Week 8 Flashcards

(39 cards)

1
Q

4 types of sedimentary rocks

A

Clastic
Biochemical
Organic
Chemical

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2
Q

What can create sedimentary rocks?

A

Weathering
Erosion
Transportation
Deposition

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3
Q

Sedimentary rocks are classified based on

A

texture and composition.

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4
Q

Lithification

A

Transforms loose sediment into solid rock.

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5
Q

Clast composition

A

Mineral make up of sediment grains.

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6
Q

The measure of uniformity of grain sizes in sediment population.

A

Sorting

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7
Q

Cross roads are created by

A

ripple and dune migration.

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8
Q

Sedimentary basins form where

A

tectonic activity creates space.

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9
Q

Passive Margins

A

The edges of continents that are not tectonic-plate boundaries.

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10
Q

A sea level rise or TRANSGRESSION shifts depositional bets

A

landward.

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11
Q

A sea level fall or REGRESSION shifts environments toward

A

the basin.

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12
Q

5 ways to create metamorphic rocks

A
Recrystallization
Phase change
Neocrystallization
Pressure solution
Plastic deformation
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13
Q

Protoliths

A

What gets changed in metamorphosis

Change in texture and mineralogy

Occur in a solid state

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14
Q

Metamorphism often imparts _____ upon a new rock.

A

Metamorphism often imparts foliation upon a new rock.

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15
Q

Phase change

A

New minerals form that have the same chemical composition but a different crystal structure.

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16
Q

Mineral grains partially dissolve where their surfaces press together.

A

Pressure solution.

17
Q

Plastic Deformation

A

Mineral grains soften and deform when a rock is squeezed.

18
Q

Burial metamorphism

A

Pressure squeezes pore space and water out. As you bury it, it gets warmer.

19
Q

Breakage of a rock by shearing within a fault zone.

A

Dynamic metamorphism

20
Q

Hydrothermal metamorphism

A

Melting. Downgoing plate releasing water. Spreading centre. Hot water rises and reacts with the rock. Rock that goes away from the ridge is hydrated.

21
Q

Trenches and accretionary prisms have a low geothermal gradient. These conditions prouce

22
Q

Average age of continental crust

A

2.5 billion years.

23
Q

4 types of metamorphic rocks

A

Gneiss
Schyst
Slate
Phylite

24
Q

Blueschist metamorphism is associate with

A

ocean crust subducting beneath a continent.

25
Contact metamorphism typically produces rocks that are called
hornfels.
26
Deep time
Time has persisted beyond persona experience and historical record. The processes that have been operating on our planet have been operating for a very long time.
27
Geologic time
James Huttton. 200 years.
28
Principle of Uniformitarianism
The processes observed today were the same in the past.
29
Relative Dates
Which came first or later?
30
Numeric Dates
How long ago did this happen?
31
Principle of Original Horizontality
Because sediments settle out of a fluid by gravity they settle horizontally.
32
Principle of superimposition
Younger strata on top, older strata on bottom.
33
Principle of Lateral Continuity
Strata often form in laterally extensive horizontal sheets.
34
Principle of cross cutting relations
Dikes, faults, erosions, must be younger than the material that is faulted.
35
Principle of baked contacts
Baked rock there first.
36
Principle of Inclusions
One rock fragment within another, the inclusions are always older.
37
Unconformity
A gap in the rock record. Often cross cutting.
38
Non conformity
Unconformity where igneous or metamorphic rock are capped by sedimentary rock.
39
Disconformity
Unconformity within sedimentary layers due to an interruption in sedimentation.