6 Billion People and Counting
Joseph Hull and Greg Langkamp

Environmental Outline # 11:
Hazards and Risk
copyright  Joseph Hull and Greg Langkamp

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Natural Hazards
    Earthquakes
        earthquake = ground shaking (waves in Earth) caused by fast movement along faults (breaks in Earth's crust)
            more slip along the fault = more groundshaking:  slip/movement CAUSES ground shaking
        many active faults near some edges of continents, on ocean floor, and occasionally within continents
        earthquakes +- unpredictable
        cause DIRECT damage from ground shaking and ground breaking
        cause INDIRECT damage from fires, landslides, tsunamis, ground liquefaction, etc.
        last monster quake in PNW:  January 1700, magnitude 9.  also AD900, downtown Seattle, magnitude 8
        earthquakes are nature's way of getting rid of Earth's internal energy by doing work (moving fault blocks around)
    Tsunamis
        very large ocean wave (has extremely long wavelength but fairly small amplitude or wave height)
        caused by fault breaking ocean floor, or rarely by large submarine landslide
        tsunamis travel very fast across ocean (100's of kms per hour) and can travel across entire Pacific Ocean
            takes about 12-14 hours for tsunami to travel from Japan to Washington State (and vice versa)
        waves become very tall and destructive when they enter shallow water, can be 20-30 meters high in extreme cases
        lots of potential damage along Pacific Rim; Washington's southwest coast at high risk (but few residents)
       tsunami in Puget Sound associated with AD900 quake, also caused seiche wave (soup bowl wave) in Lake Washington
        quakes and slides +- unpredictable, therefore tsunamis unpredictable, but warning systems can help unless quake is close.
    Mass Movements (Landslides, Mudflows, etc.)
        movement of earth materials (soil, loose rock, vegetation, sand and gravel, mud and clay) downhill and downslope
        if slides as block = SLIDE (landslide, e.g.), if flows like water = FLOW (mudflow, e.g.)
        contributing factors:  steep slopes, weak earth materials, heavy rainfall and/or lots of groundwater, human disturbance
        sort of predictable some places:  in Seattle, 4 days of rainfall averaging 1 inch per day during wet season = MASS MOVEMENTS
        can cause lots of property damage and sometimes death and injury but not on a great scale
       mass movements are nature's way of flattening out slopes without using bulldozers and dynamite
    Volcanic Eruptions
        volcanoes:  cone-shaped pile of lava flows and airfall debris, built up in layers over time
        "quiet" volcanoes like Hawai'i made up of well-behaved lava flows and very little airfall ash/tephra.
            can damage farms, homes, roads etc. (buried by lava) but not life-threatening, plenty of time to get out of way
        "explosive" volcanoes like Mt. St. Helens, Pinatubo, Etna made of both flows and ash
            ash and volcanic mass movements can travel far from volcano and cause injury and death
        volcanic mass movements:  several different flavors, depending upon type of volcano
            huge landslides on volcano can trigger eruptions.  e.g. Mt. St. Helens 1980
            eruptions/landslides can turn soupy as they move downhill, turn into lahars and travel long distances
                e.g. 300 year old lahars along Duwamish River near West Seattle bridge from Mt. Rainier!!
        volcanic eruptions are nature's way of getting rid of internal heat of Earth.
    Wildfires (in part)
 

Human-Induced Hazards
    Wildfires (in part)
    Petroleum Spills
    Automobile Accidents
    Radioactive Releases from Nuclear Power Plants
    ______________________:  insert your favorite here
 

Power Law Frequency Distribution
    many hazards show a special pattern of sizes:  many small ones, some medium ones, a few big ones
        example:  earthquakes in WA.  Magnitude 3 = once per year,  Mag 6 = once per 30 years, Mag 7 = once per 100 years
    make a plot of X = size versus Y = frequency of hazard of that size, see "L-shaped" curve of decreasing frequency with size
    power law or power function often fits this L-shaped curve the best.  power law has form Y = a X ^b
        b is negative in this case, because frequency decreases with increasing size
        example:  earthquakes in Missouri, frequency = 1927 magnitude ^(-.876)

Fractals and PLFD
    many objects show a special pattern of sizes:  many small ones, some medium ones, a few big ones
        e.g. arteries in the human body.  streets in a city.  streams in a drainage basin.  branches on a tree.  frondlets on a fern.  etc.
    these objects all have a special space-filling property: no matter how closely you look, there are ever smaller fronds, branches, etc.
    the pattern of fronds, branches, etc.  looks the same no matter what scale you are looking at.  called self-similar
    objects with this space filling self-similarity are called fractal.  (fractal is just a made up word for "fractional dimension")
    fractal objects have power law frequency distributions; many small ones, some medium ones, a few big ones  !!!!
    therefore earthquakes, landslides, petroleum spills, automobile accidents, etc. are all fractal
        fractal in a different sense than fern fronds or arteries; not filling up "space" like branches do.

    with objects that show a normal or bell-shaped distribution of sizes, there is a characteristic size (in the middle, near the mean)
        e.g. measure the height of corn stalks, typical or characteristic height is about 3 meters, some taller, some shorter
    with objects that show a fractal or power law distribution of sizes, there is NO characteristic size
        the closer you look, the smaller the size; the farther back you stand, the bigger the size.
    What is the biggest oil spill possible??  only limited by the size of the oil tanker......
    What is the "typical" oil spill size??  There is no such thing....

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