Topic 4-Coasts Falscards Flashcards
Igenous rock
Igneous rocks are formed when molten rock from the mantle cools down and hardens. Rocks form crystals as it cools. They are usually hard e.g granite
Sedimentary rock
Layers of sediment are compacted together until solid. Limestone and chalk formed from tiny shells and skeletons of sea creatures
Metamorphic
Formed when other rocks are changed by heat wnd pressure. New rock becomes harder and more compacted
Granite
Formed from magma cooled underground,resistant
-lots of joints which aren’t evenly spread so more joints more erosion.
-impermeable which creates moorlands
Limestone
Formed from tiny shells and skeletons of sea creatures. Very resistant and permeable and is resistant
Clay
Formed from muds deposited by rivers. Soft and crumbly. Weak
Chalk
A younger form of limestone. Medium resistance but stronger than clays
-forms enscarpmentd and cliffs at coasts
-permeable
Slates
Formed by heated muds. Very resitant and hard to weathering
-forms in layers creating weak planes in rocks
Formation of healand and bays
-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
Formation of a spit
-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
How do arch,stump,stack form
-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
Longshore drift
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
Traction,saltation,suspension and solution
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.
Constructive waves and destructive waves
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.
Concordant and discordsnt coastlines
Discordant-perpendicular, headlands and bays formed, coastal erosion and deposition
Concordsnt-parallel, coes, coastal erosion and landforms
Hudraulic action,abrasion,attrition in waves
Hydraulic action-waves crash against rocks and compress air into cracks. Puts pressure on rocks. Repeated action causes cracks to widen and break off
Abrasion-eroded particled in water scrape and rub ahainst rock,removing small pieces
Attrition-eroded particles in rock smash into each other and break into smaller fragments.
Mass movement, slumping and sliding
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.
Tectonic activity in the uk
-520 million years ago land that now makes up Uk used to be much closer to plat boundary than it is now. Active volcanoes formed magma through earth’s crust which cooled to form igenous rock.
-plate collisions caused rocks to be folded and uplifted forming mountains. Many of these areas remains as uplands
-the intense heat and pressure caused by plate collisions formed metamorphic rock in scotland ireland
-plate movements years ago mean that Britain was in tropics and higher sea levels meant it was partly underwater-canfiberous limestone formed in dhallow seas. Can be seen in uplands of peak district
-youngest rocks are chalk and clay in southern england.formed in shallow seas and swamps. Chalk and clay are softer rock ehich are more easily eroded-form low landscapes
Distinct land scapes-lake district uplands
Igeneous basalt rock from surface eruptions and granite iepgenous eruptuons below surface
-large volcanoes erupted at lake district 450-300 million years ago
-glacial processes 12000 years ago the uplands were under 300m of ice which eroded corries. Eroded huge areas to creat u-shaped valleys. Steepsides,flat bottom and hanging valley
-land is angular p u-shaped valleys and v-shaped valleys with steep mountains
-freeze-that weathering occured
-rockfalls and landslides occur
-misfit rivers are formed
-cold in winter and warm jn summer-rainsall year round
Distinct landscape UK-weald (lowland)
-sedimentary rock which are softer-green sand and chalk which are harder
-dry valleys,chalk froze making it impermeablr so when snow melted couldn’t infiltratr and ran over top causing valleys
-flat landscape with hills and v-shaped valleys. Shallow,floodplains, gentle landscape and vegetation
-biologicsl weathering and chemical weathering
-soil creep-soils such as sandstones and clay can absorb moisture and become saturated causing movement down slope
-floodplains formed
-wet and heavy rain. Warm in summer and cold in winter
Distinctive landscapes-upland
Settlement-farms-dispersed and isolated,farms and villages,small communities
Building material-local bricks and slate,stone
Field boundaries-follow shape of land,stine walls which are well structured, long lasting land
Farming-sheep farming and hay in winter valleys
Econimic activity-primary-agriculture,windmills
How have humans chnaged landscape-agriculture,forestry, settlement
Agriculture- people cleared land of forest to make space for farming
-hedgerows and walls to mar out fields
-differet farming-arable so flat kand with good soul for crops-dairy for warm and wet areas for dairy farming-sheep fatmint takes place in uplands which has led to a lack of tress.
Forestry-management of areas of woodland used for timber,conservation
-coniferous forests been planted for timber which are olanted in straight lunes so forests don’t look natural
-devidous woodland is being replanted in simebareas to make landscape more natural
Settlement- land was concreted over for roads and buildings which affected drainage patterns
-some rivers diverted through underground channels
-some river channels straightened or had embankments built to prevent flooding
-most of big citis are ports and industrial areas
Mechanical,chemical and bilogical weathering
Mechanical weathering-freeze-that weathering where water gets into cracks. Water freezes causing cracks to expand na d rocks fall off
Chemical weathering-seawter and rainwater have carbon dioxide dissolved which makes them weak carbonic acids. Carbonic acid reacts with rock that contains calcium carbonate.
Biological weathering-plants break down rocks by growing into cracks on their surface pushing them apart
Wave cut notch’s and platform formation
-waves cause most erosion at foot of a cliff
-forms a wave-cut notch which is enlarged as erosion continued
-rock above notch becomes unstable and collapses
-collapsed material washed away and new wave-cut notch starts to form
-repeated collapsing causes cliff retreat