Hazardous Environments Flashcards
Body Waves
Bodywaves: waves within the earth’s interior
P waves: travel by compression and expansion
S waves: travel with a side to side motion
Surface Waves:
Surface waves: when body waves reach the surface:
Long waves: sideways movement
Rayleigh waves: up and down movement - most hazardous.
Soil liquefaction
loose sand and silt that is saturated with water can behave like a liquid when shaken. Pore water pressure increases so sand grains lose contact with each other = soil loses ability to support structures. = quickly solidifies hence structures trapped in the ground.
E.g Christchurch Earthquake aftershock of 7.1 in 2011 caused widespread liquefaction. Leading to $16bn in damage.
What and causes of Tohoku earthquake
11 March 2011 earthquake and Tsunami, Japan.
Magnitude 9, lasted 6 minutes.
Tsunami waves, on average 3-6m.
Causes:
Pacific plate subducting beneath the Eurasian plate. Focus 32 km in NW Pacific ocean. Epicentre 70 km east of Tohoku. Earthquake caused an upthrust of 8m along 180 km seabed.
Impacts of Tohku earthquake
Primary:
16,000 deaths in Japan. Estimated 92% died from drowning, 4% crushed in earthquake. 127,000 buildings destroyed.
Secondary:
Fukushima nuclear incident. 4.4 million households without electricity, 1mn households without access to water. 25 million tonnes of debris in coastal areas.
World bank estimated economic cost = US$235bn.
Management before Tohuko earthquake
Many large foreshocks record: e.g first major fore shock = 7.2 magnitude on 9th march.
Recurrence interval for tsunamis on sendai plain estimates a 800 - 1100 year recurrence interval for large tsunamigenic earthquakes. = In 2007, the probability of an earthquake with a magnitude of 8.1–8.3 was estimated as 99% within the following 30 years
One minute before the earthquake was felt in Tokyo, the Earthquake Early Warning system, which includes more than 1,000 seismometers in Japan, sent out warnings of impending strong shaking to millions = saved lives as high speed trains and factory lines stopped, earthquake drills enacted.
Earthquake proof design; e.g Mori Tower, Tokyo. - 54 stories but has 192 of fluid-filled shock absorbers filled oil, which acts as a counter balance to swaying.
Tsunami wall line 40% of Japan’s coast - but these were overtopped. E.g at miyako 4m in height. Replaced by 12.5m
management after Tohoku earthquake
Residents within 20km of Fukushima were evacuated after the failing of the cooling system = radiation levels inside 1000x normal =
State of Emergency Declared.
Japanese red cross reporting $1bn in donations, 116 countries and 28 NGOs offered assistance.
What and causes of haiti earthquake
12 January 2010 Haiti Earthquake. Magnitude 7.
Focus 13 km. Epicentre 25 km west of Port au Prince. Occurred along a conservative plate boundary. Caribbean plate is moving 20mm per year faster than the North American Plate. g
impacts of haiti earthquake
160,000 deaths. 250,000 buildings severely damaged/destroyed. (there are no building codes in haiti)
management after haiti earthquake
More than 20 countries sent military personnel to assist with relief and rescue. But efforts were restricted due to congestion and blocked roads. 23 NGOs raised US$1bn for relief. Six Months after the quake, 98% of rubble remained uncleared.
Icelandic eruption
Icelandic eruption: persistent fissure eruption. Large quantities of basaltic lava build up vast horizontal plains.
hawaiian Erruption
Hawaiian Eruption: runny basaltic lava travels down the sides of the volcano in lava flows. gases escape easily. Occasional pyroclastic activity but small.
Strombolian eruption
Strombolian Eruption: frequent gas explosions which blast fragments of runny lava into the air to form cones. Very explosive eruptions with large quantities of pyroclastic rock thrown out. Common to have white steam cloud from crater.
Vulcanian eruption
Vulcanian eruption: violent gas explosions blast out plugs of sticky lava. Fragments build up into cones of ash and pumice. Occur when there is very viscous lava which solidifies rapidly. Often large quantities of volcanic ash.
Vesuvian eruption
vesuvian eruptions: very powerful blasts of gas pushing ash clouds high into the sky. lava flows and ash clouds.