Geography of Portugal

Portuguese Exclusive Economic Zone

The continental shelf has an area of 28,000 square kilometres (11,000 sq mi), although its width is variable from 150 kilometres (93 mi) in the north to 25 kilometres (16 mi) in the south.[3] Its strong relief is marked by deep submarine canyons and the continuation of the main rivers. The Estremadura Spur separates the Iberian Abyssal and Tagus Abyssal Plains, while the continental slope is flanked by sea-mounts and abuts against the prominent Gorringe Bank in the south.[3] Currently, the Portuguese government claims a 200-metre (660 ft) depth, or to a depth of exploitation.

The Portuguese coast is extensive; in addition to approximately 943 kilometres (586 mi) along the coast of continental Portugal, the archipelagos of the Azores (667 km) and Madeira (250 km) are primarily surrounded by rough cliff coastlines. Most of these landscapes alternate between rough cliffs and fine sand beaches; the region of the Algarve is recognized for its sandy beaches popular with tourists, while at the same time its steep coastlines around Cape St. Vincent is well known for steep and forbidding cliffs. An interesting feature of the Portuguese coast is Ria Formosa with some sandy islands and a mild and pleasant climate characterized by warm but not very hot summers and generally mild winters.

Alternatively, the Ria de Aveiro coast (near Aveiro, referred to as "The Portuguese Venice"), is formed by a delta (approximately 45 kilometres (28 mi) length and a maximum 11 kilometres (6.8 mi) width) rich in fish and seabirds. Four main channels flow through several islands and islets at the mouth of the Vouga, Antuã, Boco, and Fontão Rivers. Since the 16th century, this formation of narrow headlands formed a lagoon, that, due to its characteristics allowed the formation and production of salt. It was also recognized by the Romans, whose forces exported its salt to Rome (then seen as a precious resource).

The Azores are also sprinkled with both alternating black sand and boulder-lined beaches, with only a rare exception, is there white sand beach (such as on the island of Santa Maria in Almagreira. The island of Porto Santo is one of the few extensive dune beaches in Portugal, located in the archipelago of Madeira.

Tidal gauges along the Portuguese coast have identified a 1–1.5 millimetres (0.039–0.059 in) rise in sea levels, causing large estuaries and inland deltas in some major rivers to overflow.[3]

As a result of its maritime possessions and long coastline, Portugal has an Exclusive Economic Zone of 1,727,408 km² (666,956 sq mi). This is the 3rd largest EEZ of all countries in the European Union and the 20th in the world. The sea-zone, over which Portugal exercises special territorial rights over the economic exploration and use of marine resources encircles an area of 1,727,408 square kilometres (666,956 sq mi) (divided as: Continental Portugal 327,667 km², Azores Islands 953,633 km², Madeira Islands 446,108 km²).

Tectonic structures of Europe, showing Iberia and the three "Portuguese" tectonic regions (far left)

Hot, dry conditions sparked dozens of devastating wildfires in northern and central Portugal and central Spain in the summer of 2003. By the time this image was taken on January 19, 2004, the scars had begun to fade in areas, though the scars in Central Portugal and across the border in Spain are still dark red in the false-color image.

The Portuguese territory came into existence during the history of Gondwana and became aligned with European landforms after the super-continent Pangea began its slow separation into several smaller plates. The Iberian plate was formed during the Cadomian Orogeny of the late Neoproterozoic (about 650-550 Ma), from the margins of the Gondwana continent. Through collisions and accretion a group of island arcs (that included the Central Iberian Plate, Ossa-Morena Plate, South Portuguese Plate) began to disintegrate from Gondwana (along with other European fragments). These plates never separated substantially from each other since this period.[4] By the Mesozoic, the three "Portuguese plates" were a part of the Northern France Armoric Plate until the Bay of Biscay began to separate. Following the separation of the Iberian Abyssal Plain, Iberia and Europe began to drift progressively from North America, as the Mid-Atlantic fracture zone pulled the three plates away from the larger continent. Eventually, Iberia collided with southern France attaching the region into a peninsula of Europe (during the Cenozoic). Since the late Oligocene, the Iberian plate has been moving as part of the Eurasian plate, with the boundary between Eurasia and Africa situated along the Azores–Gibraltar fracture zone.[5][6][7][8][9][10][11][12][13][14]

The Iberian peninsula, defined by is coastline, is due to a fragment of the Variscan tectonic fracture zone, the Iberian-Hesperian Massif, which occupies the west-central part of the plateau.[3] This formation is crossed by the Central System, along an east-northeast to west-southwest alignment, parallel to the European Baetic Chain (an aspect of the Alpine Chain).[3] The Central Cordillera is itself divided into two blocks, while three main river systems drain the differing geomorphological terrains:[3]

• the Northern Meseta (with a mean altitude of 800 metres (2,600 ft)) is drained by the Douro River (running east to west);
• the Southern Meseta (within a range of 200 to 900 metres (660 to 2,950 ft) altitude) is drained by the Tagus River (running east to west) from Spain, and the Guadiana River (running north to south), comprising the Lower Tagus and Sado Basins.

To the north the landscape is mountainous in the interior areas with plateaus, cut by four breakings lines that allow the development of more fertile agricultural areas.

The south down as far as the Algarve features mostly rolling plains with a climate somewhat warmer and drier than the cooler and rainier north. Other major rivers include the Douro, the Minho and the Guadiana, similar to the Tagus in that all originate in Spain. Another important river, the Mondego, originates in the Serra da Estrela (the highest mountains in mainland Portugal at 1,993 m).

No large natural lakes exist in Continental Portugal, and the largest inland water surfaces are dam-originated reservoirs, such as the Alqueva Reservoir with 250 square kilometres (97 sq mi), the largest in Europe. However, there are several small freshwater lakes in Portugal, the most notable of which are located in Serra da Estrela, Lake Comprida (Lagoa Comprida) and Lake Escura (Lagoa Escura), which were formed from ancient glaciers. Pateira de Fermentelos is a small natural lake near Aveiro one the largest natural lake in the Iberian Peninsula and with rich wildlife. In the Azores archipelago lakes were formed in the caldera of extinct volcanoes. Lagoa do Fogo and Lagoa das Sete Cidades (two small lakes connected by a narrow way) are the most famous lakes in São Miguel Island.

Lagoons in the shores of the Atlantic exist. For instance, the Albufeira Lagoon and Óbidos Lagoon (near Foz do Arelho, Óbidos).

In addition to continental Europe, Portugal consists of two Autonomous Regions in the Atlantic Ocean, consisting of the archipelagos of Madeira and Azores. Madeira is located on the African Tectonic Plate, and comprises the main island of Madeira, Porto Santo and the smaller Savage Islands. The Azores, which are located between the junction of the African, European and North American Plates, straddle the Mid-Atlantic Ridge. There are nine islands in this archipelago, usually divided into three groups (Western, Central and Eastern) and several smaller Formigas (rock outcroppings) located between São Miguel and Santa Maria Islands. Both island groups are volcanic in nature, with historic volcanology and seismic activity persisting to the present time. In addition, there are several submarine volcanos in the Azores (such as Dom João de Castro Bank), that have erupted historically (such as the Serrata eruption off the coast of Terceira Island). The last major volcanic event occurred in 1957-58 along the western coast of Faial Island, which formed the Capelinhos Volcano. Seismic events are common in the Azores. The Azores are occasionally subject to very strong earthquakes, as is the continental coast. Wildfires occur mostly in the summer in mainland Portugal and extreme weather in the form of strong winds and floods also occurs mainly in winter. The Azores are occasionally stricken by tropical cyclones such as Hurricane Jeanne (1998) and Hurricane Gordon (2006).

*Tornados - counted for last 5 years [21]

• Central Intelligence Agency, ed. (2010). "Portugal: CIA World Factbook". Langley, Virginia: Central Intelligence Agency. Retrieved 27 December 2010.
• Symington, Martin (2003). "Portugal". Eyewitness Travel Guide series. Dorling Kindersley Publishing. ISBN 978-0-7894-9423-8.
• Moores, Eldridge M.; Fairbridge, Rhodes Whitmore, eds. (1997). Encyclopedia of European and Asian Regional Geology. London, England: Chapman & Hall. pp. 611–619. ISBN 9780412740404.
• Le Pichon, X.; Sibuet, J.C. (September 1971). "Western extension of boundary between European and Iberian plates during the Pyrenean orogeny" (PDF). Earth and Planetary Science Letters. 12 (1): 83–88. Bibcode:1971E&PSL..12...83L. CiteSeerX 10.1.1.493.7034. doi:10.1016/0012-821X(71)90058-6.
• Olivet, Jean-Louis; Bonnin, J.; Beuzart, Paul; Auzende, Jean-Marie (1984). Cinématique de l'Atlantique Nord et Central [Kinematics of the North and Central Atlantic] (Report). Publications du C.N.E.X.O. Série "Rapports scientifiques et techniques". 54. Institut français de recherche pour l'exploitation de la mer. pp. 1–108.
• Le Pichon, X.; Sibuet, J. C.; Francheteau, J. (23 March 1977). "The fit of the continents around the North Atlantic Ocean". Tectonophysics. 38 (3–4): 169–209. Bibcode:1977Tectp..38..169L. doi:10.1016/0040-1951(77)90210-4.
• López-Guijarro, Rafael; Armendáriz, Maider; Quesada, Cecilio; Fernández-Suárez, Javier; Murphy, J. Brendan; Pin, Christian; Bellido, Felix (2008). "Ediacaran–Palaeozoic tectonic evolution of the Ossa Morena and Central Iberian zones (SW Iberia) as revealed by Sm–Nd isotope systematics" (PDF). Tectonophysics. Elsevier. 461 (1–4): 202–214. Bibcode:2008Tectp.461..202L. doi:10.1016/j.tecto.2008.06.006. ISSN 0040-1951 – via ScienceDirect.CS1 maint: ref=harv (link)
• Savostovin, L. A.; Sibuet, J. C.; Zonenshain, L. P.; Le Pichon, X.; Roulet, M. J. (1986). "Kinematic evolution of the Tethys belt from the Atlantic ocean to the pamirs since the Triassic". Tectonophysics. 123 (1–4): 1–35. Bibcode:1986Tectp.123....1S. doi:10.1016/0040-1951(86)90192-7.
• Schouten H.; Srivastava S. P.; Klitgord, K. (1984). Trans. Am. Geophys. Union. 65: 190. Missing or empty |title= (help)
• Sclater, J. G.; Hellinger, S.; Tapscott, C. R. J. (1977). "Paleobathymetry Of Atlantic Ocean From Jurassic To Present". The Journal of Geology. 85 (5): 509–552. Bibcode:1977JG.....85..509S. doi:10.1086/628336. ISSN 0022-1376. S2CID 129522366.
• Seber, D.; Barazangi, M.; Ibenbrahim, A.; Demnati, A. (1996). "Geophysical evidence for lithospheric delamination beneath the Alboran Sea and Rif--Betic mountains" (PDF). Nature. 379 (6568): 785–790. Bibcode:1996Natur.379..785S. doi:10.1038/379785a0. hdl:1813/5287. S2CID 4332684.
• Srivastava, S.P.; Schouten, H.; Roest, W.R.; Klitgord, K.D.; Kovacs, L.C.; Verhoef, J.; Macnab, R. (19 April 1990). "Iberian Plate Kinematics: A Jumping Plate Boundary between Eurasia and Africa". Nature. 344 (6268): 756–759. Bibcode:1990Natur.344..756S. doi:10.1038/344756a0. S2CID 4362197.