Geography 4.3 - Geological Structure Flashcards

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1
Q

What is the rock type like on a concordant coastline?

A

Clays and sands

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2
Q

What features are found on a concordant coastline?

A

Concordant coastlines tend to have fewer bays and headlands.

A concordant coastline has the same type of rock along its length

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3
Q

What is the rock type like on a discordant coast

A

Limestone (hard)
Chalk (hard)
Clay and sands (soft)

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4
Q

What features are found on a discordant coast

A

Coastlines where the geology alternates between strata (or bands) of hard rock and soft rock are called discordant coastlines.

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5
Q

What are joints and faults?

A

A joint is a break (fracture) of natural origin in the continuity of either a layer or body of rock that lacks any visible or measurable movement

A fault is a crack in the Earth’s crust. Typically, faults are associated with, or form, the boundaries between Earth’s tectonic plates

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6
Q

Three factors of waves

A

First, the wind speed must be blowing faster than the transfer of energy from wave crest to wave crest. The second factor is the amount of time the wind blows, or wind duration. The third factor is the fetch, the uninterrupted distance over the sea for which the wind blows without a change in direction

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7
Q

How are spits formed

A

spit is an extended stretch of beach material that projects out to sea and is joined to the mainland at one end. Spits are formed where the prevailing wind blows at an angle to the coastline, resulting in longshore drift

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8
Q

Explain how beaches form

A

Beaches are the result of wave action by which waves or currents move sand or other loose sediments of which the beach is made as these particles are held in suspension

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9
Q

What is a bar

A

A bar is very similar to a spit. It is a ridge of sand or shingle which forms across the mouth of a river, the entrance to a bay or harbour. It is usually parallel to the coast.

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10
Q

What is the difference between a spit and a bar

A

Both of these landforms are the result of longshore drift and deposition of material by the sea so there is a definite similarity in the processes of their formation and development. Spits and bars are long, narrow accumulations of sand and/or shingle. … A bar starts in a similar way, and to begin with, is a spit

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