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Tom Pering
“Super Volcanoes”
Today’s topics…What is a super eruption?Where do super eruptions occur?What do super volcanoes look like?“Super Volcanoes” around the world.Yellowstone Caldera ChainYellowstone NowWhat would an eruption at Yellowstone be
like to live through?What are the chances of an eruption
occurring in our lifetime?
What is a super eruption?You may know about super eruptions under
the term “supervolcano”.Definition of a super eruption
VEI 8 – Ultra-Plinian, Mega-Colossal
Lord Byron - Darkness
“I had a dream, which was not all a dream.The bright sun was extinguished, and the starsDid wander darkling in the eternal space,Rayless, and pathless, and the icy earthSwung blind and blackening in the moonless air;Morn came and went -and came, and brought no day”
Plate Boundaries
Hot SpotsMantle Plume
Huge Magma Chambers
Where do super eruptions occur?
What do super volcanoes look like?Caldera Volcanoes
Well known “super volcanoes”Yellowstone, USALake Toba, INDONESIATaupo, NEW ZEALAND
Not so well known “super volcanoes”La Garita Caldera, USACerro Galán, ARGENTINAGlen Coe, SCOTLANDScafells, Lake District, ENGLAND
Glen Coe, ScotlandLast eruption 420 million years agoSilurian (Paleozoic Era)5 eruptionsRoughly 500,000 years apart.Glaciations
Scafells, Lake District, England440 – 520 million years ago (unknown last
eruption)Ordovician (Paleozoic Era)Largest known phreatomagmatic eruption VEI 7 or 8?Glaciations
Lake Toba, Indonesia74,000 years agoLargest Volcanic Lake in worldMankind survived
Taupo, New ZealandFirst Eruption – 300,000 years agoOruanui Eruption
26,500 years ago
Lots of volcanic activity nearby
La Garita Caldera, USAColorado26 million years ago
Largest known eruption5000 km³
Cerro Galán, ArgentinaAndes Mountain Range2.2 million years ago1050 km³
Yellowstone Caldera Chain
Yellowstone EruptionsHuckleberry Ridge Caldera, 2.1 million
years ago2450 km³
Mesa Falls, 1.3 million years ago280 km³
Lava Creek, 640,000 years ago1000 km³
• Source: USGS
Yellowstone
Yellowstone NowNational Park - over 3 million visitors a year.307 million people in the USAAn eruption at Yellowstone could be a small
outflow of lava or an VEI 8 eruption. Large Magma Chamber
Warning signs of an imminent eruptionHigh ground temperaturesIncreased volcanic gas emissionHydrothermal feature – activity increaseGround upliftHydrothermal explosionsEarthquakes
Harmonic tremors
Possible regional effects of an eruption at YellowstoneZone 1 – Pyroclastic Zone (Around 90,000
could be killed – 90% mortality rate)100 km radius
Zone 2 and 3 – Asphyxiation and Roof Collapse 3 million people trapped by ash
Zone 4Ashfall – 15cm
Zone 5Ashfall – 5cm
Zone 6Ashfall – 1cm
Different ways to die…Direct
AsphyxiationGas PoisoningPyroclastic FlowsRoof CollapseBurningLaharsPlane Crash
Indirect Starvation / DroughtFreezeRiots / Conflict
What could be the global effects of an eruption at Yellowstone?Water Contamination
Food Shortages
Increase Rainfall
Economic Failure
Extinction
Volcanic Winter
Triggering of an Ice Age
What are the chances of a super eruption occurring in our lifetimes?Are we overdue?
Further Readinghttp://www.yellowstonenationalpark.com/ca
lderas.htmYellowstone Volcano ObservatoryUSGS
References Brenchley, P.J., Rawson, P.F., 1990? The Geology of England and
Wales. The Geological Society. Bath. 256pp CIA World Fact book [Online] Cole, J.W., Milner, D.M., Spinks, K.D., 2005. Calderas and caldera
structures: a review. Earth Science Reviews. 69, pp. 1-26 Grotzinger, J., Jordan, T.H., Press, F., Siever, R., 2006. Understanding
Earth. W.H.Freeman. Basingstoke. Moore, I., Kokelaar, P., 1998. Tectonically controlled piecemeal
caldera collapse: A case study of Glencoe volcano, Scotland. Geological Society of America Bulletin. 110 (11), pp. 1448-1466
Riciptu, L.R., Johnson, C.M., Sawyer, D.A., Lipman, P.W., 1995. Crustal and magmatic evolution in a large multicyclic caldera complex. Journal of Volcanology and Geothermal Research. 67, pp. 1 – 28
Wilson, C.J.N., 2001. The 26.5ka oruanui eruption, New Zealand: an introduction and overview. Journal of Volcanology and Geothermal Research. 112, pp. 133 - 174