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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 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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2acf |
Folha |
SB24 |
Legenda_Completa |
393Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
393 |
Nome_Unidade |
Patamares do ParnaÃba |
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 do ParnaÃba |
Area_Poligono_Km2 |
191.013 |
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 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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2ad0 |
Folha |
SB24 |
Legenda_Completa |
367DEt22 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
367 |
Nome_Unidade |
Tabuleiros do ParnaÃba |
Letra_Simbolo |
DEt |
Categoria |
Estrutural tabular |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo tabular |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
18.43 |
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 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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2ad1 |
Folha |
SB24 |
Legenda_Completa |
367Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
367 |
Nome_Unidade |
Tabuleiros do ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
0.7 |
the_geom |
MULTIPOLYGON (((-41.30017302335131 -6.364385092280008, -41.30017730772148 -6.36534264542851, -41.300518691269495 -6.36204541064897, -41.300860070320894 -6.358748177668258, -41.3010270042778 -6.357135818245365, -41.30120106985835 -6.355455207473922, -41.30140076881531 -6.35352719770407, -41.298406952703594 -6.352773149443561, -41.2982004944422 -6.3513069406450375, -41.294309384255556 -6.348590432284878, -41.294037393296 -6.347813852409611, -41.293725380706675 -6.349411114913216, -41.2943733800124 -6.3516427600874925, -41.29438325187042 -6.353877065456308, -41.295028438096864 -6.35547033586926, -41.29631168252301 -6.357060712264084, -41.296956895729046 -6.35865382799375, -41.29728307084195 -6.360248347565153, -41.298247334731556 -6.361840054057086, -41.299846837446474 -6.362790576305885, -41.30017302335131 -6.364385092280008))) |
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 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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2ad2 |
Folha |
SB24 |
Legenda_Completa |
395Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto da Ibiapaba |
Identificacao_Unidade |
395 |
Nome_Unidade |
Serras Grande e da Ibiapaba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras Grande e da Ibiapaba |
Area_Poligono_Km2 |
2.259 |
the_geom |
MULTIPOLYGON (((-40.80186403668036 -6.326443973993206, -40.80059311476482 -6.328044863462693, -40.80060629702731 -6.331876291940136, -40.802215052866714 -6.335702134728493, -40.80413526641368 -6.337291855517344, -40.80636911492706 -6.337284029616918, -40.807963621008625 -6.336959155823181, -40.809235700351636 -6.335677547263779, -40.81083357079693 -6.336310750923064, -40.81243038184098 -6.336624813067409, -40.814028299051074 -6.337258157920266, -40.816900578982846 -6.337248756407513, -40.8184895875088 -6.335327630948108, -40.818802063248924 -6.333410815039933, -40.82039433091794 -6.332447380325197, -40.821346140096644 -6.330847616806949, -40.82294283422872 -6.33116131472581, -40.82357884826954 -6.330520516291771, -40.82421485961232 -6.3298797187568585, -40.82133388953173 -6.327335512406894, -40.816866236571904 -6.327350978048234, -40.81527502200901 -6.32863332405171, -40.81528165990498 -6.330549024800565, -40.81496804742177 -6.332146486054324, -40.81336793586582 -6.3308745694886985, -40.81272303742256 -6.328960952468971, -40.81239833090255 -6.327365579440882, -40.8104812874657 -6.3267332697075815, -40.80888678408219 -6.3270579906166855, -40.806969871047016 -6.326426118853233, -40.80536985661788 -6.325154561117152, -40.80186403668036 -6.326443973993206))) |
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 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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2ad3 |
Folha |
SB24 |
Legenda_Completa |
367Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
367 |
Nome_Unidade |
Tabuleiros do ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
1.906 |
the_geom |
MULTIPOLYGON (((-41.46263186825126 -6.32139255850301, -41.4646784158614 -6.322404146517272, -41.4667185045404 -6.322053825506837, -41.470793813868426 -6.32033176138495, -41.47214522330854 -6.3182823503335666, -41.47247578081771 -6.316237862170996, -41.472457952657585 -6.312492640006793, -41.47142901941883 -6.310795178638107, -41.47006143657114 -6.309439828369032, -41.46835682109557 -6.308767063532637, -41.4666489770537 -6.307413343734407, -41.46460733074881 -6.3074231643313015, -41.46222702404304 -6.307775099624756, -41.46121426691001 -6.309482398677443, -41.46054177996429 -6.311188062762372, -41.46021118018688 -6.313232568911382, -41.459875739359 -6.31425564126818, -41.45954029673239 -6.315278714524387, -41.45955803226244 -6.319023975359522, -41.45990879484013 -6.321235443344229, -41.46263186825126 -6.32139255850301))) |
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