Chapter #6 Flashcards
Tsunami Tigger’s include,
- Earthquakes
- Landslides
- Explosive volcanic eruptions
- Meteorite impacts
How are Tsunami’s generated?
The sudden movement of a large mass against the sea surface.
These masses include:
* the seafloor shifting up or down
* a submarine and/or subaerial landslide
* a pyroclastic flow
* an air blast from an explosive volcanic eruption
* a meteorite impact
Tsunamis are not _____
Tsunamis are not tidal waves or large storm waves
What creates the multiple waves in a Tsunami?
The equilibrium of the water is disrupted, either pushing water up or down, then the gravitational force attempts to restore equilibrium forming multiple waves.
Trough (Tsunami)
The line along which water depth is at it’s lowest
Crest (Tsunami)
The line along which water depth is at it’s highest
Tsunami wave characteristics depend on 3 variables, these are
- The area over which the generating mass moves
- The amount of movement
- The velocity of movement
Class Question #1
Why are tsunamis classified as gravity waves?
a) Gravity causes the seafloor to suddenly rise, pushing up the water’s
surface.
b) Gravity acts as a restoring force that returns water to its equilibrium
level.
c) Gravity differences between the seafloor and continental rock
create very high tsunami waves.
d) Gravity increases the complexity of tsunami waves as they
propagate across open oceans.
b) Gravity acts as a restoring force that returns water to its
equilibrium level. (correct answer)
Tsunami height variables include,
- The distance between source and location
- The amount of water pushed by mass
- The shape and velocity of the mass pushing the water
- wave reflection, refraction, and interference
Are tsunami waves faster near the shore or open sea?
They are faster at open sea
Velocity of Tsunami waves formula is
C = sqrt(gD)
Wave energy of Tsunami waves formula is
E = 0.125pgH^2L
Drawback (Tsunami)
When a approaching tsunami trough lowers at sea level
Tsunami Elevation
The greatest vertical distance from a crest and sea level
Inundation distance
The horizontal distance between the normal shore line and the inundation limit
Run-up elevation
The vertical distance from the normal shoreline to the inundation limit
Coast factors that increase wave height include,
- Sand bars due to shallow depth
- Bays and estuaries due to narrowing of wave energy focus
How many waves are in a train, and how long for the entire event
6 - 25 waves, 3-6 hours