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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 SE.23 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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58b5 |
Folha |
SE23 |
Legenda_Completa |
149Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
149 |
Nome_Unidade |
Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
3.959 |
the_geom |
MULTIPOLYGON (((-42.31546453408495 -17.777634812480457, -42.315799348893 -17.775602971741627, -42.31803976314288 -17.774663777306117, -42.31696155136374 -17.772320874284453, -42.31597550087546 -17.770561714925467, -42.31690608732046 -17.769217146980008, -42.31694516830052 -17.766598763061324, -42.31555777606534 -17.764639944867508, -42.31698858074691 -17.763689647320124, -42.317813951634 -17.762634418543012, -42.31946032976813 -17.760814678065678, -42.317383125091396 -17.757585739391097, -42.31623020267625 -17.753496173337513, -42.31576614184259 -17.75067763827518, -42.31660592057472 -17.74865179692941, -42.31492680963943 -17.745913252732386, -42.31262843408347 -17.743941953620617, -42.31061321806892 -17.74333274018176, -42.30917821860456 -17.744573739858634, -42.30670801762586 -17.747352885553997, -42.30688883406795 -17.748810217275622, -42.306949024750224 -17.751526578430237, -42.30682789099659 -17.752882229014798, -42.305696196132985 -17.754127358191358, -42.30527067777195 -17.755479723498336, -42.30383989539368 -17.756429936514785, -42.304022653767966 -17.75769313511623, -42.30338093336543 -17.760011509963135, -42.30465134109863 -17.763035309378395, -42.304515618533166 -17.765361551955205, -42.30551170367686 -17.76644178328785, -42.30772152936241 -17.767539604797197, -42.31035546975242 -17.76738163932261, -42.31165648688763 -17.768369404160122, -42.30960328332755 -17.770281001927952, -42.308072074740124 -17.77113232179369, -42.3070405688677 -17.77247635316474, -42.308411934818395 -17.775501532086885, -42.3100048309479 -17.77726906433021, -42.31160645934971 -17.778455128904294, -42.31546453408495 -17.777634812480457))) |
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 SE.23 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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58b4 |
Folha |
SE23 |
Legenda_Completa |
513Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
513 |
Nome_Unidade |
Patamares das Chapadas do Jequitinhonha |
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 |
Patamares das Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
20.223 |
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 SE.23 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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58b3 |
Folha |
SE23 |
Legenda_Completa |
554Dc31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
554 |
Nome_Unidade |
Patamares Dissecados das Chapadas de Cristalina |
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 |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
32.064 |
the_geom |
MULTIPOLYGON (((-47.720488325056564 -17.737597290158817, -47.717745587054004 -17.73600620504127, -47.71367469718189 -17.73638857895849, -47.70913909373925 -17.73970862928456, -47.707678505593734 -17.74429017214916, -47.71145701589684 -17.74700673063404, -47.714890584999054 -17.749402879264796, -47.71377761744133 -17.754467290676946, -47.71201469379002 -17.761495822255693, -47.706835860114765 -17.76726848347156, -47.70400884439712 -17.77137945050456, -47.70523732380143 -17.773968716560944, -47.709678767851074 -17.775536407944028, -47.710574528915714 -17.778618786715533, -47.717469799281304 -17.773961842707916, -47.72265956721449 -17.77471150783455, -47.722683673445815 -17.776302348363586, -47.72098647211476 -17.780246999934366, -47.71978633138539 -17.782224209539763, -47.72151623280594 -17.78503844745212, -47.719342175524396 -17.787689333854946, -47.71876357537823 -17.78938156866752, -47.716718912721404 -17.791681155876038, -47.71489682487829 -17.794801223538638, -47.710861498527784 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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 SE.23 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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58b2 |
Folha |
SE23 |
Legenda_Completa |
552Dc31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
552 |
Nome_Unidade |
Patamares das Chapadas de Paracatu |
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 |
Patamares das Chapadas de Paracatu |
Area_Poligono_Km2 |
12.603 |
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 SE.23 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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58b1 |
Folha |
SE23 |
Legenda_Completa |
149Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
149 |
Nome_Unidade |
Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
15.021 |
the_geom |
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