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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_-5406 |
Folha |
SE23 |
Legenda_Completa |
554Dc53 |
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 |
muito alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
173.809 |
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_-5403 |
Folha |
SE23 |
Legenda_Completa |
554Pgu |
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 |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
16.864 |
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_-5402 |
Folha |
SE23 |
Legenda_Completa |
532Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
532 |
Nome_Unidade |
Planalto dos Campos das Vertentes |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto dos Campos das Vertentes |
Area_Poligono_Km2 |
21.438 |
the_geom |
MULTIPOLYGON (((-45.10274388900367 -19.59485503975714, -45.09862541975717 -19.590085747831807, -45.09722651515349 -19.58996360289131, -45.09588464572707 -19.589539577304002, -45.09305291022876 -19.589965805065155, -45.087836984708794 -19.591522804362242, -45.07606397013976 -19.596332282700505, -45.07099596121619 -19.594638988451184, -45.068758575087074 -19.591601578963008, -45.06744116198302 -19.592516632323992, -45.06738993221784 -19.593145634443037, -45.06711956242578 -19.596503925221207, -45.067014094820976 -19.602025635700866, -45.067231648000174 -19.606933603615335, -45.06766454105093 -19.609080655642305, -45.06831201847318 -19.611227624844776, -45.06626307073631 -19.61235350819506, -45.065292942745415 -19.61409169511216, -45.0656177725824 -19.615523052088353, -45.06723589763495 -19.61715816824043, -45.06777658716204 -19.61930517721072, -45.068856402650084 -19.622065596546737, -45.066915177389035 -19.623395683111934, -45.066376038605306 -19.625031594185764, -45.067347455498314 -19.626258468707412, -45.065407535286745 -19.628611535122808, -45.06519189807282 -19.63075882233366, -45.06486938996034 -19.63280312472104, -45.06228176575806 -19.635258507215315, -45.06195825853766 -19.637303707527806, -45.06293023361072 -19.639859052571566, -45.06508902420666 -19.642926367506096, -45.06821858291248 -19.64517543595482, -45.07037602937773 -19.644765226084466, -45.07134696322382 -19.644560606085864, -45.075877286755684 -19.643536660908357, -45.07792759788565 -19.644557875765166, -45.077928288748446 -19.645989345334833, -45.07857625952015 -19.646602679562204, -45.08202835009423 -19.646703257159718, -45.08558785219627 -19.64608798267972, -45.08850094717852 -19.646086573021247, -45.089903238159955 -19.64629011505061, -45.091141508758476 -19.646566025742196, -45.09181883863182 -19.646716600060614, -45.09193863667764 -19.646033337616903, -45.09193775059947 -19.64447715724707, -45.09189931449747 -19.642305572185673, -45.0932399377369 -19.64148160641559, -45.09552967193322 -19.6423777849953, -45.09726670488486 -19.642526869395795, -45.09829303760628 -19.642526311580607, -45.099476615965386 -19.64230154204315, -45.10065967785798 -19.641253489165802, -45.101290364477656 -19.64005572509789, -45.10168435356621 -19.638633973544486, -45.1018417437789 -19.63713734738595, -45.10121013488487 -19.63683857701456, -45.10065627413313 -19.635791492198255, -45.100498338741325 -19.63489420012018, -45.10081329794262 -19.6336966129953, -45.10215452140558 -19.632498445619962, -45.10302155679913 -19.63107732465826, -45.10407652640894 -19.631226733045892, -45.10483256894234 -19.63076359650022, -45.107694622665186 -19.6290105233058, -45.11037200223047 -19.62646948540605, -45.11260325070205 -19.625727063961083, -45.118180109508685 -19.620962760636157, -45.11884790552142 -19.618635274522635, -45.118065976077105 -19.617471813441355, -45.11639285548947 -19.618319676593003, -45.11226444730546 -19.619909208079804, -45.109921548800855 -19.620439322380122, -45.1083582053547 -19.62012306850863, -45.10635101769473 -19.622134110777957, -45.10478985258474 -19.623721936353792, -45.10155335963833 -19.624464830973714, -45.09842828226631 -19.623408325072738, -45.09652865802064 -19.620552733412033, -45.096081001277526 -19.61833165860406, -45.09652632163813 -19.616638775072715, -45.09808845388496 -19.61505101930925, -45.099314669130955 -19.613146233660906, -45.09797443818218 -19.61103048187596, -45.09741476814342 -19.60965534049143, -45.09819592431463 -19.608280375044963, -45.09785972523386 -19.60584686912979, -45.09741152012991 -19.604260198290742, -45.09889438158414 -19.599561003966024, -45.103360344192176 -19.59556861846533, -45.10274388900367 -19.59485503975714))) |
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_-5401 |
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 |
2.794 |
the_geom |
MULTIPOLYGON (((-42.52139187776536 -19.553828065340745, -42.521714492876335 -19.5546596943513, -42.52248842226221 -19.555132685100745, -42.52441922522199 -19.5564550678142, -42.52507293679019 -19.558314397861427, -42.52473675574097 -19.56117789356523, -42.52341602473443 -19.564629307867097, -42.5231520247268 -19.567192165662863, -42.5230997496966 -19.57061221927239, -42.52259102924419 -19.57434839138263, -42.522337491858565 -19.576161852140668, -42.52187220877627 -19.577118112794746, -42.52073877991643 -19.577530577521173, -42.51916694074551 -19.57708090914217, -42.51783069031087 -19.575993304869918, -42.51639258051534 -19.574155660245, -42.513827663292396 -19.57230247557988, -42.511351527160244 -19.57205429857779, -42.50875382051785 -19.572339915591538, -42.50558400064737 -19.573151280941566, -42.50173456112401 -19.57416719379561, -42.49699719899463 -19.574315516546747, -42.49529560332201 -19.57493304618811, -42.49506749792945 -19.575143897716405, -42.49356847484819 -19.577261461178708, -42.4912707540499 -19.580009954175633, -42.49033390046808 -19.582241862101974, -42.48950207308181 -19.585010725179547, -42.48913902787008 -19.587285831670833, -42.4905997113397 -19.58746782035404, -42.493049462406454 -19.58709283975452, -42.49371025213282 -19.586137586504478, -42.494043161710614 -19.58555885338109, -42.494146518796576 -19.585221651242165, -42.49438200950019 -19.584657817331923, -42.495263066120856 -19.583443737110727, -42.49686962299614 -19.58183065045431, -42.49876172952354 -19.58035696446769, -42.49970407423967 -19.580106349029908, -42.50165012434417 -19.57957976462724, -42.50497326708225 -19.578534910519554, -42.5078543788495 -19.578165680833, -42.510885590483426 -19.577390298587293, -42.51261066683755 -19.57741410669259, -42.51519457938432 -19.5777224579404, -42.51633804689824 -19.578147295699633, -42.51805479556338 -19.578715477628705, -42.52035107219843 -19.57901979755805, -42.5217968460313 -19.578494233287334, -42.523678279239455 -19.577702821537905, -42.52470805862793 -19.576216988436382, -42.52487062918721 -19.574992871307, -42.525311595104675 -19.574317116979703, -42.52562840178378 -19.57241330778028, -42.525932708209425 -19.57132749433668, -42.52610568114103 -19.56942080634336, -42.52697809960352 -19.56875186615764, -42.52758668404659 -19.56657932649364, -42.528199406928124 -19.564134116023396, -42.527938770467465 -19.562358745183193, -42.52724044527356 -19.56098555816014, -42.52653890972231 -19.559885951750022, -42.52569470417699 -19.558647122395307, -42.52548094812615 -19.55792174557544, -42.52555839760616 -19.55734123895888, -42.52570644548596 -19.556566639908578, -42.525341530699706 -19.55588344023698, -42.52470325803836 -19.555259704826305, -42.52385674399215 -19.554860680711283, -42.523282105999634 -19.554562011329438, -42.522570334647405 -19.55426055480877, -42.52192515421242 -19.554090050052558, -42.52139187776536 -19.553828065340745))) |
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_-5400 |
Folha |
SE23 |
Legenda_Completa |
521Dt12 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos da Bacia do Alto Rio Paraná |
Identificacao_Unidade |
521 |
Nome_Unidade |
Planalto do Triângulo Mineiro |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
muito baixa |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto do Triângulo Mineiro |
Area_Poligono_Km2 |
1.79 |
the_geom |
MULTIPOLYGON (((-48.00045180454873 -19.53197930318154, -48.00029731715698 -19.532227747274124, -47.999308883471286 -19.533817330135086, -47.99861816267037 -19.535497084116592, -47.99849533723966 -19.53596133203247, -47.998108663688036 -19.53760624523221, -47.99788272155346 -19.53939563767374, -47.997908131020395 -19.54025553694403, -47.9979710032116 -19.541029955434993, -47.997996974750976 -19.541559438555172, -47.99800412885848 -19.54194659961239, -47.99784687697765 -19.543742976055103, -47.99779790386134 -19.54397850448723, -47.99761407176213 -19.544800352112688, -47.99751960717754 -19.54494455551115, -47.996681049635946 -19.546562668200238, -47.99619904660147 -19.54830666099444, -47.99608507637612 -19.54986940961785, -47.99612379376353 -19.551964954210167, -47.993672016335196 -19.55337783229388, -47.9921531211006 -19.55446285991892, -47.9917626747685 -19.554824116937205, -47.991604614458026 -19.55498020600774, -47.989919046125586 -19.559628444765114, -47.99061708488665 -19.56045282280285, -47.991948410825174 -19.56173973569224, -47.99352416470659 -19.562749948243717, -47.99527980217783 -19.56344390270849, -47.99714619751058 -19.56379205011811, -47.998211660120454 -19.563831213315723, -47.998261167581724 -19.56383039025509, -48.0004514863195 -19.563824656049402, -48.00045180454873 -19.53197930318154))) |
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PWG РPowering Growth ̩ um projeto para facilitar o |
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