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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_28cb |
Folha |
SB24 |
Legenda_Completa |
650Dt11 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do Litoral Norte |
Identificacao_Unidade |
650 |
Nome_Unidade |
SuperfÃcie Rebaixada do Vale do Rio Açu |
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 |
SuperfÃcie Rebaixada do Vale do Rio Açu |
Area_Poligono_Km2 |
20.14 |
the_geom |
MULTIPOLYGON (((-38.17800793190181 -5.1881497409387265, -38.17929069878794 -5.190073891717572, -38.182497616453006 -5.189432507824684, -38.18442176723206 -5.190073891717461, -38.18762868489706 -5.190715274710876, -38.191476986454994 -5.190715274710876, -38.193401137233934 -5.190073891717541, -38.19981497256424 -5.190073891717572, -38.20341496950645 -5.191536213646085, -38.20322570898055 -5.193302646720403, -38.203021890229294 -5.195204960161349, -38.20587116280513 -5.1989866012710735, -38.20598245570704 -5.201601985363648, -38.206091430156604 -5.204162882231457, -38.206228807894426 -5.207391246928594, -38.210434455067265 -5.207737410373443, -38.21071849244572 -5.2093153977075906, -38.215208176997024 -5.210598164593528, -38.217132327776035 -5.20995678160018, -38.22404229479735 -5.209278646912216, -38.22482892999242 -5.21059816459356, -38.22739446466406 -5.210598164593591, -38.23251130403475 -5.212162221429356, -38.23380829999436 -5.213805082258728, -38.23897887295794 -5.215184460614324, -38.24136525008753 -5.217844684004777, -38.24407043598319 -5.220860301481439, -38.247786011996176 -5.221017495780543, -38.25000304858312 -5.223282728834483, -38.251265053720566 -5.2245721695895435, -38.25379588715184 -5.227158019946243, -38.25569912779383 -5.229102635697512, -38.25728857249096 -5.230726634146153, -38.25981940502281 -5.233312484502756, -38.2617294670226 -5.235264070000244, -38.26395332586655 -5.237536272799911, -38.26541338689952 -5.242503060287044, -38.26851713433964 -5.24585264909933, -38.26972577730406 -5.247157026694166, -38.27164992808301 -5.245232875915332, -38.27421546275468 -5.244591492022686, -38.27831803413132 -5.2456013263589165, -38.27998791419227 -5.247157026694166, -38.284419381130796 -5.24835394699587, -38.28854397060914 -5.252044368971206, -38.29025005108034 -5.253570862024256, -38.29390364401926 -5.253585725119793, -38.29538111862508 -5.254853628910417, -38.29794665329677 -5.254212245017667, -38.297305269404085 -5.2522880942387475, -38.2940983517389 -5.247798409687626, -38.28960866718758 -5.244591492022686, -38.287684516408575 -5.242667341243766, -38.28191206497118 -5.240743190464978, -38.27934653029948 -5.240101807471515, -38.277422380419836 -5.237536272800005, -38.276139612634346 -5.234970739027657, -38.274215462754704 -5.232405205255326, -38.273574078861905 -5.229839670583691, -38.27357407886195 -5.227274136811575, -38.272291311975835 -5.22278445226036, -38.26844301041791 -5.218936150702634, -38.26331194197382 -5.218936150702603, -38.26010502430872 -5.218294766809858, -38.258180874429144 -5.217653383816443, -38.255615339757405 -5.215087849144777, -38.2524084220923 -5.2125223153725555, -38.249842888319954 -5.209956781600304, -38.24535320286928 -5.207391246928594, -38.240222135324565 -5.200977411598634, -38.237656600652834 -5.198411877826231, -38.233166916101595 -5.196487727047498, -38.22290477921346 -5.193280809382554, -38.2190564785549 -5.190715274710938, -38.21520817699703 -5.188791124831393, -38.21200125933193 -5.184942823273718, -38.20879434166681 -5.181735905608574, -38.20494604010894 -5.1772462210573575, -38.19986808202759 -5.179301584721385, -38.19799173111473 -5.180061060390625, -38.19622034997039 -5.180778047589937, -38.190591296332514 -5.183056474597719, -38.18838691140804 -5.183948725274422, -38.184857271127406 -5.185377389176034, -38.1824298228592 -5.186359928188927, -38.180330408602735 -5.187209690395821, -38.17800793190181 -5.1881497409387265))) |
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_28cc |
Folha |
SB24 |
Legenda_Completa |
393Dt11 |
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 |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares do ParnaÃba |
Area_Poligono_Km2 |
112.913 |
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_28cd |
Folha |
SB24 |
Legenda_Completa |
367Dt23 |
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 |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Tabuleiros do ParnaÃba |
Area_Poligono_Km2 |
11.925 |
the_geom |
MULTIPOLYGON (((-41.57923499338543 -6.19221020222649, -41.57226033453202 -6.200542011791664, -41.57084832517533 -6.195454198040092, -41.570366521482995 -6.196676905502137, -41.56890927352939 -6.197904435128796, -41.56720106975872 -6.197668811853401, -41.56623035233409 -6.198649875078967, -41.56623743899181 -6.20011423666991, -41.56673101480963 -6.201332129161627, -41.566986567960925 -6.203771530318936, -41.567484818454886 -6.2059656629719235, -41.567983098626286 -6.20815979292704, -41.57055217662682 -6.208419852581203, -41.57164936121428 -6.209850096591588, -41.57020355083846 -6.2117087866180105, -41.57044186398601 -6.212296729197573, -41.56776287264367 -6.2130421988251285, -41.56555743821036 -6.2108565305911325, -41.56414146823934 -6.210782670171017, -41.563612408770936 -6.212086497380746, -41.56020887952134 -6.214299964558476, -41.558743316436065 -6.21381909256378, -41.55824616041719 -6.211869014330402, -41.558482960005904 -6.21040343595665, -41.55920866793094 -6.20917950451747, -41.559444298400926 -6.207469864529649, -41.55894957594738 -6.20600790502772, -41.55894374834055 -6.2047875933598835, -41.5596695093256 -6.2035636628198025, -41.560151404748815 -6.202340939170213, -41.560387104466585 -6.200631299182199, -41.56176745139198 -6.1989438301809, -41.56078120807154 -6.19803156958851, -41.559637867578715 -6.196973991144203, -41.56039156510386 -6.195294421787454, -41.55961538452762 -6.194296735493416, -41.55868347734585 -6.193098875400228, -41.55790730306475 -6.192101187307429, -41.559855808384064 -6.1916034305413925, -41.56205052559646 -6.191592593710782, -41.56301180013976 -6.1886590465653315, -41.5604007651684 -6.187835354805247, -41.55866574181574 -6.18962821355868, -41.55721990086291 -6.189446716880059, -41.555661476481234 -6.192633045466145, -41.5546844206347 -6.192650571454181, -41.554374785852914 -6.1945669044264955, -41.554701332385825 -6.1961609617462505, -41.55566868005079 -6.198390117596992, -41.55632476785904 -6.202216481092733, -41.55687502884472 -6.2056653334754115, -41.555706824795394 -6.206368284955351, -41.556355261171596 -6.208599012821103, -41.55704350873613 -6.211609167815689, -41.55573752315339 -6.212750808589697, -41.556390198933734 -6.215913718829731, -41.555438647860505 -6.216901027846793, -41.55831774555271 -6.218801551636893, -41.56023407402853 -6.219430312645381, -41.56594454239201 -6.2200048993931585, -41.56513741344611 -6.2216928432365854, -41.564397966578085 -6.223239237387259, -41.565996985457716 -6.22418869483874, -41.567913341812485 -6.224817443256813, -41.570147035642385 -6.225125484439892, -41.573517654201616 -6.225367512686922, -41.57334201300864 -6.2263861396949265, -41.57621502498861 -6.227010129799938, -41.57812674983479 -6.226681507631879, -41.58122958446296 -6.226922635657374, -41.58132488831819 -6.228580387461197, -41.58291149385561 -6.22697687377012, -41.58417456918631 -6.224417589386655, -41.58608161216188 -6.223131619115275, -41.587672883382126 -6.222485470614379, -41.58861860864719 -6.2202469006604035, -41.5886092610937 -6.218332195461076, -41.58700554775306 -6.21642539440308, -41.586041145367766 -6.214834546763616, -41.58603025098058 -6.2126007198341044, -41.58954094794162 -6.21322157490254, -41.59494458111284 -6.209684438772703, -41.595893376663355 -6.208084123070783, -41.59620294039864 -6.206167847655093, -41.596189026088 -6.20329580064773, -41.59553893046257 -6.200746023897118, -41.595850008656264 -6.199148867513398, -41.595523337117534 -6.197554865052327, -41.59392434431832 -6.196605396808934, -41.59201117606021 -6.19661485138155, -41.59041375167854 -6.195984495875093, -41.59104367820838 -6.194385760282068, -41.59166580311951 -6.191191442118937, -41.59133758924352 -6.189278315229594, -41.58910403211068 -6.188970214691112, -41.587184663926436 -6.187703185940902, -41.58431184979721 -6.187079109500828, -41.580812202806165 -6.188692013912949, -41.57923499338543 -6.19221020222649))) |
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_28ce |
Folha |
SB24 |
Legenda_Completa |
395Dt11 |
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 |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serras Grande e da Ibiapaba |
Area_Poligono_Km2 |
102.622 |
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_28cf |
Folha |
SB24 |
Legenda_Completa |
395Dt11 |
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 |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serras Grande e da Ibiapaba |
Area_Poligono_Km2 |
93.29 |
the_geom |
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