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- W101070629 endingPage "611" @default.
- W101070629 startingPage "595" @default.
- W101070629 abstract "Tropical montane streams produce a disproportionately large amount of the sediment and carbon that reaches coastal regions and have often been considered to be distinct fluvial systems. They typically drain orogenic terrains that have not been recently glaciated, but have undergone climatic changes throughout the Pleistocene and currently receive 2000–3000 mm or more of precipitation each year. Steep gradient reaches with numerous boulders, rapids, and waterfalls that alternate with lower gradient reaches flowing over weathered rock or a thin veneer of coarse alluvium characterize these streams. Although their morphology and hydrology have distinctive characteristics, they do not appear to have diagnostic landforms that can be solely attributed to their low-latitude locations. Whereas they are relatively understudied, an emerging view is that their distinctiveness results from a combination of high rates of chemical and physical weathering and a high frequency of significant geomorphic events rather than the absolute magnitudes of individual floods or other geomorphic processes. Their bedrock reaches and abundance of large and relatively immobile boulders combined with their ability to transport finer-grained sediment also suggest that the restorative processes in these systems may be less responsive than in other fluvial systems." @default.
- W101070629 created "2016-06-24" @default.
- W101070629 creator A5027337904 @default.
- W101070629 creator A5068036431 @default.
- W101070629 date "2013-01-01" @default.
- W101070629 modified "2023-09-23" @default.
- W101070629 title "9.30 Streams of the Montane Humid Tropics" @default.
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