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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 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_-4efd |
Folha |
SF21 |
Legenda_Completa |
481Pgi |
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 |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
272.98 |
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 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_-4efc |
Folha |
SF21 |
Legenda_Completa |
481Dt41 |
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 |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
227.136 |
the_geom |
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-20.172201025008086, -55.55261405829575 -20.166239176789965, -55.54189160923513 -20.152366863795557), (-55.56854503199908 -20.319534548451557, -55.568114648995746 -20.31964916719823, -55.56743685263291 -20.319582600227434, -55.56693104202202 -20.319313774419648, -55.566242179261586 -20.318845447162346, -55.56583129838477 -20.31852128964874, -55.565449438369164 -20.31806214300183, -55.56521106745765 -20.31762292142334, -55.565067957816815 -20.31718410118613, -55.56514411737784 -20.3168870622666, -55.565346411087816 -20.316443740708753, -55.56579311459522 -20.316323648033144, -55.56623307380628 -20.31636269707934, -55.566816013294826 -20.316658085835844, -55.56723611530128 -20.316915672773632, -55.56776242139336 -20.317393835711165, -55.56804817485781 -20.317871460203662, -55.56844057798407 -20.318483363641445, -55.568688531921445 -20.31907534916655, -55.56854503199908 -20.319534548451557))) |
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_-4efb |
Folha |
SF21 |
Legenda_Completa |
488Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Morrarias do Baixo Paraguai |
Identificacao_Unidade |
488 |
Nome_Unidade |
Patamares e Cristas Residuais da Bodoquena Ocidental |
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 e Cristas Residuais da Bodoquena Ocidental |
Area_Poligono_Km2 |
151.468 |
the_geom |
MULTIPOLYGON (((-57.24661994439063 -20.28750962728477, -57.23919989630385 -20.27710724280829, -57.22483428941836 -20.276448831221895, -57.20688078815087 -20.27647086970659, -57.19036753192107 -20.279879609579886, -57.16667881847665 -20.291428268850975, -57.137945583999695 -20.28738551466345, -57.111372677776636 -20.28943812035253, -57.093421506198155 -20.298261653333693, -57.06828005830717 -20.293526914934972, -57.0531986802249 -20.29760119198168, -57.043862631625665 -20.307094431866346, -57.039554960103445 -20.314551721979008, -57.04889629097184 -20.32065143410706, -57.05895637800392 -20.328105556716054, -57.06183291463888 -20.336916786696246, -57.06830123366382 -20.340982386062155, -57.085545467904346 -20.343687419864, -57.102296689046256 -20.347309994486235, -57.10732413383283 -20.34391802062572, -57.12241895462207 -20.351364034244597, -57.134644397811485 -20.36423560442498, -57.16123942722262 -20.371670046012895, -57.182079668488015 -20.372327723398975, -57.19213678285802 -20.369606172408545, -57.21584943664608 -20.368899333281238, -57.22661672413531 -20.36075127118632, -57.238821545016656 -20.353955773401633, -57.24455564020122 -20.345134443288167, -57.24884950215826 -20.33428359943427, -57.24596187940272 -20.325474277675863, -57.23373224405477 -20.31396591405298, -57.223661638259955 -20.305166895962337, -57.21861376482995 -20.290936541503065, -57.22004241218257 -20.284832984342685, -57.22722394770507 -20.28414622404811, -57.23154134779527 -20.290241782742108, -57.23944786633459 -20.293620716407418, -57.24661994439063 -20.28750962728477))) |
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_-4efa |
Folha |
SF21 |
Legenda_Completa |
481Da51 |
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 |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
30.543 |
the_geom |
MULTIPOLYGON (((-55.50932169637762 -20.000456626190335, -55.509852956059994 -20.002184573866444, -55.516380448097486 -20.004354024795735, -55.51667956685629 -20.00505672042901, -55.51704120573468 -20.011896755681622, -55.518691490871014 -20.017541972234927, -55.522089018647854 -20.018374465949332, -55.5267068954266 -20.025249625332595, -55.528778906437566 -20.03130063775462, -55.527449790000006 -20.036920847639287, -55.53041495602434 -20.03855498008317, -55.53252072022337 -20.040984898160985, -55.53247158209204 -20.04621242798092, -55.52521186921787 -20.048565375709234, -55.524330891966116 -20.05177598912627, -55.52472208587183 -20.05539787399181, -55.524684983226464 -20.059419938735775, -55.52252198948482 -20.063021652419312, -55.52161844114623 -20.068644588806816, -55.517770907619266 -20.070220992405638, -55.51602233853501 -20.075032562264973, -55.51724614505356 -20.080674512473283, -55.52057795971957 -20.088745906604835, -55.5239361903397 -20.0869652560239, -55.5272924392074 -20.087650705154267, -55.53031157109523 -20.087238190824632, -55.53613944869108 -20.08693432808669, -55.53860864802597 -20.083578693389093, -55.54034504716734 -20.07610953027836, -55.54578528731752 -20.07418500669523, -55.54489289007556 -20.08047830860612, -55.54229949698483 -20.090303133753515, -55.545617441718896 -20.092299369624346, -55.55106141876194 -20.08998205102561, -55.55280628877739 -20.081725660638483, -55.557455062425525 -20.075067817082644, -55.56584205489663 -20.070016521676063, -55.57213149505769 -20.066129568657043, -55.57797736580862 -20.065388206545123, -55.58260008539367 -20.061408342879755, -55.57974202829757 -20.054689452315635, -55.57184388747131 -20.05186893854244, -55.56146274889132 -20.047058838596886, -55.55692397545614 -20.041902798863195, -55.55116570200052 -20.033190443105582, -55.544565122732465 -20.02565385487153, -55.53751039002549 -20.0220512834857, -55.530441041654015 -20.020023301987262, -55.52966946926647 -20.01332177744224, -55.528634869525014 -20.000473880463527, -55.52838029826182 -20.000473622820042, -55.528297090410376 -20.000473538561277, -55.527519420762474 -20.00047274994933, -55.51472026672489 -20.000461445861987, -55.514720232738206 -20.000461445832, -55.509431654930616 -20.000456724810988, -55.50932169637762 -20.000456626190335))) |
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_-4ef9 |
Folha |
SF21 |
Legenda_Completa |
481Dc32 |
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 |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Primeiro Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
29.613 |
the_geom |
MULTIPOLYGON (((-55.48759644972206 -20.15716039283344, -55.482942032073545 -20.15390196544696, -55.478677477750715 -20.15426720357931, -55.47694956967144 -20.156665885087445, -55.48031192938883 -20.161521278809865, -55.47158404225529 -20.160640580867266, -55.46523528835203 -20.156160950002473, -55.460565162707255 -20.15451246142127, -55.453306924678635 -20.15605735175675, -55.450711618943096 -20.160055945290978, -55.44771435166256 -20.161638449355788, -55.44339675112372 -20.167231344549197, -55.44332612750046 -20.174469799478487, -55.4453964140463 -20.18052087614514, -55.44727225619964 -20.18061695134616, -55.45707596637122 -20.18030071612794, -55.466444591942206 -20.18094600469179, -55.479652261948935 -20.181060743771784, -55.49364378055119 -20.188421040110335, -55.50069208321309 -20.208991804988717, -55.498437224244846 -20.22184261482498, -55.49959666473529 -20.234320834787916, -55.5102791348725 -20.23159613438015, -55.52142566749179 -20.22485327209984, -55.52536383603863 -20.214027331529902, -55.52381774592866 -20.197123245293227, -55.51502990642419 -20.180156837813538, -55.50018961566212 -20.172389489179302, -55.48759644972206 -20.15716039283344))) |
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