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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_-2c19 |
Folha |
SG22 |
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 |
0.083 |
the_geom |
MULTIPOLYGON (((-48.49189249999351 -27.769847500338877, -48.49124777777129 -27.769942500338875, -48.49084472221573 -27.770156389227843, -48.490576111104616 -27.770560555894463, -48.490683611104615 -27.77086944478341, -48.49071055554907 -27.77127361144994, -48.49057611110461 -27.771891667005637, -48.49060305554907 -27.772604722561006, -48.49081777777129 -27.773175000338853, -48.49105972221573 -27.773698055894563, -48.49148944443796 -27.77407833367233, -48.49186555554907 -27.774506111450012, -48.49251027777129 -27.774743889227597, -48.49253722221573 -27.774078333672193, -48.4924027777713 -27.773579167005497, -48.49232222221574 -27.772961111449963, -48.49232222221573 -27.772248055894448, -48.49232222221573 -27.771653889227608, -48.49232222221573 -27.771154722561022, -48.492188055549086 -27.770940833672135, -48.49202666666019 -27.77051305589441, -48.492134166660186 -27.770275278116706, -48.49189249999351 -27.769847500338877))) |
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_-2c18 |
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 |
0.379 |
the_geom |
MULTIPOLYGON (((-48.41984527149338 -25.410739996350117, -48.42058762488555 -25.41077401998503, -48.42173270132838 -25.410288676834266, -48.4228777777712 -25.409803333683623, -48.423928055548984 -25.40978194479465, -48.424981666660095 -25.409910833683462, -48.42603194443789 -25.409889444794675, -48.42737333332676 -25.409411667016876, -48.42781902777121 -25.409177361461246, -48.428264722215644 -25.40894305590581, -48.42839333332678 -25.407889167016823, -48.42838263888233 -25.407363889239164, -48.42837194443789 -25.406838611461332, -48.42730944443789 -25.406259444794703, -48.42625305554899 -25.405980555905852, -48.42520249999343 -25.406001667016877, -48.424681944437886 -25.406237500350198, -48.42435379415731 -25.406386166085714, -48.424257591519805 -25.40642974988464, -48.42416138888231 -25.406473333683618, -48.42389874999343 -25.406478680905916, -48.42363611110455 -25.406484028127995, -48.42301575273952 -25.406565464438305, -48.421431783493375 -25.4067733968502, -48.421164394414724 -25.40712958761095, -48.42034439886836 -25.40755053777762, -48.41938179602649 -25.407841963086558, -48.41916788418394 -25.407971485695953, -48.41895397199335 -25.408101008350112, -48.418953971993346 -25.408441003850182, -48.41895397199335 -25.408780999350093, -48.4190252759933 -25.409493366350183, -48.41948875199336 -25.410140968350127, -48.41984527149338 -25.410739996350117))) |
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_-2c17 |
Folha |
SG22 |
Legenda_Completa |
676Dc42 |
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 |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serra do Mar |
Area_Poligono_Km2 |
27.908 |
the_geom |
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-48.81309642302343 -25.393353269207022, -48.813487431310534 -25.39218024434571, -48.81485596031543 -25.38963869047942, -48.81524696860252 -25.388270161474605, -48.81563797688965 -25.38690163246969, -48.814874207368824 -25.384883378027716))) |
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_-2c16 |
Folha |
SG22 |
Legenda_Completa |
449Dc41 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
449 |
Nome_Unidade |
Planalto dos Campos Gerais |
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 |
Planalto dos Campos Gerais |
Area_Poligono_Km2 |
38.721 |
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_-2c15 |
Folha |
SG22 |
Legenda_Completa |
385Aptf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Região não identificada - domÃnio 1 |
Identificacao_Unidade |
385 |
Nome_Unidade |
PlanÃcies Alúvio-coluvionares |
Letra_Simbolo |
Aptf |
Categoria |
PlanÃcie e terraço fluviais |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie e terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies Alúvio-coluvionares |
Area_Poligono_Km2 |
68.225 |
the_geom |
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