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Questions and Answers
What are the seven ways to identify a mineral?
What are the seven ways to identify a mineral?
Color/clarity, crystal form, luster, streak, hardness, cleavage, fractures
How do you know when a mineral is harder than a streak plate?
How do you know when a mineral is harder than a streak plate?
The mineral will scratch the streak plate and make a white streak of powder from the streak plate.
What does a mineral look like when it has one cleavage?
What does a mineral look like when it has one cleavage?
Looks like pages of a book, that split apart along flat sheets.
What does a mineral look like that has two cleavages that intersect at or near 90 degrees?
What does a mineral look like that has two cleavages that intersect at or near 90 degrees?
What does a mineral look like that has three cleavages that intersect at or near 90 degrees?
What does a mineral look like that has three cleavages that intersect at or near 90 degrees?
What are some of the special characteristics a mineral can have?
What are some of the special characteristics a mineral can have?
What is the definition of magma?
What is the definition of magma?
What is the definition of intrusion?
What is the definition of intrusion?
How does intrusive igneous rock form?
How does intrusive igneous rock form?
What is another name for intrusive rock?
What is another name for intrusive rock?
What is the definition of lava?
What is the definition of lava?
How does extrusive igneous rock form?
How does extrusive igneous rock form?
What is another name for extrusive rocks?
What is another name for extrusive rocks?
What is the definition of felsic minerals?
What is the definition of felsic minerals?
What is the definition of mafic minerals?
What is the definition of mafic minerals?
Describe the color index of igneous rocks from lightest color to darkest.
Describe the color index of igneous rocks from lightest color to darkest.
What is the order of texture from intrusive to extrusive?
What is the order of texture from intrusive to extrusive?
What are the color index minerals from felsic to mafic?
What are the color index minerals from felsic to mafic?
Describe aphanitic texture.
Describe aphanitic texture.
Describe phaneritic texture.
Describe phaneritic texture.
Describe pegmatite texture.
Describe pegmatite texture.
Describe porphyritic texture.
Describe porphyritic texture.
Describe vesicular texture.
Describe vesicular texture.
Describe pyroclastic texture.
Describe pyroclastic texture.
What does a porphyritic texture indicate?
What does a porphyritic texture indicate?
What is glassy texture?
What is glassy texture?
What are the five characteristics of minerals?
What are the five characteristics of minerals?
How are minerals formed? (4 ways)
How are minerals formed? (4 ways)
What are the three degrees of crystallinity?
What are the three degrees of crystallinity?
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Study Notes
Identifying Minerals
- Seven ways to identify a mineral: color/clarity, crystal form, luster, streak, hardness, cleavage, fractures
- A mineral is harder than a streak plate if it scratches the streak plate and leaves behind a streak of powdered mineral
- Cleavage: Flat sheets, like pages of a book
- Two Cleavages that intersect at or near 90 degrees: Elongated prisms, fractured along short rectangular cross-sections
- Two Cleavages that do not intersect at 90 degrees: The mineral will not have a rectangular shape, or a shape of square/cubed
- Three Cleavages that intersect at or near 90 degrees: Shapes made of cubes and parts of cubes
- Three Cleavages that do not intersect at 90 degrees: Shapes made of rhombohedrons and parts of rhombohedrons
- Special characteristics of minerals: tenacity, reaction to acid, striations, magnetism, specific gravity
Igneous Rocks
- Magma: Rock that is heated until liquefied, found in isolated bodies beneath Earth's surface
- Intrusive igneous rocks: Form when magma intrudes into Earth's crust
- Intrusive igneous rock form: Formed by slowly cooling magma, comprised of visible mineral crystals
- Intrusive igneous rocks are also known as: Plutonic
- Lava: Bubbly magma that explodes out onto the Earth's surface
- Extrusive igneous rocks: Form when lava cools on Earth's surface
- Extrusive igneous rock form: Formed by rapidly cooling lava, comprised of tiny crystals and/or glass
- Extrusive igneous rocks are also known as: Volcanic
- Felsic Minerals: Light colored minerals, typically comprised of feldspars and silica
- Mafic Minerals: Dark colored minerals, typically comprised of magnesium and iron
- Color Index of Igneous Rocks from Lightest to Darkest: Felsic, Intermediate, Mafic, Ultramafic
- **Order of Texture from Intrusive to Extrusive **: Pegmatitic, Phaneritic, Porphyritic, Aphanitic, Glassy, Vesicular, Pyroclastic/Fragmental
Textures of Igneous Rocks
- Aphanitic texture: Fine-grained, rapid cooling
- Phaneritic texture: Comprised of visible crystals (coarse-grained), slow cooling
- Pegmatitic texture: Very coarse-grained, very slow cooling
- Porphyritic texture: Two distinct sizes of crystals, large crystals are called phenocrysts, small crystals are called the matrix, slow cooling followed by rapid cooling
- Vesicular texture: Gas bubbles trapped in cooling lava, vesicles, created extrusively
- Pyroclastic texture: Composed of fragmented rocky materials, ejected by explosive eruptions
- Glassy texture: Rapid cooling, very poor nucleation
- Porphyritic Texture indicates: That magma cooled slowly at first, then more rapidly
Minerals
-
Five Characteristics of Minerals:
- Naturally occurring
- Usually inorganic
- Definite chemical composition
- Solid substance with specific crystalline structure
- Distinctive physical properties
-
Four ways Minerals form:
- From molten rock
- From solution
- Within living cells
- By recrystallization
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Three Degrees of Crystallinity:
- Euhedral: Well-developed faces, edges, and corners
- Subhedral: Partially developed
- Anhedral: No faces, edges, or corners
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