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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_33ed |
Folha |
SB24 |
Legenda_Completa |
639Apfm |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies Deltáicas, Estuarinas e Praiais |
Identificacao_Unidade |
639 |
Nome_Unidade |
Litoral Setentrional Nordestino |
Letra_Simbolo |
Apfm |
Categoria |
PlanÃcie fluviomarinha |
Natureza |
acumulação |
Caracteristica |
fluviomarinho |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Litoral Setentrional Nordestino |
Area_Poligono_Km2 |
0.97 |
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_33ee |
Folha |
SB24 |
Legenda_Completa |
393Ai1 |
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 |
Ai |
Categoria |
Plano de inundação |
Natureza |
acumulação |
Caracteristica |
inundação |
Forma |
plano abaciado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
36.297 |
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_33ef |
Folha |
SB24 |
Legenda_Completa |
506Ai1 |
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 |
Ai |
Categoria |
Plano de inundação |
Natureza |
acumulação |
Caracteristica |
inundação |
Forma |
plano abaciado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
Baixada de Campo Maior |
Area_Poligono_Km2 |
1.609 |
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_33f0 |
Folha |
SB24 |
Legenda_Completa |
393Da22 |
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 |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
6.701 |
the_geom |
MULTIPOLYGON (((-41.214704185534515 -5.147092559895959, -41.211499284149454 -5.150328694735429, -41.211183278570196 -5.151942182807383, -41.211510500494036 -5.153553378507583, -41.21280818353566 -5.156773473039135, -41.21636507507296 -5.1622427971890446, -41.21669231588243 -5.163853984795171, -41.218952659322625 -5.166425676225552, -41.22056301955248 -5.1670648612758425, -41.224422481697 -5.167051065675629, -41.22635447006756 -5.167689098694546, -41.226418747312096 -5.167370413135639, -41.235364426012296 -5.168946756508903, -41.23889660058245 -5.167321793987118, -41.24210599857776 -5.165375527979734, -41.24403458751097 -5.165046171065477, -41.24531423914565 -5.163106809153577, -41.2453017142876 -5.159559740911043, -41.24690866608696 -5.15923154052492, -41.248839514117094 -5.159547112630973, -41.250769223605616 -5.159540224723471, -41.25237502966871 -5.1588895670217045, -41.253645501023826 -5.154370551081891, -41.25492853321012 -5.1533985880963185, -41.25653546432507 -5.153070396703416, -41.258140103967506 -5.152097289780123, -41.25748771597016 -5.149519919130981, -41.255547741619786 -5.146624667816258, -41.25395441095217 -5.146568107654161, -41.25233733548452 -5.148248414454915, -41.25073612225912 -5.150188898720771, -41.249036898219174 -5.149810550338662, -41.24440355866215 -5.1487788867583895, -41.238833017614546 -5.149263910023543, -41.236825213697514 -5.148386656441137, -41.233802724501004 -5.147066055076532, -41.23078024789493 -5.145745447416822, -41.22627321811933 -5.1444716125970045, -41.224662937029734 -5.143832403265096, -41.221769559002794 -5.144165169509223, -41.21984323186447 -5.145139438356544, -41.21791356734202 -5.145146306479179, -41.215985012583026 -5.145475642708936, -41.214704185534515 -5.147092559895959), (-41.22684126050057 -5.148916130497144, -41.22998338291155 -5.149953868997985, -41.22998706113881 -5.151002786971145, -41.23208181870583 -5.151694608441325, -41.235915251772255 -5.150981661896132, -41.23870991301694 -5.152370269094646, -41.238717299148796 -5.15446809155106, -41.238026014573734 -5.156218764905957, -41.23977577241884 -5.157960729226073, -41.24013188416389 -5.160057304322806, -41.23909064280372 -5.161459587511742, -41.23909679866315 -5.163207771543093, -41.238755460980556 -5.165306839560602, -41.23666680081706 -5.166363229101183, -41.235799116021276 -5.164822539350222, -41.2324747298098 -5.164280354276489, -41.22829248839251 -5.164994584154316, -41.22815907036959 -5.163516453043535, -41.22514662480168 -5.162907955559407, -41.22199955971671 -5.160471676847992, -41.2227795183449 -5.158610194426666, -41.22354063347825 -5.15679367720827, -41.22462578064015 -5.1542037951909165, -41.22573352506701 -5.1515599610452485, -41.22684126050057 -5.148916130497144))) |
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_33f1 |
Folha |
SB24 |
Legenda_Completa |
367Da22 |
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 |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
12.168 |
the_geom |
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