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GCSE Tectonics Ans1 - practise with past papers and mark schemes

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<strong>GCSE</strong> TECTONIC ACTIVITY, LANDSCAPE & ROCKS<br />

ANSWERS TO QUESTION 1<br />

(a)<br />

(b)(i)<br />

(ii)<br />

(iii)<br />

1: Rocks<br />

2: Hot mud<br />

3: Ash<br />

The Singapore Airlines flight was forced to l<strong>and</strong> because:<br />

* poor visibility caused by ash/smoke plume<br />

* updraughts of hot air cause turbulence<br />

* airborne ash clogs jet engines<br />

* volcanic eruptions often cause torrential rain/thunder <strong>and</strong> lightning<br />

Any two.<br />

Dormant = volcano has not erupted in the <strong>past</strong> 2,000 years, e.g. Santorini, Greece, last erupted<br />

1500 BC.<br />

Active = volcano has erupted recently <strong>and</strong> is likely to do so again, e.g. Mount Etna, Sicily, Italy<br />

Natural = because it is not caused by people/cannot controlled by people<br />

Hazard = because it is dangerous to humans/destructive to property/cannot be (easily/accurately) predicted.<br />

3x1<br />

2x1<br />

2x1<br />

2x1<br />

(c)<br />

Lava Flow<br />

Crater<br />

Parasitic Cone<br />

Vent<br />

(d)<br />

(e) (i)<br />

(ii)<br />

One <strong>mark</strong> for the shape of the cone, i.e. symmetrical, <strong>and</strong> five for labels.<br />

Volcanoes form along a constructive plat boundary because:<br />

* plates are diverging (moving apart)<br />

* convection currents cause<br />

* (molten) magma to rise from mantle<br />

* through plate boundary/fault<br />

* to erupt as lava on the surface<br />

* lava solidifies to form (a layer of) volcano<br />

* continued upwelling of magma adds layers of lava to volcano - so it grows<br />

Any five.<br />

A: Crustal melting<br />

B: Oceanic plate<br />

C: Continental plate<br />

D: Centre for earthquakes<br />

Accept reverse of boxes A <strong>and</strong> D.<br />

Magma<br />

Chamber<br />

Converging/destructive plate boundaries are associated <strong>with</strong>:<br />

* volcanoes forming/erupting in fold mountains<br />

* earthquakes which cause tsunamis (not tidal) waves<br />

* earthquakes which cause l<strong>and</strong>slides/avalanches (snow)<br />

* volcanoes release poisonous/toxic gases, e.g. sulphur dioxide, nitrous oxide, carbon monoxide etc.<br />

Any three explained.<br />

6x1<br />

5x1<br />

4x1<br />

3x2<br />

Total 30


<strong>GCSE</strong> TECTONIC ACTIVITY, LANDSCAPE & ROCKS<br />

ANSWERS TO QUESTION 2<br />

(a) (i)<br />

(ii)<br />

(iii)<br />

(iv)<br />

(b)(i)<br />

(ii)<br />

Examples of volcanoes on different continents include:<br />

*Mount Etna, Europe<br />

*Mount St. Helens, North America<br />

*Mount Kilimanjaro, Africa<br />

*Chimborazo, South America<br />

*Mount Fujiyama, Asia<br />

The distribution of volcanoes in the world is:<br />

*widely distributed<br />

*but not everywhere<br />

*in long narrow belts (called active zones)<br />

*mostly on edges of continents<br />

*also in oceans<br />

*not in shield areas<br />

Any four. Accept maximum of two for a list of named areas only, e.g. west coast South America,<br />

Mediterranean Sea.<br />

The only volcanoes found in North America are in a 300 kilometre wide chain running down the<br />

west coast of that continent because:<br />

*there is a plate boundary between the North American Plate <strong>and</strong> Pacific Plate<br />

*it is an active zone - where volcanoes form<br />

*the rest of North America is a stable continental shield area<br />

There is an apparent association between volcanoes, earthquake belts <strong>and</strong> fold mountains because:<br />

*they all occur along plate boundaries because -<br />

*plate movement is involved in all their formation<br />

*volcanoes form where converging plates cause subduction <strong>and</strong> melting of crust<br />

*or where diverging plates allow magma to rise through faults/plate boundaries<br />

*earthquakes occur when plates ‘lock’, tension builds <strong>and</strong> is then released as plates ‘jump’<br />

*fold mountains are formed as destructive margins or collision margins squeeze ocean sediment upwards<br />

Any five.<br />

Reasons why people live close to volcanoes include:<br />

*volcanoes were dormant when settlement occurred<br />

*volcanic rocks <strong>and</strong> ash weathers to form fertile soil<br />

*volcanoes provide employment through tourism<br />

*volcanoes provide geothermal heat <strong>and</strong> power<br />

*volcanic liquids <strong>and</strong> gases solidify to form industrial minerals, precious metals <strong>and</strong> gemstones<br />

*volcanoes form isl<strong>and</strong>s amidst vast oceans = l<strong>and</strong>falls<br />

*scientists/vulcanologists/seismologists live close to/study volcanoes<br />

*tourist attractions so people earn a living from tourist facilities<br />

Any four.<br />

Case study example: Mount Fujiyama, Honshu Isl<strong>and</strong>, Japan<br />

Benefits brought to people by Mount Fujiyama’s volcanic activity include:<br />

*tourist attraction <strong>and</strong> winter snow skiing<br />

*people bathe in hot ashes to ease rheumatism<br />

*drink mineralised water for health reasons<br />

*fertile slopes are farmed = rice terraces<br />

*runs a geothermal power station<br />

*tin, silver, gold <strong>and</strong> rubies mined<br />

Any three or four. F = one <strong>mark</strong> for named example + 3 = 4, H = one <strong>mark</strong> for named example + 4 = 5<br />

4x1<br />

4x1<br />

3x1<br />

5x1<br />

4x1<br />

5x1


(b)(iii) Problems suffered by people living in a volcanic area:<br />

*lava flow destroys buildings/engulfs property/farmlamd<br />

*volcanoes trigger l<strong>and</strong>slides/avalanches of snow<br />

*volcanoes release poisonous/toxic gases, e.g. sulphur dioxide, nitrous oxide <strong>and</strong> carbon<br />

monoxide<br />

Any two.<br />

2x1<br />

(c)<br />

Ways in which people can be protected from the damaging effects of volcanic activity include:<br />

*volcano watchers/scientists employed in many Asian countries to warn of/predict eruptions, e.g.<br />

Tambora, Indonesia<br />

*digging channels/culverts to lead lava flows away from towns, e.g. Mt. Etna, Sicily, Italy<br />

*hose/douse hot lava flows <strong>with</strong> sea water to cool - solidify - stop/halt, e.g. Haiemey, Icel<strong>and</strong><br />

*Italian Air Force bombed lava flows to redirect lava flow away from towns, e.g. Mt. Etna,<br />

Sicily, Italy<br />

*pre-arranged/organised/<strong>practise</strong>d evacuation procedures, e.g. Montserrat, Caribbean Sea<br />

*build dams/walls near settlements to redirect mud flows (lahars), e.g. Nevado del Ruiz,<br />

Columbia<br />

F = Any 3 x 2, H = any 4 x 2.<br />

8x1<br />

Total 35


<strong>GCSE</strong> TECTONIC ACTIVITY, LANDSCAPE & ROCKS<br />

ANSWERS TO QUESTION 3<br />

(a) (i)<br />

(ii)<br />

(iii)<br />

(iv)<br />

(v)<br />

(b)(i)<br />

(ii)<br />

(iii)<br />

(c) (i)<br />

(ii)<br />

Osaka or Kyoto (not Tarumi, Wakayama or Nara)<br />

40km<br />

The destructive effects of an earthquake are normally greatest near(est) to epicentre/in dense urban areas.<br />

Earthquake zones are hazardous places to live because:<br />

* buildings collapse/become unstable<br />

* bridges, tunnels <strong>and</strong> viaducts can collapse<br />

* gas/oil pipes fracture = explosions/fire<br />

* people can be hit by falling objects/debris<br />

* submarine earthquakes cause tsunamis (not tidal waves)<br />

Any two.<br />

Groups of people who might have been reluctant to leave Kobe despite earthquake warnings include:<br />

* Armed forces/emergency services (police, ambulance, doctors etc): sense of duty/orders from superiors<br />

* Shopkeepers/house owners: wish to protect business/property from damage/looting<br />

* Elderly/infirm: mobility difficulties<br />

* Sceptics: they have experienced minor/less intense earthquakes before<br />

Any 2 x 2<br />

A tectonic plate is a large piece of the Earth’s crust, which ‘floats’ on the mantle beneath.<br />

Pacific Plate moves west/left but the Eurasian Plate moves east/right.<br />

Pacific sinks/subducted but Eurasian Plate is buoyant/floats.<br />

Award <strong>mark</strong> only if comparison made, i.e. mentions both plates per statement.<br />

* Eurasian continental plate <strong>and</strong> oceanic Pacific Plate converge<br />

* heavier Pacific (oceanic) Plate subducted <strong>and</strong> ‘locks’ <strong>with</strong> continental plate<br />

* tension builds as crustal movement prevented<br />

* eventually extreme tension causes plates to ‘jump’ - the ‘flicking back’ of the lighter continental plate<br />

* point of earthquake inside crust is called focus<br />

* seismic waves/tremors spread out from epicentre (point on surface above focus)<br />

* earthquake was so devastating because (i) focus was ‘shallow’ <strong>and</strong> (ii) epicentre was close to Kobe<br />

H = any 5, F = any 4.<br />

An earthquake may cause more damage in an urban area than in a rural area because:<br />

* urban areas are more enclosed by tall/composite structures (more liable to collapse) than countryside<br />

* densely built city centres/CBDs have little/no open space to escape to<br />

* ‘domino’ effect = one tall/multi-storey building may fall on to another, which falls on to another<br />

<strong>and</strong> so on - effect of earthquake spreads<br />

* falling debris/masonry is more of a danger in urban areas<br />

* urban areas have gas/oil pipes which may fracture/leak <strong>and</strong> explode/start fires<br />

* urban areas have more overhead electricity cables = can electrocute if brought down.<br />

H =any 3, F = any 2<br />

An earthquake may cause more damage in an LEDC than in an MEDC because:<br />

* denser buildings less well constructed/made from flimsier materials = collapse/fires spread more<br />

easily, e.g. in shanty towns<br />

* badly built/inadequate access roads (e.g. in shanty towns) cause difficulties for emergency services<br />

* settlements in LEDCs built on steep/unsuitable slopes<br />

* LEDCs do not have sophisticated seismic equipment/satellites to detect/predict earthquakes<br />

* earthquake-prone MEDCs build earthquake-proof buildings <strong>and</strong> roads<br />

* MEDCs have disaster plans/<strong>practise</strong> evacuation procedures <strong>and</strong> stockpile emergency provisions<br />

1<br />

1<br />

1<br />

2x1<br />

2x2<br />

2x1<br />

2x1<br />

5x1<br />

3x1<br />

Place<br />

Los Angeles<br />

India<br />

Year<br />

1994<br />

1993<br />

Time<br />

05.00hrs<br />

05.00hrs<br />

Richter Scale<br />

6.6<br />

6.4<br />

Deaths<br />

57<br />

22,000<br />

4x1<br />

Total 25


<strong>GCSE</strong> TECTONIC ACTIVITY, LANDSCAPE & ROCKS<br />

ANSWERS TO QUESTION 4<br />

(a) (i)<br />

(ii)<br />

(b)(i)<br />

(ii)<br />

(iii)<br />

(iv)<br />

(v)<br />

Igneous<br />

Sedimentary rocks are changed into metamorphic rocks by:<br />

* igneous activity, e.g. sedimentary rocks melt as magma rises through them<br />

* then cool - solidify - reform as different rocks, e.g. limestone/chalk - marble<br />

* (tectonic) plate collision causes folding/faulting of sedimentary rocks<br />

* intense pressure restructures minerals so rocks alter/reform<br />

* e.g. shale - slate - schist - gneiss (increasing pressure)<br />

Sedimentary<br />

The map shows that s<strong>and</strong>stone is the least resistant rock to erosion because:<br />

* mean height above sea level is only 30 metres<br />

* compared to 70 - 80 - 115 - 360 - 380 - 460 metres above sea level<br />

* must have been eroded/denuded/lowered the most<br />

* so less resistant than limestones, coal measures <strong>and</strong> millstone grit/others<br />

Any two.<br />

The term permeable means that it allows water to pass through (reject any reference to porous/porosity)<br />

Carboniferous limestone is permeable because it has bedding planes, fractures (faults) <strong>and</strong> joints<br />

(vertical <strong>and</strong> horizontal).<br />

Reservoirs are only found in the millstone grit area because:<br />

* millstone grit is impermeable = it does not let water pass through<br />

* all other rocks on the map are permeable or porous<br />

1<br />

6x1<br />

1<br />

2x1<br />

1<br />

2x1<br />

2x1<br />

(vi)<br />

new red s<strong>and</strong>stone<br />

Rock Type<br />

building material<br />

Economic Use<br />

coal<br />

fuel<br />

limestones (carboniferous or magnesium)<br />

cement, roadstone, flux, agricultural lime<br />

Any three.<br />

millstone grit<br />

metal sharpener, wheat milling,<br />

ornamental cladding<br />

3x1<br />

(c) (i)<br />

Economic uses for igneous rocks include:<br />

* building stone (Aberdeen known as ‘the granite city’)<br />

* decorative cladding (for outside of buildings, e.g. banks, fireplaces)<br />

* chemically weathers to china clay/kaolin - pottery <strong>and</strong> paper glaze<br />

* bedding for railway tracks<br />

* sea defences, harbour walls etc<br />

* sites for reservoirs<br />

* grouse moors<br />

* tourism - Dartmoor National Park<br />

Properties:<br />

* impermeable<br />

* very resistant/hard<br />

* chemically stable<br />

* colourful/pretty minerals<br />

H = Any 3 uses <strong>and</strong> any 3 properties = 6, F = 3 + 2 = 5<br />

6x1


(c) (ii)<br />

There is little agriculture in areas of igneous <strong>and</strong> metamorphic rock because:<br />

* igneous/metamorphic rocks are very resistant so weathers very slowly so produce very thin soils<br />

* minerals in igneous/metamorphic rocks, e.g. quartz, weather to form acidic soils/low pH<br />

* often weather to form s<strong>and</strong>y/porous/dry/’hungry’ soils<br />

* because they are very resistant they form upl<strong>and</strong>s = steep slopes, cold, wet, marshy<br />

* so agriculture is very limited, e.g. sheep/<strong>past</strong>ure/hill farming<br />

There is quarrying in areas of igneous <strong>and</strong> metamorphic rock because:<br />

* igneous/metamorphic rocks have many commercial uses - for igneous uses see answer to (c)(iv)<br />

* metamorphic uses = slate - roofing material<br />

* schist/gneiss = sea defences, ballast<br />

Maximum <strong>mark</strong>s only if a balanced answer, i.e. c<strong>and</strong>idate addresses all three parts of answer = why<br />

so little agriculture, what agriculture, why quarrying, max F3/H5 if not. F = 4, H = 6.<br />

6x1<br />

Total 30


<strong>GCSE</strong> TECTONIC ACTIVITY, LANDSCAPE & ROCKS<br />

ANSWERS TO QUESTION 5<br />

(a) (i)<br />

(ii)<br />

(b)(i)<br />

(ii)<br />

(iii)<br />

(c)<br />

(d)<br />

1. Limestone<br />

2. Swallow hole<br />

3. Resurgent stream (spring)<br />

4. Scar<br />

5. Gorge<br />

There is little surface water in limestone areas because:<br />

* limestone contains bedding planes, fractures (faults) <strong>and</strong> joints (vertical <strong>and</strong> horizontal)<br />

* so it is pervious<br />

* i.e. allows water to pass through it<br />

Reject any reference to porosity/limestone being porous.<br />

Underground features commonly found in limestone areas include:<br />

* cavern<br />

* stalactite<br />

* stalagmite<br />

* limestone pillar<br />

* swallow hole or sink<br />

* underground/subterranean stream<br />

Any two.<br />

Limestone solution is:<br />

* the name of the weathering process of limestone/karst scenery/l<strong>and</strong>scapes<br />

* dissolved calcium bicarbonate in (rain) water<br />

Underground features are the result of limestone solution <strong>and</strong> chemical weathering because:<br />

* process of chemical weathering which attacks/dissolves limestone - is called carbonation/solution<br />

* rain water absorbs carbon dioxide as it passes through atmosphere/soaks into soil<br />

* to become a weak/dilute carbonic acid (carbon dioxide now in solution)<br />

* carbonic acid reacts <strong>with</strong>/dissolves calcium carbonate - the main mineral in Carboniferous Limestone<br />

* to make calcium bicarbonate, which is transported in solution<br />

* so the bedding planes, faults (fractures) <strong>and</strong> joints in the limestone are widened<br />

* rock is dissolved at a rate of approx 4 centimetres per year<br />

H = any 6, F = any four<br />

Reasons for the course of of the stream shown in the field sketch include:<br />

* source is/flows over impermeable rock<br />

* then disappears down swallow hole in permeable limestone<br />

* flows as a subterranean/underground stream through caverns<br />

* reaches impermeable bedrock/strata below permeable limestone<br />

* so emerges as a resurgent stream/Vauclusian spring<br />

Any four.<br />

Economic activities which make use of limestone areas include:<br />

* tourism - caving, hiking etc.<br />

* quarrying - roadstone. agricultural lime<br />

* hill farming<br />

* bottling spring/mineral water<br />

Any two.<br />

5x1<br />

3x1<br />

2x1<br />

2x1<br />

6x1<br />

4x1<br />

2x1<br />

(e)<br />

Limestone l<strong>and</strong>scapes produced by weathering processes attract many visitors because:<br />

* limestone/karst scenery is spectacular - limestone pavements, scars, caverns <strong>and</strong> gorges attract sightseers<br />

* limestone scenery form national parks, e.g. Yorkshire Dales <strong>and</strong> Peak District are popular day trip venues<br />

* limestone (pavements) habitats are rare so home to rare wildflowers <strong>and</strong> birds - which attract<br />

botanists <strong>and</strong> ornothologists<br />

* limestone l<strong>and</strong>scapes provide a wide variety of recreational activities, e.g. caving, canyoning, 6x1<br />

rock climbing, hang-gliding etc.<br />

H any 3 x 2, F = any 2 x 2.<br />

Total 30


<strong>GCSE</strong> TECTONIC ACTIVITY, LANDSCAPE & ROCKS<br />

ANSWERS TO QUESTION 6<br />

(a) (i)<br />

(ii)<br />

(iii)<br />

(iv)<br />

(b)(i)<br />

(ii)<br />

(c) (i)<br />

(ii)<br />

(iii)<br />

(d)(i)<br />

(ii)<br />

A: Scarp<br />

B: Dip<br />

Escarpment or cuesta<br />

Water table<br />

Clay or alluvium<br />

1. A spring may occur:<br />

* at the junction of the porous chalk <strong>and</strong> impermeable clay<br />

* or where the water table outcrops/reaches the surface<br />

2. How this may affect settlements:<br />

* spring-line settlements/villages occur along the foot of the scarp<br />

* for water supply, i.e. wet-point sites (chalk is dry, clay flood-liable)<br />

3. The best site for the village:<br />

* along the spring-line/scarp foot (= water supply <strong>and</strong> shelter)<br />

A spring appears because:<br />

* porous (water-bearing) chalk lies over<br />

* non-porous/impermeable clay<br />

* (rain) water percolates down through chalk<br />

* but cannot pass through clay so emerges as a spring<br />

Any three.<br />

A dry valley is a river (eroded/formed) valley <strong>with</strong>out (or which rarely has) a river/stream flowing<br />

through it.<br />

Dry valleys occur because:<br />

* formed during ice ages when chalk was permanently frozen<br />

* so behaved like an impermeable rock<br />

* rivers flowed during (brief) arctic summer <strong>and</strong> eroded/formed valleys<br />

* river soaked away/absorbed when ice age ended<br />

Alternative theory = prolonged saturation of chalk during a wetter climate<br />

There is little surface water on chalk upl<strong>and</strong>s because:<br />

* chalk is porous (not permeable)<br />

* so water soaks into/absorbed into pore/air spaces in rock<br />

* so water is underground/contained in aquifers<br />

People who would favour the new chalk quarry include:<br />

* local builders<br />

* cement companies<br />

* local unemployed<br />

* farmer selling mineral/quarry rights<br />

Any one.<br />

People who would be against the development of the chalk quarry include:<br />

* nearby residents<br />

* nearby quarry owner<br />

* conservation groups, e.g. R.S.P.B,<br />

* Ramblers Association<br />

* local farmer<br />

Any one.<br />

2x1<br />

1<br />

1<br />

1<br />

1<br />

2x1<br />

1<br />

3x1<br />

1<br />

4x1<br />

3x1<br />

1<br />

1


(d)(ii)<br />

(iii)<br />

FOR the chalk quarry:<br />

* provide employment for locals<br />

* profits for l<strong>and</strong>owner/local builders<br />

* can afford to take some farml<strong>and</strong> out of production<br />

* l<strong>and</strong> will have other/more uses, e.g. l<strong>and</strong>fill <strong>with</strong> domestic refuse<br />

* l<strong>and</strong> can be reclaimed/restored afterwards<br />

Any four.<br />

AGAINST the chalk quarry:<br />

* unsightly/eyesore<br />

* extra lorry traffic = congestion, air pollution, vibration<br />

* noise <strong>and</strong> dust from quarry<br />

* loss of farml<strong>and</strong><br />

* habitat/l<strong>and</strong>scape destruction<br />

* local house prices fall<br />

Any four.<br />

4x1<br />

4x1<br />

Total 30

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