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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.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_54ff |
Folha |
SD22 |
Legenda_Completa |
448Dc52 |
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 |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Complexo Serrano Moinho-Dourada |
Area_Poligono_Km2 |
128.84 |
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_5500 |
Folha |
SD22 |
Legenda_Completa |
439Dt31 |
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 |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
SuperfÃcies Intermontanas do Alto Maranhão |
Area_Poligono_Km2 |
2.555 |
the_geom |
MULTIPOLYGON (((-48.52028870289744 -15.111357057813182, -48.523177885226104 -15.111560442703022, -48.523771482162736 -15.111281256733285, -48.52461610051256 -15.10985571770717, -48.525230251208825 -15.108198418912137, -48.52550864288165 -15.105102637524421, -48.52541109645271 -15.103552320506138, -48.52395329242798 -15.10233160804531, -48.52301217521397 -15.102091676517883, -48.51929912843697 -15.101821412504439, -48.518655086297684 -15.101411990541655, -48.516243968984945 -15.100811735455949, -48.51414216365813 -15.09918329472574, -48.511484016634526 -15.099383026328294, -48.509786850037976 -15.102692779060112, -48.509228948611366 -15.104579836382158, -48.508750968544504 -15.105090934779863, -48.50837294244514 -15.106751504714724, -48.50764986785466 -15.10783320421783, -48.507057873199464 -15.112302551568597, -48.506393625384334 -15.113327484531958, -48.506413994616295 -15.116139533917279, -48.50687964392572 -15.1166040626196, -48.50722076964384 -15.117525728453826, -48.5079736307277 -15.118624151343994, -48.508675105416806 -15.11903395223757, -48.510503584975304 -15.119110977364492, -48.51141053647506 -15.117571644234914, -48.5120900659896 -15.115341673536095, -48.51395588886939 -15.112665011701093, -48.51692550872498 -15.111320201078303, -48.51905357370618 -15.111051033902976, -48.52028870289744 -15.111357057813182))) |
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_5501 |
Folha |
SD22 |
Legenda_Completa |
300Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos Alcantilados da Borda Noroeste da Bacia Sedimentar do Paraná |
Identificacao_Unidade |
300 |
Nome_Unidade |
Planalto dos Alcantilados -- Médio Araguaia |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto dos Alcantilados -- Médio Araguaia |
Area_Poligono_Km2 |
3.76 |
the_geom |
MULTIPOLYGON (((-53.4410780068855 -15.230563321351244, -53.441102814914814 -15.228373059205675, -53.43865543151843 -15.226594887726462, -53.436187630559125 -15.22678810835243, -53.43373379937207 -15.225666443093035, -53.43285601982594 -15.223904864991392, -53.429096561970105 -15.21926450440198, -53.42754550045515 -15.217714988753182, -53.42531729168854 -15.21637664867145, -53.41904292364163 -15.216090903039422, -53.41348302119265 -15.21208872713586, -53.411684643234125 -15.212508251760779, -53.41074874284714 -15.216001642396034, -53.410733672379365 -15.21731650102987, -53.41629866918249 -15.22088103624676, -53.41854093488914 -15.220904593523949, -53.418966288018765 -15.222879656348791, -53.41716878791933 -15.223299221655756, -53.40995073053733 -15.227164972424418, -53.41149767012544 -15.229152297127794, -53.41417537484096 -15.230276445539298, -53.414610139907424 -15.231595848457413, -53.41477737654371 -15.236635189995045, -53.417270357116806 -15.234252794678794, -53.41774581354494 -15.231848218792912, -53.421335355085425 -15.231667380344401, -53.421132954784454 -15.229694583275185, -53.42293799895155 -15.228617560451335, -53.42675238480654 -15.228439789441065, -53.42807458131835 -15.23042475276679, -53.428063068277496 -15.231519885352501, -53.43232693470525 -15.231127694240778, -53.43882914760018 -15.231196514692195, -53.4410780068855 -15.230563321351244))) |
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_5502 |
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 |
85.229 |
the_geom |
MULTIPOLYGON (((-50.434063752538975 -14.438228970923618, -50.43293859937507 -14.439492360000907, -50.43207858982397 -14.439826708369454, -50.431842149153496 -14.440227796028292, -50.43146595586668 -14.441065608366188, -50.43113873464324 -14.443737062858238, -50.431989584180776 -14.44506148183693, -50.437449628254775 -14.448078410044886, -50.440268903736005 -14.449934005440248, -50.44424657643818 -14.454957334482314, -50.44453662604857 -14.45570686385922, -50.44463820477792 -14.458236607796014, -50.4439203797215 -14.45984241476363, -50.443267226675424 -14.460528690191932, -50.4394915895993 -14.46073713619586, -50.42912003467112 -14.459700799075122, -50.42646592503013 -14.459742766850608, -50.42280288253357 -14.460814953000362, -50.42203330673638 -14.46132723672189, -50.42114828002859 -14.461321859542736, -50.420960537125154 -14.463045804911241, -50.42136877267191 -14.463622953359147, -50.422191858025464 -14.464030094913078, -50.42519704217287 -14.464507369805771, -50.43209341187588 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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_5503 |
Folha |
SD22 |
Legenda_Completa |
421Dt31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
12.425 |
the_geom |
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