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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_-5e5a |
Folha |
SE23 |
Legenda_Completa |
549Pri |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
549 |
Nome_Unidade |
Patamares das Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
15.676 |
the_geom |
MULTIPOLYGON (((-45.24581128306716 -18.139083793796136, -45.244646950277335 -18.14001533473358, -45.24414137815001 -18.140157880476814, -45.24108971483058 -18.140140034597522, -45.23906151929381 -18.139855141103553, -45.238911206706504 -18.139855327726455, -45.23792461214823 -18.139426318822476, -45.237175447237036 -18.139100954753893, -45.23674198551284 -18.138739045859815, -45.236389918328584 -18.138445728368755, -45.233086124346805 -18.136475755401957, -45.230610097475626 -18.137070757102062, -45.22978764500086 -18.139243684933923, -45.230204694468675 -18.142244861698693, -45.22959011181934 -18.145799520153034, -45.22897936217833 -18.15231607393224, -45.22981143237336 -18.15744802002791, -45.231879273381075 -18.16040743799071, -45.236425809582734 -18.165139854096207, -45.23911316496812 -18.1680984268981, -45.240976517766214 -18.172044992026205, -45.24077458865508 -18.17579619389802, -45.24131400817385 -18.17818889289837, -45.24139772774482 -18.17855936321231, -45.245529953930905 -18.181318980537814, -45.250695085525855 -18.184866215179074, -45.254002562375184 -18.188612810631344, -45.25566003287631 -18.192361550173516, -45.256492798166434 -18.197296311130984, -45.26063069189925 -18.20341153872289, -45.263732864194196 -18.207356172475283, -45.264975941627036 -18.210118397786765, -45.26394557492145 -18.211699727489005, -45.26229696037655 -18.213478934726723, -45.26210693083071 -18.213524386392507, -45.26286297552383 -18.21441001696789, -45.26394355251337 -18.215379254994133, -45.266482705986355 -18.215223899227855, -45.277265912331565 -18.21136188287066, -45.28137863546173 -18.21056865234415, -45.284393699544076 -18.209427179320755, -45.28649257902926 -18.20671344886376, -45.288683766700515 -18.204962143459934, -45.29032683748107 -18.20347285225323, -45.29297456693601 -18.2016322310285, -45.29571152712427 -18.197781301668474, -45.297992103935734 -18.19532927908819, -45.30020312636587 -18.193714292063902, -45.30014743896848 -18.193223595276674, -45.296329948083624 -18.192155765519622, -45.293638204653 -18.193018547082374, -45.29072445187438 -18.195170500719733, -45.28354462268012 -18.19668432246726, -45.27928035773453 -18.197119896915904, -45.272323135529696 -18.19777432976462, -45.2694021090023 -18.1954158154472, -45.26625577182299 -18.19284335772101, -45.266025823071764 -18.18962239059323, -45.2678166548262 -18.18639951867438, -45.27073348232509 -18.18553587718132, -45.27252323936442 -18.182312059178045, -45.2720710363424 -18.179735850542016, -45.26982294196401 -18.177591494791148, -45.26443798502555 -18.178243420207078, -45.26039852277526 -18.178248937233203, -45.255911166233794 -18.179113616120905, -45.2520957819173 -18.179118660213756, -45.249848242445395 -18.177189181490775, -45.24825231969962 -18.169965931431225, -45.2477593649556 -18.167046250059197, -45.24748206577718 -18.166187052166787, -45.246065231919005 -18.1618025172387, -45.24526302174447 -18.15199954152072, -45.247620101776455 -18.146718067131747, -45.2476096239257 -18.13927400815159, -45.24581128306716 -18.139083793796136))) |
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_-5e59 |
Folha |
SE23 |
Legenda_Completa |
566Da42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
566 |
Nome_Unidade |
Patamares Dissecados do Planalto de Cristalina |
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 |
Patamares Dissecados do Planalto de Cristalina |
Area_Poligono_Km2 |
112.84 |
the_geom |
MULTIPOLYGON (((-46.86593988590345 -18.06992706226534, -46.86443247150651 -18.071104391717434, -46.86268440556073 -18.072394256576082, -46.861743326111885 -18.074968289409224, -46.86105084402708 -18.075677868168, -46.86052697948511 -18.07804639970235, -46.858086457096476 -18.08095740944031, -46.857022029070194 -18.084118064194485, -46.85484979314742 -18.08650244566211, -46.851567032883246 -18.087583818847037, -46.84939011187828 -18.0894423699955, -46.846943756789756 -18.09182839968466, -46.84421147088376 -18.093167297901726, -46.84064266331293 -18.09320139325593, -46.83597797708308 -18.0935087714608, -46.83022375918393 -18.09461331457887, -46.82582750678693 -18.094392979049488, -46.82441963549913 -18.090992937933642, -46.82302267995791 -18.088643531990698, -46.819717023834585 -18.08762398975802, -46.81669709948533 -18.0876524541822, -46.81422599053021 -18.087675710558024, -46.81261524925428 -18.088225718833627, -46.80884344874165 -18.085871389307364, -46.80467866948706 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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_-5e58 |
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 |
12.691 |
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_-5e57 |
Folha |
SE23 |
Legenda_Completa |
519Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
2.374 |
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_-5e56 |
Folha |
SE23 |
Legenda_Completa |
524Pru |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
Pru |
Categoria |
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aplanamento |
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retocado desnudado |
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pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
48.589 |
the_geom |
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