Igneous Rocks Flashcards

1
Q

Rocks that formed from the solidification of magma (intrusive) or lava which flowed out to the surface of the Earth.

A

Igneous Rocks

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2
Q

Magma that reaches the Earth’s surface

A

Lava

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3
Q

molten rock solidifies at the surface

-Aphanitic

A

Extrusive (Volcanic)

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4
Q
  • igneous rocks that form at depth

- Phaneritic

A

Intrusive (Plutonic)

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5
Q

-rocks that formed from the consolidationof individual rock fragments ejected during a violent eruption.

A

Pyroclastic (Fragmental)

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6
Q

Texture/Crystal Size
*- rapid cooling and high silica content of molten rock that is ejected into the atmosphere generates rocks having a glassy texture. This is formed from granitic or felsic magma.
* are rocks that consist of unordered ions
Ex. *

A

Texture/Crystal Size
Glassy Texture- rapid cooling and high silica content of molten rock that is ejected into the atmosphere generates rocks having a glassy texture. This is formed from granitic or felsic magma.
Glass are rocks that consists of unordered ions
Ex. Pumice and obsidian

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7
Q

*Texture- produced from debris of explosive eruption.

Ex. Tuff, *, agglomerate, *

A

Pyroclastic

lapilli stone, volcanic breccia

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8
Q

Pyroclastic Texture- produced from *

Ex. *, lapilli stone, *, volcanic breccia

A

debris of explosive eruption.

Tuff, agglomerate

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9
Q

*- cooled quickly on or near Earth’s surface. These rocks are fine-grained and have size <2 mm. This texture can be observed from rocks formed from intermediate magma. Light-colored aphanitic rocks are those containing primarily nonferromagnesian silicate materials.
Ex. *

A

Aphanitic Texture

Rhyolite, Andesite, Basalt, and Komatiite

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10
Q

Aphanitic Texture- cooled *on or near Earth’s *. These rocks are fine-grained and have size *. This texture can be observed from rocks formed from intermediate magma. Light-colored aphanitic rocks are those containing primarily nonferromagnesian silicate materials.
Ex. Rhyolite, Andesite, Basalt, and Komatiite

A

quickly, surface

<2 mm

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11
Q

*- produced by slow then rapid cooling. The resulting rock has large crystals embedded in the matrix which are called *while the matrix of smaller crystals is called *. A rock with such a texture is termed *.

A

Porphyritic Texture
phenocrysts, groundmass
porphyry

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12
Q

Porphyritic Texture- produced by *then *cooling. The resulting rock has * crystals embedded in the matrix which are called phenocrysts while the matrix of * crystals is called groundmass. A rock with such a texture is termed porphyry.

A

slow, rapid
large
smaller

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13
Q

*Texture- coarse-grained texture produced when magma cools slowly at depth. Size: >2 mm.

A

Phaneritic

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14
Q

*Texture – very large crystals with 3 cm in size

A

Pegmatitic

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15
Q

Factors affecting the texture of Igneous Rocks

A
  • Rate of magma cooling
  • Amount of silica present
  • Amount of dissolved gases
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16
Q

Other classification of Igneous Rocks

*- contains tiny holes/vesicles which formed due to escaping gas bubbles in the lava or magma.

A

Vesicular

17
Q
  • mineral precipitates, vesicles at the rock may be filled by low temperature minerals deposited in the cavities after the lava solidified
A

Amygdaloidal

18
Q

are an assemblage of mafic and ultramafic lavas and hypabyssal rocks found in association with sedimentary rocks like greywackes and cherts.

A

Ophiolites

19
Q

the initial process that occurs in the formation of a crystal from a solution, a liquid, or a vapour, in which a small number of ions, atoms, or molecules become arranged in a pattern characteristic of a crystalline solid, forming a site upon which additional particles are deposited as the crystal grows

A

Nucleation

20
Q

continues as more ions or molecules become attracted

A

Growth