GEOMORPHOLOGICAL PROCESSES AND ASSOCIATED DAMAGE OF A DEBRIS FLOW IN JANUARY 2011 IN CÓRREGO DO PRÍNCIPE WATERSHED, TERESÓPOLIS – MOUNTAINOUS REGION OF RIO DE JANEIRO STATE
DOI:
https://doi.org/10.5902/2179460X14872Keywords:
corrida de detritos, danos, bacia de drenagem, catástrofeAbstract
http://dx.doi.org/10.5902/2179460X14872
The Córrego do Principe (1,197 ha) watershed located at the mountainous range “Região Serrana” of the state of Rio de Janeiro was seriously affected by a debris flow that took place on January 12th, 2011. The event was triggered by an extreme rainfall that resulted in a major disaster causing destruction and deaths. Field observations together with Quickbird satellite images analysis (0.6 m resolution August/2006 and 1:8,000 aerial pictures May/2011) identified and classified the damages affecting buildings associated with geomorphological processes of erosion and deposition. The debris flow extended for about 4.8 km, the first two being characterized by erosion and transport of blocks, boulders and fine material. The deposition of this material happened on the last 2.8 kilometers. Buildings damages of greater intensity were observed associated with the erosion / transport area and four knickpoints have proven to significantly amplify the damages in their surroundings. Blocks and boulders came primarily from exhumation of riverbed ancient deposits. The deposition zone showed more than 2 m thickness sedimentation that buried part of the buildings and roads. High damage (difficult to reconstruct) covered an average of 42 % of the buildings in the Córrego do Principe watershed.
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