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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.
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FID |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-5aba |
Folha |
SE23 |
Legenda_Completa |
294Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Formas Agradacionais Atuais e Subatuais Interioranas |
Identificacao_Unidade |
294 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais |
Area_Poligono_Km2 |
12.032 |
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_-5ab9 |
Folha |
SE23 |
Legenda_Completa |
554Da52 |
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 |
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 Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
10.173 |
the_geom |
MULTIPOLYGON (((-47.806640143648806 -17.10283923820613, -47.803622817663246 -17.102953293357025, -47.802102607934394 -17.103650724970326, -47.800988352455114 -17.10449333865204, -47.79938062427268 -17.10474043896481, -47.79792072587572 -17.104009286059654, -47.79646213766876 -17.103428009480893, -47.79588423106599 -17.10245889005934, -47.79691309007852 -17.101241813461435, -47.79544780042379 -17.10020999560612, -47.79488018461724 -17.09999206887616, -47.79359769168661 -17.100385439071708, -47.79191467319225 -17.100935135671538, -47.790631047942824 -17.10125355068231, -47.789058759746155 -17.101925417921173, -47.78783194069317 -17.1027803529651, -47.78785735315135 -17.104486780696572, -47.78788292990904 -17.106204042562467, -47.78792556441644 -17.10906614494276, -47.78798210480346 -17.112860912086624, -47.78801085810051 -17.114790346966927, -47.78436021857966 -17.117673516904468, -47.7798573440175 -17.118956386455693, -47.77716793782043 -17.124794603967835, -47.777172469209994 -17.12901906674262, -47.778578404101964 -17.13204848245628, -47.77756463864874 -17.13714213596387, -47.77636741903807 -17.139437916329967, -47.77381693508412 -17.13934651627755, -47.77169714059338 -17.13865676563619, -47.771111138592204 -17.137649757475074, -47.768682732041796 -17.13692175870573, -47.766705087449694 -17.13694884403825, -47.76605839822409 -17.137803871963694, -47.76665594648696 -17.139528679330972, -47.766933918632596 -17.140539921244784, -47.76603240961178 -17.141947505478278, -47.7661285166707 -17.142538602369164, -47.76613164604657 -17.14274987746643, -47.77083044243994 -17.150192665060626, -47.77531270604523 -17.153091352266177, -47.780469583818146 -17.15107521807936, -47.78533268136412 -17.146941740488224, -47.789041396744516 -17.13999033047768, -47.791022218127715 -17.134958260235038, -47.79398324489011 -17.130728092860004, -47.79430046593733 -17.12769758376889, -47.796372615382886 -17.120686550100814, -47.79837146807951 -17.116819137982464, -47.801596032939166 -17.1140978726613, -47.804233296104215 -17.11254873397561, -47.80687049856646 -17.11099866422049, -47.809897221097046 -17.11118964135256, -47.81267589331647 -17.110497234560533, -47.81254110956422 -17.10965205580585, -47.81337876109226 -17.106216083004966, -47.80980052271788 -17.10487420105532, -47.806640143648806 -17.10283923820613))) |
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_-5ab8 |
Folha |
SE23 |
Legenda_Completa |
069Dt21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
69 |
Nome_Unidade |
Planalto de Cristalina |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto de Cristalina |
Area_Poligono_Km2 |
3.45 |
the_geom |
MULTIPOLYGON (((-47.17276786089755 -17.27262951385859, -47.17361942085136 -17.272520922344718, -47.174573493699775 -17.272013724112252, -47.17467272505894 -17.271415506636142, -47.17465873448824 -17.27022317964813, -47.174974886522335 -17.269921635514287, -47.17539121692636 -17.269022766523864, -47.1756013456055 -17.268820840109694, -47.177089618255 -17.26840721667939, -47.178040384686625 -17.267701294629333, -47.17878801740486 -17.26779255697044, -47.179117006945376 -17.268583970954296, -47.17976332079686 -17.2691740969001, -47.179984912712605 -17.2698673016899, -47.18009816121984 -17.270462309577887, -47.180113366464134 -17.271754895696574, -47.18191543861778 -17.27084005992257, -47.181900232300805 -17.269548378516973, -47.18146990073813 -17.26925493585961, -47.1812412785135 -17.26796466891392, -47.18091228174541 -17.267173259268596, -47.180478222797724 -17.266482362469063, -47.18046675944742 -17.265507728793448, -47.1805566218046 -17.26411462855291, -47.18054026279137 -17.26272358483769, -47.18105693040681 -17.261325850572078, -47.18188738802874 -17.2594287464596, -47.182525478428694 -17.259322442122215, -47.183795566297896 -17.258512753545208, -47.18432414219947 -17.258208888744427, -47.18603295993542 -17.258488420097642, -47.1869798947997 -17.257385014822997, -47.18684694558106 -17.255199359948577, -47.18639883752119 -17.253315251640398, -47.18768200765409 -17.253699680184447, -47.18822087852936 -17.254190675859803, -47.18896493926705 -17.253983826601043, -47.189696088023275 -17.25268311417267, -47.18935560072904 -17.250997490352677, -47.188394415420895 -17.250809213747146, -47.187977949913204 -17.251608729340735, -47.18681179999272 -17.252217658367098, -47.18680126087833 -17.25132341868845, -47.18689787622589 -17.25042710959874, -47.18700175862637 -17.250227233787427, -47.1870948707738 -17.24903374804621, -47.18761286367339 -17.24783473519487, -47.187919356963036 -17.246638927078823, -47.1871624441198 -17.245752809455936, -47.187261630396314 -17.245154590489427, -47.18736762096186 -17.245054064538227, -47.18756601285224 -17.243859433096645, -47.18755898790177 -17.243263273126633, -47.18786312522915 -17.241867842153145, -47.1874328554307 -17.241574405320552, -47.18690221935926 -17.24177892298652, -47.18530539567213 -17.241895657336006, -47.18456137603466 -17.242102488230213, -47.18392217686999 -17.242109432114287, -47.18276285833671 -17.243216027537546, -47.18383723461219 -17.243999344037604, -47.183949071335554 -17.24439562089659, -47.183109346065194 -17.245498747291695, -47.18194064869925 -17.245809554609032, -47.18097387373002 -17.24522290378814, -47.18107519832979 -17.244724939113475, -47.181065859072106 -17.24393005575957, -47.18051769115803 -17.24264324787442, -47.17986915546117 -17.241855294966506, -47.17922085161719 -17.24116671004589, -47.17910996745945 -17.24077041888632, -47.178146509681945 -17.240383364591324, -47.17781896894531 -17.239789769102696, -47.176850859313895 -17.239005264703334, -47.17569500345015 -17.24040990466167, -47.17561790179418 -17.242895977409034, -47.17689980757959 -17.24318022190285, -47.17817566169432 -17.242868283845386, -47.178607314549055 -17.243360473161328, -47.17861780904286 -17.24425471844911, -47.17863180267937 -17.24544704536635, -47.17853725275691 -17.246442705498236, -47.17823396968032 -17.247837217090407, -47.17792975383106 -17.249232642024808, -47.17729985344043 -17.25003445254622, -47.17581849989714 -17.250945758171962, -47.17537307056745 -17.249359703101526, -47.17346935037812 -17.250572779942235, -47.1729549704613 -17.252169220900697, -47.17265280383258 -17.253663090003148, -47.17266910518856 -17.255055045571083, -47.17270519360769 -17.258136135320466, -47.17272615602836 -17.259925533502653, -47.17286266715807 -17.26250866851389, -47.172899939919276 -17.26568911633308, -47.17304206700624 -17.26866968177911, -47.17338155820781 -17.27051886762426, -47.17179258420103 -17.271247936531246, -47.172016490464834 -17.272140777845028, -47.17276786089755 -17.27262951385859))) |
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_-5ab7 |
Folha |
SE23 |
Legenda_Completa |
510Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
510 |
Nome_Unidade |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
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 |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
Area_Poligono_Km2 |
14.402 |
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_-5ab6 |
Folha |
SE23 |
Legenda_Completa |
549Dc32 |
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 |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
16.437 |
the_geom |
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