Rocks Flashcards

(36 cards)

1
Q

It is a concept used to explain how the three basic rock types are related and how Earth processes, over geologic time, change a rock from one type into another.

A

ROCK CYCLE

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2
Q

An aggregate of minerals or rocks that are coherent.

A

Rocks

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3
Q

WHAT IS THE IMPORTANCE OF STUDYING MINERALS?

A

Minerals are building blocks of rocks.

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4
Q

Three TYPES OF ROCKS

A

• IGNEOUS
• SEDIMENTARY
• METAMORPHIC

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5
Q

Any crystalline or glassy rock that forms from cooling of a magma.

A

IGNEOUS ROCKS

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6
Q

TYPES OF IGNEOUS ROCKS

A

PLUTONIC and VOLCANIC

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7
Q

Crystallized below the surface of the earth

(P or V) - igneous

A

PLUTONIC ROCKS

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8
Q

PHANERITIC texture: coarse-grained

(P or V)

A

PLUTONIC ROCKS

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9
Q

Examples: Granite, Diorite, Gabbro

(P or V)

A

PLUTONIC ROCKS

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10
Q

Examples of Plutonic Rocks

A

Granite, Diorite, Gabbro

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11
Q

Crystallized on the surface of the earth

A

VOLCANIC ROCKS

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12
Q

APHANITIC texture: fine-grained

(P or V)

A

VOLCANIC ROCKS

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13
Q

Examples: RHYOLITE, ANDESITE, BASALT

A

VOLCANIC ROCKS

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14
Q

VOLCANIC ROCKS

-examples

A

RHYOLITE, ANDESITE, BASALT

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15
Q

rocks that form near the surface of the earth through chemical precipitation from water or by cementation of loose fragments.

A

SEDIMENTARY ROCKS

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16
Q

Breaking down of rocks to sediments

(Classification of sedimentary rocks)

17
Q

Compaction and cementation of sediments to rocks

(Classification of sedimentary rocks)

A

LITHIFICATION

18
Q

–causes the disintegration of rock to smaller fragments

(Classification of sedimentary rocks)

19
Q

disintegration of rocks and minerals by a physical or mechanical process.

Example: frost or ice wedging, burrowing of animals, roots of plants

(Classification of weathering; sedimentary rocks)

A

Physical Weathering

20
Q

chemical alteration or decomposition of rocks and minerals

Examples: hydrolysis, hydration, oxidation

(Classification of weathering)

A

Chemical Weathering

21
Q

TYPES OF SEDIMENTARY ROCKS

A

CLASTIC and NON-CLASTIC

22
Q

Classified on particle size

  • clastic or non-clastic?
23
Q

The presence of variable grain sizes is indicative of sedimentary differentiation which is actually a function of processes happening in different sedimentary environment.

-clastic or non-clastic?

24
Q

Formed through evaporation and precipitation

(Type of Sedimentary rocks)

25
form as a result of increasing the pressure and/or temperature on a previously existing rock to form a new rock. (Type of Rocks)
METAMORPHIC ROCKS
26
Refers to the changes in mineral assemblage and texture. (METAMORPHIC ROCKS)
METAMORPHISM
27
AGENTS OF METAMORPHISM
•HEAT •PRESSURE •CHEMICALLY- ACTIVE FLUIDS
28
TWO TYPES OF METAMORPHISM
CONTACT METAMORPHISM (non-foliated rocks) and REGIONAL METAMORPHISM (foliated rocks)
29
Heat and chemically-active fluid as agents (Type of metamorphism)
CONTACT METAMORPHISM
30
Creates non-foliated metamorphic rocks (Type of metamorphism)
CONTACT METAMORPHISM
31
There are no alignment or layering of minerals. ( foliated or non-foliated?)
NON-FOLIATED ROCKS
32
•Pressure as agent •Creates foliated metamorphic rocks •Occurs at regional scale (Type of metamorphism)
REGIONAL METAMORPHISM
33
There are visible alignment or layering of minerals. (Foliated or non-foliated)
FOLIATED ROCKS
34
Cooling and crystallization of magma (Type of Rocks)
Igneous
35
Lithification of sediments (Type of rocks)
Sedimentary
36
Application of heat, pressure & fluids (Type of rocks)
Metamorphic