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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_46ef |
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 |
0.403 |
the_geom |
MULTIPOLYGON (((-51.500275524949345 -13.68431287055565, -51.49959412711193 -13.684314083280858, -51.4989117405018 -13.684649415620306, -51.498684313358375 -13.684427354941068, -51.49845568176332 -13.68364868984588, -51.49743310794521 -13.683650935852906, -51.496638250206146 -13.684097704501745, -51.4962967472656 -13.684209528833867, -51.495387635599954 -13.683766203247112, -51.49515805616193 -13.6829884047849, -51.49299887897403 -13.6829926209262, -51.492543704458214 -13.68266015539389, -51.492541852360475 -13.682326005560553, -51.492769308888526 -13.682214820034082, -51.49322357988505 -13.682213144753554, -51.49401933177892 -13.682101406133727, -51.49424646209363 -13.682101007074984, -51.494700442738605 -13.681876864987844, -51.49492760736026 -13.681543213306716, -51.4948135724515 -13.681542968886765, -51.49458581756408 -13.681432571258098, -51.49424592852653 -13.681321947476038, -51.49390385013721 -13.68098884024199, -51.49333493269206 -13.680878595236646, -51.49219775206006 -13.680436525642131, -51.49197000978877 -13.68032524642018, -51.49140228191319 -13.68077160214406, -51.49117634939622 -13.681327724418537, -51.49083632969883 -13.68221773130374, -51.4908407954006 -13.68422080568284, -51.49220697764161 -13.684996632836114, -51.49243440890128 -13.685217820059941, -51.4936880476479 -13.68677246069436, -51.494257859771025 -13.687549216347165, -51.494826750302536 -13.687993589236791, -51.49573719661578 -13.687992007623059, -51.49619238716076 -13.688324466635141, -51.49653203834018 -13.687878493686473, -51.49687200191091 -13.687322611849105, -51.49778000881611 -13.686541067263406, -51.498460815625876 -13.686095811140266, -51.49948372348407 -13.685982773394219, -51.49982399209914 -13.685647592551907, -51.500276744621026 -13.684868595376452, -51.500275524949345 -13.68431287055565))) |
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_46f0 |
Folha |
SD22 |
Legenda_Completa |
421Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
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 |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
5.717 |
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_46f1 |
Folha |
SD22 |
Legenda_Completa |
440DEa44 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Complexos Serranos do Norte de Goiás |
Identificacao_Unidade |
440 |
Nome_Unidade |
Complexo Serrano Niquelândia-Barro Alto |
Letra_Simbolo |
DEa |
Categoria |
Estrututral aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo aguçado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Complexo Serrano Niquelândia-Barro Alto |
Area_Poligono_Km2 |
40.195 |
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_46f2 |
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 |
0.09 |
the_geom |
MULTIPOLYGON (((-51.97788854427019 -14.186456302951024, -51.977511424923165 -14.185937274204681, -51.97688407049752 -14.18569581498507, -51.976130910161565 -14.185666978512891, -51.975629391820384 -14.185822993205548, -51.97538049176274 -14.186161230959295, -51.975258780221566 -14.186955856817308, -51.975260506513884 -14.187689925542317, -51.97513887292853 -14.188271807582593, -51.97482739044608 -14.188885587099762, -51.97476624189471 -14.189314105593212, -51.97495656432143 -14.189741984845577, -51.97527149177513 -14.18998448310261, -51.97570908946549 -14.189738292632043, -51.97595932431322 -14.189461603002677, -51.97614487039922 -14.188971655476738, -51.976268312033454 -14.188604289673163, -51.97736209780441 -14.187652107744704, -51.97770568354279 -14.187374398861426, -51.977891704114995 -14.187037418321424, -51.97788854427019 -14.186456302951024))) |
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_46f3 |
Folha |
SD22 |
Legenda_Completa |
421DEa43 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Letra_Simbolo |
DEa |
Categoria |
Estrututral aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo aguçado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
17.071 |
the_geom |
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