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Igneous Rock Formation
• Molten rock comes from depth (less dense so works its way to surface) - full of gases (H20, C02, S02) plus elements in silicates
• Eruption - gases escape as pressure lessons• Magma cools and hardens beneath the surface
(intrusive; plutonic) • Crystallization - process of cooling and solidifying • Lava cools and hardens on surface (extrusive) • In volcanic eruptions on or under the earth’s surface
Intrusive Igneous Rocks
Form when magma hardens beneath Earth’s surface
Coarse grained due to slow cooling
Examples- Granite, Diorite, Gabbro, Periodotite
(image on left is diorite)
Extrusive Igneous Rocks
Form when lava hardens above the Earth’s surface, when most of the gases have escaped
Fine grained due to rapid cooling
Examples- Basalt, Rhyolite, Scoria
(image on right is basalt)
Classification of Igneous Rocks
• Texture- size, shape, arrangement of crystals
• Composition- proportions of light and dark minerals in the rock
(images from top to bottom: obsidian, diorite, basalt)
Coarse Grained = Large Crystals
• Intrusive rocks• Magma cools slowly• Ions have time to
move large distances within magma
• Few centers of crystal growth develop
Fine Grained: Fast Cooling
• Extrusive rocks• Magma or lava cools
rapidly resulting in small, interconnected mineral grains
• The ions in the melted material lose their motion and quickly combine
Glassy Texture
• Fast Cooling, Extrusive
• No time for the ions in the lava to arrange themselves into a network of crystals
• Obsidian (top); pumice (bottom)
Porphyritic Texture: Different Sized Crystals
• Minerals that do not crystallize at the same rate or time in magma --different sized crystals
• Inside volcano some magma never reaches the surface--two waves of crystallization
• Large crystals called phenocrysts (visible-crystals) in a matrix of fine grained crystals
Granitic Composition
• 0%-25% dark• Felsic• Light colored• Quartz, feldspar• 10% dark silicate
materials-- with magnesium, iron
• 70% silica (light silicates)
• Example- Rhyolite(also granite)
Basaltic Composition
• 45%-85% dark minerals• Plagioclase feldspar• Rich in magnesium and
iron• Darker and denser
(because of iron) • Mafic• Ocean floor = basaltExample- Basalt(also gabbro)
Andesitic Composition
• Between granitic and basaltic
• 25%-45% ‘dark’• 25% dark silicate
minerals-- amphibole, pyroxene, biotite mica
• Other dominant mineral: Plagioclase feldsparExample- Andesite(also diorite)
Ultramafic Composition
• 85%-100% dark• Olivine and pyroxene• Almost entirely dark
silicate minerals
• Peridotite rock. Rare at E’s surface but composition of much of mantle