Chapter 1. Earth Materials And Geosphere Flashcards

(53 cards)

1
Q

Low velocity zone

A

250km

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2
Q

Transition zone

A

410 km

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3
Q

Another transition zone

A

660km

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4
Q

Crust distance

A

5-80km

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5
Q

Mantle distance

A

2885 km

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6
Q

Core distance (rad)

A

3480 km

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7
Q

Crust by %vol

A

Less than 1

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8
Q

Mantle %by vol

A

83%

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9
Q

Core %vol

A

16%

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10
Q

Lithospheric distance

A

100km

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11
Q

Asthenospheric distance with transition zone

A

400-660km

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12
Q

Crust is separated from mantle by _discontinuity

A

Moho

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13
Q

Oceanic crust thickness

A

5-7 km

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14
Q

Idealized strat of Oceanic crust composed of _ main layers

A

3

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15
Q

Layer 1

A

Sediments

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16
Q

Layer 2

A

Basalts and dikes

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17
Q

Layer 3

A

Gabbro and Oceanic crust

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18
Q

Layer 4

A

Mantle PERIDOTITE

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19
Q

Oldest Oceanic crust age

A

<180 ma

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20
Q

Location of oldest Oceanic crust

A

Along w and e borders of N Atlantic Ocean and w pacific

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21
Q

Oceanic crust density

A

2.9 to 3.1

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22
Q

Ave density of cont crust

23
Q

Greenstone belts age

24
Q

Composition of earth’s mantle

A

Ultrabasic ecglogite

25
Upper mantle comp
Peridotite
26
Lvz distance
100 to 250 km
27
Distance top of lvz marks the contact between lithosphere and asthenosphere
100km
28
Discontinuity at inner to outer core at 5150 km
Lehman
29
Density of inner core
13
30
Plates are separated by plate boundary segments that end in?
Triple junctions
31
Movement of plates
3 types, 2 hybrid(div, con, trans, - ditrans, contrans
32
Creation of red sea (Arabian separated from African)
5ma
33
Creation of Indian Ocean
115 ma
34
Creation of Atlantic ocean
180 ma
35
Earths largest mountain range (20%of earths surface)
Ocean ridge system
36
6-18cm per yr warmer and faster
E. Pacific rise
37
2-4cm/yr spreading rate
Mid Atlantic
38
Idea sites for epiclastic(detrital) of subd zones
Trench arc systems
39
Marks path of subd zone
Wadatti benioff zone
40
3 largest magnitude of equake
1909 Chile Alaska 1964 Sumatra 2004 which produced banda aceh tsunami
41
Age of himalayan mountain range
40ma
42
Tule of strike slip with horizontal motion
Trans
43
Curvilinear zones of intensity faulted or fractured Oceanic crust nearly perpen to ridge axis
Fracture zones
44
Below lvz, seismic velo is (low, high)
High
45
Location of transition zone (410-660)
Between upper and lower mantle
46
Olivine (@14Gpa) transforms into beta spinel or wadsleyite and at high pressure transforms into ringwoodite. T or f
T
47
(@660km,24gpa) ringwoodite plus garnet to pervoskite and periclase(oxide). T or f
T
48
Periclase and magnesiowustite are polymorphs ((MG. Fe) o). T or f
T
49
Lower mantle major minerals
Perovs, periclase, magnesiowustite, stishiovite, ilmenite, ferrite
50
Above core mantle boundary (130-340km)
D"layer
51
Core composition
85% Fe 5% Ni 8-10% O S H
52
Low velo of P wave @2900 km or core mantle boundary
Guttenberg discontinuity
53
Core mantle boundary density
10-12g/cm3