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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 SH.21 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 |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea8 |
Folha |
SH21 |
Legenda_Completa |
388Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
15.833 |
the_geom |
MULTIPOLYGON (((-54.778277363156185 -31.0387162291906, -54.777984790457275 -31.037075264386598, -54.77770460680653 -31.03385950102127, -54.777466547509405 -31.032683051314567, -54.77674592655005 -31.032059175641567, -54.77692139059887 -31.030372766250455, -54.776629500152936 -31.029296376038346, -54.77580212403979 -31.028501276760416, -54.77496894367472 -31.027435732375817, -54.774406414501016 -31.0263638346567, -54.77357324656247 -31.02529830114337, -54.77247524693404 -31.024508628428077, -54.771383059378685 -31.023989396164353, -54.770285071791555 -31.023199722074096, -54.769457734039506 -31.022404636609927, -54.76835975885004 -31.02161496353472, -54.767532431904314 -31.020819880891537, -54.76696994719109 -31.019748015121685, -54.766942947909776 -31.01839584918426, -54.76687154269636 -31.01487839174108, -54.76603844167186 -31.01381291650839, -54.76521114628839 -31.013017867638936, -54.76491831789552 -31.011940647410203, -54.764897128484016 -31.01085896729181, -54.764064048192 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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 SH.21 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 |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea7 |
Folha |
SH21 |
Legenda_Completa |
388Dc11 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
2.743 |
the_geom |
MULTIPOLYGON (((-55.038773793175714 -29.818681932103193, -55.03932000279175 -29.817770920991848, -55.03905469894569 -29.81679539916452, -55.038434516085545 -29.815909034476523, -55.037459563348165 -29.815643063089414, -55.03639650410967 -29.81555416328369, -55.03586414224181 -29.814667494922453, -55.03568731002673 -29.813602830354807, -55.03524441148985 -29.812627945738484, -55.03435822667759 -29.812095111266196, -55.03329518655997 -29.812007137553227, -55.032319701273444 -29.812361237063357, -55.03035341732784 -29.81298343688422, -55.02838477981191 -29.81377117736174, -55.02603579367257 -29.81400840360532, -55.02497240128456 -29.813831549461423, -55.02307465085117 -29.8143795845132, -55.022543080883985 -29.816242616156877, -55.02191390165617 -29.8163616819094, -55.021630151554874 -29.816269124590733, -55.02101002519856 -29.81538179122168, -55.0200576547886 -29.81450307917653, -55.017806454489474 -29.813714845709413, -55.01572533265619 -29.81484146009764, -55.01477483722625 -29.81573133980022, -55.013710820134115 -29.815908918345915, -55.0128254741302 -29.816618065410285, -55.012647974371426 -29.817682094234996, -55.01424270283703 -29.819012285326977, -55.015040745846704 -29.81972227404634, -55.01557204970776 -29.8206090097773, -55.0159265522846 -29.82273658473118, -55.01592668462743 -29.82380098516301, -55.01608357670203 -29.824889177459546, -55.0160838390414 -29.82701707722413, -55.01583740104435 -29.82805802510286, -55.016458189692706 -29.82885564005661, -55.01752098781295 -29.82912233707797, -55.01964789163101 -29.829477062603946, -55.020711649998056 -29.829476232607465, -55.02168621674678 -29.829122138161328, -55.02381261490595 -29.8283235398899, -55.02469931582822 -29.827703164207072, -55.02629442584558 -29.826550011950538, -55.02726897418007 -29.82619590548299, -55.02850937600431 -29.82442197509184, -55.02904140987648 -29.823446462909637, -55.03045940894062 -29.82167287648999, -55.03285205384154 -29.82034300835569, -55.0347129152992 -29.81954435753313, -55.03683965976504 -29.819367686871207, -55.03790267737724 -29.81919002566522, -55.038773793175714 -29.818681932103193))) |
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 SH.21 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 |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea6 |
Folha |
SH21 |
Legenda_Completa |
388Dc11 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
30.409 |
the_geom |
MULTIPOLYGON (((-55.01796350858549 -29.8377216732092, -55.01797213532461 -29.83814444825845, -55.01799569667135 -29.839329535704103, -55.020029885489 -29.842252338835, -55.020840011847 -29.84322429231951, -55.02145156450192 -29.844199735309047, -55.021866540800694 -29.84517959768791, -55.022479099784455 -29.84615504659523, -55.02289408301701 -29.84713491903857, -55.02291766741601 -29.848320069998632, -55.02274090054238 -29.849311337736168, -55.02216796894489 -29.85031145219303, -55.021394681106784 -29.851117676898237, -55.0204200389238 -29.85173001089344, -55.02033521861766 -29.85173217186282, -55.02037934412831 -29.851787214660582, -55.02209258109457 -29.85350171963852, -55.02311952315209 -29.854015530702952, -55.0250041060026 -29.855387058946484, -55.02825902892796 -29.858301215539072, -55.02894403385515 -29.859158602070284, -55.03048571422417 -29.860872790989873, -55.03099874690271 -29.861901048555517, -55.03168377019067 -29.86275844733143, -55.0333971490583 -29.864472064800854, 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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 SH.21 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 |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea5 |
Folha |
SH21 |
Legenda_Completa |
388Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
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 |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
95.905 |
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 SH.21 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 |
GeomorfologiaSH21.fid-6d9cbe3e_18e3b3f16e6_-ea4 |
Folha |
SH21 |
Legenda_Completa |
388Dc11 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
388 |
Nome_Unidade |
Depressão do Rio Ibicuà |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Depressão do Rio Ibicuà |
Area_Poligono_Km2 |
0.18 |
the_geom |
MULTIPOLYGON (((-55.16753087039812 -29.836875660723237, -55.16763565694587 -29.835980071419485, -55.1662992825883 -29.834824470376358, -55.16520574507206 -29.83464166324531, -55.16453662015742 -29.83385106464163, -55.163503694264506 -29.83360815115747, -55.16253207225229 -29.833912196448072, -55.161802832369744 -29.83464183369747, -55.16186329878122 -29.835676144569693, -55.162592025425276 -29.836405724533076, -55.163504295289066 -29.8368923205899, -55.16435423567983 -29.83749982599966, -55.165023369355204 -29.838290442305325, -55.166055778529525 -29.838412691156226, -55.16753087039812 -29.836875660723237))) |
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PWG РPowering Growth ̩ um projeto para facilitar o |
Sobre nós |
Privacidade |