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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_-5f53 |
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 |
2.749 |
the_geom |
MULTIPOLYGON (((-42.41645621588207 -19.394865217582865, -42.416853947368665 -19.395410872642888, -42.41817408827542 -19.395818833395953, -42.41821353520217 -19.395851902320754, -42.41858542453973 -19.396226517952634, -42.42441102710343 -19.4038033091696, -42.42616265008753 -19.41011854139134, -42.428895529642794 -19.416078333375864, -42.42908623708505 -19.416358260097155, -42.429785535225605 -19.42145665790545, -42.43164129914065 -19.427404008562565, -42.43300992651275 -19.433344458024347, -42.4335724426674 -19.434739451196247, -42.43364336759453 -19.44263914160793, -42.43443357830553 -19.448201166488722, -42.43452338634128 -19.448664781804226, -42.434655931951546 -19.452645347276114, -42.43508068570657 -19.45662914484011, -42.43774551165771 -19.460737643696334, -42.44198361409372 -19.464034850218496, -42.444402912747535 -19.46517970914523, -42.45201546597529 -19.464639471037675, -42.45435084320737 -19.46384874243063, -42.456251668483155 -19.46320539525884, -42.45400418142223 -19.462941748161434, -42.451864218846126 -19.462804203527273, -42.44895119010052 -19.46169403073066, -42.446483397605036 -19.460910662753935, -42.44480971344994 -19.45981789089014, -42.44314610538123 -19.45808410336297, -42.44225817246065 -19.45721550985958, -42.44069518162668 -19.456231727620622, -42.44037408884059 -19.45515711526405, -42.43973019854411 -19.45311713100644, -42.43918521973967 -19.451932798787617, -42.43841299378589 -19.45085271361251, -42.43763741637271 -19.449986593949408, -42.43720812884946 -19.448589877960888, -42.43711933936722 -19.447091419105103, -42.437243401232294 -19.446344570878235, -42.437487424174634 -19.445172290243598, -42.43738854869653 -19.44431573449763, -42.43695591134763 -19.44313298688075, -42.43686376012077 -19.441848495511074, -42.437101068621025 -19.441103247348437, -42.43666171768957 -19.440348435521113, -42.436566206983215 -19.439277911919294, -42.43669193392869 -19.43842453058037, -42.43670704779207 -19.437462126530797, -42.436604815913775 -19.436819538597, -42.435944978590584 -19.43574013552689, -42.435847784053735 -19.434777047217228, -42.43586626034033 -19.43360067558059, -42.43566757411351 -19.431887550434567, -42.43489041669003 -19.431127961789098, -42.4336698676756 -19.429934068975342, -42.43267390611525 -19.428744250560975, -42.43257506947667 -19.42788679199672, -42.43258850986388 -19.42703182507713, -42.43262211482399 -19.42489395597854, -42.43218618367917 -19.423925171977906, -42.431980099646175 -19.42274562477859, -42.431887027510385 -19.421461120604725, -42.432017067637894 -19.42039378819289, -42.43202546806063 -19.419859320820734, -42.43125005457523 -19.41899319183744, -42.430476338578515 -19.41801962534678, -42.43003706896177 -19.41726480633041, -42.42937995390364 -19.416079775371337, -42.42906233545182 -19.414792091886877, -42.42885363598462 -19.41371996546915, -42.429094288009864 -19.41276075803429, -42.43012447473881 -19.411706170138807, -42.43025619921882 -19.41053140326187, -42.430276365354246 -19.409248501333273, -42.42983711516848 -19.408493683983526, -42.428722302610815 -19.40772930223163, -42.42772577104047 -19.40664601926809, -42.426945393164104 -19.406100379641824, -42.425314452195096 -19.40233517293501, -42.42466152909758 -19.400828718951104, -42.424007890327765 -19.399428809184307, -42.423241025850416 -19.398028195210227, -42.420786125057404 -19.396496166071675, -42.41645621588207 -19.394865217582865))) |
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_-5f52 |
Folha |
SE23 |
Legenda_Completa |
523Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
116.871 |
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_-5f51 |
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 |
2.062 |
the_geom |
MULTIPOLYGON (((-45.429089838784584 -18.241999480405116, -45.42787388897154 -18.241807878388187, -45.427368073812 -18.242293456538555, -45.427268046458465 -18.242778128670007, -45.42737328422912 -18.244425562565315, -45.4269693832741 -18.24520194311988, -45.42534808993789 -18.245205550559806, -45.42311975661907 -18.245308099164472, -45.421294155960766 -18.244924383451334, -45.41916680138762 -18.244929050987018, -45.41734398662034 -18.245707608218257, -45.41643466367647 -18.246776099165047, -45.41572706617366 -18.247553116950066, -45.415730292102914 -18.24890974871288, -45.41583498977284 -18.24997603273139, -45.416648662604345 -18.251234193255975, -45.418879169106084 -18.252004806542356, -45.420702272330175 -18.251322038700433, -45.42171725122655 -18.252095285545003, -45.42151692130433 -18.25296791524845, -45.419190504383906 -18.25481410928322, -45.419194224719796 -18.256365060172385, -45.420006322839384 -18.256945341532862, -45.4222315290758 -18.255486196713957, -45.42263289715619 -18.253644225508292, -45.4237479392549 -18.253931887668138, -45.42526998319492 -18.254703991915683, -45.42648223565644 -18.252956919192364, -45.428812351934226 -18.2526606840175, -45.431549002260084 -18.253042274604077, -45.43205866997328 -18.254107634203155, -45.43165620411208 -18.25546517764607, -45.43003624892292 -18.256050884397805, -45.428924988388715 -18.257313304379316, -45.42933105695939 -18.257796842176983, -45.43004268843928 -18.25866743198498, -45.43024823171622 -18.259926896388986, -45.430603934089795 -18.260313835570468, -45.430959638043504 -18.260700774042714, -45.43298594486496 -18.26030846158351, -45.433990677873034 -18.256914147263807, -45.43439216252284 -18.255167958650528, -45.43397912369976 -18.25226130310243, -45.43346704745263 -18.250227057458552, -45.43336126816234 -18.248386212436973, -45.43386203285125 -18.245865223708865, -45.43315019669677 -18.244897937837628, -45.43122431427499 -18.24451454385073, -45.43010575009349 -18.243159517762688, -45.429089838784584 -18.241999480405116))) |
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_-5f50 |
Folha |
SE23 |
Legenda_Completa |
566Pgi |
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 |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados do Planalto de Cristalina |
Area_Poligono_Km2 |
6.552 |
the_geom |
MULTIPOLYGON (((-47.04015956469273 -18.25975107991466, -47.043085955482105 -18.259425350726456, -47.04429981357163 -18.257792630911872, -47.04520466303147 -18.256015054494032, -47.0439502546749 -18.254261453128127, -47.04300500963935 -18.252504540987836, -47.044215382440285 -18.25057736120376, -47.04450383370106 -18.24880637190013, -47.043871020979545 -18.24748787551209, -47.042771730836634 -18.2457326023649, -47.04304033140085 -18.242342972356525, -47.044091385890276 -18.239974842411208, -47.044063847287795 -18.237619126870413, -47.043565469406396 -18.23453218138186, -47.04416208572811 -18.232758807414008, -47.04583549593204 -18.230825782511374, -47.04581311343788 -18.22891176394695, -47.045178658645895 -18.227446030889947, -47.04238625605492 -18.226003306890956, -47.038989618494526 -18.22559772588931, -47.03666901556564 -18.224886147364717, -47.03405987618911 -18.225944619929937, -47.03131201123315 -18.228329795432362, -47.02885609713315 -18.22923932759081, -47.02652941101396 -18.22808593521816, -47.02514007767163 -18.227953372415374, -47.021765526335294 -18.22946153289444, -47.02178084004344 -18.23078664249557, -47.02333620612059 -18.231949143428697, -47.024117771630806 -18.232824400009722, -47.02414162593232 -18.234885677798534, -47.02308935671395 -18.23725282960607, -47.02141901347633 -18.239479250486703, -47.021595241476746 -18.241392572604557, -47.01991803873711 -18.24303004780073, -47.02040583420793 -18.24523368521704, -47.02119085815166 -18.24640341666758, -47.02257863593038 -18.246388759771474, -47.02459472034179 -18.247398212609532, -47.027061153483885 -18.247372111525536, -47.02906624996607 -18.2473508691331, -47.031378583191305 -18.247326345742092, -47.03385280401779 -18.24788907945356, -47.035252585529406 -18.248904959855274, -47.03573202846247 -18.25037327558083, -47.03439566177617 -18.254805017964674, -47.03395222313992 -18.25642949393769, -47.033974522395596 -18.258344424465264, -47.03491457258767 -18.259659687854697, -47.03784441630016 -18.259628503091275, -47.04015956469273 -18.25975107991466))) |
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_-5f4f |
Folha |
SE23 |
Legenda_Completa |
523Dc41 |
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 |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
71.008 |
the_geom |
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