Shorelines Flashcards

1
Q

what are shorelines

A

dynamic environments

Erosional + depositional processes combine along coasts to create landscapes that undergo rapid change

Ancient shoreline deposits occur as rock bodies that are important oil + gas reservoirs

Wind-generated waves provide most of the energy that shapes + modifies shorelines

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2
Q

what is the processes of waves?

A

Energy in normal water waves (I.e. except tsunamis), is derived from the wind

Tops of waves (crests) are separated by wave troughs

Wavelength: horizontal distance btwn wave crests

Wave height: vertical distance btwn trough + crest

Wave period: the time it takes for 2 successive crests to pass a given point

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3
Q

how do waves move in deep water

A

In deep, open waters, water molecules move in a circular path during the passage of a wave

The circular motion rapidly diminishes w/ increasing water depth

At a depth equal to abt half the wavelength, the movement of water particles becomes negligible (this depth is called wave base)

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4
Q

how do waves move in shallow water

A

As waves approach a shoreline, their characteristics will change

Waves will “feel bottom” at a water depth equal to abt half their wavelength (wave base)

Friction w/ the seafloor slows down advancing waves at their bases (at the sea surface, crests are still moving quickly)

Wavelength decreases, wave heigh increases

Eventually, the waves collapse (“break”) in the surf zone

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5
Q

what happens after a wave breaks

A

After a wave breaks, water moves up the slope of a beach as a sheet (this is called “swash”)

The sheet of water slows, stops, then returns to the sea as “backwash”)

Backwash > swash = erosion (destructive)

Swash > backwash = deposition (constructive)

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6
Q

waves are powerful agents of what?

A

erosion

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7
Q

most sediment deposited along most shorelines are deliver to the sea by what?

A

streams

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8
Q

sediment can travel alongshore by ____

A

beach drift

Along most shorelines, waves approach the shore at an oblique angle

Swash carries suspended particles up the beach at an oblique angle

Water always refunds to the sea under the influence of gravity (as backwash) in a direction perpendicular to the shoreline

As a result, each sand particle on the beach moves in a zig-zag pattern down the length of the beach

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9
Q

what is a offshore drift

A

Seaward of a beach, oblique waves can also produce turbulent longshore currents

Longshore currents easily move fine suspended sand + roll larger + gravel along the bottom

If it were not for beach drift + longshore currents, redistributing sediment from river mouths, many beaches would be nearly sandless

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10
Q

what is a tide

A

Repetitive daily changes in elevation of ocean surface due to gravitational attraction btwn Earth + the Moon (to lesser extent, the Sun)

The Moon’s gravitational force produces a bulge in the ocean. Due to inertia, a matching bulge also develops on the opposite side

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11
Q

what are tidal cycles

A

Bc position of Moon changes very little in a single day, we can imagine the tidal bulges remaining in place while Earth rotates through them

The pattern is little more complicated bc of Earth’s tilt (tides tend to be unequal due to this)

Bulges migrate very slightly as the Moon orbits around the Earth

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12
Q

as tide rises, landward- moving water generates what?

A

flood currents

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13
Q

as tide falls, seaward-moving water generates waht?

A

ebb currents

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14
Q

where do wave-cut cliffs originate from

A

originate by the undercutting action of the waves against the base of coastal land

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15
Q

what are shorelines where deposition dominates over erosion

A

“Fair-weather wave base” (FWWB) is the maximum water depth affected by normal, day-to-day

“Storm wave base” (SWB) is the water depth affected by storm waves (deeper than FWWB)

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16
Q

what are the main “zones” from sea to land?

A

Offshore -> Shoreface -> Foreshore (beach) -> Backshore

17
Q

where is the offshore zone

A

Below FWWB

Due to lack of wave agitation, mud tends to be deposited here

During storms, sand may be deposited (if above storm wave base)

18
Q

where is the shoreface

A

Above “fair-weather wave base” but below low tide level

Concave-upward shape

Mostly sand (mud tends not to settle here as it is swept away by fairweather waves)

Sand bars form in upper shoreface due to breaking waves

Loss of wave energy -> local deposition of sand from suspension

19
Q

where is the foreshore

A

Lower, “wet” part of “beach”

Btwn low + high tide levels (aka “intertidal zone”)

Exposed to air during low tide

Affected by swash + backwash (sand may or may not accumulate depending on which is dominant)

20
Q

where is the backshore

A

Upper part of “beach”

Above high-tide level

Most sediment transported + deposited by wind (and is mobile due to lack of anchoring plants; commonly form aeolian dunes)

A storm beach face (marking the position of the beach during storms (affected by large waves)) on the seaward edge of the backshore

21
Q

where beach drift + longshore currents are active, what depositional features may develop?

A

spit
baymouth bar

22
Q

what is a spit

A

an elongated ridge of sand that projects from the land into the mouth of an adjacent bay

23
Q

what is a baymouth bar

A

is applied to a sand bar (sometimes originating as a spit) that completely crosses a bay, sealing it off from the open ocean

24
Q

what is barrier islands

A

Narrow buildups of sediment that are separated from the mainland by a lagoon

Can form during marine transgression

25
Q

what is a tidal delta

A

Gaps in barrier island system are produced by tidal channels

Tidal deltas are lobes of sediment deposited by tidal currents as they move shoreward + seaward w/ the changing tides

Tidal deltas can also develop in baymouth bars

26
Q

how to protect shorelines from erosional + depositional processes?

A

Construction of seawalls (protecting shoreline from breaking waves)

Breakwaters (built away from shoreline to reduce wave energy before waves reach the shore)

27
Q

what are groins

A

A barrier built at a right angle to the beach to trap sand that is moving parallel to the shore (by longshore current)

Advantage: sand is caught on the upcurrent side

Disadvantage: Sand is eroded on the downcurrent side (+ an angry neighbour)