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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_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 |
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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 |
|
Letra_Simbolo |
|
Categoria |
|
Natureza |
|
Caracteristica |
|
Forma |
|
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Corpo d´água continental |
Area_Poligono_Km2 |
0.063 |
the_geom |
MULTIPOLYGON (((-38.98499107426091 -4.618474959791289, -38.9848155976439 -4.618535994980059, -38.984621048204986 -4.618494034411989, -38.98446273784726 -4.618379592983661, -38.984434127714906 -4.6182994840737415, -38.984346389856206 -4.618223190087972, -38.9842720033324 -4.618041991984205, -38.983999252445734 -4.617919921606909, -38.983774185412486 -4.6182994840737415, -38.983999252445685 -4.618541718265639, -38.98418998696049 -4.618652343870326, -38.98427200333241 -4.618824004663847, -38.98439979609585 -4.61898612994567, -38.98446273784722 -4.619113921809853, -38.984506606776655 -4.619386672696593, -38.984466552771316 -4.619657516121194, -38.98448944141671 -4.6197128298229995, -38.984613419256014 -4.619859695408281, -38.98481559764394 -4.619922638059156, -38.985227585167145 -4.6199436192423695, -38.98563194284204 -4.619964600425797, -38.98587799105855 -4.619905471799883, -38.98620796220986 -4.619419097752932, -38.98644638147747 -4.619277953654421, -38.986551284696205 -4.619281769478023, -38.98726272577632 -4.619632720913049, -38.98753356920099 -4.619525909333056, -38.987806320087714 -4.619512557998028, -38.9880561832284 -4.619657516121194, -38.98834991529851 -4.619728087720783, -38.98862075782389 -4.619657516121068, -38.98866844167743 -4.6194820404035495, -38.988695145246915 -4.6193866726965, -38.98807716441176 -4.618953704889437, -38.98780632008778 -4.618865967030679, -38.98726272577635 -4.618865967030584, -38.986719131464874 -4.618986129945764, -38.98660087601178 -4.618843079284524, -38.98653984082319 -4.618570328397821, -38.986581802290566 -4.6182994840737415, -38.98675727800816 -4.61802673318702, -38.986719131464895 -4.61787796013962, -38.98665428225155 -4.617818832413053, -38.98644638147747 -4.617807387640686, -38.986175537153514 -4.617843627621214, -38.98563194284204 -4.617937087866107, -38.98535919195532 -4.61802673318699, -38.98499107426091 -4.618474959791289))) |
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_2a3f |
Folha |
SB24 |
Legenda_Completa |
393Dt32 |
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 |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
55.269 |
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_2a40 |
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 |
35.857 |
the_geom |
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