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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_-2d06 |
Folha |
SG22 |
Legenda_Completa |
383Atfm1 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies Deltáicas, Estuarinas e Praiais |
Identificacao_Unidade |
383 |
Nome_Unidade |
PlanÃcies Litorâneas |
Letra_Simbolo |
Atfm |
Categoria |
Terraço fluviomarinho |
Natureza |
acumulação |
Caracteristica |
fluviomarinho |
Forma |
terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
PlanÃcies Litorâneas |
Area_Poligono_Km2 |
11.503 |
the_geom |
MULTIPOLYGON (((-48.61227987916896 -25.56604605229511, -48.60915212060354 -25.567831942618895, -48.608199938419666 -25.566107443987182, -48.60293333332697 -25.56856416701618, -48.60243424653364 -25.570606716691184, -48.60243424653364 -25.571081349098314, -48.60243424653363 -25.571555981505504, -48.60243424653363 -25.572505246319682, -48.60279934838526 -25.573016388911892, -48.60316445023688 -25.573527531504237, -48.60404069468078 -25.57396565372607, -48.60457603591549 -25.575183689632013, -48.604720350541925 -25.57482224640941, -48.605793183568586 -25.57557210187333, -48.60623130579053 -25.576740427798516, -48.60608526504987 -25.579369161130185, -48.6058662039389 -25.580464466685164, -48.605647142827934 -25.581559772239917, -48.60623130579054 -25.582582057424545, -48.607107550234424 -25.583458301868408, -48.608275876159624 -25.58418850557162, -48.609444202084816 -25.584626627793536, -48.61032044652873 -25.585356831496778, -48.610320446528725 -25.586379116681325, -48.60973628356613 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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_-2d05 |
Folha |
SG22 |
Legenda_Completa |
676Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Escarpas e Reversos da Serra do Mar |
Identificacao_Unidade |
676 |
Nome_Unidade |
Serra do Mar |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serra do Mar |
Area_Poligono_Km2 |
2.45 |
the_geom |
MULTIPOLYGON (((-48.608199938419666 -25.566107443987182, -48.60879492361668 -25.565476626177983, -48.60913979902045 -25.564097124562856, -48.608191391660085 -25.56289006064964, -48.606122139237456 -25.562976279500635, -48.60508751302615 -25.563666030308088, -48.6033631360073 -25.5639246868609, -48.602673385199765 -25.56426956226469, -48.602328509795996 -25.564786875370398, -48.60172497783939 -25.565131750774167, -48.59982816311865 -25.56513175077405, -48.599310850013 -25.565304188476002, -48.598707318056405 -25.565304188476002, -48.59793134839792 -25.565217969625063, -48.597327816441336 -25.56495931307224, -48.596896722186614 -25.564441999966593, -48.59663806563378 -25.5638384680101, -48.59655184678283 -25.562372747544003, -48.59706915988849 -25.56168299673647, -48.598190004950744 -25.56099324592883, -48.59862109920547 -25.56004483856857, -48.59879353690735 -25.55926886891011, -48.59887975575829 -25.557544491891253, -48.598621099205474 -25.557027178785543, -48.597586472994145 -25.556768522232744, -48.59629319023002 -25.556854741083757, -48.59568965827342 -25.557113397636574, -48.594597009602936 -25.557285468055234, -48.59350436093245 -25.55745753847409, -48.59224657137494 -25.558944017042023, -48.591446159838355 -25.56031615110477, -48.591103126322665 -25.561573940662363, -48.591103126322665 -25.563403452745913, -48.59133181533312 -25.564432553293077, -48.59201788236448 -25.566147720871406, -48.59178919335404 -25.567519854934172, -48.5912174708279 -25.56866329998639, -48.58973099225993 -25.569692400533434, -48.58721541314491 -25.570950190090983, -48.586643690618764 -25.57140756811177, -48.58481417853512 -25.57346576920593, -48.58481417853511 -25.574380525247772, -48.58572893457694 -25.577239137878454, -48.587558446660594 -25.57815389392019, -48.5891592697338 -25.57792520490984, -48.59053140379654 -25.577467826888906, -48.59133181533311 -25.576553070847154, -48.59167484884881 -25.575295281289602, -48.5928182939011 -25.57438052524785, -48.593961738953375 -25.574037491731982, -48.59510518400565 -25.573351424700668, -48.595676906531786 -25.57289404667987, -48.59647731806839 -25.571750601627553, -48.59979330872 -25.57106453459619, -48.60243424653364 -25.571081349098314, -48.60243424653364 -25.570606716691184, -48.60293333332697 -25.56856416701618, -48.608199938419666 -25.566107443987182))) |
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_-2d04 |
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 |
0.773 |
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_-2d03 |
Folha |
SG22 |
Legenda_Completa |
680Dc51 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Patamar Oriental da Bacia do Paraná |
Identificacao_Unidade |
680 |
Nome_Unidade |
Patamares e Cristas Alinhadas do Tibagi - Ivaà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares e Cristas Alinhadas do Tibagi - Ivaà |
Area_Poligono_Km2 |
62.764 |
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_-2d02 |
Folha |
SG22 |
Legenda_Completa |
685Dc31 |
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 |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado Rio Iguaçu |
Area_Poligono_Km2 |
30.677 |
the_geom |
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