0 a higher area between the valleys of streams or rivers: --
In the Danube-Tisza interfluve, lakes are threatened by environmental problems.
Interfluves are areas of high terrain located between valleys.
The upland interfluve deposits are located at comparatively higher levels than the adjacent river channels with their active flood plains.
The fine-grained interfluve deposits are made up of silty-heterolithic associations.
The deposits of the upland interfluve area are highly oxidized, and show prominent mottling.
The active channels of the upland interfluve regions are small to moderate in dimension, and are groundwaterfed streams originating within the alluvial plain.
The major rivers incised in the regional surface neither contribute the sediment nor control the depositional processes of upland interfluve areas.
The interfluve surface shows the presence of many abandoned channel belts which receive no sediment or water from any major river system.
The cycle starts with minor creeks or gullies, which are formed to drain the excess rainwater on a widespread interfluve area.
The area has well-drained interfluves.
