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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_-55e1 |
Folha |
SE23 |
Legenda_Completa |
529Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Mantiqueira Setentrional |
Identificacao_Unidade |
529 |
Nome_Unidade |
Serranias da Zona da Mata Mineira |
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 |
Serranias da Zona da Mata Mineira |
Area_Poligono_Km2 |
5.243 |
the_geom |
MULTIPOLYGON (((-42.00216452002945 -19.385446678555326, -42.00178472330412 -19.385237791024664, -42.00056937161284 -19.3845541561253, -42.000401917287434 -19.38450087525147, -42.000401922377556 -19.40378627429867, -42.004862508005886 -19.406470371239596, -42.005943403254754 -19.413820444579297, -42.00594340433826 -19.417711660020323, -42.00507869206402 -19.425926448390637, -42.00507869369056 -19.431763271552235, -42.00486251541141 -19.433060343420237, -42.00486251583327 -19.434573593869565, -42.005294873596704 -19.43630302284573, -42.007024303324734 -19.43846480876707, -42.00896991072889 -19.43716773646455, -42.0094022670457 -19.433708878186234, -42.00940226650341 -19.431763270465957, -42.009834623242256 -19.42981766263701, -42.010915516204435 -19.42895294782303, -42.01199640892543 -19.42722351846664, -42.01350965886748 -19.425277910366198, -42.01459055158851 -19.42354848100996, -42.01696851573146 -19.42030580087903, -42.01848176513144 -19.41641458505834, -42.01999501483249 -19.413604262415852, -42.020427371571735 -19.411658654587054, -42.02042737102979 -19.40971304686682, -42.02041726305378 -19.409662507060776, -42.019331367841914 -19.412051478208966, -42.01887561115587 -19.412507235125826, -42.01819197593631 -19.41250723529732, -42.01697662432909 -19.412127438267056, -42.01659682683672 -19.411595722092738, -42.01652086707169 -19.41053228957249, -42.01629298847468 -19.409848654425748, -42.01629298824195 -19.40901310028775, -42.01598915021856 -19.408481384094333, -42.01507763627518 -19.40734199231654, -42.014621879356305 -19.40696219509539, -42.01355844664451 -19.40643047909245, -42.01158350045471 -19.406430479587986, -42.00854512193363 -19.40726603448836, -42.00710189202555 -19.40726603485031, -42.00603845939828 -19.40703815671579, -42.00550674275688 -19.405746845908343, -42.005658661525366 -19.405139170133445, -42.00694997222089 -19.404151696737035, -42.011355620673626 -19.401493114283593, -42.01287480992351 -19.401037357099888, -42.013026728565194 -19.399973924522488, -42.0127988497147 -19.39837877577057, -42.01234309277487 -19.397923019082207, -42.01135561955309 -19.397467262527243, -42.009456632789934 -19.397315344069145, -42.008772997485856 -19.39701150637215, -42.00808936213961 -19.39655574974095, -42.007709564605136 -19.39587211463218, -42.00770956399235 -19.393669290086137, -42.00786148280318 -19.39321353324544, -42.00877299615452 -19.39222605994451, -42.0115075366099 -19.39070686991698, -42.011887333763816 -19.390023234617825, -42.01181137383016 -19.388352126360672, -42.010975819377336 -19.387288694030552, -42.00740572432117 -19.387212735458238, -42.006949967529344 -19.38728869503945, -42.00505098114652 -19.388504046989105, -42.004443305395775 -19.388504047141414, -42.00398754851945 -19.388276168854265, -42.00322795361988 -19.387516574373457, -42.00284815591668 -19.38622526352773, -42.00216452002945 -19.385446678555326))) |
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_-55e0 |
Folha |
SE23 |
Legenda_Completa |
518Aptf |
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 |
Aptf |
Categoria |
PlanÃcie e terraço fluviais |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie e terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais do Rio Doce |
Area_Poligono_Km2 |
4.071 |
the_geom |
MULTIPOLYGON (((-42.01819197616018 -19.412507235597726, -42.01887561137965 -19.41250723542616, -42.01933136806569 -19.412051478509284, -42.02041726327765 -19.409662507361176, -42.01999501337074 -19.407551260920098, -42.01999501332343 -19.407551259989734, -42.01934647389982 -19.394796721584328, -42.01934647371168 -19.394796720596652, -42.01848175807511 -19.390256970454207, -42.01848175807513 -19.390256969548744, -42.018481757534055 -19.38831136273404, -42.01848175734874 -19.388311361745558, -42.01783322065099 -19.384852504727476, -42.01783322063326 -19.384852503809395, -42.01769847571154 -19.37786995654783, -42.017628809396896 -19.377800290271487, -42.017628808413754 -19.37425976333284, -42.01762880818809 -19.374259751634987, -42.017628807644385 -19.372129538813226, -42.01697661339529 -19.37202083994257, -42.01545742401914 -19.3720208403232, -42.01477378896866 -19.372628516231302, -42.014469951262306 -19.37323619204415, -42.01439399225782 -19.374907300339377, -42.013406519374314 -19.375666895257783, -42.01348247918089 -19.376882246712192, -42.01409015507912 -19.37741396282972, -42.01424207437565 -19.37870527373227, -42.01371035819953 -19.379085071201054, -42.01219116901321 -19.379768706785654, -42.00922874998251 -19.38068022113318, -42.008165317566814 -19.38121193766928, -42.00687400687124 -19.38219941106521, -42.006342290652796 -19.382427289599754, -42.00520289866261 -19.382579208819486, -42.004747141828545 -19.38250324946654, -42.003911587523675 -19.381971533406137, -42.002772195174636 -19.380832141685094, -42.001860681400856 -19.380300425643615, -42.00040191640559 -19.38030042600905, -42.000401916726055 -19.381515777786056, -42.000401917513145 -19.384500875554483, -42.000569371838566 -19.38455415642827, -42.001784723529845 -19.385237791327583, -42.002164520255086 -19.385446678858212, -42.00284815614222 -19.386225263830543, -42.00322795384543 -19.387516574676198, -42.00398754874491 -19.388276169156878, -42.00444330562124 -19.388504047443956, -42.00505098137188 -19.388504047291736, -42.00694996775481 -19.387288695342033, -42.00740572454664 -19.38721273576085, -42.01097581960262 -19.387288694332966, -42.01181137405536 -19.388352126662856, -42.01188733398892 -19.390023234919944, -42.01150753683501 -19.390706870219162, -42.00877299637961 -19.39222606024678, -42.00786148302828 -19.39321353354756, -42.00770956421736 -19.39366929038823, -42.00770956483015 -19.395872114934072, -42.00808936236443 -19.396555750042832, -42.00877299771079 -19.397011506673916, -42.00945663301477 -19.397315344370895, -42.011355619777945 -19.397467262828883, -42.01234309299953 -19.39792301938383, -42.012798849939365 -19.398378776072075, -42.01302672878977 -19.399973924823914, -42.012874810147984 -19.401037357401297, -42.01135562089821 -19.401493114584973, -42.006949972445454 -19.40415169703847, -42.00565866174993 -19.405139170434815, -42.00550674298146 -19.405746846209798, -42.006038459622765 -19.407038157017027, -42.00710189224994 -19.40726603515161, -42.008545122158026 -19.407266034789536, -42.011583500679016 -19.406430479888925, -42.01355844686883 -19.40643047939352, -42.014621879580524 -19.406962195396357, -42.01507763649931 -19.407341992617432, -42.0159891504426 -19.408481384394932, -42.016292988466006 -19.409013100588417, -42.01629298869873 -19.4098486547264, -42.01652086729565 -19.41053228987297, -42.01659682706068 -19.41159572239317, -42.01697662455295 -19.412127438567495, -42.01819197616018 -19.412507235597726))) |
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_-55df |
Folha |
SE23 |
Legenda_Completa |
526Dc52 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Canastra |
Identificacao_Unidade |
526 |
Nome_Unidade |
Serras e Patamares da Canastra |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serras e Patamares da Canastra |
Area_Poligono_Km2 |
108.983 |
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_-55de |
Folha |
SE23 |
Legenda_Completa |
000Magua |
Nome_Dominio |
|
Nome_Regiao |
|
Identificacao_Unidade |
0 |
Nome_Unidade |
|
Letra_Simbolo |
|
Categoria |
|
Natureza |
|
Caracteristica |
|
Forma |
|
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Corpo d´água continental |
Area_Poligono_Km2 |
1.014 |
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_-55dd |
Folha |
SE23 |
Legenda_Completa |
526Dt33 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Canastra |
Identificacao_Unidade |
526 |
Nome_Unidade |
Serras e Patamares da Canastra |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Serras e Patamares da Canastra |
Area_Poligono_Km2 |
224.677 |
the_geom |
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