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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_-5df8 |
Folha |
SE23 |
Legenda_Completa |
524Dc31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
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 |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
2.066 |
the_geom |
MULTIPOLYGON (((-43.2737670444795 -18.075669421832675, -43.27303202444772 -18.07384043674464, -43.27170095924766 -18.07297469309681, -43.27091247645429 -18.07371484696674, -43.27091143260085 -18.073821453493142, -43.269012610582266 -18.07401857082877, -43.26800851822794 -18.074009564236192, -43.26643779653569 -18.074849293414893, -43.26476609328331 -18.074620137938535, -43.2651475869079 -18.076174010777688, -43.26526255127225 -18.0768761771063, -43.26464220601093 -18.077805745378495, -43.264144652805065 -18.078736415574355, -43.26401726081304 -18.079202390191757, -43.263525449857184 -18.07954853168949, -43.26473169256973 -18.08119565910377, -43.2650913054078 -18.081900928779856, -43.26421709280857 -18.08376245173369, -43.26214004781286 -18.083627200691353, -43.26212624018192 -18.085029339474687, -43.263087837745495 -18.086674274160632, -43.263809179912975 -18.087966476993838, -43.26392643575634 -18.08843555587747, -43.26537855044054 -18.08996834139065, -43.265619773143094 -18.090321076667635, -43.267078813722364 -18.091151877547492, -43.26743156700152 -18.092558215462, -43.267548843481855 -18.093026389562468, -43.268156612931804 -18.0933824146061, -43.26900332280676 -18.094325161405557, -43.26912383649695 -18.094560255279653, -43.27017654532589 -18.095018751573086, -43.27168126538673 -18.092929745471462, -43.27100850134727 -18.0931315255426, -43.27059848322608 -18.09332301013279, -43.2714386037045 -18.090986803226095, -43.27023059777745 -18.08921771812631, -43.27023314879899 -18.088957526433102, -43.27099089383537 -18.087987611373933, -43.2722876257668 -18.087739014794604, -43.27208965072694 -18.087020747322224, -43.27305427580875 -18.085857514156412, -43.27455822322482 -18.085284583127187, -43.27530256040403 -18.085682464911223, -43.27529874580524 -18.08607275362777, -43.27686180266845 -18.086411989991102, -43.277339178461155 -18.086286145547955, -43.27931858006667 -18.085783378847065, -43.279199059547366 -18.084089103928505, -43.27859360894516 -18.083302152687274, -43.27818170874155 -18.083689704363362, -43.27763474696236 -18.08387998421392, -43.27689739676099 -18.082766581439014, -43.27540620734222 -18.082036763524897, -43.27459768650048 -18.08124798638929, -43.27439779014648 -18.080725768466046, -43.27412828290835 -18.080463143070904, -43.27264061617063 -18.079473122362845, -43.272302802206674 -18.079143926035787, -43.27087933763096 -18.078545693829096, -43.27115903793462 -18.077766651267783, -43.27470614855882 -18.07710990638584, -43.27512121643632 -18.076397120349032, -43.2737670444795 -18.075669421832675))) |
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_-5df7 |
Folha |
SE23 |
Legenda_Completa |
518Atf1 |
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 |
Atf |
Categoria |
Terraço fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
PlanÃcies e Terraços Fluviais do Rio Doce |
Area_Poligono_Km2 |
1.826 |
the_geom |
MULTIPOLYGON (((-42.41559056773818 -19.393578760189566, -42.416362245769776 -19.391233778435137, -42.41694402567852 -19.390066327761527, -42.41865898418098 -19.388486943805848, -42.41979386057829 -19.387967571225477, -42.421040237435555 -19.387558134482575, -42.42228734951702 -19.387041240227067, -42.42330151702982 -19.387055619569797, -42.42476737753787 -19.38696893434193, -42.42613105445959 -19.38623964838312, -42.42693822054748 -19.385075347365724, -42.427297791356196 -19.383690692627802, -42.42754678302831 -19.382197012686717, -42.4282575086683 -19.379961261124794, -42.428725228109045 -19.37889870185758, -42.42942417107658 -19.377411378364545, -42.43045169852358 -19.37657074085654, -42.43158812993466 -19.375944747341638, -42.432494053249705 -19.375636967166113, -42.4335072070153 -19.37565126808986, -42.43474677570459 -19.375668757242387, -42.43564767566203 -19.375681462795907, -42.43610099959859 -19.37547383795138, -42.436560289747035 -19.374945722659948, -42.43805780387673 -19.372828462804865, -42.43875591942457 -19.371447636702815, -42.43799236725942 -19.36983311200762, -42.43585865400953 -19.369375917750535, -42.43372256989513 -19.369131779379664, -42.43237080062163 -19.369112704557768, -42.43090511168819 -19.369198567308793, -42.42971040248132 -19.369114867217817, -42.428999933801535 -19.37224914130113, -42.425030742024276 -19.37681824576961, -42.42116417582877 -19.381019361984045, -42.415811617202635 -19.38675153148241, -42.41489451162749 -19.389328324396885, -42.41489304284207 -19.389421313553978, -42.41498278306532 -19.389884931173196, -42.41518009501082 -19.39130997861188, -42.415176446557226 -19.391721699355156, -42.41525660904013 -19.392731501855728, -42.41559056773818 -19.393578760189566))) |
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_-5df6 |
Folha |
SE23 |
Legenda_Completa |
524Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
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 |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
21.162 |
the_geom |
MULTIPOLYGON (((-43.29073175659219 -18.095260770585824, -43.28965008674245 -18.09446962671671, -43.290197072573854 -18.094279314643483, -43.29095284970989 -18.093504460138323, -43.29205595355127 -18.092082136000595, -43.2929594019396 -18.09020175377208, -43.292829041548075 -18.089614208144955, -43.29248832751289 -18.089676246640412, -43.291463340971724 -18.09005839941179, -43.29112199570854 -18.090185484011112, -43.290229894683165 -18.09089317443506, -43.2890084244068 -18.090492018010266, -43.28894166912549 -18.090361317534228, -43.2884016456799 -18.089835189642372, -43.288266874299154 -18.089703885429554, -43.286775246333164 -18.089105155895503, -43.28664080427826 -18.088842841867315, -43.28713365968502 -18.087219962406436, -43.28624977374996 -18.087082004214498, -43.286057740171266 -18.085843366816796, -43.28749585106476 -18.08494447600605, -43.28614409330845 -18.08395575772508, -43.28443678415325 -18.084461017204642, -43.2840185674395 -18.08549906639931, -43.28407898328778 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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_-5df5 |
Folha |
SE23 |
Legenda_Completa |
519Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
38.29 |
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_-5df4 |
Folha |
SE23 |
Legenda_Completa |
549Dt11 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
549 |
Nome_Unidade |
Patamares das Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
44.747 |
the_geom |
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