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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_-5436 |
Folha |
SE23 |
Legenda_Completa |
523Dc32 |
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 |
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 |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
25.72 |
the_geom |
MULTIPOLYGON (((-47.31001910970788 -19.532670593584182, -47.306848941040066 -19.533948411378926, -47.305199934232725 -19.53011935010971, -47.30133615077894 -19.53360598745858, -47.29922110715673 -19.5377575995442, -47.29692617513236 -19.539436853525395, -47.29477986451773 -19.541389654631285, -47.2924916485007 -19.543618794051007, -47.291091428366144 -19.54707396172752, -47.28904512022098 -19.54586259818342, -47.28942322193757 -19.541870384332935, -47.28878207920595 -19.53747834744883, -47.2846146426905 -19.540005755122387, -47.28263419893059 -19.543468210372836, -47.2797627878211 -19.545430017118143, -47.27551042035874 -19.546817624844692, -47.274900979232605 -19.546633834956616, -47.27443462068929 -19.545918988721684, -47.27336959832166 -19.545788799044317, -47.27261553364188 -19.546230002778177, -47.272478221433175 -19.547241465004358, -47.27234397737205 -19.54854009371835, -47.27204819912258 -19.549120936220827, -47.27069649230325 -19.550291280257106, -47.26949716181042 -19.551458796878133, -47.26782542827307 -19.55147980705038, -47.26615369257751 -19.551500801770146, -47.26525619352555 -19.55252180411882, -47.26696218035713 -19.55495066797533, -47.26757395125612 -19.55523109176241, -47.26758402631668 -19.55595168891992, -47.26775563960842 -19.55739097983223, -47.26901445098033 -19.560402554842135, -47.26890706663021 -19.562805411371837, -47.26851295783543 -19.56337484293855, -47.26911562851988 -19.563887485086532, -47.276258271046515 -19.567519421987353, -47.27643200097919 -19.56910227052265, -47.277974723703146 -19.570668736426544, -47.27936099726097 -19.57194905701851, -47.28133789772583 -19.57206766305194, -47.28437175759971 -19.571596650881034, -47.28515960923093 -19.571586670279668, -47.29198107309672 -19.576648964114856, -47.29087920401872 -19.577970726768694, -47.29039702122218 -19.57844016820498, -47.290421474166926 -19.580169388674317, -47.289840137713576 -19.582050808420053, -47.29619805214025 -19.583411359706115, -47.298747062572 -19.58092863980096, -47.301002310176536 -19.57916944530105, -47.30388173363741 -19.578556468896235, -47.308457735736624 -19.579651248936834, -47.3098569787045 -19.58121833771372, -47.31062100262803 -19.58207375427876, -47.30897367044532 -19.583825277347334, -47.30566245310142 -19.58617338096145, -47.30417566429738 -19.588499018476583, -47.30464844712349 -19.589646285046722, -47.30491593459794 -19.589893937421852, -47.305364140387546 -19.589983937280554, -47.30629594034458 -19.58957102033849, -47.31026646505904 -19.587078076512253, -47.31395397760077 -19.584860532964004, -47.317660782586884 -19.58399828081061, -47.32167376286627 -19.58448942233599, -47.324578600459844 -19.581864510747113, -47.32831635397475 -19.584158994465902, -47.331225430326505 -19.586073056052857, -47.33411206389723 -19.586425848073162, -47.336135193944784 -19.58405783047111, -47.33690762534549 -19.58053375452406, -47.33727975306621 -19.57779607078958, -47.33790426433169 -19.57544707148942, -47.33868227999166 -19.572313973449734, -47.337808518818015 -19.5688112366048, -47.339821076715545 -19.56566213144294, -47.337712825349186 -19.56217629934746, -47.334382346565256 -19.55948655228147, -47.33230797490116 -19.558342016138706, -47.329805318065944 -19.556032524328497, -47.324427872856866 -19.554150190667738, -47.324016378499905 -19.55415548969071, -47.323788263782944 -19.55259690636827, -47.322800702581084 -19.5528236609051, -47.3225255387853 -19.55283532997032, -47.32069217508115 -19.552743309749054, -47.31884900148323 -19.552298269910636, -47.318714011209806 -19.5522521377421, -47.31581795702804 -19.552329958230626, -47.31460362374985 -19.552288636111506, -47.31273885323417 -19.551931413333907, -47.3127187600289 -19.551925348794253, -47.31125001488497 -19.551613611333767, -47.31043483310068 -19.551503026209524, -47.30933703430208 -19.5514159222913, -47.3073918972121 -19.551368545352396, -47.30569247848251 -19.551181634087772, -47.30541732899869 -19.551127347152786, -47.30407442783706 -19.550954832631394, -47.303406013124686 -19.550914593195042, -47.30267505201672 -19.55089772775706, -47.30172538057168 -19.550909839473782, -47.300409936810645 -19.55092660784766, -47.29868687532235 -19.550011993540956, -47.29940377405147 -19.548969662694233, -47.30233835153633 -19.547781652916257, -47.30600220049173 -19.5454237453285, -47.310632412010875 -19.54276530671366, -47.31220136987413 -19.541156597340013, -47.30520388344809 -19.541535061980177, -47.30364357859969 -19.538859081438005, -47.3098367433451 -19.53906898727985, -47.311451085440865 -19.53837458929546, -47.311921732417396 -19.535769321772857, -47.31331712189591 -19.53401832742279, -47.31001910970788 -19.532670593584182))) |
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_-5435 |
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 |
1.165 |
the_geom |
MULTIPOLYGON (((-42.506869262867426 -19.53603123674674, -42.507205792981296 -19.536942542926457, -42.50763013082392 -19.538090756385113, -42.50856981643376 -19.540416431892947, -42.50890536963883 -19.543936632341566, -42.50983232172392 -19.547094740982175, -42.50989208518469 -19.549593399944367, -42.510167423712765 -19.550707948789146, -42.510940343475134 -19.551180970397716, -42.51230465965029 -19.551292793600105, -42.51621279554589 -19.55088334991268, -42.51623091883535 -19.55088179319672, -42.51836043864033 -19.550727764315226, -42.520411887971136 -19.550570831282855, -42.5212805667937 -19.551138141460815, -42.52146166919951 -19.552066260093866, -42.52130857117299 -19.553045778573935, -42.52132713625843 -19.553015329667698, -42.52157162912928 -19.552662883507175, -42.52201844788789 -19.552410744823785, -42.52243292381838 -19.552093140909925, -42.522745530481075 -19.55170911771613, -42.52288813688687 -19.551291153861225, -42.52234883303914 -19.5508629276592, -42.52190892965847 -19.550662731744694, -42.52167724274168 -19.550239629948862, -42.521683174087535 -19.5498513975024, -42.521242804780535 -19.54961958694885, -42.52083571617462 -19.549516466351267, -42.52015280608079 -19.549572105708357, -42.5195703251579 -19.549725749319887, -42.5190246013846 -19.549718249461087, -42.518480824676786 -19.549645754841634, -42.517833195253544 -19.54963685043155, -42.51739085727905 -19.54953414058472, -42.51640969437876 -19.54903570421972, -42.51585931225472 -19.548337295709498, -42.515412075207614 -19.54737300205941, -42.51572032119697 -19.545407686371508, -42.516433175340794 -19.543207722813648, -42.51635293414592 -19.542102184889945, -42.51551484545487 -19.539789676180433, -42.51446277539862 -19.538762876728278, -42.51340789720394 -19.537920256282685, -42.512054577489145 -19.537533172847933, -42.5108927139741 -19.537332940997615, -42.508951889955945 -19.53730618164534, -42.506869262867426 -19.53603123674674))) |
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_-5434 |
Folha |
SE23 |
Legenda_Completa |
526Da42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Canastra |
Identificacao_Unidade |
526 |
Nome_Unidade |
Serras e Patamares da Canastra |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serras e Patamares da Canastra |
Area_Poligono_Km2 |
49.156 |
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_-5433 |
Folha |
SE23 |
Legenda_Completa |
519Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressões do São Francisco |
Identificacao_Unidade |
519 |
Nome_Unidade |
Depressão do Alto Rio São Francisco |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
195.681 |
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_-542f |
Folha |
SE23 |
Legenda_Completa |
554Dt21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
554 |
Nome_Unidade |
Patamares Dissecados das Chapadas de Cristalina |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
21.458 |
the_geom |
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