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Geologic Formation Attractions In Alentejo

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The Alentejo is a geographical, historical and cultural region of south-central and southern Portugal. In Portuguese, it literally means beyond Tagus river . Alentejo includes the regions of Alto Alentejo and Baixo Alentejo. It corresponds to the districts of Beja, Évora, Portalegre and the Alentejo Litoral. The main cities are: Évora, Beja, Serpa, Estremoz, Elvas and Portalegre. It has borders with Beira Baixa in the North, with Spain (Andalucia and Extremadura in the east, with the Algarve in the South and with the Atlantic Ocean, Ribatejo and Estremadura in the West. The Alentejo is a region known for its traditional polyphonic singing groups, sim...
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Geologic Formation Attractions In Alentejo

  • 1. Cabo Espichel Sesimbra
    Cabo Espichel is a cape situated on the western coast of the civil parish of Castelo, municipality of Sesimbra, in the Portuguese district of Setúbal.
    From Wikipedia, the free encyclopedia.
  • 3. Evora Complex Evora
    The Roman Temple of Évora , also referred to as the Templo de Diana is an ancient temple in the Portuguese city of Évora . The temple is part of the historical centre of the city, which was included in the classification by UNESCO as a World Heritage Site. It represents one of the most significant landmarks relating to the Roman and Lusitanian civilizations of Évora and in Portuguese territory.
    From Wikipedia, the free encyclopedia.
  • 4. Cabo da Roca Colares
    The Cabo da Roca Lighthouse is a beacon/lighthouse located 165 metres above the Atlantic Ocean, on Portugal's most westerly extent . It is located in the civil parish of Colares, in the municipality of Sintra, situated on a promontory that juts out into the ocean, made up of granite boulders and interspersed limestone. It is a third-order lighthouse, which originally began operating in 1772. It was the first new purpose-built lighthouse to be constructed in the country: the older lighthouses in existence at that time, were constructed on existing platforms or from pre-existing beacons.
    From Wikipedia, the free encyclopedia.

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