Coasts Falscards Flashcards

1
Q

Igenous rock

A

Magma cools down and hardens, Rocks form crystals as it cools down, Rock usually hard.

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2
Q

Sedimentary rock

A

Layers of sediment are compacted together until solid. Limestone and chalk formed from tiny shells and skeletons of sea creatures

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3
Q

Metamorphic

A

Formed when other rocks are changed by heat wnd pressure. New rock becomes harder and more compacted

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4
Q

Granite

A

Formed from magma cooled underground,resistant

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5
Q

Limestone

A

Formed from tiny shells and skeletons of sea creatures. Very resistant and permeable

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6
Q

Clay

A

Formed from muds deposited by rivers. Soft and crumbly. Weak

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7
Q

Chalk

A

A younger form of limestone. Medium resistance

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8
Q

Slates

A

Formed by heated muds. Very resitant

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9
Q

Formation of healand and bays

A

-sea attacks coast with alternating bands of hard and soft rock
- soft rick erodes more quickly than hard rock
-leaves land our called headland
- Areas with soft rock has eroded away are called bays

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10
Q

Formation of a spit

A

-Longshore drift moves sediment along coastline
-sudden change in coastline is required to occur
-behind headland a sheltered area is present where lower energy waves occur
- heaviest sediment dropped first and after smaller sediment is dropped
- ‘re-curved cause by 2nd wind’
- spit will not reafh to other side due to deep water and currents

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11
Q

How do arch,stump,stack form

A

-waves crash into headlands and enlarge cracks-abrasion and hydraulic action
-repeated erosion enlarges the crack to form cave
- continued erosion deepens crack and causes a arch
- erosion causes supporting arch to fall
-forms a stack

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12
Q

Longshore drift

A

Waves approach the sea at an angle, swash pushes material up the
beach at the same angle as the prevailing wind. Backwash carries the sediment back
dow

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13
Q

Traction,saltation,suspension and solution

A

Traction– large boulders are rolled along the sea
Saltation—smaller stones are bounced along the sea floor.
Suspension—sand and small particles are carried along in the flow.
Solution—some minerals are dissolved in seawater.

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14
Q

Constructive waves and destructive waves

A

Constructive waves— Have a
strong swash and weak
backwash, small waves under 1m
high. Encourage deposition.
Destructive waves—Strong
backwash, weak swash, taller
than 1m. Encourage erosion.

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15
Q

Concordant and discordsnt coastlines

A

Discordant-perpendicular, headlands and bays formed, coastal erosion and deposition
Concordsnt-parallel, coes, coastal erosion and landforms

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16
Q

Hudraulic action,abrasion,attrition

A

Hydraulic action—the weight and impact of water against
the coastline and cliffs erodes them.
Abrasion—breaking waves throw sand and pebbles against
the coast during storms.
Attrition—rocks and pebbles collide.

17
Q

Mass movement, slumping and sliding

A

Mass movement—the
downhill movement of
material under the
influence of gravity.
There are different types
that depend on the
material involved, how
saturated the material is
and the nature of
movement. E.g.
Sliding - loosened rocks
and soil suddenly tumble
down the slope.
Slumping—happens when
rock is saturated with
water and slides down a
curved slip plain.