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IGNEOUS ROCKS.

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Presentation on theme: "IGNEOUS ROCKS."— Presentation transcript:

1 IGNEOUS ROCKS

2 Created by the solidification (crystallization) of magma or lava
U S R C K Created by the solidification (crystallization) of magma or lava

3 Formed on surface of earth from crystallization of lava
2 TYPES OF IGNEOUS ROCKS 1. EXTRUSIVE (volcanic) Formed on surface of earth from crystallization of lava

4 Formed underground from crystallization of magma
2 TYPES OF IGNEOUS ROCKS 2. INTRUSIVE (Plutonic) Formed underground from crystallization of magma

5 Medium/Large Crystals
CRYSTALLIZATION Intrusive Rocks Cooled Slowly Medium/Large Crystals Extrusive Rocks Cooled Quickly Small/No Crystals

6 8 most common elements in crust
% of Crust by weight Oxygen 46.6 Silicon 27.7 Aluminum 8.1 Iron 5.0 Calcium 3.6 Sodium 2.8 Potassium 2.6 Magnesium 2.1 All Others 1.5 The chemical composition of a magma/lava determines which minerals will form

7 In between mafic and felsic -- some of everything
Types of Magma/Lava Type Chemical Composition Rocks from this type E=Extrusive; I=Intrusive Mafic Fe, Mg, Ca E = Basalt I = Gabbro Felsic Si, O, Al, Na E = Rhyolite I = Granite Intermediate In between mafic and felsic -- some of everything E = Andesite I = Diorite

8 *4

9 IGNEOUS ROCKS MAFIC ROCK Dark Colors High in Fe & Mg MORE DENSE FELSIC ROCK Light Colors High in Al & SiO2 LESS DENSE

10 HOW IGNEOUS ROCKS CRYSTALLIZE
Since every mineral has a unique freezing temperature, minerals crystallize out of a magma in a very specific order.

11 BOWEN'S REACTION SERIES
Temperature Discontinuous Series Continuous Series Rock Type (E/I) Ultramafic Peridotite Mafic Basalt/Gabbro Intermediate Andesite/ Diorite Felsic Rhyolite/ Granite Olivine Ca-rich 1400 C 1200 C 1050 C 800 C 600 C Pyroxene Plagioclase Feldspar Amphibole Biotite Na-rich Orthoclase Feldspar + Muscovite Mica Quartz

12 PLATE TECTONICS & IGNEOUS ROCKS
MAFIC Ocean crust, mantle rock, more dense and will sink Divergent Plate Boundaries Hot Spots FELSIC Continental Crust, less dense so will float Collision Zones Sliding Plate Boundaries INTER-MEDIATE Where mafic and felsic rock mixes Subduction Zones

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14 IGNEOUS ROCKS


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