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How Does a Volcano Work?
by Carolyn Collins
Petersen
Volcanic activity is a fascinating, frightening, and an absolutely
essential feature of our planet.
Volcanoes are scattered everywhere, from a desert in Africa to the frigid climes of
Antarctica, islands in the Pacific, and on all continents.
Every day one erupts somewhere.
Earth's volcanoes are familiar to most of us, such as the very active
Mount Agung in Bali, Bárðarbunga in Iceland, Kilauea in Hawai'i, and Colima in
Mexico.
However, there are volcanoes spread on worlds across the solar system.
Take Jupiter's moon Io, for example. It's highly
volcanic and spews sulfurous lava from beneath its surface. It's estimated that
this little world nearly turns itself inside out over millions of years due to
its volcanic activity bringing material from the interior to the surface and
beyond.
Farther out, Saturn's moon Enceladus
also has geyser features related to volcanism. Instead of erupting
with molten rock as on Earth and Io, it spews out slushy ice crystals.
Planetary scientists suspect that there is a lot more of this
"ice volcano" activity (known as cryovolcanism) spread throughout the
distant reaches of the solar system.
Much closer to Earth, Venus is known to be volcanically active, and
there's solid evidence of past volcanic activity on Mars.
Even Mercury shows the traces of volcanic eruptions very early in its
history.
Volcanoes Are Part of World Building
Volcanoes do major work in building up continents and islands,
fashioning deep-ocean mountains, and craters.
They also resurface landscapes on Earth as they spew out lava and other materials. Earth began
its life as a volcanic world, covered with molten ocean.
Not all volcanoes that have flowed since the beginning of time are
currently active. Some are long-dead and will never again be active.
Others are dormant (meaning they could erupt again in the
future). This is true on Mars, particularly, where a few volcanoes exist
among evidence of their active past.
Volcanic Eruption Basics
Most people are familiar with volcanic explosions like the one that
blew apart Mt. St. Helens in Washington State in 1980.
That was a dramatic eruption that blew part of the mountain away and
showered billions of tons of ash on surrounding states.
However, it's not the only one in that region. Mt. Hood and Mt.
Rainier are also considered active, although not as much as their sister
caldera.
Those mountains are known as "back-arc" volcanoes and their
activity is caused by plate motions deep underground.
The Hawaiian island chain stems from a hot spot, a weak point in
Earth's crust under the Pacific Ocean. Eventually, each island's surface broke
the water's surface and kept growing.
The most active Hawaiian volcanoes are on the Big Island. One of them
— Kilauea — continues to pump out thick lava flows that have resurfaced much of
the south area of the island.
Recent eruptions from a vent on the side of that mountain have
destroyed villages and homes on the Big Island.
Volcanoes also erupt all along the Pacific Ocean basin, from Japan
south to New Zealand. The most volcanic areas in the basin are along plate
boundaries, and that whole region is called the "Ring of Fire".
In Europe, Mt. Etna in Sicily is quite active, as is Vesuvius (the
volcano that buried Pompeii and Herculaneum in 79 AD). These mountains continue
to affect surrounding regions with earthquakes and occasional flows.
Not every volcano builds up a mountain. Some vent volcanoes send
pillows of lava out, particularly from undersea eruptions.
Vent volcanoes are active on the planet Venus, where they pave the surface
over with thick, viscous lava. On Earth, volcanoes erupt in various ways.
How Do Volcanoes Work?
Volcanic eruptions provide routes for material deep beneath Earth's
surface to escape to the surface. They also allow the world to vent its heat.
Active volcanoes on Earth, Io, and Venus are fed by subsurface molten
rock. On Earth, the lava comes up from the mantle (which is the layer under the
surface).
Once there's enough molten rock — called magma — and enough pressure
on it, a volcanic eruption occurs.
In many volcanoes, the magma rises up through a central tube or
"throat," and emerges out the top of the mountain.
In other places, lava, gases and ash flow out through vents. They can
eventually create become cone-shaped hills and mountains. This is the
style of eruption that most recently occurred on the Big Island of Hawai'i.
Volcanic activity can be fairly quiet, or it can be quite explosive.
In a very active flow, clouds of gas may come rolling out of the volcanic
caldera.
These are quite deadly because they're hot and moving fast, and the
heat and gas and kill someone very quickly.
Volcanoes as Part of Planetary Geology
Volcanoes are often (but not always) closely related to continental
plate movements.
Deep under the surface of our planet, huge tectonic plates are slowly moving and
jostling against each other. At the boundaries between plates, where two or
more come together, magma creeps up to the surface.
The volcanoes of the Pacific Rim have been built up this way, where
plates slide together creating friction and heat, allowing lava to flow
freely.
Deep-sea volcanoes also erupt with magma and gases. We don't always
see the eruptions, but clouds of pumice (rock from the eruption) eventually
make their way to the surface and create long rock "rivers" on the
surface.
As mentioned earlier, the Hawaiian islands are actually the result of
what's called a volcanic "plume" underneath the Pacific Plate.
Here are some more scientific details about how that works: the
Pacific Plate is moving slowly to the southeast, and as it does, the plume is
heating the crust and sending material to the surface.
As the plate moves southward, new spots are heated, and a new island
gets built from molten lava forcing its way to the surface.
The Big Island is the youngest of the islands to rise above the
surface of the Pacific Ocean, although there's a newer one being built as the
plate slides. It's called Loihi and it's still underwater.
In addition to active volcanoes, several places on Earth contain what
are called "supervolcanoes." These are geologically active regions
that lie atop massive hotspots. The best known is the Yellowstone Caldera in
northwestern Wyoming in the U.S. It has a deep lava lake and has erupted
several times throughout geologic time.
A Scientific Look at Volcanic Eruptions
Volcanic eruptions are usually heralded by earthquake swarms. They
indicate the motion of molten rock beneath the surface.
Once an eruption is about to happen, the volcano can spew out lava in
two forms, plus ash, and heated gases.
Most people are familiar with the sinuous-looking ropy
"pahoehoe" lava (pronounced "pah-HOY-hoy"). It has the
consistency of molten peanut butter. It cools very quickly to make thick black
rock layers.
The other type of lava that flows from volcanoes is called
"A'a" (pronounced "AH-ah"). It looks like a moving pile of
coal clinkers.
Both types of lava carry gases, which they release as they flow. Their
temperatures can be more than 1,200° C.
The hot gases released in volcanic eruptions include carbon dioxide,
sulfur dioxide, nitrogen, argon, methane, and carbon monoxide, as well as water
vapor.
Ash, which can be as small as dust particles and large as rocks and
pebbles, is made of cooled rock and is flung out from the volcano. These gases
can be quite deadly, even in small amounts, even on a relatively quiet
mountain.
In very explosive volcanic eruptions, ash and gases are mixed together
in what's called a "pyroclastic flow." Such a mixture moves very fast
and can be quite deadly.
During the eruption
of Mt. St. Helens in Washington, the blast from Mount Pinatubo
in the Philippines, and the eruptions near Pompeii in ancient Rome, most people
died when they were overcome by such killer gas and ash flows.
Others were buried in the ash or mud floods that followed the
eruption.
Volcanoes are Necessary to Planetary Evolution
Volcanoes and volcanic flows have affected our planet (and others)
since the earliest history of the solar system.
They have enriched the atmosphere and soil, at the same time they have
posed drastic changes and threatened life.
They're part of living on an active planet and have valuable lessons
to teach on other worlds where the volcanic activity takes place.
Geologists study volcanic eruptions and related activities and work
to classify each type of volcanic land feature. What
they learn gives them more insight into the interior workings of our planet and
other worlds where volcanic activity takes place.
Carolyn Collins Petersen
Author/co-author of seven books on astronomy
and planetary science, including Astronomy 101 and Space
Exploration: Past, Present, Future
CEO of Loch Ness Productions, a production
company specializing in educational materials for planetariums and science
centers
Member of the American Astronomical Society
and International Planetarium Society
Experience
Carolyn Collins Petersen is a science writer,
producer, and former research astronomer. She is the CEO of Loch Ness
Productions, a production company specializing educational documentary shows
for planetariums and science centers. She has published 7 books on astronomy
and planetary science, including Astronomy 101, Space Exploration:
Past, Present, Future, and Hubble Vision.
In addition to her own books and articles on
astronomy, Carolyn has written exhibition texts for the Griffith
Observatory in Los Angeles, the NASA/Jet Propulsion Laboratory in Pasadena, and
the California Academy of Sciences in San Francisco.
Previously, Carolyn worked on a Hubble Space
Telescope instrument team and served as an editor for Sky Publishing, which
publishes Sky & Telescope and Skywatch. Carolyn has written
more than 40 documentaries and several webcasts on space science, and she
regularly gives public presentations and lectures on topics in astronomy.
Education
Carolyn earned a master's degree from the
University of Colorado – Boulder, where she studied astronomy, astrophysics,
and science communication. She also received her B.S. from the University of
Colorado.
Publications
Space Exploration: Past, Present, Future, 2017, Amberley
Books
Astronomy 101: From the Sun and Moon to Wormholes and Warp Drive, Key Theories,
Discoveries, and Facts about the Universe, 2013, Adams Media
Visions
of the Cosmos (with J.C. Brandt), 2005, Cambridge University Press
Hubble
Vision (with J.C. Brandt), 2003, Cambridge University Press (two
editions)
The
New Solar System (editor, with K. Beatty and A.C. Chaikin), 1999,
Cambridge University Press and Sky Publishing
Jupiter! 1989,
Facts on File.
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The Colima volcanoes in Mexico. These are
active, but currently quiet. |
The eruption of Mt. St. Helens on May 18,
1980 blew millions of tons of ash and gas into the air. It resulted in several
deaths,
catastrophic flooding, fires, the destruction of nearby forests and buildings, and scattered ash for hundreds of miles around. |
The
Hawaiian islands are the result of a hot spot that created each island as the
Pacific plate moved. Similar hotspots exist around the planet.
|
A pahoehoe
flow on the Big Island of Hawai'i. This is thick, ropy lava that almost acts
like a "pavement" on a landscape.
|
Supervolcanoes,
such as the one in Wyoming, underlie several places on Earth. They often have
active volcanoes, geyser and hot spring activity, and other volcanic features.
They're just one part of the larger volcano collection on planet Earth.
|
Mount
Vesuvius is an active volcano that buried the cities of Pompeii and Herculaneum
in 79 AD. Today, it towers over the metropolitan area of Naples, two hours away
from Rome in Italy.
|
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