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The Madre de Dios River (Spanish pronunciation: [ˈmaðɾe ðe ðjos]) is a river shared by Bolivia and Peru which is homonymous to the Peruvian region it runs through. On Bolivian territory, it receives the Beni River, close to the town of Riberalta, which later joins with the Mamore River to become the Madeira River after the confluence.
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The Piedras is the longest tributary of the 1,347 km long Madre de Dios River and more than 99 percent of its drainage is in the Amazon lowlands, below 400 meters. [5] The capital of the Las Piedras District is the town of Planchón, which is located in the province Tambopata in the Madre de Dios Department [6]
Madre de Dios (Spanish pronunciation: [ˈmaðɾe ðe ˈðjos] ⓘ, English: Mother of God) is a department and region in southeastern Peru, bordering Brazil, Bolivia and the Peruvian departments of Puno, Cusco and Ucayali, in the Amazon Basin. Its capital is the city of Puerto Maldonado.
Puerto Maldonado (Spanish pronunciation: [ˈpweɾto maldoˈnaðo] ⓘ) is a city in southeastern Peru in the Amazon rainforest 55 kilometres (34 mi) west of the Bolivian border, located at the confluence of the Tambopata and Madre de Dios rivers. The latter river joins the Madeira River as a tributary of the Amazon.
The Manu is a tributary to the 1,347 km long Madre de Dios River, which downriver joins the Madeira River, and ultimately the Amazon River. In the late 19th and early 20th centuries, this area of what was organized as the Madre de Dios region was exploited for the production of rubber during the rubber boom , with workers brought in by ...
The Fitzcarrald Isthmus is an 11 km long land bridge that connected important rubber trade routes of the Urubamba River and the Madre de Dios River in Peru. Carlos Fermin Fitzcarrald came across the land bridge in 1893 [1] after repeated attempts to unite trade in the North and South of the Amazon basin during the Amazon rubber boom. Based on ...
Español: Garimpo de ouro ilegal em larga escala no S da Amazônia Peruana, em Madre de Dios, anteontem. A mineração ocorre na zona de amortecimento da Reserva Nacional Tambopata, ao S do Rio Malinousqui, que corre na parte de baixo da imagem de O para L. Floresta em preto, nesse realce para destacar as cavas de mineração, com solo exposto em amarelo.