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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_-54a5 |
Folha |
SE23 |
Legenda_Completa |
525Dc33 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Quadrilátero FerrÃfero |
Identificacao_Unidade |
525 |
Nome_Unidade |
Serras do Quadrilátero FerrÃfero - Pará de Minas |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Serras do Quadrilátero FerrÃfero - Pará de Minas |
Area_Poligono_Km2 |
48.161 |
the_geom |
MULTIPOLYGON (((-44.5859980520531 -19.82463626965764, -44.58394642455051 -19.82629334867839, -44.58304992985618 -19.828058834459803, -44.58288278300126 -19.82990192927247, -44.583039307402316 -19.83213074297392, -44.58344195481608 -19.833360673018575, -44.5831954371938 -19.834512275150942, -44.58164875671192 -19.83619851598747, -44.58009976591496 -19.83911462939175, -44.57828103493108 -19.839638985378592, -44.57665790068524 -19.839865576533786, -44.573654801992326 -19.840088860419925, -44.57243917325581 -19.839701892663363, -44.571384324712014 -19.839545738163896, -44.57081569528629 -19.839697994584466, -44.570410780841065 -19.839697020056065, -44.56910909572035 -19.84077014827489, -44.56918591960565 -19.842383378996356, -44.56918281182217 -19.843535546445754, -44.56828771841705 -19.84468555710957, -44.5676364356988 -19.845375284329634, -44.56593058911856 -19.846140160982667, -44.56438570978366 -19.847058133722978, -44.563653548045124 -19.84797808295248, -44.56356901082865 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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_-54a4 |
Folha |
SE23 |
Legenda_Completa |
513Dc32 |
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 |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
144.25 |
the_geom |
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-42.14114842450217 -17.656860208689494, -42.13811092439284 -17.648046413548506))) |
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_-54a3 |
Folha |
SE23 |
Legenda_Completa |
528Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
528 |
Nome_Unidade |
Depressão Interplanáltica do Médio Rio Doce |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão Interplanáltica do Médio Rio Doce |
Area_Poligono_Km2 |
57.275 |
the_geom |
MULTIPOLYGON (((-42.020424547614475 -18.756971247320273, -42.02042454564003 -18.756971247512936, -42.018419531676656 -18.75727044610272, -42.017225731566775 -18.757389826405007, -42.01555441155969 -18.758106106884902, -42.01400247166252 -18.759180527372816, -42.01233115191072 -18.76085184795144, -42.01113735202416 -18.761806888339965, -42.00994355204183 -18.76240378869155, -42.00898851199208 -18.762642548948367, -42.00648153137459 -18.761448749433878, -42.00552649126102 -18.76144874966579, -42.00469083119351 -18.76156812988104, -42.00194509134539 -18.763358830732972, -42.00040084269957 -18.763651898149075, -42.00040100781959 -18.77598719387803, -42.000400766382 -18.85762026231465, -42.000401403765196 -18.8866832325813, -42.000905130960454 -18.886705601444273, -42.002183884121045 -18.88724543780025, -42.0034672193478 -18.887514042514592, -42.00432924196813 -18.888159797807237, -42.0043292431175 -18.888159799933376, -42.0055794881438 -18.88775792138095, -42.00587454491469 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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_-54a2 |
Folha |
SE23 |
Legenda_Completa |
518Atf1 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies do Rio Doce |
Identificacao_Unidade |
518 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais do Rio Doce |
Letra_Simbolo |
Atf |
Categoria |
Terraço fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
PlanÃcies e Terraços Fluviais do Rio Doce |
Area_Poligono_Km2 |
0.269 |
the_geom |
MULTIPOLYGON (((-42.000401579143876 -18.894075183641874, -42.00073925366528 -18.893989975992998, -42.0014676059503 -18.893423353948812, -42.00227342091047 -18.89291598869948, -42.00325830586003 -18.892289243394092, -42.00415365575854 -18.89151327309508, -42.00486993555503 -18.890438852809194, -42.00489978022872 -18.889215207675562, -42.00475625136263 -18.88894970085446, -42.004329243367735 -18.88815980026882, -42.004329242218354 -18.888159798142716, -42.00346721959802 -18.887514042850263, -42.00218388437136 -18.887245438135945, -42.00090513121087 -18.886705601779965, -42.0004014040156 -18.88668323291709, -42.00040147244014 -18.889803178406996, -42.00040147118887 -18.88980317988518, -42.000401579143876 -18.894075183641874))) |
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_-54a1 |
Folha |
SE23 |
Legenda_Completa |
518Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies do Rio Doce |
Identificacao_Unidade |
518 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais do Rio Doce |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais do Rio Doce |
Area_Poligono_Km2 |
13.815 |
the_geom |
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