (Basic): Coarse texture = Gabbro Medium texture = Dolerite Fine texture = Basalt
Felsic
- Light coloured minerals (quartz, alkali feldspar, and some plagioclase feldspar)
- Rich Si, Na, Al and K and poor in Fe and Mg
- Dark coloured minerals biotite and amphibole are present, but only in minor amounts
Example- Granite
Intermediate
-Rocks contain roughly equal amounts of dark-coloured minerals and light-coloured minerals
Example- Andesite
Mafic
- Abundant dark-coloured minerals (olivine, pyroxene, and plagioclase)
- These are compositionally rich in Fe, Mg and Ca.
Example- Basalt
Ultramafic
- Fe and Mg-rich minerals from the mantle (olivine and pyroxene, but not plagioclase).
- Compositionally rich in Fe, Mg and Ca, but poor in Si
Example- Olivine