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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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-22d0 |
Folha |
SG22 |
Legenda_Completa |
676Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Escarpas e Reversos da Serra do Mar |
Identificacao_Unidade |
676 |
Nome_Unidade |
Serra do Mar |
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 |
Serra do Mar |
Area_Poligono_Km2 |
5.509 |
the_geom |
MULTIPOLYGON (((-48.70757833332711 -25.956210278125393, -48.70658277777154 -25.955960278125517, -48.70541499999375 -25.956074167014464, -48.70462138888265 -25.95690083368113, -48.70421065009183 -25.95882690200859, -48.703574704993706 -25.959624691347695, -48.70144027777153 -25.95984722257004, -48.70057904120391 -25.95934285756317, -48.70073559093854 -25.960238929689282, -48.70073559093855 -25.96182641863082, -48.700663432350304 -25.96341390757251, -48.701096383879836 -25.965795140984852, -48.70073559093855 -25.966877519808648, -48.69979752929123 -25.967382629926465, -48.69878730905565 -25.96817637439731, -48.69806572317309 -25.969330911809347, -48.69719982011403 -25.970124656280195, -48.69647823423146 -25.970557607809802, -48.69604528270193 -25.97041329063323, -48.69503506246634 -25.97041329063323, -48.69373620787774 -25.971567828045433, -48.693086780583435 -25.972000779575005, -48.6926538290539 -25.97207293816311, -48.69214871893612 -25.97207293816318, -48.691499291641804 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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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-22cf |
Folha |
SG22 |
Legenda_Completa |
675Dc32 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Patamar Oriental da Bacia do Paraná |
Identificacao_Unidade |
675 |
Nome_Unidade |
Patamar de Ponta Grossa - Itapetininga |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamar de Ponta Grossa - Itapetininga |
Area_Poligono_Km2 |
25.474 |
the_geom |
MULTIPOLYGON (((-49.67003372099483 -25.92124253334787, -49.67024944443934 -25.920415278125652, -49.67032916666157 -25.919735278125685, -49.6701774999949 -25.91917694479231, -49.66977027777267 -25.918693889236803, -49.669163333328235 -25.918168333681255, -49.66873166666156 -25.917840278125702, -49.66813555555045 -25.91701527812572, -49.66786916666156 -25.91657000034795, -49.667794166661565 -25.916056111459007, -49.66816194443934 -25.915147222570145, -49.66904333332822 -25.914163333681255, -49.67005444443934 -25.913241389236816, -49.6705613888838 -25.91284472257018, -49.67080972221712 -25.91238888923683, -49.670797777772684 -25.911809722570354, -49.670316111106004 -25.91027388923696, -49.67017694443934 -25.9097616670146, -49.669910555550445 -25.909316389236885, -49.668871666661566 -25.908886667014695, -49.666039444439335 -25.908879722570234, -49.66501388888378 -25.909093611458996, -49.66443861110601 -25.909298611459192, -49.66379527777266 -25.909311667014634, -49.66327777777266 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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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-22ce |
Folha |
SG22 |
Legenda_Completa |
385Atf1 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Região não identificada - domÃnio 1 |
Identificacao_Unidade |
385 |
Nome_Unidade |
PlanÃcies Alúvio-coluvionares |
Letra_Simbolo |
Atf |
Categoria |
Terraço fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
PlanÃcies Alúvio-coluvionares |
Area_Poligono_Km2 |
5.889 |
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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-22cd |
Folha |
SG22 |
Legenda_Completa |
385Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Região não identificada - domÃnio 1 |
Identificacao_Unidade |
385 |
Nome_Unidade |
PlanÃcies Alúvio-coluvionares |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies Alúvio-coluvionares |
Area_Poligono_Km2 |
0.516 |
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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-22cc |
Folha |
SG22 |
Legenda_Completa |
685Da34 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto das Araucárias |
Identificacao_Unidade |
685 |
Nome_Unidade |
Planalto Dissecado Rio Iguaçu |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
forte : > 150 a 200m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado Rio Iguaçu |
Area_Poligono_Km2 |
73.96 |
the_geom |
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