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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_-58c7 |
Folha |
SE23 |
Legenda_Completa |
069Dt11 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
69 |
Nome_Unidade |
Planalto de Cristalina |
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 |
Planalto de Cristalina |
Area_Poligono_Km2 |
33.004 |
the_geom |
MULTIPOLYGON (((-47.3793237413253 -16.322612556811073, -47.40329609397839 -16.29852424110888, -47.40652003161596 -16.296129821201916, -47.40933227259599 -16.29334710205922, -47.4125800886229 -16.292917097724587, -47.41664631698799 -16.2928706397483, -47.42113288175359 -16.293998139331276, -47.42482519765761 -16.29670644967415, -47.428489495205184 -16.29705731445318, -47.43133532145665 -16.297024586299106, -47.43820850552483 -16.29380181593609, -47.4414221418242 -16.29062115126919, -47.44421427629323 -16.286266489315878, -47.44538012036761 -16.281930617223015, -47.44979820092748 -16.277557100190187, -47.452580227590154 -16.27241660005509, -47.45291375043485 -16.26651768332897, -47.45448119532392 -16.261784195986014, -47.45444214298583 -16.258641104582406, -47.45238018076261 -16.256307335721583, -47.448315748509806 -16.25635436723759, -47.44552890366681 -16.2611019135591, -47.44517080787878 -16.265035502335568, -47.44439230038842 -16.267795111979492, -47.44441663284337 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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_-58c6 |
Folha |
SE23 |
Legenda_Completa |
561Dc52 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
561 |
Nome_Unidade |
Depressão Interplanáltica do Rio Corumbá |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão Interplanáltica do Rio Corumbá |
Area_Poligono_Km2 |
24.774 |
the_geom |
MULTIPOLYGON (((-47.96831441984483 -17.000213656376246, -47.96790971276419 -17.00019788889548, -47.966204056997334 -17.000222759317854, -47.96487722402336 -16.99987098494283, -47.96433317380157 -17.000303296409072, -47.963959345704076 -17.000997690979027, -47.96336909531314 -17.002013075016045, -47.9628953857082 -17.003397872751954, -47.96164972165935 -17.00468826476213, -47.96028416178574 -17.005397090607506, -47.959076347094026 -17.00557448505342, -47.957194567311944 -17.004965267394223, -47.95498005971614 -17.00420284672134, -47.95293494548783 -17.00364923221311, -47.950961696526846 -17.00420789811172, -47.94900502806276 -17.0058263781878, -47.94937014318991 -17.008046874342092, -47.95031888251479 -17.008881894483512, -47.95137335023285 -17.00939663140562, -47.95270439113921 -17.01001299266861, -47.953925559753344 -17.010684214051093, -47.95646127281072 -17.010859562384663, -47.95720214164573 -17.012438888682343, -47.95733939127023 -17.014185909498252, -47.95488562206395 -17.01570603638216, -47.953630476634764 -17.016400585652516, -47.95425820689013 -17.017886755973755, -47.95438273447586 -17.018107072820587, -47.95643669074581 -17.019332316697767, -47.95981431679716 -17.018310690705142, -47.96074496164916 -17.01781044987438, -47.96298060983133 -17.01763882528461, -47.96637582672283 -17.017797894663236, -47.970646798316565 -17.01850032371738, -47.97196953296558 -17.02000966988102, -47.97163336439129 -17.02154326378785, -47.97042910586084 -17.023020923167103, -47.96907045308088 -17.02387509432509, -47.967932754703945 -17.024933708354613, -47.96644163145223 -17.026554593799073, -47.96573757400583 -17.027676395336087, -47.96598720577991 -17.029757650449767, -47.965570130612036 -17.03080663958774, -47.96471936980093 -17.031792431113256, -47.96366497173062 -17.033614610127014, -47.96331794161438 -17.03452352171709, -47.963629961331115 -17.035978129691014, -47.965316268321395 -17.037621255732667, -47.966855752062614 -17.03905883149365, -47.97003661909239 -17.0392904417954, -47.973792398570055 -17.03937453024115, -47.974630730070395 -17.04193381888369, -47.97482962254275 -17.04323203798706, -47.97309704404981 -17.045197831219404, -47.97084322975611 -17.04607958910634, -47.966009027296785 -17.051121882064926, -47.966175006933824 -17.053666657898166, -47.9687331402781 -17.056054548599956, -47.97350977622932 -17.055377829074605, -47.97676775542617 -17.05423931271195, -47.9815577600132 -17.054410973680177, -47.985663648852665 -17.05908014514581, -47.98751970154059 -17.064873994582378, -47.99216261251196 -17.065107123755414, -47.993343584507926 -17.067640454550325, -47.99466863940181 -17.069082721182617, -47.995284602620025 -17.06897430141735, -48.00044655395828 -17.067670915349513, -48.00044648832769 -17.061679148925172, -48.00044562191798 -17.002695871634227, -47.99985739951555 -17.002588068495154, -47.99132778571138 -17.001026983165826, -47.9891920402406 -17.002332404823036, -47.98232146505996 -17.00177228114668, -47.97615257389953 -17.00214613102874, -47.97051769085494 -17.002228476689577, -47.968988310019824 -17.00158984435138, -47.96831441984483 -17.000213656376246))) |
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_-58c5 |
Folha |
SE23 |
Legenda_Completa |
548Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
548 |
Nome_Unidade |
Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
2.212 |
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_-58c4 |
Folha |
SE23 |
Legenda_Completa |
554Pgu |
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 |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
3.206 |
the_geom |
MULTIPOLYGON (((-47.66424428545763 -17.501149195541302, -47.66226404626407 -17.49462373012903, -47.65863577180731 -17.49169932553797, -47.657248432571684 -17.485928055132035, -47.656688696101504 -17.48108402735817, -47.65341677430727 -17.48018852728303, -47.64920262011506 -17.481809880680302, -47.64494859520329 -17.48061485570294, -47.64252091237321 -17.481742654699676, -47.641900508691144 -17.48394187958625, -47.642921077918686 -17.48690137128918, -47.64232101636235 -17.490508291663925, -47.64334391651855 -17.493624886093137, -47.64843580405338 -17.496373830591555, -47.65514625095343 -17.498318879707387, -47.662518030402474 -17.500880663904844, -47.66424428545763 -17.501149195541302))) |
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_-58c3 |
Folha |
SE23 |
Legenda_Completa |
177Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
177 |
Nome_Unidade |
Patamares da Borda Ocidental do Espinhaço |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares da Borda Ocidental do Espinhaço |
Area_Poligono_Km2 |
61.816 |
the_geom |
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