Paper 2 Flashcards
Population density
The average number of people in a given area per km2
Population/area
Urban core
Urban area more than 10,000 people
Igneous rocks
The earths oldest rocks, made from lava that has cooled down
Sedimentary rocks
Formed from sediment eroded and deposited by rivers.
Metamorphic rocks
Sedimentary rocks that have been heated and compressed. This makes them more resistant
Examples of igneous rocks
Basalt
Granite
Examples of sedimentary rocks
Shale
Limestone
Chalk
Clay
Sandstone
Example of metamorphic rocks
Slate
Marble
Freeze thaw action
Water becomes trapped in cracks in rocks
The water freezes and expands
Then the ice melts
The process repeats, weakening the rocks
Rock fall
Fragments of rocks break away from the cliff face due to weathering
Landslide
Blocks of rock slide downhill
Mudslide
Saturated soil flows down a slope
Slumping
Saturated soil slumps along a curved surface
Formation of Malham cove
In the Carboniferous period, the uk was covered by sea. Coral skeletons formed strata and were turned into rocks by the cementation of calcium carbonate
Tectonic processes- tilted the strata creating the steep edge
Glaciation - rivers eroded into them creating valleys, and the last ice age deepened the valley
Yourkshire dales
Had limestone in the valley sides and boulders left from glaciation - good building stone for field boundaries
Flat relief in the bottom of valleys
Lived in houses built of stone
Sheep farming, because it was too cold to grow crops
Isolated farm structure instead of villages
East anglia
Geology is mainly sand and clay, till.
Produces fertile soil for crop farming, but nothing strong enough for building
Hedges used as field boundaries
Older building were made of flint that was in the chalk
Scarp and vale
Erosion leaves alternate strata of more and less resistant rock
Resistant rock like chalk forms steep escarpments
Behind the escarpment, there is a dip slope
Softer clays form vales
Bradshaw model
Discharge, width,depth, velocity and load increases downstream
Particle size, bed roughness and gradient decreases downstream
Transportation
Traction- large boulders are rolled
Saltation- smaller pebbles are bounced
Suspensions- smaller particles are suspended in the water
Solution- dissolved sediment carries in water
Waterfalls
Water goes over hard and soft rock
Soft rock is vertically eroded
Hydraulic action causes a plunge pool to form
Constant erosion of soft rocks means there’s no support for the overhang so it collapses into the plunge pool
Retreats backwards
Meanders formation
Meander is a slight bend on the river
Water travels faster on the outside of the bend, causing erosion through abrasion
On the inner bend, the river is through helicoidal flow, it takes the sediment from the outer bend and deposits it on the inner bend