Sicily

An island still being built

Sicily is not finished. The volcano changes height, the coast changes colour, and two units of geological time are named after a city here.

The mountain has no fixed height

Etna's height is a measurement with a date on it, not a number.

The record keeps moving between craters. The North-East Crater held it through the eighties and then lost metres to rim collapse. The South-East Crater took it after some fifty paroxysms beginning in February 2021. In the summer of 2024 the Voragine's eastern rim rose by around a hundred metres in three weeks and took it back. Published figures are quietly corrected afterwards, as the surveys are reworked.

Etna's recorded summit height, by crater and survey date
DateCraterHeightHow it was measured
February 1981North-East Crater3,350 mSurvey after that winter's paroxysms
2018North-East Crater3,326 mSame crater, after decades of rim collapse
July 2021South-East Crater3,357 m ± 3 mPléiades satellite imagery
September 2024Voragine3,403 mINGV drone survey, current record
The summit from the air, and the flank underfoot.

So the durable sentence is that the mountain is re-surveyed after every major sequence. The current record, 3,403 m at the Voragine, is only as good as its September 2024 date — whatever number replaces it will have one too.

Living under it

In 1669 lava from vents near Nicolosi ran for a hundred and twenty-two days, threw up the Monti Rossi cone on the way, and reached Catania's walls in April. The walls held it about a fortnight before it began climbing over them. It filled the moat of the Castello Ursino and buried the lower ten metres of the building, then pushed the shoreline out some eight hundred metres.

A cinder cone on the upper slopes, its shoulders stained yellow where the gas comes out. Monti Rossi, above Nicolosi, was thrown up the same way in 1669.

The castle was built on the sea. It now stands inland, and the distance is walkable. That is the eruption's real memorial — not a ruin, but a changed map.

Contemporary accounts record no deaths from the flow itself. The figures of ten and twenty thousand that still circulate were invented later.

Mascali went in 1928, over roughly a day and a half. The evacuation was orderly enough that families took out their furniture and their window frames first. The government rebuilt the town on a grid, and it was finished by 1937.

Ash is the ordinary version, and it is a municipal matter rather than a spectacle. When the summit throws it, the comuni issue an ordinance: speed limits down, two-wheelers off the roads, residents to bag the fall and not hose it into the drains, because it sets. In a single week of August 2026, more than six hundred of Catania's scheduled flights were cancelled.

Old lava at the city walls, and new lava on the summit.Maurizio Moro5153 · CC BY-SA 4.0 · Wikimedia Commons

What grows on a volcano

Volcanic ash weathers into andosol — light, porous, holding water and air at the same time. It makes up about one per cent of the world's land surface, and only ever forms where a volcano has been.

Two things follow. Phylloxera never took hold in the sand, because loose grains will not hold the galleries the insect needs, so ungrafted vines survive on this mountain that died almost everywhere else in Europe. And Etna DOC, granted in 1968 and the first in Sicily, now maps a hundred and forty-two contrade much as Burgundy maps its climats. The vines are alberello, free-standing bushes no machine can work, planted from 450 metres to past a thousand. Lapilli fall on them in summer.

Bronte pistachios are grafted onto wild terebinth, whose roots force down into fissures in the lava. They crop in odd years only; in the even year the flower buds are stripped so the tree rests. Ten years before a graft bears, then two or three centuries of life, and never more than about five metres tall. Every stage is done by hand, because the terraces are too steep and too stony for anything else.

Blood oranges are red for a reason that is local in the strict sense. A jumping stretch of DNA sits beside the gene that switches on the red pigment, and cold nights switch on the jumping stretch. Plant the identical cultivars in Florida or Brazil and the fruit comes up orange.

Three things that only work here, and one of them only in odd years.Etnawinegirl · CC BY-SA 4.0 · Wikimedia CommonsPaolo Galli · CC BY-SA 3.0 · Wikimedia CommonsHalibutt · CC BY-SA 3.0 · Wikimedia Commons

The other mountains

The Peloritani, the Nebrodi and the Madonie run west from the strait as one chain, mountain for most of the north coast's length. The motorway crosses them on viaducts and through tunnels, because the strip of land below is too narrow to hold it, and villages sit high above their own beaches on roads that switchback down to the water.

Thirty wild Sicilian firs are left. Abies nebrodensis grows on scree in the Madonie, across an area smaller than two square kilometres, and only twenty-four of the thirty set fertile seed. The species was thought extinct until 1957.

The Madonie park holds more than half of all Sicilian plant species. Next door, the Nebrodi carry more than ten thousand hectares of beech above 1,200 metres, at the southern edge of the tree's European range. Only Etna's own beech woods stand further south. Griffon vultures were gone from Sicily by the 1960s; birds brought from Spain bred here again in 2005.

Beech, limestone and scree — the part of Sicily that is not a coastline.Davide Mauro · CC BY-SA 4.0 · Wikimedia CommonsGilles San Martin · CC BY-SA 2.0 · Wikimedia CommonsMinoZig · CC0 · Wikimedia Commons

What the rock remembers

The Alcantara gorge is a lava flow that cooled against a river. Basalt cracks perpendicular to whatever surface cools it, so the walls came out as five- and six-sided columns; the river then cut back down through its own obstruction. The local names describe the patterns rather than the physics — catasta, a woodpile; arpa, a harp.

The faraglioni off Aci Trezza are the oldest volcanic rock in the Etna region, erupted underwater around half a million years ago, well before the mountain existed. Homer had Polyphemus throw them at Odysseus.

At Vendicari, lagoons and old salt pans take about a hundred and eighty bird species a year. What makes them matter is the geography: Malta is eighty kilometres south, and after Malta it is another three hundred to Africa.

Cooled lava, drowned lava, and the lagoons at the end of the island.Richard Allaway · CC BY 2.0 · Wikimedia Commonsgnuckx · CC BY 2.0 · Wikimedia CommonsEinaz80 · CC BY-SA 4.0 · Wikimedia Commons

Two units of geological time are named after one Sicilian city. The Messinian is named for Messina; the Zanclean for Zancle, which is what Messina was called first. The marker defining the base of the Pliocene is driven in at Eraclea Minoa, on the south coast. The white cliff at the Scala dei Turchi is that same Pliocene marl — the shells of plankton, laid down in ninety-six cycles you can count by eye.

This coast faces Africa and shows it: the marl burns white at midday, and the scirocco arrives here first, leaving red dust on the cars and yellowing the light. Away from the water the heat can go further than visitors expect — 48.8°C was recorded at Floridia, near Syracuse, on 11 August 2021, an extreme rather than an ordinary August afternoon.

The Scala dei Turchi. Every one of those steps is plankton — Pliocene marl, laid down in cycles you can count from the beach.Enrico Strocchi · CC BY-SA 2.0 · Wikimedia Commons

The islands

Stromboli has thrown bombs from its summit at intervals of minutes for as long as anyone has written it down — at least two thousand years, though the rock puts the present pattern nearer twelve hundred. Five hundred people live on it. Sailors called it the lighthouse of the Mediterranean and navigated by it.

The English word volcano comes from the island two along. The Romans took Vulcano for the chimney of the forge.

On Pantelleria the vines sit one to a hand-dug hollow, cut low, below the wind; UNESCO put the practice on its intangible heritage list in 2014. And Lampedusa, administered from Sicily, is not geologically Sicilian at all. It sits on the African shelf — 113 kilometres from Tunisia, 205 from the island that governs it.

Two of them Aeolian, one on the Sicily Channel rift, one on the African shelf.Norbert Nagel · CC BY-SA 3.0 · Wikimedia Commonskuhnmi · CC BY 2.0 · Wikimedia CommonsMario Squitieri · CC BY-SA 4.0 · Wikimedia CommonsPier B. · CC BY-SA 3.0 · Wikimedia Commons

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