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19 Cards in this Set

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Felsic Minerals

Light Colored because they lack Iron and Magnesium.

Mafic Minerals

Have Magnesium and Iron. Dark because of Iron and magnesium

Chemical Composition 4 Groups

Felsic (Acidic) Compositional Group



Mafic (Basic) compositional group



Ultramafic (UltraBasic) Compositional group



Intermediate compostion group

Felsic (acidic) Compositional Group

THe name felsic refers to feldspars (Far-) and other silica-rich (-sic) minerals but it is now also used (in place of "acidic") to describe magmas, lavas, and igneous rocks containing more than 60% silica

Mafic (basic) Compositional group

Mafic refers to the minerals with Magnesium (ma-) and iron (-fic) in their chemical formulas, but now refers to magmas and lavas and igneous rocks contained 45%-53% Silica

Ultramafic (Ultrabasic) Compositional group

As the name implies, this term was orginally used to describe igneous rocsk made almost entirely of mafic minerals. However it now also is used (in place of Ultrabasic) to describe Magmas, lavas, and igneous rocks containing less than 40% Silica

Intermediate Compositional groups

Magmas, lavas and ignous rocks that contain 54-64% silica. A compositon between mafic and felsic.

Physical Composition

Volcanic Glass


Mineral grains (Crystals)


Pyroclasts


Xenoliths

Volcanic Glass

No definite form


Called obsidian


Transparent or translucent when held up to a light.


Associated wtih felic rocks because high percentage of silica that can polymerize rather than mineral crystals


Can be Red-Brown, black, gray or tan.


Darker color comes from oxidation and irons.


A little bit of magnetite or hematite to darken the glass


Mineral grains (Crystals)

Most igneous rocks, even pieces of volcanic glass, contain some proportion of mineral crystals- either mafic (dark colored ferromagnesian minerals)

Mafic

Iron and Magnesium
Dark Colored


Black, brown, blood red

Felsic

Has Silica and Potassium Fieldspar


Light Colored


White, Light Gray, and Pastels

Intermediate

Mixture of Mafic and Felsic Minerals


Medium Colors

Igneous Composition

Mafic

Felsic

Intermediate

Pegmatitic

Crystals caused by inrusive cooling that are 1 CM or greater

Glassy

Caused by Extrusive cooling
Looks like glass

Phaneritic

Crystals caused by intrusive cooling
Small 1-2 mm

Igneous Texture

Intrusive Cooling Phaneretic, Pegmatitic



porphyritic texture



Extrusive Cooling, Aphanite, Glassy, vesicular,

Prophytrite Texture

Create by 2 different stages of cooling.
If it was a chocolate chip cookie, the cookie part would be the Matrix and the chip part would be the Phenocrysts