Hazardous Environments Flashcards

(32 cards)

1
Q

Definition of a hazard

A

A physical event that may potentially cause damage to people

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2
Q

Definition of risk

A

Exposure of people to a hazardous event

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3
Q

Disaster

A

The realisation of risk

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4
Q

Vulnerability

A

The susceptibility to loss

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5
Q

Describe and explain a divergent plate boundary and the hazards associated (draw diagram)

A

DIAGRAM draw correctly
- shallow, weak and narrow belt of earthquakes due to weak volcanic activity (basaltic lava, low silica content)
=> harmless at oceanic boundary
- little risk to humans

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6
Q

Describe and explain a conservative plate boundary and the hazard associated

A

DIAGRAM
- shallow and powerful earthquakes
- relatively narrow belt
=> hazardous to human life because human settlements may be in close proximity + they are powerful

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7
Q

Describe and explain a destructive convergent plate boundary and associated hazards

A

DIAGRAM
- deepest and most powerful earthquake
- broader belt of earthquakes
- highly explosive volcanoes(andesitic volcanic eruptions)
=> although there are mountains which may reduce population density, associated risk of landslides and there are likely to be human settlements on the coast

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8
Q

Describe and explain a collision plate boundary and associated hazards

A

DIAGRAM

- shallow, broad zones of seismic activity

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9
Q

Types of waves

A

Body waves: P-waves (fastest and longitudinal) & S-waves (slowest and transverse)
Surface waves: Love waves and Raleigh waves

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10
Q

Two seismic scales

A

Modified Mercalli scale: subjective & qualitative, measure of intensity
Moment Magnitude scale: calibrated measure of energy release, logarithmic scale

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11
Q

Three secondary hazards earthquakes + brief explanation

A
  1. Soil liquefaction - loose sand and silt that is saturated with water can behave like a liquid when shaken by an earthquake. Pore water pressure increases so sand grains lose contact with each other. Soil loses its ability to support structures.
  2. Mass movements - may be triggered by earthquakes, reducing the shear strength of the slope for a short time period
  3. Tsunami - when a large volume of water is instantaneously displaced vertically du to upward or downward movement of the sea bed -> becomes especially hazardous once in increases in height as it approaches the shore with a shallowing sea bed
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12
Q

6 types of volcanoes with brief description

A
  1. Fissure volcano - gentle basaltic slope
  2. Shield volcano - gentle slope of basaltic lava flows
  3. Dome volcano - steep convex slope from thick and fast-cooling lava
  4. Ash-cinder volcano - cinder, fine ash
  5. Composite volcano - branch pipe (stratovolcano)
  6. Caldera volcano - old cone, new cone -> highly explosive
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13
Q

7 types of volcanic eruption

A
  1. Pelean eruption - highly viscous magma -> explosion out of weakness in the side of volcano
  2. Plinian eruption - very violent explosion resulting in narrower cloud e.g. Mt Pinatubo
  3. Icelandic eruption - fluid basalts issue quietly from fissures and mid-oceanic ridges
  4. Hawaiian eruption - fluid basalts issue from vents in volcanoes. Gases escape easily and quietly with occasional spurts of gases form lava lakes causing lava fountains.
  5. Strombolian eruption - less fluid lava and gases escape with moderate explosions in which lava bombs are ejected
  6. Vulcanian eruption - eruptions more violent as more viscous lava solidifies more quickly and traps gases. Tephra released + ash-laden clouds in mushroom shape
  7. Vesuvian - high gas content, long periods of inactivity, wide and dark ash cloud
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14
Q

Nuees ardentes

A

Dark glowing, fast-moving, incandescent mass of gas - enveloped particles that is associated with certain types of volcanic eruptions (contain dense lava fragments derived from a growing lava dome) e.g. Martinique 1902

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15
Q

Lava flows

A

Streams of molten rock that poor or ooze from an erupting vent. with speed depending on the… type of lava, viscosity, steepness, width of flow, rate of lava production

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16
Q

Lahar

A

A hot or cold mixture of water and rock fragments that flows down the slopes of a volcano

17
Q

Pyroclastic flows

A

80/100 km/hr, between 200-700 degrees celcius

Contains a high density mix of hot lava blocks, pumice, ash and volcanic gas

18
Q

Ash fallout and tephra

A

Fragments of rock that are produced when magma or rock is explosively ejected;
ashes < 4mm, cinders 4-5mm, lapilli are pebble sized, volcanic block are large fragments

19
Q

Steam and poisonous gas emission

A

Magma contains dissolved gases which provide the driving force that causes most volcanic eruptions - Mt Pinatubo released 250 megatons of gas

20
Q

Characteristics of basaltic lava

A

Low viscosity, hotter (up to 1200 degrees), lower silica content, associated with frequent but gentle eruptions, found at constructive margins and hotspots

21
Q

Andesitic

A

High viscosity, less hot (900 degrees), higher silica content, pyroclastic flows likely, destructive margins, infrequent but violent eruptions

22
Q

Aa lava

A

Free chunks, lava flows rapidly, viscosity increases as heat is lost quickly, up to 10m thick

23
Q

Pahoehoe lava

A

Smooth surface, slow flow, flows far

24
Q

Factors contributing to increased sheer stress

A

Undercutting/slope steepening (erosion)
Loading of slope - weight of water, infrastructure etc.
Lateral pressure - water in cracks, subsequent freezing
Transient stress - earthquakes or winds

25
Factors contributing to reduced shear strength
Weathering Changes in pore-water pressure Changes of structure Organic effects - decay of roots, burrowing
26
Scale to measure hurricane magnitude
Saffir-Simpson scale - looks at damage done, working back to estimate wind speeds and height of storm surge
27
Explain the formation of a hurricane
Diagram with detailed annotations N.B. low pressure area has to be far enough away for the equator so that the coreolis force creates rotation in the rising air mass. Conditions must be unstable
28
Factors affecting the impact of tropical storms
1. Unpredictability - e.g. Hurricane Charley (2004) hit Florida's Punta Gorda unexpectedly 2. Strongest storms do not always cause the greatest damage 4. Population distribution 5. Hazard mitigation effectiveness 6. Levels of development
29
4 conditions needed for tornado formation + explanation of formation
DIAGRAM Moisture, instability, lift, wind shear - elongated funnels of cloud that descend from the base of a well-developed cumulonimbus cloud - for a vortex to be classified as a tornado, it must be in contact with the ground and that cloud base - pressure gradients can reach 25mb per 100m - wind speeds can exceed 300mph - most destructive and deadly tornadoes develop from supercells, which are rotating thunderstorms with a well-defined low-pressure system called a mesocyclone
30
Scale to measure size of volcanoes
Fujita scale: F5 = 261-318 mph & 1-3 mile path width
31
Hazards associated with tornadoes
Strength of winds Strong rotational can twist objects from their fixings Strong uplift can left debris to great heights Pressure gradient can result in explosions of walls and glass Precipitation - hail stones/heavy rainfall is common
32
How many deaths and injuries caused by tornadoes every year in the US
80 deaths, 1,500 injuries