Chapter 7 - Sediments and Sedimentary Rocks Flashcards

(32 cards)

1
Q

Stratification

A

Arrangement of sediment in distinct layers (layering of rocks) (strata)

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2
Q

Bedding

A

Layered arrangement of strata in a body of sediment or sedimentary rock

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3
Q

Bed

A

individual layer - distinguished by differences in thickness or character

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4
Q

Bedding plane

A

top or bottom surface of a bed

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5
Q

Clastic Sediment

A

loose, fragmental detritus produced by mechanical breakdown of older rocks

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6
Q

Clast

A

an individual particle of clastic sediment

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7
Q

Poortly Sorted

A

Wide particles size range

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8
Q

Well Sorted

A

Narrow size range (same size particles)

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9
Q

non-sorted sediment

A

different sizes arranged chaotically - without obvious order

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10
Q

rhythmic layering - Varves

A

paired lighter (nonorganic) and darker (organic) colored lake sediments

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11
Q

cross bedding

A

beds inclined with respect to thicker stratum in which they occur (created from sand dunes)

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12
Q

graded bedding

A

particles grade upward from coarser to finer (created from streams)

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13
Q

Mineral composition

A

most coarse clastic sediments consist of those mineral grains and rock fragments least susceptible to chemical/physical breakdown (quartz is common)

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14
Q

Chemical Sediment

A

formed by precipitation of minerals from solution in water

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15
Q

Biogenic Sediment

A

composed mainly of fossils (remains of plants and animals)

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16
Q

Bioclastic sediment

A

composed largely of fossil fragments

17
Q

Deep-sea ooze

A

Accumulation of microscopic marine organisms on sea floor

18
Q

Sedimentary Facies

A

any sediment that can be distinguished from a contemporary sediment that formed in different depositional environment

19
Q

Facies

A

The character of a rock expressed by its formation, composition, and fossil content

20
Q

Lithification

A

process whereby unconsolidated sediment is converted into rock (e.g. sand into sandstone)

21
Q

Diagenesis

A

all changes that occur after deposition and during and after lithification

22
Q

Compaction

A

weight of sediment reduces pore spaces and forces out water - fine grain rocks (e.g. mudrocks)

23
Q

Cementation

A

dissolved substances precipitate from water in pores - course grain rocks (e.g. sand and gravel into stone)

24
Q

Recrystallization

A

less stable minerals may recrystallize to more stable forms

25
Chemical alteration
if oxygen is present organic remains conveted to CO2 and Water. if oxygen is absent organic matter transforms into mostly carbon (e.g. plants turn into coal)
26
Clastic Sedimentary Rocks
classified on basis of predominant particle size
27
Sole marks
collective term for features preserved on bedding surfaces
28
ripple marks
preserved in sand that was moved by wind, streams, or waves
29
mud cracks
polygonal markings caused by shrinking and cracking of drying mud
30
trace fossils
footprints and trails of animals
31
raindrop impressions
small indents left from raindrops
32
color
may indicate if sediment was deposited in reducing (black) or oxidizing (red) environment