Igneous Textures Flashcards

1
Q

Broad classification of igneous rocks based on the degree of crystallinity.

A

Igneous Textures

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2
Q

Fully developed crystals with clear faces, formed from slowly cooling magma.

A

Euhedral/ Idiomorphic

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3
Q

Partially complete crystal form

A

Subhedral

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4
Q

Crystals that lack any observable faces; fitting into available spaces between other crystals.

A

Anhedral/ Xenomorphic

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5
Q

A mix of euhedral, subhedral, and anhedral grains.

A

Hypidiomorphic-granular Texture

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6
Q

Wholly glassy texture

A

Holohyaline

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7
Q

Partially crystalline/ partially glass texture

A

Hypocrystalline

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8
Q

Wholly crystalline texture

A

Holocrystalline

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9
Q

contains small crystals less than 1 mm in diameter, and are associated with volcanic rocks that cool quickly on Earth’s Surface

A

Aphanitic

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10
Q

Igneous rocks with crystals so small that even a microscope can’t see them clearly.

A

Cryptocrystalline

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11
Q

Rocks with small crystals that are visible with a petrographic microscope.

A

Microcrystalline

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12
Q

Very small crystals that can’t be seen with the naked eye but can be identified using a petrographic microscope.

A

Microlites

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13
Q

large crystals averaging 1mm to 30mm

A

Phaneritic

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14
Q

1 mm - 3 mm

A

Fine-grained

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15
Q

3 mm - 10 mm

A

Medium-grained

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16
Q

10 mm - 30 mm

A

Coarse-grained

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17
Q

This texture has two different crystal sizes because the rock cooled in two stages.

A

Porphyritic

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18
Q

Phenocrysts forms in what size of crystal?

A

LARGE

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19
Q

What is fine-grained material in a porphyritic rock.

A

Groundmass

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20
Q

Type of porphyritic texture where all crystals are visible to the naked eye, with phenocrysts being larger than the surrounding groundmass.

A

Porphyritic-Phaneritic

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21
Q

Type of porphyritic texture where the phenocrysts are embedded in a groundmass that is too fine-grained to see clearly.

A

Porphyritic-Aphanitic

22
Q

Large crystals averaging more than 30 mm in diameter, and develop most commonly in granitic plutons with high volatile contents.

A

Pegmatitic

23
Q

What is an igneous rocks with pegmatitic texture?

24
Q

This measures how many new crystals form in a certain amount of space over a certain amount of time.

A

Crystal Nucleation Rate

25
rate at which your magma cools, which is the main factor for the formation of textures.
Cooling rate
26
the availability ions that can fill specific ionic sites in a crystal lattice structure that can be enhance crystal growth
ion availability
27
rate at which elements migrate through magma that depends primarily on the viscosity of the melt.
Diffusion
28
An element that thicken magma, slowing crystal growth.
Network Formers
29
an igneous rock texture primarily composed of glass that develop in lava that solidifies without experiencing significant crystallization
Glassy/ Holohyaline
30
an amorphous solid possessing a disordered form
Glass
31
This happens when molten rock comes into contact with air or water, causing it to cool very quickly.
Quenching
32
An igneous rock texture that contains recognizable phenocrysts in a glassy groundmass
Vitrophyric
33
A rock with a vitrophyric texture.
Vitrophyre
34
A process where a glass turning into crystals
Devitrification
35
are rounded masses of crystals that grow out from a central point during devitrification, often looking like small, radiating clusters.
Spherulite
36
Black, glassy obsidian with cristobalite seeds that grew as “white snowflakes” within the obsidian.
Snowflake obsidian
37
An igneous rock texture characterized by a cloudy appearance and rounded cracks
Perlitic
38
A type of volcanic rock that is rich in silica (SiO₂) and has a glassy texture.
Perlite
39
These are curved or spherical cracks that form in perlitic rocks as they cool, giving them a distinctive pattern.
Perlitic cracks
40
A texture in igneous rocks that forms when gas bubbles get trapped in cooling lava.
Vesicular
41
These are spherical or ellipsoidal void spaces
Vesicles
42
A depth where volatiles exsolve from the liquid as a separate phase
Level of exsolution
43
A process where small gas bubbles form in the magma above the level of exsolution.
Vesiculation
44
This occurs when gas bubbles take up 70-80% of the magma's volume
Fragmentation surface
45
A term used before a rock’s name if it contains 5-30% vesicles
Vesicular
46
A term used for rocks with less than 5% vesicles.
Vesicle-bearing
47
An igneous rock texture primarily made up of cemented or welded pyroclasts
Pyroclastic
48
The rock particles of different sizes that are blown out during a volcanic eruption.
Pyroclasts
49
Airborne pyroclastic material.
Tephra
50
Rock fragment pyroclasts.
Lithic
51
Glassy fragment pyroclasts.
Vitric
52
Mineral or crystalline pyroclasts.
Crystals