Evolução geomorfológica do Distrito Federal.
ABSTRACT: This work constitutes a synthesis on the physical aspects of Federal District and a proposal of geomorphologic evolution is presented, with the following stages: formation of double surface (After-Gondwana Surface, Medium to Superior Cretaceous) - differential physical denudation processes in arid climate associates to the regional uplift; complex lateritic regolit generation (South American surface, Paleocene to Inferior Miocene) - Weathering chemical processes in humid and hot conditions. Differentiation of complex lateritic regolit below the initial double surface; Lateritic regolit denudation (Inferior Miocene) - Uplift and change for climatic conditions more droughts. Processes of differential physical weathering. Bellowing of the base level and dissection of the South American surface; formation of new lateritic facies (Pliocene to Medium Miocene) - Processes of chemical weathering in humid and hot climatic conditions. Bellowing of the saprolitDegradation of the massive crusts inside plain surface in hydrated conditions and high biological activity; dissection of the residual surfaces and sedimentation (Superior Pliocene) - Uplift and changes for climatic conditions more droughts. Processes of differential physical weathering. Dissection of the residual surfaces; domain alternations between erosive and pedogenetic processes (Quaternary) - Several short climatic oscillations, among the dry and humid. During the dry cycles, larger erosive activity and increase of the indent of the slopes of larger steepness. During the humid cycles, larger pedogenetic and chemical activity.
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Format: | Folhetos biblioteca |
Language: | Portugues pt_BR |
Published: |
2004
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Subjects: | Mapeamento, Classificação, Pedology, Relief, Geomorfologia, Pedologia, Relevo, Solo, cartography, geomorphology, soil classification, |
Online Access: | http://www.infoteca.cnptia.embrapa.br/infoteca/handle/doc/569549 |
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dig-infoteca-e-doc-5695492023-05-08T12:49:09Z Evolução geomorfológica do Distrito Federal. MARTINS, E. de S. REATTO, A. CARVALHO JÚNIOR, O. A. de GUIMARÃES, R. F. Mapeamento Classificação Pedology Relief Geomorfologia Pedologia Relevo Solo cartography geomorphology soil classification ABSTRACT: This work constitutes a synthesis on the physical aspects of Federal District and a proposal of geomorphologic evolution is presented, with the following stages: formation of double surface (After-Gondwana Surface, Medium to Superior Cretaceous) - differential physical denudation processes in arid climate associates to the regional uplift; complex lateritic regolit generation (South American surface, Paleocene to Inferior Miocene) - Weathering chemical processes in humid and hot conditions. Differentiation of complex lateritic regolit below the initial double surface; Lateritic regolit denudation (Inferior Miocene) - Uplift and change for climatic conditions more droughts. Processes of differential physical weathering. Bellowing of the base level and dissection of the South American surface; formation of new lateritic facies (Pliocene to Medium Miocene) - Processes of chemical weathering in humid and hot climatic conditions. Bellowing of the saprolitDegradation of the massive crusts inside plain surface in hydrated conditions and high biological activity; dissection of the residual surfaces and sedimentation (Superior Pliocene) - Uplift and changes for climatic conditions more droughts. Processes of differential physical weathering. Dissection of the residual surfaces; domain alternations between erosive and pedogenetic processes (Quaternary) - Several short climatic oscillations, among the dry and humid. During the dry cycles, larger erosive activity and increase of the indent of the slopes of larger steepness. During the humid cycles, larger pedogenetic and chemical activity. 2023-05-08T12:49:08Z 2023-05-08T12:49:08Z 2006-05-04 2004 Folhetos Planaltina, DF: Embrapa Cerrados, 2004. http://www.infoteca.cnptia.embrapa.br/infoteca/handle/doc/569549 Portugues pt_BR (Embrapa Cerrados. Documentos, 122). openAccess 57 p. |
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Mapeamento Classificação Pedology Relief Geomorfologia Pedologia Relevo Solo cartography geomorphology soil classification Mapeamento Classificação Pedology Relief Geomorfologia Pedologia Relevo Solo cartography geomorphology soil classification |
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Mapeamento Classificação Pedology Relief Geomorfologia Pedologia Relevo Solo cartography geomorphology soil classification Mapeamento Classificação Pedology Relief Geomorfologia Pedologia Relevo Solo cartography geomorphology soil classification MARTINS, E. de S. REATTO, A. CARVALHO JÚNIOR, O. A. de GUIMARÃES, R. F. Evolução geomorfológica do Distrito Federal. |
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ABSTRACT: This work constitutes a synthesis on the physical aspects of Federal District and a proposal of geomorphologic evolution is presented, with the following stages: formation of double surface (After-Gondwana Surface, Medium to Superior Cretaceous) - differential physical denudation processes in arid climate associates to the regional uplift; complex lateritic regolit generation (South American surface, Paleocene to Inferior Miocene) - Weathering chemical processes in humid and hot conditions. Differentiation of complex lateritic regolit below the initial double surface; Lateritic regolit denudation (Inferior Miocene) - Uplift and change for climatic conditions more droughts. Processes of differential physical weathering. Bellowing of the base level and dissection of the South American surface; formation of new lateritic facies (Pliocene to Medium Miocene) - Processes of chemical weathering in humid and hot climatic conditions. Bellowing of the saprolitDegradation of the massive crusts inside plain surface in hydrated conditions and high biological activity; dissection of the residual surfaces and sedimentation (Superior Pliocene) - Uplift and changes for climatic conditions more droughts. Processes of differential physical weathering. Dissection of the residual surfaces; domain alternations between erosive and pedogenetic processes (Quaternary) - Several short climatic oscillations, among the dry and humid. During the dry cycles, larger erosive activity and increase of the indent of the slopes of larger steepness. During the humid cycles, larger pedogenetic and chemical activity. |
format |
Folhetos |
topic_facet |
Mapeamento Classificação Pedology Relief Geomorfologia Pedologia Relevo Solo cartography geomorphology soil classification |
author |
MARTINS, E. de S. REATTO, A. CARVALHO JÚNIOR, O. A. de GUIMARÃES, R. F. |
author_facet |
MARTINS, E. de S. REATTO, A. CARVALHO JÚNIOR, O. A. de GUIMARÃES, R. F. |
author_sort |
MARTINS, E. de S. |
title |
Evolução geomorfológica do Distrito Federal. |
title_short |
Evolução geomorfológica do Distrito Federal. |
title_full |
Evolução geomorfológica do Distrito Federal. |
title_fullStr |
Evolução geomorfológica do Distrito Federal. |
title_full_unstemmed |
Evolução geomorfológica do Distrito Federal. |
title_sort |
evolução geomorfológica do distrito federal. |
publishDate |
2004 |
url |
http://www.infoteca.cnptia.embrapa.br/infoteca/handle/doc/569549 |
work_keys_str_mv |
AT martinsedes evolucaogeomorfologicadodistritofederal AT reattoa evolucaogeomorfologicadodistritofederal AT carvalhojunioroade evolucaogeomorfologicadodistritofederal AT guimaraesrf evolucaogeomorfologicadodistritofederal |
_version_ |
1779391467999985664 |