THE ROCK CYCLE Flashcards

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1
Q

=process involving
the transformation and generation of
igneous, sedimentary, and
metamorphic rocks.
=Rocks are constantly being
transformed, generated, and destroyed in a process called

A

ROCK CYCLE

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2
Q

outermost layer of our planet composed of
the _ and the _

A

crust and the upper mantle

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3
Q

composed of rock and minerals

A

EARTH

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4
Q

extends to a depth of about 100 kilometers down the
surface containing different rocks and minerals
from both the continents and the oceans.

A

LITHOSPHERE

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5
Q

naturally-occurring
aggregate or combination of
minerals and mineraloids, such as
fossils and glass.

A

ROCKS

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6
Q

are the natural building
blocks of Earth’s lithosphere.

A

ROCKS

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7
Q

EXAMPLES OF IGNEOUS ROCKS:

A

GRANITE, DIORITE, CYANITE, BASALT, ANDESITE

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8
Q

_ rocks are formed through the cooling of magma or lava

A

IGNEOUS ROCKS

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9
Q

IGNEOUS IS BASED ON LATIN WORD WHICH MEANS

A

IGNIS

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10
Q

IGNIS MEANS

A

FIRE

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11
Q

Magma or lava may be solidified in
one of three ways:

A

=Below the surface:from a slow-cooling
magma;
=On the surface:from fast-cooling lava
=On the surface: the consolidation of
particles erupted by explosive volcanic
activity;

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12
Q

_ rocks accumulate on earth’s surface

A

SEDIMENTARY ROCKS

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13
Q

SEDIMENTARY ROCKS IN A PROCESS CALLED_

A

DESPOSITION

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14
Q

THE PROCESS BY WHICH THESE UNCONSOLIDATED MATERIAL BECOMES INTO ROCK IS CALLED _

A

Lithification

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15
Q

EXAMPLES OF SEDIMENTARY ROCKS:

A

CLAY, LIMESTONE, SANDSTONE, CONGLOMERATE, BAUXITE

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16
Q

_ ROCKS formed from the exposure of sedimentary or igneous rocks

A

METAMORPHIC ROCKS

17
Q

THE ORIGINAL ROCK WHICH CAN EITHER BE IGNEOUS, SEDIMENTARY, OR A METAMORPHIC ROCK, IS REFERRED TO AS THE _

A

PROTOLITH

18
Q

EXAMPLES OF METAMORPHIC ROCKS:

A

SLATE SCHIST, GNEISS, MARBLE, QUARTZITE

19
Q

CLASSIFICATION OF ROCKS:

A

TEXTURE AND COMPOSITION

20
Q

_refers to the size, shape, and
arrangement of mineral grains and other contituents, which are controlled by processes involved in the
formation of the rock

A

TEXTURE

21
Q

Rocks can also have a distinct grain size:

A

APHANITIC AND PHANERITIC

22
Q

Rocks have grains too small to see or identify /have crystals too small for the eye to see

A

APHANITIC

23
Q

Rocks have grains which are big enough to see/have crystals which are visible

A

PHANERITIC