Chapter 8 Flashcards
(57 cards)
What makes an
how does magma work its way up the volcano?
By assimilation,
This make the magma volatile and silica rich
Within what distance is an explosion inevitable
2km of the surface
that’s the point when the pressure of overlying rock will become less than the pressure within the magma for most magma that has high silica/volatile composition
What happens as the magma gets closer to the surface?
at about 2 km depth, small crystals of various minerals begin to form, the liquid part of the magma is accordingly reduced a bit, and there are fewer opportunities for water to attach to silica – so bubbles of water begin to form. These little ‘balloons’ of water now race for surface, blow the top cap to bits – and a great explosive eruption begins.
The cool air right above the volcanic vent has suddenly been heated by the eruption and (since warm air is much lighter than cool air) helps to lift the fragmented rock + magma up into the atmosphere.
What is a Plinian eruption? Peléan eruption ?
A Plinian eruption is where the magma erupts from the top.
A Peléan eruption is where the magma erupts from the side.
Note that volcanoes always erupt from the wekest spots of the surface.
What is the ring of fire
The cascade range of Western North America is a sudbuction zone which has many volcanoes
What is the Juan de Fuca? What volcano best indicates the active volcanism in this area?
The only large strip of active subduction along the West Coast of North America, excluding Alaska.
The volcanoes are opposite the subducting plate.
Mt. Helens is a good indicator. Mt. Baker in Washington, visible from Canada, is another
What was done to predict Mount Helens’ eruption
Washington 1980
In 1975 three geologists working for the US Geological Survey wrote a report for Science noting that Mount St. Helens has the most extensive record of recent activity of any volcano in the continental US.
They said it was the most likely to erupt
Three years later, in 1978, two of them produced a detailed map of the areas at risk from ash and lahars (which we discussed under ‘hazards’ in the previous chapter).
People didn’t pay attention to the papers until 1980.
Explain what happened leading up to the Mount Helens eruption
On the 21st of March 1980 a magnitude 4.2 earthquake occurred beneath the volcano. Seismic activity increased rapidly, indicating that magma was on the move, and March 27th the first little eruptions of ash and gas were noted.
tilt-meters showed an enormous bulge developing on the north side, ballooning up and out at 1 m per day
It was obvious even to sightseers. By 12 May, the bulge had grown by 150 m.
Explain what happened just before the eruption (Mt. Helens)
On 18 May at 8:32 am two geologists flying over the volcano were horrified to witness the whole northern side of the volcano being to move (Fig. 5b), and the final stage began.
A magnitude 5.1 earthquake preceded an avalanche
What happened after the avalanche (Mt. Helens)
The avalanche essentially removed ‘the cork’, and the volcanic vent was cleared of overlying rock pressure, and threw pyroclastic material high into the atmosphere with a terrific blast (Fig. 5c and d); this was the Plinean phase of the eruption, and
the height of the column reached 20 km. The Plinean phase lasted about 9 hours.
What happened after the Plinean phase (Mt. Helens)
Because the side of the vent had also been opened by the slide, a lateral blast (the Peléan phase) of hot pyroclastic material and gases (nuée ardente) took place at the same time. It was moving at 1080 km/h
What happened after the inital blast (Mt. Helens)
Following the initial blast, pyroclastic flows continued to spill out of the volcano; they had temperatures of 300-370°C and moved at about 100 km/h. About 1 km3 of pyroclastic debris was blasted out by the volcanic eruption.
Within 10 minutes of the eruption’s start, the interaction of hot rock and snow + ice triggered lahars. The largest traveled 120 km down-stream.
How much lava and pulverized rock was ejected (Mt. Helens)
In all, Mount St. Helens tossed out 1 km3 of lava and pulverized rock, so it didn’t even come close to being a “world-class” catastrophe
Give background on Mount Mazama
It is a still-active subduction zone. Mount Mazama destroyed itself in a catastrophic eruption about 4860 BC. Prior to eruption it stood about 3350 m high and lost 1000 m off the top!
The total volume of magma expelled is estimated between 46 and 58 km3
Provide background on the surrounding lake (Mount Mazama)
Crater Lake is about 8 km wide and 600 m deep – making it the second deepest lake in North America (number 1 is Great Slave Lake in northern Canada).
Barring another large explosion the destruction of Crater Lake will likely occur when the water erodes the rim of the caldera (basin) resulting in a massive flood. We can predict that future eruptions will be confined to the caldera.
enough fine dust would have been blasted into the atmosphere that some portion of sunlight would be reflected back to space for many months, thus lowering global temperatures significantly.
Give background on Krakatau
1883
- Produced by the same subduction activity that produced the 2004 Sumatra-Java subduction and Indonesia earthquake and tsunami
Krakatau was a volcano built up from the sea floor rather than on land. It consisted of three cones on three closely grouped islands, but the central cone, Rakata, was the largest one.
In 535 AD Krakatau erupted massively – and the fine ash thrown into the atmosphere apparently reflected so much sunlight back into space that global climate cooled for 1 to 2 years. The records are really poor, however.
What happened leading up to the eruption (Krakatau)
For several years prior to 1883 there were reports of periods of intense seismic activity and small eruptions – mostly steam and ash – from Krakatau. Beginning 20 May 1883, steam vented out almost continuously, with a few interspersed periods of ash eruption. On 20 July, serious eruptions began; by 11 August 11 different vents were pouring out steam and ash
Provide some facts on the explosion’s effect on the island (Krakatau)
Four enormous explosions blew up the whole island, taking the rock level from 813 m above sea level to as much as 300 m below sea level.
Provide some facts on the noise produced (Krakatau)
The noise of this disintegration ranks as the loudest sound in historical time, and was heard clearly in Perth, Australia, 3100 km away. The air blast was recorded as it made 7 complete circles of Earth.
Provide some facts on the violence of the explosion (Krakatau)
The violence of this event was unmatched by any other in historical time; for example, it has been estimated at an explosive equivalent 13,000 times greater than the infamous Hiroshima hydrogen bomb.
Provide background on how much pyroclastic material was ejected (Krakatau)
About 25 km3 of pyroclastic junk was tossed as far as 50 km into the atmosphere. Within 13 days the dust circled Earth; global temperatures dropped 0.5°C over the next year. Within 5 years all the dust had fallen to the ground and the climate returned to normal.
Provide facts on the tsunami produced
within the confines of the Sunda Strait, waves attained heights of 37 m, wiping out 295 towns and villages, drowning 36,417 people, and destroying shorelines.
while there were reports of tsunami around the Pacific, they were likely not true tsunami but surface waves caused by the enormous pressure variations in the atmosphere.
Provide introductory facts on the Santorini in the Aegean Sea case study
In the Late Bronze Age the Mediterranean was pretty much dominated by the people called Minoans
Their main base was Knossos on the island of Crete, but their secondary base – occupied by the high society, principal leaders and nobility – was on a great volcano called Santorini.
The principal city was Akrotiri, the ruins of which appear now (mostly buried) on the island of Thera, the largest island remnant of Santorini; both Crete and Santorini are in the Aegean Sea (Fig.14). The Minoans were generally peaceful, wonderfully organized, and accomplished craftsmen