GeologyIgneous Rocks and VolcanoesHS-ESS3-1

Volcanic Hazards and Monitoring

Pyroclastic flows, lahars, ash, gases and lava each threaten in their own way; swelling ground, gas and small earthquakes can give warning.

Not started Jump to practice

Eruption styles explain how volcanoes erupt. To protect people, scientists also need to know what each eruption does to the land around it, how far each hazard can reach, and how to tell when a volcano is waking up.

  • Pyroclastic flows: avalanches of hot ash, rock and gas, hundreds of degrees Celsius, racing downhill often faster than 80 km/h. They are the deadliest volcanic hazard.
  • Lahars: volcanic mudflows of water, ash and rock that flow down river valleys like wet concrete, sometimes tens of kilometers from the volcano. Melting snow, heavy rain or a burst crater lake can start them, even without an eruption.
  • Ash fall: fine particles of rock and glass, heavy when wet, that collapse roofs, ruin crops and damage jet engines far downwind.
  • Volcanic gases: sulfur dioxide makes acid rain and haze; carbon dioxide, heavier than air, can pool in low places.
  • Lava flows: usually slow enough to walk away from, but they bury whatever they reach.

Why it works

Hazards follow physics. Hot flows are denser than air, so gravity drives them down valleys; that is also where lahars go, because they are mostly water. Wind decides where ash falls. Monitoring works because magma has to make room for itself as it rises: it pushes the ground up (swelling measured by GPS and tilt meters), cracks rock (swarms of small earthquakes), and releases gas as the pressure falls (more sulfur dioxide).

Key idea

Each hazard reaches a different distance: pyroclastic flows and lava near the volcano, lahars far down river valleys, ash far downwind. Swelling ground, small earthquakes and changing gases warn that magma is moving.
Hazard zones around a composite volcano: flows follow the valleys, and ash falls downwind.

Worked examples

Worked example: How much warning?

A lahar races down a valley at 30 km/h. How long until it reaches a town 45 km away?
  1. Time = distance ÷ speed $= 45 \div 30 = 1.5\,\text{h}$, or 90 minutes.
  2. In 1985, lahars from Nevado del Ruiz in Colombia took roughly two and a half hours to reach Armero, about 74 km away, and killed more than 20,000 people. Today, lahar warning systems give towns time to move to high ground.

Answer: 90 minutes.

Worked example: Reading swelling ground

GPS shows the ground on a volcano rising 9 cm in 3 months. At that rate, how much in a year?
  1. $9 \div 3 = 3\,\text{cm per month}$.
  2. $3 \times 12 = 36\,\text{cm}$ in a year: a strong sign that magma is collecting below.

Answer: $36\,\text{cm}$.

Common mistake

It is tempting to think a volcano that has been quiet for centuries is dead. Many dangerous volcanoes rest hundreds or thousands of years between eruptions. Mount Pinatubo in the Philippines had been quiet for about 500 years before it erupted in 1991, one of the largest eruptions of the 20th century; monitoring gave enough warning for large evacuations. Check the record, not the calendar: a volcano that erupted in the last 10,000 years is generally treated as active.

Practice

Pass with 3 right answers, the last 2 in a row. Each right answer earns 2 XP.

Loading practice…

Builds on

Leads to

This is one of the top rungs of Geology.

Sources and further reading

  • USGS Volcano Hazards Program, volcano hazards and monitoring
  • NGSS HS-ESS3-1 (nextgenscience.org)
@teddyrookbook GitHub