Does Madeira has an Active Volcano?

Most visitors to Madeira Island associate its mountainous and rugged terrain solely with its natural beauty, but few realize that they are actually traveling across an ancient volcano — which, technically, is still considered active.

The island’s origin is entirely volcanic. Madeira emerged from the depths of the Atlantic Ocean around 5 million years ago, the result of intense underwater eruptions. Over millions of years, these eruptions sculpted the dramatic landscape we see today: deep valleys, steep cliffs, and high peaks like Pico Ruivo, which rises to 1,862 meters.

Although the last known eruption occurred around 6,500 years ago, Madeira is classified as being part of a dormant volcanic system — meaning that, despite the lack of recent eruptive activity, the potential for future eruptions cannot be entirely ruled out. As a result, the island is regularly monitored by seismic networks.

Locals don’t live in fear, as the recorded seismic activity is usually weak and imperceptible. Still, seismologists keep constant watch, especially given the geological history of the region.

Interestingly, in some parts of the island, geothermal heat is still noticeable. There are reports of old hot springs, now less active, and certain patches of ground that retain elevated temperatures even without direct sunlight.

Madeira may not have geysers or flowing lava, but remembering that we walk on an ancient — and technically active — volcanic structure gives new meaning to the phrase “islands of fire.” It’s one more reason to look at the landscape with awe… and a touch of respect for the power of nature.