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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.
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FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5f03 |
Folha |
SE23 |
Legenda_Completa |
527Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
527 |
Nome_Unidade |
Serranias do Alto Mucuri |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serranias do Alto Mucuri |
Area_Poligono_Km2 |
20.691 |
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_-5f02 |
Folha |
SE23 |
Legenda_Completa |
524Arc |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
Arc |
Categoria |
Rampa de colúvio |
Natureza |
acumulação |
Caracteristica |
coluvial ou enxurrada |
Forma |
plano coluvial |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
6.43 |
the_geom |
MULTIPOLYGON (((-43.77538198830681 -18.140526225856643, -43.77678487005486 -18.140088726898814, -43.77839011721676 -18.13950068264156, -43.781302346792266 -18.139079049764586, -43.782862044572255 -18.13878708787061, -43.78394472291324 -18.138314073319506, -43.78474200785019 -18.137011472472828, -43.78428128273449 -18.136114815779248, -43.78342379073501 -18.134915626712385, -43.78250601041799 -18.1345085871168, -43.78169011510569 -18.134403116068356, -43.780559437888826 -18.13430378109315, -43.7794834357997 -18.132726354425227, -43.779181401754215 -18.13116738682023, -43.77896335853481 -18.129218558578813, -43.77974475339855 -18.128161679267343, -43.781150041985384 -18.12777024545648, -43.78293929078877 -18.127617090701456, -43.784571958380084 -18.126323379277654, -43.78533638644513 -18.124705176392943, -43.7841799848169 -18.12245401988743, -43.78205283953006 -18.120909732926176, -43.781366329344415 -18.120826770251043, -43.78059343820088 -18.120661926424912, -43.778947791659526 -18.11946947839629, -43.77787377832621 -18.11775560173409, -43.77722831291288 -18.116935476207086, -43.776483494868096 -18.116405705308694, -43.77504690264651 -18.114787110268797, -43.775123062769815 -18.1128040004288, -43.77530439075655 -18.110781796146, -43.77474513154338 -18.10993690823991, -43.773976475774035 -18.109171115263674, -43.77280664753615 -18.10888262368205, -43.7718689438609 -18.108780860219436, -43.77012813559398 -18.108926097987858, -43.76859276845254 -18.11010012356208, -43.76812725186573 -18.110856244809916, -43.76670452329999 -18.11321570483938, -43.766225173698494 -18.115000125325977, -43.76528210548265 -18.116334248785027, -43.76479646419896 -18.119012367282615, -43.76359325288582 -18.12037644090048, -43.76252673047751 -18.120173493360074, -43.760603008625914 -18.118091692106866, -43.75640549986582 -18.117618224292425, -43.75453907188402 -18.117606167830782, -43.752199478458635 -18.118483865932664, -43.75218681607714 -18.12027126419843, -43.75271230330297 -18.123070655014192, -43.75866319163916 -18.128355875874508, -43.760631187907016 -18.130872655232036, -43.76286295342964 -18.131908169229234, -43.765172451741215 -18.131971794264615, -43.76703059025914 -18.13332476915717, -43.767014939622264 -18.135558574263626, -43.76766199812746 -18.136827874475546, -43.76909929228066 -18.137819375141543, -43.77145522554457 -18.13909597020544, -43.77305151031902 -18.14006496229879, -43.77538198830681 -18.140526225856643))) |
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_-5f01 |
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 |
163.967 |
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_-5f00 |
Folha |
SE23 |
Legenda_Completa |
531Dc41 |
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 |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serra da Saudade |
Area_Poligono_Km2 |
81.978 |
the_geom |
MULTIPOLYGON (((-45.90088136491872 -18.46169006037391, -45.90177623071221 -18.46475849503429, -45.90091635674738 -18.468394682234205, -45.89711557787784 -18.46980897756835, -45.893885049136024 -18.468148721266278, -45.891070410916875 -18.467603467576588, -45.88638353156692 -18.467625444166305, -45.88374506418822 -18.467078352737136, -45.88170044586461 -18.468205795805005, -45.87938214341878 -18.473244952245516, -45.87675922627881 -18.475771300048166, -45.87382848137213 -18.475505585023686, -45.87352451702385 -18.473272046130216, -45.87292273590136 -18.470202113774, -45.8720325768303 -18.46797126938216, -45.867343799282445 -18.467433370119146, -45.8644104074105 -18.46660900480736, -45.861465888418365 -18.46354969504458, -45.85997302120055 -18.45796954970463, -45.85703522164992 -18.456027154168968, -45.852352748501744 -18.456886026954873, -45.847694914038584 -18.46277400430271, -45.84565693242484 -18.465297318645593, -45.84538618798398 -18.469767533301088, -45.84189073603379 -18.473694492205453, -45.840444656694096 -18.477612310261517, -45.84192482275558 -18.480678461360377, -45.84223658137804 -18.484587565979542, -45.840195551794544 -18.486552329084592, -45.84018142379276 -18.486568659118205, -45.83873941089707 -18.488235225356863, -45.83875028552034 -18.49047013058377, -45.842280261329115 -18.493527179079273, -45.84258523609214 -18.496040028143167, -45.8449364149167 -18.497426729586564, -45.84932914007722 -18.49712691019238, -45.85402146159058 -18.498223720749014, -45.85725177189426 -18.499605391614036, -45.86047421048684 -18.499590767902742, -45.86486555016425 -18.499012242489666, -45.86633837341212 -18.500681935924607, -45.866947202263006 -18.50514902202997, -45.86433109404125 -18.509350707652185, -45.85760706282239 -18.512174759235396, -45.85409350213315 -18.512750070430965, -45.85117137696996 -18.51415951705378, -45.849425593924835 -18.516681563115494, -45.84973072838664 -18.519194388740093, -45.84977164294791 -18.519806034745965, -45.84715246395394 -18.528706944350926, -45.844050155754815 -18.531691407537647, -45.84097412699585 -18.539875807695132, -45.84492480887886 -18.55100033206487, -45.841061408332706 -18.55770341484116, -45.844990609255014 -18.56437078529377, -45.85125420289347 -18.57028467087546, -45.859848615082846 -18.57470288871218, -45.8645439014725 -18.57839574933773, -45.86846697649579 -18.583576867057396, -45.870043812854945 -18.58728391396455, -45.87163299971153 -18.59321857108049, -45.87008907064393 -18.596197157243562, -45.87010416380178 -18.599168537673602, -45.876168550935176 -18.59295533904843, -45.88096648177869 -18.589717519229104, -45.884081601276215 -18.586946574721704, -45.887674469738684 -18.583483791585966, -45.89127077720004 -18.5807104686669, -45.894153247151536 -18.57954818967975, -45.89894202731526 -18.574702255968894, -45.89749664442468 -18.57447869042856, -45.89362396997213 -18.570362544453264, -45.89337490839635 -18.568755999494467, -45.88347593590546 -18.562830794880433, -45.883441656343784 -18.55616958586319, -45.88341329403199 -18.550656078500676, -45.884349936641435 -18.54559895284093, -45.88939538827317 -18.54396662513365, -45.89539248272061 -18.544063907005555, -45.90016196468336 -18.544041235336756, -45.90136379716377 -18.5459297100387, -45.900187770577084 -18.54896641148039, -45.904957382323104 -18.548943612921743, -45.909702912566345 -18.544374181027063, -45.91167056397667 -18.540575383932108, -45.9104596867053 -18.537171476201145, -45.90807304364163 -18.53680339859525, -45.90646530910681 -18.533401366928345, -45.90842997196359 -18.529223955104875, -45.91000857375116 -18.526942590284182, -45.91357075434246 -18.5242729771684, -45.91275985418774 -18.521245802950567, -45.91432328906329 -18.516312047122113, -45.91947972107183 -18.514392841174704, -45.920656010534046 -18.51150875895798, -45.9206357484231 -18.50771954312519, -45.920214556960524 -18.503174954835895, -45.91819698416493 -18.497500323684285, -45.91816872307497 -18.492196494003473, -45.9147543147369 -18.483131468219614, -45.91537216785676 -18.47926595115471, -45.91961620521306 -18.476602897680415, -45.91959453787047 -18.472538036982453, -45.919778372998685 -18.467048805747975, -45.91869119647694 -18.46278486499131, -45.90868825300426 -18.46323975411449, -45.90634725226976 -18.46325096083048, -45.90088136491872 -18.46169006037391))) |
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_-5eff |
Folha |
SE23 |
Legenda_Completa |
523Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
523 |
Nome_Unidade |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
14.697 |
the_geom |
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