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Is there a volcano on Funchal?

Funchal, the capital city of Madeira, is seen here along the southeast flanks of the massive shield volcano forming the island.



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The youngest activity at Madeira lies in the west-central part of the island, and consists of cinder cones in the upper Sao Vicente valley, a series of intracanyon flows, and a tephra layer on top of the Paul da Serra plateau dated at about 6500 years ago.

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It cannot be assumed that volcanic activity on Madeira is extinct but in the absence of significant seismic activity it is considered that the volcanic hazard level is very low.

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On March 4th, 1930, a sector of the Cape Girão cliff, located in the southern shore of Madeira Island, collapsed into the sea and generated an 8 m tsunami wave height.

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To achieve this, we use the prime example of Madeira, a volcanic island in the Atlantic Ocean highly vulnerable to cliff-failure. Particularly, we explore the March 4th, 1930 Cabo Girão event that triggered a deadly tsunami.

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In the area you have selected (Madeira Islands (Por.)) earthquake hazard is classified as very low according to the information that is currently available. This means that there is less than a 2% chance of potentially-damaging earthquake shaking in your project area in the next 50 years.

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Briefly, we can say that on Madeira Island, the most frequent hazards have essentially been flash floods in the autumn and winter and forest fires in the summer.

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Fires were started, which are said to have burned for seven years. The settlers constructed a large number of canals (levada]s), since in some parts of the island there was water in excess, while in other parts it was scarce.

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Although located in the African Plate, some 650 km (360 mi) off the North African coast, Madeira belongs and has always belonged ethnically, culturally, economically and politically to Europe, some 955 km (583 miles) from the European mainland.

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Madeira is renowned for its landscapes, lore—and its legendary wine, which graced the tables of America's Founding Fathers.

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Together with the islands of Porto Santo and Desertas and the Selvagens—Madeira forms an autonomous region of the country of Portugal.

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The sea between the islands of Madeira Archipelago has a depth of around 4000 meters, already at a distance of 5 km from the coast of the sea reaches a depth of 3000 m The archipelago is bathed by the Gulf Stream and therefore the temperature of the water around the island of Madeira does not drop below 18 ° C, which ...

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Crime and safety Portugal is a low-crime country in general, but even more so in the small island community of Madeira. Violent crime involving tourists is extremely rare in Madeira and so you have little to worry about with regard to personal safety.

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Violent crime involving tourists is extremely rare in Madeira and so you have little to worry about with regard to personal safety. But as with any travel destination, it's important to take basic travel safety precautions such as keeping your valuables close by and/or hidden, especially at night.

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Natural Disasters The rainy season is from October through March. Floods may occur, especially on Madeira Island. Forest fires occur during the dry season.

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The coldest record in Funchal is 7.5 °C (45.5 °F), recorded in March 2011, when snowfalls above 500 meters (1,650 feet) occurred in inland areas.

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Madeira is part of massive underwater shield volcano in the Atlantic Ocean, of which the island is just the highest point. Formed hundreds of thousands of years ago, the island has seen volcanic activity as recently as 6,500 years ago, but today is considered to be dormant and unlikely to erupt.

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Calheta Beach is one of the island of Madeira's few yellow sandy beaches. A peaceful swimming experience is guaranteed by two piers, so you can exercise in the sea all year round. Ribeira do Natal Beach enjoys properties that make it one of the best places for swimming. The transparency of its waters is remarkable.

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Locally with an expressive geomorphological degraded scarp, is running parallel to the elongation of the island, and has the maximum extension of 56 km. It corresponds to a major dextral fault with a northern collapse, confirmed by several field observations.

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