Mount Etna: Europe's Biggest Volcano - A Comprehensive Guide, Exercises of Geology

Etna has impressive credentials. It is the biggest and tallest active volcano in Europe, over 3000m in height, and one of the most active volcanoes in.

Typology: Exercises

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4Catalyst April 2013
4
Stefania
Hartley
Where can you find pristine rock which
has never seen the sun, a fertile soil
for a vineyard, and ski slopes with a
sea view? Stefania Hartley tells us about Mount
Etna on the Italian island of Sicily.
Etna has impressive credentials. It is the biggest
and tallest active volcano in Europe, over 3000m
in height, and one of the most active volcanoes in
the world. It is a candidate for UNESCO‘s World
Heritage list.
Etna has been designated a Decade Volcano
by the International Association of Volcanology
and Chemistry of the Earth’s Interior. ‘Decade
volcanoes’ are 16 volcanoes deemed worthy of
particular study in light of their history of large,
destructive eruptions and their proximity to
populated areas.
The geology of Etna
Etna has several layers of solidified lava, ash
and pumice on its slopes and changes height
periodically, following an eruption.
Etna is a type of volcano known as a
stratovolcano. Other stratovolcanoes include
Vesuvius and Krakatoa. Most volcanoes have iron-
rich magma, but these three stratovolcanoes have
a high silica (silicon dioxide) content which makes
the magma more viscous. This means that the
lava covers a shorter distance before it solidifies
and gives stratovolcanoes a characteristic conical
shape with steep sides.
Mount Etna
Europe’s biggest volcano
Key words
volcano
geology
igneous rock
tectonic plates
Mount Etna is known
as in Sicilian dialect
Mungibeddu, ‘The
Mountain’. This
eruption occurred on
30 July 2011.
gnuckx
Panoramic view of snow-capped Etna rising out of the clouds
Etna erupting, seen from space in July 2001.
Sicily lies off the toe of Italy.
Leandro
NASA/GSFC
pf3

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Stefania

Hartley

W

here can you find pristine rock which

has never seen the sun, a fertile soil

for a vineyard, and ski slopes with a

sea view? Stefania Hartley tells us about Mount

Etna on the Italian island of Sicily.

Etna has impressive credentials. It is the biggest and tallest active volcano in Europe, over 3000m in height, and one of the most active volcanoes in the world. It is a candidate for UNESCO‘s World Heritage list. Etna has been designated a Decade Volcano by the International Association of Volcanology and Chemistry of the Earth’s Interior. ‘Decade volcanoes’ are 16 volcanoes deemed worthy of particular study in light of their history of large, destructive eruptions and their proximity to populated areas.

The geology of Etna

Etna has several layers of solidified lava, ash and pumice on its slopes and changes height periodically, following an eruption. Etna is a type of volcano known as a stratovolcano. Other stratovolcanoes include Vesuvius and Krakatoa. Most volcanoes have iron- rich magma, but these three stratovolcanoes have a high silica (silicon dioxide) content which makes the magma more viscous. This means that the lava covers a shorter distance before it solidifies and gives stratovolcanoes a characteristic conical shape with steep sides.

Mount Etna

Europe’s biggest volcano

Key words volcano geology igneous rock tectonic plates

Mount Etna is known as in Sicilian dialect Mungibeddu, ‘The Mountain’. This eruption occurred on 30 July 2011.

gnuckx

Panoramic view of snow-capped Etna rising out of the clouds

Etna erupting, seen from space in July 2001. Sicily lies off the toe of Italy. Leandro

NASA/GSFC

The thicker magma has another, more catastrophic effect too – it makes it difficult for trapped gases to escape from the magma chamber. Pressure builds up inside the magma causing periodic explosive eruptions. As part of the volcanic mountain suddenly gives way there is an explosion of hot gases and a rain of extremely hot large boulders, known as volcanic bombs, and finer ash called pyroclastic flow. Two clues that this have happened in the past on Etna include ‘graded beddings’ where larger rocks are found at the bottom with smaller rocks, dust and ash on the top, and pumice stones.

Magma or lava? When molten rock is under the Earth’s surface we call it magma; when it comes to the surface it is lava.

Pumice stone is so light that a piece 15 cm long can balance on a rolled up banknote. You can see the holes in the stone made by expanding gases.

Pumice is such a light rock that some samples can float on water. It is formed when super-heated, highly pressurised rock explodes violently out of the volcano. The unusual foamy structure forms because of rapid cooling and rapid depressurisation which happen at the same time. The depressurisation creates bubbles by lowering the solubility of gases including water and carbon dioxide which are dissolved in the lava. This causes the gas to come rapidly out of solution, like bubbles of carbon dioxide when a carbonated drink is opened. It cools quickly leaving large air bubbles which give it a low density. You may have used pumice to rub dead skin off the soles of your feet.

A brief history of Etna

Etna started its life as an underwater volcano during the Quaternary era, about 600 000 years ago. The area lies above the convergent plate margin where the African plate and the Eurasian plate meet. This causes the presence of other volcanoes (nearby in the volcanic Aeolian Islands, for example) and devastating earthquakes. Etna has experienced a variety of eruption styles and for some time has also had basaltic (iron-rich) lava. Since the 1970s more explosive eruptions known as ‘paroxysms’ have been observed, especially from the craters at the summit. These have included lava fountains and gas and ash columns.

Igneous rocks

Igneous rocks are rocks originating from magma or lava. Magma that cools down inside the Earth’s crust will cool down more slowly than if it was on the Earth’s surface. The rock thus formed is called intrusive and it typically contains large crystals because the crystals have had time to grow. If, instead, the magma comes out to the surface (where it is now called lava) it will cool down more quickly. Such extrusive rock will have small crystals as the crystals will not have had time to grow much before the rock solidified. If magma is rich in iron it will be less viscous than the silica-rich magma typical of Mount Etna. The table shows the types of igneous rock which are typical of these different conditions.

Robert DuHamel

An erupting hornito on Etna seen from behind in November 2006. Hornitos (from the Spanish ‘little oven’) are small cones formed on the surface of a basaltic lava flow when the lava is forced up through an opening and accumulates around it.

Iron-rich Silica-rich Intrusive Gabbro Granite Extrusive Basalt Rhyolite

desmoheart

Rock samples for sale in a tourist shop near Mt Etna

Giorgio Hartley