Minerals and Rocks Flashcards

memorize

1
Q

the fundamental components of rocks

A

Minerals

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2
Q

the most abundant components of rocks on the Earth’s surface

A

Silicate minerals

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3
Q

fundamental
chemical building block of silicate minerals

A

Silicon tetroxide, SiO4

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4
Q

Minerals are classified according to their

A

chemical composition

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5
Q

are the essential building blocks of the geosphere

A

Minerals and rocks

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6
Q

is usually called silica, is one of the most common
minerals in the Earth’s crust.

A

Quartz

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7
Q

is a sodium- or calcium-rich feldspar.

A

Plagioclase feldspar

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8
Q

are rich in alkali
metal ions.

A

Alkali feldspar

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9
Q

usually occur as stubby prisms.

A

Alkali feldspar crystals

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10
Q

form
flat, book-like crystals that split into individual sheets, separating into smooth
flakes along the cleavage planes.

A

Micas

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11
Q

form prismatic or needle-like crystals.

A

Amphiboles

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12
Q

form short or columnar prismatic crystals.

A

Pyroxene

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13
Q

is a green, glassy mineral.

A

Olivine

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14
Q

is made up of calcium carbonate

A

Calcite

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15
Q

naturally occurring aggregates of minerals, rock fragments or
organic matter.

A

Rocks

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16
Q

two important
characteristics that may help to confirm the origin of a rock.

A

Texture and mineral composition

17
Q

refers to the sizes and shapes of the component minerals or grains, and
to their collective arrangement in a rock.

A

Texture

18
Q

refers to the crystals, mineral grains, fragments of other rocks,
and/or fossils, that make up a rock.

A

Composition

19
Q

form when hot, molten rock (magma) cools and solidifies.

A

Igneous Rocks

20
Q

are formed when rising magma is trapped
deep within the Earth, where it cools very slowly over many thousands or
millions of years until it finally solidifies.

A

Intrusive Igneous Rocks

21
Q

are produced when magma is erupted at,
or very near, the Earth’s surface.

A

Extrusive Igneous Rocks

22
Q

are formed from the eroded fragments of pre-existing
rocks, or from the skeletal fragments of once-living plants or organisms.

A

Sedimentary Rocks

23
Q

are made up of fragments (clasts) of pre-existing
rocks.

A

Clastic sedimentary rocks

24
Q

form when large quantities of living plants or
organisms die and accumulate.

A

Biological sedimentary rocks

25
Q

are formed by chemical precipitation from
solutions.

A

Chemical sedimentary rocks

26
Q

are formed when a pre-existing rock is subject to high temperature, high pressure, hot and mineral-rich fluid, or a combination of
these conditions.

A

Metamorphic rocks

27
Q

exhibit a platy or sheet-like structure.

A

Foliated metamorphic rocks

28
Q

display a massive structure.

A

Non-foliated metamorphic rocks

29
Q

is composed of crystalline calcite minerals

A

Marble

30
Q

is a conceptual model that explains how
geological processes acting on any one of the three main rock types

A

Rock Cycle