1A: The Challenge of Natural Hazards Flashcards
(145 cards)
What is a natural hazard?
An event that has the potential to cause damage, disruption, destruction and death
What are Tectonic Hazards?
Hazards which involve the movement of tectonic plates e.g. volcanoes
What are Atmospheric Hazards?
Hazards which involve the conditions in the air around us e.g hurricanes
What are Geomorphological Hazards?
Hazards which occur on the Earth’s surface e.g. flooding
What are Biological Hazards?
Hazards which involve living organisms e.g. forest fires
Define ‘Hazard Risk’
The chance or probability of being affected by a natural hazard
How is Deforestation a human influence which increases hazard risk?
Cutting down trees increases the risk of flooding. Trees intercept and absorb water, slowing the movement of water down
How is Urbanisation a human factor which increases hazard risk?
More people are living in urban areas therefore there is a greater risk of injury and death
How is Climate Change a human factor which increases hazard risk?
In a warmer world, the atmosphere will have more energy, leading to more intense storms and hurricanes. Climate change may cause some parts of the world to become wetter and increase the risk of flooding
How is Poverty a human factor which increases hazard risk?
In poorer parts of the world, poverty may force people to live in areas of risk and poorly constructed buildings
Describe the process of convection currents in the Earth’s mantle
- The core heats up the magma in the mantle
- The hot magma is less dense than its surroundings, so it rises upwards
- When it reaches the top, it cools
- It becomes more dense, and therefore sinks back down to the bottom
- It is heated up again, and the cycle continues
- The plates, which lie on top, are pushed and pulled by the convection currents in the magma
Compare the thickness and density of continental crust to oceanic crust
Continental crust is thicker and is less dense (cannot sink) than oceanic crust
Describe what happens at a constructive plate margin
- At a constructive plate margin, the plates are moving away from each other
- When the two plates are pulled apart, magma rises in between the gap left by the two plates separating. Lava (when magma is above ground it is classed as lava) then pours out onto the surface
- Volcanoes form in the areas where lava pours out. This lava is usually runny and free-flowing, which creates flatter volcanoes. Earthquakes also occur here as the plates shake and vibrate when they move apart
- This process can happen on continental crust or oceanic crust
-When new land is formed on the ocean floor, this is known as sea floor spreading (as the floor spreads and gets wider) - When lava cools, it forms rock. Over time, this rock builds up and can form islands, for example Iceland is a volcanic island. Iceland sits on the Mid-Atlantic ridge, which is where the lava pours out from
Describe what happens at a destructive plate margin
- The denser oceanic crust is subducted below the continental crust
- The plate that is subducting leaves a deep ocean trench
- Friction between the two plates causes strong, deep earthquakes
- The oceanic crust is melted as it is pulled deeper into the mantle, creating magma
- This magma causes pressure to build up under the crust
- Eventually the magma pushes out through weaknesses in the crust, creating explosive volcanoes
(When two continental plates meet, fold mountains are formed)
Describe what happens at a conservative plate margin
- At a conservative plate margin, parallel plates move in different directions or at different speeds in relation to each other
- When these plates move side by side, friction builds between the plates
- The friction builds up over many years, and eventually the pressure becomes so large that the plates eventually move in a sudden jolt
- This releases a lot of energy which sends vibrations through the the ground (Earthquake)
- On oceanic crust, this movement can displace a lot of water, which causes tsunamis
- On continental crust, fault lines can occur where the ground is cracked by the movement
- There are no volcanoes on conservative plate margins because no magma is being generated
Primary effects of tectonic hazards
The effects that are directly caused by the natural hazard itself. For example, people being killed or injured when an earthquake causes buildings to fall down, or lava and ash damaging infrastructure
Secondary effects of tectonic hazards
The effects that are as a result of the primary effects. For example, homelessness due to homes being destroyed or a tsunami or landslide caused by the original earthquake
Immediate responses to tectonic hazards
Actions taken as soon as the hazard happens and in its immediate aftermath. Immediate responses usually aim to reduce loss of life and provide vital aid and resources. e.g. search and rescue, food and water, shelter.
Long-term responses to tectonic hazards
Actions taken after the immediate responses when the effects of the hazard have been minimised. Long-term responses aim to restore normality and reduce risk in the future. e.g. rebuilding infrastructure and homes, building defence mechanisms, setting up warning systems
When was the Nepal earthquake?
25th April 2015
What was the magnitude of the Nepal earthquake?
7.9
How many people died in the Nepal earthquake?
9,000
How many people were injured in the Nepal earthquake?
19,000
Overall, how many people were affected by the Nepal earthquake?
Over 8 million (1/3 of Nepal’s population)