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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_2a24 |
Folha |
SB24 |
Legenda_Completa |
650Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do Litoral Norte |
Identificacao_Unidade |
650 |
Nome_Unidade |
SuperfÃcie Rebaixada do Vale do Rio Açu |
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 |
SuperfÃcie Rebaixada do Vale do Rio Açu |
Area_Poligono_Km2 |
60.015 |
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_2a25 |
Folha |
SB24 |
Legenda_Completa |
395Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto da Ibiapaba |
Identificacao_Unidade |
395 |
Nome_Unidade |
Serras Grande e da Ibiapaba |
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 |
Serras Grande e da Ibiapaba |
Area_Poligono_Km2 |
2.374 |
the_geom |
MULTIPOLYGON (((-41.21237636416269 -5.80000117831214, -41.21397868355422 -5.802229252278543, -41.21470112334296 -5.801050465007453, -41.21561928708525 -5.799552314987817, -41.219174074208915 -5.797378393698595, -41.218527881641236 -5.79514648772087, -41.21915026915443 -5.791313421577883, -41.21850533473823 -5.789400721866595, -41.21881652624646 -5.78748419014408, -41.22007505910152 -5.783329368156843, -41.22102497071061 -5.781729494022039, -41.22261375170807 -5.778885817027989, -41.221967435033896 -5.778214366101381, -41.221951306592395 -5.774064647766662, -41.22279697868243 -5.771933331859244, -41.221962852988085 -5.770107384349696, -41.221292822090895 -5.768640637756644, -41.222872651236706 -5.76512297644573, -41.22335002576791 -5.764662602698577, -41.22052581549885 -5.764854907429766, -41.21829990889847 -5.7661406492730265, -41.21767737839308 -5.7699737145168495, -41.215777566866 -5.773173456491246, -41.21514758997407 -5.7750912679489925, -41.214836310332245 -5.777007806866054, -41.214843729739194 -5.778923071443703, -41.21612472586024 -5.780514023404619, -41.21708702473123 -5.782106249704816, -41.215819664130976 -5.784026613438437, -41.21423363955562 -5.7859482542095195, -41.21328377021469 -5.787548135538797, -41.21297505903652 -5.790103095981899, -41.21299130169199 -5.794252831403709, -41.21236262432049 -5.796489861718361, -41.21205140583249 -5.798406405132047, -41.21237636416269 -5.80000117831214))) |
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_2a3c |
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 |
2.761 |
the_geom |
MULTIPOLYGON (((-41.95940344320007 -6.277255221935578, -41.96100651892136 -6.27884126809466, -41.96260600454916 -6.279789278536949, -41.9642108995991 -6.281694330413575, -41.96485754542506 -6.283285786894108, -41.966457050838 -6.284233788343071, -41.96805295626467 -6.284543759471405, -41.970290113383776 -6.285488138451152, -41.97125560394869 -6.287077774703885, -41.97062698413372 -6.288676456337662, -41.9722265174256 -6.289624444296891, -41.97414857907943 -6.291208638751832, -41.97384070876739 -6.293124514868477, -41.97480814276722 -6.295033145147582, -41.97639862258405 -6.294386066747678, -41.98054336766803 -6.294362517999884, -41.98086585376184 -6.294998723596334, -41.98279163321301 -6.297220912399111, -41.983739875680484 -6.295779939476792, -41.98468811365122 -6.29433896835288, -41.98276599893749 -6.292754795481583, -41.982740448298784 -6.2882886758659025, -41.98272957459587 -6.2863746208763995, -41.98025168515291 -6.285362084077211, -41.97984570150364 -6.283466189997067, -41.9795160118402 -6.281926570439308, -41.976888640683946 -6.280689864130409, -41.97631154572701 -6.279073550388629, -41.971896149673334 -6.277970325055134, -41.971073305074725 -6.276516356929066, -41.97055297982186 -6.275596935934576, -41.968967923816315 -6.27720103148709, -41.9665169169079 -6.278645668247588, -41.96519342512212 -6.277134969088211, -41.96398640633331 -6.275757207713667, -41.962461761386905 -6.274016872964977, -41.96219706707669 -6.273714730884931, -41.96193237276645 -6.273412588804631, -41.96002308778093 -6.274061451459606, -41.95907563581755 -6.275661947925134, -41.95940344320007 -6.277255221935578))) |
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_2a3d |
Folha |
SB24 |
Legenda_Completa |
395Dt32 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto da Ibiapaba |
Identificacao_Unidade |
395 |
Nome_Unidade |
Serras Grande e da Ibiapaba |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serras Grande e da Ibiapaba |
Area_Poligono_Km2 |
71.586 |
the_geom |
MULTIPOLYGON (((-40.95514595480637 -4.797455956860757, -40.95400518907266 -4.798894744430703, -40.954296304115616 -4.8006166160976, -40.955004144310315 -4.800685158826679, -40.955456689459176 -4.80606853207055, -40.95603729806728 -4.808938043889099, -40.95661545782168 -4.810946216528133, -40.957197711289886 -4.8143899490701605, -40.95806373593719 -4.8169715339423105, -40.95835404878489 -4.818406286254275, -40.95807273815076 -4.820129769506365, -40.95607000281288 -4.820422548295058, -40.954922663934326 -4.819564448473604, -40.9546307233137 -4.8175554682435004, -40.95233197972166 -4.814403695207735, -40.9514684273105 -4.812683440521731, -40.94974622469306 -4.8109656086093375, -40.948025659740935 -4.809822001017993, -40.9460196958368 -4.808966312278885, -40.94258265425057 -4.808114659697257, -40.9359940024058 -4.80612342039304, -40.933706699089434 -4.806991226597386, -40.93313911536241 -4.80871553992372, -40.93170881559377 -4.809006640577511, -40.92999300445799 -4.809585420863919, 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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_2a3e |
Folha |
SB24 |
Legenda_Completa |
000Magua |
Nome_Dominio |
|
Nome_Regiao |
|
Identificacao_Unidade |
0 |
Nome_Unidade |
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Letra_Simbolo |
|
Categoria |
|
Natureza |
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Caracteristica |
|
Forma |
|
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
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Nivel_Altimetrico |
|
Legenda |
Corpo d´água continental |
Area_Poligono_Km2 |
0.063 |
the_geom |
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