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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_-57fe |
Folha |
SE23 |
Legenda_Completa |
510Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
510 |
Nome_Unidade |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
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 dos Rios Jequitaà - Verde Grande |
Area_Poligono_Km2 |
20.066 |
the_geom |
MULTIPOLYGON (((-44.055239632761165 -16.84388040811935, -44.056855982121455 -16.842155124153066, -44.05768333095637 -16.83807885982941, -44.058981174274514 -16.834126767189755, -44.05851540856921 -16.832657653033063, -44.05825430280487 -16.831557351043745, -44.057767226205065 -16.830414434573587, -44.057426792784746 -16.829415001227524, -44.05693996306416 -16.828224179093368, -44.0564012727681 -16.82765226837327, -44.05588306671757 -16.827113893635882, -44.04425198498409 -16.82527860546969, -44.04261244539981 -16.823781401989038, -44.04111080991967 -16.818940523237053, -44.04026343774496 -16.813892992332224, -44.03895528591492 -16.81388688282238, -44.03611077412918 -16.815765360858634, -44.031979366862146 -16.813433865105555, -44.03134556753684 -16.80943760395524, -44.03135196781717 -16.80817674176052, -44.03221312287433 -16.801018560825874, -44.03221464855515 -16.800717580508458, -44.03090524644667 -16.7976482156166, -44.02931995816399 -16.796620280196827, -44.028006727634846 -16.79431735951072, -44.0242966263555 -16.79429980727567, -44.02216819538039 -16.79582085423572, -44.019500029337955 -16.799381134840658, -44.01948430272469 -16.802443349371703, -44.019734131289326 -16.805506828511607, -44.0197236441531 -16.807548605177164, -44.019438413103835 -16.811375104412967, -44.019163287882684 -16.813415617700873, -44.01915673057479 -16.814690936104963, -44.020462113619054 -16.81852501575297, -44.02065089816831 -16.821053113671486, -44.01914995549759 -16.821299942325016, -44.01712012514171 -16.821830755543036, -44.014952409977695 -16.815260155980607, -44.014795423017944 -16.806770336161854, -44.01562863405827 -16.800600041100008, -44.01725725656526 -16.79520453101966, -44.01707129289152 -16.792502898841622, -44.01285772348239 -16.79441158042085, -44.009635249900015 -16.79825559080683, -44.006783269185874 -16.80769622666787, -44.00695703676322 -16.81271348768241, -44.00594564292886 -16.814830862944195, -44.005544941408196 -16.81482892543711, -44.00433873690634 -16.815788409572182, -44.004928250792396 -16.817913523832882, -44.00794225406289 -16.8158058275697, -44.00914342739918 -16.815811619539865, -44.009521083567066 -16.820251390496626, -44.007707235460295 -16.82255742587153, -44.004695129024505 -16.824280077693253, -44.00428332269511 -16.82640034140044, -44.004265180825655 -16.82987287471929, -44.004253080710136 -16.832188498825353, -44.00844683352505 -16.835168918441788, -44.01001996523048 -16.83568266706825, -44.01141497177697 -16.836702611449752, -44.01332770206387 -16.839243517760814, -44.01405893225668 -16.8417633727731, -44.01605916328188 -16.844097693012518, -44.018597430563986 -16.846034158750154, -44.018589439421035 -16.847584239344396, -44.02018912744328 -16.8495288522793, -44.02220040319624 -16.8499261995451, -44.02341140266341 -16.84915735696189, -44.02422664247089 -16.847223357236143, -44.02544649462709 -16.844903517844198, -44.027056133536995 -16.8449111523705, -44.02866473362345 -16.84530652606202, -44.02865682480841 -16.846856611434028, -44.02985790916742 -16.848024657498033, -44.03106388985718 -16.84841811048345, -44.033082117915704 -16.84726526025217, -44.03348476811463 -16.84726715646366, -44.03589870661365 -16.847666265235436, -44.03751229483818 -16.846898322473372, -44.038299234168996 -16.846820662894974, -44.03982867510771 -16.84654310509202, -44.040127058140904 -16.84823653413878, -44.03918841787417 -16.84898686899141, -44.03795750014631 -16.84999433435124, -44.03882468561517 -16.851685910448044, -44.0414431545023 -16.853048529914087, -44.04320223444031 -16.85153824683255, -44.04425677004927 -16.85069895076096, -44.0453172216114 -16.848678324583584, -44.045499508808064 -16.84732879762542, -44.04550627926385 -16.84597845423011, -44.043940582533025 -16.84394560674891, -44.04359897358113 -16.842256499284602, -44.044484719677 -16.840066037307107, -44.045186569912794 -16.839731255973646, -44.04571290231686 -16.838835259621206, -44.04608318521358 -16.83873755460736, -44.04633002125711 -16.838738700985196, -44.04678219859862 -16.838780570376418, -44.04721352935353 -16.838862112188757, -44.04752211047114 -16.8389033137181, -44.04768556433316 -16.83906224837942, -44.048014595067436 -16.839143314144145, -44.048383391865954 -16.83934297019612, -44.04856709296819 -16.839582442154654, -44.048998083281575 -16.839920676905642, -44.049195372100755 -16.8400707284668, -44.050209186725105 -16.84060327828248, -44.052562740335404 -16.84313322882774, -44.055239632761165 -16.84388040811935))) |
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_-57fd |
Folha |
SE23 |
Legenda_Completa |
513Dt31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
513 |
Nome_Unidade |
Patamares das Chapadas do Jequitinhonha |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
0.086 |
the_geom |
MULTIPOLYGON (((-42.25572630049433 -16.082384973506354, -42.25616473740209 -16.08236079764849, -42.256606918321076 -16.082063916575358, -42.25688866012345 -16.082022374476868, -42.25713793268972 -16.082100534834186, -42.25768792286739 -16.081911606687243, -42.25780155801968 -16.081595154118588, -42.25801222347616 -16.081083058343047, -42.25819112083218 -16.08057145791334, -42.25818001325142 -16.080223600936126, -42.257994779025346 -16.08003969118207, -42.25765150614422 -16.080004580950035, -42.257509649290476 -16.080063272597418, -42.2573246265687 -16.079864011461286, -42.25701610332276 -16.07954304626839, -42.25645801894704 -16.079233328921223, -42.25579855334249 -16.079436203268788, -42.25543472650491 -16.079673578016546, -42.255127970618595 -16.08038042098495, -42.25498059723654 -16.080908679285535, -42.25499999383792 -16.08174073179053, -42.25518315480751 -16.082075443815643, -42.25572630049433 -16.082384973506354))) |
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_-57fc |
Folha |
SE23 |
Legenda_Completa |
554Dc21 |
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 |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
49.537 |
the_geom |
MULTIPOLYGON (((-47.859136927185304 -16.7999835526368, -47.85753001175606 -16.800293956362818, -47.85722384561992 -16.800383095816226, -47.85703711392939 -16.80043445413735, -47.8560792503861 -16.800640106719364, -47.85504208232037 -16.800808928836716, -47.85416944380326 -16.800821043387185, -47.853530811361956 -16.799868175003706, -47.853527206017496 -16.799627114757037, -47.85401506329777 -16.79889881987238, -47.85401954724746 -16.798885212125317, -47.854280177273054 -16.798196191774476, -47.85449665560778 -16.79768929402175, -47.854493063045204 -16.79744913677466, -47.85410468680716 -16.79649189211229, -47.854101095008694 -16.796251734754755, -47.85321854930842 -16.79566255840552, -47.85185353509026 -16.796161904776138, -47.85172887517501 -16.796163633256974, -47.850369259832036 -16.79702501374654, -47.84973566913418 -16.798290821908324, -47.849557566442954 -16.79866895339508, -47.849065993601606 -16.799777470307447, -47.84906055847509 -16.79979018813804, -47.8486279120537 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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_-57fb |
Folha |
SE23 |
Legenda_Completa |
103Ai1 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressões do São Francisco |
Identificacao_Unidade |
103 |
Nome_Unidade |
Depressão do Médio Rio São Francisco |
Letra_Simbolo |
Ai |
Categoria |
Plano de inundação |
Natureza |
acumulação |
Caracteristica |
inundação |
Forma |
plano abaciado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
Depressão do Médio Rio São Francisco |
Area_Poligono_Km2 |
101.317 |
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_-57fa |
Folha |
SE23 |
Legenda_Completa |
069Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
69 |
Nome_Unidade |
Planalto de Cristalina |
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 de Cristalina |
Area_Poligono_Km2 |
29.661 |
the_geom |
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