what are seismic sea wave?
an abnormally long wavelength wave produced by sudden displacement of water
what is a near field tsunamis?
tsunami that strikes areas adjacent to its point of origin
there is little warning
what is far field tsunami?
tsunami that strikes areas distant from its point of original
can impact multiple countries around
what are masses that may cause tsunamis?
the seafloor shifting up or down
a submarine and/or subaerial landslide
a pyroclastic flow
an air blast form an explosive volcanic eruption
a meteorite impact
are tsunamis large tsunamis?
not tsunamis
what are tsunami wave train?
groups of waves
consistent w/ earthquakes
what are the tsunami wave characteristics?
long wave lengths
velocity dependent of water depth
the wave is so big that there is frictional interaction w/ the ocean bottom
wave slows down in shallower water → more friction
wave increases its height as the water becomes shallower near the coast
wave height depends on?
the distance between source and location
the amount of water pushed by a mass
the shape and velocity of the mass pushing the water
what creates waves refraction interference?
islands
are tsunami waves big or small while crossing open ocean?
small
what creates towering waves as they approach shore?
shoaling
wave velocity across open oceans?
around 700 km/hr
does wave velocity slow or speed up as they enter shallow water?
slow
how are big waves caused?
water at rear of wave catches up to slower water, increasing height
front slows down, back catches up → cause big wave
what can prevent water from flowing inland?
steep cliffs
water may flow many km into gently sloping coasts
what occurs in a mega-thrust earthquake?
Megathrust earthquakes have \n an M W > 8.6.
at subduction zone
Accretionary prism (AP) at \n convergent margin.
Shortens horizontally
Thickens vertically
Land elevation slowly \n rises.
Two motions occur to AP \n when slip occurs:
Face quickly moves \n seaward.
Land elevation quickly \n sinks.
sumatra tsunami - Dec 26, 2004
9.1 magnitude subduction zone earthquake
indian plate and burma plate
paleoseismic studies show that giant seismic events occur every 230 yrs
tsunami waves generated by this event rose 10 metres or more above sea lvl
230,000 deaths
Chile Tsunami - may 26, 1960
caused by 9.5 magnitude earthquake in subduction zone along the coast of Chile
2000 people killed in Chile: 5700 people killed around the Pacific
Hilo, Hawaii, 61 deaths
Japan, 185 deaths
left a sand layer over the soil in a farmer’s field
alarm sys was placed after this
how can volcanoes generate tsunamis?
caldera collapse
submarine eruption
debris cloud collapse may trigger tsunamis
debris displaces sea surface when it falls
flank collapse
do volcanos generate big tsunamis?
only small vol of water it moved
generate (relatively) small tsunamis
only impact local area
Krakatau Eruption - 1883
in Sunda Strait
tsunami killed 36,000 on Sumatra and Java
pyroclastic flow may have displaced sea surface
how frequent and severe are flank collapse?
<1% of tsunamis are caused by volcano flank collapse
can produce large near-field tsunamis
what is example of flank collapse generated tsunami?
Anak Krakatau 2018
400 deaths
7,000 injured
47,000 displaced from homes
what percentage of tsunamis are caused by fast-moving landslides or rock avalanches?
around 1%
These types of tsunamis are created by fast-moving landslides (sediment) or fast-moving rock avalanches (broken bedrock) falling into the ocean and displacing a large volume of water. \n • Size of tsunami waves based on the mass of the materia
example of rock avalanche generated tsunami?
Lituya Bay Alaska - July 9, 1958
released a 7.3 magnitude earthquake
wave was 150 meters high and surged metres above sea lvl
what % of tsunami are from submarine landslide?
around 5%
do submarine landslide generate big tsunamis?
typically not as large as ones generated by landslide/rock avalanches from above sea lvl bc of the gentle slopes of the ocean floor
example of submarine landslide?
Storegga slide
tsunami laid sediment (TLS) found above sea lvl on the Shetland Islands, Norway and Scotland
TLS consist of mud fragments ripped from the sea floor a\layers of well-sorted sand
we knew it happened cuz found an area of sand missing
Papua New Guinea landslide
an Mw 7.0 earthquake off northern coast of Papua New Guinea
15-m-high wave front devasted northern coastline; 2,000 people died, 1,000 injured, 10,000 displaced
tsunami generated
region is remote, isolated and lacks modern medical facilities
infection and post traumatic stress created long impact
example of tsunamis from meteorite impact?
66 Ma, a 14-km-diameter asteroid struck the Yucatan Peninsula.
Impact created the 150-km-diameter Chicxulub crater.
Impact ended the Mesozoic Era and the Age of Dinosaurs.
Mega-tsunamis were generated from the impact and falling debris.
what can we do in trough arrives on shore first?
we can tell that all the water runs away from shore providing some warming
how can offshore coral reef play role in tsunami?
if coastal area surrounded by it, can provide some protection by forcing wave to break on reef
how does lack of warming impact region?
difficult to disseminate info between and within countries
what is the time between waves?
typic more than 30 mins
which waves are the worse?
second or third waves often worse than first
rising water hazards
boats carried inland as anchor and chains are lost
larbors fill like bathtubs
water moving onshore issue
vehicles, trees, and debris and tumbled and crushed
buildings are crushed or carried off foundations
drawback from tsunamis?
debris and sediment are tumbled and crushed
sand stripped from beach
human and animal fatalities occur at all stages
tsunami aftermaths?
tsunamis destroy power lines, roads, bridges, water and gas line; fires starters
essential services cant reach victims
debris rots and molds
crops destroyed, salt deposition in soils
contamination of water supplies
disease due to water rotting things
relief and recovery?
tsunami relief and recovery are challenging:
roads are buried or damaged
communication sys destroyed
hovercraft may be the only to way to access communities
ships often become floating hospitals
near-field tsunami warming system?
arrival of tsunami less than 30 mins after tsunami trigger
what are some far-field tsunami warming system?
travel time of tsunamis in the Pacific Ocean can be accurately calc based on topography of the ocean floor
tidal sensors and ocean-bottom sensors can detect waves as they move across the ocean
downside: cannot forecast the actual height of a tsunami wave
some adaptations to tsunami hazards?
land-use zoning
engineering structs to resist erosion
orient streets and buildings at right angle to the waves
well-rooted vegetation
tsunami hazards adaptations in Japans?
seawall with stairway evacuation route used to protect a coastal town in Japan
water gate used to protect Okushiri Island → they automatically close within secs after earthquake shaking triggers seismic sensor
tsunamis stones in Japan warm not to build below certain elevations
tsunami inundation map increase public awareness
tsunami from Cascadia Subduction-Zone earthquakes
cascadia subduction zone located 1,900 km offshore southern british columbia
sequences of tsunami-laid sediment (TLS) indicate historic tsunami impacts along the Pacific Northwest coastline
Mud → contains the remains of marine plants
tsunami → laid sand
peat at the base → consists of partially decayed saltwater marsh plants
huge tsunami-flattened forest are now below sea level why?
bc of displacement during an earthquake of the coastal bulge offshore
example of forest that got flattened?
ancient Sitka spruce forest in the bay at Neskowin, Oregon, was felled by a giant tsunami following a large subduction-zone earthquake of 1700
Japan earthquake
March 11 2011
Magnitude 9.0 earthquake
subduction zone earthquake
generated a tsunamis that swept across the pacific ocean