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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 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.
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FID |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4e4b |
Folha |
SD22 |
Legenda_Completa |
439Dc52 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
439 |
Nome_Unidade |
SuperfÃcies Intermontanas do Alto Maranhão |
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 |
SuperfÃcies Intermontanas do Alto Maranhão |
Area_Poligono_Km2 |
68.654 |
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_4e4c |
Folha |
SD22 |
Legenda_Completa |
298Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
298 |
Nome_Unidade |
Chapada dos Guimarães |
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 |
Chapada dos Guimarães |
Area_Poligono_Km2 |
6.459 |
the_geom |
MULTIPOLYGON (((-52.37946203963119 -15.811048550491364, -52.376002379083204 -15.810034301772008, -52.37124068649827 -15.808104620363164, -52.37116123107267 -15.808078625340828, -52.37102368038483 -15.80812082411552, -52.37101771668176 -15.808148035408223, -52.370255172246075 -15.809873077498722, -52.37089300022556 -15.810427380773067, -52.37036654048163 -15.811262610882533, -52.36918635161258 -15.811995241346427, -52.36916805205066 -15.81200391519219, -52.36839891153736 -15.814089303228576, -52.368293985060305 -15.815778963206196, -52.36629224712601 -15.817526006652747, -52.364227600313896 -15.817821396261671, -52.36258273598123 -15.817559519362058, -52.35969036119178 -15.818166915202557, -52.358515031284945 -15.819763591872881, -52.357019904266664 -15.820630401062576, -52.35650757664094 -15.82199309901923, -52.355661971112625 -15.823513642071502, -52.35684143207682 -15.827798438419782, -52.35895967901721 -15.829678113754134, -52.35916948725784 -15.832500190190327, -52.36020865848276 -15.834930252145504, -52.3629081482395 -15.836495405659221, -52.36399812695982 -15.841343052671963, -52.36479040060511 -15.843688899928198, -52.369562088875405 -15.844394311629287, -52.373295039393675 -15.842588760379272, -52.3758470383109 -15.842863338053519, -52.379059591103484 -15.842984716945143, -52.38032237474906 -15.840986783992143, -52.381685997901194 -15.837699975752344, -52.381386841035564 -15.835360808210984, -52.37926991063523 -15.833400457076566, -52.37929875273729 -15.83122509556462, -52.38072773778196 -15.829068234840284, -52.379024135150445 -15.827032257396306, -52.376884963882 -15.82676383611132, -52.37508426910639 -15.825774116134614, -52.37438813905685 -15.82238202098466, -52.37446826750833 -15.816341123180118, -52.37520151096126 -15.81442777427756, -52.376405977493164 -15.813274226198912, -52.377825528687275 -15.813250673011256, -52.3789072845375 -15.81284261315186, -52.37946203963119 -15.811048550491364))) |
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_4e4d |
Folha |
SD22 |
Legenda_Completa |
448Dt42 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
448 |
Nome_Unidade |
Complexo Serrano Moinho-Dourada |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Complexo Serrano Moinho-Dourada |
Area_Poligono_Km2 |
41.376 |
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_4e4e |
Folha |
SD22 |
Legenda_Completa |
448Dc51 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
448 |
Nome_Unidade |
Complexo Serrano Moinho-Dourada |
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 |
Complexo Serrano Moinho-Dourada |
Area_Poligono_Km2 |
13.091 |
the_geom |
MULTIPOLYGON (((-49.68852208926185 -15.714268123832163, -49.689020078900334 -15.712250123092694, -49.68948360335024 -15.711667141046865, -49.69072179451402 -15.711301120025226, -49.69135093850368 -15.709967512368186, -49.690301939364645 -15.707685297605403, -49.69028734678942 -15.706879782114873, -49.69109478106877 -15.705601037515752, -49.691740832556434 -15.705244411844413, -49.69380504777653 -15.704634659601345, -49.69428893515148 -15.70514387325224, -49.69490374595714 -15.706399013889728, -49.69550241494944 -15.706733448149853, -49.69685877935945 -15.706308721229297, -49.697618040695055 -15.705662991547419, -49.69949738840037 -15.704653613869283, -49.70121692627437 -15.704681539547643, -49.702350886571864 -15.705065361514668, -49.70373152911002 -15.706020336828912, -49.70556198043496 -15.705585916962159, -49.70709181407021 -15.704927556896653, -49.70883663146631 -15.706336064454334, -49.71020825471051 -15.70683019752747, -49.71137644431015 -15.705832583051231, -49.71200794927969 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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_4e4f |
Folha |
SD22 |
Legenda_Completa |
298Da52 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
298 |
Nome_Unidade |
Chapada dos Guimarães |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Chapada dos Guimarães |
Area_Poligono_Km2 |
1.096 |
the_geom |
MULTIPOLYGON (((-52.27961190170066 -15.851749488626107, -52.27882369121002 -15.85165015402295, -52.27853768269367 -15.851646479443655, -52.27791029318645 -15.852442176394351, -52.276467124374996 -15.852624122277348, -52.27523639430682 -15.85240753537447, -52.27360067447544 -15.851583459726918, -52.27194536647591 -15.852365199629885, -52.271316990711 -15.853160874129259, -52.27111778226301 -15.853823188914506, -52.271095937884034 -15.855468556209228, -52.269508337076964 -15.857854059403232, -52.26896919659389 -15.859367606407083, -52.27060243138015 -15.860386837103935, -52.27203441342198 -15.86100826801247, -52.27347059021828 -15.861227130215758, -52.275125315899835 -15.860645790229324, -52.276594220884895 -15.85845371723289, -52.2778233776315 -15.858871581427845, -52.2788410510589 -15.859688853539678, -52.27988020835491 -15.858898547722452, -52.28131477308242 -15.859318649558503, -52.28255931784704 -15.858530586124605, -52.283798726554906 -15.85814507106173, -52.28320559493754 -15.856328580513456, -52.28322192474027 -15.855122682569151, -52.28222893906255 -15.85409902537462, -52.2815823106083 -15.853817811160477, -52.28070859718235 -15.853125455199596, -52.280111767811285 -15.852618664142, -52.27961190170066 -15.851749488626107))) |
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