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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 SH.21 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, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-eac |
Folha |
SH21 |
Legenda_Completa |
388Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
19.035 |
the_geom |
MULTIPOLYGON (((-55.065881474948895 -30.018091456741963, -55.06635694523515 -30.017140224541166, -55.0668710450781 -30.016112072905507, -55.067898927847075 -30.014226212736702, -55.069779795146104 -30.011899081714116, -55.07046432857144 -30.011041703835833, -55.07097840036552 -30.010013583166117, -55.07200652803884 -30.007956422049492, -55.07217786561073 -30.00589955426602, -55.07217774430225 -30.003671040870525, -55.072177622995845 -30.001442557586522, -55.07217741132725 -30.00041353337923, -55.071663534449755 -29.99732834326308, -55.07166311897908 -29.995271288869397, -55.071664000556964 -29.99304291545283, -55.07166379473487 -29.99201487989122, -55.072006074731746 -29.990985620352077, -55.073033441889905 -29.990471659710877, -55.07364689295147 -29.989584680840935, -55.07423262746657 -29.988757725847552, -55.07423248487751 -29.98652850771474, -55.07423326747484 -29.985500509126, -55.07354786845471 -29.983443258842488, -55.07303343643172 -29.982415260411706, -55.071320828225744 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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 SH.21 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, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-eab |
Folha |
SH21 |
Legenda_Completa |
389Pgu |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
389 |
Nome_Unidade |
Planalto da Campanha |
Letra_Simbolo |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto da Campanha |
Area_Poligono_Km2 |
2.24 |
the_geom |
MULTIPOLYGON (((-55.1503305492982 -29.61249843800117, -55.14987701372374 -29.61184721101253, -55.14963489566397 -29.61074958350026, -55.1485164082427 -29.609890738556896, -55.14740683765212 -29.609472772756398, -55.14410485071454 -29.60953962288383, -55.14300419074355 -29.609562520900713, -55.13949570879626 -29.610294285395366, -55.138179654592754 -29.610541248155883, -55.13666993579319 -29.612114501807216, -55.136032652443156 -29.613229507902837, -55.13583404067396 -29.61433537828669, -55.134773848227525 -29.616340404768764, -55.13413160426883 -29.617234986312933, -55.13393397852537 -29.61834087780162, -55.13461177083449 -29.61920803442611, -55.13572630588221 -29.6198465232121, -55.1373299363337 -29.62289994030929, -55.13890591971102 -29.624630644694225, -55.13980014359481 -29.62527371600836, -55.1419966509016 -29.625008411185064, -55.143092429952524 -29.62476599101792, -55.14461998958094 -29.62407348614812, -55.14548651623181 -29.623395657730562, -55.146583278326155 -29.623152289038266, -55.14854159879374 -29.622010629727168, -55.14962844968529 -29.621328213102768, -55.150720247095954 -29.620865313579078, -55.15158774034945 -29.620186542276457, -55.15200563226499 -29.619076040271338, -55.15220318231328 -29.61797013202278, -55.15193826505463 -29.61577209384872, -55.15169613473705 -29.61467444257323, -55.1503305492982 -29.61249843800117))) |
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 SH.21 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, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-eaa |
Folha |
SH21 |
Legenda_Completa |
388Dc51 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
25.224 |
the_geom |
MULTIPOLYGON (((-55.037749487856956 -29.965111313369835, -55.03488132119703 -29.964930305829405, -55.03380511735342 -29.964952759114794, -55.03273396472078 -29.965243858886318, -55.031942469090225 -29.966068517781228, -55.030085852117104 -29.967452922900797, -55.02929434149521 -29.968277585789256, -55.028508875132516 -29.969371840528908, -55.027717353762284 -29.970196508806243, -55.02665726560239 -29.971025847952653, -55.02532256934257 -29.971592133513944, -55.0220928670845 -29.97165751213268, -55.019433522150635 -29.973328305892338, -55.018642958746746 -29.974152966425628, -55.017857430355384 -29.975247232022, -55.01734045557386 -29.97633497006835, -55.01606008045567 -29.979595428074155, -55.01396089060684 -29.98233257092227, -55.0131702828592 -29.983157261901173, -55.011022751216586 -29.983470693272626, -55.00994546718608 -29.983492130175005, -55.00777581283727 -29.982727079635662, -55.00668848147571 -29.9822111466306, -55.00424425334029 -29.981182053488492, -55.00150337174736 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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 SH.21 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, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea9 |
Folha |
SH21 |
Legenda_Completa |
388Dc41 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
63.722 |
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 SH.21 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, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea8 |
Folha |
SH21 |
Legenda_Completa |
388Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
15.833 |
the_geom |
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