Porto Santo Island: Difference between revisions
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===Physical geography=== |
===Physical geography=== |
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[[Image:Porto santo aerialview.jpg|left|thumb|235px|The island of Porto Santo as seen from the air]] |
[[Image:Porto santo aerialview.jpg|left|thumb|235px|The island of Porto Santo as seen from the air]] |
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[[Image:BasaltColumns PortoSanto.JPG|thumb|left|235px|[[Basalt]] columns, a geological formation.]] |
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The island is characterized by two areas: the ''accidented'' northeast (mountainous, with rocky ledges and cliffs), and a coastal plain in the southwest (that includes a nine kilometre long white sand beach, giving the island an advantage over neighbouring Madeira). The mountainous northeast part of the island, consists of two geomorphological structures that includes:<ref>Rocha et al, 2002, p.11</ref> an area of peaks, Pico do Castelo (437 meters), Pico da Juliana (447 meters), Pico da Gandaia (499 meters) and Pico do Facho (517 meters); and between the eastern coast and this area, a series of minor peaks, Pico do Maçarico (285 meters), Pico do Concelho (324 meters) and Pico Branco (450 meters). The southwest part of the island, although relatively flat, includes a series of elevations 100 meters in height or greater, such as Pico Ana Fereira (283 meters), Pico do Espigão (270 meters) and the Cabeço do Zimbralinho (183 meters). The slope of the western part of the island slopes from 150 meters to the south coast reaching the sandy beaches of Porto Santo. A third system, in the west-northwest, that includes Cabeço da Bárbara Gomes (227 meters) and Cabeço das Canelinhas (176 meters) is distinct from the areas identified. The island is encircled by an oceanic platform between 20 and 37 km2, with a minimum depth of 8 meters (Baixa do Noroeste), and limited by the flanks of a large submarine volcano.<ref>Rocha et al, 2002, p.12</ref> |
The island is characterized by two areas: the ''accidented'' northeast (mountainous, with rocky ledges and cliffs), and a coastal plain in the southwest (that includes a nine kilometre long white sand beach, giving the island an advantage over neighbouring Madeira). The mountainous northeast part of the island, consists of two geomorphological structures that includes:<ref>Rocha et al, 2002, p.11</ref> an area of peaks, Pico do Castelo (437 meters), Pico da Juliana (447 meters), Pico da Gandaia (499 meters) and Pico do Facho (517 meters); and between the eastern coast and this area, a series of minor peaks, Pico do Maçarico (285 meters), Pico do Concelho (324 meters) and Pico Branco (450 meters). The southwest part of the island, although relatively flat, includes a series of elevations 100 meters in height or greater, such as Pico Ana Fereira (283 meters), Pico do Espigão (270 meters) and the Cabeço do Zimbralinho (183 meters). The slope of the western part of the island slopes from 150 meters to the south coast reaching the sandy beaches of Porto Santo. A third system, in the west-northwest, that includes Cabeço da Bárbara Gomes (227 meters) and Cabeço das Canelinhas (176 meters) is distinct from the areas identified. The island is encircled by an oceanic platform between 20 and 37 km2, with a minimum depth of 8 meters (Baixa do Noroeste), and limited by the flanks of a large submarine volcano.<ref>Rocha et al, 2002, p.12</ref> |
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Revision as of 16:58, 1 November 2012
Template:Geobox Porto Santo Island (Portuguese pronunciation: [ˈpoɾtu ˈsɐ̃tu]) is a Portuguese island 43 kilometres (27 mi) northeast of Madeira Island in the North Atlantic Ocean; it is the northernmost and easternmost island of the archipelago of Madeira, located in the Atlantic Ocean west of Europe and Africa.
History
Porto Santo was officially discovered and recognized by the crown of Portugal in 1418, after captains in the service of the Infante D. Henrique came across the island and its sheltered anchorage. João Gonçalves Zarco and Tristão Vaz Teixeira had been ordered (by King John I) to discover new territory west of Africa, and had been sent off-course by a storm. The island's name Porto Santo (English: Holy Harbour) was derived from the sailors' stories of their discovery of a sheltered bay during the tempest, which was seen as divine deliverance.[1]
Bartolomeu Perestrelo, a third member of the team that later explored the islands of the Madeira, became the first Captain-donatorio of Porto Santo, by royal award in November 1445.
During the first centuries of settlement, life on Porto Santo was harsh, owing to the scarcity of potable water and constant attacks by Barbary Coast pirates and French privateers.
The famous explorer Christopher Columbus married Bartolomeu Perestrelo's daughter, Filipa Moniz Perestrelo, a Portuguese noblewoman, and for a while lived on Porto Santo.[2]
Geography
Physical geography
The island is characterized by two areas: the accidented northeast (mountainous, with rocky ledges and cliffs), and a coastal plain in the southwest (that includes a nine kilometre long white sand beach, giving the island an advantage over neighbouring Madeira). The mountainous northeast part of the island, consists of two geomorphological structures that includes:[3] an area of peaks, Pico do Castelo (437 meters), Pico da Juliana (447 meters), Pico da Gandaia (499 meters) and Pico do Facho (517 meters); and between the eastern coast and this area, a series of minor peaks, Pico do Maçarico (285 meters), Pico do Concelho (324 meters) and Pico Branco (450 meters). The southwest part of the island, although relatively flat, includes a series of elevations 100 meters in height or greater, such as Pico Ana Fereira (283 meters), Pico do Espigão (270 meters) and the Cabeço do Zimbralinho (183 meters). The slope of the western part of the island slopes from 150 meters to the south coast reaching the sandy beaches of Porto Santo. A third system, in the west-northwest, that includes Cabeço da Bárbara Gomes (227 meters) and Cabeço das Canelinhas (176 meters) is distinct from the areas identified. The island is encircled by an oceanic platform between 20 and 37 km2, with a minimum depth of 8 meters (Baixa do Noroeste), and limited by the flanks of a large submarine volcano.[4]
The island's submarine activity occurred during the Miocene epoch, producing basaltic eruptions that persisted to the Quaternary period. There were three phases of distinct volcanism, followed by periods of calm associated with sedimentation:[5]
- 1st Phase - associated with basaltic lava, pyroclastic flows, trachyte domes that were to form Pico do Concelho, Pico do Facho, Pico do Juliana and the Ponta da Calheta. This period was followed by a period of marine fossil accumulation, concentrated in the northeast of the island to about 300 meters altitude (around Pico do Juliana, Pico de Ana Ferreira and Ribeira do Moledo;
- 2nd Phase - this was a period of fissural volcanism that cut across and metamorphosed the older formations, occurring in the early Pliocene period;
- 3rd Phase - was an intrusive phase, resulting in a number of faults and dikes that cut across the Calcareous fossils. Likely occurring in the Pliocene, it was followed by deposits of layers of detritic and calcareous sediments, that included brownish-red alluvial layers, along the island's flanks and beach.
Climate
| Climate data for Vila Baleira | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Mean daily maximum °C (°F) | 18.0 (64.4) |
18.0 (64.4) |
19.0 (66.2) |
19.5 (67.1) |
21.0 (69.8) |
22.1 (71.8) |
24.0 (75.2) |
25.0 (77.0) |
25.0 (77.0) |
23.2 (73.8) |
21.0 (69.8) |
19.2 (66.6) |
21.1 (70.0) |
| Mean daily minimum °C (°F) | 13.2 (55.8) |
13.1 (55.6) |
13.3 (55.9) |
14.0 (57.2) |
15.1 (59.2) |
17.1 (62.8) |
19.0 (66.2) |
20.0 (68.0) |
20.0 (68.0) |
18.1 (64.6) |
16.2 (61.2) |
14.4 (57.9) |
16.1 (61.0) |
| Average precipitation mm (inches) | 48.7 (1.92) |
40.2 (1.58) |
37.2 (1.46) |
23.5 (0.93) |
14.0 (0.55) |
7.0 (0.28) |
3.2 (0.13) |
4.0 (0.16) |
23.7 (0.93) |
39.9 (1.57) |
50.0 (1.97) |
69.9 (2.75) |
361.3 (14.22) |
| Source: World Meteorological Organization (UN), Instituto de Meteorologia, Normais Climatológicas do Porto Santo (1971-2000). | |||||||||||||
Human geography
The main urban area, which is one of only five Portuguese municipalities that have only one parish, is the city of Vila Baleira ([ˈvilɐ bɐˈlɐiɾɐ]), also known as Porto Santo.
Although a small island, the Porto Santo community has its own schools, health-care centre, police detachments, a gymnasium, churches, several local squares, a Congress Centre, museum, shopping centres, bars, hotels and restaurants.
Economy
The main industry on the island of Porto Santo is tourism, which has emerged through hotel construction in the 20th century and is based on the attractions of the beaches and temperate climate.
The island has a golf course that was designed by Spanish golfing champion Seve Ballesteros; Porto Santo Golfe hosted the Madeira Islands Open in 2009, as part of the European Tour. Once the planned second course is completed, Porto Santo Golfe will be the largest course in Madeira: there is currently one 18-hole golf course and one nine-hole course. In addition, Porto Santo's Golf Complex includes eight tennis courts and an equestrian centre (Pico Ana Ferreira).
The island has an international airport, with routine flights to Madeira Airport (about a 15-minute flight away); the nearest place to Porto Santo is Machico (on Madeira). The Porto Santo Airport (PXO) has many connections with both domestic (Ponta Delgada, Lisbon, Oporto and Faro) and (occasionally) international flights (including several charters to England, Italy, Germany, Belgium, France and Spain).
References
- Notes
- ^ The discoveries of Porto Santo and Madeira were first described by Gomes Eannes de Azurara in Chronica da Descoberta e Conquista da Guiné. Arkan Simaan relates in French these discoveries in his novel L’Écuyer d’Henri le Navigateur.
- ^ His home now serves as a museum that presents a permanent exhibition of his life and familial relations, as well as temporary art exhibitions.
- ^ Rocha et al, 2002, p.11
- ^ Rocha et al, 2002, p.12
- ^ Rocha et al, 2002, p.12
- Sources
- Rocha, António; Silva, João; Soares, Helena; Abenta, Jaime; Almeida, Fernando; Gomes, Celso (2002). Geologia, génese e dinâmica da areia de praia da ilha do Porto Santo: O sistema de informação geográfica (in Portuguese). Oeiras, Portugal.
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