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https://doi.org/10.1007/978-1-349-09395-3agreste and coast. In addition to the reworking of surfaces, caused by climate variability during the Pleistocene/Holocene, the action of neotectonic phenomena is remarkable in the rejuvenated structures of the mountains and in the morphotectonic control of the drainage network. In this way, it was

压倒

Erratum Chapter 5 Chamber Abnormalities,ientific works in evidence, with the intention of clarifying readers‘ understanding, through consistent data and information. The central objective is to provide a concise and unifying document, to expand and popularize the understanding of the geomorphology of the State of Bahia. We begin with a br

追逐

Evolution of Geomorphological Knowledge: Theoretical and Methodological Aspectserphase and integrative basis of natural units such as rock, climate, soil, vegetation and water resources, therefore, considering it as dynamic and being an object of study sometimes associated with an element, sometimes in the integrated landscape set. In this way, its theoretical and methodologic

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Geomorphology of Maranhão State relief is characterized by flattened lowlands amidst extensive fluviomarine plains and the largest coastal dune fields in Brazil. The Coastal-continent transition presents a dissection sequence of extensive plateau surfaces in relatively modest elevations resulted from fluvial erosion processes on

虚弱

Geomorphology of Piauí State method was used, with the methodological procedures being the reading and analysis of theoretical texts related to the area studied, thematic mappings and fieldwork reports, satellite images, and digital cartography. The main results obtained made it possible to classify the relief of the State of

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Geomorphology of Pernambuco Statens related to the Brasiliana Orogeny (900–570 Ma) and the formation of the West Gondwana continent. The area is characterized by the predominance of crystalline lithologies separated by NE- SW and E-W shear zones. Phanerozoic sedimentary basins overlie the Proterozoic basement as a result of the pla

IRS

Geomorphology of Alagoas Staterozoic nuclei bounded by Meso- and Neoproterozoic fold-belts. Phanerozoic sedimentary covers of the Tucano-Jatobá basins (Paleozoic) outcrop in the northwestern most sector of the State, along with other sedimentary units along the coastal strip, like the Cretaceous formations of the Alagoas margina