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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_-57af |
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 |
14.135 |
the_geom |
MULTIPOLYGON (((-42.79158747910266 -16.036085301033825, -42.79159475300496 -16.035424941199945, -42.79138230969835 -16.034101883152644, -42.79070917582382 -16.03321406717322, -42.789584501622635 -16.03210114935757, -42.78844769621609 -16.032089427156496, -42.786848695512454 -16.03273336195956, -42.786602263009435 -16.034492575076026, -42.78635003234957 -16.03669171462851, -42.78587809235284 -16.038228150907674, -42.784266861399146 -16.03997325511986, -42.78264829559748 -16.042378698859, -42.78285187006131 -16.044582543144223, -42.7839692589762 -16.046355855014067, -42.784397413740365 -16.048782467282766, -42.78438036720689 -16.050323598508953, -42.78595274931322 -16.052101610731043, -42.787977691967455 -16.05410383110987, -42.78861637177708 -16.058030559693012, -42.78973630874572 -16.059583434933373, -42.789937520327996 -16.062007701472613, -42.790345380579694 -16.066194954256414, -42.79372089787259 -16.069532852341656, -42.79416375039141 -16.070638743677307, -42.79527408273755 -16.073072382452686, -42.79479480336302 -16.075269190280114, -42.794086038847986 -16.077684074355002, -42.7936042961436 -16.080101296088916, -42.79358242924715 -16.082082369896394, -42.794008288665125 -16.08472940002739, -42.7946587829095 -16.087598289769435, -42.794409852294216 -16.089577924066003, -42.79439041355214 -16.091338576860682, -42.7943660942729 -16.09354097329719, -42.794353943193784 -16.094641267970164, -42.79705661140549 -16.097091341351383, -42.79703475439201 -16.09907241663563, -42.79655538334277 -16.101270121471252, -42.79653351537622 -16.103251195310946, -42.796743572589676 -16.10479467417944, -42.79785892754031 -16.106788382221225, -42.799199892115205 -16.109003954587365, -42.80031772159774 -16.110777234216073, -42.80190279921155 -16.111453995131292, -42.80418460182754 -16.11081704221441, -42.80510206228321 -16.11016513742052, -42.80670651138219 -16.10908120004702, -42.80763120180898 -16.107769823150257, -42.80810080542347 -16.10645286640313, -42.808109268798354 -16.10568229251187, -42.80811773171363 -16.104911718560803, -42.80767957937319 -16.103365899632813, -42.80769118775476 -16.102308957697392, -42.80747768920168 -16.10098589158576, -42.80681006862352 -16.099657260030238, -42.80683182952999 -16.097676171806715, -42.80638886330824 -16.096570293143266, -42.806624114102135 -16.095912271097614, -42.80504881254406 -16.0943547736257, -42.804837755849206 -16.09281128532365, -42.80485469219005 -16.091270138896988, -42.80738357458959 -16.08887389096281, -42.80875594857511 -16.08822752600915, -42.80921729745664 -16.087571816252705, -42.80922213095139 -16.08713097100251, -42.80990998056712 -16.086698027806353, -42.810151506441564 -16.085379623852802, -42.810386737201085 -16.08472069048265, -42.810635489522056 -16.082741919684636, -42.810649955798795 -16.08142118876532, -42.81112427239549 -16.079664269487772, -42.81114114571439 -16.078123114658784, -42.81229991574378 -16.076152746132205, -42.81298197301116 -16.07615972101654, -42.814121446996204 -16.075951823975682, -42.81480925624212 -16.07551795513474, -42.81687318492459 -16.073997696673615, -42.817119450815625 -16.07223842762154, -42.81712905340951 -16.071358537924187, -42.817141070600066 -16.07025732062633, -42.81556585263382 -16.06869991213456, -42.81422250613662 -16.066703966251634, -42.813770843794785 -16.066479807876544, -42.81287048238675 -16.06558971894071, -42.81288973569811 -16.06382813663251, -42.81290898661505 -16.062066554012006, -42.81292341829612 -16.060745818529774, -42.81294025684624 -16.059204659119917, -42.81249731221677 -16.05809879581336, -42.8109173981253 -16.05698221482293, -42.810021909933205 -16.055651273233558, -42.80821983903632 -16.054091508215393, -42.806647214055005 -16.052314536641838, -42.80642168109325 -16.05209177924122, -42.803937704519285 -16.05052500020857, -42.80280802747965 -16.0498529771106, -42.80055260364839 -16.048068061867145, -42.798977682858336 -16.04651056597646, -42.796268326491244 -16.044720949895634, -42.79492381662849 -16.04294625707876, -42.7949407838038 -16.041404210417458, -42.79269521556769 -16.038739353723965, -42.79225969105353 -16.03697310610899, -42.79158747910266 -16.036085301033825))) |
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_-57ae |
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 |
62.996 |
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_-57ad |
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 |
1.626 |
the_geom |
MULTIPOLYGON (((-43.361783158071 -16.858301944345104, -43.362673608072576 -16.857881622695075, -43.36333798111114 -16.85788692467607, -43.36333981608118 -16.857673675404335, -43.364453550947864 -16.85704186282924, -43.364457225935105 -16.85661446040824, -43.365797918332234 -16.855342849146783, -43.366691069980455 -16.854496001102884, -43.367356370900104 -16.85450129651297, -43.36824951969059 -16.853653537063735, -43.368474638223326 -16.85322789476161, -43.36937420472451 -16.851739483137685, -43.37026826182787 -16.850892623823487, -43.37160245451274 -16.850261614098702, -43.372491015956065 -16.850055398335925, -43.373824304840106 -16.849638534552227, -43.37382795707703 -16.849211129821654, -43.37405487942596 -16.848572229073774, -43.37406035273768 -16.847931573633108, -43.3738389054288 -16.847929819122864, -43.372287836672996 -16.84791752342623, -43.37095821615491 -16.847906973873048, -43.37007515049225 -16.84747252957004, -43.36919485461673 -16.846824839132896, -43.368759289522394 -16.845966512050854, -43.369209501910326 -16.84511522358042, -43.36944009401449 -16.84404892461142, -43.369447407755864 -16.843195020139127, -43.367896380971295 -16.84318269462117, -43.36633252214615 -16.844665817360745, -43.36610558055669 -16.845304707946752, -43.364322085487935 -16.846571896131525, -43.36253855955154 -16.84783997018393, -43.36164815841841 -16.848260295728014, -43.35853867079562 -16.8490894073241, -43.35698391446117 -16.849504396328612, -43.356089802972285 -16.85035209684023, -43.35584989744311 -16.85248642310173, -43.35538483634806 -16.855046373644765, -43.35647642942223 -16.8569781060371, -43.360901908752254 -16.857654209562405, -43.361783158071 -16.858301944345104))) |
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_-57ac |
Folha |
SE23 |
Legenda_Completa |
069Pgu |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
69 |
Nome_Unidade |
Planalto de Cristalina |
Letra_Simbolo |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto de Cristalina |
Area_Poligono_Km2 |
9.762 |
the_geom |
MULTIPOLYGON (((-47.35450570266001 -17.049139751575606, -47.35909134238018 -17.04197834498289, -47.35922055013439 -17.034764780629715, -47.358931703759346 -17.029253394828977, -47.36215111542291 -17.02242760035084, -47.36713234990858 -17.015582183667348, -47.37547458530062 -17.013151679852154, -47.37518978680571 -17.008063961909585, -47.377787649687875 -17.004427618407853, -47.383931533630395 -17.002446156420074, -47.38501111854512 -17.00073710484614, -47.38343685820853 -16.998146802171075, -47.39065728477274 -16.994244789251503, -47.38511551238459 -16.99155199408325, -47.375923344444175 -16.996325940923096, -47.36669776906112 -16.998554374225787, -47.36421391120077 -16.99370443200072, -47.36543973987138 -16.98605447561126, -47.356414772301186 -16.986582732839835, -47.356958362056034 -16.99484904210196, -47.360108201851254 -17.000115930570395, -47.362804685794806 -17.004327520425367, -47.359121331095885 -17.00924816337021, -47.351891635646716 -17.012514262199456, -47.34910428905572 -17.01869808985834, -47.34983402567461 -17.024204433181936, -47.35055058824306 -17.02865132466174, -47.35217262712708 -17.03499553833024, -47.34918032337506 -17.042454542888088, -47.3470121254717 -17.045237446911578, -47.35189854715778 -17.04836240184242, -47.35266905520267 -17.048926178889968, -47.35450570266001 -17.049139751575606))) |
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_-57ab |
Folha |
SE23 |
Legenda_Completa |
069Dc31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
69 |
Nome_Unidade |
Planalto de Cristalina |
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 |
Planalto de Cristalina |
Area_Poligono_Km2 |
17.911 |
the_geom |
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