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Serra Do Mar: The Most “Tormented” Relief in Brazil
World Geomorphological Landscapes, 2015The Serra do Mar is a system of escarpments and mountains that stretch more than 1,500 km between the states of Santa Catarina and Rio de Janeiro with a general ENE orientation. It has high lithological and structural complexity along its entire length, with some stretches quite recessed from the coast and some very close to it. It caught the attention
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Landslides in the Serra do Mar, Brazil
CATENA, 1979Abstract This paper discusses the environmental and the soil mechanical conditions for the massive planar slides which ravaged the area of Caraguatatuba, Serra do Mar, in 1967. Special attention is given to the hydrology of slopes on weathered gneiss during days of heavy rainfall.
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Journal of South American Earth Sciences, 1989Abstract The Serra do Mar rift system is the most significant Cenozoic tectonic feature of the onshore continental area of southeastern Brazil. This system exhibits a two-fold tectonic evolution, marked by a distensive synsedimentary stage in Paleocene-Oligocene times and a strike-slip stage of post-Oligocene age.
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