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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_-542f |
Folha |
SE23 |
Legenda_Completa |
554Dt21 |
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 |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
21.458 |
the_geom |
MULTIPOLYGON (((-47.95261477148108 -16.18037320850086, -47.95231821291118 -16.180308747838737, -47.94704424924734 -16.18155470547947, -47.94551043330009 -16.18288775218922, -47.94203901464579 -16.18657227378514, -47.9399036590455 -16.189986987453306, -47.94152065780536 -16.18980444424615, -47.94275766301669 -16.190353504964545, -47.9434097844065 -16.190909758132396, -47.94342238963068 -16.191759318982907, -47.94255681594381 -16.192563252548833, -47.9414054229721 -16.193881344538376, -47.93949431301321 -16.19526683733616, -47.938626930589734 -16.196013894355556, -47.93782261800807 -16.19704452667365, -47.93760905654872 -16.198462508028786, -47.9376375613764 -16.200386442410235, -47.93795275748162 -16.201853998535835, -47.93963779433636 -16.204944272912464, -47.940425469762246 -16.205122094669697, -47.94121315951363 -16.205300816092326, -47.94355937753528 -16.205268297375234, -47.94947634877701 -16.20497035374145, -47.955978714476366 -16.206391543255574, -47.957265439361656 -16.210262854073743, -47.95629227614908 -16.212437298480598, -47.95566260392242 -16.21514695282889, -47.95718241920965 -16.21966336175239, -47.96362929662276 -16.224835154430128, -47.96667322024601 -16.226629284815115, -47.967481268940055 -16.2283463090755, -47.96661126751549 -16.229978456803813, -47.966863764888075 -16.231919973732015, -47.968687081185394 -16.23427112484227, -47.97039761060893 -16.236515475104934, -47.969585170777236 -16.239055239280148, -47.97106538487975 -16.240337506088846, -47.971643351162044 -16.24141569863139, -47.97417354528191 -16.242404184650916, -47.97683124199504 -16.240746898916786, -47.97972757207593 -16.24016620089799, -47.98166162385703 -16.24240728817477, -47.982500841754934 -16.24617626471213, -47.98322307879139 -16.249623612446054, -47.98535849241984 -16.25045767255065, -47.98636336786033 -16.250335146137413, -47.98993801962999 -16.250284704888248, -47.993102872871304 -16.25261662621786, -48.00044409383906 -16.256533647453125, -48.00044438061566 -16.245348554772907, -48.00044402796095 -16.234113799186314, -47.99677673461614 -16.234012177690875, -47.996745897167536 -16.231976408144753, -47.99517686492517 -16.230820202023317, -47.99417170366229 -16.230298937004783, -47.993594889306216 -16.228807239806795, -47.991699032344485 -16.227977075099155, -47.989927071239585 -16.22810862214255, -47.98624404715805 -16.22633921503191, -47.9836868268211 -16.225839744659403, -47.98032432728674 -16.22331623105239, -47.980513533928054 -16.22117078711226, -47.9809299680185 -16.21934361316578, -47.98101764061981 -16.217841619168098, -47.980878369585774 -16.215915701645443, -47.98129546677384 -16.214195071508673, -47.98216123977797 -16.212790502229627, -47.982591235540355 -16.211927526242917, -47.983234717429 -16.210470997139733, -47.98387728424118 -16.209016286213153, -47.984848433369415 -16.207288768186977, -47.987373796393435 -16.205753388720794, -47.98776984576696 -16.20264065483256, -47.984621113160294 -16.199577772793656, -47.98081625036514 -16.197060412174448, -47.9802251832424 -16.19460445417985, -47.980173680006644 -16.19117653248304, -47.97703811386507 -16.18897024228301, -47.975062047146224 -16.19017632366286, -47.97344332417555 -16.193092171732857, -47.97083085786863 -16.196235925664507, -47.96897067423624 -16.197761811628215, -47.967321342386406 -16.19864180594404, -47.966098175948794 -16.198337426288585, -47.964420006459854 -16.19728990197971, -47.962838618515896 -16.195275704989534, -47.95588121244899 -16.187185998913144, -47.95240217592402 -16.184234572835805, -47.95147667073289 -16.1815691048081, -47.95261477148108 -16.18037320850086))) |
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_-542e |
Folha |
SE23 |
Legenda_Completa |
523Dt32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
523 |
Nome_Unidade |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
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 Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
239.692 |
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_-542d |
Folha |
SE23 |
Legenda_Completa |
561Dt31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
561 |
Nome_Unidade |
Depressão Interplanáltica do Rio Corumbá |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão Interplanáltica do Rio Corumbá |
Area_Poligono_Km2 |
0.064 |
the_geom |
MULTIPOLYGON (((-48.00044519324591 -16.494135751545834, -47.99936656414416 -16.495243254984597, -47.99940956829608 -16.49804703149778, -48.000445001200355 -16.501690518575924, -48.00044519324591 -16.494135751545834))) |
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_-542c |
Folha |
SE23 |
Legenda_Completa |
531Dt31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
531 |
Nome_Unidade |
Serra da Saudade |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serra da Saudade |
Area_Poligono_Km2 |
187.208 |
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_-542a |
Folha |
SE23 |
Legenda_Completa |
526Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos da Canastra |
Identificacao_Unidade |
526 |
Nome_Unidade |
Serras e Patamares da Canastra |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras e Patamares da Canastra |
Area_Poligono_Km2 |
2.04 |
the_geom |
MULTIPOLYGON (((-46.28224274405627 -19.75009772446339, -46.28319432617275 -19.749639147690228, -46.28454647864809 -19.74962945271159, -46.285740227274275 -19.749620885007758, -46.285780131464385 -19.749598914014115, -46.2863682398401 -19.749274844316634, -46.28648086051934 -19.74868132679109, -46.286602631736024 -19.748038953426448, -46.28779334526073 -19.747653627113504, -46.288827722539075 -19.747646185559923, -46.289220793757984 -19.74704070939983, -46.28928909600282 -19.745683132979234, -46.28943937197778 -19.74455174940334, -46.29023093789605 -19.744018393966705, -46.29134907669431 -19.744462094600372, -46.29230327898607 -19.744455212033902, -46.29372764478998 -19.743465515861217, -46.29237008812837 -19.74279677470571, -46.293080268388245 -19.742113107200485, -46.29347634535406 -19.7418843679835, -46.29347149146174 -19.741281756703547, -46.29338622572638 -19.74052883852982, -46.29362112426178 -19.74007447988335, -46.293374693317915 -19.739096845871863, -46.29209420390407 -19.738276656429445, -46.29176676658362 -19.73707282046643, -46.29040953079929 -19.736554946304846, -46.289455374725115 -19.736561816149536, -46.28786203060248 -19.73634739682348, -46.28754818019417 -19.736953203854164, -46.2867584474436 -19.737712413383544, -46.28580850698236 -19.738246889650966, -46.28453263393418 -19.737879274498795, -46.28246219056312 -19.73766732415683, -46.27857240684247 -19.738818205152874, -46.27667113460493 -19.739962071498113, -46.27491937246034 -19.739748666814762, -46.2737304787294 -19.740360677855737, -46.27294364748024 -19.74149657878499, -46.27239476087139 -19.742555794055004, -46.27240610839541 -19.74398779796476, -46.27328924196696 -19.744885948277563, -46.27456216012819 -19.744876893950487, -46.275516966913706 -19.744945088782075, -46.276476327099026 -19.745465910577664, -46.27775104585351 -19.745682700941718, -46.27854986118693 -19.746053768325535, -46.279667993980205 -19.7464984462937, -46.280788782411435 -19.74739485830765, -46.28055864424013 -19.748451816300534, -46.280007382084634 -19.74920929392847, -46.280012792747335 -19.749887799280945, -46.28112794214116 -19.749954816285193, -46.28224274405627 -19.75009772446339))) |
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