component 2 (paper 2) Flashcards
geology
rock type
igneous rock
the earths oldest rocks and they are hard and fairly resistant to erosion
sedimentary rock
remains of animals and plants crushed together, layers of broken up rocks and some can crumble easily e.g sand stone and chalk
metamorphic rock
made by intense heat and pressure compressed over time underground
e.g marble and slate
what is the tees - exe line
the boundary between the highland areas of the uk and the lowland areas of the uk
what are the rocks like in the north
older and more resistant which creates upland landscapes such as the lake district (igneous / metamorphic)
what are the rocks like in the south
rocks are younger , less resistant which creates lowland landscapes such as the fens (sedimentary rock)
what is the landscape of the UK influenced by
geology - rock type
glaciation - the movement of ice on the land
tectonic processes - the movement of the crust
how does geology affect the UKs landscape
UK upland landscapes eg the pennines are formed from older , more resistant rocks whereas lowland landscapes eg the fens are made from younger , less resistant rocks
how has glaciation affected the UKs land scape
in the upland areas the wright of the ice eroded the river valleys making them wider and deeper ( U shaped valleys)
in the lowland areas the glaciers retreated and deposited everything they had eroded from the landscape , this created boulder clay which is very soft and not very resistant to erosion
how have tectonics affected the UKs landscape
the tectonic processes caused molten magma to intrude the plate , some magma reached the surface as lava , while some cooled and solidified underground . today these are areas of high relief eg the cairngorm mountains
anticline
an arch shaped fold in rocks created by tectonic activity
biological weathering
plant activity eg tree and shrub roots breaks rocks apart
chemical weathering
chemical reactions break down rocks
rainwater is mildly acidic and causes alkaline rocks such as limestone to dissolve
dry valleys
steep sided river valleys that formed during the last ice age
landslides
the rapid movement of rock fragments and soil under the influence of gravity
physical weathering
physical forces break rocks apart eg freeze thaw weathering which occurs when rainwater freezes in cracks and expands
rockfall
fragments of rock fall freely from a cliff face
scree
angular pieces of rock creates by physical weathering
slope processes
the downward movement of material on valley sides eg rockfalls, landslides or soil creep
soil creep
the slow , gradual downslope movement of soil
what is the general shape of the landscape in the lake district and the weald
lake district - an upland landscape , glaciers creates deep U shaped valleys and hollows now filled by lakes
the weald - a lowland landscape
weathering processes in the lake district and in the weald
lake district - grounds are covered in scree which makes it rough , scree consists of angular rock pieces created by freeze thaw weathering , each winter cracks expand and eventually the rock
the weald - chalk is calcium carbonate an alkali so is affected by solution , tree and shrub roots break up solid rocks
main slope processes in the lake district and the weald
lake district - scree fragments are unstable and move easily during rockfall , increasing danger for walkers
land slides are common as rain adds to the weight of the weathered rock so it slides easily
the weald - soil creep and rain discharges soil particles
effects of glaciation on the lake district and the weald
lake district - glaciers creates deep U shaped valleys and hollows filled now by lakes
the weald - unusual to find rivers , except when it’s saturated after wet weather. as climate warmed , water seeped through the chalk once again leaving dry valleys where rivers had once followed
what does Bradshaw model show
how river characteristics change from downstream from source to mouth
what are the 4 methods that rivers use to transport their load
traction
saltation
suspension
solution
how do meanders occur
the flow of the river swings from side to side and pushes the fastest current towards one river bank
how does an oxbow lake form
- as a meander bends and develops, it’s neck becomes narrower
- eventually the river may erode right through the neck, especially during a flood
- water then flows through the new , straighter channel and the old bend is abandoned
- opposition on the neck seals of the bend, leaving behind a horse - shoe shaped lake called an oxbow lake
what are floodplains
the wide flat areas of land that lie either side of a river channel . they are made by meanders as they migrate across the valley floor
what are levees
natural embankments formed along the banks of a river channel
how do deltas form
- the speed of a river decreases as it approaches the sea and it deposits most of the material that it has been carrying
- over time sediment builds up to create an almost flat area of new land, which is the delta
- because the river is now flowing very slowly over the almost flat gradient, it’s channel fills up with sediment and the river splits and spreads out into many different streams called distributaries
confluence
the point where a tributary meets the main river channel
watershed
the boundary between 2 basins
drainage basin
area of land drained by a main river channel and its tributaries
factors that affect the flow
the surface the precipitation lands on eg if it’s permeable it will lead to infiltration
amount of rainfall
how deep the the soil / rock is
physical cause of river flooding process
intense rainfall infiltrates the soil
the soil is quickly saturated so no more rain can infiltrate
surface run off takes water to the river quickly
discharge increases , causing the river to flood
how does urbanisation lead to river flooding
impermeable surfaces mean that water can’t infiltrate into the soil
this means there is a large amount of surface run off
discharge increases causing the river to flood
how does deforestation lead to river flooding
no trees, reduces the amount of interception
the soil becomes saturated quickly from the infiltration
no more rain can infiltrate which means surface run off takes start to the river quickly
discharge increases causing the river to flood
flooding case study - Sheffield 2007 key info
3 river flow through sheffield
there are a number of large reservoirs in the upper courses of sheffield’s rivers
there is steep relief to the west of sheffield
there are two confluences in the NW of the city
sheffield is a large city - an urban area with concrete and tarmac surfaces