Chapter 8 Flashcards

(57 cards)

1
Q

What makes an

A
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2
Q

how does magma work its way up the volcano?

A

By assimilation,

This make the magma volatile and silica rich

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3
Q

Within what distance is an explosion inevitable

A

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

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4
Q

What happens as the magma gets closer to the surface?

A

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.

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5
Q

What is a Plinian eruption? Peléan eruption ?

A

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.

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6
Q

What is the ring of fire

A

The cascade range of Western North America is a sudbuction zone which has many volcanoes

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7
Q

What is the Juan de Fuca? What volcano best indicates the active volcanism in this area?

A

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

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8
Q

What was done to predict Mount Helens’ eruption

A

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.

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9
Q

Explain what happened leading up to the Mount Helens eruption

A

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.

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10
Q

Explain what happened just before the eruption (Mt. Helens)

A

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

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11
Q

What happened after the avalanche (Mt. Helens)

A

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.

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12
Q

What happened after the Plinean phase (Mt. Helens)

A

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

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13
Q

What happened after the inital blast (Mt. Helens)

A

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.

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14
Q

How much lava and pulverized rock was ejected (Mt. Helens)

A

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

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15
Q

Give background on Mount Mazama

A

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

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16
Q

Provide background on the surrounding lake (Mount Mazama)

A

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.

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17
Q

Give background on Krakatau

A

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.

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18
Q

What happened leading up to the eruption (Krakatau)

A

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

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19
Q

Provide some facts on the explosion’s effect on the island (Krakatau)

A

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.

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20
Q

Provide some facts on the noise produced (Krakatau)

A

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.

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21
Q

Provide some facts on the violence of the explosion (Krakatau)

A

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.

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22
Q

Provide background on how much pyroclastic material was ejected (Krakatau)

A

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.

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23
Q

Provide facts on the tsunami produced

A

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.

24
Q

Provide introductory facts on the Santorini in the Aegean Sea case study

A

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

25
What happened with the eruption (facts plis)
About 1600 BC the Santorini volcano erupted 60 km3 of pyroclastic material (second largest ever) (the largest was 100 km3 from Mount Tambora in Indonesia in 1815) the roof and rim of the volcano magma chamber caved in, creating what’s called a collapsed caldera, letting in the sea, and the resultant explosion set of a tsunami through the Aegean Sea This destroyed the Minoan civilization because everything they had was either in the shipping lines or in the harbours around the region – and that was destroyed. Not long afterward, the Mycenaean warriors arrived on the scene and readily defeated the last of the Minoans
26
Explain why Santorini is thought to be atlantis
About 350 BC, Plato wrote a couple of stories in which he described a wonderful city called Atlantis that suddenly sank into the sea one day One stumbling block has always been that Plato said Atlantis was “beyond the Pillars of Hercules”, which was Gibraltar, placing the lost city in the Atlantic Ocean. So it appears that Atlantis is modeled after Santorini
27
Mount Vesuvius background info
5 February AD 62, an earthquake jolted what is now Naples Many buildings in Pompeii were destroyed For the next 16 years, small earthquakes struck the area, but were not associated with the volcano The story was recorded by Pliny the Younger, with help from the records of his father, Pliny the Elder
28
Tell the story of Mt. Vesuvius
At about 1 pm on 24 August 79 AD, from their vantage point across the Bay of Naples at Misenum, the Pliny family noted a curious large cloud developing above Mount Vesuvius It was for the meticulousness of his descriptions that this phase of an eruption is called a Plinian eruption The Elder sailed to Stabiae to pick up some people, found them extremely frightened and, to calm them, had them organize a great meal and get the baths going. the Younger stayed back Back in Misenum, The Younger kept a record of waht happened (the ash, eruption, **darkness**, etc)
29
What happened to Herculaneum
Herculaneum was the first to be destroyed, by lahars (20 m deep) The lack of remains indicates that people must have evacuated (but still died at the beach) It was buried in a matter of minutes Only some 40,000 m2 of Herculaneum has ever been excavated; in time, another town (Ercolano) was built on top of the buried one
30
What happened to Pompeii
Pompeii was 9 km downwind from the volcano It was buried very quickly under 3 m of ash no one ever attempted to dig anything out, to recover anything or any bodies in 1595 a few coins and fragments of a marble tablet were dug up at an excavation site for a new aqueduct, baering the name Pompeii Instead of preserving the treasures below they were pillaged by wealthy collectors, such as the British ambassador to Naples Gradually, in the 19th Century, more order was maintained, and, although too late for almost the whole city, some parts were studied properly
31
What happened after this eruption
Vesuvius continued to blow. It apparently blew about 650 BC, 79AD, 203, 472, 512, 685, 993, 1036, 1049, 1138; it waited until 1631 to awake again, destroying 6 towns. The final gasps of that sequence seem to have been about the 1890s should the volcano reactivate again, several hundreds of thousands live too close
32
What is Campi Flegrei and its history, what it is now
A region that consists of a number of volcanic rings and cones within a 13 km diameter crater Known eruption times in the ancient past are: 47,000 years ago, 36,000, 15,000- 9500, 8600-8200 and 4800-3800 histrorical eruptions: 1158 and 1538 Naples sits on the old crater floor, where you can see the ridges of a major Plinian eruption (4400 years ago)
33
Where can mantle plumes develop and what effect do they have on temperature
They can form anywhere (they are deep beneath the crust) The cores may be about 300°C hotter than surrounding rocks, but the edges are only some 100°C or so hotter than the background temperature. Even that relatively small difference is enough to reduce viscosity and initiate magma flow
34
Two points to describe Hawaiian eruptions
- mantle plume - very benign
35
How long have Hawaiian volcanoes been around
Some 75 million years ago the first eruptions took place over that plume The first island gradually built up from the sea floor. As the surface approached sea level – but was still below – it was called a seamount Over time, as the Pacific Plate drifted over the mantle plume, a string of volcanic islands was formed
36
What happened to the Pacific plate in its development
About 43 million years ago, the direction of drift of the Pacific Plate changed reflected by a ‘dog’s leg’ pattern change in the string of islands n fact, the earliest volcanic islands formed (named the Emperor Islands) are now starting down the subduction zone to the north called the Aleutian Trench
37
What happened as they moved off the mantle plume
Having moved off the mantle plume, the volcanoes lost their magma feed and began to weather and erode away. As they fell below sea level, they again were called seamounts.
38
Describe the progression in composition of the lava
In the beginning, it is pure basalt Over time, assimilation happens and the lava cahnges in composition Now, the composition of magma erupting at Kilauea is not equivalent to MORB – it’s more properly called alkali basalt to reflect the small modification in composition.
39
Describe the process of magma rising up Mauna Loa, on the mainland
magma rises from the hotspot on the top of the plume into a shallow magma chamber at about 3-6 km depth, then rises from there along individual vents or fissures to surface Small earthquakes will also occur as a result
40
Describe one of the only cases where there wre fatalities from a Hawaiian eruption
there are only one or two rare cases where people were killed by an eruption in Hawaii. In 1790, as members of King Keoua's army were traveling past Kilauea, a sudden eruption of gases developed into something called a 'ground surge', in which a hurricane-like wind carried the hot gasses directly from the vents through the adjacent valley.
41
Describe what happens when a giant resurgent caldera appears under a continent
Like with one under an ocean (Hawaii) they constantly spew lava. With continental calderas, the lava gets stored and builds up That goes on for the life of the mantle heat plume – which we already know is 100 million years or maybe even 200 million years.
42
Why does the lava get stored with the continental mantle plume
It must break through the crust, assimilating, which increases explosion risk, just like with subduction zone volcanoes
43
Describe the process of a giant resurgent caldera eruption
Once a mantle heat plume is established and viscous rhyolitic magma forms in the hotspot The land bulges At some point the upward pressure of that magma becomes greater than the confining pressure of the surrounding rocks A plinean eruption occurs
44
Describe what type of magma is spewed out in order
Rhyolitic (with inital explosion) middle-chamber less-modified andesitic magma follows only unmodified basalt concludes the eruption stages
45
Describe the Yellowstone National Park volcano
Volcanic rocks first appeared from this plume/hotspot about 17 million years ago in the northeastern part of Nevada North American plate migrated to the southwest over the stationary plume The caldera dated more recently than 11 mya
46
What is the Snake River Plain
the broad, rather featureless arcuate depression that extends across southern Idaho is the Snake River Plain started at about 11 mya and finishing about 700,000 years agp
47
Why does the snake river plain consist mainly of basalt sequences
After the magma chamber has been emptied, there’s a channel open for partial melt magma of basalt composition to come roaring straight up through the existing plumbing
48
why is the North American plate moving southwest at all?
it started as the bulk of the Farallon plate was subducted under California and the transform San Andreas came into being. during the time of the Farallon subduction, the western edge of the North American plate was under compression – thus it shortened by building great mountain ridges inland but more or less parallel to the coast. The land has been "relaxing" allowing great extension of the lithosphere in a so-called ‘basin and range’ type of structure
49
How fast is the North American plate moving
way back at Yellowstone, the motion is really slow: about 4.5 mm per year (slower than it used to be)
50
What is the explosive history of Yellowstone
Right now the site of Yellowstone is - by far - the largest heat flow anomaly in the US Three enormous eruptions have occurred at Yellowstone * 2 million years ago (volume erupted: 2200 17 km3) * 1.3 million years ago (volume erupted: 280 km3) * 600,000 years ago (volume erupted: 1000 km3)
51
What is the explosive period of yellowstone
explosive period as about once every 650,000 years
52
Is the volcanic activity going to stop soon?
There’s no signal that activity at Yellowstone is abating. The last eruption threw tephra as far as present-day Louisiana
53
How much activity has there been in the last 600,000 years
in the last 600,000 years the volcano has erupted another 1000 km3 in dribs and drabs, equaling the amount discharged during the 3rd major eruption During the past 150,000 years, extensive flows of rhyolite have buried much of the Yellowstone basin The youngest lavas erupted in the park only about 70,000 years ago a large reservoir of hot magma again exists at shallow depth beneath the park
54
How long does it take for an ash flow holocaust to occur
Judging by the last three eruptive cycles, it took from about 200,000 to 600,000 years to generate the magmas needed for an ash flow holocaust.
55
What do we know about future rhyolite eruptions, what don't we know
We can't tell whether rhyolite eruptions of the last 150,000 years represent the end of the third caldera-forming cycle or a significant precursor of the fourth Evidence suggests that Yellowstone's thermal frequent earthquakes suggest that fresh magma has been injected into Yellowstone's magma reservoir since the last eruption
56
What is under Old Faithful
seismic evidence shows there to be a very large body of rhyolitic magma sitting some 5-10 km under Old Faithful 35 years ago, you could comfortably walk over the ground. Now, it is too hot
57
Explain the current prediction of the Yellowstone caldera volcano
First, there will be a series of small to moderate eruptions the Yellowstone volcano will eventually stage another caldera-forming cataclysmic eruption that could reduce large areas of western North America to a rhyolite desert This will be the most catastrophic event humans have ever witnessed much of the USA would be wiped out (most people, most industry, most agriculture) by lava flows and pyroclastics, affecting the rest of the world as well.