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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_-541b |
Folha |
SE23 |
Legenda_Completa |
545Dc42 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos do Centro-Sul de Minas |
Identificacao_Unidade |
545 |
Nome_Unidade |
Depressão de Belo Horizonte |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão de Belo Horizonte |
Area_Poligono_Km2 |
63.777 |
the_geom |
MULTIPOLYGON (((-44.214827120712634 -19.599368012879637, -44.21392680128343 -19.597641741501423, -44.21514469154842 -19.596211156897002, -44.21970133146987 -19.59307360061922, -44.21732253993946 -19.58416508397098, -44.22006301176522 -19.580732252958256, -44.22582852376881 -19.577887103396296, -44.22342620946421 -19.573858252644815, -44.217372445350165 -19.573832094709065, -44.21555631801666 -19.573824207728645, -44.21163346594464 -19.571223582964326, -44.211345220176746 -19.56835234019658, -44.212867885757404 -19.56634927572168, -44.21439841724527 -19.5629112376826, -44.21236802769272 -19.560132708301833, -44.211954312454814 -19.55954172422007, -44.21160709118588 -19.558999826630625, -44.21079155341045 -19.557727541450426, -44.20565995444749 -19.55483505307532, -44.20233691001298 -19.55367186878795, -44.20083590508617 -19.551082609082876, -44.19752858305056 -19.546762066764767, -44.192399003619215 -19.54358186544058, -44.189668652255385 -19.54500462883392, -44.18481356880616 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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_-541a |
Folha |
SE23 |
Legenda_Completa |
561Dt32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
561 |
Nome_Unidade |
Depressão Interplanáltica do Rio Corumbá |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão Interplanáltica do Rio Corumbá |
Area_Poligono_Km2 |
13.38 |
the_geom |
MULTIPOLYGON (((-48.000445462360936 -16.63619207135358, -47.99986442589954 -16.636542519523115, -47.99876552983113 -16.63720908885484, -47.99876476447895 -16.637209165706743, -47.99836911979772 -16.637643424183295, -47.99805508849123 -16.637987472445356, -47.997723154440536 -16.63874623213797, -47.99731820726967 -16.640892974830997, -47.99697646851954 -16.643009006770736, -47.99676720203659 -16.643645901177, -47.995938487655785 -16.644623130429704, -47.995018928332534 -16.645782259882925, -47.993929219105446 -16.648107746588522, -47.99367405911858 -16.6497701508414, -47.9930209063906 -16.65204147435477, -47.99291041463842 -16.652947826156772, -47.992724547458046 -16.655091405329408, -47.99251525997371 -16.655728299210637, -47.99137119605694 -16.660527750746667, -47.99188069890318 -16.663174162655054, -47.99269270088092 -16.66509203377307, -47.993090766994186 -16.666594205703383, -47.992313440382844 -16.66684652779977, -47.992145367267014 -16.668085997609953, -47.992252614770536 -16.668958502854633, -47.99326752685867 -16.673197623516014, -47.993172827160365 -16.67397462572237, -47.9928897663151 -16.679260967898397, -47.99351444357059 -16.684182027020867, -47.990095416342605 -16.68740082703977, -47.98622162232649 -16.68481565453329, -47.984104153516476 -16.67780316630873, -47.9863900158556 -16.672135764318373, -47.98595370210908 -16.667564082617165, -47.98390479429914 -16.66495337788696, -47.97955005454215 -16.66660077164091, -47.97846791401375 -16.667496725088075, -47.97753118638724 -16.665925502993403, -47.97481814133582 -16.667549193558145, -47.973769549775 -16.67055667290989, -47.975101502370954 -16.67405908453768, -47.97587197343508 -16.67668916802334, -47.97482611233146 -16.679873596759222, -47.97303875482917 -16.68236437107145, -47.972355400598886 -16.685367509463408, -47.97402825394834 -16.68728031733894, -47.976040963263735 -16.68760352261162, -47.976812469769776 -16.69023357532738, -47.97616095434862 -16.695348282861403, -47.97639272431457 -16.698514331393433, -47.976469145661554 -16.703443383667036, -47.97945546874576 -16.70762618619653, -47.98081251051541 -16.712712822472447, -47.981785134799004 -16.716572456671447, -47.9838566060605 -16.72059137555666, -47.98501885843398 -16.724404894843513, -47.98682694677603 -16.72371778315067, -47.98863909451478 -16.72281118215699, -47.99042832079692 -16.720496301641486, -47.992605770034054 -16.719584381709126, -47.99510638221594 -16.716027545127844, -47.99287954230379 -16.713770859007518, -47.99302101441973 -16.71112769141866, -47.992797158360524 -16.70848981604477, -47.99002887577423 -16.706593072347236, -47.98686338374744 -16.7025891192542, -47.98773739333631 -16.700111431129372, -47.99155394063267 -16.698999780752814, -47.99465447750158 -16.698778811892744, -47.997384192830836 -16.698211026433206, -48.00044515744046 -16.69677879880763, -48.000445469159416 -16.653513357493026, -48.000445462370934 -16.636192157296954, -48.000445462360936 -16.63619207135358))) |
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_-5419 |
Folha |
SE23 |
Legenda_Completa |
521Dt12 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos da Bacia do Alto Rio Paraná |
Identificacao_Unidade |
521 |
Nome_Unidade |
Planalto do Triângulo Mineiro |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
muito baixa |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto do Triângulo Mineiro |
Area_Poligono_Km2 |
100.117 |
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_-5418 |
Folha |
SE23 |
Legenda_Completa |
519Dc31 |
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 |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
37.056 |
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_-5417 |
Folha |
SE23 |
Legenda_Completa |
523Dc33 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
523 |
Nome_Unidade |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
363.97 |
the_geom |
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