volcanic and slope failure-landslide hazards Flashcards
what are examples of volcanic hazards? (7)
- Lava flows
- Ash falls and other ejecta (tephra)
- Ballistics (explosions and blasts)
- Pyroclastic flows
- Debris avalanches and landslides
- Lahars or mud flows- tend to follow the eruptions.
- Gas emissions. Less of a hazard, but assessing the eruption.
what is lava flow?
- Molten rock or magma erupting at the surface
* Composition and temperature controls behaviour of lava flows
what are balsaltic properties?
Basaltic/mafic- low viscosity, flows fast
what are silicic properties?
Silicic/felsic- high velocity, flows slowly. Leads to more violent eruptions.
why is lava flow destructive?
Destructive due to high temperatures but in many cases flows slowly enough or on predictable paths for people to escape.
what is tephra?
• Tephra- anything ejected out of a volcano. Ash is defined as smaller than 2.5 mm. Other terms include lapilli, blocks, and bombs.
what are the hazards of ash fall?
- Weight of the ash can cause damage to structures
- Hazards to flying aircrafts
- Visibility hazard
- Abrasive material, corrodes.
- Electronics, machinery, power generation, telecoms.
- Proximal burial
- Inhalation
- Transported far from volcano so can affect a large area dependent on the wind direction.
- Large eruptions can impact climate (local or global)
what are ballistic explosions?
- Vertical or lateral explosions of debris, magma, gas.
* Can lead to pyroclastic flows, mud flows, debris avalanches, landslides, ash falls etc.
where are explosive eruptions most commom?
Explosive eruptions are more common for silicic magmas (continental), or underwater eruptions
how can a volcano trigger an explosion?
Volcanic eruption, earthquake (indirectly), or landslide can trigger an explosion.
what happened at Mt St Helens?
Mt St Helens- an earthquake triggered a landslide which released pressure leading to an unexpected lateral blast.
Includes individual bombs, blocks etc. Now Helens has a huge gap where the landslide occurred.
what are pyroclastic flows?
- High speed avalanches of hot ash, rock and gas.
- During explosive eruptions
- Destroys everything in their path.
what are lahars or mud flows?
- Dilute downstream
- Often triggered by rain fall or landslides during or following an eruption
- Can occur between eruptions
- More distal nature and delay increase hazard and risk.
what are the temperature and speed of pyroclastic flows?
• Temperature up to 1500 degrees celcius. 150-250 km/h.
where do lahars originate from?
Originate on slopes of volcano
• Water saturated debris, high percentage of rock and ash debris
what is the speed of lahars?
Flow rates up to 10 metres per second. Can travel 100 km from volcano dependent on travel networks
what can also cause a lahar?
• Slow melt or water trapped beneath ice may also lead to lahar
waht gas emissions are dangerous with a volcano?
• All magmatic materials contain dissolved gases- water, CO2, SO2, H2S.
* Change in gas emission scan be used to predict eruptions * SO2 can lead to acid rain
what are aerosols?
• Aerosols in atmosphere can affect earths surface temperature, destroy ozone.
what is a consequence of gas emissions?
Close to vents- hazardous to humans and livestock- potential suffocation
• Local and downwind corrosion
what are fumaroles?
Long term “fumarole” systems emit gas on most active volcanoes, and for 1000’s year post eruption.
what is slope failure?
• Takes many forms both on land and offshore- rock falls, avalanches, debris flows, turbidity currents. All involve different quantities of debris and fluid, different flow types/processes.
what are submarine slope failures?
Submarine slope failures: can be triggered by earthquakes, can generate tsunami waves, but dissipate rapidly, can result from collapse of steep slopes, such as marine volcanic islands such as Hawaii.
what are subaerial slope failures?
Subaerial slope failure: similar triggering mechanisms. Rainfall, high runoff, coastal erosion increase probability.
what are mitigations of volcanoes?
- Understand geology and past failure history. Failure planes, rock and sediment permeability versus overpressure.
- Improving slope stability (engineering)
- Controlling water flow and sediment saturation
- Controlling runoff, deforestation, development, fire. Can use drains, mesh traps, vegetation on the slopes., spray cement.
- Assessing timing of triggering events
- Adapting building codes and development or planning.
how are the tsunamis measured?
• Tsunami size defined by intial landslide parameters
what is a worse case model?
Worst-case models assume failures are very large, entire landslides fails as a single coherent block, and landslides reaches high peak velocity.
what is the mode of failure?
• The mode of failure is critical for whether a tsunami is generated and for its magnitude
how can models casue tsunamis?
• Models with above parameters can result in large tsunamis than can cause destruction on ocean basin scale.
what analysis from El Hierro landslide?
• Analysis of seafloor bathmetry and of marine sediment cores reveals: landslide processes range from avalanches to debris flow