Mount Etna Eruption: What is a Volcano and How do they erupt? (Indian Express)
- 15 Nov 2023
Why is it in the News?
- Mount Etna, Europe's tallest and most active volcano, erupted again on the island of Sicily on Sunday, November 12, 2023.
- The eruption sent a lava fountain into the air and ash miles into the sky.
- The ash fell on the nearby city of Catania, causing some disruption to air travel.
About Mount Etna:
- Mount Etna is a large stratovolcano on the eastern coast of Sicily, Italy.
- It is the highest and most active volcano in Europe, and one of the most active in the world.
- Its recorded volcanic activity dates back to 1500 B.C. Since then, it has erupted more than 200 times.
- Mount Etna is a complex volcanic system, made up of several different lava domes and craters.
- The summit crater, known as the Voragine, is a large depression that is often filled with lava.
- The volcano also has several calderas, which are large, sunken depressions that are formed by the collapse of the volcano's summit.
- In recent years, Mount Etna has become increasingly active, with several eruptions in the past decade. The most recent eruption began in 2022 and has produced a number of lava flows and ash clouds.
- The eruption has also caused a number of earthquakes, some of which have been felt in nearby towns and cities.
Other volcanoes erupt for much longer than Etna:
- One of the most famous long-term eruptions was the Kilauea volcano in Hawaii.
- Its spewing spree in 1983 continued — almost nonstop — for 35 years until 2018, only to start again in 2021. The eruption is still ongoing.
- Dukono in Indonesia started erupting in August 1933 and is still continuing.
- Santa Maria in Guatemala began erupting in June 1922 and continues to this day.
- Yasur in Vanuatu first rumbled to life in about 1270 (± 110 years) and as of June 2023, was still erupting.
- Lava domes: Lava domes are formations created by the slow extrusion of viscous lava, typically rhyolitic or andesitic, forming a steep-sided mound or dome-shaped structure near a volcano's vent.
- Crater: A volcanic crater is a bowl- or funnel-shaped depression that usually lies directly above the vent from which volcanic material is ejected.
What is a volcano?
- Volcanoes are openings, or vents where lava, tephra (small rocks), and steam erupt onto the Earth’s surface.”
- Volcanoes can be on land and in the ocean.
- They are, in part, a result of their own eruptions but also the general formation of our planet, as tectonic plates move.
- Mountain ranges like the Andes in South America and the Rockies in North America, as well as volcanoes, formed through the movement and collision of tectonic plates.
- How do volcanoes erupt?
- Essentially, it’s a case of magma, or molten rock, below the surface of the Earth, bubbling up, rising, and overflowing, like boiling milk out of a pot on a stove.
- The magma finds its way to vents in the volcano and gets spewed across the land and into the atmosphere.
- When magma erupts from a volcano, it is called lava.
- There are four main types of volcanoes:
- Cinder cones
- Composite or stratovolcanoes
- Shield volcanoes and
- Lava domes
- Their type is determined by how the lava from an eruption flows and how that flow affects the volcano, and, as a result, how it affects its surrounding environment.
- Each volcano is unique and can vary in size and composition, but a crucial aspect of these mountains is the amount of silicon dioxide present in the magma and rocks below the surface.
- A high silica content can lead to violent eruptions that are categorized as explosive.
- Silica makes magma preventing it from readily flowing.
- Eruptions such as Alaska’s Novarupta in 1912 and Washington’s Mount St. Helens in 1980 all were composed of high amounts of silica.
- When silica values are low, eruptions are categorized as effusive with magma that is thinner and tends to be less explosive.
Types of Volcanoes:
- Cinder Cones: Cinder cones are considered to be the most common and simplest type of volcano in the world.
- Their structures are typically small, so their footprint doesn’t cover much terrain.
- Many are considered by volcanologists to be monogenetic and only erupt once during their lifespan.
- Once a cinder cone volcano becomes dormant, it usually never erupts again.
- Composite Volcanoes: Composite volcanoes are some of the largest and the most picturesque of any mountain in the world.
- Eruptions can be explosive and produce devastating impacts.
- Unlike a cinder volcano, composite volcanoes are usually active over a period of thousands of years.
- Mount St. Helens, Krakatoa, Mount Pinatubo, and Hunga-Tonga-Hunga-Ha’apai are all considered to be composite volcanoes, which also can be known as stratovolcanoes.
- The last significant composite volcano eruption was in Tonga in early 2022.
- Shield Volcanoes: This type of volcano is typically the largest on Earth and covers a broad swath of terrain.
- Hawaii’s Mauna Loa and K?lauea are classic examples of shield volcanoes and are among the most active in the world.
- Mauna Loa, from the sea floor base to its top elevation, is more than 33,000 feet tall.
- The great width of these volcanoes is a result of thin lava flows.
- Eruptions are not considered to be eruptive and usually rank low on the VEI.
- Threats from landslides and volcanic smog are usually significant with these types of volcanoes.
- Lava Domes: Lava dome features are usually quite small and due to thick magma, the lava doesn’t have wide impacts.
- These types of volcanoes can be explosive and are frequently found in the craters of composite volcanoes.
- Domes tend to grow from material that builds up over time by hardening lava from eruptions.
- Explosive eruptions can occur with little warning, which makes these features dangerous, if in the immediate area.
Volcanoes that are particularly active in the Pacific Ring of Fire:
- Some of the most active volcanoes are located in the Pacific Ring of Fire, which includes New Zealand, Southeast Asia, Japan, and the western coast of the Americas.
- About 90% of all earthquakes worldwide strike within this region.
Can scientists predict volcanic eruptions?
- Scientists are capable of predicting volcanic eruptions hours, or sometimes several days, in advance.
- This is not the case with earthquakes, which are much harder to predict.
- Scientists use seismographic data from earthquakes and other tremors, because those can be a precursor to volcanic eruptions.
- They monitor the ground for signs of deformation, which may be caused by the movement of magma.
- They also take readings of volcanic gas emissions, and changes in gravity and magnetic fields.