カスティリオーネディシチリアでののおすすめランニングルート

What you see here are not the summit craters, but the northeast crater.

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Shelter temporarily closed Reopened at the end of October

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This is really a really beautiful spot!!

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Very cold water all year round. Very busy in summer. After rain in winter, the gorge is partially closed due to the risk of floods.

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Starting point for hikes into previous eruptions. Parking lot with supplies (toilet, souvenir, snack).

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Hiking in the area of previous eruptions is reminiscent of lunar landscapes. Simply magnificent.

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A bivacco with six places to stay overnight. It even has a water point

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The formation of the Alcantara riverbed can be traced back to around 300,000 years ago, although the current configuration of the river in the gorge section is mainly the result of the lava flows that occurred in the last 8,000 years. The interaction between the river water and the underlying magmatic mass played a crucial role in this process, causing accelerated cooling. This phenomenon has generated a series of irregular fractures, some of which have a chaotic arrangement, while others show a more regular geometry. Among these formations, we can identify prismatic structures of various configurations, including those known as "woodpiles," "harps," "rosettes," and the impressive vertical formations called "organ pipes," which can reach remarkable heights, even up to 30 meters.

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