Sicily Geography

Sicily's shape — a rough triangle, which gave it the Greek name Trinacria — and its position in the narrows between Europe and Africa explain most of its history and all of its climate.

Structure

The island is separated from Calabria by the Strait of Messina, at its narrowest barely 3 km across. The north coast is backed by mountains — the Madonie and Nebrodi ranges, continuations of the Apennines, rising above 1,900 m and holding beech forest and snow in winter. The interior is a plateau of clay hills, historically the wheat country that made Sicily Rome's granary and later supported the vast latifondi estates. The south and west fall away to lower, drier ground and a long coastline.

Etna

Etna dominates the east at roughly 3,350 m — the height changes with each eruption. It is the most active volcano in Europe, erupting frequently but usually effusively rather than explosively, which is why towns sit on its flanks at all. Its slopes are exceptionally fertile: volcanic soils support vineyards to around 1,000 m, along with pistachios at Bronte and citrus lower down. The volcano also makes its own weather, catching cloud and holding snow into spring.

Water and its absence

Sicily has no major perennial river. Watercourses are fiumare — wide stony beds that flood briefly after rain and stay dry the rest of the year. Rainfall arrives almost entirely between October and March, and the summer is reliably dry. This is the central constraint on Sicilian agriculture and settlement: terracing, cisterns and the Arab-introduced irrigation systems of the citrus gardens all exist to manage it, and drought years still put inland towns on rationed supply.

The smaller islands

Three archipelagos belong to Sicily and none resemble it. The Aeolians to the north are volcanic, with Stromboli in near-continuous eruption. The Egadi lie off Trapani. The Pelagie to the south include Lampedusa, which is geologically part of Africa and closer to Tunisia than to Sicily.

Seismic risk

The island sits on the boundary where the African plate meets the Eurasian. The 1693 earthquake destroyed the south-east and the 1908 Messina earthquake and tsunami killed tens of thousands. Both events reshaped the built landscape: the Baroque of the Val di Noto and the low, regular grid of modern Messina are each a direct consequence.