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Weathering and what type of process is it?
Happens outside the water when rock is broken down by natural processes from the Earth
(ie, rainfall, temperature or chemical reactions)
in situ (at one place)
and its a sub ariel process
erosion and what type of process?
when rock is broken down by the force of water
its a marine process. This continuos action helps shape coast lines
name four different types of erosion
attrition, -
abrasion,
solution
and hydraulicaction
attrition
material (mainly rocks) carried by waves gets rounder and smoother
this is because it collides with other rocks/ materials causing sharp edges to get knoched off
abrasion
waves throw stones and rocks at cliffs
rocks scrape against the cliff wearing it away
rocks keep rubbing against cliff over time until it’s loose therefore eventually eroding
solution
chemical reaction its when salt water reacts with different rocks
chemical reaction between them causes rocks to slowly erode and disslove
hydraulic action
waves crash against cliffs at high forces
over time waves force air pockets into the cracks in the rocks
the air then expands causing cracks to widen and loosen
where would erosion be higher
large fetch (so long fetch allows waves to grow in height and strength, making them more destructive to the coastline because they generate more force)
softer rock (really weak so it erodes wuite quickly)
area with a lot of destructive waves (because strong the backwashes leads to erosion)
rocks with more gaps (hydraulic action)
name 3 main different types of weathering
freeze thaw
chemical
biological
what is mechanical weathering give examples
Mechanical weathering (also called physical weathering)
is the breakdown of rocks into smaller pieces without any chemical change.
The rock’s minerals stay the same, only the size and shape change. examples are feeze thaw and exfoliation
freeze thaw weathering when does it occus and how
occurs when rocks are porous (contain holes) or are permable (allows water to pass through)
water first enters cracks in the rock
temperature drops below 0 degrees celcius and the water turns into ice. It expands by freezing and begins to push the rock apart
then when temperature rises the ice in the crack will melt so the water makes it way deeper into the crack
process repeats until rock splits entirely
biological weathering + how could it be chemical
weathering cause by plants and animals
animals might burrow into cracks and plants might grow their roots within
so as burrow or roots grows the crack becomes larger causing small pieces of rocks to break away
(or lichens and mosses release chemicals that dissolve the rock)
chemical weathering
rainwater and sea waters are weak acids
so because of them coastlines made of limestone or chalk dissolves in water over time
(another examples is carbonation its when weak carbonic acids attack rocks)
exfoliation
common in hot climates aka onion skin weathering
surface layers of the rock are heated so it expands during day
at night the outer layer cools down and contracts more than rest of the rock
cracks will form and rocks start to peel away like an onion
what is meant by permability and what are impermable rocks
the permability of a rockk defines hiw vulnerable a rock is to erosion
Impermable rocks are less vulnerable as water is not absobed into the rock
what does igneous and sedimentry mean
igneous is the strongest rock therefore it erodes slowly
sedimentry is the weakest rock so it erodes really quickly
what is mass movement
the shifting of loose material downa slope
how does mass movement happen and what does it cause
Weathering weakens coastal rocks.
Gravity causes them to collapse (mass movement).
Material falls to the sea and is eroded by waves.
how are waves created
Waves are caused when the wind blows over the sea transferring some of its energy.
Friction with the sea water causes ripples to form and these develop into waves as they reach the coast.
what does a fetch do and what is it
a fetch determines the height if a wave
a fetch is how far and how long wind has been blowing over the sea
what is long shore drift and how does it work
long shore drift is the movement along the shore by wave action. It haooens when waves aproach the beack at an angle due to prevailing winds
the swash (waves moving up the beach) carries material up along the coast line
the backswash (waves moving back down the beach) carries material back down the beach at right angle
once the waves loose energy material is deposited further down the bay to form a beach
what type of weathering caused this
mechanical weathering (freeze thaw) this is possible due to low temperature
what type of weathering caused this and why
chemical weather the holes seen are formed due to rain (which is slightly acidic) -
so when the acid reacts with certain minerals dissolved the parts of rocks
so over a long period pits and holes such as the one you see are formed
what type of weathering is seen
biological weathering
the trees is seen growing in the cracks of the rock which will eventually erode it
3 main things waves do
they wear away or erode coasts
carry and transport eroded material
they drop or deposite it in sheltered areas when they loose energy
so waves shape the coastline by eroding transporting and depositing material
what’s traction, saltation and suspension
traction is when rocks roll aong the sea bed
saltation is when rocks bounce along the sea bed
suspension is when rocks are carried by the water
7 features of destructive waves
height- is high (more than 1m)
length- short
Frequency - more than ten a minute
energy- high
beach gradient- steep
main process- erosion
strong back wash but weakerswash
7 features of constructive waves
height- is low (less than 1m)
length- long
Frequency - fewer than ten a minute
energy- low
beach gradient- flat
main process- depostion
strong swash but weaker back wash