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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_-5949 |
Folha |
SE23 |
Legenda_Completa |
027Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos Cimeiros |
Identificacao_Unidade |
27 |
Nome_Unidade |
Planalto dos Geraizinhos |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto dos Geraizinhos |
Area_Poligono_Km2 |
0.983 |
the_geom |
MULTIPOLYGON (((-42.51153194396928 -16.010658513422225, -42.512550740161 -16.010670322279033, -42.513168510429615 -16.010183366771404, -42.51357931186968 -16.009892741344537, -42.51398738961718 -16.00989746785102, -42.51439453368423 -16.0099021827704, -42.51500618385702 -16.00990926451537, -42.515515114387 -16.009915155634452, -42.516439451530324 -16.009333275773017, -42.516649121705626 -16.008842489907394, -42.517069392336865 -16.007860927866165, -42.51778310577236 -16.00777071956404, -42.518801892173755 -16.007782496702752, -42.5196171086684 -16.00779191709885, -42.52001787865572 -16.008388221688854, -42.521338370891186 -16.00869976154755, -42.52164129888617 -16.008900182986753, -42.5220435729923 -16.009299578184432, -42.522342555419286 -16.00989560795418, -42.522334041098965 -16.010585647015176, -42.52263696172169 -16.010786970749795, -42.52273874884616 -16.01078814551628, -42.52294232312038 -16.010790494904885, -42.523656992447656 -16.010699375753354, -42.52376607507309 -16.010108958319805, -42.524081168744054 -16.00932308940971, -42.525213908949304 -16.008349722808536, -42.525928558393424 -16.008259497893388, -42.526534135083104 -16.008759690838872, -42.52673405932939 -16.009058284502498, -42.52713756872639 -16.009358320068557, -42.527239355474606 -16.009359492600343, -42.527954008687836 -16.00926926132002, -42.52877773948139 -16.00858770212087, -42.52888559398712 -16.008095728187033, -42.529304872424596 -16.00711412270707, -42.52971780395477 -16.006724121096067, -42.530532089095296 -16.00673348872216, -42.53073659427847 -16.006735840887263, -42.53186686043634 -16.0059602329932, -42.531969866601806 -16.005862051103367, -42.53369993258943 -16.005981297240353, -42.53411890816712 -16.005098137879653, -42.53341517186138 -16.00430054609165, -42.53229581662225 -16.00418922222839, -42.53066876295684 -16.0039726889037, -42.5297541920963 -16.003765244529145, -42.52872692865534 -16.004443564996134, -42.52852214866657 -16.00453967048971, -42.527910508554946 -16.004532629531244, -42.52710379472605 -16.003833200524586, -42.525782106570006 -16.00362014758589, -42.52476211171009 -16.00370775793874, -42.52404018723832 -16.00438957339314, -42.52321890137876 -16.00487331541313, -42.5224046282904 -16.00486392112857, -42.521996558150505 -16.00485921205434, -42.521284069880096 -16.004850988177378, -42.52026894234703 -16.00454388127468, -42.51955430668369 -16.004634088863725, -42.51863001141487 -16.00521508352136, -42.517811145127546 -16.005501907105952, -42.51719556212221 -16.00588953978197, -42.51638280061573 -16.00568231294488, -42.51609940574601 -16.00390311166816, -42.51590558950811 -16.00311227310346, -42.51560175371558 -16.002910931514137, -42.5150916231828 -16.00300349061173, -42.51457201024032 -16.003786976231385, -42.51456346149154 -16.004477914792897, -42.51455247601478 -16.005365748192983, -42.51485510701496 -16.005664635878933, -42.51484900553825 -16.006157776367715, -42.51484167454455 -16.006750267471517, -42.514730417609336 -16.00743911371331, -42.514116042048094 -16.00772828841509, -42.51381068735333 -16.00772475236885, -42.51340261407319 -16.007720026150373, -42.51279190511731 -16.007712951599835, -42.51238261276024 -16.00780667070746, -42.51187123823683 -16.00799857054377, -42.51135282920651 -16.008682694067407, -42.51124248110837 -16.009372450553165, -42.51123392896137 -16.0100624838169, -42.51133204325457 -16.010359908590964, -42.51153194396928 -16.010658513422225))) |
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_-5948 |
Folha |
SE23 |
Legenda_Completa |
517Dt21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
517 |
Nome_Unidade |
Depressão do Rio São Marcos |
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 |
Depressão do Rio São Marcos |
Area_Poligono_Km2 |
14.154 |
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_-5947 |
Folha |
SE23 |
Legenda_Completa |
027Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos Cimeiros |
Identificacao_Unidade |
27 |
Nome_Unidade |
Planalto dos Geraizinhos |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto dos Geraizinhos |
Area_Poligono_Km2 |
1.516 |
the_geom |
MULTIPOLYGON (((-42.36245652363537 -16.011130218304352, -42.3625969236527 -16.01160342714063, -42.36307565134764 -16.012269567325596, -42.36374550605566 -16.01331560313385, -42.3642279526805 -16.013699077721313, -42.36451122989865 -16.01445765392646, -42.36538150258954 -16.015034663788477, -42.36634611374235 -16.015895538792364, -42.36790361483755 -16.016197360730512, -42.36907575500178 -16.01611780064469, -42.36956781712262 -16.015840219670313, -42.370355829315635 -16.015284456913275, -42.37036819279464 -16.014340733455, -42.37066909801872 -16.0136841596307, -42.37175277167457 -16.01294233393748, -42.37235549948952 -16.011629190946817, -42.37334605398447 -16.010508663758092, -42.374036006406946 -16.009950779651138, -42.37530861987239 -16.00968363353082, -42.37609043243736 -16.009599255998705, -42.37687225659087 -16.009513972426742, -42.37814024152064 -16.00952946448589, -42.37951488335675 -16.008885985942324, -42.380686997612045 -16.0088054521549, -42.38080225850403 -16.00748632681072, -42.38061080044691 -16.007201277717694, -42.38041689269437 -16.00710407179138, -42.37983760960392 -16.006625513034827, -42.37915413901744 -16.00661717018247, -42.37876385134985 -16.006612405121192, -42.37817842009549 -16.006605256202405, -42.377298275761234 -16.00678328143067, -42.37719901045533 -16.00687600506334, -42.37660987493558 -16.007152421978144, -42.37582929925002 -16.007142881593076, -42.375441478267604 -16.006949364739015, -42.37446946785321 -16.00665386392654, -42.3736876554183 -16.006739140267072, -42.373110860904966 -16.006071820605012, -42.37252790311253 -16.005875911340183, -42.37194371772384 -16.00577392165997, -42.3715546630979 -16.00567522277079, -42.37117426120307 -16.00491546425017, -42.370696758602556 -16.004154516336833, -42.36992484198991 -16.003484800888483, -42.36934189580681 -16.00328888450825, -42.368366200750515 -16.003276928380156, -42.36767903190836 -16.003552119003512, -42.36679642471079 -16.003918846131576, -42.365914124576335 -16.004190734036907, -42.365427986665374 -16.00408993053864, -42.364939671790985 -16.004083938120083, -42.36425219830085 -16.00445304852035, -42.36346668585188 -16.004820952444522, -42.36227974256787 -16.006032953236137, -42.36226734786424 -16.006976671260038, -42.36225248498919 -16.008108229687895, -42.36223637527736 -16.009334611297692, -42.36222397767656 -16.01027832899897, -42.36231612411645 -16.010657009456843, -42.36245652363537 -16.011130218304352))) |
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_-5946 |
Folha |
SE23 |
Legenda_Completa |
566Dc31 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
566 |
Nome_Unidade |
Patamares Dissecados do Planalto de Cristalina |
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 Dissecados do Planalto de Cristalina |
Area_Poligono_Km2 |
24.592 |
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_-5945 |
Folha |
SE23 |
Legenda_Completa |
554Dc31 |
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 |
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 Dissecados das Chapadas de Cristalina |
Area_Poligono_Km2 |
40.619 |
the_geom |
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