Final Exam 2 Flashcards

1
Q

How do we know what the seafloor is like? Explain how man has been able to map the seafloor.

A

• Mapping the sea-floor was done almost by accident during WWI with the invention and use of sonar in submarines. Sonar has allowed us to map the seafloor.

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2
Q

How does the seafloor change as one travels from Atlantic coast of New England to the divergent plate boundary at the Mid Atlantic Ridge. Where would you find the coastal plain, continental shelf, continental slope, continental rise, abyssal plain, abyssal hills and rift valley?

A
  • The sea-floor gets newer and newer as you go from the coast of New England to the divergent plate boundary at the Mid Atlantic Ridge.
  • The coastal plane is located near the sea, it is a flat low-elevation area.
  • Continental shelf is the piece of continent that is submerged under water.
  • Abyssal Plain is essentially deep ocean where there is no continental landmass below the water.
  • An oceanic trench is a very deep (deeper than the abyssal plain) drop off between the continental shelf and abyssal plain.
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3
Q

➢ Have portions of the continental shelf ever been exposed at the surface? If so, when might this occur and how might this change its surface? Does the continental shelf area have any economic importance? Please explain.

A
  • Yes they have, during periods of glaciations where the sea level is low. This would change the surface by adding additional coastal regions.
  • The continental shelf area has huge economic importance in mining oil.
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4
Q

Identify the type of mass movement of sediment which occurs along the continental slope and rise. What submarine features do they give rise to?

A
  • The mass moving of sediment which occurs along the continental slope and rise is waves from the ocean which gives rise to beaches.
  • The submarine feature they give rise to is coral reefs.
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5
Q

How do waves form? What factors would increase a waves’ height? Understand and be able to explain the following terms: wavelength, wave height, and wave period.

A
  • Waves form from wind. Higher waves can be caused by higher wind speed, increased storm duration, and larger areas of wind.
  • Wave length is the distance between crests
  • Wave height is the vertical distance between crests and trough
  • Period is the time between successive waves to pass
  • It is also important to note that water moves faster on the top of the ocean than at the bottom (as depicted by the size of the arrows).
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6
Q

What causes breakers (breaking waves) in the surf zone? What is a long shore current? And how does it move sediment?

A
  • The swash zone is an upper part of the beach where erosion occurs.
  • Breaking waves are caused when a wave reaches certain height and cannot sustain itself, this generally occurs on the continental slope.
  • The long shore current (long shore drift) is the direction in which sediment moves because of waves, it moves sediment through a swash backwash motion. Whatever angle the wave comes in at (generally due to wind) is the direction of long shore current.
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7
Q

What are rip currents and why are they dangerous to swimmers? What do you need to do to escape one?

A

• Rip Currents are excessive water moving back to the sea creating a circular flow of water. They are dangerous to swimmers because they don’t allow you to swim back on shore, to get out of a rift current you must swim along the shore (the same direction as the long shore drift).

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8
Q

Explain what causes ocean tides on earth. Why are tides higher at some locations?

A

• The moon’s gravity causes tides on earth, the water is literally pulled towards the gravity of the moon causing a high tide. Tides are higher at some locations because the pull from the moon changes relative to how close something is to it.

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9
Q

identify some erosional coastal landforms

A

Example: Sea stack, wave cut cliffs, sea arch

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10
Q

How do seasonal changes affect beach profiles? Man-made structures like groins, breakwaters, jetties are used to prevent beach erosion. In general what is there affect where there constructed? And the affect down-current (down coast) of the structures?

A
  • Seasonal changes also effect the tides in the same way as the moon does. The sun’s position creates the seasons, although smaller, the sun has a gravitational pull that effects the tides. An example is the highest high tides will occur during the summer during a high tide, and the lowest low tides will occur during the fall during a low tide.
  • In the area where these man-made structures are created they reduce the erosion and wave impact, however the affect down-current is amplified due to these structures.
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11
Q

What are glaciers?

A

River of ice that flows down a valley like a very slow moving river until it meets a sea or lake then it is considered an iceberg which is a piece of ice floating in water.

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12
Q

Describe the two main types of glaciers and the environment in which they form. Be able to recognize modern examples of each.

A
  • Alpine glaciers – form on mountains

* Continental glaciers – form on continental land (such as Antartica)

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13
Q

How does the abundance of glacial ice affect sea level? Explain using the hydrologic cycle.

A

• As the amount of glacial ice increases sea level decreases, as glacial ice decreases sea level rises.

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14
Q

Ice ages have occurred (or are occurring) on earth during which geologic periods? What evidence supports this hypothesis?

A

• Ice ages occur during glacial periods. Glacial periods occur when temperature levels are low, this occurs when CO2 levels are low. CO2 levels can be calculated from rocks.

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15
Q

What factors are believed to cause ice ages (long-term causes)?

A
  • CO2 levels

* Change in the eccentricity and tilt of the Earth’s orbit/axis

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16
Q

What factors cause the glacial and interglacial fluctuations within ice ages? (i.e. describe the three astronomical factors that affect the amount of solar radiation striking the earth.)

A
  • Short term orbit of earth around sun
  • Eccentricity
  • Earth’s Angel of Orbit
17
Q

Consider the video, “The Great Floods”. Briefly explain how the Channeled Scablands formed. Be sure to include which type of glaciation was involved. What key geologic feature (sedimentary structure) indicates the volume of water that was involved in flooding?

A

• The “mega ripples” indicates the volume of water that was involved in flooding.

18
Q

What is the Palouse loess and how did it form?

A

• The Palouse Loess formed from the accumulation of wind-blown silt and sediment that is loosely cemented together. ‘Loess’ originates from the word ‘Loose”

19
Q

Be able to put the following events that formed the Palouse region in relative order: the formation of the Palouse Loess, the formation of the Columbia River Basalts, the formation of the Channeled Scablands.

A

Oldest to Youngest: Columbia River Basalts → Palouse Loess → Lake Flood)

20
Q

Consider the video, “The Little Ice Age, Big Chill”. What are some of the consequences of a small change in the temperature on humankind? What factors contributed to the advance of the Little Ice Age? Could global warming lead into global cooling and the onset of a glacial advance?

A

• Small changes can cause famines (due to crop death) and they can cause harsh winters.
• They caused wars
• The possible factors contributing to the Little Ice Age were:
o Increased volcanic activity
o Less fresh water circulating with the salt water oceans (slowed down the ocean conveyor)
o Low solar activity

21
Q

Describe the differences between P and S waves (velocity, type of motion)

A
  • P Waves are much faster than S waves and can travel through the entire earth (including its liquid outer core)
  • S Waves are slower, and cannot travel through liquid – thus they have a larger shadow zone because they cannot travel through the earth’s outer core
22
Q

How does Moment-Magnitude differ from the Richter scale?

A

• Moment-Magnitude scale can find the magnitude of an earthquake quicker and is more reliable with larger earthquakes. The Richter scale was created first. Both scales are on a scale of 10 and the values are fairly similar.

23
Q

Describe the different effects of earthquakes (tsunami, liquefaction)

A
  • Tsunamis often occur following an earthquake.
  • Liquefaction is where the ground moves so rapidly that liquid is brought up to the top and the ground acts plastic like.
24
Q

Is it possible to experience a tsunami, without feeling an earthquake? Explain your answer.

A

• Yes it is, an earthquake can spark a tsunami far enough away where you don’t feel the earthquake but the tsunami will still make its way to you.

25
Q

Understand the relationship between earthquakes and plate tectonics.

A

• Earthquakes occur when there is large plate movement. This is also why after-shocks occur, it is essentially the plates trying to balance out.

26
Q

How are mid-plate earthquakes explained?

A

• When plates (at plate lines) clash together it creates shockwaves that can cause mid-plate earthquakes.

27
Q

From the video, “The Day the Earth Shook” describe the similarities and differences between the Kobe and Northridge earthquakes. Geologically, why were there more fatalities in the Kobe earthquake?

A

• The earthquakes were similar magnitudes however there was much more damage in Kobe than in Northridge due to Northridge being less populated and having better constructed buildings.

28
Q

Describe the differences between P and S waves (velocity, type of motion, ability to move through solids and liquids, etc.). What do seismic waves tell us about the earth’s interior?

A
  • P Waves → Faster than S Waves → Can move through solids, liquids, and gasses (such as the earth’s outer core)
  • S Waves → Slower than P Waves → Cannot move through liquids (cannot move through the earth’s outer core)
  • Seismic waves tell us that the earth’s outer-core is liquid. S-wave’s shadow zone is much larger in comparison to P-wave’s shadow zone because S-wave’s cannot travel through the earth’s outer core.
29
Q

How does the velocity of both P and S waves change as they move through the earth?

A
  • P-Waves velocity increases as it enters the mantle, once it hits the outer-core (liquid) the velocity slows down, and then speeds back up once It hits the inner core. P waves travel fastest through solids.
  • S-waves velocity is slower than P-waves. Similarly to P-waves S-wave’s velocity increases as it enters the mantle. Once the S-wave reaches the liquid outer-core the velocity goes to 0 because S-waves cannot travel through liquid.
30
Q

What are earthquake shadow zones? What causes P wave shadow zones to form? What causes S wave shadow zones to form?

A
  • Earthquake shadow zones are areas that cannot feel the P or S waves of an earthquake.
  • Refraction of P-waves when they hit the outer-core causes P-wave’s small shadow zone.
  • S-waves cannot travel through liquid, so they cannot go through the outer-core which creates a large shadow zone.
31
Q

What do seismic waves tell us about the Earth’s interior?

A

• They tell us that the outer-core is liquid.