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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_-56c7 |
Folha |
SE23 |
Legenda_Completa |
524DEc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
5.319 |
the_geom |
MULTIPOLYGON (((-44.441386715555446 -17.743744792547965, -44.44320336591924 -17.743749956643878, -44.445761064464286 -17.746009605022127, -44.44715045258148 -17.746013525528884, -44.44875364338019 -17.74612017273213, -44.44907434429153 -17.746121073655985, -44.451533356040315 -17.745821557173084, -44.45132329647998 -17.74448959060763, -44.45345848106836 -17.74521230816689, -44.4535650775293 -17.745519916069075, -44.453134052411144 -17.74643974391267, -44.45430530852814 -17.748081695952216, -44.45569471462581 -17.748085556381103, -44.457514187230935 -17.747169567549264, -44.4575151127949 -17.746862259035442, -44.45912137438726 -17.7456374498973, -44.460939606484715 -17.745437279117375, -44.46029114819333 -17.747790946160375, -44.46029145424605 -17.747688811232553, -44.45740081482422 -17.74942166305255, -44.45696856171129 -17.750751846306194, -44.45750184822408 -17.751265808344122, -44.458784076562445 -17.7514736224104, -44.4607061732006 -17.75188836407953, -44.46187873256299 -17.752813518252864, -44.46262677584855 -17.753122880585497, -44.46476515502147 -17.752821417462982, -44.466157027948746 -17.75200631725978, -44.46487844152732 -17.75056841220534, -44.46680391226332 -17.750164209102692, -44.467123373176506 -17.75026811701406, -44.46840228008064 -17.75160296902489, -44.468720575669245 -17.7524227259833, -44.470646661993776 -17.75181331156674, -44.47097365068811 -17.74935660563008, -44.47161656999355 -17.74884585139358, -44.470767998552624 -17.746795422243693, -44.47077311315232 -17.74505460591667, -44.47003235687201 -17.742595016568316, -44.46929101830069 -17.740339694659564, -44.46811876420902 -17.739005137778207, -44.46619769526184 -17.738283162208067, -44.46577464289914 -17.73654118054795, -44.46363889611536 -17.73602377188772, -44.46139536157324 -17.7359145881305, -44.46086578178254 -17.734172304386004, -44.459589528845484 -17.73232582908964, -44.457231738616855 -17.73446960057985, -44.4571245415379 -17.73467447970471, -44.45370022946465 -17.736098495489294, -44.45273631331411 -17.73671043249746, -44.45167079543037 -17.73568338918295, -44.453491404400516 -17.734357086154084, -44.45413679650609 -17.73302750084239, -44.454458404395936 -17.732721083529974, -44.45670528940624 -17.73170324471586, -44.45809734087 -17.73078515760719, -44.460452315658756 -17.729562397155767, -44.45789096172736 -17.72853127050219, -44.45607600338814 -17.72801466742444, -44.4527624283169 -17.728107595843298, -44.45158727062292 -17.7281043169768, -44.45137255267327 -17.728308892673855, -44.45094499694661 -17.728409833344735, -44.449127871997796 -17.728609918908862, -44.448058346603354 -17.728914226429534, -44.44666940628161 -17.72880727725659, -44.44452781662382 -17.7302356495671, -44.44367111250424 -17.73064267046369, -44.44243007408969 -17.730894036977137, -44.44174294335538 -17.732275887047788, -44.44184856947283 -17.732583498270348, -44.44206108482601 -17.733095684612692, -44.442059182521184 -17.733710300892096, -44.44173564883761 -17.734631313412883, -44.441305544391426 -17.735243807297046, -44.44162082964542 -17.73698643331911, -44.44225839678913 -17.738216585284068, -44.44217414841319 -17.739228663371126, -44.442103610319634 -17.740077182554803, -44.44182826685846 -17.740357498362847, -44.44021688144739 -17.74169242043232, -44.441386715555446 -17.743744792547965))) |
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_-56c6 |
Folha |
SE23 |
Legenda_Completa |
549Dc51 |
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 |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
51.43 |
the_geom |
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-45.755294005763545 -17.583696249808547, -45.76090969797534 -17.58282420765138, -45.76090318050032 -17.581266014557038, -45.761131271489845 -17.58037485549049, -45.761363094002654 -17.58015071495319, -45.7552668629283 -17.577157975205775))) |
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_-56c5 |
Folha |
SE23 |
Legenda_Completa |
556Dc53 |
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 |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Sul - sudeste Goiano |
Area_Poligono_Km2 |
24.901 |
the_geom |
MULTIPOLYGON (((-47.82045249698185 -17.849551691371346, -47.821817190875066 -17.84646451434655, -47.82364473543102 -17.844509295978444, -47.82639463417616 -17.842094632131317, -47.82836964077752 -17.83969207515881, -47.82907903513786 -17.835600321012116, -47.827835742540664 -17.830424392224334, -47.82670556314614 -17.82751148665221, -47.82396975650891 -17.82584443731316, -47.82018043283995 -17.826121340465868, -47.818129314106855 -17.828599858449067, -47.81586981237251 -17.832639023336583, -47.81381157071597 -17.834672440144004, -47.81281652995665 -17.83542904149554, -47.80993192745327 -17.834135068892003, -47.80556665628026 -17.832268165301773, -47.80460705267087 -17.830353155947368, -47.801799856262434 -17.829057029516743, -47.79659869623297 -17.828167199733624, -47.79254537703806 -17.831416433687046, -47.7889542993663 -17.834510000074893, -47.787653411537626 -17.835492995590258, -47.79047429885123 -17.83500388987173, -47.79246762067778 -17.835861226305912, -47.79684625596955 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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_-56c4 |
Folha |
SE23 |
Legenda_Completa |
423Pge |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Chapadões Residuais das Altas Bacias do Tocantins-Paranaiba |
Identificacao_Unidade |
423 |
Nome_Unidade |
Chapadões Residuais do Alto Tocantins - ParanaÃba |
Letra_Simbolo |
Pge |
Categoria |
Pediplano degradado etchplanado |
Natureza |
aplanamento |
Caracteristica |
degradado etchplanado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões Residuais do Alto Tocantins - ParanaÃba |
Area_Poligono_Km2 |
0.959 |
the_geom |
MULTIPOLYGON (((-48.00044627276944 -16.973752191090377, -48.000446037351566 -16.95328515012549, -47.9981751794039 -16.956150120877254, -47.99615889246511 -16.961286714424602, -47.99573774780189 -16.96478272058359, -47.99745388760202 -16.97081793892659, -47.997667187180326 -16.972160413962094, -47.99819614520337 -16.975489594421337, -47.99727371310005 -16.977431817293333, -47.99672152813621 -16.97763238739378, -47.99490319901065 -16.978292858937337, -47.994451434613964 -16.97986066289695, -47.995715426241084 -16.981403238751216, -47.99677650934381 -16.982040649459964, -47.99714705170584 -16.97975563406946, -47.99779518361525 -16.978608938388586, -47.99899173498201 -16.977013535623563, -47.99904159106526 -16.976165978060262, -47.998792309335315 -16.97581698384108, -47.998842165532764 -16.97536827688965, -47.99963986633452 -16.97392244321006, -48.00044627276944 -16.973752191090377))) |
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_-56c3 |
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 |
1433.781 |
the_geom |
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