Restless Earth Flashcards

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1
Q

Oceanic and continental plates differences

A

Oceanic: dense because it’s made of a rock called basalt which is darker and more dense than continental crust. Newer- less than 200 million years old. Thinner 50-100km
Continental : less dense and cannot sink, cannot be renewed or destroyed. Older- most over 1500 million years old. Thicker 200km

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2
Q

Earth is divided into..

A

7 major and 8 minor tectonic plates

Largest plates: Antarctic, Eurasian, North American plates

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3
Q

Constructive boundary

A

Where plates pull apart

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4
Q

Destructive boundary

A

Continental plate and an oceanic plate move together resulting in one plate skinning beneath the other. Plate being forced down causes severe earthquakes

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5
Q

Conservative boundary

A

Where plates slides past each other. Plates can get stuck which causes earthquakes

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6
Q

What are Fold mountains

A

Large mountain rangers where rock layers have been crumpled as they have forced together
Form at collision and at destructive margins

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7
Q

Fold mountains formation

A
  1. Rivers deposited huge quantities of sediments in depressions called GEOSYNCLINES
  2. Over million of years the sediments were compressed into sedimentary rocks such as sandstone and limestone.
  3. The plates moved together forcing the sedimentary rocks upwards into a series of folds
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8
Q

Fold mountains location and example

A

Usually form along coastlines of a country or the edge of a country within continents. Found in linear patterns along plate boundaries.
West of south (Andes) and North America (Rockies)

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9
Q

What r ocean trenches

A

Deep sections of the ocean, usually where an oceanic plate is sinking below a continental plate. Oceanic crust is forced to dip downwards at an ANgle at the subduction zone. DESTRCUTIVE MARGIN

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10
Q

Location and example of oceanic trenches

A

They are found on the borders of the Pacific Ocean , the ring of fire.
Mariana Trench

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11
Q

THE ANDES CASE STUDY

Farming and hydro

A

Farming : in Bolivia, subsistence farmers grow a variety of crops including potatoes on the steep slopes. Most crops are grown on the low valleys- soy beans rice and cotton. LLAMAS have been used for transport for hundreds of years as Machu Picchu is located in a remote area. They carry over 25% of their body Wright. Still used for meat, milk and wool. ADAPTATION to condition: they build terraces which are steps cut into hillsides to create areas of flat land- retain water and stop soil from moving downslope. Usually 2-6m wide.
Hydroelectric power: form mountains have steep slopes and narrow valleys which is an advantage for hydro power. Narrow valleys are more easily dammed than wider valleys. - the relief encourages rapid flow of water that is needed for generation of electricity. Glacial melt water is also ideal. THE EL PLATINAL PROJECT began in 2009, 2nd largest in Peru, dams the CAÑETE river.60% of SWITZERLANDS ENERGY comes fm hydroelectric power production.

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12
Q

What r ocean trenches

A

Deep sections of the ocean, usually where an oceanic plate is sinking below a continental plate. Oceanic crust is forced to dip downwards at an ANgle at the subduction zone. DESTRCUTIVE MARGIN

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13
Q

Location and example of oceanic trenches

A

They are found on the borders of the Pacific Ocean , the ring of fire.
Mariana Trench

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14
Q

THE ANDES CASE STUDY

Farming and hydro

A

Farming : in Bolivia, subsistence farmers grow a variety of crops including potatoes on the steep slopes. Most crops are grown on the low valleys- soy beans rice and cotton. LLAMAS have been used for transport for hundreds of years as Machu Picchu is located in a remote area. They carry over 25% of their body Wright. Still used for meat, milk and wool. ADAPTATION to condition: they build terraces which are steps cut into hillsides to create areas of flat land- retain water and stop soil from moving downslope. Usually 2-6m wide.
Hydroelectric power: form mountains have steep slopes and narrow valleys which is an advantage for hydro power. Narrow valleys are more easily dammed than wider valleys. - the relief encourages rapid flow of water that is needed for generation of electricity. Glacial melt water is also ideal. THE EL PLATINAL PROJECT began in 2009, 2nd largest in Peru, dams the CAÑETE river.60% of SWITZERLANDS ENERGY comes fm hydroelectric power production.

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15
Q

ANDES CASE STUDY

mining

A

Gold mining: Yanacocha,Peru. Disadvantage: rocks are sprayed with cyanide and therefore contaminates local water supplies. Campaigns to stop expansion of the mine to a nearby mountain cuz it is a site of spiritual importance to locals.
Copper mining: Chiquicamata, Chile. Mine is a large open pit of copper ore. Useful because it can be used to for electrical wiring cuz copper is a good conductor & resistant to corrosion.
Developments to open another copper mine in 2017 at cost of $42 billion- estimated to produce 140,000 tonnes of ore per day.

Mining Disadvantage : increasing amount of mines being opened - 40% of Columbias land are mines- means that it is disrupting Eco systems that people reply on. Land is being taken away from locals for mining so there’s a lack of harvest and plants grown for medicinal purposes.
Advantage: people are attracted to area cuz more jobs created. IN CAJAMARCA- inhabitants grew by 30,000 as 240,000 jobs were introduced in mining

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16
Q

Volcanoes what is it

A

A volcano is where magma erupts through the ground, usually happening at or near plate edges.
Found at constructive or destructive plate boundaries

17
Q

Composite volcano

A

Steep sided with distinctive cone shape, high with narrow base
Secondary cones called parasitic cones formed when main vent is blocked
Explosive eruptions of lava and ash
e.g. SOUFRIÈRE HILLS

18
Q

Shield volcano

A

Gentle slopes and wide base.
Usually non violent eruptions, frequent Eruptions of basic lava.
Lava flows at high speeds and for long distances before Cooling
E.g. MAUNA LOA

19
Q

Volcano case study SOUFRIÈRE HILLS

Primary and secondary effects

A

Location: south of Montserrat. In Carribeans.
Cause : Montserrat is situated on destructive plate boundary. Atlantic plate forced under Carribean plate.
Primary effect: 23 people died in 1997, 2/3 of island as blankets in thick layer of ash, forest fires caused by pyroclastic flows
Secondary: ovr half of population left island and has not returned. Tourist industry is still suffering with few visitors. Southern area destroyed so people have to endure harsh living conditions in the north.

20
Q

SOUFRIÈRE hills

Positive and negative impacts

A

Pos: lava and ash deposited during eruption breaks down to provide valuable nutrients for the soil- creates fertile soil. Volcano attracted more tourists to come.
Neg: many people died and many settlements and woodlands destroyed. Collapse of industry. Unemployment level rose from 7% to 50%

21
Q

SOUFRIÈRE hills

Immediate and long term response

A

Immediate: Evacuation- People left the island completely- by November 1997, population had fallen from 12000 to 3500. Shelters built for evacuees. Charities set up temporary schools and sent emergency food.
Long term: British government gave £41 million for compensation and redevelopment. Islanders were offered £2500 each to relocate and permanently live in UK. Montserrat volcano observatory build to monitor volcano. Exclusion zone was Set.
Monitoring : volcanic Gas emissions measured by multi-component gas analyser system, which detects pre eruption degassing of rising magmas.

22
Q

Super volcanoes

A

Much bigger scale than volcanoes, emit at least 1000km3 of material. They don’t look like normal volcanoes, they are large depressions called calderas. Don’t erupt often- only about 18 in 2 million years.

23
Q

Effects of super volcano eruption

A

Full scale eruption would kill everything within an 100 mile radius, there would be ash 10 feet deep within an 1000 mile radius, which would cause earths temperature to drop because th ash would block the sun. Difficult to grow crops and people would die from starvation and toxic gas produced.

24
Q

Monitoring volcanoes

A

SATELLITES- infra red detectors on satellites can pick up heat signals whcih indicate how close magma is to surface of ground.
GOLBAL POSITIONING SYSTEM- measures ground deformation caused by pressure of rising magma.
REMOTE SENSING- used to monitor gases. Chemical composition and amours of gas released by volcano may alter.

25
Q

Earthquake what are they

A

Vibrations of the earths crust caused by movement at plate boundaries and major fault lines. They cause sudden and bread period of intense ground shaking.

26
Q

Earthquakes at margins

A

Destructive - pressure from sinking of sub ducting plate can trigger strong earthquakes as this pressure is periodically released.
Constructive - friction and pressure caused by plates moving apart is less tense than the other margins.
Conservative- plates slide past each other and tend to stick which caused stress and pressure to build. Release results in powerful earthquakes.

27
Q

Earthquake measurement scales

A

RICHTER SCALE - used to measure magnitude of a tremor. It is a logarithmic scale. Uses seismograph.
Advantage: not subjective. Can compare numbers.
Dis: doesn’t show what damage is caused.
MERCALLI SCALE- measures the EFFECTS of earthquakes using subjective scale.
Advantage: tell us us impacts and damage.
Dis: subjective

28
Q

3 P’s

A

Prediction : attempts to fore cast an event. Foreshocks give short notice a few minutes before earthquake. Animal behaviour.
Protection : constructing buildings that are safe to live in and will not collapse. Earthquake proof building: transamerica pyramid in San Fran.
Steel frames, weights on top of building to reduce movements, shatter proof glass, rubber shock absorbers to absorb earth tremors, strong foundations.
Preparation : organising activities and drills so people know what to do in event of earthquake e,g drop cover hold. National earthquake drill in Japan 1st September

29
Q

Earthquake Christchurch case study

Impacts

A

Cause : Pacific plate forced under Australian plate.
Magnitude 6.3. 185 deaths.
Social impacts : 165,000 houses damaged. 4 months after earthquake, 50,000 residents had already moved out of Christchurch. In September 2012 , 13 schools closed down and 18 merged. Tourist numbers declined.
Economic impacts: decline in employment, loss of hotels and visitor accommodations, estimated cost $30 billion
Environmental : liquefaction caused power cuts. Earth rose by 1m and Christchurch moved closer to Sydney. Rock falls.

30
Q

Christchurch

Immediate and long term responses

A

Immediate: St. John’s ambulance had 16 ambulance operational within half an hour of event, Urban Search and rescue was there within couple of hrs. 300 Australian police flew in. Chemical toilets provided for 300,000 people.
Long term: government intends to spend $1 billion in the next 10 years renewing education system in affected areas. International aid was provided $6~7 million. Red Cross grants families with children under 5 years who were living in damaged house electricity bills

31
Q

Haiti earthquake

Secondary effects

A

Cause of earthquake : North American and Carribean plates collided. Focus point was 13km below surface so tremors were very strong.
Magnitude 7.0
Secondary effects : electricity supplies disrupted. Roads blocked and airport unusable. No signal or Internet. Hospitals and key buildings destroyed. Main prison wrecked and 4000 inmates escaped.

32
Q

Haiti

Impacts

A

Social: 1.5m made homeless. 3 million affected. Over 220,000 deaths. 300,000 injured. 180,000 homes destroyed.
Economic : 30,000 commercial buildings collapsed. Estimated 1 in 5 jobs lost. Clothing industry which accounts for 2/3 of haitis exports reported structural damage
Environmental: sea levels in local area changed with some parts of land Sinking below sea. Roads were littered with cracks and fault lines

33
Q

Haiti

Responses

A

Immediate : search and rescue, aid like food and water and medical supplies was brought from USA and Dominican Republic. £100 million was used to support over 1.2 million people from UKS disaster emergency committee
Long term,: several thousands decided to move away from port au prince. World bank pledged $US 100m to support reconstruction and recovery programmes