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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_-5f65 |
Folha |
SE23 |
Legenda_Completa |
524Pru |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
Pru |
Categoria |
Pediplano retocado desnudado |
Natureza |
aplanamento |
Caracteristica |
retocado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
12.477 |
the_geom |
MULTIPOLYGON (((-43.875875816005085 -18.666177402586754, -43.87692532219972 -18.666183681655774, -43.87815022065305 -18.666191002658792, -43.879908023878805 -18.6650321529105, -43.88114167302143 -18.663703889440185, -43.882199773581604 -18.662540846614622, -43.88308246648648 -18.661377657791917, -43.8830966769796 -18.659206233404486, -43.88433571500434 -18.65704298936577, -43.88503971200518 -18.656379358862832, -43.88574806799332 -18.655047037771258, -43.88697383823509 -18.655054302682014, -43.887855510230125 -18.65389108117456, -43.88978089663492 -18.653902466792815, -43.89135878090222 -18.65341024680073, -43.89188722050533 -18.652912731322097, -43.89224244760689 -18.652079835771225, -43.89365020565121 -18.650918780887956, -43.89557893326704 -18.6502623132743, -43.89629028405227 -18.648596509951698, -43.89612354731552 -18.647259002657, -43.89438657256672 -18.645245357754106, -43.89492362279076 -18.64341135418668, -43.896328049070405 -18.642751791712456, -43.8984298923001 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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_-5f64 |
Folha |
SE23 |
Legenda_Completa |
531Dt31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
531 |
Nome_Unidade |
Serra da Saudade |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serra da Saudade |
Area_Poligono_Km2 |
133.069 |
the_geom |
MULTIPOLYGON (((-45.596479689049474 -18.650645747442027, -45.59326668244344 -18.651240652810102, -45.5885250181127 -18.65286245598847, -45.58455185452785 -18.65521289929599, -45.58134567914842 -18.65785280567334, -45.57920537659663 -18.65888157556306, -45.57743945749224 -18.66127656997548, -45.57470177790572 -18.664008917599517, -45.57470965236877 -18.666346937196757, -45.57808334576691 -18.66633658369685, -45.579622496175844 -18.667793229056926, -45.58116470564147 -18.670418419801766, -45.58086539471836 -18.67246456613765, -45.57811008328913 -18.6742263740988, -45.573513136291325 -18.675409041365985, -45.56861860840761 -18.679223361713767, -45.569855438968375 -18.682141484947508, -45.57353476249465 -18.68183836144631, -45.57660246684519 -18.681828962035627, -45.578751366759406 -18.682406179691093, -45.58242463606395 -18.68005768308869, -45.58364169857807 -18.67713112994715, -45.587315791479774 -18.675074453865115, -45.59160640685927 -18.67418433215402, -45.59498738044328 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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_-5f63 |
Folha |
SE23 |
Legenda_Completa |
549Da32 |
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 |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
20.699 |
the_geom |
MULTIPOLYGON (((-44.796322629226246 -18.66508765898981, -44.795817577484726 -18.6695428348259, -44.79400964973394 -18.673918855537252, -44.79171155731726 -18.676574387386346, -44.78728272947016 -18.679071130491696, -44.784983711751465 -18.68157021922003, -44.78481665232331 -18.684697161841395, -44.78694523375488 -18.68657587059995, -44.79104441190226 -18.685485982997818, -44.79317648750633 -18.685331988168848, -44.79251528213792 -18.689396532362156, -44.79103194824193 -18.695649150080698, -44.788896426799454 -18.699242958294498, -44.78676198950138 -18.70189860286265, -44.7844614234778 -18.706117594205416, -44.78281435035818 -18.71174451870995, -44.780350265197036 -18.715337839018723, -44.78116288526192 -18.7214366770615, -44.787557630517256 -18.720974969006257, -44.792642791215926 -18.719417104512853, -44.794612699523974 -18.717230287449578, -44.79723836893352 -18.71551322817125, -44.7993730013736 -18.712701112123284, -44.80314749237795 -18.709890699602497, -44.80626344174416 -18.70973758948971, -44.80937773708085 -18.710209851643103, -44.813151494356475 -18.707868303954015, -44.81397439275219 -18.704741991508154, -44.81168379776414 -18.70051807707416, -44.811849776773656 -18.69879832067469, -44.81447652127457 -18.69567380356966, -44.81661129217791 -18.69223605403172, -44.81628753338362 -18.68817045981121, -44.81874896975646 -18.685983857089884, -44.818095494041344 -18.684263298636033, -44.817606148358486 -18.681604755446493, -44.81974067757379 -18.678166963103045, -44.8230228500799 -18.675355658364012, -44.821222638305514 -18.67207045298368, -44.82040612730707 -18.66941160180477, -44.8209027056741 -18.66519043059729, -44.82318441599616 -18.66220282356029, -44.82299064390514 -18.661611556099313, -44.82372347454913 -18.66174871890963, -44.82490852034536 -18.661970354259697, -44.82594492361542 -18.661971317348883, -44.827325479208305 -18.662960444523208, -44.828361392324844 -18.66345486853559, -44.829397804799285 -18.66345581264824, -44.83008893316666 -18.662633981205335, -44.83078100397984 -18.661811244149774, -44.832335295418446 -18.66164814614622, -44.83302702872099 -18.66115528737413, -44.83354539652735 -18.660496877045716, -44.83371957332242 -18.658852114761288, -44.83372037532485 -18.658028753301945, -44.83354860530628 -18.657206142779827, -44.83303169726757 -18.65638232188347, -44.83234111417459 -18.65572374017018, -44.831651647666426 -18.65489976138941, -44.83147878012986 -18.654241639543454, -44.83061642925461 -18.653747389078266, -44.82975264322182 -18.6537466085656, -44.82871628967377 -18.653745666882607, -44.82681615030161 -18.653743925475258, -44.82526209435509 -18.653742486958805, -44.824398477751444 -18.65357719030123, -44.8235358110257 -18.653411890576184, -44.82301835565494 -18.65225905830711, -44.8230193794132 -18.651271205169557, -44.82336621066176 -18.649626614007715, -44.82371262599954 -18.6492970518896, -44.82440406182705 -18.648146256616133, -44.82423217795182 -18.647487224999512, -44.82371483389543 -18.647157756971996, -44.82319620320217 -18.64715726991688, -44.82198698632201 -18.64748511233758, -44.82060416586117 -18.648800635703083, -44.81991140587172 -18.650281302688388, -44.81852994597795 -18.650279974025093, -44.81732034635926 -18.650936769100543, -44.814211570548885 -18.651592592352095, -44.81317523095413 -18.651591565082672, -44.81161988470961 -18.651918995892483, -44.81006602963209 -18.65175294042772, -44.80868437433 -18.651916030720358, -44.80626769573372 -18.651749063621775, -44.796322629226246 -18.66508765898981))) |
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_-5f62 |
Folha |
SE23 |
Legenda_Completa |
561Da52 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
561 |
Nome_Unidade |
Depressão Interplanáltica do Rio Corumbá |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão Interplanáltica do Rio Corumbá |
Area_Poligono_Km2 |
2.086 |
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_-5f61 |
Folha |
SE23 |
Legenda_Completa |
547Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
547 |
Nome_Unidade |
Planalto de PatrocÃnio |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto de PatrocÃnio |
Area_Poligono_Km2 |
78.093 |
the_geom |
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