Exam II Review Flashcards

1
Q

How old is the Earth?

A

4.565 Ga

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2
Q

Order of eras

A

(youngest to oldest) Cenozoic, Mesozoic, Paleozoic

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3
Q

Meaning of ka, Ma, Ga

A

thousands, millions, billions

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4
Q

What distinguishes the mechanical layers? How do they relate to the compositional layers?

A

Lithosphere: rigid solid (crust and upper mantle, including Moho)
Asthenosphere: weak solid (mantle)
Outer core: liquid (core)
Inner core: solid (core)

The lithosphere is primarily oxygen/silicon/aluminum/magnesium, the asthenosphere is primarily oxygen/silicon/magnesium, the outer core is mostly liquid iron, and the inner core is mostly solid iron.

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5
Q

What layers within the Earth are liquid?

A

Outer core

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6
Q

Differences between continental and oceanic crust

A

Continental: less dense, thicker, more buoyant, plagioclase feldspar (must abundant mineral)
Oceanic: thinner, more dense, made of basalt and gabbro

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7
Q

About how fast do plates move?

A

1-15 cm/yr

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8
Q

Types of plate margins and most highlighted examples of each

A

Convergent: north american plate meeting pacific plate
Divergent: mid atlantic ridge, east african rift
Transform: fracture zones around mid atlantic ridge

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9
Q

Volcanism, earthquakes, and mountains at different kinds of plate margins (info in the table)

A

table, bitch, table

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10
Q

Where are volcanic arcs formed? Know highlighted examples

A

Subduction zones (either oceanic subducts continental or oceanic subducts oceanic)

Mariana Islands, Cascades, Andes

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11
Q

What is the difference between a theory and a hypothesis?

A

Hypothesis: An explanation for observations to be tested (may be supported, not confirmed)

Theory: An explanation for observations that have been tested numerous times and is supported by evidence

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12
Q

What are the four components of the definition of a mineral used in lecture?

A

1) solid
2) naturally occurring
3) crystalline structure
4) definable composition

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13
Q

Cleavage vs crystal form (how are they different?) Why is one more useful than the other?

A

Cleavage: a mineral breaking on planes of atomic weakness

Crystal form: how a mineral grows unimpeded (has crystal faces)

Cleavage is more useful bc most minerals don’t have a perfect environment to grow unimpeded in

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14
Q

Most abundant mineral in crust of the Earth

A

fuckin plagioclase feldspar

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15
Q

In order, what are the two most abundant elements in the crust and the Earth as a whole?

A

Crust: oxygen, silicon

Earth as a whole: iron, oxygen

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16
Q

What are the three rock types, what differentiates them, and what are their rock forming processes?

A

1) Igneous: made from magma
2) Metamorphic: recrystallizing in solid state
3) sedimentary: rock fragments/dissolved rock components compacted on surface

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17
Q

Origin of mafic versus felsic magma

A

Mafic magma comes from mantle (50% SiO2)

Felsic magma comes from crust (75% SiO2)

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18
Q

How do we interpret grain size in igneous rocks? (cooling rate and depth)

A

Larger grains form at a slower cooling rate deeper w/in earth

Small grains form at fast cooling rate at or near surface of earth.

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19
Q

Which is more explosive, basaltic magma or rhyolitic magma? Why?

A

Rhyolitic magma is more explosive because its high viscosity traps more dissolved gas and keeps it at a higher pressure than the atmosphere

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20
Q

What kinds of volcanoes are created by effusive and explosive eruptions of basaltic, andesitic, and rhyolitic lava?

A

Effusive Basalt: shield
Effusive Andesitic: composite
Effusive rhyolitic: dome

Explosive basalt: cinder cones
Explosive Andesitic: composite
Explosive rhyolitic: calderas

be able to recognize all of these in photos

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21
Q

What is the leading cause of fatalities in volcanic eruptions?

A

pyroclastic flows

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22
Q

What are the two types of weathering? Examples of each?

A

Physical: frost wedging, root wedging

Chemical: dissolution, hydrolysis, oxidation, hydration (creates clay minerals like Kaolinite)

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23
Q

Relationship between grain size and surface area to volume ratio (reading)

A

Small grain size means high surface area to volume ratio 🤷🏻‍♀️

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24
Q

What is soil?

A

Unconsolidated geologic material that has been modified at Earth’s surface by weathering and addition of organic material

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25
Q

What group of minerals is a product of weathering and common in soils?

A

Clay minerals

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26
Q

Order of the five horizons in soil

A

OAEBC

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27
Q

Origin of O and E horizons

A

wet conditions (that’s what she said)

O is top soil with organic material
E is transition soil

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28
Q

How do soils vary according to latitude, slope, and age?

A

Latitude: thin soils in desert, thick/organic in tropical conditions, slow chem weathering in arctic (chem weathering happens at high temps)

Slope: accumulates at base of slopes, closer to oceans/shores etc

Age: the older, the thiccer (the younger, the thinner, the less organic)

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29
Q

What are the key nutrients in soil

A

Nitrogen
Phosphorus
Potassium

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30
Q

What, and when, was the dustbowl

A

A period of massive windblown soil loss in the 30s

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31
Q

What is the SD state soil?

A

Houdek soil
a loam
old glacial deposits -> thousands of years as a grassland

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32
Q

Four classes of sedimentary rocks:

A

clastic, chemical, biochemical, organic

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33
Q

What are the two aspects of lithification, turning sediment into sedimentary rock?

A

compaction + cementation (but also be aware of physical and chemical weathering, I think?)

34
Q

What are the grain size boundaries for sand/sandstone? (mm)

A

1/16-2 mm

35
Q

What is the concept of uniformitarianism; what are simple examples of its application?

A

Definition: processes we see active today were active in the past and explain analogous characteristics observed in rocks

ex: crossbedding=sand dunes, poor sorting and striations=prolly glaciers?

36
Q

What is the basic unit of mapping sedimentary rocks?

A

formation: a mappable unit of related beds

- formations are basic units of geologic maps

37
Q

Know what sedimentary rocks are clastic, chemical, biochemical, and organic

A

Clastic: conglomerate, breccia, sandstone, mudstone, arkose, siltstone, shale

Chemical: evaporites (halite and gypsum), some limestones and cherts, travertine

Biochemical: most limestones, most cherts, carbonate rocks containing calcite, chalk, fossiliferous, micrite

Organic: coal, oil shale

38
Q

What are transgressions and regressions? (Be able to to recognize sequence as presented in lecture)

A

Trans: when the sea advances upon the land

Regs: retreat of the sea from the land’s surface

Sequences to recall:

  • trans: (from top to bottom) limestone-shale-sandstone
  • regs: (from top to bottom) sandstone-shale-limestone

so wherever sandstone is determined where the ocean STARTED

39
Q

Know the highlighted feature of rocks distinctive to each of the following paleo-environments: dunes, glaciers, streams, swamps, deep open oceans, and arid lakes

A

Dunes: grains are pocked/frosted, large cross beds

glaciers: poorly sorted boulder conglomerates, glacial striations, boulders floating in silt and clay
streams: conglomerates, sandstones, shales, channels in beds, cross bedding, current ripples
swamps: coal, lots of organic material and water

deep open oceans: shales and bedded cherts (silica shells accumulating)

lakes: thin beds of shale, wave ripples, rain drop impressions, mud cracks, halite and gypsum (evaporites)

40
Q

Know two sedimentary structures that can be used to determine paleocurrent directions (and be able to tell direction based on a picture of cross beds)

A

crossbedding and ripples

41
Q

General aspects of the two highlighted ways in which tectonics creates sedimentary basins

A

convergent boundaries: compressional thrust faulting and folding creates foreland basins (Appalachian Basin)

divergent boundaries: extension from tectonic divergence causing faulting in which some blocks are down-dropped…creates continental rift basins (Newark Basin)

42
Q

How is metamorphism different from igneous processes?

A

It recrystallizes in the solid state, not the liquid state

43
Q

How does foliation orientation relate to directions compressional tectonic stresses?

A

Foliation orientation forms perpendicular to tectonic stress

44
Q

General ideas of metamorphic grades and facies

A

grade: conditions of pressure and temp (low, intermediate, high)
facies: fields on a PT graph that are named after some rocks that form there

45
Q

Basics of two “environments” of metamorphism discussed in lecture

A

1) contact metamorphism (heat from igneous intrusion)

2) regional metamorphism: heavy on pressure and temp

46
Q

What makes a good metamorphic index mineral? (be able to distinguish good and poor index minerals on a diagram)

A

A ‘good’ index mineral is one that has a limited PT range of stability and defines its conditions more narrowly

47
Q

What controls the mineralogy of a metamorphic rock?

A

The starting material (protolith) and the conditions of metamorphism (pressure, temp)

48
Q

Know plausible protoliths for marble, quartzite, and amphibolite

A

marble: limestone
quartzite: sandstone
amphibolite: basalt

49
Q

Recognize schist vs gneiss vs quartzite in pics

A

schist has lots of foliation, gneiss is banded, and quartzite has neither/looks more grainy

50
Q

Know the sequence of four metamorphic rocks created by progressive metamorphism (low to high grade) of a shale protolith

A

With shale as protolith (from low to high) we have…

1) slate
4) phyllite
3) schist
4) gneiss

51
Q

Two settings in which we find extensive exposures of metamorphic rocks

A

1) shields (Canadian Shield)

2) exhumed orogenic belts (Black Hills)

52
Q

Where do we find metamorphic rocks in SD?

A

Black Hills (specifically Custer, SD)

53
Q

Epicenter vs focus (hypocenter)

A

Focus/hypocenter: the place inside Earth’s crust where an eq originates

Epicenter: The point on the Earth’s surface directly above the focus

54
Q

Characteristics of eqs at different plate tectonic boundaries

A

Subduction zones: most powerful, can be deepest (Wadati Benioff)

Mid-ocean ridges: very shallow and weak

Transform fault zones: powerful, shallow

Continental collision: powerful, deep

55
Q

Where is the greatest concentration of intraplate eqs in the US? Why there?

A

New Madrid, Missouri (failed rifts from Precambrian and Mesozoic)

-crust is stronger in intraplate eqs and can transmit lots of energy

56
Q

Be able to roughly determine distance from an eq using seismometer record

A

1) find out delay time

2) look for where the delay time (vertical axis) is the same size between the two lines on the graph

57
Q

Characteristics of different types of seismic waves

A

Surface (rayleigh and love): slow, on surface, undulating water motion

S-Waves: shear motion perpendicular to ray path, moves thru interior, undulating water motion, can’t go thru liquid

P-waves: compression-motion parallel to ray path, move thru liquid, fastest waves

58
Q

Difference between magnitude and intensity

A

Magnitude: measure of energy

Intensity: measure of the effect on humans

59
Q

Difference between richter magnitude and moment magnitude

A

Richter: based on local seismograph measurement

Moment: represents actual energy release

60
Q

how much more energetic is an earthquake 1 magnitude than another? Difference of 2? etc

A

32x increase per magnitude (going up twice would be 1000x, 32 x 32)

61
Q

Basics of damaging secondary effects of earthquakes

A

fires, liquefaction, landslides, subsidence/lift, tsunamis

62
Q

At what kind of plate tectonic boundary are the greatest tsunamis generated? Why?

A

subduction zones (thrust faults); sudden vertical displacement of sea flow, pushes water up and down up and down

63
Q

Several parts of the US are most subject to tsunami hazards, where?

A

Washington + Oregon (pacific northwest), as well as CA, Hawaii, and Alaska

64
Q

What causes large local variations in shaking by earthquakes (eg, the San Francisco Bay Area eq in 89)

A

amplification of seismic waves in sediments

65
Q

How good are we at forecasting specific timing of earthquakes?

A

We can make long term predictions but not short term ones

66
Q

What are the three elements of long-range earthquake forecasts?

A

1) probability
2) specified magnitude
3) defined period of years

67
Q

Most fatal, most costly, and most powerful earthquakes?

A

Most fatal: Shaanxi China 1556 830,000 killed

Most costly: Japan 2011 $360 billion damage

Biggest: Chile 1960, M 9.5

68
Q

EQ in US that did tremendous damage via fire?

A

1906 San Francisco

69
Q

Types of Faults (identify in photos)

A

normal (hanging wall block goes down, foot wall block goes up)
reverse
thrust
strike slip

70
Q

Fault activity

A

active: movement in past 12 ka

potentially active: active in 2.6 Ma but not last 12 ka

inactive: no activity in 2.6 Ma

71
Q

Different ways that we learn about the interior of the earth

A

Seismic wave fronts and travel times, reflection and refraction of wave energy, magnetism, gravity

72
Q

what kind of seismic waves are not transmitted through a fluid/liquid

A

S waves cannot go through liquid/fluid

73
Q

What is refraction?

A

the bending of a ray as it passes through a boundary between two different materials

74
Q

What is the Moho?

A

crust-mantle boundary

75
Q

How do seismic waves refract when they speed up?

A

If a ray passes into a layer in which it travels more rapidly, it would bend up and toward the boundary

76
Q

The “low velocity zone” LVZ corresponds to what mechanical layer?

A

The asthenosphere! (specifically under the oceanic lithosphere!)

77
Q

What does the S wave shadow zone tell us?

A

that s waves can’t pass through the core/liquid/fluid

78
Q

Is there a P wave shadow zone?

A

Yes, bitch, there is. It’s caused by the waves’ velocity slowing down as it passed through the fluid of the outer core.

79
Q

What does seismic tomography tell us?

A

it creates a 3D image of variations in seismic-wave velocities within the earth to understand where waves will speed up and slow down (with anomalies of course)

80
Q

Use of seismic reflection studies

A

often used by gas and oil companies bc it defines subsurface bedding, stratigraphic formation contacts, folds, and faults