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Igneous Rock Formation
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Presentation transcript:

Daily Routine Sit in your appropriate seat quietly Have all necessary materials out All back packs on the floor All cell phones on silent and away in backpacks All IPods off and headphones out of your ears Hats off No food or drink except for water

Bell Work Compare and contrast rocks and minerals Describe one other mineral property talked about on Friday

Earth Science Announcements Mineral Quiz on Wednesday

How are minerals affect by the different stages of the rock cycle? Igneous Rocks How are minerals affect by the different stages of the rock cycle?

I will be able to… Describe how and where igneous rocks form Explain how minerals form igneous rocks due to different cooling periods at different temperatures Compare and contrast felsic, mafic, and intermediate groups of igneous rocks Describe what igneous rock texture is

What are Igneous Rocks? Igneous rocks form due to the solidification of magma or lava Magma: is the molten or semi-molten form of rocks High in Iron, Silicon, and Oxygen Magma contains: Minerals Gases (CO2 and Sulfur dioxide) Water and Water vapor

How do minerals condense to form rocks from magma? Fractional crystallization: the removal and separation of a melt of different minerals at different temperatures and different periods of cooling based on chemical composition

Bowen’s Reaction Series Minerals first to form: Form at high temperatures Contains less silica (Si and O) High in iron Darker in color Minerals last to form: Form at lower temperatures Contains lots of silica (Si and O) Lighter in color

Felsic Vs. Mafic Igneous Rocks Intermediate Mafic Minerals have higher silica content Lighter in color usually need longer periods of time to cool Minerals often found in felsic rocks are quartz, micas, k-feldspar Examples: granite and rhyolite Minerals have medium silica content Contain some minerals with higher iron content 50-50 mix in dark and light color Usually need longer periods of time to cool, but some minerals crystallize faster at hotter temperatures Common minerals: quartz, micas, k-feldspar, and amphibole Examples: diorite and andesite Minerals have a lower content in silica Higher in iron (Fe) Cool quicker than the other minerals Often darker in color Common minerals: olivine plagioclase, amphibole, and pyroxene Examples: gabbro and basalt

Where can Igneous Rock form?

Intrusive vs. Extrusive Texture: Coarse (large visible crystals) Conditions to form intrusive igneous rocks: Deep below the surface Cool magma temperatures ( Long and slowing during crystallization Texture: Fine (microscopic crystals) Conditions to form extrusive igneous rocks: Forms on the surface Hot lavas that cool rapidly Short and rapid cooling which yields little crystal development