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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_-5c34 |
Folha |
SE23 |
Legenda_Completa |
534Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
534 |
Nome_Unidade |
Planalto da Zona Metalúrgica Mineira |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto da Zona Metalúrgica Mineira |
Area_Poligono_Km2 |
5.51 |
the_geom |
MULTIPOLYGON (((-43.07024058003558 -18.00997317369629, -43.06832604985991 -18.008031547049985, -43.06736314611533 -18.007665980685587, -43.06573614084107 -18.006723702854806, -43.06455105369215 -18.0062131596747, -43.06299305046998 -18.005698880017, -43.0613699808961 -18.0044006511712, -43.0601017710899 -18.004672536503342, -43.05889877625738 -18.005800627354827, -43.057716064482875 -18.005075952380633, -43.057059960034564 -18.003858758220115, -43.056180114634635 -18.002639317058474, -43.05424942005478 -18.00219260266285, -43.05339231089876 -18.002689013581335, -43.05267678935163 -18.00310282397833, -43.050446530512346 -18.00293764321103, -43.0499269635382 -18.00278966909591, -43.04887606363774 -18.003563269890712, -43.04886039693584 -18.00498693141454, -43.04854889662204 -18.006265771842987, -43.048610146526784 -18.00747789991547, -43.05208835773406 -18.00922222936293, -43.05326889749192 -18.010230597254086, -43.05318883414394 -18.01072849111016, -43.05154701396334 -18.01113930130806, -43.04924347321212 -18.010760149220964, -43.04731523357738 -18.010170641428502, -43.04625014560349 -18.012226056597715, -43.0458742317487 -18.012578216465226, -43.04607679642668 -18.01450277441876, -43.04756006536109 -18.014945067085375, -43.04927258702527 -18.014891865253034, -43.04896185055099 -18.01609934006878, -43.0490246813301 -18.0171678368004, -43.04990672390469 -18.01810275005211, -43.05027026542315 -18.018961065294498, -43.05011089405692 -18.019885483528327, -43.050108537389505 -18.02009957457163, -43.04942107901683 -18.021730578709146, -43.051416994417366 -18.022961295528013, -43.052978069617815 -18.023119753779465, -43.05447238664452 -18.022564714565043, -43.055882101264125 -18.023006210987898, -43.05535308778719 -18.023712805580924, -43.05497090293874 -18.024634989655947, -43.05496464223391 -18.025204997129105, -43.055699296489855 -18.026067035713336, -43.058669375718786 -18.026738305698036, -43.05955324258332 -18.027601828943357, -43.06044336236033 -18.027895339758118, -43.06178400204471 -18.027837404998255, -43.062674735358584 -18.0279890715755, -43.06408529878277 -18.02835914980534, -43.06542282431051 -18.028586647088385, -43.06735134713 -18.029175094792343, -43.06861662593742 -18.029187732441947, -43.07062906735453 -18.028923230209696, -43.07338185890732 -18.029093412264917, -43.074219115643736 -18.02739152306212, -43.0728147250034 -18.026452407411874, -43.07222684525618 -18.025805102821664, -43.07290326901898 -18.025171297656982, -43.07402708826952 -18.02446966798287, -43.073444624160615 -18.023324621352256, -43.07300421500305 -18.022750160251825, -43.07189574533761 -18.021955829111395, -43.069755326106474 -18.020367009933192, -43.06828497396624 -18.018643018491726, -43.06829895096516 -18.01736116812185, -43.06949187925395 -18.01715985737643, -43.068915677505004 -18.01544478858946, -43.0678026116505 -18.01507772299225, -43.06885351314151 -18.014304018900788, -43.06848694981852 -18.013801659142885, -43.07161907985037 -18.013192341951047, -43.07192750680261 -18.01226937992035, -43.07024058003558 -18.00997317369629))) |
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_-5c33 |
Folha |
SE23 |
Legenda_Completa |
531Dc51 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
531 |
Nome_Unidade |
Serra da Saudade |
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 |
Serra da Saudade |
Area_Poligono_Km2 |
243.373 |
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_-5c32 |
Folha |
SE23 |
Legenda_Completa |
531Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
531 |
Nome_Unidade |
Serra da Saudade |
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 |
Serra da Saudade |
Area_Poligono_Km2 |
54.935 |
the_geom |
MULTIPOLYGON (((-45.91816872307497 -18.492196494003473, -45.922523648931254 -18.489143324793517, -45.92689676090652 -18.489501532100157, -45.92927867966436 -18.489110292710507, -45.93044360368366 -18.48417927574085, -45.929628546004416 -18.48039396086936, -45.92841874659647 -18.476990139100124, -45.929985467973985 -18.47281357027847, -45.93353804382303 -18.468628122177495, -45.937881819041046 -18.463681378331447, -45.94104549527135 -18.461013269522667, -45.943019852427845 -18.45872969004767, -45.94338145310896 -18.4522870484709, -45.946135628931025 -18.447347128955734, -45.94730814440467 -18.44393062202062, -45.94570267807763 -18.440907537057974, -45.94173466965166 -18.441685495957252, -45.93854459563403 -18.439427524264985, -45.93773167963383 -18.436021780377743, -45.93454995319351 -18.435279244670927, -45.93099302416374 -18.438707394997156, -45.92582772695707 -18.438353096234987, -45.92421458404811 -18.433814292664163, -45.92577904600034 -18.429260003193125, -45.925758768202066 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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_-5c31 |
Folha |
SE23 |
Legenda_Completa |
549Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
549 |
Nome_Unidade |
Patamares das Chapadas do Alto Rio São Francisco |
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 do Alto Rio São Francisco |
Area_Poligono_Km2 |
45.196 |
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_-5c30 |
Folha |
SE23 |
Legenda_Completa |
513Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
513 |
Nome_Unidade |
Patamares das Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
8.665 |
the_geom |
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