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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_4a4d |
Folha |
SD22 |
Legenda_Completa |
410Dt11 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
SuperfÃcie do Araguaia |
Identificacao_Unidade |
410 |
Nome_Unidade |
SuperfÃcie Central 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 Central do Médio Araguaia |
Area_Poligono_Km2 |
66.814 |
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_4a4e |
Folha |
SD22 |
Legenda_Completa |
443Pru |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
443 |
Nome_Unidade |
SuperfÃcie Oriental do Médio Araguaia |
Letra_Simbolo |
Pru |
Categoria |
Pediplano retocado desnudado |
Natureza |
aplanamento |
Caracteristica |
retocado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
SuperfÃcie Oriental do Médio Araguaia |
Area_Poligono_Km2 |
22.65 |
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_4a4f |
Folha |
SD22 |
Legenda_Completa |
444Dc52 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
444 |
Nome_Unidade |
Depressões Intermontanas das Altas Bacias dos Rios Crixás-Açú |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressões Intermontanas das Altas Bacias dos Rios Crixás-Açú |
Area_Poligono_Km2 |
7.012 |
the_geom |
MULTIPOLYGON (((-49.855922636742754 -14.053128314758164, -49.85630147736021 -14.05692492417308, -49.85699355647001 -14.058425630880881, -49.85757645580753 -14.059062016508982, -49.85803175591593 -14.06084814031241, -49.85800909507985 -14.063434517617903, -49.85775821594596 -14.065157278136873, -49.85715404413752 -14.066933200562463, -49.85667618260865 -14.067677182537247, -49.854896585767285 -14.069330223345204, -49.85412624659937 -14.069783685312022, -49.853280372443145 -14.072248506931876, -49.85283865317607 -14.075636076938082, -49.8533556120517 -14.077134811254693, -49.8540581201837 -14.077542785763821, -49.856527975050405 -14.077792235928, -49.85800360043111 -14.077402992270219, -49.859306336440895 -14.076493055462771, -49.86050257858383 -14.07437593847788, -49.8605090659167 -14.073685837626943, -49.861762236593485 -14.071627668498454, -49.862593280270254 -14.070885898561931, -49.863131382251 -14.070027703903731, -49.866093550555895 -14.067868015023661, -49.868704018877686 -14.065474861882908, -49.87059313643034 -14.064914644545413, -49.87536441161858 -14.064493425728923, -49.87701606037916 -14.064103405780205, -49.8779602602348 -14.063766111400678, -49.878673015131056 -14.063082162642557, -49.87851686934657 -14.060724135536418, -49.87658807281986 -14.059214901533107, -49.87447459818726 -14.058508050978821, -49.87153609237528 -14.05808147869721, -49.8677707470213 -14.05787973439603, -49.866841287765595 -14.056492145665176, -49.86598432979433 -14.053496703449984, -49.8636768866461 -14.048131859374614, -49.863170246472194 -14.04554126790722, -49.863199963807666 -14.035482209973011, -49.864181243038956 -14.030891727516705, -49.864893163337136 -14.023596658376292, -49.86473043463122 -14.02204388219452, -49.86444281250159 -14.021351630306809, -49.86368449348562 -14.020483793723253, -49.862745850176566 -14.020188060765438, -49.86127582972431 -14.020004146718666, -49.859097957632635 -14.020101507643057, -49.856968593690276 -14.021348832206364, -49.85649067695257 -14.022150854228622, -49.855780476227885 -14.022604425147257, -49.85439802709335 -14.025812320614422, -49.85401834548465 -14.028798255065764, -49.85392489049619 -14.039431337172926, -49.85448902666612 -14.042195224232682, -49.85489480990396 -14.04283137494195, -49.854947050625235 -14.04363586278771, -49.855927517096646 -14.045886000771539, -49.85638156487663 -14.047785539417424, -49.85654546427649 -14.049224903228652, -49.85612099306404 -14.050715361639684, -49.855922636742754 -14.053128314758164))) |
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_4a50 |
Folha |
SD22 |
Legenda_Completa |
444Dt21 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
444 |
Nome_Unidade |
Depressões Intermontanas das Altas Bacias dos Rios Crixás-Açú |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressões Intermontanas das Altas Bacias dos Rios Crixás-Açú |
Area_Poligono_Km2 |
94.695 |
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_4a51 |
Folha |
SD22 |
Legenda_Completa |
410Pri |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
SuperfÃcie do Araguaia |
Identificacao_Unidade |
410 |
Nome_Unidade |
SuperfÃcie Central do Médio Araguaia |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
SuperfÃcie Central do Médio Araguaia |
Area_Poligono_Km2 |
8.689 |
the_geom |
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