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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_-5a9c |
Folha |
SE23 |
Legenda_Completa |
530Pgi |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Depressões do Espinhaço |
Identificacao_Unidade |
530 |
Nome_Unidade |
Depressões Interiores do Espinhaço |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressões Interiores do Espinhaço |
Area_Poligono_Km2 |
15.961 |
the_geom |
MULTIPOLYGON (((-43.147273615533045 -16.388448402502274, -43.148696326356266 -16.388460931892947, -43.14912962545538 -16.38777800146654, -43.15013365048438 -16.386826296280418, -43.15142314071189 -16.385877094484517, -43.15227934730151 -16.38560991979148, -43.15356142368941 -16.3853464803927, -43.15513025598306 -16.384949102494016, -43.15613130780588 -16.384408482819417, -43.15727755161337 -16.38345798499863, -43.159132198140085 -16.382924825328413, -43.16042068708445 -16.381975552751392, -43.162708541763045 -16.380760301272538, -43.16500057507098 -16.378995658438235, -43.166719310512875 -16.377775393216094, -43.16757838038439 -16.37709612502573, -43.16871777014562 -16.376969597191827, -43.1698558858575 -16.37697949871293, -43.17212735178578 -16.37741038982437, -43.17482561840592 -16.377845863407597, -43.17724319834547 -16.377866819597372, -43.178669683101944 -16.37746711889557, -43.17938482780409 -16.37706215831113, -43.180536958125465 -16.37556216517723, -43.180552237879425 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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_-5a9b |
Folha |
SE23 |
Legenda_Completa |
509Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
509 |
Nome_Unidade |
Chapadas dos Rios Jequitaà - Verde Grande |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas dos Rios Jequitaà - Verde Grande |
Area_Poligono_Km2 |
2.811 |
the_geom |
MULTIPOLYGON (((-44.62945139539575 -16.396769957567766, -44.62945512227821 -16.394799257899447, -44.6291665354464 -16.393391230849563, -44.62887861485615 -16.39113887407509, -44.63005024851889 -16.388607946187054, -44.63121708653714 -16.38860999495386, -44.63267358388117 -16.389456874132435, -44.634129979154665 -16.390866931807558, -44.63558807594255 -16.39086946299659, -44.63588339414478 -16.389181312269535, -44.634719700407096 -16.387489728548104, -44.63355497226715 -16.38636222948588, -44.632680440446016 -16.3857975157142, -44.632682022221864 -16.384953187281358, -44.632682548895346 -16.38467204578603, -44.63268465887292 -16.383545671745125, -44.63210547928078 -16.381292808242357, -44.62918942954354 -16.381287690380983, -44.62919209063556 -16.379880174910152, -44.629194751467026 -16.37847265925081, -44.62803010818203 -16.37734513038526, -44.62686387408553 -16.377061019815798, -44.625698716300604 -16.37621461985793, -44.62482586697479 -16.37480554579664, -44.62482801898372 -16.373680075698356, -44.62337113276505 -16.37311428557898, -44.62220438797934 -16.373112195214734, -44.62074696880418 -16.372828432583084, -44.62133305624314 -16.37142196726214, -44.62046134830479 -16.369449688559204, -44.61900614536496 -16.368039540454628, -44.6178394313398 -16.368037426538372, -44.61725607439166 -16.36803636715646, -44.61608715752461 -16.369160617095293, -44.61608495602022 -16.370286086532648, -44.61695568670241 -16.37225838064315, -44.61695403855516 -16.373102708568204, -44.61782682331172 -16.374511814149834, -44.61782463102648 -16.375637283245077, -44.61724015272537 -16.376199409803956, -44.61840417735468 -16.377609042278443, -44.61956985615382 -16.37817434077193, -44.61985999014284 -16.378738053427544, -44.61985890043179 -16.37930033590232, -44.61985726403317 -16.380144663549164, -44.618688288028466 -16.381268925430522, -44.61781311386727 -16.38154847999003, -44.617809273174174 -16.383519179495778, -44.61780872521586 -16.38380032054188, -44.61839048412756 -16.384646610513656, -44.61926184641127 -16.386336849231004, -44.61926075269521 -16.386900035250907, -44.621009905387034 -16.387465477536225, -44.621009360131644 -16.387747522572308, -44.622466890110545 -16.38803128531421, -44.6221734790038 -16.389157134664256, -44.62158788620084 -16.39028155399724, -44.62187695667007 -16.391408449670212, -44.62304326953996 -16.39169168512505, -44.62479355276604 -16.39169481471774, -44.62595879704052 -16.392541220268626, -44.627120301455854 -16.39535831891337, -44.627993789516104 -16.396486241909365, -44.62945139539575 -16.396769957567766))) |
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_-5a9a |
Folha |
SE23 |
Legenda_Completa |
512Kd |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
512 |
Nome_Unidade |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Letra_Simbolo |
Kd |
Categoria |
Carste descoberto |
Natureza |
dissolução |
Caracteristica |
carste descoberto |
Forma |
carste |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Area_Poligono_Km2 |
41.711 |
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_-5a99 |
Folha |
SE23 |
Legenda_Completa |
512Da43 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
512 |
Nome_Unidade |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Area_Poligono_Km2 |
66.479 |
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_-5a98 |
Folha |
SE23 |
Legenda_Completa |
195Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
195 |
Nome_Unidade |
Maciços de Pedra Azul |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Maciços de Pedra Azul |
Area_Poligono_Km2 |
0.851 |
the_geom |
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