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Igneous Rock Classification Lab

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Presentation on theme: "Igneous Rock Classification Lab"— Presentation transcript:

1 Igneous Rock Classification Lab
What is a rock? rocks are composed of minerals, mineraloid or organic materials Granite (composed of minerals) Opal (composed of mineraloids) Coal (composed of organics) Elements Minerals Rocks

2 Igneous Rock Classification Lab
Let’s form an igneous rock Two major types of igneous rocks Intrusive – magma solidifies below the Earth’s surface magma cools very slow crystals form interlocking “mosaic” textures very coarse-grained visible minerals referred to as Plutonic rocks Extrusive – magma solidifies above the Earth’s surface magma cools very fast minerals can not be seen with un-aided eye very fine-grained texture (no visible minerals referred to as Volcanic rocks Extrusive rocks Intrusive rocks

3 Igneous Rock Classification Lab
Identification of Igneous rocks is based on two main characteristics Texture – the appearance of the rock due to the rate of magma cooling Composition – the type of minerals found in the rock (mineral composition) Textures of igneous rocks Intrusive rocks (Textural terms) phaneritic texture – crystals are visible and form a mosaic of interlocking mineral aggregates (less than 1 cm) Interlocking crystal grains phaneritic texture

4 Igneous Rock Classification Lab
pegmatitic texture – crystals are very large (>1cm) Large orthoclase and plagioclase minerals Extrusive Igneous Rocks (textural terms) aphanitic texture – crystals are too small to see See, you really can not see any mineral crystals

5 Igneous Rock Classification Lab
porphyritic texture – crystals can be separated into two distinct visible sizes. There can be small grains or large grains, but crystals appear in 2-distinct sizes Phenocrysts Groundmass (matrix)

6 Igneous Rock Classification Lab
Vesicular texture- sponge like appearance, texture contains numerous cavities or holes Vesicles – gas bubbles cavities Pyroclastic texture – textures created by rapidly cooling lava that is “hurled” through the air picking up fragments (tuffaceous texture) rock fragments – pieces of rock “incorporated” into the rock (tuffaceous)

7 Intrusive Extrusive Igneous Rock Textures Rock cooled slowly
Rock cooled rapidly Texture types: phanartitic pegmatitic Texture types: aphanitic porphyritic vesicular pyroclastic tuffaceous

8 Igneous Rock Classification Lab
Igneous Rock Composition mineral composition = mineral assemblages= chemistry The mineral is either ferromagnesian (dark colored) or felsic (light colored ferromagnesian (mafic) minerals rich in Fe, Mg – creates a dark colored rocks Pyroxene (Augite) Amphibole (hornblende) Mica - Biotite

9 Igneous Rock Classification Lab
Igneous Rock Composition Mineral composition = Mineral assemblages = Chemistry The mineral is either ferromagnesian (dark colored) or felsic (light colored) Felsic – mineral composition is light colored minerals Ca-plagioclase K-feldspar (orthoclase) Mica- muscovite Quartz

10 Texture Origin Intrusive Extrusive X Igneous Rock Classification
Felsic Mafic 80% Origin Texture 40% 20% Rock Descriptions Very coarse crystal grains, usually all grains are approximately the same size w/ respect to each other. Grains> one inch Coarse Very Granite Pegmatite Mafic Pegmatite Intrusive A mosaic of coarse-grains that are easily visible to the unaided eye – grains greater than 1 mm Phane- ritic Grano- diorite Diorite Gabbro Peridotite Granite Aphan- itic Fine to very fine grains, usually to small to be distinguished with the unaided eye or even with a hand lens Rhyolite Dacite X Andesite Basalt Glassy Glassy – non-crystalline, non-granular Color varies between black and brown Obsidian Extrusive Por- ous Highly vesicular, finely crystalline to glassy Pumice (light), Scoria (dark) Pumice Scoria Composed of fragments of all sizes Produced in volcanic environments, Ash Partially re-fused or cemented Rhyolitic Tuff Basaltic Tuff mental Frag-

11 Igneous Rock Classification Lab
Let’s use Texture and Composition to identify igneous rocks Steps for identifying igneous rocks Identify the texture (phaeritic/aphanitic) If the rock is phaneritic, estimate the % of felsic and mafic minerals High mafic = dark colored rock High felsic = light colored rock 50% felsic, 50% mafic = intermediate color Use your igneous rock schematic and cross reference the texture and composition (light, intermediate, dark) and name the rock. Add modifying terms (porphyritic, vesicular ect…….)


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