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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_-1182 |
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 |
32.485 |
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_-1181 |
Folha |
SH21 |
Legenda_Completa |
388Dc11 |
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 |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
10.517 |
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_-1180 |
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 |
34.936 |
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_-117f |
Folha |
SH21 |
Legenda_Completa |
389Dt31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
389 |
Nome_Unidade |
Planalto da Campanha |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto da Campanha |
Area_Poligono_Km2 |
9.512 |
the_geom |
MULTIPOLYGON (((-55.53298309381299 -30.360745947390946, -55.530835362042026 -30.35956615258467, -55.530196311870675 -30.358348581962737, -55.52986320583522 -30.357124757314345, -55.52922995292991 -30.356214022966725, -55.52832071872862 -30.35684740095057, -55.52772421470701 -30.357783213489764, -55.526814971438654 -30.358416593052585, -55.52532178162624 -30.360601320554608, -55.523189536004914 -30.361567521847444, -55.52165281880288 -30.36159883036696, -55.51854748958686 -30.36012353885947, -55.51761310661676 -30.35952678309149, -55.51667295568763 -30.358623201288076, -55.51510437634836 -30.357115680836174, -55.51447118007604 -30.356205853539972, -55.51353682031418 -30.355609099512424, -55.51290263322923 -30.35469928247148, -55.51196251039479 -30.353794774559002, -55.510393992348654 -30.352288212840744, -55.509262375638265 -30.35250882784481, -55.5090749630272 -30.352433769749247, -55.506434231035804 -30.352433989192953, -55.5053033457839 -30.352434071751254, -55.503040054978044 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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_-117e |
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 |
5.327 |
the_geom |
MULTIPOLYGON (((-55.37499567063148 -30.286390163646935, -55.37479204443777 -30.28396646738603, -55.37415017836626 -30.282801674956463, -55.37361503664799 -30.28178177908444, -55.37000741992224 -30.281597658050075, -55.36897891186094 -30.281618327282274, -55.367938723785755 -30.281124116818926, -55.367146737595974 -30.280110088003234, -55.366359098896545 -30.279353973936878, -55.36300405375633 -30.278905993808845, -55.36197456096427 -30.278927581009675, -55.36095139838131 -30.27920612797304, -55.35993256383113 -30.279741645208734, -55.35790554764683 -30.281328492573945, -55.35688769824897 -30.281864001873338, -55.35560564049052 -30.282147465366474, -55.35457180453681 -30.281911112296, -55.35377886801056 -30.28089704758398, -55.35299126062276 -30.28013995661724, -55.35195210810393 -30.279645690359363, -55.35116451456745 -30.278889538323703, -55.349862175366866 -30.278143222032508, -55.34857048565811 -30.277911773067867, -55.34754731281205 -30.27819027228563, -55.346790647721555 -30.278977796206814, -55.34630249239006 -30.28027528317426, -55.346065894708914 -30.281310896461648, -55.345577731456075 -30.282608400943268, -55.344564171969836 -30.283401789658537, -55.34354528770386 -30.283937264775517, -55.34151382778401 -30.285267059107962, -55.33817899865728 -30.28584951420894, -55.33509242166345 -30.285912125926828, -55.33380601586354 -30.285938518858266, -55.33251430195491 -30.285706989184984, -55.331475165958594 -30.285212634557794, -55.32941182039404 -30.284997668911235, -55.32710119188622 -30.285301544982072, -55.3260822693629 -30.28583790465185, -55.32355711947453 -30.28820625184046, -55.322800358263095 -30.288994701573912, -55.32256465963297 -30.29003034757346, -55.3225848432489 -30.291060175033472, -55.32286391105157 -30.292084170485314, -55.323655762284176 -30.293098391965806, -55.325472878353324 -30.29383416147103, -55.328559550792676 -30.293771646276337, -55.33164722141095 -30.293709094685248, -55.332676779427146 -30.29368854822847, -55.33370002846195 -30.29341007337233, -55.337301469682 -30.293336722537727, -55.33935526702635 -30.293037658492008, -55.34037850643873 -30.29275916183568, -55.34268918521889 -30.292455168856137, -55.34397030762611 -30.292171747355248, -55.347056956104616 -30.292109041303643, -55.35065937538016 -30.292035525188354, -55.35194580936247 -30.292009058543762, -55.353236571775774 -30.292240517584023, -55.356582107057605 -30.292172785712538, -55.357610657449165 -30.292152157898474, -55.35964742370966 -30.291080122028934, -55.36271905208702 -30.290245352985295, -55.36633212372005 -30.29068749603437, -55.36942408871028 -30.2908815453195, -55.37251172046522 -30.290819509625486, -55.37354026430071 -30.290798827030823, -55.37482134530646 -30.290515275869677, -55.37529433340197 -30.28844483025815, -55.37499567063148 -30.286390163646935))) |
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