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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 SD.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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4ad1 |
Folha |
SD22 |
Legenda_Completa |
446Dt11 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Depressões Interplanálticas das Altas Bacias do Tocantins |
Identificacao_Unidade |
446 |
Nome_Unidade |
Depressão Intermontana do Rio Preto |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão Intermontana do Rio Preto |
Area_Poligono_Km2 |
8.549 |
the_geom |
MULTIPOLYGON (((-48.04219359825423 -14.1572926826175, -48.04189092284891 -14.156033387314219, -48.040289837742925 -14.153176690140205, -48.03887917966466 -14.152267838012998, -48.03840446748546 -14.151411657968177, -48.03664686064534 -14.151134853823546, -48.033371529531 -14.15121205783534, -48.03015762510667 -14.151861369398725, -48.026247640095775 -14.153087894340187, -48.02158410495519 -14.155351041494503, -48.01953977047933 -14.155764730908206, -48.01790550811299 -14.156404357362765, -48.01756033063201 -14.157038191431495, -48.015176090994125 -14.159171823170984, -48.01343679390463 -14.161131523010573, -48.00996011230439 -14.165737716071913, -48.00880613588293 -14.16792219043315, -48.008703103301166 -14.169756763089934, -48.009059526743386 -14.17044313466869, -48.00913568006079 -14.172792830069827, -48.008503753479154 -14.174286961082766, -48.00686642855686 -14.174582613574636, -48.004350470484574 -14.174541011005513, -48.0010093055351 -14.173642800682995, -48.00044014623891 -14.173311948872877, -48.00043980322255 -14.198729021461792, -48.004402645344086 -14.199073785327316, -48.00558564002983 -14.198951245459208, -48.00628348079732 -14.198316934837393, -48.008135197502874 -14.195611606891084, -48.008130036401454 -14.194866668596719, -48.00951278103888 -14.191993775285333, -48.009507639550954 -14.191247957411768, -48.00996814227319 -14.190270382256038, -48.01085812173386 -14.184017941757613, -48.01195148786723 -14.18154625041573, -48.013455522407156 -14.17924512521481, -48.01427147276708 -14.178781524116983, -48.01601249068693 -14.176937063145902, -48.01635764332145 -14.176132637211246, -48.01769339603844 -14.174749106235398, -48.01815446289466 -14.173886722915555, -48.02176419228762 -14.17140106161364, -48.02660570154833 -14.16953780077773, -48.02951661644423 -14.167514020396897, -48.03027631463013 -14.167395519598681, -48.03074060178978 -14.166933299329433, -48.03237526468544 -14.166523115167434, -48.03418424266832 -14.165767015199393, -48.03458810362793 -14.165076497070942, -48.03563835768908 -14.16461127859887, -48.037349965743275 -14.163028912298644, -48.03900778619503 -14.161496279060895, -48.039875462222426 -14.160115749178006, -48.04121262316504 -14.159018799975783, -48.04219359825423 -14.1572926826175))) |
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 SD.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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4ad2 |
Folha |
SD22 |
Legenda_Completa |
421Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
47.978 |
the_geom |
MULTIPOLYGON (((-48.33455228186506 -14.217404341493225, -48.3322626077013 -14.21656116261515, -48.331494028599906 -14.215706953465695, -48.33106859550065 -14.214046120815032, -48.33065387507069 -14.21336157472454, -48.329647459647354 -14.212165286639758, -48.32823345493469 -14.211142822885607, -48.327109602449276 -14.209774200053594, -48.3249249145582 -14.207725973304097, -48.32409242548837 -14.206184440374697, -48.32302878862539 -14.205102039439387, -48.32272860679965 -14.204302199296931, -48.32001597339298 -14.201969571327739, -48.31965890190349 -14.201341686162381, -48.31689301895055 -14.19969898702014, -48.31431885146641 -14.19983238232819, -48.31233564431608 -14.200648111398582, -48.312543614068154 -14.204201723321152, -48.31302271583077 -14.205517337876163, -48.314386299012604 -14.207514818510743, -48.316808966968715 -14.210077575002549, -48.31769848586678 -14.211331983451135, -48.318018216931236 -14.2143692674509, -48.31785811935239 -14.216262401596008, -48.31751497282697 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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 SD.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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4ad3 |
Folha |
SD22 |
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 |
0.193 |
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 SD.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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4ad4 |
Folha |
SD22 |
Legenda_Completa |
443Dt11 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
443 |
Nome_Unidade |
SuperfÃcie Oriental do Médio Araguaia |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
SuperfÃcie Oriental do Médio Araguaia |
Area_Poligono_Km2 |
47.797 |
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 SD.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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4ad5 |
Folha |
SD22 |
Legenda_Completa |
341Dc41 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Depressões Interplanálticas das Altas Bacias do Tocantins |
Identificacao_Unidade |
341 |
Nome_Unidade |
Depressão do Alto Tocantins |
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 Alto Tocantins |
Area_Poligono_Km2 |
20.335 |
the_geom |
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