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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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_3869 |
Folha |
SC23 |
Legenda_Completa |
329Dc42 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
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 |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
45.592 |
the_geom |
MULTIPOLYGON (((-47.52542119196603 -10.436374084012618, -47.52284486956979 -10.435480039347935, -47.520924212025754 -10.437464477459955, -47.52003230661182 -10.437540855898279, -47.51768375037598 -10.436621540798113, -47.51642592264061 -10.435532253241364, -47.51593109365558 -10.435521228967495, -47.513511794238326 -10.437688763152165, -47.5104426335544 -10.438007958465997, -47.509323505434054 -10.439430994337748, -47.50838168103117 -10.44172766535931, -47.50842072911285 -10.444334025942279, -47.50963704974786 -10.447258017761367, -47.509501043543395 -10.448897222350636, -47.50890458819099 -10.453324102673964, -47.50779611972038 -10.454264402361554, -47.505721629747974 -10.454316138561062, -47.50484457846389 -10.453813610363072, -47.503789251849895 -10.452439202448932, -47.501528151609634 -10.45200289448276, -47.49997050001935 -10.451003977487881, -47.50001673397183 -10.448976940830343, -47.49847545441336 -10.447302058088924, -47.49680422992803 -10.446975122903737, -47.496526371789194 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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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_386a |
Folha |
SC23 |
Legenda_Completa |
329Dc42 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
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 |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
18.711 |
the_geom |
MULTIPOLYGON (((-47.58376215708814 -10.639192719607035, -47.581907429605415 -10.64276383773668, -47.582136151008484 -10.64565649519611, -47.583423037995345 -10.6475621065611, -47.586209555874724 -10.648489490230965, -47.586192309690276 -10.649211681225317, -47.586629660529404 -10.649509091412668, -47.58668340257719 -10.653553457358424, -47.58944333224179 -10.65563668566586, -47.596509315899475 -10.656802443602778, -47.597661747756774 -10.658126790578853, -47.59745419727639 -10.66072204123183, -47.59686344622357 -10.66070816590478, -47.59565182625068 -10.66198232741832, -47.592658485400456 -10.663649413791497, -47.58984954044678 -10.66373195337945, -47.588499814525555 -10.664570041076878, -47.58804020387855 -10.665281598814648, -47.58872357139955 -10.667752109044939, -47.593120505517405 -10.669293077178589, -47.59572634194025 -10.671659721656475, -47.598086088645196 -10.671855921256546, -47.59973760984124 -10.670736645354268, -47.602978716468655 -10.671096501425234, -47.60477082963988 -10.670268061573553, -47.60657662657659 -10.668864356078956, -47.60836525923857 -10.668181042532744, -47.614292850302924 -10.667443248000641, -47.61474894404855 -10.666876799225284, -47.61533975193108 -10.666888857267786, -47.61703733791406 -10.66374891988256, -47.61615915792727 -10.663295782432199, -47.61574579937129 -10.661986821818116, -47.6116934154975 -10.658287831723833, -47.61205076775721 -10.65555241151368, -47.614172872111936 -10.65328868478964, -47.614802951440254 -10.651569581442647, -47.61514406445525 -10.64955457968886, -47.61474009355242 -10.64781280638807, -47.61540792064405 -10.644505048016725, -47.61455126953254 -10.643188137419957, -47.61207588135327 -10.641544383588224, -47.611675352397015 -10.639659228086277, -47.61138047392466 -10.639651869832354, -47.61163062418811 -10.63518114203484, -47.61035048124249 -10.632986229142125, -47.60990814280316 -10.632976525354131, -47.608192534383235 -10.630484262918214, -47.60841619437771 -10.627167632954905, -47.60935393498203 -10.624877919414319, -47.60955445742465 -10.622572026470218, -47.60670381024002 -10.618032320400532, -47.602742128318695 -10.616790626663008, -47.600549992825556 -10.615732101596569, -47.59954109267651 -10.614698672726451, -47.59910119745786 -10.608046753504635, -47.59840847876607 -10.606009891074946, -47.597828162537354 -10.60556322664952, -47.59770389333923 -10.604549229655442, -47.595709063583485 -10.601329013725286, -47.59498380356967 -10.600736597261013, -47.591583949529245 -10.600806145669322, -47.59022860917321 -10.60193192680036, -47.588099138985704 -10.604629283287618, -47.58834508984642 -10.606801568546539, -47.58891854950791 -10.607534997164008, -47.589184260933855 -10.60884078839023, -47.58898105815935 -10.611290967679444, -47.58446468603561 -10.614946997167392, -47.58177953396889 -10.616043437584686, -47.58072332468632 -10.617031421015154, -47.58025433743239 -10.618176682474685, -47.57991207528885 -10.620191656427306, -47.579983898962055 -10.623513906636909, -47.58255559389997 -10.627325144602974, -47.58500407730609 -10.630121493515754, -47.585137719055695 -10.630702677271382, -47.58601138924696 -10.631299266511165, -47.58608669365152 -10.634479015395755, -47.585757349925395 -10.635915133070823, -47.58423207215576 -10.638048376226909, -47.58421232402641 -10.638913961845295, -47.58376215708814 -10.639192719607035))) |
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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_386b |
Folha |
SC23 |
Legenda_Completa |
329Dc42 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
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 |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
125.612 |
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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_386c |
Folha |
SC23 |
Legenda_Completa |
323Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
323 |
Nome_Unidade |
Chapadões do Alto ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
5.305 |
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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_386d |
Folha |
SC23 |
Legenda_Completa |
329Dc51 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
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 Médio Tocantins |
Area_Poligono_Km2 |
33.883 |
the_geom |
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