natural + tectonic hazards

0.0(0)
studied byStudied by 1 person
0.0(0)
full-widthCall Kai
learnLearn
examPractice Test
spaced repetitionSpaced Repetition
heart puzzleMatch
flashcardsFlashcards
GameKnowt Play
Card Sorting

1/23

encourage image

There's no tags or description

Looks like no tags are added yet.

Study Analytics
Name
Mastery
Learn
Test
Matching
Spaced

No study sessions yet.

24 Terms

1
New cards

What is a natural hazard?

A natural process which could cause death, injury, damage, or is a threat. It must affect humans to count as a hazard.

2
New cards

What are the types of natural hazard?

  • Geological hazards

    • Caused by land + tectonic processes

    • Examples: volcanoes, earthquakes, landslides

  • Meteorological hazards

    • Caused by weather + climate

    • Examples: tropical storms, climate change, extreme weather (e.g. heatwaves)

3
New cards

What is hazard risk?

The probability that a natural hazard will occur.

4
New cards

What affects hazard risk?

  • Vulnerability: the more people in areas exposed to natural hazards, the greater the probability they will be affected. Also, if a town is located at the base of a volcano or on a floodplain, for example.

  • Capacity to cope: HICs can cope better as they can afford to evacuate people, repair damage, etc

  • Nature of natural hazards: some hazards are less able to be predicted. Some hazards have a higher frequency. More severe hazards cause greater effects than less severe hazards.

5
New cards

What is the earth’s structure?

  • Crust: divided into tectonic plates, rocky outer layer with two types of crust, max temperature 400ºC

    • Continental crust is thicker (30-50km) and less dense

    • Oceanic crust is thinner (5-10km) and more dense

  • Mantle: semi-molten, 500-3000ºC

  • Outer core: liquid iron + nickel, 4000-6000ºC

  • Inner core: solid iron + nickel, 5500ºC

<ul><li><p>Crust: divided into tectonic plates, rocky outer layer with two types of crust, max temperature 400ºC</p><ul><li><p>Continental crust is thicker (30-50km) and less dense</p></li><li><p>Oceanic crust is thinner (5-10km) and more dense</p></li></ul></li><li><p>Mantle: semi-molten, 500-3000ºC</p></li><li><p>Outer core: liquid iron + nickel, 4000-6000ºC</p></li><li><p>Inner core: solid iron + nickel, 5500ºC</p></li></ul><p></p>
6
New cards

Why do plates move?

Convection currents. The outer core heats the lower part of the mantle, which rises to the surface. At the crust, it cools and is forced sideways then falls as it cannot penetrate the rock.

7
New cards

Explain a destructive palate boundary.

Two plates move towards eachother (e.g. along the west coast of South America).

Where an oceanic plate meets a continental plate, the denser oceanic plate is subducted into the mantle (slab pull theory) and destroyed.

Where two continental plates meet, the ground is folded upwards to create mountain ranges.

<p>Two plates move towards eachother (e.g. along the west coast of South America).</p><p>Where an oceanic plate meets a continental plate, the denser oceanic plate is subducted into the mantle (slab pull theory) and destroyed. </p><p>Where two continental plates meet, the ground is folded upwards to create mountain ranges.</p>
8
New cards

Explain a constructive plate boundary.

Two plates are move away from eachother (e.g. at the mid-Atlantic ridge).

Convection currents move the plates away from eachother. Magma rises from the mantle to fill the gap and cools, creating new crust.

<p>Two plates are move away from eachother (e.g. at the mid-Atlantic ridge).</p><p>Convection currents move the plates away from eachother. Magma rises from the mantle to fill the gap and cools, creating new crust.</p>
9
New cards

Explain a conservative plate boundary.

Two plates move sideways past eachother at different speeds / opposite directions (e.g. along the west coast of the USA).

<p>Two plates move sideways past eachother at different speeds / opposite directions (e.g. along the west coast of the USA).</p>
10
New cards

Where are volcanoes found?

  • Destructive margins: a pool of magma forms in the mantle due to the oceanic plate melting, which then rises through cracks in the crust (vents) and erupts as lava.

  • Constructive margins: magma rises up to fill the gap, forming a volcano

  • Hotspots (e.g. Hawaii): volcanoes form over parts of the mantle that are really hot

11
New cards

Where are earthquakes found?

  • Destructive margins: tension builds up when one plate gets stuck as it’s moving past the other into the mantle

  • Constructive margins: tension builds along cracks within the plates as they move away from each other

  • Conservative margins: tension builds up when plates lock together then suddenly release into an earthquake

12
New cards

What happens in a volcanic eruption?

Lava and gases are emitted. Some volcanoes emit ash, which can cover land, block out sun, and form pyroclastic flows.

13
New cards

What happens in an earthquake?

Seismic waves (vibrations) are sent out from the focus (the point in the Earth where rocks are moving) and spread out. The closer to the focus, the stronger the waves, the more damage. The epicentre is the point on the Earth’s surface right about the focus.

<p>Seismic waves (vibrations) are sent out from the focus (the point in the Earth where rocks are moving) and spread out. The closer to the focus, the stronger the waves, the more damage. The epicentre is the point on the Earth’s surface right about the focus.</p><p></p>
14
New cards

How are earthquakes measured?

Using the Richter scale. It measures how powerful an earthquake is (magnitude). It is logarithmic, meaning a magnitude 5 earthquake is ten times more powerful than a magnitude 4 earthquake.

15
New cards

What are the primary and secondary effects of a volcanic eruption?

PRIMARY

  • Buildings and roads destroyed by lava + pyroclastic flows

  • People and animals injured or killed by lava, pyroclastic flow, and falling rocks

  • Crops damaged

  • Water supplies contaminated by ash

SECONDARY

  • Flooding caused by hot rocks, ash and gas melting ice and snow on the volcano

  • Transport networks blocked or destroyed so help can’t get through

  • People left homeless + unemployed as businesses are destroyed

  • Ash makes soils more fertile

16
New cards

What are the immediate and long-term responses to a volcanic eruption?

IMMEDIATE

  • Evacuate people asap

  • Provide food, drink and shelter for evacuees

  • Treat injured people

  • Foreign governments may send aid workers, supplies or financial donations

LONG-TERM

  • Repair and rebuild or resettle people elsewhere

  • Repair and reconnect infrastructure (roads, rail, power lines, etc)

  • Improve monitoring and evacuation plans

  • Boost economy if possible - attract tourists to volcano

17
New cards

What are the primary and secondary effects of an earthquake?

PRIMARY

  • Buildings and bridges collapse

  • People are injured or killed by collapsed buildings / debris

  • Roads, railways, ports and airports are damaged

  • Electricity cables, communication networks, gas, etc are damaged

SECONDARY

  • Landslides / tsunamis triggered

  • Leaking gas ignites and starts fires

  • People left homeless + unemployed as businesses are destroyed

  • Shortage of clean water + sanitation, so disease spreads

  • Aid can’t get through due to blocked or damaged roads

18
New cards

What are the immediate and long-term responses to an earthquake?

IMMEDIATE

  • Rescue people trapped by collapsed buildings + treat injuries

  • Put out fires

  • Set up temporary shelters

  • Temporary supplies of water, food, electricity, gas, etc

  • Foreign governments may send aid workers, supplies or financial donations

LONG-TERM

  • Re-house people

  • Repair / rebuild damaged buildings, roads, railways and bridges

  • Reconnect broken electricity, water, gas and communications

  • Improve building regulations so less damage in future

19
New cards

HIC earthquake case study

  • Japan, March 11th 2011

  • 9.0 magnitude with epicentre 70km offshore

  • 1 minute warning given and lasted 6 minute

  • PRIMARY EFFECTS: 22000 dead, 130000 homeless, 330000 buildings destroyed, 170000 homes lost water supplies

  • SECONDARY EFFECTS: tsunami wave 38.9m high, $235 total cost, nuclear crisis as 9m wave flooded Fukushima power plant

  • IMMEDIATE RESPONSE: only 58% of people in coastal areas followed tsunami warnings and went to higher ground

  • LONG-TERM RESPONSE: new settlements built to accommodate 20000 left homeless, most of city being rebuilt, investigating why so many buildings collapsed

20
New cards

LIC earthquake case study

  • Haiti, January 12th 2010

  • 7.0 magnitude with epicentre 25km away from Port-au-Prince (capital city) where 3 million live

  • Earthquake lasted 30-40 seconds

  • PRIMARY EFFECTS: 220000-300000 deaths, 300000 injured, 1.5 million people homeless, 4000 schools damaged / destroyed

  • SECONDARY EFFECTS: 20% of jobs lost, overcrowded tent cities and poor sanitation led to disease, $13.9 billon to rebuild, landslides, crime increased

  • IMMEDIATE RESPONSE: USA sent rescue teams and 10000 troops, first aid for 11000 people, mass graves to bury the dead

  • LONG-TERM RESPONSE: improved water supply, $1.1 billion donated but only 2% of it released due to corruption, giving seeds to households to grow their own food, free medical care

21
New cards

Why do people continue to live in hazardous areas?

  • People don’t want to leave friends / family

  • They’re employed in the area

  • Soil around volcanoes is fertile due to minerals in volcanic ash

  • Volcanoes are tourist attractions so people work in that industry

  • People are confident of their government support

22
New cards

How can monitoring + prediction reduce the effects of tectonic hazards?

  • EARTHQUAKES: Seismometers and lasers monitor earth movements, increase in radon gas levels indicates an earthquake could be likely

  • VOLCANOES: change in shape of volcano may signify magma building up, tiny earthquakes could indicate an eruption, increase of volcanic gases (sulphur)

23
New cards

How can protection reduce the effects of tectonic hazards?

  • EARTHQUAKES: buildings built with flexible steel beams in an X shape, buildings built with shock absorbers, automatic shut-off switches turn off gas + electricity to prevent fires

  • VOLCANOES:

24
New cards

How can preparation / planning reduce the effects of tectonic hazards?

  • EARTHQUAKES: people know what to do if an earthquake happens, emergency services can train + prepared for disasters to reduce number killed, emergency supplies stockpiled

  • VOLCANOES: evacuation routes planned by governments, areas most vulnerable are identified