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District de Faro

Peaks and Reservoirs of Algarve

Explore the geographical extremes of the Algarve, from the 902-meter summit of Fóia in the Monchique mountains to the dramatic coastal sinkholes along the Atlantic shore. This collection highlights the region's vital water infrastructure, including the Arade and Odeleite reservoirs, alongside prominent vantage points like São Miguel and Torre de Aspa. These sites showcase the transition from the rugged interior peaks to the unique limestone formations of the southern coastline.

A

Fóia

The highest point in the Algarve at 902 meters, located in the Serra de Monchique. It offers 360-degree views extending to the Atlantic Ocean and the Alentejo plains.

B

Torre de Aspa

Situated near Vila do Bispo, this is the highest cliff on the Costa Vicentina at 156 meters, providing a vantage point over the western Algarve coastline.

Barragem de Odeleite C

Barragem de Odeleite

A large reservoir on the Odeleite River known for its dragon-like shape when viewed from above. It serves as a primary water source for the eastern Algarve.

São Miguel D

São Miguel

Also known as Monte Figo, this 411-meter peak is the highest point in the Serra de Monte Figo, offering views over the Ria Formosa and the central coast.

Albufeira do Arade E

Albufeira do Arade

A reservoir on the Arade River near Silves, created by a dam completed in 1956 to support regional irrigation and agriculture.

Guilhim F

Guilhim

A peak in the Faro district providing views of the Barrocal region, a limestone transition zone between the coast and the mountains.

G

Algar

A natural vertical cave or sinkhole formed by marine erosion in the limestone cliffs characteristic of the central Algarve coast.

H

Barragem de Beliche

A dam on the Beliche River in the eastern Algarve, inaugurated in 1986 to manage water supplies for domestic and agricultural use.

I

Barragem de Alcoutim

A reservoir located near Alcoutim in the northeastern Algarve, utilized for local water management and irrigation.

J

Algar

A coastal sinkhole typical of the region's Karst topography, created by the collapse of limestone cavern roofs over time.

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