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The contact between the sedimentary shed edge depressions and the cuestiform reliefs when combined with intense agricultural use may start linear erosive processes. As far as it is concerned, this article aims to discuss the evolution of linear erosive features, from their interactions with lithology, soils, declivity and land use in a depression-cuesta transition located in Analândia (SP). Committed to achieving its goals, a set of cartographic techniques were used in order to map each of the considered variables. Through the methodology used an expressive association of the erosive features with the sandy lithologies and with the thick soils and the little thick soils was verified. The rill erosion and ravines presented a considerable incidence on the slopes gradient from 5 to 12%, which, theoretically, is evaluated as suitable for various types of land use. On that same ground, linear erosive features correlated to areas of clean pasture, but also to arboreal vegetation, a fact theoretically unexpected. In this way, it is possible to claim that the geomorphological characteristics of the cuesta-depression contact, together with an intense use of the earth, can be dynamizing the linear erosive processes over diverse physical conditions, some of these considered of low potential for the development of these processes.

AVALIAÇÃO DAS CARACTERÍSTICAS AMBIENTAIS DE OCORRÊNCIAS DAS FEIÇÕES EROSIVAS LINEARES NOS LIMITES DEPRESSÃO-CUESTA - ANALÂNDIA (SP)