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Igneous Rocks & Rock Structures. These notes go on pp. 7 & 9 of your Igneous rock INB!!!. Igneous rocks are formed by the crystallization of molten rock ( lava or magma ). Classification. Mineral Composition Texture of Grain Size. Mineral Composition.
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Igneous Rocks & Rock Structures These notes go on pp. 7 & 9 of your Igneous rock INB!!!
Igneous rocks are formed by the crystallization of molten rock (lava or magma).
Classification • Mineral Composition • Texture of Grain Size
Silica Composition Felsic rocks - more than 65% silica content Intermediate rocks - 50-65% silica content (also called andesitic) Mafic rocks - less than 40-50% silica
1. Igneous rocks formed above ground from lava are called “Extrusive” or “Volcanic” rocks. Obsidian Rhyolite
cools rapidlyand crystals have a limited time to form; as a result there are small or no mineral crystals
Resulting Textures: • Glassy • Porous/Vesicular • Fine-Grained
2. Igneous rocks formed underground from Magma are called Plutonic or Intrusive rocks. Notice the large crystals
Resulting Textures 1. Coarse Grained
Igneous rocks that begin to cool underground and then are erupted to the surface have both fine and coarse grains. These rocks have undergone two stages of cooling, therefore they have two sizes of crystals. These rocks have porphyritic texture.
Igneous Rock Structures These notes go on p. 9 of your INB!!!
Dikes Dike: Sheet-like Igneous rocks that cut acrossthe structure of pre-existing rock.
Sills Sills: Sheet-like Igneous rock that lies parallel to the layering of pre-existing rock.
Laccoliths Laccoliths: verticallydeveloped sills.
Batholiths Batholiths: a large Plutonic mass of Igneous Rock. Usually makes up the core of volcanicmountains