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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_-5aa1 |
Folha |
SE23 |
Legenda_Completa |
103Ai1 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressões do São Francisco |
Identificacao_Unidade |
103 |
Nome_Unidade |
Depressão do Médio Rio São Francisco |
Letra_Simbolo |
Ai |
Categoria |
Plano de inundação |
Natureza |
acumulação |
Caracteristica |
inundação |
Forma |
plano abaciado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
Depressão do Médio Rio São Francisco |
Area_Poligono_Km2 |
22.666 |
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_-5aa0 |
Folha |
SE23 |
Legenda_Completa |
510Da43 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
510 |
Nome_Unidade |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
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 Jequitaà - Verde Grande |
Area_Poligono_Km2 |
67.304 |
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_-5a9f |
Folha |
SE23 |
Legenda_Completa |
130Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
130 |
Nome_Unidade |
Serras do Espinhaço Central |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Central |
Area_Poligono_Km2 |
12.159 |
the_geom |
MULTIPOLYGON (((-42.86171912032966 -16.63080195994396, -42.862902460252506 -16.629130097951748, -42.864396772447016 -16.62577556771956, -42.86529177552154 -16.62381883966391, -42.86737403880546 -16.619909270110902, -42.86796301556071 -16.619354266716176, -42.86883409427541 -16.619643281065162, -42.8688154949348 -16.62132805010968, -42.86968563699105 -16.621617955758186, -42.87114476756834 -16.62135194200962, -42.872316525512 -16.620802899093572, -42.87321545489566 -16.618565187378255, -42.873234012590316 -16.616880413049152, -42.87324328565586 -16.616038477456666, -42.873255652223484 -16.614915595431594, -42.87326801783513 -16.613792713275988, -42.873577012571474 -16.612110910967242, -42.874482047421964 -16.609312195587304, -42.877137434269876 -16.606250380672115, -42.878013698778744 -16.60597835048215, -42.87947979738908 -16.605151280254834, -42.880061602041735 -16.605157215391507, -42.88210026241086 -16.605177999433117, -42.883272162847064 -16.604262072046982, -42.88385528352479 -16.603805431809082, -42.884162351728115 -16.60323033534314, -42.88475547553486 -16.602116065494833, -42.88478312636978 -16.599589332623708, -42.88393055388715 -16.597614699818216, -42.88277834720563 -16.596479954284344, -42.88164153337467 -16.59394136496392, -42.879363978293625 -16.589144211527504, -42.87792264639907 -16.587725519471615, -42.87618784652947 -16.586584803036413, -42.87298804919167 -16.586271134962317, -42.86891115406249 -16.586229414386708, -42.86714857393069 -16.587615337739866, -42.86566707608765 -16.58984705988592, -42.8636192997172 -16.59066806591696, -42.863300038575225 -16.593191772982877, -42.86241140878012 -16.594586622129878, -42.861816278929226 -16.595704410864958, -42.86121183753631 -16.597663224154537, -42.861196306251145 -16.599067043782718, -42.86002559100952 -16.599616949641817, -42.86001004917933 -16.601020767914513, -42.859712476433394 -16.601578753528706, -42.85854485473237 -16.601847704628288, -42.857069366148345 -16.603517450950427, -42.85531900236391 -16.60378037342756, -42.85385999975031 -16.604046289253905, -42.85240411655454 -16.604031251538782, -42.85007414446335 -16.60400716420603, -42.84745907195642 -16.603418149752184, -42.84629675538216 -16.603125135510023, -42.84541108962133 -16.604238949497475, -42.843660715653115 -16.604501771077864, -42.841913476265454 -16.6044836364807, -42.840766850611814 -16.602786791430958, -42.83991252777006 -16.60109388292485, -42.83817695525106 -16.599951949610055, -42.835835408956854 -16.601051477765584, -42.835810262082816 -16.603297189418978, -42.83579768718698 -16.604420045049697, -42.834907874857876 -16.605814736090853, -42.834597630515354 -16.607496433886265, -42.834588194159686 -16.60833834876866, -42.83456616036658 -16.610304020998203, -42.83455987168282 -16.610864996317446, -42.83455357262888 -16.61142687494601, -42.83570018105171 -16.613123752611752, -42.8368490185549 -16.614539676655795, -42.83771686773757 -16.615109753546854, -42.84121153113191 -16.61514610115703, -42.84299335143483 -16.61207661403741, -42.84417045428769 -16.61096493710458, -42.845047696888955 -16.61069396711775, -42.84649736901593 -16.611270041941385, -42.84795110785502 -16.61156607889063, -42.84968591739817 -16.612707035287002, -42.84996479373721 -16.613832916048953, -42.849961666044734 -16.614113858149256, -42.84993978056223 -16.616079549272445, -42.84993040591097 -16.61692147200248, -42.84991790217769 -16.618044336645227, -42.84989601077296 -16.62001002696874, -42.84989288175033 -16.620290968889293, -42.84988037511671 -16.62141383314044, -42.84985535894989 -16.623659561251227, -42.84984909927205 -16.624221444872134, -42.85012798479614 -16.625347326310543, -42.85156526980115 -16.627047147768796, -42.85418067255942 -16.627636148090314, -42.85739355868016 -16.62682640842619, -42.85767871975447 -16.627391302072226, -42.85824905646984 -16.628520185330906, -42.858236591894304 -16.629643054864236, -42.85851459469368 -16.63076892142787, -42.86171912032966 -16.63080195994396))) |
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_-5a9e |
Folha |
SE23 |
Legenda_Completa |
510Dt21 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
510 |
Nome_Unidade |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
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 das Chapadas dos Rios Jequitaà - Verde Grande |
Area_Poligono_Km2 |
26.476 |
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_-5a9d |
Folha |
SE23 |
Legenda_Completa |
515Kd |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
515 |
Nome_Unidade |
Serras de Unaà |
Letra_Simbolo |
Kd |
Categoria |
Carste descoberto |
Natureza |
dissolução |
Caracteristica |
carste descoberto |
Forma |
carste |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras de Unaà |
Area_Poligono_Km2 |
44.36 |
the_geom |
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