Ocean Environments Test Flashcards

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1
Q

Coast

A

the zone where the land meets the sea

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2
Q

Drowned coast

A

“Submergent coast”
2 types: ria, fjords

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3
Q

Ria coast

A

sea-level rise has drowned a region of coastal river valleys forming a series of wide estuaries often separated by a long peninsula

*Prevalent in Northwestern Europe, eastern US, and Australia

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4
Q

Fjord coast

A

sea-level rise has drowned one or more deep glacier-carved valleys

*Prevalent in coastal Norway, Chile, Canada, and New Zealand

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5
Q

Estuary

A

salt water meets fresh water

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6
Q

Emergent coast

A

occur where land has uplifted faster than the sea has risen since the last ice age.

Areas that were formerly sea floor may become exposed above the shoreline while former beaches often end up well behind the shoreline or even on clifftops.

Staircase structures called marine terraces are created by a combination of uplift and waves gradually cutting flat platforms at the base of cliffs.

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7
Q

Global sea-level change

A

Most important cause: the increase or decrease in the extent of the world’s ice sheets and glaciers

Related to Earth’s climate

If it cools, more water is frozen into glaciers=less oceans

If it warms up, more water melts from glaciers=more ocean volume

Affects ocean water temperature

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8
Q

Local sea-level change

A

Occurs when a particular area of land rises or falls relative to the general sea level

One cause occurs in regions where oceanic crust is being forced beneath continental crust.

Another cause is the glacial rebound-gradual rise of a specific area of land after an ice sheet that once weighed it down rises.

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9
Q

Coastal landscapes

A

can be classified into primary or secondary.

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10
Q

Primary coasts

A

have formed as a result of land-based processes like land erosion and volcanic activity.

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11
Q

Secondary coasts

A

have been shaped by marine erosional processes or by activities of organisms like corals and mangroves and people.

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12
Q

Wave-erosion coasts

A

secondary coast

waves hurl beach material against the cliffs which abrade the rock
each wave compresses air within cracks in the rock and on reexpansion, the air shatters the rock.

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13
Q

Marine-deposition coasts

A

Formed by sediment brought to the coast by rivers, eroded from headlands, or moved from offshore by waves.

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14
Q

Spit formation

A

sand and water are carried past the headland by longshore drift but the sand settles at the mouth of an estuary where the waves are opposed by the sluggish outflow from a river.

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15
Q

Beaches

A

deposits of sedimentary material

Commonly occur on coasts above the low-tide line

Sources of beach material-sediment brought to the coast by rivers or eroded from cliffs or the sea floor or the biological material such as shells.

Wind can also influence beach development and is instrumental in forming coastal dunes

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16
Q

Foreshore

A

the area between the average high and low tide lines

The seaward side of the foreshore is the nearshore while behind is the backshore

Backshore is submerged only during the very highest tides and includes a flat-topped accumulation of beach material called a berm.

17
Q

beach face

A

The sloping area Seward of the berm making up most of the foreshore

18
Q

beach cusps

A

a series of crescent-shaped troughs

19
Q

swash zone

A

the part of the beach face that is covered and uncovered with water as the waves arrive

20
Q

surf zone

A

Seaward of the swash zone extending out to where the waves break

21
Q

what affects the type of beach that will form?

A

Level of wave energy, the direction the waves arrive from, and the geological makeup of a coast

22
Q

Dissipative beaches

A

Gentle sloping, absorb wave energy over a broad area, made up of fine sand

23
Q

Reflective beaches

A

Steep, shorter, and consists of coarser sediment

24
Q

Pocket beaches

A

Isolated between two headlands

25
Q

Headland

A

formed when the sea attacks a section of the coast; Looks like eroded rock

26
Q

Drift-aligned beaches

A

waves arrive at an angle and sediment is moved along the beach by longshore drift

27
Q

Beach Composition

A

Most beaches are composed of sand, gravel or pebbles produced from rock erosion

Sand grains of quartz and other minerals such as feldspar

Other materials: fragmented and skeletal remains of marine organisms

Higher wave energies=coarser materials

28
Q

Coastal Dunes

A

:

Formed by the wind blowing sand off the dry parts of a beach

Develop in the area behind the backshore which together with the upper beach face supplies the sand

For dunes to develop, the sand has to be continually replaced

29
Q

saltation

A

The actual movement of sand to form a dune occurs through a jumping and bouncing movement along the ground

30
Q

foredunes

A

The dunes closest to the shore. Behind them is a primary dune ridge, secondary dune ridge, etc.

31
Q

Marram Grass

A

common colonizer of embryo dunes (dunes in the beginning stages).

Develops deep roots that allow it to tap into groundwater.

Roots bind the sand together while the grass traps more blown sand assisting in foredune development.

32
Q

Estuary

A

connects to an open sea, is narrow, and receives freshwater from 1 or more rivers.

33
Q

Coastal lagoons

A

linked to the sea by one or more narrow channels through water flows in and out. Sometimes the channels open only at high tide.

34
Q

Estuary formation 4 ways

A

First- the sea level may rise and flood an existing river valley on a coastal plain.

second- the sea level can rise to flood a glacier-carved valley forming a fjord

Third- the coastal wave action can also create an estuary

Fourth- the estuaries result from movement at tectonic faults in Earth’s crust.

35
Q

Estuary environments

A

long and funnel-shaped, tides rush in

Fluctuations in salinity, reduction in photosynthesis, high concentrations of nutrients