EarthSci Flashcards

(51 cards)

1
Q

Low-velocity zone of the mantle

A

Asthenosphere

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2
Q

Increase in s wave velocity between crust and mantle

A

Mohorovicic discontinuity

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3
Q

Inner core thickness

A

1,250 km

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4
Q

Outer core thickness

A

2,200 km

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5
Q

Mantle thickness

A

2,900 km

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6
Q

Density of oceanic crust

A

3 g/cm³

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7
Q

Density of continental crust

A

2.7 g/cm³

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8
Q

Fastest seismic wave

A

P waves

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9
Q

Foliated metamorphic rock originates from basalt

A

Serpentine

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10
Q

Foliated metamorphic rock originates from shale

A

Slate

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11
Q

Foliated metamorphic rock originates from conglomerate

A

Gneiss

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12
Q

Non-foliated metamorphic rock originates from sandstone

A

Quartzite

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13
Q

Non-foliated metamorphic rock originates from limestone

A

Marble

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14
Q

Physical and chemical changes in sediments

A

Diagenesis

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15
Q

Fragments of rock

A

Clasts

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16
Q

Pebbles/gravel cemented by a matrix of mud/sand

A

Conglomerate

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17
Q

Compaction and cementation of sediments

A

Lithification

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18
Q

Mainly composed of quartz

A

Sandstone

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19
Q

Made from dead organisms with calcium carbonate

A

Limestone

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20
Q

American mineralogist that classified minerals based on chemical properties

A

James Dwight Dana

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20
Q

Hydrocarbon-metal bond

21
Q

Examples of Sulphates

A

Anhydrite, Gypsum, Barite, Celestine

21
Q

Examples of Silicates

A

Quartz, Feldspar, Pyroxene, Mica, Garnet, Olivine, Amphibole

21
Q

Examples of Halides

A

Fluorites, Halites, Sylvites

22
Examples of carbonates
Aragonite, Calcite, Dolomite
23
Examples of Oxides
Hematite, Cuprite, Corundum, Chromite, Rulite
23
Example of Sulphides
Realgar, Cinnabar, Chalcopyrite, Pyrite, Argentite, Stibite, Galena
23
Contains important metals
Sulphides
24
Contains natural salts
Halides
25
Forms from high evaporation rate/slow evap. rate of salt water
Sulphates
26
Largest and most abundant group
Silicates
27
Found in marine environments
Carbonates
28
Rate of temp. change w/ respect to depth in Earth's interior
Geothermal gradient
29
Partial melting of magma from higher geothermal gradient due to convection
Decompression melting
30
Ways to generate magma
Decompression melting, Transfer of Heat, Flux melting
31
Water/CO2 lowering melting temp. of rock, producing magma
Flux melting
32
Low degree of partial melting produces
Siliceous magma
33
High degree of partial melting produces
Less sileceous magma
34
Rising and storage of magma which alters its chemical composition
Magmatic differentiation
35
Factors that affect metamorphism
Temperature Pressure Fluid-phase Time
36
Chemical reaction between a solid mineral and dissolved ions
Metasomatism
37
States that any geological features or intrusions are the youngest in rock layers
Principle of cross-cutting relationships
38
Gap or break in rock sequence/geologic record due to erosion
Unconformity
39
Break in rock sequence that are tilted/folded
Angular unconformity
40
States that sedimentary rock layers are deposited from oldest at the bottom to youngest at the top
Principle of superposition
41
States that sediments accumulate in horizontal strata
Principle of original horizontality
42
States that evolving organisms later disappear and recently appear
Principle of faunal succession
43
States that rocks incorporating other rocks like gravel indicate the gravel are fragments of older rocks
Principle of inclusion
44
States that the surrounding rock around intrusions are older than the intrusion
Principle of chilled/baked margins
45
45
Widely-distributed organism remains that existed for only a specific amount of time
Index fossils