Final Study Flashcards

0
Q

The _______ explains how our solar system probably formed from a giant cloud of gases and dispersed solid particles.

A

nebular theory

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1
Q

Name the third planet from the Sun

A

Earth

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2
Q

As the solar system was forming, ____ came closest to undergoing nuclear fusion and becoming a second sun.

A

Jupiter

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3
Q

____ refers to the bright head of a comet.

A

Coma

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4
Q

One of the discoveries which led to modern view of the solar system was that the orbits of the planets are

A

ellipses

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5
Q

Total amount of solid material dissolved in water.

A

Salinity

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6
Q

Through volcanic eruptions, large quantities of water and dissolved gases have been emitted through geologic times. This is the principal source of water in the ocean and atmosphere.

A

Outgassing

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7
Q

A layer of rapid temperature change below the zone or mixing

A

Thermocline

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8
Q

Mass per unit volume but can be thought of as a measure of how heavy something is for its size.

A

Density

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9
Q

Rapid change of density with depth

A

Pycnocline

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10
Q

Zone of rapidly changing salinity that corresponds to the thermocline.

A

Halo line

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11
Q

Measurement of ocean depths and the charting of the shape or topography of the ocean floor.

A

Bathymetry

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12
Q

Also called sonar.
Invented in 1920s.
Primary instrument for measuring depth, that reflects sound from the ocean floor.

A

Echo sounder

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13
Q

Employs and array of sound sources and listening devices.

Obtains a profile of a narrow strip of the seafloor.

A

Multibeam sonar

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14
Q

Continental margins, ocean basin floor, and oceanic (mid-ocean) ridge

A

3 topographic units

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15
Q

Found along most coastal areas that surround the Atlantic Ocean.
Not associated with plate boundaries

A

Passive continental margin

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16
Q
Features:
Continental shelf
Continental slope
Submarine canyons and turbidity currents
Continental rise.
A

Passive continental margin features.

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17
Q

Flooded extension of the continent. Varies Greatly in width. Gently sloping. Contains oil and important mineral deposits. Some areas are mantled by extensive glacial deposits. Most consist of thick accumulations of shallow-water sediments.

A

Continental shelf

18
Q

Marks the seaward edge of the continental shelf.

Relatively steep structure. Boundary between continental crust and oceanic crust.

A

Continental slope.

19
Q

Deep, steep-sided valleys cut into the continental slope. Some are seaward extensions of river valleys. Most appear to have been eroded by turbidity currents.

A

Submarine canyons.

20
Q

Downslope movements of dense, sediment-laden water

A

Turbidity currents

21
Q

Deposits are called

A

Turbidity

22
Q

Found in regions where trenches are absent. Continental slope merges into a more gradual incline. At the base of the continental slope turbidity currents that follow submarine canyons deposit sediment that forms deep-sea fans.

A

Continental rise

23
Q

A cone shaped deposit at the base of the continental slope. The sediment is transported to the fan by turbidity currents that follow submarine canyons.

A

Deep-sea fans

24
Q

Located primarily around the margins of the pacific ocean where oceanic lithosphere is being subducted beneath the leading edge of a continent.

A

Active continental margin

25
Q

Continental slope descends abruptly into a deep-ocean trench.
Located primarily around the pacific ocean. Accumulations of deformed sediment and scraps of ocean crust form accretionary wedges. Some subduction zones have little or no accumulation of sediments.

A

Active continental margins

26
Q

Long, relatively narrow troughs that are the deepest parts of the ocean. Mostly located in the pacific ocean. Sites where moving lithospheric plates plunge into the mantle. Associated with volcanic activity (volcanic island arcs and continental volcanic arcs)

A

Deep-ocean trenches

27
Q

Chaotic accumulation of deformed sediment and scraps of ocean crust

A

Accretionary wedge

28
Q

Likely the most level places on Earth. Sites of thick accumulations of sediment. Found in all oceans.

A

Abyssal plains

29
Q

Isolated volcanic peaks. Many form near oceanic ridges. May emerge as an island.

A

Seamounts and guyots

30
Q

Flat-topped seamounts that have sank into deeper, colder water where carbonate material no longer accumulates.

A

Guyots

31
Q

Any submarine mountain of volcanic or tectonic origin.

A

Seamounts

32
Q

Characterized by an elevated position, extensive faulting, and numerous volcanic structures that have developed on newly formed crust.

A

Mid-ocean ridge

33
Q

Interconnected ridge system is the longest topographic feature on Earth’s surface . 23% of earths surface, winds through all major oceans, over 70,000 km in length. Along the axis of some segments are deep downfaulted structures called rift valleys. Consist of layer upon layer of basaltic rocks that have been faulted and uplifted. Has been studied more than any other ridge system.

A

Mid-ocean ridge

34
Q

Mud is the most common sediment on the deep-ocean floor

A

Mud

35
Q

Masses of water that flow from one place to another

A

Ocean currents

36
Q

Deleon from friction between the ocean and the wind that blows across the surface

A

Surface currents

37
Q

Large whirls of water within an ocean basin

A

Gyres

38
Q

5 gyres

A

North pacific, south pacific, north atlantic, south Atlantic, Indian ocean

39
Q

Currents are deflected to the right in the northern hemisphere and to the left in the southern hemisphere.

A

Coriolanus effect

40
Q

Currents from low latitudes into higher latitudes (warm currents) transfer heat from warmer to cooler areas.

A

Importance of surface currents

41
Q

Influence of cold currents is most pronounced in the tropics or during the summer months in the middle latitudes.

A

Climates influence on surface currents

42
Q

The rising of cold water from deeper layers. Most characteristic along west coasts of continents.

A

Upwelling.

43
Q

A response to density differences. Factors creating a dense mass of water is temperature and salinity. (temperature: cold watere is dense; salinity: density increases with increasing salinity.)

A

Deep-ocean circulation