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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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-20f1 |
Folha |
SG22 |
Legenda_Completa |
456Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
456 |
Nome_Unidade |
Serras do Leste Catarinense |
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 |
Serras do Leste Catarinense |
Area_Poligono_Km2 |
4.669 |
the_geom |
MULTIPOLYGON (((-49.04034166666082 -26.592785278122612, -49.03957666666083 -26.59213222256705, -49.03760833332748 -26.589831944789115, -49.0374644444386 -26.589901944789172, -49.03683638888304 -26.59017277812264, -49.036873611105264 -26.5908530559003, -49.03697416666081 -26.591516389233703, -49.03699444443859 -26.592518889233617, -49.03676416666082 -26.593526667011417, -49.03678472221637 -26.594529167011352, -49.03707583332749 -26.596529167011226, -49.03709611110527 -26.59753166701119, -49.03829916666082 -26.599178889233627, -49.0391480555497 -26.599830278122532, -49.04015694443859 -26.60014416701147, -49.04192777777194 -26.60094388923364, -49.04288194443861 -26.60267972256705, -49.04306916666082 -26.603678889233688, -49.04243666666083 -26.605446667011318, -49.04172249999416 -26.60730000034477, -49.04193027777195 -26.60930166701139, -49.04203583332749 -26.61038611145585, -49.04400555554971 -26.61276972256681, -49.04460722221638 -26.613593333677898, -49.04479472221637 -26.61459250034474, -49.04405666666082 -26.615276111455984, -49.04314805554972 -26.61579611145569, -49.04240999999415 -26.61647972256687, -49.0423469444386 -26.617483889233455, -49.04278305554971 -26.61839444478904, -49.04305388888304 -26.61939194478902, -49.04299083332748 -26.62039611145568, -49.04215611110527 -26.620622778122343, -49.042073055549714 -26.621302500344616, -49.04227083332749 -26.62235777812245, -49.04336805554971 -26.624277500344707, -49.044267222216384 -26.62514194478912, -49.04608749999417 -26.62792972256692, -49.04663777777193 -26.628977778122408, -49.0473608333275 -26.62984583367785, -49.04842222221639 -26.630000833678004, -49.05053027777195 -26.62960500034462, -49.05158083332751 -26.6292305559002, -49.054750555549724 -26.628989722566793, -49.05790944443862 -26.62821944478901, -49.059219444438625 -26.628091667011248, -49.05954888888307 -26.626714444789016, -49.059947777771946 -26.62578694478898, -49.0600111111053 -26.62478277812241, -49.059740277771965 -26.623785278122316, -49.0579972222164 -26.62293305590014, -49.057913611105285 -26.62293472256678, -49.05580055554973 -26.62172416701115, -49.05514749999418 -26.621037778122297, -49.05428694443861 -26.62125333367806, -49.05371944443862 -26.62210055589997, -49.052812777771955 -26.622704167011364, -49.05212916666084 -26.621965833678, -49.05225388888306 -26.61987361145572, -49.05240055554973 -26.6188677781223, -49.05305166666084 -26.618018889233298, -49.0529072222164 -26.61501305590022, -49.05301249999417 -26.612934444789023, -49.052951388883066 -26.60992694478908, -49.052674444438615 -26.608999444788935, -49.05239805554972 -26.608115833677875, -49.0522433333275 -26.607003055900208, -49.05222138888306 -26.60591694478915, -49.052618611105274 -26.604905833677982, -49.05335666666085 -26.6042222225669, -49.05323861110529 -26.60329750034476, -49.05198472221639 -26.602495000344668, -49.05037777777194 -26.60152472256688, -49.04876222221638 -26.60013666701138, -49.04638638888304 -26.598346111455744, -49.04570305554972 -26.59760777812242, -49.045098333327495 -26.596616944789144, -49.04416777777194 -26.59605083367806, -49.04195555554972 -26.594090000344647, -49.041272222216385 -26.59335166701145, -49.04034166666082 -26.592785278122612))) |
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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-20f0 |
Folha |
SG22 |
Legenda_Completa |
000Magua |
Nome_Dominio |
|
Nome_Regiao |
|
Identificacao_Unidade |
0 |
Nome_Unidade |
|
Letra_Simbolo |
|
Categoria |
|
Natureza |
|
Caracteristica |
|
Forma |
|
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Corpo d´água continental |
Area_Poligono_Km2 |
0.206 |
the_geom |
MULTIPOLYGON (((-50.67738166666275 -26.614784167011422, -50.6772836111072 -26.615321667011266, -50.67687444444054 -26.61595000034463, -50.67687444444055 -26.616500555900164, -50.67687444444054 -26.6169863892336, -50.67687444444055 -26.617601667011375, -50.67698305555164 -26.617893055900335, -50.67741777777387 -26.618184722566795, -50.67741777777387 -26.61850833367811, -50.67683805555164 -26.61880000034455, -50.67625861110719 -26.61912388923349, -50.675896388884965 -26.61938277812243, -50.67542555555164 -26.619609444789145, -50.674882222218315 -26.619803889233598, -50.67451999999608 -26.620095278122424, -50.67430249999608 -26.620386667011296, -50.673904166662744 -26.620581111455902, -50.67354194444052 -26.62084000034466, -50.67317972221831 -26.621261111455798, -50.67274499999608 -26.621487778122596, -50.672274166662746 -26.621681944789145, -50.67169444444053 -26.621681944789145, -50.671332222218304 -26.621876389233446, -50.67089749999607 -26.622426944789133, -50.67075277777384 -26.62271833367789, -50.67060777777386 -26.623009722566785, -50.67078888888496 -26.623430833677983, -50.67153472221828 -26.623646944789243, -50.67191166666275 -26.62352777812242, -50.672020555551626 -26.62352777812238, -50.67241888888497 -26.62352777812228, -50.672889722218294 -26.623527778122316, -50.67325194444052 -26.623495555900185, -50.67346944444052 -26.623139167011296, -50.67365055555164 -26.622653611455732, -50.67375916666275 -26.622167778122467, -50.67375916666275 -26.621617222566844, -50.67415777777386 -26.621358333677936, -50.6745922222183 -26.621099167011256, -50.67484583332941 -26.62084000034482, -50.67528055555164 -26.62058111145572, -50.675860277773864 -26.620160000344544, -50.67625861110719 -26.620030555900307, -50.67651222221831 -26.62003055590022, -50.67672944444052 -26.620160000344587, -50.67709166666275 -26.619965833677874, -50.67730916666275 -26.619447500344513, -50.677598888884965 -26.6191886114558, -50.67792499999608 -26.6188647225669, -50.678323333329416 -26.618800000344475, -50.67868555555164 -26.61889694478921, -50.67904777777386 -26.619026667011426, -50.67955499999608 -26.619026667011347, -50.6798086111072 -26.618929444789178, -50.67980861110719 -26.618540833678008, -50.67962749999609 -26.618120000344707, -50.67937388888497 -26.61799027812245, -50.67930138888497 -26.617634167011424, -50.67922888888498 -26.61731027812252, -50.67893916666276 -26.61714833367799, -50.67875805555164 -26.616727222567054, -50.67872166666275 -26.616371111455678, -50.67861305555164 -26.615982500344618, -50.67843194444054 -26.615691111455746, -50.67806972221832 -26.615367222566867, -50.6778524999961 -26.61504333367785, -50.67738166666275 -26.614784167011422))) |
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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-20ef |
Folha |
SG22 |
Legenda_Completa |
675Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Patamar Oriental da Bacia do Paraná |
Identificacao_Unidade |
675 |
Nome_Unidade |
Patamar de Ponta Grossa - Itapetininga |
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 |
Patamar de Ponta Grossa - Itapetininga |
Area_Poligono_Km2 |
41.611 |
the_geom |
MULTIPOLYGON (((-50.187205869995445 -25.95409666234769, -50.18535164495743 -25.955662223084445, -50.18390214391945 -25.956045096821146, -50.181412499995496 -25.955021667014503, -50.180882222217704 -25.954259444792278, -50.17855527777328 -25.953791667014485, -50.178040555551064 -25.95380194479227, -50.1775361111066 -25.954327500347752, -50.17695222221771 -25.9550630559033, -50.17652749999549 -25.955378333681153, -50.17602861110661 -25.956161111458815, -50.175522524516005 -25.959092231149544, -50.17285628197854 -25.960806244209408, -50.17019003944108 -25.960996690105006, -50.16714290511255 -25.958711339358583, -50.16523844615721 -25.95966356883615, -50.161619974142084 -25.95833044756748, -50.15850611110659 -25.955486389236686, -50.15771305555103 -25.954472222570015, -50.15718805555103 -25.95396777812565, -50.156668055551016 -25.95372055590336, -50.156142777773255 -25.953216111458875, -50.15503416666213 -25.952127222570006, -50.153589999995475 -25.95119805590343, -50.15230611110659 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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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-20ee |
Folha |
SG22 |
Legenda_Completa |
456Da35 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
456 |
Nome_Unidade |
Serras do Leste Catarinense |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito forte : > 200m |
Nivel_Altimetrico |
|
Legenda |
Serras do Leste Catarinense |
Area_Poligono_Km2 |
35.728 |
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 SG.22 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 |
GeomorfologiaSG22.fid-6d9cbe3e_18e3b3f16e6_-20ed |
Folha |
SG22 |
Legenda_Completa |
685Dc33 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto das Araucárias |
Identificacao_Unidade |
685 |
Nome_Unidade |
Planalto Dissecado Rio Iguaçu |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado Rio Iguaçu |
Area_Poligono_Km2 |
43.911 |
the_geom |
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