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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_-5ed2 |
Folha |
SE23 |
Legenda_Completa |
514Aptf |
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 |
Aptf |
Categoria |
PlanÃcie e terraço fluviais |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie e terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais do Rio São Francisco |
Area_Poligono_Km2 |
0.565 |
the_geom |
MULTIPOLYGON (((-44.52475317894416 -17.894625691311845, -44.52392186317299 -17.895898993498523, -44.52350924869266 -17.896985315892703, -44.523505055288666 -17.898556196651057, -44.52422445113119 -17.900672060268167, -44.5247547261257 -17.9029085753887, -44.52566616100919 -17.904179802942707, -44.52645206531826 -17.905087373514146, -44.52827914768652 -17.90605892873809, -44.530232136463766 -17.906908751334147, -44.53199759021968 -17.907275447994977, -44.53511783590658 -17.90800781325255, -44.53650456818922 -17.908434122428087, -44.538457934992465 -17.909163652424525, -44.53978111678364 -17.909710903789925, -44.541452907864226 -17.909805235000476, -44.542208149676284 -17.910561728294695, -44.54283603072155 -17.911651440445784, -44.54497938400097 -17.912320794232954, -44.54678141732624 -17.91318817720029, -44.54895496910115 -17.91424982942453, -44.55112862000421 -17.915282534762635, -44.552546187281 -17.91625201690651, -44.55326811402323 -17.917522682929793, -44.555062924054305 -17.9186737832666, -44.55739681649179 -17.91870983827224, -44.559069974569866 -17.918290635296415, -44.56011230158121 -17.91753827877959, -44.56210932851238 -17.916334333853914, -44.563562040998306 -17.915703093780444, -44.564778605891355 -17.91511289174812, -44.56477955003569 -17.91511289386011, -44.56413008040147 -17.91506986279504, -44.56310662836531 -17.91506756737639, -44.56225952279141 -17.915150625507987, -44.56096719702551 -17.915446888761974, -44.5594963135626 -17.916169357234367, -44.558692625695805 -17.91663663498107, -44.55797893605612 -17.91736080765666, -44.557532870789714 -17.917530621600243, -44.55677533848331 -17.91765724412353, -44.55579498403731 -17.91778335502536, -44.55463766175299 -17.917694843168608, -44.554148390335875 -17.91739545158663, -44.553792033579924 -17.917181325701417, -44.553392355339405 -17.916923714875747, -44.553081319715744 -17.91670969174681, -44.55276934069452 -17.91649566596215, -44.55254832281425 -17.916153502042167, -44.55245895087787 -17.916024949616617, -44.55210401077483 -17.9156246306246, -44.551882693905874 -17.91502667539154, -44.551705109961866 -17.914684610559824, -44.551577579668056 -17.914337237821748, -44.551411911505255 -17.91413800867963, -44.55103964623786 -17.913871417828545, -44.550505802950724 -17.91365687646219, -44.550105190984716 -17.913400160736227, -44.54970574112459 -17.91305758103129, -44.54926140633044 -17.912544068693155, -44.54863820194625 -17.912200968428206, -44.54828302388679 -17.911900969554647, -44.54792741173148 -17.911772700748912, -44.54748254406502 -17.911472492066718, -44.54712758515204 -17.911087529638593, -44.54659375508455 -17.91087297776968, -44.54602707543195 -17.91058242434618, -44.5455084900096 -17.91031457789878, -44.54505860755366 -17.91013275654986, -44.54446942646483 -17.910152166925894, -44.54384554749865 -17.910448976390082, -44.54328022051648 -17.910369919320495, -44.54291058318329 -17.91019099290482, -44.54193168933789 -17.909761169957882, -44.541346578660004 -17.90966669530096, -44.54065993050277 -17.909406574621826, -44.54006956259723 -17.90915481375998, -44.5391878522355 -17.908753226218554, -44.538149665506666 -17.908258166906435, -44.53721717396653 -17.90814658603367, -44.536244071294725 -17.907677883104927, -44.53512437003646 -17.907311864239237, -44.533878887136815 -17.906668959707776, -44.53307779711173 -17.906496212028703, -44.532108674941966 -17.906677366424198, -44.531295618879945 -17.906747718289797, -44.530227464353715 -17.90653183472156, -44.5292487536974 -17.90605223757152, -44.52867104031247 -17.905666703462575, -44.528226672826555 -17.905195625179058, -44.527649076916035 -17.90476760745922, -44.52724897367372 -17.904339115335866, -44.52680438553153 -17.903953899067883, -44.52636074339192 -17.903568684111278, -44.52600524317506 -17.90305533614689, -44.52556183088022 -17.902585158113702, -44.525251160640934 -17.9019010904697, -44.52476452050146 -17.90100328436823, -44.524454424315635 -17.900105908333355, -44.524367503699175 -17.899422385614788, -44.524324951733625 -17.898739875064976, -44.524505787837946 -17.897835562989457, -44.52459725566846 -17.896811724269618, -44.524645565487596 -17.89675038039543, -44.52475317894416 -17.894625691311845))) |
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_-5ed1 |
Folha |
SE23 |
Legenda_Completa |
549Da52 |
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 |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
14.272 |
the_geom |
MULTIPOLYGON (((-46.29283778236553 -17.87611126230951, -46.29075050408809 -17.87511296355446, -46.28765731996952 -17.87661999399352, -46.285729055252595 -17.878306360302417, -46.28456314388752 -17.878127888302092, -46.28126572246172 -17.878149594810097, -46.28049701670805 -17.879269803896626, -46.27661993752237 -17.87966756277086, -46.27490451187223 -17.883954169610362, -46.271468516987035 -17.891969800867177, -46.279057331703996 -17.894895063046462, -46.281228691329275 -17.90008604789088, -46.277412388854884 -17.909034174480862, -46.28191123888689 -17.914023681109693, -46.28694981895386 -17.91306052119837, -46.291024723928736 -17.91303352406757, -46.30153572099893 -17.917424977379664, -46.30368214208338 -17.92139855392693, -46.30445249858582 -17.922307914474572, -46.303702205715794 -17.924141094586066, -46.30333059083661 -17.9256057432147, -46.303916966408174 -17.927429959920786, -46.30487763975858 -17.92815459284046, -46.30602767015606 -17.928695404967055, -46.306593975729605 -17.927777978502448, -46.30658726895939 -17.926863498557893, -46.306960197452476 -17.925581379987875, -46.30771851187399 -17.924845203665374, -46.308284797547756 -17.923927773274322, -46.309619714244036 -17.92355279690151, -46.310767034295544 -17.923727609990188, -46.31172906249041 -17.924635646657844, -46.313065728360066 -17.92462662502265, -46.31345342614585 -17.925355082929872, -46.31364949926689 -17.92608483459005, -46.31366163242187 -17.92773035171247, -46.314058778986535 -17.92973835255379, -46.3140668718924 -17.930835363407766, -46.31407631212478 -17.932114908032073, -46.315030297754596 -17.931925009710895, -46.31558980991508 -17.930093083314844, -46.31595727725401 -17.928079912710817, -46.31594242624936 -17.92606932943179, -46.31498307074242 -17.9255272871902, -46.31439794491953 -17.923886548111756, -46.314772158129784 -17.922786952243676, -46.315531774479346 -17.92223328208226, -46.316295033058225 -17.92204557432418, -46.31706679584878 -17.9231365106938, -46.31711236211943 -17.92342628274341, -46.318424264218514 -17.92160280753357, -46.31912379619592 -17.920458526303563, -46.320205095680976 -17.91834923535388, -46.32070700834105 -17.917163817791952, -46.32105714415159 -17.91613395883844, -46.32138569821163 -17.911810340770632, -46.321271486094815 -17.911811116396645, -46.31947859590136 -17.910873517257716, -46.31886990018639 -17.90897901497798, -46.31846129455783 -17.907462699443176, -46.31865343217086 -17.906511630916878, -46.31963982226766 -17.90574495109781, -46.31963280342498 -17.904796135802506, -46.31962858564375 -17.904225942946262, -46.31962015723554 -17.903086460763774, -46.31960751913939 -17.901377689049887, -46.31880953583359 -17.90081377869505, -46.31800314138065 -17.899110381314795, -46.3164156088848 -17.899121122196664, -46.31562278605672 -17.899126481408214, -46.314230656124124 -17.898755434179062, -46.313630452484915 -17.898000392527628, -46.31283249554905 -17.89743555162337, -46.312234148922464 -17.897060038826375, -46.31182936637477 -17.89592322342719, -46.311816808245254 -17.89421444509035, -46.311804251516044 -17.892505666445317, -46.311790295335584 -17.890606219911046, -46.310600171700536 -17.890614231942315, -46.30883122019336 -17.892905216591732, -46.308454307950605 -17.89556638535056, -46.308469617391765 -17.89765469388487, -46.308884133278774 -17.90012076880614, -46.30889945853785 -17.902209979641686, -46.308716567226924 -17.904299619220907, -46.307131763447394 -17.904689815433148, -46.30554511825139 -17.904700464556388, -46.303759315202264 -17.904712434901562, -46.30296413365256 -17.904527986158495, -46.30216202817593 -17.9033947119673, -46.300964889499014 -17.902452944389342, -46.30075698845353 -17.901125013413125, -46.30035226630446 -17.899988170474547, -46.30033566049481 -17.897709187350976, -46.30092336053242 -17.896756392026383, -46.30111464155836 -17.89580534079206, -46.30210383255146 -17.89541918082138, -46.30209828886537 -17.894659218801593, -46.30189455102272 -17.89390148551461, -46.30050619956854 -17.893910762242974, -46.299717977716135 -17.894675120647786, -46.297749258406135 -17.896777573372983, -46.295766702064086 -17.89698055127769, -46.29437832328129 -17.896989785859486, -46.29337121502599 -17.89490715285042, -46.2937538608868 -17.893005963451596, -46.29374422811601 -17.89167670286501, -46.29453108247225 -17.89072169873095, -46.29531931173807 -17.88995736071777, -46.296897556112064 -17.888807309110017, -46.29688652425538 -17.887288284470962, -46.29609237052906 -17.88710379559715, -46.29470312493737 -17.887113033852092, -46.29410303574531 -17.886357019615275, -46.294096160659656 -17.885408192730708, -46.29487515899157 -17.883503464320047, -46.29644603303373 -17.881214821092065, -46.296435010013575 -17.8796957949972, -46.295039882040555 -17.878755294906664, -46.29324471010706 -17.877437889477854, -46.29283778236553 -17.87611126230951))) |
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_-5ed0 |
Folha |
SE23 |
Legenda_Completa |
524DEa33 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
DEa |
Categoria |
Estrututral aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo aguçado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
14.573 |
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_-5ecf |
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 |
6.435 |
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_-5ece |
Folha |
SE23 |
Legenda_Completa |
523Dc31 |
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 |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
132.494 |
the_geom |
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