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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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f52 |
Folha |
SF21 |
Legenda_Completa |
478Dc52 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
478 |
Nome_Unidade |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
11.834 |
the_geom |
MULTIPOLYGON (((-55.689322731991865 -20.343770263107153, -55.6809838196558 -20.341738766623912, -55.67300784392546 -20.346325050014883, -55.669642764472954 -20.34905606031032, -55.668775218683564 -20.352595721764764, -55.67125847209895 -20.35537145917548, -55.669989150807 -20.357331171963175, -55.66703735843738 -20.360459082649456, -55.666999553838096 -20.364791649756413, -55.65987951858034 -20.366706560086246, -55.659425816741916 -20.371036103934333, -55.65727774443298 -20.37771529415822, -55.65723977552727 -20.382048047074218, -55.656242212839985 -20.393818827880416, -55.66548524697855 -20.397637251750467, -55.668606701561934 -20.39433100217063, -55.67261692087651 -20.390197127451753, -55.67529950230421 -20.386469857695662, -55.678016868000306 -20.37857887285591, -55.68248682969588 -20.372367465726605, -55.68785435430341 -20.364496828985573, -55.689322731991865 -20.343770263107153))) |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f51 |
Folha |
SF21 |
Legenda_Completa |
481Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
481 |
Nome_Unidade |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
86.764 |
the_geom |
MULTIPOLYGON (((-55.50868210056443 -20.322877784392297, -55.50987103397332 -20.311820574910175, -55.507327856355644 -20.29961933154122, -55.50434219389886 -20.299592997659452, -55.49662136667982 -20.30435348658495, -55.49273661993223 -20.309145969946513, -55.48968495010267 -20.315957752782378, -55.48622667401439 -20.3186402077267, -55.47398814049478 -20.320646852626503, -55.457778693979634 -20.316162420054038, -55.44708931326437 -20.318882234355595, -55.43892509097391 -20.324842764752802, -55.433307175243975 -20.33669616382036, -55.4329579091612 -20.371278467604448, -55.42683067929986 -20.386505231590554, -55.42387764781784 -20.395120735449456, -55.42231793729872 -20.410594499582547, -55.41637744427013 -20.428236793310685, -55.40741511977325 -20.428155859170484, -55.41580844125823 -20.440122052118422, -55.42385346777898 -20.447037382109965, -55.427722947418864 -20.444657663619275, -55.43153919163056 -20.447509693836246, -55.43575676847248 -20.45277955387527, -55.44608064906792 -20.445627046834403, -55.44992221782793 -20.446064368311443, -55.457577456775184 -20.44935156836748, -55.45881426084099 -20.453790356517093, -55.46219549241385 -20.457441795780735, -55.46553234185562 -20.465522204337056, -55.46720227797349 -20.469560651159753, -55.46717380585198 -20.472377264496718, -55.46978924305065 -20.467168548146972, -55.47287544827034 -20.457536039577683, -55.47671083912869 -20.45837411790289, -55.48394219160398 -20.461657444086427, -55.4898239042099 -20.46138545104833, -55.48434596458023 -20.454099232315944, -55.48352554553548 -20.450673690144683, -55.47974343023294 -20.444607483731385, -55.48019825105035 -20.44179615316165, -55.47658495879214 -20.440357302134373, -55.471872136676474 -20.44212582741371, -55.46761323805121 -20.441082085592214, -55.46742271978648 -20.438869221223474, -55.46937430652967 -20.43566935986841, -55.47196074936536 -20.43307692867741, -55.475208528963286 -20.42828008432369, -55.476761068593866 -20.42246210104697, -55.47465879999748 -20.41922565233282, -55.47296978397947 -20.417401521258444, -55.47237306309938 -20.41297264027283, -55.46940112753975 -20.411337344227412, -55.468377262639976 -20.40710572597048, -55.46710679118912 -20.406089662947767, -55.46009409861372 -20.403212626711536, -55.45353208405547 -20.39792548685411, -55.451038828430256 -20.391269072654417, -55.45342837291509 -20.387066013560883, -55.45795955956404 -20.38187888268132, -55.46456529031871 -20.376818266176357, -55.46637984765401 -20.371571590761814, -55.4731150779475 -20.36651117903127, -55.47688238965619 -20.36575632620615, -55.479817842936164 -20.36460098130725, -55.479871308177664 -20.359087085321253, -55.48193847702566 -20.36146822171918, -55.483992182105915 -20.365030732554512, -55.48859578752762 -20.364283276783507, -55.48863398089608 -20.360344516374465, -55.492018097652455 -20.35604212988855, -55.49624895777691 -20.35056414148748, -55.502944120752474 -20.349440146795576, -55.50795263212049 -20.349877045878777, -55.51462232241516 -20.351509207567293, -55.51912263718916 -20.34629209324919, -55.52297713078721 -20.344717289147187, -55.52640525080665 -20.343137423226906, -55.52002227718508 -20.341473538715068, -55.50893574419665 -20.34097764283505, -55.506000316473475 -20.335723624788955, -55.50605793747977 -20.329692308328337, -55.50868210056443 -20.322877784392297))) |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f50 |
Folha |
SF21 |
Legenda_Completa |
478Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
478 |
Nome_Unidade |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
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 Dissecado da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
53.661 |
the_geom |
MULTIPOLYGON (((-55.38271192312247 -20.501882024184127, -55.363489330727816 -20.522612928450084, -55.35319929068514 -20.526537711277765, -55.34330380280656 -20.53327911241549, -55.33677709968501 -20.544477193918098, -55.32504896571113 -20.56246152351672, -55.315886072250365 -20.580066161674853, -55.31446737354546 -20.592519046312976, -55.31564298858659 -20.602181300409164, -55.321156894035646 -20.60585422885835, -55.33361721117828 -20.599540790775233, -55.33923596652507 -20.593563441654034, -55.34401215619701 -20.58637010789884, -55.350908726397336 -20.580806174676795, -55.36209983431511 -20.572868692818137, -55.37280822310324 -20.57015463044698, -55.38010926527044 -20.56660411714556, -55.38404969306835 -20.557390708663508, -55.38962880435206 -20.55502990242614, -55.39603453787132 -20.555089162242012, -55.40419901112199 -20.55033971457041, -55.40813472806357 -20.541527530521947, -55.40993415821856 -20.532696774759668, -55.41337553354741 -20.53031514744073, -55.4112905011269 -20.525470089363978, -55.409661263123034 -20.517814210128602, -55.40546149383009 -20.51093858679326, -55.40124650201804 -20.505672005247025, -55.39401349753367 -20.503193020251842, -55.38271192312247 -20.501882024184127))) |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f4f |
Folha |
SF21 |
Legenda_Completa |
478Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
478 |
Nome_Unidade |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
534.125 |
the_geom |
MULTIPOLYGON (((-55.29474633341106 -20.43915205148567, -55.29153118172095 -20.45786846519162, -55.290103371967575 -20.46701264556202, -55.275369368479716 -20.480606026359442, -55.267764767331855 -20.48885598285498, -55.26324116769047 -20.497970670084097, -55.25957851992852 -20.50917374222671, -55.25326444039687 -20.520350420205975, -55.24875403695498 -20.528215413470647, -55.2451084071613 -20.537753392928533, -55.239257946591245 -20.54685277426546, -55.23752244715768 -20.551712391553178, -55.228960503156365 -20.5579888972524, -55.22136750253955 -20.56457162481392, -55.21860360991517 -20.574119160433902, -55.2140710275371 -20.583647092185466, -55.21395466251944 -20.593635876089152, -55.212550321512126 -20.600282890290302, -55.21028566138959 -20.604839304232804, -55.21242908099926 -20.610688624367217, -55.21765726282479 -20.617403494537125, -55.218051420375204 -20.621571517031633, -55.21792078174964 -20.632810018414748, -55.217392109577105 -20.640298031569603, -55.21287083357818 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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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f4e |
Folha |
SF21 |
Legenda_Completa |
481Dc43 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
481 |
Nome_Unidade |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
54.979 |
the_geom |
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