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  Earth Science News
During a volcanic eruption, molten rock rises from inside the Earth and flows out as lava, or blasts into the air as ash.
CreditDoukas, USGS
Guide to Reading

In this chapter the author explains that there are many possible manifestations of volcanic activity, and numerous variables to consider when trying to understand what has occurred or predict what will occur at some specific location. The nature of volcanic activity depends on the chemistry of the situation (chemical compositions, temperatures, and pressures) and the environment in which it's occurring (submarine or subaerial/not underwater).

There's lots of vocabulary to learn and many classification schemes to use. Keep reminding yourself that scientists establish classification schemes to organize data, discern patterns, and thus reach an understanding of why things happen as they do. Look for these patterns; make logical associations of such things as lava types, cone types, and styles of eruption. But be aware that volcanoes are the result of the interplay among so many factors they're not always perfectly predictable. They've been known to fool even the smartest volcanologists.

The chapter begins with discussion of the three types of volcanic products: lavas, pyroclastic debris, and gases. It continues with the vocabulary of volcanic structures: "magma chambers," "chimneys," "fissures," "craters," and "calderas." With these basic terms to build on, the author discusses the three basic types of cones (shield, cinder, and composite or stratovolcanoes), the differences between summit eruptions and flank eruptions, and eruptive styles (effusive and explosive).

Any history buff will feel right at home in this chapter because woven throughout it are accounts of historic volcanic eruptions that have affected human society, often in devastating fashion. Pay particular attention to the geographic locations of these eruptions; they're determined by plate tectonics. The phenomena of hot spots, mid-ocean ridges, convergent margins, and continental rifts reappear, this time with emphasis on their association with volcanic activity.

The chapter continues with societal issues:

    • What specifically are the dangers? (lava; ash, pumice, and lapilli falls; pyroclastic flows; blast; landslides; lahars; earthquakes; tsunamis; gas)
    • Can humans protect themselves and their property? (prediction and control)
    • How is climate affected?

This chapter will probably convince you that volcanoes are natural hazards that pose significant threats to humans and their property. The next chapter continues the theme of “humans beware!” It’s about earthquakes.

Key Terms
active volcanoes magma chamber
angle of repose obsidian
black smoker pahoehoe
caldera Pele’s hair
chimney Pele’s tears
cinder cones pillow lava
columnar jointing pumice
crater pyroclastic debris
dormant volcanoes pyroclastic flow (or nuée ardente)
effusive eruptions recurrence interval
explosive eruptions shield volcanoes
fissure silicic and rhyolitic
flank eruption stratovolcanoes (or composite cones)
flood basalts summit eruption
ignimbrite tsunamis
lahar tuff
lapilli or cinders vesicles
lava viscosity
lava dome volcanic ash
lava flow volcanic danger assessment maps
lava lake volcanic gas
lava tube volcano
mafic and basaltic