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Geological Oceanography > Exam 1 > Flashcards

Exam 1 Flashcards

1
Q

geologic record is divided into 3 eons

A

The Archaean, The Proterozoic and the Phanerozoic

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2
Q

How long ago was earth formed

A

4.5 bya

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3
Q

Terrestrial planets (inner planets) Mercury, Venus, Earth and Mars

A

metallic cores (iron and nickel, surrounded by rock), High density, Little atmosphere

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4
Q

Jovian planets (outer planets) Jupiter, Saturn, Neptune, Uranus and Pluto)

A

Metallic cores (iron and nickel, surrounded by liquid helium), low density, lots of atmosphere, most have rings and numerous satellites

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5
Q

what information is used to calculate the age of the earth?

A

age of meteorites (should be the same age as planets)

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6
Q

why are meteorites used to calculate the age of the earth?

A

they are materials left over from formation of inner rocky planets when solar system formed

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7
Q

what chemicals are in the inner core

A

iron (94%) Nickel (6%)

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8
Q

what chemicals are in outer core

A

iron (85%), oxygen (5%), Sulfur (5%), Nickel (5%)

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9
Q

what chemicals are in the mantle

A

oxygen (44%), calcium (2.5%), magnesium (22.8%), silicon (21%), aluminum (2.4%), iron (6.3%)

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10
Q

Do s-waves pass through the core?

A

No, that’s how they know the core is liquid

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11
Q

Do p-waves pass through the core?

A

yes

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12
Q

premordial helium

A

there is no processes on earth capable of creating 3H. we find 3h in rocks and fluids thats how we know earth is still degassing. primordial helium emanates from the ground at sites of lava plumes like those found in hawaii

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13
Q

topography

A

defining form and shape

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14
Q

geomorphology

A

focuses on the evolution of topographic and bathymetric features

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15
Q

continental crust

A

20 to 60 km thick, made of granite, less dense, most is above sea level, light color, coarse

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16
Q

oceanic crust

A

only about 10 km thick, made of basalt, very dense, below sea level, dark color, fine texture

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17
Q

emergent coasts

A

where tectonic forces are pushing upwards (usually active continental margins). sea cliffs and marine terraces

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18
Q

submergent coasts

A

where sea level is rising faster than land and/or coastal areas are sinking

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19
Q

what type of coast are estuaries associated with

A

submergent coastlines formed when sea level rises and flood existing river valleys

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20
Q

continental margins

A

the submerged edge of continents they include: continental shelf, slope, rise and submarine canyons
they are influenced by tectonic uplift and subsidence.
they are areas of high sediment deposition from continents

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21
Q

what do active continental margins have

A

narrower shelf, deep sea trench, tend to be narrower (like west coast), may have high sediment accumulations but sediments go into deep trench

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22
Q

what do passive continental margins have

A

thick accumulations of sediments, wider shelf, a continental rise, tend to be wider (like east coast)

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23
Q

where are active margins location

A

around the pacific

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24
Q

where are passive margins located

A

around the Atlantic and parts of the Indian ocean

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25
Q

what is the continental shelf’s geomorphology influenced by?

A

erosion and deposition of sediments on beaches, at high latitudes glaciers and glacial deposits, mid-latitudes terrigenous fluxes and waves, low latitudes more carbonates

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26
Q

____ changes have great impacts on morphology and erosion

A

sea level

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27
Q

continental slope

A

slope between the outer edge of the continental shelf and deep ocean floor (from 100-200m to 1400-3200m depths)

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28
Q

shelf breaks

A

marks the boundary between the relatively flat continental shelf and the drop off into deeper water of the continental slope

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29
Q

continental rise

A

a wide gentle incline from a deep ocean plain to a continental slope

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30
Q

mid-ocean ridges

A

associated with divergence of ocean curst (new crust) and are volcanic (basalt) from consistent and frequent eruptions

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31
Q

crust sinks as it cools and moves away from ___

A

Mid-ocean ridges

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32
Q

new basalt forms from

A

diversity of lava flows and eruptions

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33
Q

bathymetry

A

measure of depth of water

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34
Q

the earth’s crust is ___ than the mantle, inner core, and outer core and so ‘floats’ on top of them

A

lighter

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35
Q

igneous type of rock and source material

A

melting of rocks in hot, deep crust and upper mantle

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36
Q

rock forming process of igneous

A

crystallization (solidification of magma or lava)

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37
Q

example of igneous rock

A

granite

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38
Q

sedimentary type of rock and source material

A

weathering and erosion of rocks exposed at surface

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39
Q

rock forming process of sedimentary

A

deposition, burial and lithification

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40
Q

example of sedimentary rock

A

sandstone

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41
Q

type of rock and source material of metamorphic

A

rocks under high temperatures and pressures in deep crust and upper mantle

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42
Q

rock forming process for metamorphic

A

recrystallization of new minerals in solid state

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43
Q

examples of metamorphic rocks

A

gneiss

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44
Q

intrusive

A

formed within the earth’s curst and thus cools slowly

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45
Q

extrusive

A

formed on the surface cool rapidly

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46
Q

extrusive oceanic curst

A

basalt (mafic)

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47
Q

intrusive ocean curst

A

gabbro (mafic)

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48
Q

extrusive continental curst

A

rhyolite (felsic)

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49
Q

intrusive continental crust

A

granite (felsic)

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50
Q

which is more dense oceanic curst or continental crust

A

oceanic crust

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51
Q

igneous rocks

A

solidification of magma, basalt and granite are two of the most common forms of igneous rock

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52
Q

intrusive cools ___ and ___ minerals form

A

slowly, more

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53
Q

extrusive cools ___ and ___ mineral frm

A

faster, less

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54
Q

lighter colored rocks have more ____

A

silica

55
Q

metamorphic rock is modification of sedimentary and igneous rocks by:

A

heat, pressure and or chemically active solutions

56
Q

ophiolites

A

masses of oceanic crust and underlying mantle that have thrust (or obducted) onto continental margins during subduction

57
Q

the lithosphere is fairly ___

A

rigid

58
Q

the asthenosphere is ___

A

plastic

59
Q

isostasy

A

is the state of gravitational equilibrium between the lithosphere and the asthenosphere such that the crust “floats” at an elevation that depends on its thickness and density

60
Q

how do we know where the plates are?

A

the locations of the plant boundaries and the distribution of earthquakes

61
Q

what are the three types of plate boundaries?

A

divergent, convergent and transform boundaries

62
Q

divergent boundary

A

two places move away from the axis of a mid-ocean ridge. New oceanic lithosphere forms

63
Q

convergent boundary

A

two plates move toward each other, the downgoing plate sinks beneath the overriding plate

64
Q

transform boundary

A

two plates slide past each other on a vertical fault surface

65
Q

what elements are found in divergent boundaries

A

enriched in iron and magnesium and depleted in silica

66
Q

when the plate of oceanic crust collides with plate of continental curst which plate subducts?

A

oceanic crust is subducted under continental plate

67
Q

accretionary prism

A

sediment scraped off when plates subduct

68
Q

how do earthquakes happen

A

at convergent boundaries the downgoing plate grinds along the base of the overriding plate, a process that generates large earthquake

69
Q

Lithosphere

A

curst and upper mantle temp<1280C rigid

70
Q

Asthenosphere

A

upper to mid mantle, temp >1280C Plastic

71
Q

Lithosphere ___ while asthenosphere ___

A

bends, flows

72
Q

ocean crust

A

basalt (extrusive), gabbro (intrusive),

ocean curst is more dense and mafic

73
Q

continental crust

A

rhyolite (extrusive), granite (intrusive),

continental crust: less dense and felsic

74
Q

a mineral

A

a solid formation that occurs naturally in the Earth

75
Q

a rock

A

a solid combination of more than one mineral formations which is also occurring naturally

76
Q

metamorphic rocks

A

are formed when igneous or sedimentary rocks are exposed to conditions of high heat and pressure. Examples of metamorphic rock include marble, slate, schist, and gneiss

77
Q

igneous rock

A

is formed by the cooling and crystallization of molten magma at volcanoes and mid-ocean ridges, where new crust is generated. Examples of igneous rock are basalt, granite, and andesite

78
Q

sedimentary rocks

A

Over time, igneous rocks may experience weathering and erosion from exposure to water and the atmosphere to produce sediments. The deposition and hardening of these sediments forms

79
Q

differences between oceanic and continental curst

A

continental crust: thick and old >2 billion years

oceanic crust: thin and young <200 million yr

80
Q

tectonic theory

A

earth’s lithosphere is broke into plates that move and interact. Plates move in response to forces in the mantle. plate boundaries are locations of great geologic change

81
Q

paleomagnetism

A

a record of Earth’s magnetic field in the past

82
Q

curie temperature

A

The Chinese figured out thousands of years ago that if you heated iron above a certain temperature (Curie temperature) and cooled it slowly you could form a magnet out of it.
Above the Curie temperature, the iron is so hot that the atoms become disordered and vibrate about.
Once the iron begins to cool, the atoms vibrate less and less and they lock into place in accordance with the field of the Earth.
After the iron is cooled all the way, the orientation in which it cooled is “locked in.”

83
Q

the North Pole of the Earth has a ___ polarity

A

south

84
Q

what causes a planet’s magnetic field?

A

the iron core of the Earth is an electromagnet. Core is surrounded by liquid iron and nickel, as electrons flow around the core the magnetic field is produced

85
Q

characteristics of Earth’s magnetic field

A

nearly dipolar, approximately aligned with Earth’s rotation axis, changes slowly with time, spontaneously reverses every ~200,000 years, is at least 3 Ga old

86
Q

magnetic declination

A

the angle between magnetic North and geographic North. The declination is positive when the magnetic north is east of true north, and negative when west of true north

87
Q

normal polarity

A

magnetic polarity, same as today

88
Q

reversed polarity

A

polarity chrons; the time interval of a reversal

89
Q

forces that drive plate tectonics: mantle convection currents

A

warm mantle currents drive and carry plates of lithosphere along a like a conveyor belt

90
Q

forces that drive plate tectonics: ridge push

A

buoyant upwelling mantle at mid-ocean ridges

91
Q

forces that drive plate tectonics: slab pull

A

older, colder plates sink at subduction zones, because as they cool, they become more dense than the underlying mantle

92
Q

Is this the way plates move about, passively dragged to and fro on
the backs of convection currents rising up from the mantle?

A

The answer appears to be no.
Almost all scientists now accept that the lithospheric plates somehow participate in the flow of this mantle convection, however the nature of the relationships are not well understood.
The main evidence comes from the rates of plate movement

93
Q

why not along convection

A

the faster-moving plates (the Pacific, Nazca, Cocos, Indian, and Australian plates) are being subducted along a large fraction of their boundaries.
the slower-moving plates (the North American, South American, African, Eurasian, and Antarctic plates) do not have significant attachments of descending lithospheric slabs.
These observations suggest that the gravitational pull exerted by the cold (and thus dense) slabs of subducting lithosphere pulls the plates downward into the mantle.
the plates are not dragged along by convection currents rising from the mantle, but rather “fall back” into the mantle under their own weight.

94
Q

slab pull

A

older, colder plates sink at subduction zones, because as they cool, they become more dense than the underlying mantle. The cooler sinking plate pulls the rest of the warmer plate along behind it.
Similar to an anchor pulling on an anchor line

95
Q

slab-pull theory issues

A

if the only important force in plate tectonics is the gravitational pull of subducting slabs, why did Pangaea break apart and the Atlantic Ocean open up?
There are only 2 subducting slabs of lithosphere currently attached to the North and South American plates are found in the small island arcs that bound the Caribbean and Scotia seas, which are thought to be too small to drag the Atlantic apart.
Possibiilities: Overriding plates feel a force of suction from the subduction trench?
What about a pushing force?

96
Q

ridge push

A

newly-formed plates at oceanic ridges are warm, and so have a higher elevation at the oceanic ridge than the colder, more dense plate material further away; gravity causes the higher plate at the ridge to push away the lithosphere that lies further from the ridge

97
Q

What drives plate tectonics?

A

is not a direct result of mantle convection, but to gravity acting on density differences in the lithosphere that have resulted from its own thermal history.

98
Q

Global Pattern of Volcanism:

Divergent Plate Boundaries

A

Basalt-producing spreading centers

mantle source for lava (decompression melting)

axial volcanoes of mid-ocean ridge

99
Q

Global Pattern of Volcanism:

Volcanism in subduction zones

A

chains of volcanoes
island arcs
formation of new continental crust

100
Q

Global Pattern of Volcanism

Intraplate volcanism

A

hot spots and mantle plumes
sea mounts and island chains
large igneous provinces

101
Q

Why does liquid Magma form?

A

The Earth remains hot inside because of decay of radioactive elements.
Even though there is a lot of heat in the Earth, most of the crust and mantle remain solid because of immense pressures.
Magma forms only in special places, where conditions trigger melting of pre-existing solid rock:
decompression
addition of volatiles
heat transfer

102
Q

Decompression melting

A

takes place where mantle rock rises slowly
as rock moves up, its pressure becomes less
temperatures remain nearly unchanged because rock is such a good insulation

103
Q

Melting Due to Addition of Volatiles

A

when volatiles mix with hot mantle rock magma can form
volatiles are substances that evaporate relatively easily such as:
water
carbon dioxide
when volatiles mix with hot, dry rock, they cause chemical bonds to break so that the rock begins to melt
this is called flux melting

104
Q

composition of lava

A

The composition of newly formed lava depends on several things:
The chemical species present in the melt
The temperature and pressure at which the melt cools
Whether it is intrusive or extrusive

105
Q

mafic melts

A

Mafic melts contain a relatively high proportion of magnesium and iron oxide compared to silica,
ma in mafic stands for magnesium and -fic comes from the Latin word for iron

106
Q

felsic melts

A

have a fairly high proportion of silica compared to magnesium and iron oxide

107
Q

Lava Types Basaltic Lavas aa

A

lava that looks like clumps of moist, freshly plowed earth.
forms when lava loses its gases and consequently flows more slowly than pahoehoe, allowing a thick skin to form.
As the flow continues to move, the thick skin breaks into rough, jagged blocks.

108
Q

Lava Types Basaltic Lavas pahoehoe

A

Hawaiian for “ropy”
Forms when a highly fluid lava spreads in sheets and a thin,
glassy, elastic skin congeals on its surface as it cools

109
Q

Lava Types Basaltic Lavas pillow lavas

A

piles of ellipsoidal, pillowlike blocks of basalt about a meter wide
Pillow lavas are an important indicator that a region on dry land was once under water.

110
Q

andesitic lavas

A

<1000 C
Andesite is an extrusive igneous rock with an intermediate silica content. Andesitic magmas are produced mainly in the volcanic mountain belts above subduction zones.
Viscous
The temperatures of andesitic lavas are lower than those of basalts, and because their silica content is higher, they flow more slowly and lump up in sticky masses

111
Q

rhyolitic lavas

A

<600,800C
Rhyolite is an extrusive igneous rock of felsic composition (high in sodium and potassium with a silica content greater than 68 percent.
Highly viscous.
Rhyolitic magmas are produced in zones where heat from the mantle has melted large volumes of continental crust.
Found in Yellowstone.

112
Q

mafic lava

A

relatively low viscosity. it can erupt in fountains, move long distances and form thin lava flows

113
Q

felsic lava

A

when it erupts it may form a mound-like lava dome around the volcano’s vent

114
Q

Major volcanic gasses:

A

CO2, H2O, SO2

115
Q

most earthquakes occur at ______

A

plate boundaries (convergent, divergent and transform)

116
Q

the elastic rebound theory

A

Explains how earthquakes recur on active faults in Earth’s crust

Plates get locked together by friction, causing a buildup of stress

Instead of slipping along the fault as stress builds up, the blocks are strained elastically near the fault.

At some point, the strength of the rocks is exceeded. Somewhere along the fault surface, the frictional bond that locks the fault can no longer hold, and it breaks.

117
Q

seismic wave types

A

p waves - primary or compressional

s waves - secondary or shear waves

118
Q

how do we study earthquakes

A
  1. we need p and s wave arrival times from at least three seismographs
  2. then graph of distance traveled versus time elapsed
  3. finally triangulate the position of the epicenter
119
Q

main types of fault movement

A

normal fault (tension forces), reverse fault (compression forces), strike slip fault (shearing forces)

120
Q

Tube Worm: Riftia pachyptila

A

Unusual animal
No mouth
No anus
No digestive tract
Dependent upon bacteria living in its gut or “troposome”
Gills extracts hydrogen sulfide, carbon dioxide & oxygen from seawater; blood delivers these to troposome
In return, bacteria provide nourishment for Riftia

121
Q

vent ecosystems depend on 2 types of bacteria

A

free living bacteria, symbiotic bacteria

122
Q

3 endmember types of HTVs

A

Type 1: the most commonly reported (Black Smokers)
mafic-hosted
high-temperature system neovolcanic end-member fluid temperatures up to 407 °C low dissolved CH4 (e.g., East Pacific Rise, 9–10 °N)

Type 2: a distinct form of high-temperature venting (also often Black smokers) associated with serpentinization of ultramafic rocks
high H2, CH4, and Fe concentrations
e.g., Rainbow, 36 °N MAR

Type 3: White Smokers
involves serpentinization of ultramafic rock but yielding substantially lower fluid temperatures exiting the sea floor (∼40–90°C).
Lost City site, 30 °N MAR

123
Q

black smokers

A

sulfide rich, the chimney is made of sulfide ore deposits

124
Q

common characteristics of black smoker fluids

A 
Anoxic
Highly reduced
Acidic (pH 2-4)
Enriched in Silica, Hydrogen, Sulfide, Methane, Dihydrogen, Iron, Zinc, Copper.
Depleted in Magnesium
125
Q

white smokers

A

Cooler than black smokers (300 C down to 40 C)
Further off axis that black smokers
Example Lost City
60 meter tall chimneys
Chimneys made of Carbonate
Interaction of downward seeping seawater with mafic or ultramafic rocks produces an alkaline fluid that precipitates silica and Ba or Ca sulfates when it mixes with seawater, hence the white color
High concentrations of methane (CH4) and Hydrogen (H2)
High pH (9-11)
Low concentration of magnesium
Ultra Mafic rocks
More long lived that Black Smokers

126
Q

serpentinization

A

is a processes whereby rock (usually ultramafic) is changed, with the addition of water into the crystal structure of the minerals found within the rock

127
Q

lost city

A

The heat that creates the venting is not a result of interaction of seawater with hot magma
The heat is a result of an exothermic serpentinization reaction
These reactions give H2 and CH4 off as biproducts

128
Q

stromatolites

A

fossilized microbial formations (cyanobacteria) that date back 3.5 billion years
provide records of ancient life on earth

129
Q

chemotroph

A

do not gain energy from carbon, gain energy from oxidation of electron donors

130
Q

autotrophs

A

can fix carbon from carbon dioxide

need light and carbon to survive (in no light use energy from inorganic oxidation)

131
Q

island chains

A

made from hot spots

132
Q

island archs

A

made from subduction zone (aleutian islands)

133
Q

Geobiology

A

the study of the interactions between the biosphere and Earth’s physical environment
we study this bc microbes that move chemicals around resorvoirs can tell us a lot about early Earth

134
Q

how to megafauna survive at vents

A

H2, Ch4, H2S seeps out of rocks and provides energy for microbial species

Geological Oceanography (1 decks)

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