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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_-5839 |
Folha |
SE23 |
Legenda_Completa |
027Dr |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos Cimeiros |
Identificacao_Unidade |
27 |
Nome_Unidade |
Planalto dos Geraizinhos |
Letra_Simbolo |
Dr |
Categoria |
Em ravinas |
Natureza |
dissecação |
Caracteristica |
dissecação |
Forma |
em ravina |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto dos Geraizinhos |
Area_Poligono_Km2 |
7.173 |
the_geom |
MULTIPOLYGON (((-42.3629854338996 -16.03391152485715, -42.36195085835007 -16.03673039902728, -42.363361000159486 -16.038731231361048, -42.36331923296654 -16.041905548372707, -42.362066588056635 -16.043477091592525, -42.36283522522667 -16.047454412965788, -42.36342285185163 -16.049644737431322, -42.365855890955366 -16.05185686714712, -42.366440955644094 -16.05424496356737, -42.36701466631347 -16.05742595157603, -42.368815037461715 -16.06101944230712, -42.37270293389026 -16.06335417631958, -42.37358704636998 -16.062893543499438, -42.374465903542465 -16.06290432750195, -42.37485506717551 -16.0630030374128, -42.37533516775054 -16.063575250997495, -42.376010172508586 -16.064243789769193, -42.3763993280122 -16.064343400442834, -42.37678972728098 -16.064348186523727, -42.37698492696492 -16.064350579297816, -42.37747865028415 -16.063884240925585, -42.37787645782574 -16.063323693066295, -42.37807289925507 -16.06323126065286, -42.37924285050712 -16.06334043078323, -42.38022008782705 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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_-5838 |
Folha |
SE23 |
Legenda_Completa |
130Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
130 |
Nome_Unidade |
Serras do Espinhaço Central |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Central |
Area_Poligono_Km2 |
5.265 |
the_geom |
MULTIPOLYGON (((-43.469703878447 -17.031606051032192, -43.47061459690088 -17.03027454616897, -43.47070143346494 -17.029645330465893, -43.47226774858016 -17.028318746685162, -43.473251204892726 -17.028090271455525, -43.47563176512875 -17.027242399854984, -43.476943025835965 -17.027015459496, -43.47883041607001 -17.02639971653547, -43.48030064330164 -17.026726097055526, -43.48153208362767 -17.026262666810695, -43.481051950881415 -17.024999337556647, -43.480730500912316 -17.02420982266257, -43.48049170778794 -17.02342092497231, -43.48049933716812 -17.022475722558223, -43.47984848906105 -17.02199913314592, -43.47829182561179 -17.02214473465252, -43.47788325315613 -17.02214167744145, -43.477475648909774 -17.02190276390409, -43.476173355108536 -17.021026374226903, -43.47585193161817 -17.020236853509108, -43.474137898686116 -17.019751374495314, -43.473154178492166 -17.019902138357786, -43.472259503136414 -17.019265551001755, -43.47406447508035 -17.018727849191368, -43.475373759663036 -17.018737666095934, -43.477730977125894 -17.02064493275203, -43.47903137848584 -17.02175625787508, -43.48067737330511 -17.020666961774904, -43.48264323479007 -17.02044486905171, -43.482483608713 -17.01997195174458, -43.48093966184393 -17.018543441571516, -43.48291564900461 -17.01706167493895, -43.482440592500474 -17.015169417860225, -43.478936619062615 -17.01325363755648, -43.476320673622986 -17.012918678922553, -43.473773051760354 -17.014237949010383, -43.47213345868961 -17.014541031027473, -43.46935664929599 -17.013890291505362, -43.468628638560844 -17.01286093720821, -43.46937519671421 -17.01160771858641, -43.47182258226979 -17.012570465198316, -43.47387261908995 -17.01203460034773, -43.473387798464245 -17.011243851499557, -43.473968353857444 -17.01030385135498, -43.47335684697249 -17.00892023681419, -43.471596110260336 -17.010268879568613, -43.47102320751145 -17.01026457626741, -43.47053009196175 -17.010497637044168, -43.46971462303923 -17.01017612015299, -43.47045669464603 -17.00947320778041, -43.46964284514745 -17.00883721998621, -43.46964603778125 -17.00844414011675, -43.47014745363172 -17.007188169465678, -43.470069582966325 -17.006714955693546, -43.469579037377436 -17.006632647317772, -43.46900742364253 -17.006471107299145, -43.46801895874251 -17.007329402216648, -43.46553902500611 -17.007375787425268, -43.4647280004937 -17.009508695017974, -43.46373920263314 -17.0102883431943, -43.46323965929597 -17.01130844640662, -43.463143176253155 -17.013118701498612, -43.46256127621043 -17.01421589676334, -43.45960821494191 -17.0151388146129, -43.45723743122466 -17.014805466929435, -43.45404860912276 -17.014466782150972, -43.45308301681172 -17.012412606328375, -43.45103812146059 -17.012317527222915, -43.4498845366924 -17.01325399202959, -43.448153141760905 -17.01489362398292, -43.450032052456116 -17.01530195017674, -43.45158189810678 -17.015864995835496, -43.44969196085595 -17.016794948484442, -43.44886742822058 -17.017575768094837, -43.44689964057895 -17.018033378708576, -43.44663473663773 -17.020314046893915, -43.447768253003225 -17.021819191280706, -43.44841836235111 -17.022374491841905, -43.450141046515526 -17.021915905922196, -43.450876758856815 -17.022000130855506, -43.45235142502812 -17.021774593122338, -43.454733911325185 -17.02069112093922, -43.45504619693887 -17.022583089762918, -43.45454205181802 -17.024153471026537, -43.4545330003361 -17.025255892336872, -43.45591435170371 -17.026446592699227, -43.45738323631916 -17.026930366549998, -43.45835602970996 -17.028118855965303, -43.45983395721139 -17.02750018995959, -43.46105514168833 -17.028296543629743, -43.4621219123069 -17.02798922975856, -43.46188418394183 -17.026964462658043, -43.4631233722333 -17.02555685697198, -43.46427504692126 -17.02485706950629, -43.46558822062555 -17.024394355016714, -43.46631369051717 -17.025738184217754, -43.46737274343507 -17.026376037144413, -43.468017156471944 -17.02764062993882, -43.468008829308516 -17.028663538487322, -43.468324456134845 -17.030162418598767, -43.4686423616863 -17.031266405275936, -43.469703878447 -17.031606051032192))) |
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_-5837 |
Folha |
SE23 |
Legenda_Completa |
069Pgu |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
69 |
Nome_Unidade |
Planalto de Cristalina |
Letra_Simbolo |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto de Cristalina |
Area_Poligono_Km2 |
5.675 |
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_-5836 |
Folha |
SE23 |
Legenda_Completa |
069Dt32 |
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 |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto de Cristalina |
Area_Poligono_Km2 |
49.762 |
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_-5835 |
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 |
80.202 |
the_geom |
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