Mamberamo River
The Mamberamo is the second-longest river on the island of New Guinea, after Sepik River and the second largest in Oceania by discharge volume after Fly. It is located in the Indonesian province of Papua. It is the second largest river in Indonesia by volume of discharge after Kapuas and also the widest.
The river is formed from the confluence of its upper tributaries, the Tariku and Taritatu Rivers in the Lakes Plains region, an interior basin with extensive freshwater swamp forests and grasslands. It flows northwards between the Van Rees Range and Foja Mountains through a series of rapids and gorges. The last 160 km of the river are navigable. In the coastal lowlands, the river is lined with marshes and forms a broad river delta. The Mamberamo discharges into the Pacific Ocean at the northern point of Point D'Urville or Cape Narwaku.
The river's huge valley is home to various uncontacted peoples and incredible biodiversity. In the 1990s, the Indonesian Government had plans to construct a large hydroelectric dam on the Mamberamo that would have submerged much of the area. This plan was shelved after the Indonesian financial crisis from 1998 to 1999, but there are concerns by environmental groups that it could be resurrected sometime in the future. At present, the Mamberamo remains the second largest river in the world to be completely unfragmented by dams in its catchment, behind only the relatively nearby Fly.
The Mamberamo area also broadly refers to several nearby mountain ranges, including the Van Rees and Foja Mountains, which were the subject of a recent rapid biological assessment conducted by Conservation International, the Indonesian Institute of Sciences, and Cenderawasih University. The scientific team discovered the first new bird species from New Guinea in 60 years, and a wealth of other new plants and animals. The Foya Mountains appear to be a globally outstanding repository of biodiversity.
Hydrology
Its length from the confluence of the Tariku and Taritatu is. From the source of the Waruta, it covers a total distance of. It has a catchment area of with an annual rainfall of 3,578 mm. Average width is, depth .Tributaries
The main tributaries from the mouth:Discharge
Average monthly flow at delta in 2003–2012: 5,014 m3/sMamberamo River average discharge:
Geology
The region is geologically young and remains tectonically active, with frequent earthquakes and landslides in the steepest areas. The mountain basin called "Mamberamo" is composed mostly of high floodplains, extensive swamps, forested wetlands, meandering rivers and backwater lakes. The sediment-rich rivers in the catchment belong to 'white-water' systems similar to the Amazonian moors. Three soil orders are present, of which the inceptisols are the most widespread, followed by ultisols and entisols. All soils are fine textured with poor drainage. The diversity of the region is a result of its geological history, which gives rise to a diversity of habitats. Riparian forests within the Mamberamo Basin are heavily influenced by dynamic river meanders that continually modify the landscape, with some banks eroding rapidly while others grow as new sediments accumulate.Ecology and vegetation
The Mamberamo Basin is one of the most important biodiversity hotspots in New Guinea. Both Asian and Australo-Pacific elements are present in terms of botanical affinities. One survey at the foothills of the Foja Mountains identified 487 putative plant species, 156 of which are not assigned to known taxa, indicating a high proportion of undescribed species. The floodplain forests of the basin include swamp forests, seasonally flooded lakeside forests and sago forests.Seven general vegetation categories are distinguished in the landscape: primeval forest, swamp forest, lakeside forest, sago forest dominated by sago palm, secondary forest, mixed forest and sago woodland. Two other types are also recognised: montane forest and damar forest.The region has a low population density. The majority of people live from subsistence activities: hunting, fishing and small-scale agriculture. Trades include crocodile skins, dried fish and gaharu. Mixed crop gardens are located near the dwelling or on the river banks and are mostly planted with sweet potatoes and manioc. In these gardens, people plant bananas, coconuts and various vegetables.
Crocodiles are common in the rivers. The globally endangered Scott's kangaroo is thought to occur in the Foja Mountains, while the northern cassowary, Victoria-crowned dove and black-spotted couscous form significant populations. Local endemic species include Philemon brassi, Amblyornis flavifrons, the Salvadoran fig parrot, and a number of frog, invertebrate and plant species. More than 70 new species have been reported. Noteworthy vertebrates include the rediscovery of the endemic Berlepsch's bird of paradise. As well as several new species, including the honeyeater, the pigeon, the dwarf opossum, the giant rat, a Dorcopsulus and a bow-fingered gecko.
History
In 1545, the Spanish navigator Iñigo Ortiz de Retes sailed along the northern coast of the island as far as the mouth of this river that he charted as San Agustín. At this spot, on 20 June 1545, he claimed the territory for the Spanish Crown, and in the process bestowed the name to the island by which it is known today.The first European to enter the mouth of the Mamberamo was Dutchman Dr D. F. van Braam Morris in 1883. The residents from the northern Moluccas rowed up the river to ascertain that it was navigable by steamer. The following year in 1884 Van Braam Morris returned to the steamship Havik and travelled along its course.