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Cabo da Roca (Portuguese: [ˈkaβu ðɐ ˈʁɔkɐ]) or Cape Roca is a cape which forms the westernmost point of the Sintra Mountain Range, of mainland Portugal, of continental Europe, and of the Eurasian landmass. [1] It is situated in the municipality of Sintra, near Azóia, in the south west of the Lisbon District.
Westernmost point — Cabo da Roca (38.780963, -9.500552), civil parish of Colares, municipality of Sintra, also the westernmost point of continental Europe; [2] Easternmost point — Ifanes e Paradela (41.574886, -6.190217), municipality of Miranda do Douro; Centermost — Penhascoso, Portugal (39.5571,-8.04276), Municipality in Portugal
Cabo da Roca, a tourist attraction and limit of continental Europe, with the lighthouse in the background Close-up of the base and main tower of the Cabo da Roca complex Main beacon on the lighthouse The initiative to construct the lighthouse came from the Junta Geral da Fazenda do Reino on 1 February 1758, in an order to construct six ...
The Portuguese Riviera (Portuguese: Riviera Portuguesa) is a term used in the tourist industry for the affluent coastal region to the west of Lisbon, Portugal, centered on the coastal municipalities of Cascais (including Estoril), Oeiras and Sintra.
Azóia is a village in the municipality of Sintra (freguesia Colares) in the southwest of the district of Lisbon, Portugal.Azóia lies 1 km from the Cabo da Roca, the most westerly point of the European continent, which makes it the westernmost village on the European continent.
[4] [5] [6] Politically, the islands belonging to Portugal and Spain are parts of the European Union, while Cape Verde is a member of the African Union. Geologically, most of Macaronesia is part of the African tectonic plate. The Azores are located in the triple junction between the African, Eurasian, and North American plates. [Note 1] [7] [8]
Westernmost point —Monchique Islet, Flores Island, Azores Islands, Portugal (39°29′42.8″N, 31°16′30″W) Easternmost point — Big Diomede , Russia (65°46'N, 169°03'W). The International Date Line runs between the Russian Big Diomede and the neighbouring U.S.-governed Little Diomede .
Basalt columns seen on Porto Santo Island, Portugal. Columnar jointing of volcanic rocks exists in many places on Earth. Perhaps the most famous basalt lava flow in the world is the Giant's Causeway in Northern Ireland, in which the vertical joints form polygonal columns and give the impression of having been artificially constructed.