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List Of Fajãs In The Azores
The following is a list of the fajãs of the islands of the Azores: Faial * Fajã do Varadouro (Castelo Branco (Horta), Castelo Branco, Horta (Azores), Horta) * Fajã da Praia do Norte (Praia do Norte, Horta (Azores), Horta) Flores * Fajã de Lopo Vaz (Lajes das Flores (parish), Lajes, Lajes das Flores) * Fajã da Ponta Ruiva (Cedros (Santa Cruz das Flores), Cedros, Santa Cruz das Flores * Fajã do Conde (Santa Cruz das Flores (parish), Santa Cruz, Santa Cruz das Flores) Graciosa * Fajã da Folga * Fajã da Beira Mar Pico * Fajã da Baixa (Piedade (Lajes do Pico), Piedade, Lajes do Pico) * Fajã do Calhau (Piedade (Lajes do Pico), Piedade, Lajes do Pico) São Jorge * Fajã d'Alem (Norte Grande (Azores), Norte Grande, Velas (Azores), Velas) * Fajã da Abelheira * Fajã da Betesga * Fajã da Caldeira de Cima * Fajã da Caldeira de Santo Cristo * Fajã da Choupana * Fajã da Ermida (Rosais, Velas, Azores, Velas) * Fajã da Fonte do Nicolau * Fajã da Fragueira * Fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. Azor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã D'Alem
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. Azo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Neca
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. Azo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Fragueira
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Fonte Do Nicolau
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Velas, Azores
Velas () is a municipality in the São Jorge Island, in the Portuguese autonomous region of Azores. The municipality encompasses the western portion of the island, with its municipal seat in the town of Velas on the south coast, and is divided into six parishes. The population in 2011 was 5,398, in an area of 117.38 km². History The origin of the name ''Velas'' has never been clarified by historians, although it may refer to the number of sailing ships that congregated in the municipality (''"velas"'' is Portuguese for sails), but may also refer to the ''"sails"'' of the windmills that populated the municipality during early settlement. There may also been confusing in the similarity between ''velas'', the word ''velhas'' (which means ''"old"'' in Portuguese) or ''"belas"'' (which means ''"beautiful"'', in the same language). Another reference is to the Portuguese term ''"vilar"'', which means vigilant, and may have been used to situation in the Canal, where residents were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rosais
Rosais (literally, archaic Portuguese for "rosaries") is a civil parish in the municipality of Velas in the Portuguese archipelago of the Azores. The population in 2011 was 743, in an area of 24.23 km². History Although Rosais was first mentioned in written documents in 1568, it existed as a settlement before then. It was considered the "granary" or "breadbasket" of São Jorge, due to the area's fertility. To this day the area supports rich pastures. Geography The parish of Rosais is located on the island of São Jorge and extends approximately from Figueiras to Ponta dos Rosais. The parish had approximately 820 inhabitants according to the 2001 census. It contains the localities Arrifana, Canada da Trás, Canada das Faias, Fajã de João Dias, Quarteiro, and Rosais. The western corner of the island is essentially a plateau, with tall cliffs extending until the Ponta dos Rosais, where the Ponta dos Rosais Lighthouse stands as a beacon. The rest of the parish consist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Ermida
The Fajã da Ermida (''Fajã of the Hermitage'') is a permanent debris field, known as a fajã, built from the collapsing cliffs on the northern coast of the Freguesia (Portugal), civil parish of Rosais, in the municipality of Velas, Azores, Velas, island of São Jorge Island, São Jorge, in the Portugal, Portuguese archipelago of the Azores. Fajã da Ermida is accessible by trail from the neighbouring Fajã da Maria Pereira and Fajã Amaro da Cunha, along the northern coast of the island. While at one time the area was inhabited constantly, today the region is mostly used for some grazing and subsistence farming. References See also * List of fajãs in the Azores {{DEFAULTSORT:Faja da Ermida São Jorge Island Rosais, Faja Ermida Fajãs of the Azores, Ermida ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Choupana
() is a Portuguese term of obscure origin used to describe Supralittoral zone, supratidal scree, talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these Microclimate, microclimates allow the cultivation of a variety of staple fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Caldeira De Santo Cristo
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. Azo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Caldeira De Cima
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fajã Da Betesga
() is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.G. Lameiras et al. (2009), p.827 Although relatively common world-wide, they are distinctive features of the Azores and Madeira, as well as of the Canary Islands, where the equivalent term in Canarian Spanish is (). The term also designates a small flat piece of land, generally cultivable and located by the sea, formed of materials fallen from cliffs. Another Canarian word for lava is , literally, "low island". Geology Fajãs are created from collapsing cliffs or lava flows and are identifiable along the coast as "flat" surfaces, relative to other geological forms. Tides and tidal currents have only minor influence on coastal morphology, and therefore sedimentation and deposits there became permanent. Composed of fertile soils, these microclimates allow the cultivation of a variety of staple and exotic plants, such as coffee. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
