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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_-4ef2 |
Folha |
SF21 |
Legenda_Completa |
487Dc43 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Sul-Matogrossenses |
Identificacao_Unidade |
487 |
Nome_Unidade |
Depressão Setentrional da Bodoquena |
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 |
Depressão Setentrional da Bodoquena |
Area_Poligono_Km2 |
13.895 |
the_geom |
MULTIPOLYGON (((-57.23563762352976 -20.046861036947927, -57.24026557707096 -20.04247728033681, -57.24826943063173 -20.041670946992237, -57.257102758359196 -20.03330118837101, -57.26425479870377 -20.028118056299757, -57.26551469042719 -20.02532939217263, -57.267199788755875 -20.025726027647412, -57.26679415528206 -20.034879061548388, -57.27016410701945 -20.034873705026392, -57.27393945613237 -20.025715267768554, -57.27730284175282 -20.022128307431842, -57.28615370593916 -20.025297549780063, -57.288256691488186 -20.023304440016872, -57.28614037216306 -20.01773659359995, -57.28108176933453 -20.015357688863194, -57.27181276211437 -20.013381390025245, -57.26591051858755 -20.011003392047023, -57.263388569493245 -20.013394306834694, -57.25665285766777 -20.015394516883624, -57.252866368212786 -20.018981292367872, -57.24949509919608 -20.01739467447205, -57.24864831770788 -20.014609254883414, -57.24612672736332 -20.018592731372618, -57.24107927545602 -20.022977283612164, -57.238973389975776 -20.022980316271752, -57.238544312410646 -20.018603003343834, -57.239379978862395 -20.013827579939292, -57.240217057750414 -20.010642160086753, -57.24569345580636 -20.010634925787283, -57.250321023904085 -20.007445202887805, -57.24737099770511 -20.00625466401969, -57.241894445355506 -20.00546695549224, -57.23684116169236 -20.005871974281966, -57.23305667957954 -20.010253378037554, -57.23095209249533 -20.011053122645556, -57.23306870829097 -20.018610096597044, -57.233500195487515 -20.02497716159495, -57.237299810015635 -20.031737317133597, -57.2343578194604 -20.035720010064612, -57.22593395964461 -20.036128929130136, -57.22676777910146 -20.03055744274868, -57.22549905159894 -20.026977811175424, -57.21959881138351 -20.02459610762106, -57.221278057664264 -20.0210135320208, -57.22127564942074 -20.019023806581973, -57.21790598206996 -20.019425662821337, -57.215808274743516 -20.025795687156684, -57.215813958194666 -20.029774303320803, -57.221296546750715 -20.033747965406363, -57.223409379934196 -20.038121704470814, -57.23563762352976 -20.046861036947927))) |
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_-4ef1 |
Folha |
SF21 |
Legenda_Completa |
478Dc42 |
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 |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
100.474 |
the_geom |
MULTIPOLYGON (((-54.553085776616655 -20.000495879320283, -54.55262961630814 -20.00134528703472, -54.55187164301635 -20.01240469268809, -54.55413885849138 -20.017418964654638, -54.56000528128081 -20.01694634951292, -54.56637287939321 -20.022015761915547, -54.55979921118986 -20.03022747217897, -54.55740530953969 -20.033516033891576, -54.554968203329764 -20.03957231005287, -54.548514929730196 -20.04003514746639, -54.54748788812695 -20.030610450125167, -54.54515303013321 -20.030024546918504, -54.542147239044375 -20.034965137107275, -54.540888974928734 -20.040483798213216, -54.53610699723385 -20.046504723240712, -54.53328187873607 -20.039823727513898, -54.53283321154499 -20.030960273286453, -54.528714943385864 -20.032010472127823, -54.528601657134395 -20.039205021456965, -54.5238638578585 -20.04245888771098, -54.533081953850264 -20.052551280803783, -54.533616456005554 -20.055880412238427, -54.52713629481709 -20.05800476342198, -54.52590405697354 -20.06186078957145, -54.522790656599945 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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_-4ef0 |
Folha |
SF21 |
Legenda_Completa |
480Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
480 |
Nome_Unidade |
Planalto de Campo Grande |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto de Campo Grande |
Area_Poligono_Km2 |
3.703 |
the_geom |
MULTIPOLYGON (((-54.61200332231592 -20.118977434789983, -54.61009291588919 -20.112804442724812, -54.60560066816482 -20.111797417955373, -54.599140697224954 -20.108399921757464, -54.594562443053825 -20.113065693197182, -54.59502644585241 -20.11543668791514, -54.58999631615618 -20.1167871417714, -54.58693479746205 -20.120528069502384, -54.591383543586055 -20.12437195824574, -54.59840148518303 -20.123994130430244, -54.60238636311939 -20.12546682731672, -54.603831605041826 -20.129269884757917, -54.60682223269904 -20.130256666003476, -54.61183743993893 -20.129851123810887, -54.61193074405551 -20.123706224328195, -54.61200332231592 -20.118977434789983))) |
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_-4eef |
Folha |
SF21 |
Legenda_Completa |
496Dt11 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
496 |
Nome_Unidade |
Segundo 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 |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Segundo Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
130.329 |
the_geom |
MULTIPOLYGON (((-54.93447718975401 -20.00050451170222, -54.93574293161555 -20.004551510043395, -54.93894395289158 -20.020282188241335, -54.93923431713487 -20.030747859876158, -54.95403602469925 -20.048703789981303, -54.95863375779332 -20.055598097903886, -54.97010168059267 -20.063746814018398, -54.96884179760668 -20.074990270204946, -54.97729639267837 -20.080117676453582, -54.98371573711228 -20.077978269197775, -54.98570468661859 -20.072366782382403, -54.98702823158183 -20.06876088686895, -54.98622648667437 -20.064928454980425, -54.986700401287294 -20.06111071935175, -54.98505762248544 -20.056263315007136, -54.98618216095723 -20.05164850245049, -54.99321300470301 -20.051528238072443, -55.00111837258897 -20.049604653326558, -55.00670601235453 -20.04564411599214, -55.01061816154469 -20.039449715852633, -55.013693058371565 -20.032040123132724, -55.01629857392249 -20.02804563999814, -55.02638771582287 -20.021719770614787, -55.03554362868244 -20.021822075774097, -55.039139598074456 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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_-4eee |
Folha |
SF21 |
Legenda_Completa |
478Dc41 |
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 |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
293.317 |
the_geom |
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