Chapter 6: Sedimentary Rocks Flashcards

1
Q

Sedimentary Rock

A

forms at or near the surface of the Earth by

  • cementing together loose clasts
  • growth of mounds of shells
  • cementing together of shells and shell fragments
  • the accumulation and subsequent alteration of organic matter derived from living organisms
  • the precipitation of minerals directly from surface-water solutions
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2
Q

basement

A

the igneous or metamorphic rock that lies under sedimentary rock beds

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3
Q

Clasts

A

solid fragments and grains broken off of pre-existing rocks

note: comes from the Greek work Klastos, meaning broken

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4
Q

Classes of sedimentary rocks

A
  • clastic sedimentary rock
  • biochemical sedimentary rock
  • organic sedimentary
  • chemical sedimentary
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5
Q

How are clasts produced?

A
  • weathering
  • erosion
  • transportation
  • deposition
  • lithification
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6
Q

transportation

A

gravity, wind, water, or ice that can carry sediment

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7
Q

deposition

A

the process by which sediment settles out of the transporting medium

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8
Q

lithification

A

the transformation of loose clasts into solid rock, takes place in two stages

  1. compaction; weight of over burden squeezes air or water out from between grains so the grains can fit together more tightly
  2. cementation; when minerals (commonly quartz or calcite) precipitate from ground water and fill the remaining spaces between clasts to form a cement that binds grains together

starts as sediment —-> lithifies into sedimentary rock

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9
Q

well sorted v. poorly sorted

A

well sorted: the clasts in the sediment are generally the same size

poorly sorted: the clast sizes in sediment are ranging in sizes (big and small)

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10
Q

breccia

A

cemented angular clasts

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11
Q

conglomerate

A

burial or lithification of gravel bars/mounds that occur at former rivers

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12
Q

arkose

A

lithification of quartz and sometimes feldspar clay

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13
Q

siltstone

A

lithified mudflats/deltas

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14
Q

shale

A

lithified mud (aka mudstone)

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15
Q

examples of biochemical sedimentary rock

A

biochemical limestone

  • made from shells/broken up shell of sea creatures
  • largely CaCO3, also know as (carbonate rock)

fossiliferous limestone
- has fossils in it

biochemical chert
- formed from the shells of silica-secreting plankton that accumulated on the sea floor

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16
Q

organic sedimentary rocks

A

coal, oil shale

17
Q

chemical sedimentary rock

A

Halite (when when 90% of water evaporates) and gypsum (when 80% of water evaporates)
Travertine (Chemical limestone): forms as hot springs and in caves
Dolostone: carbonate rock containing the mineral dolomite
Chemically precipitated chert: flint

18
Q

bedding

A

a single layer of sediment or sedimentary rock with a recognizable top and bottom

19
Q

strata

A

several beds together

20
Q

why does bedding form?

A

Bedding forms from sediment accumulation by water, wind, glaciers. Changes in climate, water depth, water current velocity, or sediment source control the type of sediment deposited.

21
Q

stratigraphic formation

A

a sequence of strata that is distinctive enough to be traced as a unit across a fairly large region

22
Q

cross beds

A

distinct internal layers within sand dunes

23
Q

depositional environments

A

the conditions in which sediment was deposited

examples: beach, glacial, river environments

24
Q

non-marine depositional environment, and some examples

A

Terrestrial depositional environments

  • glacial environments
  • mountain stream environments
  • alluvial-fan environments
  • desert environments
  • river environments
  • lake environments
25
Q

Examples of coastal and marine depositional environments

A
  • marine delta deposits
  • coastal beach sands
  • shallow-marine clastic deposits
  • shallow-water carbonate environments
  • deep marine deposits
26
Q

subsidence

A

places where the surface of the earths lithosphere sinks, providing space in which sediment can collect

27
Q

categories of basins

A
  • rift basins: form at continental rifts
  • passive-margin basins: form along the edges of continents that er not plate boundaries
  • intracontinental basins: develop in the interiors of continents
  • foreland basins: form on the continental side of a mountain best
28
Q

transgression

A

when the shoreline migrates inland

the opposite of transgression is regression

29
Q

diagenisis

A

all the physical, chemical, and biological processes that transform sediment into sedimentary rock and that alter characteristic of sedimentary rock after the rock has formed