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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_2a47 |
Folha |
SB24 |
Legenda_Completa |
643Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Aplanamentos Residuais do Domo da Borborema |
Identificacao_Unidade |
643 |
Nome_Unidade |
Serras de Santana e Cuité |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras de Santana e Cuité |
Area_Poligono_Km2 |
18.298 |
the_geom |
MULTIPOLYGON (((-36.032477666589735 -6.599182218058983, -36.03403197387526 -6.601041634737681, -36.03401252873389 -6.6043146192980045, -36.03357970571755 -6.605308159717757, -36.03272166794933 -6.606014507037755, -36.0317289405169 -6.605439261086879, -36.03087428419952 -6.605576394209105, -36.02888290909761 -6.605422027378529, -36.02830862002553 -6.606272398426133, -36.02758440227699 -6.608402631549876, -36.02771986535815 -6.609541913402193, -36.027569006783 -6.610964075205529, -36.02613655853399 -6.612520775586959, -36.02641603005439 -6.613376314139152, -36.026837807597424 -6.6142327169400055, -36.02754590499822 -6.6148062406889006, -36.02924928120802 -6.6155281094082445, -36.030949242692074 -6.616819191425947, -36.03194195933263 -6.617394445470676, -36.03379790013166 -6.616409545737498, -36.03678544527071 -6.616569974897832, -36.03778669377968 -6.615722194796959, -36.03793496680401 -6.6147269312764, -36.03879225633625 -6.614162772167716, -36.039645322652134 -6.61431004874336, 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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_2a48 |
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 |
2.655 |
the_geom |
MULTIPOLYGON (((-41.92750881056882 -6.21777627594099, -41.928155175806424 -6.219367828648931, -41.92720763570955 -6.220968326913251, -41.92561900579812 -6.221934355272728, -41.924990236695685 -6.223533070181463, -41.923089843307274 -6.2257770045914524, -41.922779909950556 -6.2273739307485885, -41.92597843424295 -6.2292701692691494, -41.92725536003253 -6.2295820262757085, -41.92981811849705 -6.231800861506708, -41.93112349883607 -6.23426120967312, -41.93242889176559 -6.236721553342987, -41.933362222574196 -6.238480635358912, -41.93717523743294 -6.236225939661471, -41.93844147388058 -6.234623651746258, -41.93843076025704 -6.232709519414866, -41.93682967653407 -6.231442395336384, -41.93554560473149 -6.229854451607861, -41.933765389546714 -6.227273088868204, -41.934569626272925 -6.226350573306545, -41.93286590742142 -6.224327232702109, -41.9336258849123 -6.222463820335546, -41.93420129364046 -6.2210529522184945, -41.93482283938814 -6.219528950287482, -41.93516482368333 -6.218690417015767, -41.93708103974385 -6.2193177292164, -41.93837562641969 -6.2204295952361255, -41.93941445489881 -6.219049223129692, -41.939944763525695 -6.218344558441208, -41.93834909462074 -6.218034480293589, -41.9364400767338 -6.215915843927749, -41.937070292845405 -6.214404088064862, -41.93768326535608 -6.212933688425654, -41.93520886258462 -6.210640356054473, -41.93543417063614 -6.209755962754339, -41.93352504842789 -6.210404730081179, -41.93193293364372 -6.210732687650305, -41.93066488146483 -6.212015935673732, -41.93035668020225 -6.213931873843622, -41.92845634347112 -6.216175780374624, -41.92750881056882 -6.21777627594099))) |
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_2a49 |
Folha |
SB24 |
Legenda_Completa |
393Dt22 |
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 |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
100.562 |
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_2a4a |
Folha |
SB24 |
Legenda_Completa |
506Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
506 |
Nome_Unidade |
Baixada de Campo Maior |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Baixada de Campo Maior |
Area_Poligono_Km2 |
1.234 |
the_geom |
MULTIPOLYGON (((-41.967628301790484 -5.157425448247678, -41.96881665604951 -5.159780761894315, -41.97008201655758 -5.158179715942953, -41.97103512885376 -5.157856252286005, -41.972633582059906 -5.159443975680667, -41.97453533342456 -5.15783997725488, -41.97516129304485 -5.155603853456925, -41.97515234389132 -5.1536897121323415, -41.97419029323308 -5.152099028169536, -41.97291154181993 -5.1508288436983065, -41.971314597676205 -5.149560132316406, -41.97066926935705 -5.14764893807018, -41.97288024091606 -5.14412933602233, -41.972554596403235 -5.142535690591962, -41.97127593222421 -5.141265489932843, -41.96968350087855 -5.140953837971547, -41.96959401114042 -5.142895871769416, -41.9695200032313 -5.144503441402941, -41.96621750921629 -5.148307662690662, -41.96665324243888 -5.15023109760904, -41.96496256465628 -5.152141887160237, -41.96573337538066 -5.153669666244011, -41.966439955625184 -5.155070129205008, -41.967628301790484 -5.157425448247678))) |
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_2a4b |
Folha |
SB24 |
Legenda_Completa |
367Dt33 |
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 |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
82.888 |
the_geom |
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