Corvo Island


Corvo Island, literally the Island of the Crow, is the smallest and the northernmost island of the Azores archipelago and the northernmost in Macaronesia, has a population of approximately 468 inhabitants constituting the smallest single municipality in the Azores and in Portugal, and lies within the North American Plate.

History

of the Carthaginian Empire exploring the islands in approximately 200 BCE notwithstanding,
the mainstream history of the Azores originates with non-official exploration during the period of the late-13th century, resulting in maps, such as the Genovese Atlas Medici from 1351, which mentions obscure islands in an undefined Atlantic archipelago. The Medici Atlas refers to an Insula Corvi Marini, in a seven-island archipelago, but it is improbable that it refers specifically to Corvo, although the island's name could have originated from this atlas. It is likely that the name referred to the two islands of Corvo and Flores, which also appeared on the later Aragonese Mapa Catalão of 1375.
The navigator Diogo de Teive discovered both islands of the Azores' Western Group on his 1452 return from the Banks of Newfoundland following his second voyage of exploration. Subsequently, the Portuguese Court, when referring to the new Ilhas das Flores, began to identify Corvo as Ilha de Santa Iria, but other nautical charts continued to refer to this island as Ilhéu das Flores, Ilha da Estátua, Ilha do Farol or Ilha de São Tomás. For a while it was also known as Ilha do Marco, which was attributed to its reference as a geographic marker for sailors, or, likely, the location of a small promontory where a marker was placed, which received the name Ponta do Marco.
Unsuccessful attempts at settlement of the island occurred in the following years; not until 1580 did a permanent settlement became viable.
A religious parish of Corvo was finally constituted in 1674, and then on 20 June 1832, integrated into a functioning civilian administration.

Geography

Physical geography

The island is located on the North American Plate, west of the Mid-Atlantic Ridge on a sea-mount of approximately 1.5-1.0 million years age. The islands of Corvo and Flores emerged from a submarine mount oriented along a north-northeast to south-southwest line, while Corvo is controlled by faults oriented north to south, parallel to the mid-Atlantic Ridge, and transform faults oriented west to east which crosscut secondary cones on the outer slopes. The island formed from a 5 km diameter central volcano that emerged around 730,000 years ago, whose central cone was approximately in altitude. The crater collapsed 430,000 years ago during a Plinian eruption, forming a subsidence caldera, referred to as the Caldeirão. Within the caldera are several cinder and spatter cones giving rise to small lakes, peat bogs, and islets. The highest point on the island, the Morro dos Homens, crowns the southern rim of the Caldeirão at above sea level.
Two main volcanic complexes are usually recognized:
While the initial phases were dominated by basaltic lava flows and pyroclastic deposits, the final phase was characterized by pumice, surges, lahars, and pyroclastic flows characteristic of Plinian and sub-Plinian eruptions.
Sheer cliffs dominate the coastal areas, the exception being along the southern margin which is composed of ancient lava flows. The western cliffs, with an almost vertical slope rises above sea level; one of the major coastal elevations in the Atlantic. Remnants of the ancient volcano are partially preserved in the southern and eastern flanks of the island. In addition to marine erosion, the island is constantly eroded by strong northeast and western winds. In the south, secondary cinder cones, such as Coroínha, Morro da Fonte, Grotão da Castelhana and Coroa do Pico, are visibly preserved with little erosion, and responsible for many basaltic flows that formed the southern lava fajã. The last eruption took place about 80-100,000 years ago in the vicinity of Vila Nova do Corvo.
In the extreme northeast, along the Ponta Torrais there are two small islets, Ilhéu dos Torrais and the Ilhéu do Torrão, in addition to several submarine reefs, that are dangerous to navigation. At the end of October 2012, following several days of excess rainfall, a landslide occurred that dislodged geological debris along the northwestern corner of the island, resulting in the formation of small islets, that progressively transformed into a peninsula and, finally a fajã.

Ecoregions/Protected areas

The Corvo Nature Park was created under Regional Legislative Decree 44/2008/A, on 5 November 2008, in order to conserve and protect species habitat and natural resources on the island. It includes principally two categories, and associated areas of intervention:
;Protected Areas for the Management of Habitats and Coastal Species
;Protected Areas for the Management of Resources
Like many of the other Azorean islands, the climate is humid, with of precipitation annually, comfortable although generally windy. Temperatures are in Vila do Corvo, with a variance between in February to in August. In the higher elevations fog is common and almost permanent. Due to maritime agitation, in particular on the western coast, there is elevated erosion along the coast. The relative humidity is between 74% in October and 85% in June, when fog is more frequent.

Human geography

There is one urban center on the island: Vila do Corvo. Principally, it is a collection of many residential homes, interspersed with commercial businesses located on the southern one-third of the island. Functionally, by law, Vila do Corvo is the only Portuguese top-level municipality without a civil parish. The urbanized area is divided between the village, the airport, and the island's ports. The lands immediately around the settlement are small zones along the eastern coast that can sustain cultivation of some crops and fruit trees, and where some older trees have survived settlement; the best pasture-lands are located in the north in the zone of Terras Altas.
The southern coast, referred to as Enseada de Nossa Senhora do Rosário, is the location of three ports, constructed at various times for diverse needs: Porto Novo, the Porto do Boqueirão and Porto da Casa. Portinho da Areia, on the extreme west of the southern coast is the only beach and principal swimming area on the island.

Economy

Subsistence agriculture has predominated on the island since it was first settled. It currently occupies 17.5% of the area of the municipality, and concentrated on small parcels in the eastern half of the island and along the northern parts of Vila do Corvo. In this patchwork of volcanic hedge-rows, farmers concentrate on semi-permanent crops.
Dairy production is the primary activity, and cheese is one of the primary commercialized products, although the raising of pigs and poultry is also common. Until the 1960s, the raising of sheep and the commercialization of wool was also important on the island. This was until a change in forestry policy forced many farmers to vacate uncultivated lands, lands that were routinely used to graze sheep. It was quickly the end of the wool industry on the island, an industry that had been integral to the island's small export industry.

Transport

The island is served by the Corvo Airport, located on the southern margin of the island between the village and southern ocean ports. Inter-island flights are handled by SATA Air Açores: there are no direct flights to Corvo from outside the archipelago. Since the 1990s, the airport was serviced by one Bombardier Dash 8 Q200 aircraft, big enough to handle the low volume of traffic to the island. These flights have since been operated by alternating DeHavilland Dash 8 aircraft, as part of the fleet revitalization program of the late 20th century.