Essentials of Oceanography Chap 2 Flashcards

1
Q

What is magnetic dip

A

The degree to which a magnetite particle
points into Earth

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2
Q

Relation of magnetic dip and latitude

A

Higher latitudes experience higher magnetic dip

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3
Q

How can we use paleomagnetism to find the original latitude a rock originated from

A

By looking at the magnetic dip, we can indicate the latitude the rock formed from

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4
Q

Where is sea floor spreading the greatest

A

Pacific

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5
Q

Difference between slopes of mid-ocean ridges that spread fast and slow

A

Slowly spreading mid-ocean ridges often have steeper slopes due to increased cooling periods and Quickly spreading mid-ocean ridges often have gentle slopes due to decreased cooling periods

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6
Q

What is an oceanic rise

A

gently sloping and fast-spreading mid-ocean ridge.

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7
Q

What is the difference between Oceanic Rises and Oceanic Ridges

A

Rises are fast spreading, ridges are slow.

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8
Q

relation of mid-ocean ridge spreading rate and earthquake size

A

A mid-ocean ridge with a faster spreading rate generally produces smaller earthquakes compared to a slow-spreading ridge

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9
Q

Volcanoes at Continental-Oceanic Convergent zones lead to what type of volcanic arc

A

Continental arc with intermediate composition

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10
Q

Volcanoes at Oceanic-Oceanic Convergent zones lead to what type of volcanic arc

A

Island Arc with Basaltic composition

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11
Q

Are earthquakes at spreading centers shallow or deep

A

Shallow

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12
Q

Are earthquakes at subduction zones shallow or deep

A

Deep

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13
Q

Why do earthquakes at subduction zones form so deep

A

1.Brittle fracturing(due to oceanic plate staying cold)
2. Stress accumulation(due to bending, stretching, and compression)
3.Phase Changes in minerals(minerals transforming into denser minerals can suddenly release energy and trigger deep earthquakes.)
4.Water trapped in minerals within the subducting plate is released due to high pressure and temperature which weakens the plate and can lead to deep earthquakes.

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14
Q

where do ALL transform faults form

A

between two segments of a mid-ocean ridge

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15
Q

3 stages of development in coral reefs

A

Fringing, Barrier, Atoll

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16
Q

What are Fringing Reefs

A

First stage of development in a coral reef, where reefs develop along the margin of a landmass where the temperature, salinity, and turbidity of the water are suitable for reef-building corals.

17
Q

What are Barrier Reefs

A

Second stage in development where the reef is a linear
or circular reefs separated from the landmass by a well-developed lagoon. The reef grows upward as the island or landmass subsides.

18
Q

What are atoll reefs

A

Final stage of reef development where the island or landmass completely submerges due to erosion and subsidence, leaving behind a ring-shaped reef surrounding a central lagoon

19
Q

Where do Coral Reefs form

A

The corals require a solid surface to settle on, often found on the new volcanic islands formed.

20
Q

What is a terrane

A

crust fragment formed on a tectonic plate and accreted or “sutured” to crust lying on another plate.

21
Q

What is western North America

A

Terrane, its crustal material sutured onto the American Plate

22
Q

What is the Wilson Cycle

A

a model that describes the opening and closing of ocean basins

23
Q

What are the different stages of Wilson Cycle

A

Embryonic(Uplift), Juvenile(Spreading), Mature(Spreading), Declining(Convergence), Terminal(convergence and uplift), Suturing(Convergence and Uplift).