Geology Exam #2 Flashcards

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1
Q

What is the “norm” on Earth?

A

Change. There is no static period of earth. It is a dynamic planet with multiple types of change that occurs over different time periods (i.e. plate tectonics, volcanic eruptions, mass movement, etc.)

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2
Q

What makes Earth unique within our solar system?

A

Temperature range. Earth has liquid water that can only exist from 0-100 degrees celsius. Atmospheric composition (other planets might have toxic air, while we have a non toxic environment with oxygen, carbon dioxide, and nitrogen.)

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3
Q

What are the four “spheres” of Earth?

A

Lithosphere (rock), hydrosphere (water), biosphere (life, organisms), and atmosphere (air)

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4
Q

What two sources of energy drive interactions among the “spheres”?

A

The sun (radiant heat) and leftover heat (inner earth).

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5
Q

How old is Earth?

A

Around 4.5-5 billion years old (at least 4 billion years old).

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6
Q

On this diagram of Earth’s interior, note the properties of the Lithosphere and Asthenosphere, as well as the Crust and Mantle described in class.

A

The lithosphere is the uppermost layer of the earth. It includes the crust and some other layers. The plates sit in the lithospheric layer. It includes continental/oceanic crust and part of the upper mantle. The Asthenosphere is in between the mantle and lithosphere. This area is warm and shifts the tectonic plates above it.

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7
Q

What is Plate Tectonics?

A

Everything that happens as it relates to the tectonic plates moving around. The Asthenosphere convects heat and moves the plates above it on the lithosphere. There are convergent plates, divergent plates, and transform boundaries.

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8
Q

What phenomena do plate tectonics help to explain?

A

Earthquakes (strike-slip, convergent), volcanoes (divergent), mountain building (convergent), pangea. Subduction zones in convergent plate boundaries explain volcanic activity (Ring of Fire) as the denser plate dips below the other plate forming a new crust.

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9
Q

How many major tectonic plates are there on Earth?

A

8 major tectonic plates.

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10
Q

Where do plates interact?

A

At plate boundaries

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11
Q

Name/describe the different plate boundary types:

A

Divergent (spreads apart - mid atlantic ridge) creates new rocks and is usually volcanically active.
Convergent (oceanic intersects with continental) forces subduction and introduces water to rock underground. These zones naturally form magma. There are volcanic eruptions, earthquakes, etc.
Transform (strike-slip) where plates move past one another rigidly. This is often in the South West (California) and sees a lot of earthquakes.

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12
Q

Why do plates move? What causes new crust to form in one place and old crust to be consumed in another place?

A

As magma moves upwards from the ridges in divergent boundaries, it moves rocks out of the way forcing the plates apart (ridge push). At subduction zones, gravity pulls slabs of rock downwards under other plates. Ridge push and slab pull are the two main driving forces as to why plates move.

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13
Q

How fast do plates typically move?

A

A few centimeters per year (less than 10. Compared to growth of a fingernail).

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14
Q

What information can geologists get from the rock record preserved in the lithosphere?

A

Ideas of past climate (temps, water level, atmospheric pressure, etc.), where the sea level was, mass extinction, fossil foils, and more.

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15
Q

What guiding principle do geologists use to interpret the rock record?

A

Scientific method and the Principle of uniformitarianism (use what we see now to incur what happened in the past.)

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16
Q

Describe the relationship between elements, minerals, and rocks.

A

Elements are what form minerals, and minerals are discrete known combinations of elements together. Minerals are the building blocks of rocks.

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17
Q

What are the eight most common elements in Earth’s crust, in order?

A

Oxygen (46.6), Silicon (27.7), Aluminum (8.1), Iron (5.0), Calcium (3.6), Sodium (2.8), Potassium (2.6), Magnesium (2.1).
SIO4 (oxygen and silicon) naturally work together to form most of the rock we see and interact with. Oftentimes, the upper crust of earth is referred to as the silicate earth.

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18
Q

What is the common building block of most rock forming minerals (RFM)?

A

Oxygen & Sillicon

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19
Q

As we describe the rock cycle in class, make notes on the diagram about the processes and rock types that result from them.

A

In our rock cycle, rocks are born of magma. When magma hits the surface and cools, it becomes igneous rock. After long periods of weathering from the atmosphere, igneous rock turns into sediment (little pieces of rock transported from the hydrosphere). This sand is deposited along the coastline. These deposits become compacted and lithified to become sedimentary rock, (sandstone). Anywhere through the rock cycle, high temperatures and high pressure can alter rock type. Some metamorphisms cause crystals while others cause foliation (high degree of metamorphism).

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20
Q

Describe each of the following major rock types on Earth–how they are made and their appearance. Give one example of each rock type.

A

Igneous: magma cooling. Happens quickly (extrusive - magma through volcanic process/rapid motion is quickly brought to the surface and cools giving it no time to form crystals. It is smooth like glass or obsidian) or slow (intrusive - slowly pushed to surface where it forms bigger crystals over a long period of time). Ex: granite, diorite, basalt, etc.
· Sedimentary: unlike igneous, sedimentary rocks are glued together with some material. There are individual layers easily seen. Ex: conglomerate, sandstone, shale, limestone, etc.
· Metamorphic: Harder to distinguish. Foliation or lineations where crystals have aligned into bands. Heated and/or pressured to realign material. Ex: marble, gneiss, schist, metaconglomerate, etc.

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21
Q

Give one example of how part of the rock cycle in the lithosphere is linked to the hydrosphere or atmosphere:

A

Weathering. Water is the strongest example of this. For example, water slowly breaks down rocks such as limestone. Moving winds carrying sediment also is an example of weathering.

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22
Q

What are some agents of change when it comes to metamorphism of rocks?

A

Heat/pressure & hydrothermal metamorphism

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23
Q

Where do we find the highest temperatures and pressures related to metamorphism in the crust?

A

Anywhere near magma there will be high temperatures or pressure around plate boundaries, fault lines, and hotspots (Hawaii). Plate boundaries, divergent boundaries (upwelling magma), and convergent boundaries (creating magma).

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24
Q

Describe the concept of a “biogeochemical cycle”, including flux and reservoirs.

A

Matter moving around through the spheres of the Earth. Matter can either be accumulated and then it can be stored elsewhere. Flux is how it moves/amount of chemicals moved during these processes over time, and reservoirs is where it collects (crust or oceans).

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25
Q

What are the six most important biogeochemical cycles to life on Earth?

A

CHNOPS (carbon, hydrogen, nitrogen, oxygen, phosphorus, and sulfur).

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26
Q

Where does the nitrogen in soil come from, naturally?

A

Nitrogen is naturally in the atmosphere. Trees, plant life, and bacteria use nitrogen through their respective processes and deposit it into the soil where it can be used by even more organisms.

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27
Q

Where does phosphorus in soil come from, naturally? Does it cycle quickly?

A

Phosphorus comes from decomposers, excretions, etc. It comes from man-made fertilizers too. It does NOT cycle quickly, but it needs to.

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28
Q

Give four examples of natural hazards faced by humans:

A

Earthquakes, volcanoes, hurricanes, flooding, tornadoes, landslides (mass wastings).

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29
Q

What does it take to cause a natural disaster?

A

Eruptions and earthquakes commonly cause other natural disasters.

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30
Q

What is the role of science when it comes to natural disasters?

A

The role of science is to predict and prevent natural disasters as well as mitigate them.

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30
Q

Mass wasting is a general term for what?

A

Landslides (sediment movement, soil creep (thousands of years)). Topography and edge of slope/steepness affect mass wasting.

30
Q

What is science good at, and not always good at, with natural disasters?

A

Science is good at where they will be, but it is bad at when they will come.

30
Q

As scientists concerned for society, what two factors play a role in determining the effects of natural disasters? What is their relationship to one another?

A

Magnitude & Recurrence frequencies. They have an inverse relationship. A really strong magnitude earthquake is very rare while tiny earthquakes are fairly common.

31
Q

Why are so many people susceptible to natural hazards?

A

So many people are susceptible to natural hazards because they often live close to plate boundaries. Western coast - earthquakes. Japan - tsunamis. Additionally, how you build a building plays into this issue.

32
Q

What are the main factors involved in whether mass wasting will occur?

A

Substrate (sediment), and the angle of incline/repose are the main factors involved in mass wasting. Blocky sediment is less likely to move and fall compared to round rocks.

33
Q

Do all mass wasting events occur rapidly? What plays a role in determining how rapidly they occur?

A

No (soil creep happens really slowly over a very long period of time). Major factor is friction. Clast type: angular rocks have more friction than smooth rocks. Water also plays a role in mass wasting risks.

34
Q

Provide two geotechnical solutions for mitigating mass wasting risk to people and property:

A

Retaining walls, fences, planting vegetation on slopes, and more.

35
Q

What are the main reasons why we have rockslides on I-40?

A

Angles of slopes are incredibly high with little to no vegetation to hold the rocks back from falling. These rocks are also limestone and shale, so they give way very easily. Water saturation is another reason why mass wasting can occur.

36
Q

What does the explosivity of a volcano depend upon?

A

Viscosity: if lava is very viscous it will move down the slope very slowly. If it is not very viscous, lava will flow fast and far.

37
Q

How does volcano shape act as a reference for how explosive a volcano might be?

A

If the volcano is steep (cinder cones), it will be more explosive. Low grade angles are not as explosive.

38
Q

Contrast the two styles of eruptions:

A
  • Effusive: slow with a consistent flow.
  • Explosive: very fast and relatively short lived.
39
Q

Airborne hazards from volcanoes include:

A

Tephra, ash, aerosols, gasses of various sorts (methane, carbon dioxide), etc.

40
Q

Ground-level hazards from volcanoes include:

A

Lava, lahars (mudflows: ash, water, sediment), and pyroclastic flows (this is the most dangerous hazard and has taken the most lives).

41
Q

At Mt. St. Helens, what were the precursors, or warning signs, that eruption was about to occur?

A

There were minor seismic events and a landslide that happened before the eruption.

42
Q

At Mt. St. Helens, what was the most deadly and damaging hazard?

A

The most deadly and damaging hazard was ash and pyroclastic flows.

43
Q

Describe how volcanic aerosols and gasses have disrupted regional and global atmospheric conditions in the past.

A

Aerosols increase albedo and can cool earth down. Gasses can increase the greenhouse effect and heat it up.

44
Q

Lake Nyos was especially deadly because its “eruption” was quiet. What erupted from the crater that was so dangerous?

A

It acted as a bowl of carbon dioxide that created a crater lake and suffocated the area.

45
Q

What likely triggered the Krakatoa eruption of 1883?

A

Volcano under a lake

46
Q

Can we stop volcanic eruptions?

A

No. There are too many factors to stop.

47
Q

What are some of the ways we can monitor volcanoes to determine whether an eruption will occur?

A

Seismometer networks, satellite networks, frequency, weather patterns, etc.

48
Q

Based on close monitoring and research, how do we classify volcanic activity?

A

Active (erupted recently), Dormant (not recent, but has potential), Extinct (will most likely not erupt in the near future).

49
Q

Mitigation, or minimizing damage to people and property, involves what kinds of techniques?

A

Modeling and mapping potential, response preparation, emergency preparedness of the public, degassing with pumps, diverting lahars, and spraying down (spraying water along the eruption).

50
Q

Are volcanoes all bad? What have they done for Earth?

A

No, they keep temperatures warm by putting some Carbon dioxide into the atmosphere and can increase the fertility of soils.

51
Q

What are two common causes of seismicity, or ground shaking?

A

Subduction slabs, deformation from landslides, etc.

52
Q

What are some non-fault-related ways to make seismic shaking?

A

Deformation from nearby landslides. Large amounts of mass wasting in the area.

53
Q

When an earthquake occurs, shaking radiates outward in all directions from the source. Describe how each type of seismic wave acts differently with respect to ground motion.

A

P-waves: compressional body waves of an entire block in an arch shape. Very compressed. P-waves are the primary waves that move quickly and get to new areas quicker.
S-waves: shear surface waves where the entire block travels in one direction in unison. These are slower and cause more damage along the way.
Love waves: shear surface waves make a back and forth motion across the surface.
R-waves: rolling surface waves (like waves of the ocean) ripple up and down along the surface.

54
Q

What do seismologists do to find the earthquake epicenter? Describe the steps:

A

Use multiple seismometers and seismographs to detect the distance from the measurement in conjunction.

55
Q

One measure of earthquake intensity is the damage it causes. What scale is used for this measure? Give an example of an index value.

A

The magnitude scale measures earthquake intensity. It ranges from 1 to 8.

56
Q

The Magnitude scale is an attempt to get at the amount of energy released. Which is more accurate, Richter or Moment magnitude?

A

Richter is good for fast measurements, but the Moment Magnitude scale is more accurate.

57
Q

Describe how the incremental increase of 1.0 magnitude affects the intensity of the earthquake. How much more intense is it?

A

An incremental increase of 1.0 magnitude affects the intensity of the earthquake logarithmically, so an increase from a 1 to a 2 is 10 times the intensity. Likewise, a 3 on the scale would be 100 times that of a 1 on the scale and so forth.

58
Q

How many great quakes can we expect in a given year?

A

About two per year.

59
Q

Why do some smaller earthquakes result in much higher human casualties?

A

If there is water upstream and a small earthquake breaks a dam or diverts water, there could be far more damage than expected. Rock type present also could result in more human casualties. For example, loose sediment leads to more mass wasting and more debris. Tsunamis also occur and can cause human casualties. Population density, and how one builds a structure also account for this.

60
Q

When it comes to the type of built structure, what factors are important to consider in a shaking event?

A

A brick building isn’t useful during an earthquake if it sits on the wrong building material. Smaller structures do fine on sand while larger buildings do not.

61
Q

Why would people feel a lower magnitude earthquake over a wider area in Virginia than a larger magnitude earthquake in central California?

A

Different types of rock and waves are both causes to this situation. For example, the central basin of California is mainly sand. Waves struggle to get through this material, so residents in these areas might not feel this earthquake as much. Virginia is over a seismic zone, so it is not surprising that they would feel more earthquakes. The East Coast has a lot of colder, harder bedrock while the West is structured with loose sediments.

62
Q

What kind of plate boundary causes seismicity throughout coastal California?

A

Transform boundaries (San Andreas Fault)

63
Q

What do engineers look for when assessing fault creep along portions of the San Andreas Fault Zone?

A

The slide distance in different areas across the fault line.

64
Q

What was the plate tectonic setting of the Tohoku earthquake in 2011?

A

Subducting zone.

65
Q

Why was that earthquake so destructive in a country that builds buildings to withstand earthquakes?

A

Structures were built along the coast, so Tsunami’s took out a lot of the buildings and caused mass destruction.

66
Q

Do all earthquakes occur at tectonic plate boundaries? Give 3 examples of areas where they occur away from plate boundaries and indicate their cause.

A

No. They also occur away from the main plates and can be caused by faults.

67
Q

What sorts of evidence have humans relied upon to predict earthquake occurrence?

A

Seismographs, map out fault zones, reoccurrence levels, wildlife, etc.

68
Q

What are three kinds of evidence used to determine recurrence intervals for earthquakes?

A

Modern data from seismographs, prehistoric indicators, and sedimentary layer deformation.

69
Q

In the event that we cannot predict exactly when an earthquake will occur, what are four things we can do?

A

Predict recurrence intervals, prepare the public, build structures to withstand seismic waves, and prepare the government for aftermath action.

70
Q

Give an example of a built structure that was modified to be earthquake resistant:

A

The oil pipeline with wheels on it to move with earthquakes.

71
Q

Describe the process of the “Stick-Slip Cycle” of earthquakes:

A

???

72
Q

Where is the epicenter of an earthquake relative to the fault rupture, or focus?

A

“On the surface” - the epicenter is felt above the surface, but it is usually far underground just above the fault rupture.

73
Q

Describe the relationship between tectonic plate subduction and earthquake depth: Where do deeper earthquakes occur? Where do shallow earthquakes occur?

A

If something is subducting it has to go way below the surface. The deeper earthquakes are in subduction zones. Shallow earthquakes can be found sometimes in convergent plate boundaries, but usually the most shallow earthquakes are found along transform boundaries and mid ocean ridges.

74
Q

When earthquakes occur, the ground shakes in response. How does the response differ depending on earth materials at the surface?

A

If you have looser ground, this earthquake might not be as violent; on the other hand, firmer material might cause incredibly violent shakes.