A volcano on Earth is a vent or fissure in the planet's crust through which lava, ash, rock and gases erupt. A volcano is also a mountain formed by the accumulation of these eruptive products.
Volcanoes have existed for a long time on Earth, likely causing disasters such as the Permian mass extinction about 250 million years ago, the greatest mass extinction in Earth's history.
Volcanoes can and have existed on other worlds as well: although volcanoes on the moon and Mars have long been dormant, volcanoes are still very active on Jupiter's moon Io. Researchers are currently striving to find ways to predict when volcanic eruptions might happen on Earth by analysing clues such as crystals and gases linked with volcanoes.
What does dormant mean?
As if asleep for a long time.
Let's take a look at how volcanoes form on Earth.
The Earth's crust is 3 to 37 miles (5 to 60 kilometres) thick. It is broken up into seven major and 152 smaller pieces called tectonic plates (picture 1).
These plates float on a layer of magma — semi-liquid rock and dissolved gases. At the boundaries of these plates — where they move past, are pushed under, or move away from each other — magma, which is lighter than the surrounding solid rock, is often able to force its way up through cracks and fissures.
Magma can explode from the vent, or it can flow out of the volcano like an overflowing cup. Magma that has erupted is called lava.
Principal types of volcanoes
Cinder cone volcanoes (picture 2) also called scoria cones) are the most common type of volcano and are the symmetrical cone-shaped volcanoes we typically think of.
They may occur as single volcanoes or as secondary volcanoes known as “parasitic cones” on the sides of stratovolcanoes or shield volcanoes.
Airborne fragments of lava, called tephra, are ejected from a single vent. The lava cools rapidly and fall as cinders that build up around the vent, forming a crater at the summit.
Cinder cone volcanoes are fairly small, generally only about 300 feet (91 meters) tall and not rising more than 1,200 feet (366 meters). They can build up over short periods of a few months or years.
Stratovolcanoes (picture 3) are also called composite volcanoes because they are built of layers of alternating lava flow, ash and blocks of unmelted stone. They are larger than cinder cones, rising up to 8,000 feet (2,438 meters). Stratovolcanoes result from a conduit system of vents leading from a magma reservoir beneath the surface. When dormant, they typically have steep concave sides that sweep together at the top around a relatively small crater.
Stratovolcanoes can erupt with great violence. (Picture 4) Pressure builds in the magma chamber as gases, under immense heat and pressure, are dissolved in the liquid rock. When the magma reaches the conduits the pressure is released and the gases explode, like soda spewing out of a Pepsi can that you shook up and opened suddenly. Because they form in a system of underground conduits, stratovolcanoes may blow out the sides of the cone as well as the summit crater.
Stratovolcanoes are considered the most violent (Picture 4) . Mount St. Helens, in Washington state (picture 5), is a stratovolcano that erupted on May 18, 1980. Approximately 230 square miles (596 square kilometres) of forest was completely obliterated and 57 people were killed. Over the course of the day, winds blew 520 million tons of ash eastward across the United States and caused complete darkness in Spokane, Washington, 250 miles (402 kilometres) from the volcano. (Picture 6 - before and after)
Shield volcanoes (picture 7) are huge, gently sloping volcanoes built of very thin lava spreading out in all directions from a central vent. They have wide bases several miles in diameter with steeper middle slopes and a flatter summit. The gentle convex slopes give them an outline like a medieval knight’s shield. Eruptions of these volcanoes are not generally explosive, but are more like liquid overflowing around the edges of a container.
￼The world's largest volcano, Mauna Loa in Hawaii (picture 7), is a shield volcano. Mauna Loa is about 55,770 feet (17,000 meters) from its base beneath the ocean to the summit, which is 13,681 feet (4,170 metres) above sea level. It is also one of the Earth's most active volcanoes and is carefully monitored. The most recent eruption was in 1984.
Lava domes (picture 8) are built up when the lava is too viscous to flow. A bubble or plug of cooling rock forms over a fissure. This cooler, thick lava usually rises near the end of an explosive eruption and lava domes often form within the craters of stratovolcanoes. Mount St. Helens (in the picture) has several well-defined lava domes inside the crater, according to NASA.
Other volcanic landforms
Besides well-known symmetrical volcanoes such as Mount Fuji in Japan and Kilimanjaro in Tanzania, volcanic activity is responsible for several other distinctive landforms.
Calderas (picture 9): A caldera is a bowl-shaped depression formed when a volcano collapses into the void left when its magma chamber is emptied. There are three types, according to San Diego State University. The first type is a crater lake caldera. This is the result of a stratovolcano collapsing into its magma chamber during a violent eruption. Basaltic calderas have a concentric ring pattern resulting from a series of gradual collapses rather than a single event. They are often found at the summit of shield volcanoes such as the craters at the tops of Mauna Loa and Kilauea. Resurgent calderas are the largest volcanic structures on Earth. They are the result of catastrophic eruptions that dwarf any eruptions ever recorded by human beings. Yellowstone caldera, sometimes called a “super volcano”, is one example.
￼Volcanic plugs (picture 10): When magma solidifies in the fissure of a volcano the hard dense rock may form a "neck" that remains when softer surrounding rock has been eroded away, according to the U.S. Geological Survey. This can result in dramatic landmarks such as Ship Rock in New Mexico, and Devil's Tower in Wyoming.￼
Tuff cones (picture 11): also known as maars, tuff cones are shallow, flat-floored craters that scientists think formed as a result of a violent expansion of magmatic gas or steam, according to the U.S. Geological Survey. Maars range in size from 200 to 6,500 feet (60 to 1,980 meters) across and from 30 to 650 feet (9 to 198 meters) deep, and most are commonly filled with water to form natural lakes. Maars occur geologically young volcanic regions of the world such as the western United States and the Eifel region of Germany.
￼Lava plateaus (picture 12): Shield volcanoes may erupt along lines of fissures rather than a central vent spilling liquid lava in successive layers. Over time as these layers form broad plateaus such as the Columbia Plateau, according to the Encyclopedia Britannica. These plateaus are often cut by deep canyons that expose the layers of rock.
￼Volcanoes in history
A.D. 79: One of the most famous volcanoes is Mount Vesuvius (picture 13), which sits along the Bay of Naples in southern Italy. It has erupted dozens of times in the past 2,000 years. The A.D. 79 eruption, which buried Pompeii, made Vesuvius famous, but another eruption in 1631 killed about 3,000 people. (Pictures 14 & 15)
1669: In Sicily, Mount Etna sent a river of lava flooding through Catania killing some 20,000 people there and in the surrounding region.
1783: The eruption of Mount Skaptar in Iceland devastated farming and fishing, causing a famine that killed a quarter of the country's people.
1815: Whirlwinds and tsunamis from the eruption of Mount Tambora, on Sumbawa Island in Indonesia, killed at least 10,000 people. The volcano sent a cloud ejecta into the atmosphere that was more than four times the amount ejected by Mount Pinatubo in 1991, leading to the “Year Without a Summer” of 1816 in Europe and North America.
1883: Another Indonesian volcano, Krakatoa (picture 16), erupted in an explosion heard 3,000 miles away. Seventy-pound boulders landed on islands 50 miles away, and a 130-foot tsunami devastated hundreds of villages, including Java and Sumatra, according to San Diego State University. About 36,000 people died. Dust high in the atmosphere caused the moon to appear blue, and sometimes green, for two years, according to NASA.
1902: Mount Pelée, on the island of Martinique, smothered the town of Saint-Pierre in deadly gas and hot ash, killing 29,933.
1980: Mount St. Helens in Washington state (picture 8) blew 1,300 feet off its top, killing 57 people and causing a midday darkness in towns 85 miles away.
1991: After 600 years of dormancy, Mount Pinatubo (picture 17) in the Philippines rumbled for days before erupting and killing more than 840 people, according to the U.S. Geological Survey. The cataclysmic ejected more than 1 cubic mile (5 cubic kilometres) of material and buried a U.S. air base 15 miles away, according to the National Oceanic and Atmospheric Administration. Nearly every bridge within 18 miles (30 km) of Mount Pinatubo was destroyed, according to the U.S. Geological Survey.
Pinatubo’s cloud of sulphuric acid, some 20 million tons of it, climbed to more than 12 miles in the stratosphere. Over the next several weeks, the cloud encircled the equator and spread to the poles, covering the entire planet. The particles reflected sunlight and cooled the Earth by nearly a full degree Fahrenheit.