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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_-236f |
Folha |
SG22 |
Legenda_Completa |
383Apfm |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies Deltáicas, Estuarinas e Praiais |
Identificacao_Unidade |
383 |
Nome_Unidade |
PlanÃcies Litorâneas |
Letra_Simbolo |
Apfm |
Categoria |
PlanÃcie fluviomarinha |
Natureza |
acumulação |
Caracteristica |
fluviomarinho |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies Litorâneas |
Area_Poligono_Km2 |
0.249 |
the_geom |
MULTIPOLYGON (((-48.659379838802195 -25.864125784325918, -48.66109113264334 -25.864125784325918, -48.66280242738382 -25.863970957042493, -48.66371511799365 -25.86366130034808, -48.664000333342436 -25.863403251906984, -48.66514119620294 -25.86319681432991, -48.66599684267388 -25.86283554497284, -48.666282059063484 -25.862422666221573, -48.66702361899367 -25.86216461534814, -48.66799335290464 -25.86206139506585, -48.66827856799367 -25.861596902348104, -48.667308834993634 -25.86108079734818, -48.66639614499361 -25.86082274334813, -48.66514119620293 -25.860513079063768, -48.66325877306761 -25.860513079063768, -48.6625742549916 -25.860719522036707, -48.66234608199361 -25.861596902348165, -48.661547478993604 -25.862113005348167, -48.66023548617246 -25.862577496203006, -48.65818193399358 -25.86309359434813, -48.657155156993625 -25.863248423348164, -48.65715515699363 -25.863506471348096, -48.65829601993905 -25.863970957042493, -48.659379838802195 -25.864125784325918))) |
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_-236e |
Folha |
SG22 |
Legenda_Completa |
383Apfm |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies Deltáicas, Estuarinas e Praiais |
Identificacao_Unidade |
383 |
Nome_Unidade |
PlanÃcies Litorâneas |
Letra_Simbolo |
Apfm |
Categoria |
PlanÃcie fluviomarinha |
Natureza |
acumulação |
Caracteristica |
fluviomarinho |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies Litorâneas |
Area_Poligono_Km2 |
0.114 |
the_geom |
MULTIPOLYGON (((-48.64607097239117 -25.864068937280127, -48.65088398699362 -25.864149576348076, -48.65159702577582 -25.86377325817777, -48.65088398699362 -25.863128138348102, -48.649992687993674 -25.862724937348236, -48.64922022912397 -25.862536774900658, -48.648596319993594 -25.86245613534807, -48.64788327999357 -25.8623217343481, -48.64633836199366 -25.86229485334813, -48.64559561299366 -25.86229485334813, -48.64506083399364 -25.86267117634811, -48.645090544087005 -25.863047498091987, -48.645417353221944 -25.863477579075514, -48.64571445325311 -25.86374637834108, -48.64607097239117 -25.864068937280127))) |
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_-236d |
Folha |
SG22 |
Legenda_Completa |
675Dc33 |
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 |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Patamar de Ponta Grossa - Itapetininga |
Area_Poligono_Km2 |
180.111 |
the_geom |
MULTIPOLYGON (((-50.80233817822964 -25.865081563069353, -50.8014865754631 -25.864618257790664, -50.801061749212714 -25.864387135661843, -50.8003851315041 -25.86280836100845, -50.80038513150409 -25.86077850788259, -50.80015959226789 -25.86010189017398, -50.799934053031684 -25.859425272465444, -50.79858081761444 -25.858748654756763, -50.79835527837825 -25.85694434086712, -50.798806356850655 -25.85468894850507, -50.79993405303169 -25.853561252324, -50.80173836692133 -25.85040370301713, -50.80173836692133 -25.846569536001777, -50.79880635685066 -25.84544183982063, -50.797002042961026 -25.84544183982068, -50.795197729071376 -25.847246153710266, -50.79361895441792 -25.848373849891335, -50.79204017976449 -25.848599389127518, -50.790686944347264 -25.848373849891335, -50.78933370893003 -25.846343996765516, -50.787754934276585 -25.84544183982068, -50.785274002678335 -25.8449907613482, -50.780312139481815 -25.844990761348296, -50.77895890406458 -25.84363752593101, -50.780988757190435 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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_-236c |
Folha |
SG22 |
Legenda_Completa |
383Apfm |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies Deltáicas, Estuarinas e Praiais |
Identificacao_Unidade |
383 |
Nome_Unidade |
PlanÃcies Litorâneas |
Letra_Simbolo |
Apfm |
Categoria |
PlanÃcie fluviomarinha |
Natureza |
acumulação |
Caracteristica |
fluviomarinho |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies Litorâneas |
Area_Poligono_Km2 |
0.238 |
the_geom |
MULTIPOLYGON (((-48.63325408370268 -25.86799641694953, -48.63102940099358 -25.868048024348067, -48.62851950386566 -25.8687705281858, -48.62800611499364 -25.869183385348055, -48.62914697794433 -25.869854275103044, -48.63085827178548 -25.87073158714145, -48.63251252342791 -25.87114443711448, -48.633824514683276 -25.87114443711455, -48.634851291993634 -25.871041224348108, -48.63582102491404 -25.870783192938394, -48.6367907579936 -25.87031873534818, -48.637018930872664 -25.869647848318, -48.636562586088125 -25.869234992049744, -48.635307637031524 -25.86877052818568, -48.63325408370268 -25.86799641694953))) |
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_-236b |
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 |
5.597 |
the_geom |
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