Coasts PowerPoint Flashcards

1
Q

What are the physical factors influencing coastal landscapes?

A
  • winds: speed, direction and frequency
  • waves: wave formation, development and breaking
  • tides: tidal cycles and range
  • currents: global patterns
  • geology: lithology and structure
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2
Q

the energy of a wave is dependent on

A

the strength of the wind, its duration and the length of fetch

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3
Q

the source of energy for coastal erosion and sediment transport is

A

wave action

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4
Q

wave energy is generated by

A

frictional drag of winds moving across oceans; and is a result of fetch

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5
Q

fetch is

A

the length of open water which the wind can blow unobstructed

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6
Q

how do ocean waves build

A

Ocean waves build in response to the shear of wind blowing over the water surface. Higher-energy wind yields higher-energy waves. Within a passing wave, water follows a circular path. The circle radius decreases with depth.

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7
Q

how do waves break

A

As a wave approaches shore, friction slows its base.

Water motion in the wave becomes more elliptical, the wave oversteepens, and it crashes ashore as a breaker.

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8
Q

what is tidal range

A

Vertical distance between the high tide and the low tide

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9
Q

tidal range- place with highest tidal range

A

The Bay of Fundy, on the east coast of Canada, is often stated to have the world’s highest tides because of its shape, bathymetry, and its distance from the continental shelf edge

A max range of 16.8 m has been recorded

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10
Q

what are spring tides

A

Spring tides occur twice each lunar month all year long without regard to the season

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11
Q

what is a neap tide

A

When the sun and moons are at right angles to each other, there is least gravitational pull, meaning the tidal range is at its lowest. The neap tide occurs 7 days after the spring tide.

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12
Q

Two factors that will affect the horizontal distance over which the shoreline can migrate between high and low tide

A
  • Position of moon (neap and spring tides related to tidal range)
  • Slope of shoreline- if tidal range large and slope gentle the position of the shoreline can move a long way leaving a broad tidal flat exposed to the air
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13
Q

When a tidal current moves towards the land and away from the sea, it…

A

floods

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14
Q

when it moves toward the sea away from the land it…

A

ebbs

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15
Q

Tidal currents that ebb and flood in opposite directions…

A

results in horizontal motion producing currents called ‘rectilinear’ or ‘reversing’ currents.

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16
Q

2 types of ocean current

A
  1. Surface Currents: located at the ocean’s surface

2. Deep Currents: below 300 metres

17
Q

Thermohaline Circulation

A

Driven by temperature and salinity, which causes differences in density

18
Q

where may rip currents form

A

Rip currents may form around low spots in the ocean floor near the shoreline or in breaks between sandbars.
They may also form around human-made structures such as jetties and piers.