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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 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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2a9f |
Folha |
SB24 |
Legenda_Completa |
393Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
393 |
Nome_Unidade |
Patamares do ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
142.705 |
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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2aa0 |
Folha |
SB24 |
Legenda_Completa |
393Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
393 |
Nome_Unidade |
Patamares do ParnaÃba |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
21.149 |
the_geom |
MULTIPOLYGON (((-41.419588652279536 -4.609790664547637, -41.420916560635824 -4.6130893247524964, -41.42814522130999 -4.609101397151939, -41.430771971034666 -4.607110754997461, -41.433396340254006 -4.604459287406395, -41.435360031525335 -4.6011493326159565, -41.43666540107245 -4.5978416926805, -41.43662718348279 -4.586611391543261, -41.43461636953487 -4.576048574423409, -41.43129811400183 -4.568132639251439, -41.43128484360563 -4.5641689798560705, -41.43193210276935 -4.560863736613902, -41.43192104110824 -4.557560689515972, -41.431249455283194 -4.5535992226679936, -41.4299151320627 -4.548318693195222, -41.42792914569851 -4.545022160786284, -41.42462656085216 -4.541729961310995, -41.42133061390179 -4.540419589734674, -41.418690785336516 -4.5384464259043416, -41.41209895618688 -4.535825648577442, -41.40749302796587 -4.536501449524844, -41.402237318882214 -4.539821533379426, -41.4029065565773 -4.5431224778623625, -41.40291748693753 -4.54642559420812, -41.40424504905481 -4.549724357835036, -41.405587984183136 -4.557647550535815, -41.40757188232156 -4.560283816886428, -41.40824335303332 -4.564245362874816, -41.40495805855259 -4.566237737123346, -41.404968997906025 -4.56954084807318, -41.40564063409305 -4.573502479497163, -41.40762692083077 -4.576799340158631, -41.40829859209137 -4.5807608699592555, -41.40962861745173 -4.584720204514777, -41.41227313238426 -4.588014525490775, -41.41228871044066 -4.592638851142711, -41.41361655224717 -4.5959375446225925, -41.415604998257116 -4.599894648859401, -41.41693287064042 -4.60319332705075, -41.41760238802484 -4.6064942022858215, -41.419588652279536 -4.609790664547637))) |
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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2aa1 |
Folha |
SB24 |
Legenda_Completa |
393Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
393 |
Nome_Unidade |
Patamares do ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
5.018 |
the_geom |
MULTIPOLYGON (((-41.82224497091424 -6.207500421694061, -41.819959432067684 -6.208261796731401, -41.81873640354771 -6.207200249578889, -41.816848519728936 -6.210023662149232, -41.81555850430705 -6.20913176130866, -41.8120583896684 -6.210426883980368, -41.810153994296854 -6.212032484098653, -41.8088905871164 -6.214272771757756, -41.81112225927036 -6.21426074152679, -41.81303850680713 -6.214888546555849, -41.81494629172356 -6.213921060395314, -41.817496773542786 -6.213907312459353, -41.82068996665414 -6.214847294653646, -41.82229081205682 -6.216114923251894, -41.8245224941034 -6.216102889423563, -41.82484980236202 -6.217696444921638, -41.8242240693708 -6.219933269291488, -41.8248701935901 -6.221525103487241, -41.8270967962657 -6.22055589602421, -41.82933019871523 -6.220862906584404, -41.82902329607379 -6.223098003356559, -41.82775653801933 -6.2247001581722285, -41.82688321177627 -6.228198915733626, -41.826500050222755 -6.228216640471829, -41.82683261501879 -6.2307673462222715, -41.82938317867626 -6.230753559615273, -41.83319869185163 -6.22881856930792, -41.83542180965431 -6.227211253282952, -41.83733471980698 -6.227200919173333, -41.83893571449723 -6.228468508201314, -41.83957335271361 -6.228465062898614, -41.84211872368574 -6.22749413323387, -41.84465383069532 -6.2246089111586835, -41.843356631488916 -6.222681724268625, -41.8436802750102 -6.221423579021483, -41.841763966319476 -6.220795803669851, -41.83849367702714 -6.2214295864926745, -41.83793648406706 -6.2204973996217525, -41.83887414331261 -6.216982677295333, -41.83597547637269 -6.2182925092784975, -41.835292291991195 -6.217269172520978, -41.83406535321903 -6.215431338672076, -41.83313121302063 -6.214032077205419, -41.83209948109173 -6.212486621047543, -41.830869776904194 -6.21064460085451, -41.83149547032525 -6.208407794471109, -41.83370844827187 -6.204886195028844, -41.836256443465686 -6.203367590828735, -41.835924892205526 -6.20200270864528, -41.831454903706415 -6.200750507017397, -41.82658396776138 -6.199610557868223, -41.826345591661216 -6.199182671230652, -41.82507885249257 -6.20078480536169, -41.82381372670756 -6.202706000968286, -41.822545232961694 -6.203989088013093, -41.82223482746086 -6.205586086116075, -41.82224497091424 -6.207500421694061))) |
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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2aa2 |
Folha |
SB24 |
Legenda_Completa |
367Dc21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Baixas Chapadas e Tabuleiros do Médio Rio ParnaÃba |
Identificacao_Unidade |
367 |
Nome_Unidade |
Tabuleiros do ParnaÃba |
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 |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
93.129 |
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, tem como objetivo,além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campo e registrosfotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamento das informaçõesgráficas e alfanuméricas em banco de dados para posterior consulta, tratamento e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSB24.fid-6d9cbe3e_18e3b294723_2aa3 |
Folha |
SB24 |
Legenda_Completa |
395Dt42 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto da Ibiapaba |
Identificacao_Unidade |
395 |
Nome_Unidade |
Serras Grande e da Ibiapaba |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serras Grande e da Ibiapaba |
Area_Poligono_Km2 |
35.96 |
the_geom |
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