CV Lattes
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Universidade de São Paulo (USP). Faculdade de Filosofia, Letras e Ciências Humanas (FFLCH) (Institutional affiliation from the last research proposal) Birthplace: Brazil
bachelor's at Geografia from Universidade de São Paulo (2000), master's at Physical Geography from Universidade de São Paulo (2005) and doctorate at Physical Geography from Universidade de São Paulo (2011). He is currently an adjunct professor at the Federal University of São Carlos. He has experience in Geography with emphasis in Geomorphology, acting on the following topics: climatic geomorphology, pedo-geomorphological interactions, characterization of physical and landscape units, geomorphological mapping and GIS. (Source: Lattes Curriculum)
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During the project evaluation period (Regular Research Grant) "Geomorphological-Pedological Evolution of Cuesta Escarpment Foothills in the State of São Paulo" (Fapesp Process 2016/08722-3), which is tied to the present proposal, the reviewer asked for the revision of some aspects of the proposal then submitted. The main change referred to the need for the project to include also the inve…
The cuesta escarpments, located between the Peripheral Depression of São Paulo and the Western Plateau of the State of São Paulo are among the most expressive landforms of the Paraná Sedimentary Basin. Those features are characterized by dissymmetrical forms, comprised by a gentle backslope and a cliff-like frontslope (escarpment). The landforms on the bottom of the frontslope have their …
Ancient surfaces remain as chronogeographic markers in the landscape, tracing back to past processes that highlight the polygenetic nature of the involved regions and their configurations as inherited mosaics, allowing for the study of paleoenvironmental conditions and paleogeographic reconstructions. Summit surfaces, located at the top of tabular landforms, for example, could provide a m…
Periglacial environments cover cold areas and are associated with the peripheral areas of the ice sheets. In these periglacial areas, the surface morphogenesis would be caused by the erosive advance and the abrasive effect of the glaciers, which could flatten structural banks, pediments and terraces of varying nature according to the substrate resistance, involving processes of cryoplanat…
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| 1 / 1 | Ongoing scholarships in Brazil |
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| 4 / 4 | All research grants and scholarships |
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