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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_3824 |
Folha |
SC23 |
Legenda_Completa |
329Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
42.076 |
the_geom |
MULTIPOLYGON (((-47.86413818261494 -8.264066125231373, -47.8613512622052 -8.26232741422913, -47.8598527105767 -8.262099961546607, -47.859051963281864 -8.266600442839197, -47.85916248702222 -8.269074046275234, -47.860869054494394 -8.272916367389714, -47.86281873125659 -8.274713114567488, -47.865078214182866 -8.276028980924844, -47.86463321544204 -8.279196913842034, -47.869202679244744 -8.281063653736119, -47.87474463935019 -8.279943225949252, -47.87778017480345 -8.282252173504867, -47.88043693988995 -8.283576344701405, -47.884390313273194 -8.28483158927157, -47.88556914446533 -8.28553957436949, -47.88952915749493 -8.28650205686535, -47.89168518284351 -8.288011013480487, -47.89312991481159 -8.290188736821776, -47.893677033122714 -8.292444739508548, -47.893628784116615 -8.294589916436834, -47.89429276702644 -8.296067218187247, -47.89785050560272 -8.297215668262174, -47.89931729306565 -8.298416233989586, -47.89939902001586 -8.299200018031632, -47.89734594530065 -8.301984794260157, 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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_3825 |
Folha |
SC23 |
Legenda_Completa |
329Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
2.81 |
the_geom |
MULTIPOLYGON (((-47.781923934472005 -8.33942488105987, -47.7813315744194 -8.335124354188515, -47.78127340607795 -8.334691912874167, -47.7814620919148 -8.33400501383525, -47.78310260078314 -8.328049295560382, -47.782812664769594 -8.327654702939698, -47.781118643767925 -8.327714572477527, -47.78086392737608 -8.328071526084397, -47.77824155183348 -8.331750117093119, -47.77683420448175 -8.332305364996282, -47.776233002472765 -8.332486998830769, -47.77418326131131 -8.330687626080037, -47.77338791682246 -8.33067044554473, -47.77135435841903 -8.33257712201756, -47.7690760733283 -8.335805973698081, -47.76689012731046 -8.337855720899183, -47.766540504776664 -8.338618580077684, -47.76512282650169 -8.33966097017522, -47.7641279036353 -8.339640340505683, -47.761959665231615 -8.338714986143499, -47.76108910079331 -8.337526676832375, -47.76091739862902 -8.336351705619608, -47.75943760191673 -8.33573404290726, -47.75799706561539 -8.337849854425338, -47.75797557779342 -8.338824242996036, -47.758636673725604 -8.34039992919519, -47.760405471323914 -8.341413074105715, -47.76117128575919 -8.342796403376637, -47.76132153731073 -8.344944854851287, -47.76024005187949 -8.348928839489732, -47.762363267558236 -8.349094415130045, -47.76275078045924 -8.34780479667374, -47.764318609964945 -8.346876371947028, -47.76584427065391 -8.351428276265077, -47.769398835255025 -8.350039299302411, -47.76664010064491 -8.346139208527486, -47.771091373297814 -8.344277706749047, -47.771537409326946 -8.337990102247492, -47.77379912544258 -8.335483096914158, -47.77843781624784 -8.334304876160376, -47.7787451642897 -8.344736701358945, -47.77839547129728 -8.347068956848377, -47.777462741390174 -8.348708374890796, -47.77825368220999 -8.350685838389435, -47.7808380585834 -8.351203137549884, -47.783472441525284 -8.346444681957879, -47.78246727455462 -8.343376167644523, -47.781923934472005 -8.33942488105987))) |
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_3826 |
Folha |
SC23 |
Legenda_Completa |
323Aii |
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 |
Aii |
Categoria |
Plano inundável indiferenciado |
Natureza |
acumulação |
Caracteristica |
inundação |
Forma |
plano abaciado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
6.104 |
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)
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Bacias e Coberturas Sedimentares Fanerozóicas |
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323 |
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Area_Poligono_Km2 |
16.811 |
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_3828 |
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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 |
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aplanamento |
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degradado inumado |
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pediplano |
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|
Aprofundamento_Incisoes |
|
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|
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Area_Poligono_Km2 |
82.716 |
the_geom |
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