Lesson 4.3 Flashcards

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1
Q

were
formed from organic,
mechanical or chemical
sediments.

A

Sedimentary rocks

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2
Q

is
where harden sediments
become sedimentary rocks.

A

lithification

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3
Q

is a collective process where sediments are
lithified (becomes rock)

A

Diagenesis

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4
Q

four main parts

A

Compaction

Cementation

Recrystallization

Chemical changes(oxidation/reduction)

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5
Q

Types of Sedimentary Rock

A

Non-clastic sedimentary
rocks(biological, chemical, both)

Clastic sedimentary
rocks(coarse, medium, fine, very fine)

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6
Q

Non-clastic sedimentary
rocks can be

A

biological,
chemical, or a
combination of both.

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7
Q

are made up of
sediments from
preexisting rocks.

A

Clastic sedimentary
rocks

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8
Q

(over 2 mm)

A

coarse

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9
Q

(1/16 to 2 mm)

A

medium

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10
Q

(1/16 to 1/256 mm)

A

fine

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11
Q

(< 1/256 mm)

A

very fine

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12
Q

are lithified accumulation of
dead organisms.

ex coal, limestone

A

Biological sedimentary rocks

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13
Q

form from chemical
precipitation

ex rock salt

A

Chemical sedimentary rocks

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14
Q

is when sediments are smashed together.

A

compaction

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15
Q

Since most
sediments can be found in water, water molecules are present in between particles.
The various dissolved minerals present in the surrounding water will eventually fall
out and attach to the sediment grains. Therefore, _ acts as glue that
binds the particles together.

A

cementation

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16
Q

Ions of chlorine, magnesium, potassium, calcium, carbonate, sodium, and sulfate
are commonly dissolved in seawater. However, others such as silica and
phosphorus which contributes to the make up of sedimentary rock are only found
in trace amounts in seawater. These ions will _ to form a rock after the
water evaporates.

A

crystallize

17
Q

Biological precipitation of the decayed shells of microorganisms form the carbonate
sediments. Through inorganic processes, other calcium-rich and bicarbonate-rich
chemical sediments are precipitated as calcium carbonate and carbonic acid.
However, these processes are less common.

Biological precipitation of the decayed shells of microorganisms form the carbonate
sediments. Through inorganic processes, other calcium-rich and bicarbonate-rich
chemical sediments are precipitated as calcium carbonate and carbonic acid.
However, these processes are less common.

A
18
Q

When preexisting rocks are physically weathered and eroded, they form sediments
called

which are composed of individual minerals or rock
fragments

A

clasts or detritus

19
Q

the clastic sedimentary rocks. The components of these rocks are called _ if minerals

A

grains

20
Q

the clastic sedimentary rocks. The components of these rocks are called _ if pieces of rocks

A

fragments

21
Q

refers to the amount of sediments it can carry

A

Stream capacity

22
Q

refers to the sizes of the sediments

A

competence

23
Q

gravel rounded, gravel angular

sand

silt

clay

A

conglomerate

breccia

sandstone

siltstone

shale