Difference between revisions of "Portugal"

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Less than one-eighth of Portugal rises above 2,300 feet (700 metres). Most of the country’s mountains are north of the Tagus River, which flows northeast to southwest and divides the country. North of the Tagus, more than nine-tenths of the land rises above 1,300 feet (400 metres); in the south, only one range, São Mamede, surpasses 3,200 feet (1,000 metres).--->[[Relief-Portugal|>>>Read More.<<<]]
Less than one-eighth of Portugal rises above 2,300 feet (700 metres). Most of the country’s mountains are north of the Tagus River, which flows northeast to southwest and divides the country. North of the Tagus, more than nine-tenths of the land rises above 1,300 feet (400 metres); in the south, only one range, São Mamede, surpasses 3,200 feet (1,000 metres).--->[[Relief-Portugal|>>>Read More.<<<]]


 
*Drainage
 
 
 
 
 
Drainage
All of Portugal’s main rivers flow from Spain over the edge of the Meseta in a series of defiles (narrow gorges), and their usefulness, either for navigation or as routeways for roads and railways, is thus limited. The longest river crossing Portugal, the Douro, which extends some 200 miles (300 km) in the country, has been made navigable from near Porto to the Spanish frontier. In its upper reaches, the Douro riverbed drops 16 feet (5 metres) per mile in gorges 90 to 160 feet (30 to 50 metres) deep, a navigability problem resolved by locks built into five dams, including one that is 115 feet (35 metres) high. The longest river wholly in the country is the 137-mile (220-km) Mondego River, which rises in the Estrela Mountains. Other mainly Portuguese rivers include the Vouga, Sado, and Zêzere (a tributary of the Tagus). Like the Mondego, all are navigable for short distances. Rich silt land (campo) in the lower Tagus valley is the result of regular flooding, which is especially severe when strong southerly gales drive high seas up the estuary. The Guadiana, which flows south into the Gulf of Cádiz, forms part of the frontier with Spain, as does the Minho in the north.
All of Portugal’s main rivers flow from Spain over the edge of the Meseta in a series of defiles (narrow gorges), and their usefulness, either for navigation or as routeways for roads and railways, is thus limited. The longest river crossing Portugal, the Douro, which extends some 200 miles (300 km) in the country, has been made navigable from near Porto to the Spanish frontier. In its upper reaches, the Douro riverbed drops 16 feet (5 metres) per mile in gorges 90 to 160 feet (30 to 50 metres) deep, a navigability problem resolved by locks built into five dams, including one that is 115 feet (35 metres) high. The longest river wholly in the country is the 137-mile (220-km) Mondego River, which rises in the Estrela Mountains. Other mainly Portuguese rivers include the Vouga, Sado, and Zêzere (a tributary of the Tagus). Like the Mondego, all are navigable for short distances. Rich silt land (campo) in the lower Tagus valley is the result of regular flooding, which is especially severe when strong southerly gales drive high seas up the estuary. The Guadiana, which flows south into the Gulf of Cádiz, forms part of the frontier with Spain, as does the Minho in the north.


Portugal has more than 500 miles (800 km) of coastline, four-fifths of which faces westward. Except at the mouths of the larger rivers, there are few major indentations or natural harbours; the most important are those of Lisbon, on the Tagus, and Setúbal, on the Sado. The entrance to the Tagus is a long, narrow deepwater channel opening out into a broad expanse of inland water. Other harbours depend on the protection of headlands (e.g., the artificial harbours of Leixões and Sines).
Portugal has more than 500 miles (800 km) of coastline, four-fifths of which faces westward. Except at the mouths of the larger rivers, there are few major indentations or natural harbours; the most important are those of Lisbon, on the Tagus, and Setúbal, on the Sado. The entrance to the Tagus is a long, narrow deepwater channel opening out into a broad expanse of inland water. Other harbours depend on the protection of headlands (e.g., the artificial harbours of Leixões and Sines).


Soils
*Soils
Most of Portugal’s soils are arid, acidic, and sandy, though in the north the soil often is rocky. Except for parts of northern Portugal that receive significant precipitation and along the country’s primary rivers, which deposit fertile alluvium, the soils are not suitable for intensive agricultural production. In the central and southern parts of the country, the soils are generally poor and incapable of significant agricultural production without extensive irrigation schemes.
Most of Portugal’s soils are arid, acidic, and sandy, though in the north the soil often is rocky. Except for parts of northern Portugal that receive significant precipitation and along the country’s primary rivers, which deposit fertile alluvium, the soils are not suitable for intensive agricultural production. In the central and southern parts of the country, the soils are generally poor and incapable of significant agricultural production without extensive irrigation schemes.


Climate
*Climate
Climate, through its effect on vegetation, divides Portugal. As in Spain, three sets of influences are involved: Atlantic, continental (Mesetan), and Mediterranean. The Atlantic climate predominates overall, putting most of the country into the humid zone of the Iberian Peninsula; this is especially true in the northwest, where the climate is mild and rainy. Summer temperatures near sea level may average up to 76 °F (24 °C) but are rather lower at exposed higher elevations. Winter temperatures average 37 to 40 °F (3 to 4 °C) but tend to be milder south of the Douro. Annual rainfall averages more than 40 inches (1,000 mm).
Climate, through its effect on vegetation, divides Portugal. As in Spain, three sets of influences are involved: Atlantic, continental (Mesetan), and Mediterranean. The Atlantic climate predominates overall, putting most of the country into the humid zone of the Iberian Peninsula; this is especially true in the northwest, where the climate is mild and rainy. Summer temperatures near sea level may average up to 76 °F (24 °C) but are rather lower at exposed higher elevations. Winter temperatures average 37 to 40 °F (3 to 4 °C) but tend to be milder south of the Douro. Annual rainfall averages more than 40 inches (1,000 mm).


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Mediterranean, Saharan, and oceanic influences produce seasonal precipitation, occasional dry winds, and thermal equability, respectively, in the Madeiras. Climate varies markedly with altitude. In the Azores the anticyclone dominates, though conditions can be highly variable. Rainfall, for example, is irregular both in annual total and in regime: Horta (on Faial Island) may have more than 40 inches (1,000 mm) a year or may suffer severe drought.
Mediterranean, Saharan, and oceanic influences produce seasonal precipitation, occasional dry winds, and thermal equability, respectively, in the Madeiras. Climate varies markedly with altitude. In the Azores the anticyclone dominates, though conditions can be highly variable. Rainfall, for example, is irregular both in annual total and in regime: Horta (on Faial Island) may have more than 40 inches (1,000 mm) a year or may suffer severe drought.


Plant and animal life
*[[Plant and animal life-Portugal]]
VEGETATION
:VEGETATION
Portugal’s vegetation is a mixture of Atlantic, or European, and Mediterranean (with some African) species. Overall, the former accounts for some two-thirds of species, but the regional distribution is revealing. North of the Mondego valley, nearly three-fifths of the plants are European species (some seven-eighths in the northern interior), and only one-fourth are Mediterranean. In the south the proportions are three-tenths and nearly one-half, respectively. One-third are foreign species, introduced in periods of colonization.
Portugal’s vegetation is a mixture of Atlantic, or European, and Mediterranean (with some African) species. Overall, the former accounts for some two-thirds of species, but the regional distribution is revealing. North of the Mondego valley, nearly three-fifths of the plants are European species (some seven-eighths in the northern interior), and only one-fourth are Mediterranean. In the south the proportions are three-tenths and nearly one-half, respectively. One-third are foreign species, introduced in periods of colonization.--->[[Plant and animal life-Portugal|>>>Read More.<<<]]
 
Millennia of human activity have left Portugal with only one-fourth of its area under woodland. The remainder of the country features two types of Mediterranean scrublands—called maquis and matorral, or steppe. Mixed deciduous trees are confined to the north and northern interior, where the landscapes of the Minho are lush and green except for the heaths (mato) of the Cambrian schists. These carry erica, heather, cistus, and bracken. The original oak climax (with Quercus robur as the dominant species) has been largely replaced by maritime pine with some cork oak and extensive plantations of eucalyptus. Olives extended into the north in Roman times but are now generally limited to elevations below 1,200 feet (400 metres); inland, where the summer drought is longer, they can be found in some areas with elevations as high as 2,200 feet (700 metres). In the Douro valley, juniper scrub has been replaced by vineyards.
 
The thickest forests in Portugal are found in the traditional province of Beira, where cultivation is limited to less than one-fourth of the area. Pines prevail in the north, chestnut groves on the granites, and ericas on the dense maquis. The elevational succession of vegetation is strongly marked on the Estrela Mountains, where a zone of Pyrenean oak extends above the pedunculated oaks, chestnuts, and pines to 5,500 feet (1,700 metres), while southern slopes are covered with a maquis of cistus and tree heath. The central ridge marks the southern limit of deciduous oak, which is thereafter replaced by Q. lusitanica (Portuguese oak). Heat-loving stone pines mix with maritime pines.
 
In the south the Alentejo still has extensive matorral and charneca, uncultivated land dominated by cistus or groves of cork oak, often managed in estates, and holm oak. Most of the Algarve landscape is dominated by the vine and by trees typical of Mediterranean arboriculture—olive, fig, almond, and carob.
 
The rich vegetation of both Madeira and the Azores has been Europeanized. The climate encourages year-round growth of a considerable variety of flora. A wealth of ferns, mosses, heaths (especially tree heaths), and junipers reflects the influence of grazing and human activities on these islands. About 100 plants are peculiar to Madeira, either as indigenous or as highly individualized varieties. Only Madeira has much woodland, most of it the result of reforestation (e.g., of poplar, pine, and eucalyptus). Two-thirds of Madeira is a conservation area; its Laurel Forest (Laurisilva) was designated a UNESCO World Heritage site in 1999.
 
Parks, reserves, and other protected areas covering more than 5 percent of the mainland have been declared from the far north of Portugal (Peneda-Gerês and Montesinho) to the extreme south (Formosa River), from the east (Malcata Mountains and Guadiana valley) to the west (Berlengas Islands, Sintra), and in several areas of natural beauty in between. Since the mid-1980s, environmental concerns and ecological associations have grown slowly but steadily. In 1990, as part of an effort to expand protection of the environment, the government established an environment ministry.


==Demography of Portugal==
==Demography of Portugal==