sandy bed. In times of drier climate, wind dominates and blows a lot of sediment into a weaker fluvial system, leading to aggradation and floodplain re-distribution. Currently, the Kobuk River in its middle and lower reaches is an anastomizing stream, with several braided channels in places, wide migrating meander bends, and oxbow lakes. It is controlled by yearly cycles of freeze and thaw, much like its surrounding landscape. For six months of the year, the river is largely still, frozen on top by a thick layer of ice. In the spring, warmer temperatures cause this ice to begin to melt. But the resulting process is not gradual. Rather, the pressure of melting ice from upstream builds up upon ice "dams" in the river's channel, eventually causing an "ice break-up" event, in which a flood of ice and water moves powerfully downstream. These annual spring break-up events have several important consequences. First, the river has deeply undercut and eroded banks, caused by large, fast-moving chunks of ice carving out the river's channel before it begins spilling out onto its floodplain, which is 1 to 6 miles (1.6-9.7 km) wide except at the confluence of major tributaries. Second, the river moves laterally very quickly and dramatically, re-inventing side channels every year as its secondary streams become drowned in each yearly flood by an overwhelming amount of sediment. Lastly, since the river is surrounded mostly by permafrost and because during the spring break-up event there are still large parts of frozen ground close to its banks, floods often transports large amounts of fine sediment across broad expanses of floodplain in thin sheets of water that slide easily across the frozen ground. These characteristics also translate into a relatively variable habitat for the Kobuk's native species. Farthest west, the Kobuk empties into Hotham Inlet, the easterly arm of Kotzebue Sound. During recent geologic times however, when sea level was lower, the Noatak, Kobuk, and Selawik Rivers were joined. Now, they have separate deltas with many lakes and swamps and intricately webbed channel systems. The deltas are composed primarily of silt, sand, and gravel. Surface water and hydrology The Kobuk River is ice covered 6 months of the year and in general, late October to late May is a period of relatively low flow. Annually, the hydrograph reflects two flood peaks: the first is associated with spring break-up and the second, a lesser peak, is