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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_-5864 |
Folha |
SE23 |
Legenda_Completa |
514Ai1 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies do São Francisco |
Identificacao_Unidade |
514 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais do 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 |
PlanÃcies e Terraços Fluviais do Rio São Francisco |
Area_Poligono_Km2 |
9.649 |
the_geom |
MULTIPOLYGON (((-46.56446836715445 -17.32764277511971, -46.56529804006158 -17.32485034349604, -46.563909420879334 -17.322074338218947, -46.559639514512945 -17.321452484631962, -46.55639496489605 -17.32114969560486, -46.55414732661477 -17.317561572008195, -46.55412390633697 -17.314775791013684, -46.55015762486015 -17.309726166855043, -46.54435599920037 -17.3096073925598, -46.53938123242414 -17.30620452930699, -46.534071033405716 -17.303622812158597, -46.53098308838961 -17.30151558025953, -46.52789656956757 -17.29957275125116, -46.524311902629904 -17.299272001409676, -46.52104485830693 -17.296182774473138, -46.51219842867229 -17.299035681610725, -46.51170546027368 -17.301333814772285, -46.51173760055664 -17.30526724383708, -46.511929297092614 -17.30788824479007, -46.51827132133815 -17.31160949986453, -46.51710983167875 -17.315551051670706, -46.518327846734664 -17.318492293936284, -46.520727175984256 -17.31978531293237, -46.525164143539314 -17.319915144634347, -46.52892042948722 -17.320214540248138, -46.53183745947414 -17.322322183197322, -46.53374011154353 -17.32542163447794, -46.538363858751275 -17.327516995687052, -46.543462521028054 -17.325183378377794, -46.546193986699585 -17.32532587019629, -46.549608886219985 -17.325627502382336, -46.55080271552205 -17.325618261231064, -46.554726636268136 -17.325587836952625, -46.56036306748505 -17.32636361079164, -46.56446836715445 -17.32764277511971))) |
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_-5863 |
Folha |
SE23 |
Legenda_Completa |
554Dc42 |
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 |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
21.92 |
the_geom |
MULTIPOLYGON (((-47.59492043903367 -17.33247828314878, -47.59317099897245 -17.32930377247434, -47.598739394197764 -17.32467692130436, -47.59894446309396 -17.32020543330238, -47.59614980931638 -17.31852297462897, -47.59495432060477 -17.316218250357164, -47.59195490016403 -17.312733854422735, -47.588522306141655 -17.31020060992313, -47.58522114770792 -17.310672241806905, -47.58368064288585 -17.309231693531455, -47.58193127997724 -17.305558478202343, -47.58018585492162 -17.302229295379732, -47.57773832240118 -17.299854740378038, -47.574517041877854 -17.299638737257386, -47.57045671435699 -17.299055915133916, -47.56727690070915 -17.30094637573045, -47.56221351903002 -17.305736611333597, -47.553563734231815 -17.31406601590421, -47.55273755142461 -17.316131294485142, -47.547432773668895 -17.32345234548084, -47.54607078725475 -17.326902691765838, -47.54571338852977 -17.32826202069311, -47.54461877603167 -17.330715454195026, -47.54455713078111 -17.333065433085768, -47.542439135641274 -17.336255326567407, -47.54447621136463 -17.340837499108382, -47.5463779069536 -17.342348717942876, -47.54838895003077 -17.345033566538746, -47.55029697643506 -17.346997153459746, -47.55032945728546 -17.349345922515226, -47.55166743247395 -17.35095548555667, -47.55599186810459 -17.35090024545776, -47.558315346745154 -17.348972945903263, -47.55885194062449 -17.34697818082322, -47.55870779364633 -17.343366402157468, -47.55990755965912 -17.341724423076712, -47.56198268671912 -17.342239760894877, -47.562113095736485 -17.344858210191763, -47.563452064701245 -17.346467673627494, -47.5647737794147 -17.34690231403378, -47.56757320476051 -17.345330088299324, -47.56960811712865 -17.34295479655476, -47.57129584406313 -17.342662153988275, -47.57151537576309 -17.344918166274113, -47.56875594165546 -17.349290671322183, -47.56849902691777 -17.35110122292829, -47.570868634170125 -17.352425523925373, -47.57292499789125 -17.351586213904675, -47.57485451588814 -17.34839937274597, -47.57563642149376 -17.34378132860604, -47.573532273061595 -17.34118831527389, -47.573123424021155 -17.33884442499796, -47.57489377350163 -17.337736937189195, -47.57790404468898 -17.337878803527538, -47.578964796700866 -17.33976268905213, -47.580587185524266 -17.341458687150322, -47.580420623780526 -17.342997123956422, -47.57988679056637 -17.345171613194218, -47.579726539392496 -17.347161552439605, -47.58116348352225 -17.34904056208909, -47.57978972907171 -17.351678380337415, -47.581872585573976 -17.352735290477032, -47.58297815898689 -17.3510953107507, -47.58435439240454 -17.34863807730989, -47.586722126354 -17.343186671993003, -47.5880060293797 -17.34226599615131, -47.589501850753415 -17.341704738103672, -47.590823238425614 -17.34204889082011, -47.59249965028929 -17.34262867330441, -47.59356183635149 -17.34299693876166, -47.59344971361063 -17.342513395906124, -47.591969866222485 -17.336646679940678, -47.59492043903367 -17.33247828314878))) |
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_-5862 |
Folha |
SE23 |
Legenda_Completa |
549Dc21 |
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 |
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 das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
61.5 |
the_geom |
MULTIPOLYGON (((-45.4749379669003 -17.340736902480398, -45.47195814264574 -17.341062124026905, -45.46963683807797 -17.33979579504845, -45.46764523842107 -17.337893225451847, -45.464328705041645 -17.335674634540663, -45.46366295640925 -17.334404386793548, -45.46531038492791 -17.331221540205725, -45.4653039786112 -17.328677972979822, -45.46695534550639 -17.32708416478349, -45.46827556162193 -17.325173847884468, -45.46959319287715 -17.322627180976763, -45.46859553375938 -17.32072137761837, -45.46660896931824 -17.320726013885448, -45.46396309430448 -17.322003950610544, -45.463636627457625 -17.323912846606593, -45.46198843615662 -17.326777508749103, -45.46033291843601 -17.327099494371613, -45.458013445260725 -17.326469367396147, -45.45058366390126 -17.330379334648278, -45.449512686141816 -17.33038174144526, -45.44915684232605 -17.330726023495252, -45.447372391513966 -17.331072597635934, -45.446304005697215 -17.331760141186088, -45.44380864539988 -17.33313691055509, -45.441670751740034 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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_-5861 |
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 |
4.358 |
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_-5860 |
Folha |
SE23 |
Legenda_Completa |
069Dc51 |
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 |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto de Cristalina |
Area_Poligono_Km2 |
95.699 |
the_geom |
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