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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_-5777 |
Folha |
SE23 |
Legenda_Completa |
027Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos Cimeiros |
Identificacao_Unidade |
27 |
Nome_Unidade |
Planalto dos Geraizinhos |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto dos Geraizinhos |
Area_Poligono_Km2 |
0.912 |
the_geom |
MULTIPOLYGON (((-42.5072664321188 -16.09561314357217, -42.50737190938827 -16.095546626286275, -42.507607313999614 -16.095251281570103, -42.50806864372634 -16.094671320184613, -42.508307611903774 -16.093790672904742, -42.5087818996996 -16.0924710514295, -42.50948044079404 -16.091374448909605, -42.51017713833041 -16.090500035441085, -42.510642218905474 -16.089842425031666, -42.51202735210174 -16.088754711047763, -42.512035608372244 -16.088091777793025, -42.51090411263404 -16.087195166682537, -42.509767122618314 -16.086740204697115, -42.50978087852124 -16.0856365218483, -42.50979188697496 -16.08475321420805, -42.51049131252213 -16.083657517142232, -42.51164110861707 -16.083007874412626, -42.51255839021787 -16.082798141468242, -42.513482984432635 -16.081925459075627, -42.51345454115865 -16.081808601146435, -42.513265107707205 -16.08103948688264, -42.51235700880315 -16.08058720430111, -42.51144891444016 -16.080134918419734, -42.51030370310573 -16.08034289745016, -42.509844162138315 -16.080557953409166, -42.5093763591956 -16.081435940603118, -42.508225644502616 -16.08208465739784, -42.50798576362326 -16.08296529649132, -42.50797474848084 -16.083848603060765, -42.507963732652165 -16.08473190954993, -42.50818709443551 -16.085176230860306, -42.508181586596834 -16.0856178841317, -42.508173330149155 -16.08627991241322, -42.50793344121719 -16.08716055039305, -42.50700328718453 -16.088474854297193, -42.50655198683659 -16.088027872560158, -42.50518888552476 -16.087349842208273, -42.50450413823869 -16.08734184832431, -42.50404457565348 -16.087556888524073, -42.504039057803254 -16.087998540298614, -42.503573028670736 -16.088656123052534, -42.50334508971512 -16.088653460370473, -42.501754071828685 -16.087971843071653, -42.50084320913613 -16.087740787967427, -42.500608812036674 -16.088179762205606, -42.50059776053156 -16.089063063359525, -42.50059223452092 -16.089504713906308, -42.50050900209422 -16.08973498599562, -42.50035507649541 -16.09016406106475, -42.50030323655999 -16.09034953505544, -42.50033960131763 -16.090579399334874, -42.50049745173054 -16.09065802646315, -42.50081080996611 -16.090853191745847, -42.501087788190425 -16.090894369669066, -42.50140304201174 -16.091012775581127, -42.50167716599648 -16.091207481007586, -42.502147903879006 -16.09151920413253, -42.50250096113433 -16.09175277013279, -42.502775547206106 -16.091985418578968, -42.503442915193304 -16.09241325359763, -42.50347641596123 -16.09287252369395, -42.50410167373822 -16.09353020787919, -42.504138517089615 -16.09372213888584, -42.50425477887221 -16.093914094307706, -42.504411200267796 -16.094107422090442, -42.5046848575616 -16.094340057892495, -42.50484130473943 -16.094456604813686, -42.505154174725554 -16.094766479046303, -42.505344587490946 -16.095380240277628, -42.50549816993156 -16.09572619299607, -42.50565172800305 -16.096148926347727, -42.50576703341579 -16.096417651085765, -42.50599040083125 -16.096413032508927, -42.5072664321188 -16.09561314357217))) |
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_-5776 |
Folha |
SE23 |
Legenda_Completa |
512Dt21 |
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 |
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 Urucuia - Paracatu |
Area_Poligono_Km2 |
7.652 |
the_geom |
MULTIPOLYGON (((-46.08138704817957 -16.298596095100457, -46.0825020445425 -16.29558588643931, -46.08276461869427 -16.291760219110202, -46.082235015292504 -16.29092683962262, -46.081537985171195 -16.290451348267354, -46.08083990843232 -16.28978423670632, -46.08024051142787 -16.289020806967628, -46.07944178482703 -16.28825839266985, -46.081326455361165 -16.288057142075182, -46.082314241219514 -16.287285597434373, -46.08280550222527 -16.28642077949386, -46.08111335773905 -16.285375508211605, -46.080809987116346 -16.28432222736712, -46.08001483618795 -16.284038853714133, -46.080738524107865 -16.283576889146694, -46.080441511833534 -16.281119844439466, -46.07874950242898 -16.281458395624345, -46.07875578649172 -16.282608103375384, -46.077365467175476 -16.282327753093334, -46.07567506019696 -16.281761484210417, -46.075571165151004 -16.280899706751576, -46.075863007784676 -16.27984429380599, -46.07595802507775 -16.279077316685846, -46.07594967007985 -16.277544371062547, -46.0759345240029 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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_-5775 |
Folha |
SE23 |
Legenda_Completa |
103Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Médio Rio São Francisco |
Area_Poligono_Km2 |
207.287 |
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_-5774 |
Folha |
SE23 |
Legenda_Completa |
149Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
149 |
Nome_Unidade |
Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
5.381 |
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_-5773 |
Folha |
SE23 |
Legenda_Completa |
510Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
Area_Poligono_Km2 |
27.125 |
the_geom |
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