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Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha SE.23 conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5cec |
Folha |
SE23 |
Legenda_Completa |
519Dc32 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressões do São Francisco |
Identificacao_Unidade |
519 |
Nome_Unidade |
Depressão do Alto Rio São Francisco |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
172.606 |
the_geom |
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gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha SE.23 conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5ceb |
Folha |
SE23 |
Legenda_Completa |
524DEc31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
10.546 |
the_geom |
MULTIPOLYGON (((-44.29497789467217 -17.72589798664982, -44.29556859518921 -17.725577437467635, -44.29716583442612 -17.72471186343343, -44.2987651465082 -17.724036992622967, -44.30266730565614 -17.724390730391, -44.30285380601662 -17.722011590741257, -44.30339058987673 -17.720993063596826, -44.30658908927233 -17.719644106474288, -44.30996223964124 -17.718975395465876, -44.3119156932243 -17.718642404887845, -44.312633950924386 -17.716264208527065, -44.31281771972852 -17.71456473047933, -44.31513474065309 -17.711852264228693, -44.31779919687379 -17.711011923241447, -44.31763154847375 -17.708460704250196, -44.317109333880985 -17.705908253046065, -44.31711512081172 -17.704378071212176, -44.31765339455848 -17.702679816081776, -44.31960635990582 -17.702175914932564, -44.32067674578062 -17.700649413182735, -44.317850583486994 -17.69740929936965, -44.31927101902427 -17.69707437748344, -44.32034073662225 -17.69571779589391, -44.32052952337931 -17.692657135418997, -44.31840678732327 -17.69094966397257, -44.317170393724126 -17.68975501605138, -44.31646037510164 -17.689752550100355, -44.312735546923015 -17.689569649341806, -44.31238100975092 -17.689568410343814, -44.31042427453832 -17.691091763118937, -44.309181142729635 -17.69142724504764, -44.30793540017657 -17.69244330147677, -44.30650062510022 -17.696519084410046, -44.30437340034975 -17.69600180547011, -44.30135587623939 -17.696500873166354, -44.30029128363347 -17.69649708794222, -44.29816436235246 -17.69614966507625, -44.29620649631899 -17.697672865315518, -44.29602922040429 -17.697672230720887, -44.29283570413598 -17.697830692938968, -44.292299601425384 -17.698679274971195, -44.290341267695496 -17.70054225487683, -44.28997801958081 -17.702751727518997, -44.28996799089896 -17.70530231737374, -44.289962641818 -17.706662571434975, -44.28724510809291 -17.708990957810904, -44.28276312888738 -17.71011980978165, -44.28066863656455 -17.711543827400405, -44.27673115890726 -17.712086135178858, -44.27702931265373 -17.713696055909725, -44.276408611199344 -17.716326636836445, -44.276402750392975 -17.717788113108174, -44.27685720297061 -17.718520987432093, -44.27990275698074 -17.719848157104373, -44.28172358179655 -17.72204752404426, -44.28598922329928 -17.723233543375045, -44.28903608260885 -17.724267737928674, -44.294066148920116 -17.724870665851977, -44.29497789467217 -17.72589798664982))) |
gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha SE.23 conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5cea |
Folha |
SE23 |
Legenda_Completa |
519Dt31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressões do São Francisco |
Identificacao_Unidade |
519 |
Nome_Unidade |
Depressão do Alto Rio São Francisco |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
44.158 |
the_geom |
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gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha SE.23 conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5ce9 |
Folha |
SE23 |
Legenda_Completa |
518Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies do Rio Doce |
Identificacao_Unidade |
518 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais do Rio Doce |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais do Rio Doce |
Area_Poligono_Km2 |
1.135 |
the_geom |
MULTIPOLYGON (((-42.0515128608614 -18.947346105887977, -42.05122176489349 -18.95057358594871, -42.052614666076515 -18.953975026919252, -42.05625914326845 -18.957872706753463, -42.06200662854242 -18.96149675075874, -42.065379086733145 -18.962471118421668, -42.067762447347185 -18.964659427953205, -42.07015566850579 -18.96623303869713, -42.0723671289055 -18.969033412969626, -42.07606333031683 -18.97001273003224, -42.07880444412461 -18.97014809918996, -42.08122286927824 -18.97034063616874, -42.083961213688774 -18.970690763031307, -42.08618366939262 -18.972876340444422, -42.08729665400452 -18.973814762506656, -42.08823861222361 -18.975366229779244, -42.08951386182308 -18.9763071947365, -42.08981242640379 -18.97769414970752, -42.091879085982185 -18.97957025813832, -42.09218597519971 -18.979932609507376, -42.09229477228243 -18.980061621017036, -42.092291289559654 -18.979934264607557, -42.09224411580914 -18.9782786013861, -42.091350171839636 -18.974942971919088, -42.088384172772855 -18.972178762491858, -42.08255738575961 -18.969671902654493, -42.07624498003672 -18.967760306650156, -42.073229294635446 -18.96786342680499, -42.07027071832523 -18.964645868429088, -42.066058062037854 -18.96065364060524, -42.06086673741877 -18.958155343465453, -42.05663762309118 -18.955069122544685, -42.054134572491655 -18.953066585691115, -42.05433009891908 -18.950956178179517, -42.051951758730546 -18.94790922997709, -42.0515128608614 -18.947346105887977))) |
gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha SE.23 conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5ce8 |
Folha |
SE23 |
Legenda_Completa |
177Dt21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
177 |
Nome_Unidade |
Patamares da Borda Ocidental do Espinhaço |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares da Borda Ocidental do Espinhaço |
Area_Poligono_Km2 |
42.496 |
the_geom |
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