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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_-4ebd |
Folha |
SF21 |
Legenda_Completa |
496Dc43 |
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 |
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 |
Segundo Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
50.866 |
the_geom |
MULTIPOLYGON (((-55.11230379394781 -20.154529004910962, -55.12021502191811 -20.166686668279148, -55.118418609848106 -20.17431335119913, -55.12261375418686 -20.179991151937553, -55.12562205071338 -20.178011025063046, -55.12824326194333 -20.172808196511955, -55.13254852395823 -20.16923175846177, -55.13679677618381 -20.170484452557808, -55.139297086221156 -20.1753398957965, -55.13625692856019 -20.18013647856936, -55.13324370159552 -20.182519317391066, -55.13274475021238 -20.188550906101693, -55.13012040259585 -20.194156572774965, -55.13091457467256 -20.198994538479358, -55.13298895614557 -20.20384479209157, -55.13675477757435 -20.209921642300163, -55.14099471885885 -20.211978746296847, -55.14486136800093 -20.209604079604382, -55.14574241641257 -20.207199477954973, -55.146667195337905 -20.201174049116688, -55.150082744377286 -20.200806881288933, -55.153858825974304 -20.20607733481621, -55.1581612643841 -20.202903744516306, -55.16029265745595 -20.202926046455527, -55.15893810781631 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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_-4ebc |
Folha |
SF21 |
Legenda_Completa |
496Dc42 |
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 |
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 |
Segundo Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
187.5 |
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_-4ebb |
Folha |
SF21 |
Legenda_Completa |
487Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Sul-Matogrossenses |
Identificacao_Unidade |
487 |
Nome_Unidade |
Depressão Setentrional da Bodoquena |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão Setentrional da Bodoquena |
Area_Poligono_Km2 |
30.208 |
the_geom |
MULTIPOLYGON (((-56.941952891545895 -20.000493468261165, -56.94041047136935 -20.00363197979003, -56.941672247567105 -20.0107958630494, -56.94672676088319 -20.011991159740372, -56.94714581682223 -20.016766812773785, -56.943775035307944 -20.021540291106138, -56.945036709757055 -20.023133147096807, -56.946721944459775 -20.02751108997468, -56.953036448088525 -20.036664764280996, -56.95944210293215 -20.032687477557516, -56.96301245698253 -20.02942178975934, -56.96370976565591 -20.022084670547105, -56.969976166824864 -20.02154735624706, -56.97376687214461 -20.01756798855318, -56.97882285664843 -20.01279361426283, -56.987749959209275 -20.013988286831133, -56.991961893382 -20.02115143131046, -56.99996662738525 -20.02552870780806, -57.002492880372124 -20.02990692392216, -56.999123416834955 -20.037068941275955, -56.992382064594075 -20.03308942615935, -56.989013062218284 -20.039058378930715, -56.99280402785379 -20.042241959567356, -57.00460035664238 -20.047018007276048, -57.01176247665958 -20.049007766472975, -57.023137555243785 -20.049801343695616, -57.03409164226851 -20.046616318589233, -57.034932093669795 -20.041841138110893, -57.0281919734389 -20.03985219036841, -57.023977493562306 -20.03706861915447, -57.02271272041199 -20.031098511805283, -57.02397573767162 -20.02353720381409, -57.02186922119952 -20.019160385027924, -57.02397399235082 -20.010007123412976, -57.026922354360664 -20.00682347528676, -57.031134273895546 -20.006026302678126, -57.034579547288224 -20.000473731578765, -57.028794974787886 -20.000469064078498, -57.00051879868102 -20.00044396328696, -56.941952891545895 -20.000493468261165))) |
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_-4eba |
Folha |
SF21 |
Legenda_Completa |
496Pgi |
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 |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Segundo Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
48.393 |
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_-4eb9 |
Folha |
SF21 |
Legenda_Completa |
483Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
483 |
Nome_Unidade |
Planaltos Sul-Matogrossenses |
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 |
Planaltos Sul-Matogrossenses |
Area_Poligono_Km2 |
92.855 |
the_geom |
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PWG РPowering Growth ̩ um projeto para facilitar o |
Sobre nós |
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