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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_-55e4 |
Folha |
SE23 |
Legenda_Completa |
130DEc43 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
130 |
Nome_Unidade |
Serras do Espinhaço Central |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Central |
Area_Poligono_Km2 |
20.089 |
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_-55e3 |
Folha |
SE23 |
Legenda_Completa |
513Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
513 |
Nome_Unidade |
Patamares das Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
9.935 |
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_-55e2 |
Folha |
SE23 |
Legenda_Completa |
554Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
554 |
Nome_Unidade |
Patamares Dissecados das Chapadas de Cristalina |
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 |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
79.161 |
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_-55e1 |
Folha |
SE23 |
Legenda_Completa |
529Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Mantiqueira Setentrional |
Identificacao_Unidade |
529 |
Nome_Unidade |
Serranias da Zona da Mata Mineira |
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 |
Serranias da Zona da Mata Mineira |
Area_Poligono_Km2 |
5.243 |
the_geom |
MULTIPOLYGON (((-42.00216452002945 -19.385446678555326, -42.00178472330412 -19.385237791024664, -42.00056937161284 -19.3845541561253, -42.000401917287434 -19.38450087525147, -42.000401922377556 -19.40378627429867, -42.004862508005886 -19.406470371239596, -42.005943403254754 -19.413820444579297, -42.00594340433826 -19.417711660020323, -42.00507869206402 -19.425926448390637, -42.00507869369056 -19.431763271552235, -42.00486251541141 -19.433060343420237, -42.00486251583327 -19.434573593869565, -42.005294873596704 -19.43630302284573, -42.007024303324734 -19.43846480876707, -42.00896991072889 -19.43716773646455, -42.0094022670457 -19.433708878186234, -42.00940226650341 -19.431763270465957, -42.009834623242256 -19.42981766263701, -42.010915516204435 -19.42895294782303, -42.01199640892543 -19.42722351846664, -42.01350965886748 -19.425277910366198, -42.01459055158851 -19.42354848100996, -42.01696851573146 -19.42030580087903, -42.01848176513144 -19.41641458505834, -42.01999501483249 -19.413604262415852, -42.020427371571735 -19.411658654587054, -42.02042737102979 -19.40971304686682, -42.02041726305378 -19.409662507060776, -42.019331367841914 -19.412051478208966, -42.01887561115587 -19.412507235125826, -42.01819197593631 -19.41250723529732, -42.01697662432909 -19.412127438267056, -42.01659682683672 -19.411595722092738, -42.01652086707169 -19.41053228957249, -42.01629298847468 -19.409848654425748, -42.01629298824195 -19.40901310028775, -42.01598915021856 -19.408481384094333, -42.01507763627518 -19.40734199231654, -42.014621879356305 -19.40696219509539, -42.01355844664451 -19.40643047909245, -42.01158350045471 -19.406430479587986, -42.00854512193363 -19.40726603448836, -42.00710189202555 -19.40726603485031, -42.00603845939828 -19.40703815671579, -42.00550674275688 -19.405746845908343, -42.005658661525366 -19.405139170133445, -42.00694997222089 -19.404151696737035, -42.011355620673626 -19.401493114283593, -42.01287480992351 -19.401037357099888, -42.013026728565194 -19.399973924522488, -42.0127988497147 -19.39837877577057, -42.01234309277487 -19.397923019082207, -42.01135561955309 -19.397467262527243, -42.009456632789934 -19.397315344069145, -42.008772997485856 -19.39701150637215, -42.00808936213961 -19.39655574974095, -42.007709564605136 -19.39587211463218, -42.00770956399235 -19.393669290086137, -42.00786148280318 -19.39321353324544, -42.00877299615452 -19.39222605994451, -42.0115075366099 -19.39070686991698, -42.011887333763816 -19.390023234617825, -42.01181137383016 -19.388352126360672, -42.010975819377336 -19.387288694030552, -42.00740572432117 -19.387212735458238, -42.006949967529344 -19.38728869503945, -42.00505098114652 -19.388504046989105, -42.004443305395775 -19.388504047141414, -42.00398754851945 -19.388276168854265, -42.00322795361988 -19.387516574373457, -42.00284815591668 -19.38622526352773, -42.00216452002945 -19.385446678555326))) |
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_-55e0 |
Folha |
SE23 |
Legenda_Completa |
518Aptf |
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 |
Aptf |
Categoria |
PlanÃcie e terraço fluviais |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie e terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais do Rio Doce |
Area_Poligono_Km2 |
4.071 |
the_geom |
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