The Park comprises an interfluvial peneplain of schist and granite between the Comoé and Volta rivers, with a mean altitude of 250 m to 300 m and a series of ridges and granite inselbergs rising to 600 m. ❋ Unknown (2009)
This interfluvial ecoregion is bound by the Solimões River (Amazon) to the south and the Japurá and Caquetá Rivers to the north. ❋ Unknown (2008)
This westernmost line was meant to distinguish the Napo ecoregion, to the west, from these interfluvial ecoregions as an area of Pleistocene refugia and butterfly endemism (see Napo moist forest description). ❋ Unknown (2008)
This interfluvial ecoregion is bound by the Tapajós River to the west, the Xingu River to the east and the Solimões (Amazon) River and várzea to the north. ❋ Unknown (2008)
The Tapajós-Xingu moist forest ecoregion lies in central-eastern Brazil south of the Amazon River, comprising the interfluvial plain between the Tapajós and Xingu Rivers, both major tributaries to the Amazon River. ❋ Unknown (2008)
This interfluvial region extends west from the Amazon City of Manaus at the confluence of the Rio Negro and Rio Solimões (Amazon), following these rivers until the latter forks with the Japurá at the City of Tefé. ❋ Unknown (2008)
This interfluvial ecoregion is bound on the east and across the southwest by the Tocantins River (the Tucurui Reservoir is not considered for historic coverage) and by the Pindare River and São Marcos Gulf in the east. ❋ Unknown (2008)
This interfluvial ecoregion is bound by the Purus and Solimões (Amazon) Rivers to the north and the Madeira River to the south. ❋ Unknown (2008)
The Purus-Madeira moist forest region lies in the center of the Brazilian Amazon south of the Amazon River on the interfluvial plain between the Purus and Madiera rivers. ❋ Unknown (2008)
This interfluvial ecoregion is bound by the Amazon Delta to the north, the Xingu River to the west, and the Tocantins River to the east. ❋ Unknown (2008)
The lowland forests occur on the alluvial plains and the interfluvial hills. ❋ Unknown (2008)
Its western flank constitutes a contact zone with the Srubnaya culture in the Volga-Ural interfluvial and extending eastward to the Minusinsk depression Fig. ❋ Unknown (2008)
One of the main canals which fertilized the interfluvial plain, passing through Nippur, was the nâr Kabari, which is identical with the river ❋ 1840-1916 (1913)
No common name has ever included all its parts, both the interfluvial region and the districts beyond Tigris; but since the term _Mesopotamia_, though obviously incorrect, is generally understood nowadays to designate it, this name may be used for want of a better. ❋ Unknown (1894)
