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The Calabrian area shows basement (crystalline and metamorphic rocks) of Paleozoic and younger ages, covered by (mostly Upper) Neogene sediments.Studies have revealed that these rocks comprise the upper Unit of a pile of thrust sheets which dominate the Apennines and the Sicilian Maghrebides.).This subduction system therefore shows the southern plates of African affinity subducting below the northern plates of European affinity.presented a complete bibliography of the literature on the Calabrian geology as published up until that moment.Mountain areas have a typical mountainous climate with frequent snow during winter.Erratic behavior of the Tyrrhenian Sea can bring heavy rainfall on the western slopes of the region, while hot air from Africa makes the east coast of Calabria dry and warm.

The Mediterranean climate is typical of the coastal areas with considerable differences in temperature and rainfall between the seasons, with an average low of 8 °C (46 °F) during the winter months and an average high of 30 °C (86 °F) during the summer months.

The main tectonic elements of the Calabrian Arc are the Southern Apennines fold-and-thrust belt, the "Calabria-Peloritani", or simply Calabrian block and the Sicilian Maghrebides fold-and-thrust belt.

The foreland area is formed by the Apulia Platform, which is part of the Adriatic Plate, and the Ragusa or Iblean Platform, which is an extension of the African Plate. The Tyrrhenian oceanized basin is regarded as the back-arc basin.

It is separated from Sicily by the Strait of Messina, where the narrowest point between Capo Peloro in Sicily and Punta Pezzo in Calabria is only 3.2 km (2 mi).

Three mountain ranges are present: Pollino, La Sila and Aspromonte.

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In general, most of the lower terrain in Calabria has been agricultural for centuries, and exhibits indigenous scrubland as well as introduced plants such as the prickly pear cactus.

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