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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_-5c3c |
Folha |
SE23 |
Legenda_Completa |
523Pgi |
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 |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
34.344 |
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_-5c3b |
Folha |
SE23 |
Legenda_Completa |
550Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Chapadões Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
550 |
Nome_Unidade |
Chapadas de Paracatu |
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 |
Chapadas de Paracatu |
Area_Poligono_Km2 |
8.658 |
the_geom |
MULTIPOLYGON (((-47.60171275391543 -17.970920146784092, -47.599482627932815 -17.972387807083155, -47.59764092521679 -17.97247751276806, -47.594407239228744 -17.970691099221646, -47.593077487941166 -17.968421296795956, -47.592846050450966 -17.96659468091915, -47.59132210744838 -17.965046335607973, -47.59017974554534 -17.96630337846245, -47.58776481734677 -17.969146115022905, -47.58813778502973 -17.971362806082375, -47.58969988905381 -17.97552518365934, -47.591621011275066 -17.976218391517744, -47.595315004850164 -17.976756900715063, -47.597832224312334 -17.976200283603173, -47.59792789148498 -17.978094631490432, -47.59639990026451 -17.980925586995586, -47.5947609397156 -17.98088160815141, -47.59344350292011 -17.979461484267734, -47.59159599498273 -17.97915926703928, -47.59025357314757 -17.980680897267032, -47.5881876826298 -17.984106921057766, -47.58956317926135 -17.9871771996819, -47.58908600197575 -17.990177403353044, -47.58641815659955 -17.99187657890326, -47.583193044009356 -17.99108783947622, -47.5821488798402 -17.990935585782495, -47.58032850566641 -17.991209101507827, -47.57903961835524 -17.992141125840607, -47.57852962247102 -17.99289660228028, -47.58010313668303 -17.99362343398653, -47.581244759125354 -17.994439997403283, -47.580781868592645 -17.99512440824134, -47.579484681866816 -17.996266072689377, -47.57805357376512 -17.997480859524256, -47.57817862425822 -17.999200543162278, -47.578993202615415 -18.000241831742866, -47.58118612465275 -17.99987845936202, -47.58226922161801 -17.998811886386786, -47.583687070861885 -17.99668871094251, -47.58520466660315 -17.994612062513593, -47.589121584820305 -17.996041755873563, -47.59094156359118 -17.99754819539248, -47.59211187593205 -17.998966678094426, -47.596380180934254 -17.999697010619222, -47.59806501296029 -18.001506821753004, -47.59770430757784 -18.002977407521158, -47.59609457651509 -18.006296252796886, -47.59475927951136 -18.010956143092034, -47.592642463640814 -18.014526513871683, -47.590295757570175 -18.019809539604964, -47.59146755322101 -18.02138241965272, -47.59388576873167 -18.020983346586515, -47.59539506933567 -18.01949735678466, -47.598663024389374 -18.016155339398278, -47.60330319755046 -18.008053522393926, -47.604910402121405 -18.004250600879796, -47.604837310950764 -17.99927637833515, -47.60771727290344 -17.99724717718376, -47.6080242032561 -17.989879135457457, -47.61021975610434 -17.98367956703846, -47.614472298162234 -17.97605967427955, -47.61446378001149 -17.976057982953122, -47.61376036313196 -17.976225510795693, -47.611894686206305 -17.976482753271753, -47.610013339743695 -17.976380753957596, -47.60915965138594 -17.976212527723042, -47.60821161477787 -17.975981446432066, -47.60690459776934 -17.97527473537272, -47.60650239213812 -17.975068816384876, -47.605854215741424 -17.974756926763604, -47.60426312825255 -17.973790306050102, -47.6029047590523 -17.972539679542287, -47.602182446355094 -17.971611044486135, -47.60171275391543 -17.970920146784092))) |
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_-5c3a |
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 |
18.199 |
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_-5c39 |
Folha |
SE23 |
Legenda_Completa |
552Dc32 |
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 |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas de Paracatu |
Area_Poligono_Km2 |
12.858 |
the_geom |
MULTIPOLYGON (((-47.510619827337266 -17.983384257653878, -47.510729598624415 -17.986006516375497, -47.51130481641276 -17.99097186016823, -47.508961644117264 -17.998737789546364, -47.507115791175764 -18.000833546023184, -47.50335516595641 -18.005233638000494, -47.49901773916084 -18.009709763891102, -47.495369031395875 -18.011828701550005, -47.48943753625749 -18.020987361787352, -47.48734701012161 -18.02619393411529, -47.485924242666634 -18.032773762323316, -47.48222399443582 -18.041558590165923, -47.48183626429809 -18.044809569930678, -47.481774876403584 -18.045413677211293, -47.48170927543266 -18.046053965474442, -47.481224129894755 -18.0474772728643, -47.48131231619423 -18.0485807197264, -47.48183189136678 -18.049609984037396, -47.48220413738042 -18.050434313025495, -47.483457555039166 -18.05235189238335, -47.484195277141765 -18.053516527609503, -47.48485155146768 -18.053991281975247, -47.488429676601314 -18.05698437640111, -47.48890095223928 -18.0597410912848, -47.48826505748367 -18.060715675244364, -47.48713378970141 -18.062318921927808, -47.48535398255332 -18.064068698680014, -47.48661338397585 -18.066400717982, -47.48951500734597 -18.06746789145942, -47.491611978991266 -18.067786747482792, -47.49167005994276 -18.066750067768044, -47.491117826818645 -18.06341367734108, -47.4929034501682 -18.06214787522232, -47.4937447760812 -18.06041016106301, -47.494019032747154 -18.059370689819524, -47.494420208090006 -18.05715546595665, -47.49599927231822 -18.056512784731606, -47.49590611280325 -18.055064411635616, -47.49402937267314 -18.05501911107593, -47.49273427960475 -18.055243557937548, -47.493227634446 -18.054408084650124, -47.49406406286709 -18.05232542669249, -47.49497903611941 -18.05072494536748, -47.495391857213015 -18.04926913194049, -47.49386215105204 -18.04825295379788, -47.49269014493768 -18.047025322186045, -47.492826781498906 -18.046470822008377, -47.49323280418837 -18.04453190594104, -47.494238968133956 -18.04431119366399, -47.49407406584978 -18.04279419811837, -47.49540570855055 -18.040014227433293, -47.495282381695624 -18.03642483576434, -47.497900385441994 -18.032750372288536, -47.497805286314325 -18.031162935350626, -47.49944610694248 -18.029829436794948, -47.501647998405964 -18.027384102401683, -47.50301262604029 -18.026951894813383, -47.50429281534594 -18.025623029775055, -47.50555933961216 -18.02339659389147, -47.50826992882678 -18.02122097829484, -47.51093611904595 -18.020978664934255, -47.5129933377357 -18.01853510626299, -47.51558386272235 -18.01808689401865, -47.51824410253099 -18.017430918917547, -47.51912527243869 -18.018524004832937, -47.51956048880824 -18.018726062921807, -47.52136113991315 -18.018494880675274, -47.522648015822455 -18.01764991670775, -47.524235513720654 -18.017697852140827, -47.52749304971646 -18.018484416966245, -47.529007842607356 -18.018464622704993, -47.53303052992913 -18.017306549707495, -47.53315123234001 -18.015647697952947, -47.532558782570284 -18.01455000240021, -47.531044027306514 -18.014569820289424, -47.52894769939742 -18.01425222501088, -47.527082274846975 -18.0149675027606, -47.52601550872802 -18.016085982482714, -47.52470697963579 -18.015343510677987, -47.523031090250235 -18.014191272302657, -47.519622377238825 -18.01292340226923, -47.51880997909334 -18.011553055319947, -47.51792687539941 -18.010320902664702, -47.51763318367511 -18.00997971798909, -47.51588370082889 -18.008690180671998, -47.51627083622445 -18.00550784748261, -47.51804194998805 -18.003206160435596, -47.51642614761767 -18.0011553277146, -47.514992061314395 -17.996807195431042, -47.52126992249697 -17.992507846998986, -47.52242213832006 -17.990435464487554, -47.52194891698028 -17.98735554893785, -47.52019256927056 -17.984703255500797, -47.51694968057728 -17.983305768524257, -47.51354266994548 -17.985510340825105, -47.51224492458999 -17.984909408042647, -47.510619827337266 -17.983384257653878))) |
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_-5c38 |
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 |
1.955 |
the_geom |
MULTIPOLYGON (((-42.130440337655216 -19.051463862389973, -42.12854781029366 -19.053131796573332, -42.126049909479015 -19.05802433375103, -42.12411507969872 -19.05911010447018, -42.123445861306145 -19.06163038848725, -42.12415063162246 -19.063268342919585, -42.12425559227108 -19.065659858144787, -42.12487587124866 -19.067848143065135, -42.13437956870048 -19.074886849516027, -42.137241458352406 -19.07594977648568, -42.140851421596636 -19.076475327904046, -42.144129419824154 -19.078529648483006, -42.146310459415865 -19.081371390224575, -42.149772957563464 -19.083974727321554, -42.154676462903666 -19.08489835235743, -42.15477112784805 -19.084916066730422, -42.1547925966091 -19.084437871835433, -42.154825524212356 -19.083678155238843, -42.15405614982402 -19.081242035358304, -42.15219209234816 -19.07851451951516, -42.14933699802105 -19.076157188640856, -42.14692168718624 -19.075128443186255, -42.1434051670064 -19.074192750453978, -42.14039759897034 -19.07398087182484, -42.13600588036448 -19.07341698504193, -42.1334777396642 -19.072276172896796, -42.13080246192785 -19.06959094304912, -42.13032396006612 -19.06710512462778, -42.129957503324384 -19.064840447223528, -42.12856485493269 -19.061624419537413, -42.12809492990673 -19.058643060558826, -42.12895869140471 -19.055572321496175, -42.13044033346073 -19.051463874021206, -42.130440337655216 -19.051463862389973))) |
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