ISS007-E-10797 Click the photo number to access all resolutions available and the database record.
Numerous changes in river pattern are visible in the decade since the Landsat imagery was acquired. A pilot study was undertaken to characterize these rapid changes. Tie points were selected for geomorphic features which do not undergo short-term change- i. e. oxbow lakes and subsidence lakes in the floodplain. The ISS image was enhanced slightly to reveal the Mamore River channel.
The ISS image (top) shows Mamore River meandering in a floodplain with numerous contorted channel traces indicating former positions of the river. The darker areas are riverine forest, the lighter areas tropical savanna. The river trace as it was in 1990 (bottom) is superimposed on the 2003 handheld image.
Interpretation
- Meander cutoffs: In two locations, the Mamore has straightened its course by meander cutoff (c-upper image). The opposite trend appears to the north (right) where the course has become more sinuous.
- Some structural control, possibly by buried faults, appears to have maintained the position and straightness of the E-W stretch (EW).
- An old course has controlled the position of a sector of the new course: the radius of curvature of the northernmost meander is sharper than most bends because the new course has occupied a prior course (a-far right, upper image).
- Ten-fifteen years of river movement has had
wider impacts on the valley floor:
- two new lakes been formed where the large meanders have been cut off (n)
- several lakes have decreased in size, especially two elongated lakes that have been reduced in length by more than 50% (s)
- lakes have been destroyed entirely (x-lower figure)
- many lakes are further from the main river and many closer: this nearness factor determines whether or not lakes receive nutrient rich inflow from the main river during floods. It is possible that these kinds of disturbances-the creation and destruction of habitat-may be a major cause of biodiversity generation in equatorial rainforests.
