Coasts ch. 10 Flashcards

1
Q

What is the coast

A

The land of the continent adjacent to the beach

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Coast description

A

Land extending inland as far as marine influence is seen

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Offshore

A

Extends from breakers to edge of continental shelf

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Shelf

A

Continent that is submerged

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Examples of places that get marine influence

A

La Jolla, Point Loma

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Berm

A

The dry area at the foot of the coastal cliff (not part of the coast, part of the beach)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

instances when the berm is submerged

A

Tsunamis, storm surges, high tides (spring tides)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

wave cut platform

A

flat eroded bedrock at the beach, eroded by wave energy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Notch

A

Cave cut into sea cliff by wave energy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Where do you find offshore extending the farthest out

A

Passive Margins (longest cont. shelf)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Sources of sand on the beach

A

Erosion of the coastal cliff, rivers, cliff erosion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

where is there more sediment

A

continental shelves

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

summertime beach

A

alot of sand, low energy, low tide, wide berm

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Sandy beach

A

Wide Berm

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Wintertime beach

A

wave energy is higher, short, high waves

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Rocky beach…

A

Narrow berm

17
Q

green algae

A

water is polluted

18
Q

summertime vs. wintertime beach is b/c of

19
Q

Longshore current ->

A

movement of water in surfzone, paralell to the shore

20
Q

why is the longshore current parallel to the shore?

A

waves approach at an angle (from left to right)

21
Q

drift->

A

net movement of sand grains

22
Q

CA longshore current

A

N to S b/c of westerly winds

23
Q

oceanside compartment

A

transports sediments (sand) from N to S

24
Q

Classification of coasts

A

Depositional coast -> flat coast

25
why is it flat
because it is not active
26
Depositional coast-passive margin
the transition from land to sea is not associated with a plate boundary
27
Depositional coast-Subsidence
the gradual caving in or sinking of an area of land.
28
Depositional coast-Deposit sediment
the laying down of sediment carried by wind, flowing water, the sea or ice.
29
Depositional coast--Deltas
wetlands that form as rivers empty their water and sediment into another body of water (submergent coasts)
30
Depositional coast--barrier islands
thin ribbons of sand that line the US Atlantic and Gulf coasts and absorb the much of the force of storms like Hurricane Ian as they reach land
31
Erosional coasts
Eroding
32
Erosional coasts--coast is lifted
because it is tectonically active
33
Erosional coasts--active margin
A linear zone where tectonic plates either converge with one another (convergent margins) or shear past one another
34
Erosional coasts--tectonic uplift
the geologic uplift of Earth's surface that is attributed to plate tectonics.
35
Erosional coasts--cliffs
erosion and weathering. Weathering happens when natural events, like wind or rain, break up pieces of rock.
36
Erosional coasts--Headlands, sea caves, arches, stacks
caused by erosion, when part of the coast separates from
37
Erosional coasts--marine terraces
erosional landforms that develop due to the landward retreat of the active sea cliff in response to erosion by ocean wave energy
38
Marine terrace
any relatively flat surface of marine origin, bounded by a steeper ascending slope on one side and by a steeper descending slope on the opposite side.