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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_-5980 |
Folha |
SE23 |
Legenda_Completa |
195Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
195 |
Nome_Unidade |
Maciços de Pedra Azul |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Maciços de Pedra Azul |
Area_Poligono_Km2 |
0.821 |
the_geom |
MULTIPOLYGON (((-42.127943412824024 -16.426091633132614, -42.12828205762884 -16.426096269531598, -42.1287900250404 -16.426103223108033, -42.129297992697225 -16.426110175458405, -42.13014579949703 -16.42604050196776, -42.13040292241838 -16.425798390403457, -42.130915675824426 -16.425479403560697, -42.13095498508449 -16.425414921679955, -42.13126272421777 -16.424911616808817, -42.131354101219706 -16.424423413728892, -42.13093846332694 -16.423927374181954, -42.130603414129666 -16.42367806559551, -42.130180580246375 -16.423672281918382, -42.1296738252894 -16.423583171837087, -42.12925005648541 -16.423577373519723, -42.12874209542871 -16.423570422094194, -42.12815113636696 -16.42348105905807, -42.12764438365168 -16.423391944290852, -42.1275661896548 -16.422982696575485, -42.12748346409274 -16.42281811248209, -42.12732133756885 -16.422326441380346, -42.127326141569945 -16.421999604272255, -42.12733213978303 -16.421591509303436, -42.127336943538936 -16.421264672169457, -42.127428068054726 -16.42085774260593, -42.12735014667118 -16.420366321423995, -42.12718323118292 -16.42020058476342, -42.12710144220348 -16.420036013526108, -42.12667768204394 -16.420030211233907, -42.12634145069952 -16.419862155463417, -42.12609273536565 -16.41953274959023, -42.12592582170783 -16.419367012198453, -42.12594023763448 -16.418386501769064, -42.12577332494161 -16.418220764415732, -42.12543709747466 -16.418052707785403, -42.1252713804003 -16.417805712408523, -42.12485096457558 -16.417636501738347, -42.124427210453796 -16.417630695728917, -42.12408858145505 -16.417626055434983, -42.12382907352137 -16.418030675132353, -42.12339663561704 -16.418678551941543, -42.12339063031886 -16.419086645607866, -42.1231349800207 -16.419165317902973, -42.12254284309427 -16.419157199061317, -42.12220661781437 -16.418989137445347, -42.12212509451699 -16.418743294666633, -42.12187640154723 -16.41841298225004, -42.12162530323295 -16.41824608745811, -42.12154379415104 -16.41799934174257, -42.12154739675085 -16.417754666490833, -42.12146921617414 -16.417345418690616, -42.12121838058907 -16.4170972533912, -42.120879753472146 -16.41709260807037, -42.12028401997744 -16.417329158861506, -42.12002958182089 -16.417325667325695, -42.11961037047339 -16.417075189685594, -42.11936289446625 -16.41666271507559, -42.11902787409548 -16.416413392144072, -42.118775845650866 -16.41624648186348, -42.11869888188871 -16.41575507386166, -42.11870850121851 -16.415102307056124, -42.118716922763184 -16.4145307974916, -42.1187241466655 -16.41404054518283, -42.118647444847674 -16.413467867100888, -42.1180601442431 -16.41313290363469, -42.117552215315506 -16.41312592944701, -42.11712940910298 -16.41312012311159, -42.11661666149499 -16.41343998097576, -42.116350193167285 -16.41425266845257, -42.116257563814365 -16.414823923031364, -42.116335733025096 -16.415233170966985, -42.1164196579972 -16.415315597593537, -42.11683404123996 -16.41589291468661, -42.11699371431909 -16.416548909141316, -42.11690229618226 -16.41703800402803, -42.116292373325386 -16.418172872173596, -42.11611101884209 -16.418986727573568, -42.11627069015539 -16.41964272242662, -42.116517898460906 -16.420136470089577, -42.116596068462314 -16.42054571817218, -42.117012608084984 -16.42104088939507, -42.117433021267296 -16.421210115830473, -42.11785584507503 -16.42121592433334, -42.11819447842451 -16.42122057566344, -42.11861702676838 -16.421308555568352, -42.11903383582525 -16.421722453715738, -42.119283462129424 -16.422052782165242, -42.11961875346518 -16.42222083602466, -42.120042515731825 -16.42222665331411, -42.12038115148524 -16.422231301395716, -42.12055408752852 -16.4219880474338, -42.12098171538313 -16.421667917489216, -42.121577201264536 -16.421512637037157, -42.121830709758456 -16.421516114729947, -42.12225233944441 -16.421603171968822, -42.12258856889656 -16.42177123419488, -42.122917581948805 -16.422429549729095, -42.123250211870435 -16.422842286699854, -42.123325730356136 -16.42349622292467, -42.12340390192304 -16.42390637369197, -42.12390826039375 -16.424158013788997, -42.123986446538886 -16.424567261690225, -42.12457832709019 -16.424657552371293, -42.12508628910726 -16.424664514317417, -42.12559545992351 -16.424589314472307, -42.12602069753578 -16.424431689367246, -42.12652865961194 -16.42443864773089, -42.12686730113244 -16.42444328595858, -42.12711481485148 -16.424854852648494, -42.12744265323826 -16.4255944219719, -42.12769229932071 -16.42592474333353, -42.127943412824024 -16.426091633132614))) |
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_-597f |
Folha |
SE23 |
Legenda_Completa |
512Pgi |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
512 |
Nome_Unidade |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Area_Poligono_Km2 |
9.467 |
the_geom |
MULTIPOLYGON (((-45.597230190276896 -16.45364560763866, -45.5954176108598 -16.4530451084289, -45.594932415890106 -16.455825269606976, -45.59477477259897 -16.45788946513019, -45.595109631885876 -16.459873617370874, -45.59272580216055 -16.460277213520435, -45.59181942818975 -16.459803386604374, -45.59009081034116 -16.459411421360432, -45.58927024022959 -16.46004921691006, -45.58976728075309 -16.46115878991647, -45.59174469828451 -16.46234463853043, -45.592322750505524 -16.4629775872877, -45.59248958288336 -16.463929892589803, -45.59295330875914 -16.464548699191273, -45.591887578313276 -16.465901329514267, -45.59024612492378 -16.466779189238565, -45.58860132163453 -16.466862462204308, -45.58564567243176 -16.46842827568668, -45.58534971951609 -16.468144354440504, -45.58535656539593 -16.47042503520011, -45.58535913254059 -16.471280177361677, -45.58182376947538 -16.47357072956932, -45.58065005166509 -16.476140340317624, -45.58213420143568 -16.478701666698484, -45.5847937295128 -16.479549402955957, -45.587454140819744 -16.48068275426315, -45.58723550045916 -16.48429831223235, -45.58725566301879 -16.48446006484296, -45.58882128607984 -16.48540844126499, -45.59055061639739 -16.48595950446472, -45.5904700951903 -16.486595216510878, -45.588994101746934 -16.488027635377097, -45.58932776416155 -16.489614955829918, -45.59138044903879 -16.48833909855761, -45.5936833845521 -16.48833257680763, -45.59433770552281 -16.4872188475568, -45.596641563460096 -16.48721229101962, -45.5992796905848 -16.489269396570503, -45.59969270648884 -16.489823244459163, -45.600682180464815 -16.49045588950264, -45.59928775211808 -16.49188904884457, -45.596987210189546 -16.492689303527293, -45.59658003105668 -16.494040077294223, -45.59682839459723 -16.494674852496207, -45.597492670407796 -16.49649895431424, -45.59814831698072 -16.496730301698957, -45.598735492279225 -16.496937436113544, -45.59955646925059 -16.49669734285973, -45.60350478931599 -16.49668598657875, -45.60679536597711 -16.496676465172257, -45.610577781711584 -16.49634816751444, -45.61057280332405 -16.494760832255913, -45.61418670038867 -16.49300380582902, -45.61829983485998 -16.492991688531312, -45.620102475915054 -16.49092171539203, -45.620751517445484 -16.487903286679305, -45.619429102729555 -16.486001663968644, -45.617945780634706 -16.485053278270684, -45.616459527989775 -16.48347031170701, -45.61645048500348 -16.480612022969527, -45.61430853653791 -16.47934825836767, -45.61069439095833 -16.48094618530342, -45.60806523922869 -16.482065709490275, -45.608383176981086 -16.478570982680203, -45.609525589666816 -16.47539204988194, -45.6081939616889 -16.47047385993385, -45.603080576491216 -16.465883868752087, -45.60011787045959 -16.4654159891974, -45.599666661220475 -16.463696137768512, -45.59857229699738 -16.462722084110307, -45.60021241423191 -16.461129130743487, -45.59971116743741 -16.458669980518177, -45.59904648707308 -16.45636948879463, -45.59879549068163 -16.45486149210338, -45.59755838651104 -16.453754051870504, -45.597230190276896 -16.45364560763866))) |
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_-597e |
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 |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
2.682 |
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_-597d |
Folha |
SE23 |
Legenda_Completa |
510Dc21 |
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 |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Jequitaà - Verde Grande |
Area_Poligono_Km2 |
40.905 |
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_-597c |
Folha |
SE23 |
Legenda_Completa |
195Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
195 |
Nome_Unidade |
Maciços de Pedra Azul |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Maciços de Pedra Azul |
Area_Poligono_Km2 |
0.737 |
the_geom |
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