AMAZÔNIA AZUL / SYSGAAZ – Brazilian Navy

© copyright. Picture credit: Brazilian Navy (MB)

The Blue Amazon

 

In 1986, alongside Argentina, Uruguay and 21 African countries, Brazil proposed the South Atlantic Peace and Cooperation Zone. The unstated goal then, as now, was to minimize external meddling in the region, especially by NATO.

Brazil, in particular, wants to safeguard its on- and offshore natural resources, which the navy calls the Amazônia Azul, or Blue Amazon. These include extensive petroleum and gas reserves, as well as fishing and mining concessions within and beyond its current maritime frontiers.

To Brazilian leaders, preserving influence over the Blue Amazon is a question of national security and sovereignty. The Brazilian navy’s PROMAR program actively promotes public awareness campaigns extolling the economic, environmental, and scientific importance of the South Atlantic.

To secure the boundaries of the Blue Amazon, Brazil is petitioning the UN Commission on the Limits of the Continental Shelf to extend its exclusive economic zone, the area stretching 200 nautical miles out from the coast, in which a country has special rights to explore and use marine resources.

To shore up its demands, Brazil is creating a sophisticated surveillance system to monitor the Blue Amazon. The so-called Blue Amazon Management System is intended to scan more than 4,600 miles of coastline for foreign military and commercial vessels through a combination of satellites, radar, drones, naval vessels, and submarines.

In January 2015, Brazil named three finalists to develop the $4 billion project: a consortium led by the aerospace conglomerate Embraer, another led by the multinational construction company Odebrecht, and a third by the aerospace upstart Orbital Engenharia. The Brazilian army is also building a multibillion-dollar terrestrial border surveillance system – SISFRON -, and the two programs may eventually be integrated.

BRAZILs-COST-AMBITION-Igarapé-Institute3

© copyright. Picture credit: Brazilian Navy (MB)

AMAZÔNIA AZUL

The Blue Amazon (Portuguese: A Amazônia Azul) or Brazilian maritime territory (Portuguese: território marítimo brasileiro) is the exclusive economic zone (EEZ) of Brazil. It is currently  an offshore area of 3.6 million square km on the Brazilian coast, rich in marine biodiversity and energy resources. The size is equivalent to the surface of the Amazon rainforest. The name is a reference to the biologically rich region of the Brazilian Amazon, with the addition of the adjective blue denoting the ocean. Brazil celebrates the day of Amazônia Azul on November 16th.

The area may be expanded to 4.4 million square kilometres in view of the Brazilian claim that was submitted to the United Nations Commission on the Limits of the Continental Shelf (CLCS) in 2004. It is proposed to extend Brazil’s continental shelf to 900 thousand square kilometers of marine soil and subsoil, which the country will be able to explore. With the extension, the area will become more contiguous, including the areas of Brazilian archipelagos in the South Atlantic . The region with the largest Blue Amazon is the Northeast, due to the existence of several islands that are well spaced from each other in a contiguous marine zone (the island of Trindade is too far from the coast for the same to occur).

If considering all claims attended, and if including the volume of its 60,000 km of internal rivers, the total would reach 5,7 million km2.

Brazil has about 7,000km of cost border, including 17 states and 280 cities. It is totally linked to the ocean, through various factors (historical, climatic, geographical, environmental, economical), highly influencing food, health, sports, well-being etc. 97% of the Brazilian Petroleum is extracted from the marine subsoil. And the trend is quickly going up, as per the pré-sal new reservoirs, now estimated in 38 e 44 billion barrels. Naval construction, tourism, nautic sports, maritime transportation and fishing also have strong growth potential though the Brazilian seas. Its vast biodiversity and maritime mineral resources represent a huge strategic reserve for current and future Brazilian generations. Long course cabotage currently drains 95% of the foreign trade. 90% of Brazilian GDP (PIB), 80% of the Brazilian population and 85% of its industrial park located less than 200 km away from its coast.

Hence Brazil is a coastal country, with an unquestionable maritime vocation.

Economic potential

This region has many riches and potential for various types of economic use:

  • Fishing, due to the enormous diversity of marine species that reside in this region.
  • Metallic minerals and other mineral resources in the seabed;
  • Enormous biodiversity of marine species that reside in this region.
  • Oil, as found in the Campos Basin and in the Pre-salt layer (Campos BasinSantos Basin and Espírito Santo Basin – prospecting in these areas already accounts for two million barrels of oil per day, 90% of the current Brazilian production );
  • Use of tidal energy and wind energy on the high seas or offshore.

History

With the entry into force of the United Nations Convention on the Law of the Sea (UNCR) in 1995, and in accordance with its provisions, by which rocks without permanent human occupation do not give the right to the establishment of an Exclusive Economic Zone, aiming to explore, to conserve and manage the resources of the region, Brazil – which already occupied the archipelago of Trindade and Martin Vaz, now also occupies the Saint Peter and Saint Paul Archipelago. This decision elevated them to the status of an archipelago, allowing the country to expand its EEZ by 450 thousand square kilometers, an area equivalent to the Brazilian state of Bahia.

Geography

Region EEZ Area (km2)
Mainland Brazil 2,570,917
 Trindade and Martim Vaz Islands 468,599
 Saint Peter and Saint Paul Archipelago 413,636
Bandeira de Fernando de Noronha.png Fernando de Noronha Islands 363,362
Total 3,830,955

References

  1. ^ Wiesebron, Marianne (January–June 2013). “Blue Amazon: Thinking The Defense of The Brazilian Maritime Territory”Austral: Brazilian Journal of Strategy & International Relations2 (3): 101–124. Retrieved 20 December 2017.
  2. ^ Ortiz, Fabiola. “The Blue Amazon, Brazil’s New Natural Resources Frontier”Inter Press Service. Inter Press Service News Agency. Retrieved 20 December 2017.
  3. ^ UN Continental Shelf and UNCLOS Article 76: Brazilian Submission
  4. ^ Gonçalves, J. B. – Direitos Brasileiros de Zona Econômica Exclusiva…
  5. ^ Ilhas do Brasil: O Brasil além das 200 milhas. O Globo, 12 de outubro de 2008, p. 59.
  6. ^ See Around Us Project (n.d.). “Exclusive Economic Zones (EEZ)”. Retrieved 3 June 2015EEZ waters of: Mainland Brazil 2,570,917 km2, Fernando de Noronha Islands 363,362 km2, Saint Peter and Saint Paul Archipelago 413,636 km2, and the Trindade and Martim Vaz Islands 468,599 km2

 

SISGAAZ – Sistema de Gerenciamento da Amazônia Azul

(Blue Amazon Management System)

 

© copyright. Picture credit: Brazilian Navy (MB) / Brazilian Air Force (FAB).

Future RFPs would be prepared by Fundação EZUTE

 

PNM – Programa Nuclear da Marinha (Brazilian Navy Nuclear Program)

© copyright. Picture credit: Brazilian Navy (MB)

 

The Submarine Development Program (PROSUB) is one of the main strategic projects of the Brazilian Armed Forces and aims to increase the national defense structure and ensure Brazilian maritime sovereignty, supporting AMAZÔNIA AZUL program. See more details on the respective use case at our case list: PROSUB / PNM

 

AMAZÔNIA FLUVIAL (the The Amazon River Basin):

Amazon River, Portuguese Rio Amazonas, Spanish Río Amazonas, also called Río Marañón and Rio Solimões, the greatest river of South America and the largest drainage system in the world in terms of the volume of its flow and the area of its basin. The total length of the river—as measured from the headwaters of the Ucayali-Apurímac river system in southern Peru—is at least 4,000 miles (6,400 km), which makes it slightly shorter than the Nile River but still the equivalent of the distance from New York City to Rome. Its westernmost source is high in the Andes Mountains, within 100 miles (160 km) of the Pacific Ocean, and its mouth is in the Atlantic Ocean, on the northeastern coast of Brazil. However, both the length of the Amazon and its ultimate source have been subjects of debate since the mid-20th century, and there are those who claim that the Amazon is actually longer than the Nile. (See below The length of the Amazon.).

© copyright. Picture credit: Brazilian Navy (MB)

 

The waterway mesh has more than  60,000 km of Rivers, just inside Brazil. It has a huge importance from the logistic, strategic and environmental perspectives.

The vast Amazon basin (Amazonia), the largest lowland in Latin America, has an area of about 2.7 million square miles (7 million square km) and is nearly twice as large as that of the Congo River, the Earth’s other great equatorial drainage system. Stretching some 1,725 miles (2,780 km) from north to south at its widest point, the basin includes the greater part of Brazil and Peru, significant parts of ColombiaEcuador, and Bolivia, and a small area of Venezuela; roughly two-thirds of the Amazon’s main stream and by far the largest portion of its basin are within Brazil.

The Tocantins-Araguaia catchment area in Pará state covers another 300,000 square miles (777,000 square km). Although considered a part of Amazonia by the Brazilian government and in popular usage, it is technically a separate system. It is estimated that about one-fifth of all the water that runs off Earth’s surface is carried by the Amazon. The flood-stage discharge at the river’s mouth is four times that of the Congo and more than 10 times the amount carried by the Mississippi River. This immense volume of fresh water dilutes the ocean’s saltiness for more than 100 miles (160 km) from shore.

The extensive lowland areas bordering the main river and its tributaries, called várzeas (“floodplains”), are subject to annual flooding, with consequent soil enrichment; however, most of the vast basin consists of upland, well above the inundations and known as terra firme. More than two-thirds of the basin is covered by an immense rainforest, which grades into dry forest and savanna on the higher northern and southern margins and into montane forest in the Andes to the west. The Amazon Rainforest, which represents about half of the Earth’s remaining rainforest, also constitutes its single largest reserve of biological resources.

Since the later decades of the 20th century, the Amazon basin has attracted international attention because human activities have increasingly threatened the equilibrium of the forest’s highly complex ecology. Deforestation has accelerated, especially south of the Amazon River and on the piedmont outwash of the Andes, as new highways and air transport facilities have opened the basin to a tidal wave of settlers, corporations, and researchers. Significant mineral discoveries have brought further influxes of population. The ecological consequences of such developments, potentially reaching well beyond the basin and even gaining worldwide importance, have attracted considerable scientific attention (see Sidebar: Status of the World’s Tropical Forests).

The Amazon River basin (ca. 6 million km2) is the largest in the world with mean discharge measured in the Amazon River at the outlet of ca. 206 000 m3  and sediment yields estimated to 800-1200 Mt.yr-1.  It is home to the largest rainforest in the world. The Amazon River brings nearly on fifth of the freshwaters delivered to the oceans (Callède et a., 2010), 7% of dissolved chemical species and 5% of the riverborne sediments (Degens et al., 1991), worldwide.

It is bounded to the west by the Andes Mountains, which represents only 10% of the area, but plays a key role on climate (precipitation gradient), hydrology and supplies (weathering, erosion) considerable volumes of material (Dunne et al., 1998; Aalto et al., 2006). In the last few years, the region has gone through severe drought episodes that have caused significant problems to the local population as well as to many ecosystems. Moreover, flood events are also common and affect yearly the routine of many large cities in the region (Marengo et al., 2008; Espinoza et al., 2009; Lewis et al., 2011). Detailing all aspects of this huge river basin is critical to understand its short- and long-term physico-chemical behavior, and the use of isotope tracers allow to trace the origin of chemical elements (Allègre et al., 1996), their recycling in the basin (Dosseto et al., 2006; Wittmann et al., 2011), and also potentially track the impact of deforestation on erosion (Poitrasson et al., 2009).

It must be stressed that the topic of environmental monitoring is pertinent for a long term study over a regional size object such as the Amazon Basin, as it is possible to encompass the local to global complex relationship on climate. Actually, the human uses of these rich ecosystems may have a significant impact on the greenhouse gas production or retention. Moreover, the Amazon Basin has a huge hydro-electric potential, largely unused. Hydroelectric reservoirs can be an important outgassing source of methane, which is one of the major greenhouse effect gas. Consequently, observing technical and operational recommendations, as well as limiting the numbers or the size of the dams, could be very efficient for greenhouse effect mitigation.

With the introduction of Global Positioning System (GPS) technology in the 1990s, researchers again attempted to navigate the entire length of the Amazon. The American geographer Andrew Johnston of the Smithsonian Institution’s Air and Space Museum in Washington, D.C., employed GPS gear to explore the various Andean rivers that flow into the Amazon. Using the definition of the river’s source as being the farthest point from which water could flow into the ocean and where that water flows year-round (thereby eliminating those rivers that freeze in winter), he concluded that the source was Carruhasanta Creek on Mount Mismi.

By the early 21st century, advanced satellite-imagery technology was allowing researchers to match the river’s dimensions even more precisely. In 2007 an expedition that included members of Brazil’s National Institute for Space Research and other organizations traveled to the region of Carruhasanta and Apacheta creeks in an attempt to determine which of the two was the “true” source of the Amazon. Their data revealed that Apacheta was 6 miles (10 km) longer than Carruhasanta and carries water year-round, and they concluded that Apacheta Creek was indeed the source of the Amazon River. The team then proceeded to measure the river’s length. As part of this process, they had to determine from which of the Amazon’s three main outlets to the sea to begin the measurement—the Northern or Southern channels, which flow north of Marajó Island, or Breves Channel, which flows southward around the western edge of the island to join the Pará River estuary along the southern coast of the island. They chose to use the southern channel and estuary, since that constituted the longest distance from the source of the river to the ocean (at Marajó Bay); according to their calculations, the southern outlet lengthened the river by 219 miles (353 km). Their final measurement for the length of the Amazon—from Apacheta Creek to the mouth of Marajó Bay—was about 4,345 miles (6,992 km).

This team of researchers, using the same technology and methodology, then measured the length of the Nile River, which they determined to be about 4,258 miles (6,853 km); that value was some 125 miles (200 km) longer than previous calculations for the Nile but nearly 90 miles (145 km) shorter than the length the group gave for the Amazon. These measurements infer that the Amazon may be recognized as the world’s longest river, supplanting the Nile. However, a river like the Amazon has a highly complex and variable streambed—made more so by seasonal climatic factors—which complicates the process of obtaining an accurate measurement. Thus, the final length of the river remains open to interpretation and continued debate.

Landforms and drainage patterns

The Amazon basin is a great structural depression, a subsidence trough that has been filling with immense quantities of sediment of Cenozoic age (i.e., dating from about the past 65 million years). This depression, which flares out to its greatest dimension in the Amazon’s upper reaches, lies between two old and relatively low crystalline plateaus, the rugged Guiana Highlands to the north and the lower Brazilian Highlands (lying somewhat farther from the main river) to the south. The Amazon basin was occupied by a great freshwater sea during the Pliocene Epoch (5.3 to 2.6 million years ago). Sometime during the Pleistocene Epoch (about 2,600,000 to 11,700 years ago) an outlet to the Atlantic was established, and the great river and its tributaries became deeply entrenched in the former Pliocene seafloor.

The modern Amazon and its tributaries occupy a vast system of drowned valleys that have been filled with alluvium. With the rise in sea level that followed the melting of the Pleistocene glaciers, the steep-sided canyons that had been eroded into the Pliocene surface during the period of lower sea levels were gradually flooded. In the upper part of the basin—in eastern ColombiaEcuador, Peru, and Bolivia—more-recent outwash from the Andes has covered many of the older surfaces.

Physiography of the river course

The Amazon River’s main outlets are the two channels north of Marajó Island, a lowland somewhat larger in size than Denmark, through a cluster of half-submerged islets and shallow sandbanks. There the mouth of the river is 40 miles (64 km) wide. The port city of Belém, Brazil, is on the deep water of the Pará River estuary south of Marajó. The Pará is fed chiefly by the Tocantins River, which enters the Pará southwest of Belém. The port city’s link with the main Amazon channel is either north along the ocean frontage of Marajó or following the deep but narrow furos (channels) of Breves that bound the island on the west and southwest and link the Pará River with the Amazon. There are more than 1,000 tributaries of the Amazon that flow into it from the Guiana Highlands, the Brazilian Highlands, and the Andes. Six of these tributaries—the Japurá (Caquetá in Colombia), JuruáMadeiraNegroPurus, and Xingu rivers—are each more than 1,000 miles (1,600 km) long; the Madeira River exceeds 2,000 miles (3,200 km) from source to mouth. The largest oceangoing ships can ascend the river 1,000 miles to the city of Manaus, Brazil, while lesser freight and passenger vessels can reach Iquitos, Peru, 1,300 miles (2,090 km) farther upstream, at any time of year.

The sedimentary axis of the Amazon basin comprises two distinct groups of landforms: the várzea, or floodplain of alluvium of Holocene age (i.e., up to about 11,700 years old), and the terra firme, or upland surfaces of Pliocene and Pleistocene materials (those from 11,700 to 5,300,000 years old) that lie well above the highest flood level. The floodplain of the main river is characteristically 12 to 30 miles (19 to 50 km) wide. It is bounded irregularly by low bluffs 20 to 100 feet (6 to 30 metres) high, beyond which the older, undulating upland extends both north and south to the horizon. Occasionally these bluffs are undercut by the river as it swings to and fro across the alluvium, producing the terra caída, or “fallen land,” so often described by Amazon travelers. At the city of Óbidos, Brazil, where the river width is some 1.25 miles (2 km), a low range of relatively hard rock narrows the otherwise broad floodplain.

The streams that rise in the ancient crystalline highlands are classified as either blackwater (JariNegro, and Tocantins-Araguaia) or clearwater (TrombetasXingu, and Tapajós). The blackwater tributaries have higher levels of humic acids (which cause their dark colour) and originate in nutrient-poor, often sandy uplands, so they carry little or no silt or dissolved solids. Clearwater tributaries have a higher mineral content and lower levels of humic acids. Some rivers flow as clearwater during the rainy season and blackwater during the dry season. Where such blackwater tributaries enter the main river, they are sometimes blocked off to form funnel-shaped freshwater lakes or estuaries, as at the mouth of the Tapajós.

In contrast, the Madeira River, which joins the Amazon some 50 miles (80 km) downstream from Manaus, and its principal affluents—the Purus, Juruá, Ucayali, and Huallaga on the right or southern bank and the Japurá, Putumayo (Içá in Brazil), and Napo from the northwest—have their source in the geologically youthful and tectonically active Andes. There they pick up the heavy sediment loads that account for their whitewater designation. Where the silt-laden waters of the Amazon (Solimões in Brazil), derived from these streams, meet those of the Negro at Manaus, the darker and hence warmer and sediment-free waters of the latter tend to be overrun by those of the Amazon, creating a striking colour boundary that is erased by turbulence downstream.

The mother river, the Marañón above Iquitos, rises in the central Peruvian Andes at an elevation of 15,870 feet (4,840 metres) in a small lake in the Cordillera Huayhuash above Cerro de Pasco. The Huallaga and Ucayali, major right-bank affluents of the Marañón, originate considerably farther south. The headwaters of the deeply entrenched Apurímac and Urubamba, tributaries at the confluence of the Ucayali, reach to within 100 miles (160 km) of Lake Titicaca, the farthest of any stream in the system from the great river’s mouth.

The Negro River, the largest of all the Amazon tributaries, accounts for about one-fifth of the total discharge of the Amazon, and 40 percent of its aggregate volume is measured just below the confluence at Manaus. Its drainage area of about 292,000 square miles (756,000 square km) includes that of the Branco, its major left-bank tributary, with its source in the Guiana Highlands. Another of the Negro’s affluents, the Casiquiare, is a bifurcation of the Orinoco River; it forms a link between the Amazon and the Orinoco’s drainage system. The Branco watershed, approximately coincident with the state of Roraima, includes extensive tracts of sandy, leached soils that support a grassy and stunted arboreal cover (campos). Other tributaries of the Negro, such as the Vaupés and Guainía, drain eastward from the Colombian Oriente. The river traverses some of the least populous and least disturbed parts of the Amazon basin, including several national parks, national forests, and indigenous reserves. In its lower reaches the Negro becomes broad and island-filled, reaching widths of up to 20 miles (32 km) in certain locations.

The Madeira River, the second largest affluent of the Amazon, has a discharge of perhaps two-thirds that of the Negro. Silt from its turbid waters has choked its lower valley with sediments; where it joins the Amazon below Manaus, it has contributed to the formation of the 200-mile- (320-km-) long island of Tupinambarana. Beyond its first cataract, 600 miles (970 km) up the river, its three major affluents—the Madre de Dios, the Beni, and the Mamoré—provide access to the rubber-rich forests of the Bolivian Oriente; the meandering Purus and Juruá rivers that flank the Madeira on the west are also important tributaries that lead into those forests. Mamoré’s tributary, the Guaporé, opens up to the Mato Grosso Plateau.

Hydrology of the Amazon River

Most of the estimated 1.3 million tons of sediment that the Amazon pours daily into the sea is transported northward by coastal currents to be deposited along the coasts of northern Brazil and French Guiana. As a consequence, the river is not building a delta. Normally, the effect of the tide is felt as far upstream as Óbidos, Brazil, 600 miles (970 km) from the river’s mouth. A tidal bore called the pororoca occurs at times in the estuary, prior to spring tides. With an increasing roar, it advances upstream at speeds of 10 to 15 miles (16 to 24 km) per hour, forming a breaking wall of water from 5 to 12 feet (1.5 to 4 metres) high.

At the Óbidos narrows, the flow of the river has been measured at 7,628,000 cubic feet (216,000 cubic metres) per second; its width is constricted to little more than a mile. Here the average depth of the channel below the mean watermark is more than 200 feet (60 metres), well below sea level; in most of the Brazilian part of the river its depth exceeds 150 feet (45 metres). Its gradient is extraordinarily slight. At the Peruvian border, some 2,000 miles (3,200 km) from the Atlantic, the elevation above sea level is less than 300 feet (90 metres). The maximum free width (without islands) of the river’s permanent bed is 8.5 miles (14 km), upstream from the mouth of the Xingu. During great floods, however, when the river completely fills the floodplain, it spreads out in a band some 35 miles (55 km) wide or more. The average velocity of the Amazon is about 1.5 miles per hour, a speed that increases considerably at flood time.

The rise and fall of the water is controlled by events external to the floodplain. The floods of the Amazon are not disasters but rather distinctive, anticipated events. Their marked regularity and the gradualness of the change in water level are due to the enormous size of the basin, the gentle gradient, and the great temporary storage capacity of both the floodplain and the estuaries of the river’s tributaries. The upper course of the Amazon has two annual floods, and the river is subject to the alternate influence of the tributaries that descend from the Peruvian Andes (where rains fall from October to January) and from the Ecuadoran Andes (where rains fall from March to July). This pattern of alternation disappears farther downstream, as the two seasons of high flow gradually merge into a single one. Thus, the rise of the river progresses slowly downstream in a gigantic wave from November to June, and then the waters recede until the end of October. The flood levels can reach from 40 to 50 feet (12 to 15 metres) above low river.

Waterways Logistic

The waterways are of extreme importance for life, economy and integration at the region, allowing efficuency and capilarity.

 

A barge travels on the Mississippi River near Baton Rouge, Louisiana.

© copyright. Picture credit: Brazilian Navy (MB)

Early settlement patterns

The Amazon basin has long been relatively uninhabited. At the time of the European conquest, the bottomlands and fringing upland surfaces of the Amazon River and its major tributaries supported relatively dense, sedentary populations of indigenous peoples who practiced intensive root-crop farming, supplemented by fishing and by hunting aquatic mammals and reptiles. The more-elevated areas away from the rivers and their floodplains were—and still are in some of the more remote sectors—inhabited by small, widely dispersed, seminomadic tribes of Indians. These groups traditionally have relied predominantly on hunting large and small animals and on gathering wild fruits, berries, and nuts while practicing small-patch agriculture of low yield. In the early 1990s the Indian population of the Amazon basin numbered about 600,000, of whom perhaps close to one-third lived in Brazil and the rest in the Oriente regions of the four Andean countries. However, by the early 21st century the Indian population had dropped to fewer than 200,000, partly as a result of deforestation and commercial exploitation on their lands.

The Amazonian Indians early devised means of making the poisonous bitter cassava (manioc) edible; the end product, called farinha, became a food staple widely used today in much of tropical America. Amazonian Indians perfected the use of quinine as a specific against malaria, extracted cocaine from the leaves of the coca tree, and collected the sap of the Brazilian rubber tree. They were skilled navigators in their dugout canoes and sailing rafts (jagandas), and they invented the blowgun and the hammock. One of their arrow poisonscurare, has been used to treat a host of paralyses and spastic disorders, including multiple sclerosis.

The early European explorers of the Amazon provisioned themselves from the food supplies of the Indians they met and commandeered their canoes. Large numbers of Indians were taken into slavery, especially during organized raids (bandeiras) from the 16th to the 18th century; many others succumbed to such European diseases as influenzameasles, and smallpox. The result was a complete breakdown of native life and a precipitous decrease in the Indian population; survivors fled into increasingly inaccessible sections of the Amazon basin. As late as 1906 there were reports of the wholesale capture of Indians who were enslaved in order to tap rubber, which was plentiful and commanded a high price on the world market but which was difficult to exploit because rubber trees were sparsely scattered over a huge area.

Settlement by Europeans and mestizos (those of mixed Indian and European ancestry) did not occur to any appreciable degree until the 1870s and ’80s, when victims of severe droughts in northeastern Brazil began to move into Amazonia to profit from the rubber boom. Another wave of immigration began at the end of World War II, spurred by the rapid economic development of the region.

Most of the surviving Indian peoples live in the remote areas of the basin. Those living north of the Amazon River speak languages of the Arawaks and Caribs, while those to the south speak predominantly Tupian languages. Tupian was used as a lingua franca between Europeans and Indians until the Portuguese became dominant in the 19th century; nonetheless, Brazilian Portuguese has been heavily influenced by Tupian. Finally, there are known to be “undiscovered” Indian groups living in the Amazon region—i.e., those located so remotely that they have yet to be encountered or who have intentionally been left alone by outsiders.

Contemporary settlement patterns

The increasingly effective control of malaria, improved diets and sanitation, and the greater ease of transportation had made the Amazon basin more attractive for human settlement by the late 20th century. Increased activities related to resource exploitation have contributed to the transformation of the Amazon and its vast hinterland, especially in Brazil. Indeed, its vast area notwithstanding, the Amazon basin in the early 21st century had a predominantly urban population. Almost one-third of the estimated nine million Brazilians living in the 1.9 million-square-mile (5.2 million-square-km) area officially designated as Legal Amazonia are concentrated in Belém and Manaus, cities with more than one million inhabitants each, and in Santarém. These cities, which are logistic bases of operations for cattle ranching, mining, timber, and agroforestry projects, are still growing rapidly, with modern residential towers and shantytowns standing side by side. Even frontier trading centres in the interior, such as Marabá, Pôrto Velho, and Rio Branco, have significant populations. Some places in the upper reaches of the drainage area have become significant urban centres with most of the amenities of modern life—such as Florencia and Leticia in Colombia; IquitosPucallpa, Tarapoto, and Puerto Maldonado in Peru; and Santa Cruz in Bolivia. These cities and towns, and even the more isolated settlements and mission stations of the Oriente, are all accessible by plane.

 

Economy

 

Development of the Amazon basin

Since World War II the economic development of the Amazon basin has been a priority for the countries it spans. From the mid-1940s onward a number of “penetration roads” have been built from the populous highlands of ColombiaEcuadorPeru, and Bolivia into the Oriente. These roads have funneled untold numbers of landless peasants into the lowlands. They also have served to facilitate development of major oil discoveries and timber resources. Tropical hardwoods, river fish, and, since the 1980s, clandestinely produced cocaine have been objects of commercial exploitation, along with Brahman-type livestock raised on pastures newly carved from the selva. Such activities have led to widespread displacement of indigenous groups, who have been either forced onto new reserves or left to survive as best they could.

The opening of the Amazon basin has been pursued most aggressively in Brazil. In the mid-1950s the decision was made to refocus the country toward its interior by constructing a new inland capital, Brasília. One consequence of this decision was the initiation of a massive road-building program that aimed at integrating the North (consisting of the present-day states of AcreAmapáAmazonasParáRondônia, and Roraima) with the rest of Brazil while establishing an escape valve for the crowded and drought-stricken Northeast. A 1,100-mile- (1,770-km-) long highway linking Brasília with Belém, the trade centre at the mouth of the Amazon, was completed in 1964. The even more ambitious 3,400-mile (5,100-km) all-weather Transamazonian Highway from the Atlantic port of Recife to Cruzeiro do Sul on the Peruvian border—with extensions north to Santarém and Manaus (later to the Venezuelan border) and southward to Cuiabá (Mato Grosso) and Pôrto Velho (Rondônia)—was to provide the frame for a network of nearly 20,000 miles (32,000 km) of highways and feeder routes that was to supersede the traditional fluvial transport system. By the early 21st century the highway had not been completed, and it remained largely unpaved and impassable at several points.

Mining & Energy

The exploitation of the enormously rich mineral complex of the Serra dos Carajás area west of the town of Marabá on the Tocantins River has been highly profitable, but it has also had harmful effects on the environment. This site, one of the world’s largest and richest iron ore deposits, also produces gold, copper, nickel, manganese, tin, and bauxite. The million-acre concession is run by Vale do Rio Doce (CVRD; now known as Vale); initially, it was a partnership between private capital and the federal government, but it was privatized in 1997. Vale’s plans for the local smelting of the iron ore in the 2000s required the clearing of thousands of acres of forest annually to provide charcoal for producing pig iron. A rail line connects the Carajás development with the Atlantic coast.

Gold mining reached a feverish pitch in the 1980s, stimulated by high world prices of gold. At the height of the Amazon “gold rush,” as many as a half million transient miners (garimpeireos) came equipped with picks, shovels, and sluice boxes to search for the mineral in the alluvial deposits of the Tocantins valley at Serra Pelada. Brazil’s annual production peaked in 1987 but declined thereafter. Large amounts of the mercury used to extract the gold were released into rivers and caused the fish, which are so important in the local diet, to become unsafe to eat. Moreover, since the 1990s mercury contamination has grown among Amazonian peoples, especially those groups that are more isolated and consume large amounts of fish. On the Madeira River, teams operating from rafts pump up from the riverbed auriferous sediments, which have to be subjected to a treatment similar to that used in gold mining. Bauxite mining, both at Carajás and on the Trombetas River north of the Amazon, requires the use of large settling ponds to trap effluents.

The energy requirements of both the Carajás development and the city of Belém are met by the giant Tucuruí hydroelectric plant on the Tocantins River, one of the largest hydroelectric power stations in the world. A more modest hydroelectric facility on a small river north of Manaus supplies that city with power. A growing sensitivity to the harmful consequences for both human beings and the environment due to the construction of large dams has caused several ambitious projects to be placed on hold.

The principal oil developments within Amazonia have taken place in the Oriente regions of the Andean countries. Oil pipelines originate from districts in both Colombia (the upper Putumayo) and Ecuador (Agrio Lake), as well as northeastern

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