Figure I: The Upper Mainstem Willamette River, Oregon, USA. Photo by Steve Cline,
USEPA-Corvallis. Despite being channelized in the early 20th century and having multiple
hydropower dams in its major tributaries, the upper mainstem of this floodplain river retains channel
complexity in the form of side channels, islands, and alcoves.
Figure II: Rio das Velhas, Minas Gerais, Brazil. Photo taken by Carlos Alves, Manuelzao Project.
Lacking mainstem or major tributary dams, the das Velhas floods during the rainy season and
supports multiple, permanent, off-channel lakes (lagoas) providing reproductive and rearing habitat
for aquatic vertebrates.
Figure III: Upper Danube River, Germany. Photo taken by Ashley Steel. This large floodplain river
has lost much of its floodplain connectivity as a result of channelization and system-wide dams and
locks.
Figure IV: Tagliamento River, Italy. Photo taken by Susanne Muhar. The Tagliamento is one of the
largest undammed rivers in western Europe and its braided and anastamosed channels are indicative
of high bedload from the Alps.
Figure V: Mekong River and its tributary in Cambodia. Photo taken by Seiichi Nohara during the
rainy season. The tributary of this floodplain river is visible only because the riparian forest canopy
is barely higher than the water level.
Figure VI: The River Enns, Styria, Austria. Photo from Gesaeuse National Park. Hydropower dams,
canals, and channelization limit connectivity of the Enns with its floodplain.
Figure VII: Intermittent tributaries of the Calapooia River, Oregon, USA. Photo by Randy Colvin,
Department of Fisheries and Wildlife, Oregon State University. Nearly all of the visible channels
(agricultural ditches) are only wet during the rainy season, yet they provide overwintering refuge
habitat for spawning and rearing native fish, including salmonids.