It also gives us a scale of tectonic manipulation that was perhaps suggested in the past but not so nicely proven.
As mentioned, this bit of tectonic good luck will give us a pretty exact understanding, comparable to ordinary volcanoes, of the genesis of super volcanoes. Thus our modeling will have credence.
This luck should not be underestimated. We have one such in the North American Plate and that will eventually go extinct. I know of one other in Sumatra and that is it. They are simply not common at all. So getting one cut and laid out for inspection is a lousy bet.
I grabbed a list from Wikipedia and it adds a bit. We can include North Island in New Zealand. I also think that the other Idaho events on the list are all part of the Yellowstone event which is migrating eastward as is perhaps North Island. So we have three VE8’s known to science. I suspect that we must have another one in Alaska that is unrecognized. The rest are simply extinct if they are recognized at all.
Scientists find “Rosetta Stone” of supervolcanoes in Italian Alps
September 22nd, 2009
WASHINGTON - A team of scientists has found the “Rosetta Stone” of supervolcanoes, in the form of a fossil supervolcano in the Italian Alps’ Sesia Valley.
A team led by James E. Quick, a geology professor at Southern Methodist University, US, found the fossil.
The discovery will advance scientific understanding of active supervolcanoes, like Yellowstone, which is the second-largest supervolcano in the world and which last erupted 630,000 years ago.
A rare uplift of the Earth’s crust in the Sesia Valley reveals for the first time the actual “plumbing” of a supervolcano from the surface to the source of the magma deep within the Earth, according to a new research article reporting the discovery.
The uplift reveals to an unprecedented depth of 25 kilometers the tracks and trails of the magma as it moved through the Earth’s crust.
Supervolcanoes, historically called calderas, are enormous craters tens of kilometers in diameter, which erupt hundreds to thousands of cubic kilometers of volcanic ash.
Their eruptions are sparked by the explosive release of gas from molten rock or “magma” as it pushes its way to the Earth’s surface.
Supervolcanoes have spread lava and ash vast distances and scientists believe they may have set off catastrophic global cooling events at different periods in the Earth’s past.
Sesia Valley’s unprecedented exposure of magmatic plumbing provides a model for interpreting geophysical profiles and magmatic processes beneath active calderas.
The exposure also serves as direct confirmation of the cause-and-effect link between molten rock moving through the Earth’s crust and explosive volcanism.
“It might lead to a better interpretation of monitoring data and improved prediction of eruptions,” said Quick, lead author of the research article reporting the discovery.
Calderas, which typically exhibit high levels of seismic and hydrothermal activity, often swell, suggesting movement of fluids beneath the surface.
“We want to better understand the tell-tale signs that a caldera is advancing to eruption so that we can improve warnings and avoid false alerts,” Quick said.
Quick likens the relevance of Sesia Valley to seeing bones and muscle inside the human body for the first time after previously envisioning human anatomy on the basis of a sonogram only.
“We think of the Sesia Valley find as the ‘Rosetta Stone’ for supervolcanoes because the depth to which rocks are exposed will help us to link the geologic and geophysical data,” Quick said. (ANI)
Known super eruptions (from Wikipedia)
Lake Taupo, North Island, New Zealand - Oruanui eruption ~26,500 years ago (~1,170 km³)
Lake Toba, Sumatra, Indonesia - ~75,000 years ago (~2,800 km³)
Whakamaru, North Island, New Zealand - Whakamaru Ignimbrite/Mount Curl Tephra ~254,000 years ago (1,200-2,000 km³)
Yellowstone Caldera, Wyoming, United States - 640,000 years ago (1,000 km³)
Island Park Caldera, Idaho/Wyoming, United States - 2.1 million years ago(2,500 km³)
Kilgore Tuff, Idaho, United States - 4.5 million years ago (1,800 km³)
Blacktail Creek, Idaho, United States - 6.6 million years ago (1,500 km³)
La Garita Caldera, Colorado, United States - Source of the truly enormous eruption of the Fish Canyon Tuff ~27.8 million years ago (~5,000 km³)
The Lake Toba eruption plunged the Earth into a volcanic winter, eradicating an estimated 60% of the human population (although humans managed to survive, even in the vicinity of the volcano), and was responsible for the formation of sulfuric acid in the atmosphere. However the coincidental agreement in above sources about percentage value of extinction is contrary to differing estimates of human population size at that time.
Cross-section through Long Valley Caldera
VEI-7 volcanic events, less colossal but still supermassive, have occurred in the geological past. The only ones in historic times are
Tambora, West Nusa Tenggara, Indonesia - 1815 (160 km³)
Baekdu Mountain, China/North Korea - ~969 AD (96±19 km³)
Lake Taupo, North Island, New Zealand - Hatepe eruption ~181 C.E. (120 km³)
Kikai Caldera, Ryukyu Islands, Japan - ~6,300 years ago (~ 4,300 BC) (150 km³)
Campi Flegrei, Naples, Italy - 39280 years ago (500 km³)
Laacher See, Rhineland-Palatinate, Germany - ~12,900 years ago (~300 km³)
Aira Caldera, Kyūshū, Japan - ~22,000 years ago (~110 km³)
Reporoa caldera, New Zealand - 230,000 years ago (~100 km³)
Aso, Kyūshū, Japan - four large explosive eruptions between 300,000 to 80,000 years ago (last one > 600 km³)
Long Valley Caldera, California, United States - ~760,000 years ago (600 km³)
Valles Caldera, New Mexico, United States - ~1.12 million years ago (~600 km³)
Mangakino, North Island, New Zealand - three eruptions from 0.97 to 1.23 million years ago (each > 300 km³)
Henry's Fork Caldera, Idaho, United States - 1.3 million years ago (280 km³)
Walcott Tuff, Idaho, United States - 6.4 million years ago (750 km³)
Bennett Lake Volcanic Complex, British Columbia/Yukon, Canada - ~50 million years ago (850 km³)
Bruneau-Jarbidge, Idaho, United States - ~10-12 million years ago (>250 km³) (responsible for the Ashfall Fossil Beds ~1,600 km to the east)