dobramentos e falhamentos
DESCRIPTION
Forças endógenas na formação da superfície da Terra: Movimentos orogenéticos (dobramentos), falhamentos e Epirogenéticos Forças exógenas: intemperismo e erosão. Dobramentos e falhamentos. Falhas :. - PowerPoint PPT PresentationTRANSCRIPT
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Dobramentos e falhamentos
Forças endógenas na formação da superfícieda Terra: Movimentos orogenéticos (dobramentos), falhamentos e
Epirogenéticos
Forças exógenas: intemperismo e erosão
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Falhas:
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Localização do Rift Valley, na África (trata-se de uma fossa tectônica,
originada de falhamentos)
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Outro exemplo de forças endógenas: movimento epirogenético
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Diques (proteções) e polders (terrenos abaixo do nível do mar) na Holanda
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Tipos de rochas
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Granito: rocha magmática cristalina (ou intrusiva),formada do lento resfriamento do magma
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Pia de granito
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Basalto: rocha magmática vulcânica (ou extrusiva)formada do rápido resfriamento do magma
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Solos de terra roxa: decomposição do basalto
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Calçamento utilizando basalto (escuro) e granito (claro)
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Localização do Grand Canyon – Arizona/EUA
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Monte Everest (8.848 m – divisa da China com o Nepal): relevomontanhoso (estrutura geológica: dobramentos modernos)
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Everglades – Flórida – EUA: relevo plano (estrutura sedimentar)
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Planalto na Mongólia
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