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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_-548c |
Folha |
SE23 |
Legenda_Completa |
521DEc51 |
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 |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto do Triângulo Mineiro |
Area_Poligono_Km2 |
135.469 |
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_-548b |
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 |
0.945 |
the_geom |
MULTIPOLYGON (((-44.995610970952995 -19.991825297803025, -44.99372015863022 -19.991514377980323, -44.99100629896036 -19.991281113875043, -44.9895263637778 -19.99376883945714, -44.98668092361715 -20.000487440389715, -45.00364287327653 -20.00048790345439, -45.003850298000714 -19.999546274456055, -45.00204158893186 -19.99907910685898, -45.000972817313226 -19.999779460597573, -44.9987530439578 -19.999546311893948, -44.9971078451453 -19.99775792857658, -44.99727327098378 -19.99519150608094, -44.995610970952995 -19.991825297803025))) |
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_-548a |
Folha |
SE23 |
Legenda_Completa |
528Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
528 |
Nome_Unidade |
Depressão Interplanáltica do Médio Rio Doce |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Depressão Interplanáltica do Médio Rio Doce |
Area_Poligono_Km2 |
13.436 |
the_geom |
MULTIPOLYGON (((-42.17528382228089 -19.00615440609086, -42.174210516861436 -19.005759902627272, -42.17218105661987 -19.005759903129043, -42.17015159637825 -19.005759903630764, -42.16848027621181 -19.005879284056096, -42.16657019611477 -19.006356804576484, -42.165376396102886 -19.006834324919787, -42.16370507574078 -19.006237425272477, -42.162153135197286 -19.004924245523394, -42.160243054774064 -19.0042079659229, -42.15845235456063 -19.004207966365456, -42.155825994247394 -19.00420796701423, -42.15308025408283 -19.00480486775308, -42.15105079361268 -19.00396920816975, -42.147708153148564 -19.003730448971268, -42.143887992594784 -19.00337230987846, -42.13935155241122 -19.004685491131905, -42.1382771326085 -19.00587929151831, -42.13744147296463 -19.007550611894185, -42.13636705329224 -19.009221932329055, -42.13505387355876 -19.01077387281072, -42.133024413316 -19.01077387331208, -42.13135309305085 -19.01053511370051, -42.129204252924026 -19.011012634279595, -42.12765231303134 -19.012087054771836, -42.125980992896366 -19.012325815208843, -42.124190292486496 -19.011609535578316, -42.12262942538715 -19.01017367832933, -42.12218451418253 -19.011378085551446, -42.12149858820456 -19.01367151172128, -42.12147391133943 -19.01609622171221, -42.121880812882566 -19.016942226127252, -42.12297247400482 -19.018706276624417, -42.12447795707389 -19.02008943691212, -42.12628071876526 -19.021962053281843, -42.12870067397023 -19.02355262751392, -42.13037634899524 -19.024925755727203, -42.13110325452471 -19.02543904644691, -42.13258299533504 -19.027776088863302, -42.13346335949386 -19.029581958503925, -42.13385181781399 -19.03172869743187, -42.13551587261821 -19.033952117386708, -42.13763224834888 -19.037316551261107, -42.13764704763145 -19.037339352621128, -42.13936125355847 -19.039024511133242, -42.13950037216841 -19.039161195874268, -42.13970393520242 -19.039249221335716, -42.1398047831245 -19.03929231664661, -42.141215239093455 -19.03870382858864, -42.14223629488375 -19.038456003356508, -42.143808091573426 -19.038480336669643, -42.14625176301269 -19.038430561872893, -42.14700018134259 -19.037913949475772, -42.14784010040301 -19.037487229771973, -42.14866949928804 -19.03767610735552, -42.1500607128609 -19.03743395516935, -42.15089912897541 -19.037094776588294, -42.151765101829625 -19.03508478440787, -42.15280807495961 -19.033605702113633, -42.15392510605866 -19.03318322437141, -42.15652931397263 -19.032343948527917, -42.15830316341092 -19.031315789653696, -42.15878579670889 -19.030179260834025, -42.15954759289247 -19.02887186488775, -42.15975061632152 -19.027819512736958, -42.16013457393601 -19.026510814061858, -42.16071391615793 -19.025547312803088, -42.16183984979185 -19.024596725011495, -42.16323393594959 -19.024178438840853, -42.16417925025561 -19.022961415252848, -42.16559367205001 -19.02139945747895, -42.16672103559412 -19.020361274495986, -42.16776432780482 -19.018793601283168, -42.16843541954459 -19.01739718188969, -42.1697656725818 -19.01530660076558, -42.17115818444255 -19.014975799869504, -42.1722646374404 -19.015168803856863, -42.17375610534368 -19.014487367328893, -42.1744330787767 -19.01273887772913, -42.17575579040699 -19.011087836077962, -42.17579144421463 -19.008977403621873, -42.17618140575354 -19.007751808623134, -42.17528382228089 -19.00615440609086))) |
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_-547e |
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 |
4.64 |
the_geom |
MULTIPOLYGON (((-42.08731536615256 -18.988015011968546, -42.08569023152807 -18.988330442700708, -42.084496431270956 -18.98791261295192, -42.08354139115629 -18.98791261318705, -42.082466970767534 -18.98695757335415, -42.081332860501426 -18.986480053584682, -42.07978092023379 -18.98618160393622, -42.0785274299696 -18.985763774202006, -42.07745301013262 -18.98683819457637, -42.076975490432325 -18.98815137482818, -42.07655766070682 -18.989345175053035, -42.076915801107006 -18.99065835509916, -42.0773336314495 -18.991732775106076, -42.0773336318879 -18.993344405270776, -42.07763208247595 -18.995373865404733, -42.07697549294914 -18.997403325773824, -42.07608014313381 -18.998477746104115, -42.074707273196054 -18.99931340652768, -42.07273750318636 -19.000149067098345, -42.07052897280685 -18.99973123759947, -42.06676850198055 -18.99835836838522, -42.065037491577165 -18.997642088738008, -42.063664621411824 -18.99764208907598, -42.06336617173299 -18.998955269283968, -42.063366172025326 -19.000029689393976, -42.06408245230647 -19.000745969290843, -42.06503749263265 -19.001521939135106, -42.0659328428542 -19.001939768957353, -42.066649123330265 -19.00337232892755, -42.06712664358275 -19.00408860888324, -42.06808168374649 -19.004267678666434, -42.068678583867126 -19.004446748537603, -42.069454554188056 -19.00528240843187, -42.07094680433536 -19.00516302805217, -42.07184215431314 -19.0046855077828, -42.07279719433066 -19.00432736751091, -42.073513474546886 -19.00480488738316, -42.07512510508215 -19.006058377114194, -42.07542355523186 -19.00647620708327, -42.076318905518434 -19.00713279692989, -42.076975495629924 -19.007252176780156, -42.077572395701786 -19.007252176633227, -42.07793053569617 -19.007073106526715, -42.07858712558013 -19.006356826291555, -42.07966154567694 -19.006237446014627, -42.081153795742736 -19.005819615604405, -42.08222821588826 -19.00587930534553, -42.08395922637276 -19.006894035022448, -42.08843597687859 -19.006774653906778, -42.08909256703878 -19.007073103775376, -42.08927163712534 -19.007311863755618, -42.08945070734195 -19.0080281437845, -42.08992822764328 -19.00892349375813, -42.09100264795137 -19.009580083560174, -42.092256138199524 -19.009938223287524, -42.093330558491374 -19.01053512308352, -42.093987148863 -19.011609543031213, -42.09404683932564 -19.013280863186814, -42.09404684213437 -19.013280864591177, -42.094285599386886 -19.01340024314008, -42.0951212594711 -19.013340552927993, -42.0968477443988 -19.012163403490423, -42.09559120058065 -19.010709170111035, -42.095134971040764 -19.00850446490073, -42.09486610846865 -19.00496739210128, -42.09507831138665 -19.000838388316517, -42.095115743349474 -19.00010405741079, -42.094988101226264 -18.998764029227164, -42.094869551127715 -18.998540065411046, -42.09383024823262 -18.99657267469922, -42.091498655664196 -18.993818440050617, -42.08931938552438 -18.991369035278403, -42.08792123043409 -18.989685788302353, -42.08731536766564 -18.98801501614093, -42.08731536615256 -18.988015011968546))) |
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_-547d |
Folha |
SE23 |
Legenda_Completa |
529Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Mantiqueira Setentrional |
Identificacao_Unidade |
529 |
Nome_Unidade |
Serranias da Zona da Mata Mineira |
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 |
Serranias da Zona da Mata Mineira |
Area_Poligono_Km2 |
70.667 |
the_geom |
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