G Rocks, Resources And Scenery Flashcards
Describe features of rock type and landscape. Malham Cove (4)
Landscape dominated by steep almost vertical cliff type feature
Rock overhangs in places ledges visible and bedding planes especially near top
Cliff height lower in middle
Variation in colour area left lighter
Joints/vertical cracks in rock
Carbonation (3)
Rain water weak carbonic acid
As rain mixes with CO2, as it falls through atmosphere
Limestone is soluble in weak acid so dissolved by it over long period of time
Occurs especially at joints
Suggest environmental disadvantages of quarry (4)
Half square km
Large hole in ground - bare rock visible in area around
Minor roads take rock away have to go through Westbury lorries noisy
Dust
Blasting of rock noise
How quarry managed during extraction and restored following the extraction of resources (9)
Describe how impact on environment can be reduced (8)
At Lafarge Cement in Hope in Derbyshire,
over 75000 trees have been planted to make the quarry and cement works less obvious and make it blend in with the environment
2.5m tonnes of limestone that could not be used for making cement have been used to help conceal the entrance by altering the landscape
Much is transported by train, so traffic on narrow roads in the countryside is reduced
Road cleaning is arranged to get rid of dust in immediate area
After an area is finished it is restored to farming or a different use, such as fishing lakes and a 9- hole golf course has been opened wetland reserve
£15m spent improve transport rail used rather than road to reduce impact of heavy traffic 1 train = 57 lorries
Produce 1m tonnes CO2/year 2003 7000 trees planted
Describe formation of igneous rocks (2)
Characteristics of igneous (2)
Formed by cooling of molten magma Either underground (intrusive - granite) or on ground (extrusive - basalt) Contain many interlocking crystals (crystalline) as a result are tough and resistant to erosion
Era vs period (2)
Era represents longer time than period
Data
Explain formation of an escarpment and vale (8)
Harder chalk laid down on top of softer clay
Due to tectonic movement, chalk and clay layers are tilted at an angle to the surface, uplifted
Clays eroded more quickly create vale
Resistant chalk eroded slowly leaving escarpment
Steep scarp slope right angles to dip of rocks while gentler dip slope goes parallel with it
Springs occur at junction of clay and chalk
Favour of quarry local cafe owner
Against holiday home owner (6)
F More customers more profit more workers from quarry Use profit employ more staff increase quality of food Support family A Ruin landscape less want to come Digging noise want peace on hol Dust and pollution ruin fresh air
Contrast position of granite and chalk on geological time scale (3) Limestone
Granite older rock Chalk formed during Cretaceous period 65-145 mya Granite Permian period 280mya Granite at least twice as old as chalk Limestone 340mya Carboniferous period
Characteristics of carboniferous limestone (2)
Made of CaCO3
permeable rock
Tough and resistant but chemically weak
Formed in layers
Underground features of carboniferous limestone (3)
Stalagmites thicker and shorter formed in cavern floor
Stalactites icicle like calcite feature hanging down from ceiling
Pillars formed when mites and tites join
Curtains water emerges along crack in cavern
Explain formation of mites and tites (4)
Tite
When eater rich in dissolved caco3 drips from cavern roof leaves minute deposit of calcite as evaporates
100 years icicle like tite form hanging down from ceiling
Mite
Water drops to cavern floor icicle grow from floor same way
Describe impact of quarrying on this area (4)
Ruin landscape attractive with waterfalls
Employment
Lorries spoil peace lead to traffic add to pollution ruin fresh air
Describe links between diff rock types in rock cycle (4)
All rocks on the surface are weathered which weakens the rock and makes it easy for sediment to be eroded.
This is transported by rivers and deposited in oceans where subsequent deposition above leads to the lower layers being compressed to form sedimentary rock.
Thus some of the sediments may have come from igneous rock that was initially formed by the cooling of magma following a volcanic eruption.
Igneous or sedimentary rock altered by being subjected to pressure during earth movements or heating during volcanic eruptions and it will change as a result to metamorphic rock – limestone to marble/clay to slate
Explain formation of limestone pavement (6)
Limestone is calcium carbonate.
Rainwater mixes with carbon dioxide in the atmosphere as it falls and becomes weak carbonic acid.
Calcium carbonate is soluble in this – the process of carbonation takes place.
As limestone has joints and is permeable, the water enters via these joints and the joints get bigger as limestone solution takes place and the dissolved limestone is removed.
This results in the enlarged gaps/grykes between the limestone blocks/clints.
The surface of the clints is smooth due to the action of the water, but is often uneven and pitted due to the impact of solution where the water sits in hollows.
Clints vary in size due to joint patterns