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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_-5ab0 |
Folha |
SE23 |
Legenda_Completa |
554Dt32 |
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 |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
20.383 |
the_geom |
MULTIPOLYGON (((-47.76147639344948 -17.713582633804076, -47.76091570165037 -17.714439369050883, -47.76068627039077 -17.717977964428222, -47.760503783794356 -17.720397946426395, -47.76030842515837 -17.72197738715223, -47.75922085792992 -17.722518245547445, -47.75682941806839 -17.723813392242825, -47.75553517615023 -17.725197861104988, -47.753894467218885 -17.725431301781192, -47.752466831023916 -17.725240925596808, -47.75188484986456 -17.72304206690202, -47.753050555204936 -17.720396979075865, -47.752813410366535 -17.719244418849872, -47.75072667726408 -17.718958513881265, -47.748713975438065 -17.716358866170335, -47.74502390477221 -17.71157471234704, -47.74344714818282 -17.708758485373483, -47.74287972769654 -17.70750485988006, -47.74258037556477 -17.7022533259588, -47.74130855914591 -17.697856091456703, -47.73942626534967 -17.696621690890808, -47.734357274738855 -17.69479950137342, -47.73050994324954 -17.694012254382898, -47.728428269644986 -17.69404116596023, -47.726603217328645 -17.6965896289261, -47.72500868906403 -17.699869970364716, -47.724281584961744 -17.702507944736368, -47.722664782812345 -17.704317507886337, -47.72071443824102 -17.70581651505663, -47.72051712854605 -17.70729032830261, -47.72089028263899 -17.710229124287146, -47.72324718341377 -17.713875499829243, -47.72472489181133 -17.717323628224385, -47.72639644404465 -17.71919231503644, -47.72741300288352 -17.721175743354586, -47.72678722869144 -17.72328674414002, -47.725620446150444 -17.725826082486734, -47.72554201026444 -17.72792947864291, -47.72646205799565 -17.730754987740657, -47.72691287038428 -17.73158946268004, -47.7281283419848 -17.73220289186424, -47.7290022953314 -17.731981227521853, -47.73017701657646 -17.729967335591198, -47.732481805670666 -17.7301456571783, -47.73184969758069 -17.73183593686578, -47.731106703680396 -17.733423006077324, -47.7302518795713 -17.734906876936112, -47.73114495358922 -17.73594559149747, -47.73256948535865 -17.735925748673623, -47.734524786286116 -17.73474169309894, -47.73594612283184 -17.73451236482164, -47.738050608353916 -17.735954056782496, -47.73753038091983 -17.73774844422551, -47.73580258193151 -17.739454929773096, -47.735379497544464 -17.740511977338265, -47.73431358750688 -17.742491873012593, -47.734231431662174 -17.744280147117628, -47.73533359399435 -17.74468559111965, -47.73761778209945 -17.743496906950757, -47.74012533190689 -17.74262114302107, -47.740808580925204 -17.744293960050605, -47.73886281156403 -17.746107373181864, -47.737028861476105 -17.748025769299154, -47.73759386454782 -17.74917377471747, -47.739138324401964 -17.749782519884775, -47.74046166113139 -17.7502895908043, -47.741683726611164 -17.7513245415094, -47.743864115596686 -17.750558048257936, -47.74483137847059 -17.74928295784125, -47.74713960434175 -17.749670530658587, -47.746842871013726 -17.751777864822863, -47.74621245776353 -17.75357290949959, -47.746013781831586 -17.754942893482202, -47.74646890965999 -17.755987650409676, -47.74832529655208 -17.7555408042695, -47.74990761157272 -17.754551451738884, -47.75038836210003 -17.754250314611614, -47.750827442012394 -17.75424415094697, -47.752034171166 -17.75433286122075, -47.75322836557122 -17.751816487762195, -47.756788246859955 -17.749256916163066, -47.7592369308478 -17.748909106564636, -47.76072548342683 -17.749986228536127, -47.76401366445152 -17.751037963170155, -47.76599073532849 -17.751951021573614, -47.76698362426026 -17.752720830578127, -47.76750347226876 -17.75459629614058, -47.76769396315743 -17.75631928539695, -47.76868688504715 -17.757089081108486, -47.770796589754184 -17.755961179892928, -47.77126332998392 -17.754386028877967, -47.774692869375905 -17.754024145634265, -47.77580714541499 -17.751969345250302, -47.77577085112784 -17.749616589699926, -47.77410861711424 -17.74791445190365, -47.77521467850921 -17.74538930036261, -47.775178406306196 -17.74303654205005, -47.772878364546585 -17.742441486419608, -47.76960574699485 -17.74233152171309, -47.767960519182445 -17.741727153626687, -47.76773631346433 -17.737808478504878, -47.76887377089754 -17.737321945199444, -47.772325667013185 -17.738371252090346, -47.77263326477022 -17.737111701560565, -47.77159364945434 -17.73336169222726, -47.770073850556884 -17.730246054001242, -47.76855169708803 -17.726973303346437, -47.76684643736971 -17.72244880992932, -47.76431156714479 -17.71715124179123, -47.76263536080198 -17.714508190184002, -47.76147639344948 -17.713582633804076))) |
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_-5aaf |
Folha |
SE23 |
Legenda_Completa |
548Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
548 |
Nome_Unidade |
Chapadas do Alto Rio São Francisco |
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 |
Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
57.895 |
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_-5aae |
Folha |
SE23 |
Legenda_Completa |
553Dt41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Chapadões Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
553 |
Nome_Unidade |
Chapadas de Cristalina |
Letra_Simbolo |
Dt |
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Homogênea tabular |
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dissecação |
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dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Chapadas de Cristalina |
Area_Poligono_Km2 |
7.379 |
the_geom |
MULTIPOLYGON (((-47.86967382726855 -17.754011484694153, -47.870278854472325 -17.75454530102956, -47.87293031436509 -17.756884830432373, -47.87314773456939 -17.75828393459437, -47.87491247025044 -17.758911783496057, -47.87394629826362 -17.75948669721931, -47.87347561755303 -17.76052116745847, -47.87465380513119 -17.761064615331605, -47.87642755535596 -17.762253951834804, -47.877038598675696 -17.763926277857816, -47.87550414378079 -17.765444108425758, -47.87377219933519 -17.766871824133457, -47.874475254074824 -17.768168984566888, -47.876231138496756 -17.76823710606151, -47.87730840533507 -17.76859510106046, -47.87645756946852 -17.77019589954419, -47.87559981180302 -17.771423877433197, -47.874555955835476 -17.77321441811483, -47.874933154010186 -17.774700560358887, -47.875075994884114 -17.775263712027364, -47.87566311779674 -17.77514402348095, -47.880572414093905 -17.774146309692522, -47.881677461200184 -17.770650974985585, -47.88280701606606 -17.768685778657872, -47.88425671373522 -17.7685253739342, -47.88540186388916 -17.76753421959024, -47.88784933005486 -17.766244847037328, -47.89131690690678 -17.7652193992265, -47.89279696665622 -17.7670070403967, -47.8940925671146 -17.766291726091154, -47.89477099046724 -17.763358872163206, -47.89284131265451 -17.760743565021905, -47.89109126366225 -17.760212287167672, -47.89074964229146 -17.757016386336282, -47.8923523193986 -17.757409891055154, -47.89586898444715 -17.75944554047602, -47.89731634215526 -17.759146031378155, -47.899304964012074 -17.756471895058464, -47.90071414880421 -17.75380722783684, -47.90110900608591 -17.75129572466543, -47.89787590195836 -17.74883790052891, -47.89491962488774 -17.74554160219987, -47.893984277639404 -17.74151925125278, -47.891416489493956 -17.73529339701019, -47.88919706870718 -17.732681371038844, -47.88788698988759 -17.73242255650334, -47.88717725843599 -17.733407288072563, -47.8863358314152 -17.735229185288297, -47.88551573958645 -17.738442213855887, -47.88439305134104 -17.740825367331475, -47.88294451567537 -17.74098572738527, -47.88104421610766 -17.74017842957059, -47.87871760991842 -17.739934493669406, -47.87714400285221 -17.741349046581146, -47.87630817941837 -17.743588903977443, -47.87647622992225 -17.744375621798362, -47.87694044039547 -17.745002684343167, -47.87781917762997 -17.74574194689461, -47.8789406221516 -17.746160702772205, -47.879318435916346 -17.74651091702431, -47.87995258377966 -17.74745150753226, -47.879973488768265 -17.74875777413863, -47.879389358957376 -17.750943378723687, -47.87784354536276 -17.75239185171624, -47.87653281263958 -17.753044069562474, -47.8753328487607 -17.75290366468074, -47.87417717048726 -17.752880889954575, -47.87306136847713 -17.752817793521007, -47.87223702729207 -17.75294906929462, -47.87092816626589 -17.753720415784304, -47.87026819563029 -17.753877267205702, -47.86967382726855 -17.754011484694153))) |
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_-5aad |
Folha |
SE23 |
Legenda_Completa |
556Dc51 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
556 |
Nome_Unidade |
Planalto Dissecado do Sul - sudeste Goiano |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
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dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Sul - sudeste Goiano |
Area_Poligono_Km2 |
22.357 |
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_-5aac |
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 |
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aplanamento |
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degradado inumado |
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pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
2.442 |
the_geom |
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