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Laboratory Manual for Introductory Geology 4e

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EXERCISE 5.15

Stratovolcano Disaster Case Histories (continued )

Name:

Course:

Section:

Date:

False-color satellite image showing Vesuvius and the Naples metropolitan

area (outlined in white).

Vesuvius

0 5 10 miles

0 5 10 km

II. Cascade Range, western North America [VEI 3–7]: The Cascade Range is a chain of stratovolcanoes that extends

from northern California to southern British Columbia. The range is being formed by the subduction of a small plate within

the Pacific Ocean (the Juan de Fuca Plate) beneath North America. Its prominent peaks include Mts. Rainier, Baker, Hood,

Shasta, Lassen (VEI 5 3), and St. Helens (VEI 5 5), as well as Mt. Mazama, the apparently extinct stratovolcano whose

eruption produced what is now Crater Lake (VEI 5 7).

Mt. St. Helens has been by far the most active of these peaks, and it and Mt. Lassen are the only peaks to have erupted

since 1900. In 2004, 24 years after its explosive 1980 eruption, Mount St. Helens erupted again, this time quietly, exuding

mostly viscous lava. In 2017, around the anniversary of the 1980 eruption, geologists detected several swarms of small

earthquakes beneath the mountain, similar to those that had preceded that eruption. Preliminary analysis suggests that

the earthquakes indicate magma rising from depth, but an imminent eruption is not anticipated.

Locations of major Cascade Range stratovolcanoes and their eruptive

histories over the past 4,000 years.

Eruptive history of Mt. St. Helens since

1400 c.e.

Pacific Ocean

Wash.

Oreg.

Calif.

Baker

Glacier Pk.

Rainier

St. Helens

Adams

Hood

Jefferson

Three Sisters

Newberry

Crater Lake

Medicine Lake

Shasta

Lassen

4000 2000

Years ago

0

200

2000

1900

1800

1700

1600

1500

Dome eruption

Ash fall 1 nuée ardente 1 lahars

Dormant interval

Dome eruptions 1 ash falls 1 lava

Ash falls 1 lahars

Dormant interval

Nuée ardente

Dome eruption 1 lahars

Dormant interval

Ash falls 1 nuée ardente

1400

Nuée ardente

(continued)

138 CHAPTER 5 USING IGNEOUS ROCKS TO INTERPRET EARTH HISTORY

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