Tectonic Processes & Hazards Flashcards
What is the word for splitting up land-use between different areas of a city to make sure there are no houses on unstable land?
Zoning
Examples of good government preparation for natural disasters?
Meeting basic needs
Tackling corruption
Land-use planning
Community awareness programmes
What are the 3 types of boundaries?
Divergent
Convergent
Conservative
Tsunamis
Caused by submarine shock waves generated by earthquake or volcanic eruptions. Displacement of the water column.
What is a risk?
The likelihood of humans being affected by a hazard.
What is the hazard risk equation?
Risk = (hazard x vulnerability) / capacity to cope
Vulnerability
How susceptible a population is to damage caused by a hazard
Capacity to cope/resilience
How well a population can recover from a disaster
What is a disaster?
When a hazard affects a humans wellbeing.
What does Dreggs disaster model suggest?
A disaster only happens when a hazardous even meets a vulnerable population
Conservative PB
Plates move past each other but at different speeds, causing friction and collisions
Constructive PB
Plates moving apart from one another
Primary hazards of a volcano are…
Pyroclastic flow
Tephra (ash falls)
Lava flows
Volcanic gas
Secondary hazards of volcanoes are…
Lahars
Jokulhaups
Destructive
Plates move towards each other, colliding head-on if both continental. If one is continental and the other is oceanic, subduction will occur where the oceanic plate is thrust under the continental. If its two oceanic plates, the heavier plate will be forced under the other.
Earthquakes at constructive boundaries
Plates move at different speeds which builds pressure until plates crack, causing fault lines. This results in the release of seismic waves, producing earthquakes.
Earthquakes at destructive boundaries
One plated forced under, getting stuck due to friction which produces energy. As plates suddenly jerk past each other this energy is quickly released forming a powerful earthquake.
Earthquakes at conservative boundaries
Plates lock with one another which, when pressure is build produces sudden seismic waves.
P Waves
Immediate shock - fastest traveller
S Waves
Longer wavelength, arrives seconds later
L Waves
Only travel through the crust, causes horrizontal movement
Volcanoes at constructive boundaries
Magma is less dense than the plate so rises above it, forming a volcano, such as those within the Rift Valleys
Volcanoes at destructive boundaries
Subduction causes the melting of the oceanic plate, allowing for magma to rise on the crust to form a volcano. Usually more explosive. E.g Mt. St. Helens
Volcanoes at conservative boundaries
Volcanoes do not form at conservative boundaries
Parks Model:
Takes into account that different hazard events have diferent impacts so vary in their duration, speed and destruction of quality of life. The 3 lines are representative of a countrys response and ability to manage the disaster
Strategies to modify the event :
- Land-use Zoning: Where it is the safest to build infrastructure
- Hazard-Resistant Design: Invest and produce in long-term construction projects
- Engineering Defences: Stronger sea walls or mangrove forests
- Diversion of Lava Flows: Spraying seawater to cool and solidify lava flow