Igneous Rocks Flashcards
Rocks that formed from the solidification of magma (intrusive) or lava which flowed out to the surface of the Earth.
Igneous Rocks
Magma that reaches the Earth’s surface
Lava
molten rock solidifies at the surface
-Aphanitic
Extrusive (Volcanic)
- igneous rocks that form at depth
- Phaneritic
Intrusive (Plutonic)
-rocks that formed from the consolidationof individual rock fragments ejected during a violent eruption.
Pyroclastic (Fragmental)
Texture/Crystal Size
*- rapid cooling and high silica content of molten rock that is ejected into the atmosphere generates rocks having a glassy texture. This is formed from granitic or felsic magma.
* are rocks that consist of unordered ions
Ex. *
Texture/Crystal Size
Glassy Texture- rapid cooling and high silica content of molten rock that is ejected into the atmosphere generates rocks having a glassy texture. This is formed from granitic or felsic magma.
Glass are rocks that consists of unordered ions
Ex. Pumice and obsidian
*Texture- produced from debris of explosive eruption.
Ex. Tuff, *, agglomerate, *
Pyroclastic
lapilli stone, volcanic breccia
Pyroclastic Texture- produced from *
Ex. *, lapilli stone, *, volcanic breccia
debris of explosive eruption.
Tuff, agglomerate
*- cooled quickly on or near Earth’s surface. These rocks are fine-grained and have size <2 mm. This texture can be observed from rocks formed from intermediate magma. Light-colored aphanitic rocks are those containing primarily nonferromagnesian silicate materials.
Ex. *
Aphanitic Texture
Rhyolite, Andesite, Basalt, and Komatiite
Aphanitic Texture- cooled *on or near Earth’s *. These rocks are fine-grained and have size *. This texture can be observed from rocks formed from intermediate magma. Light-colored aphanitic rocks are those containing primarily nonferromagnesian silicate materials.
Ex. Rhyolite, Andesite, Basalt, and Komatiite
quickly, surface
<2 mm
*- produced by slow then rapid cooling. The resulting rock has large crystals embedded in the matrix which are called *while the matrix of smaller crystals is called *. A rock with such a texture is termed *.
Porphyritic Texture
phenocrysts, groundmass
porphyry
Porphyritic Texture- produced by *then *cooling. The resulting rock has * crystals embedded in the matrix which are called phenocrysts while the matrix of * crystals is called groundmass. A rock with such a texture is termed porphyry.
slow, rapid
large
smaller
*Texture- coarse-grained texture produced when magma cools slowly at depth. Size: >2 mm.
Phaneritic
*Texture – very large crystals with 3 cm in size
Pegmatitic
Factors affecting the texture of Igneous Rocks
- Rate of magma cooling
- Amount of silica present
- Amount of dissolved gases