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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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_383c |
Folha |
SC23 |
Legenda_Completa |
323Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
323 |
Nome_Unidade |
Chapadões do Alto ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
5.217 |
the_geom |
MULTIPOLYGON (((-46.68653585468207 -8.948128634066464, -46.683316001427436 -8.949418471633892, -46.68216007494277 -8.947732387683837, -46.68154570963997 -8.944399608934429, -46.68270086966394 -8.941986875593283, -46.682961229066855 -8.939553267525353, -46.681699765297296 -8.938157138363836, -46.679599259510674 -8.9384983087549, -46.6782046813202 -8.942466343834935, -46.67591117298003 -8.942509953124658, -46.674931689873475 -8.941802592364589, -46.673976725337326 -8.94012155301227, -46.67280782557392 -8.939020376994776, -46.671915595218174 -8.93880325605824, -46.67110368302202 -8.939467891906386, -46.670348236229195 -8.941792579916362, -46.671103201808556 -8.943469450307418, -46.67236292572537 -8.944962825539836, -46.67451310167224 -8.9466723686863, -46.67526106449212 -8.948643469143411, -46.67442806104034 -8.950086468031238, -46.67397909505389 -8.952126264699682, -46.672728681134224 -8.954340242955308, -46.67192453482794 -8.954614285068066, -46.670701275554414 -8.955756515409506, -46.67009353656004 -8.956132781491092, -46.66935998188028 -8.957579169863003, -46.66939857895417 -8.964119934341616, -46.6698550454314 -8.965788307039587, -46.673778282234 -8.97214644688191, -46.6754989265203 -8.975389410972003, -46.6757213208318 -8.978518565443805, -46.67514125356024 -8.981822766435437, -46.673365773801436 -8.985099341363401, -46.67172406333778 -8.987010697338874, -46.66924104803506 -8.988350242221966, -46.66736470215743 -8.989933546416264, -46.66630436638194 -8.992543899640918, -46.666065743005355 -8.994100028758343, -46.66493217699489 -8.995634344911833, -46.66467605535287 -8.997971558169615, -46.665637250229764 -8.999360055685177, -46.6669199534088 -8.999877925187857, -46.66781677496982 -8.999898884474575, -46.669552098205216 -8.998280790595611, -46.67100140184532 -8.992069710394214, -46.67251847060728 -8.988427970082892, -46.67278874017597 -8.98777907491758, -46.68130752808143 -8.982358992428857, -46.681722335461366 -8.981684302688459, -46.68186300858803 -8.980029309394995, -46.68280883238536 -8.978099381477989, -46.683255098876394 -8.976158588999404, -46.682723447167184 -8.973413275779961, -46.681794414334796 -8.972336092557706, -46.68079134719195 -8.970927814652745, -46.68104741608132 -8.96868866676498, -46.680086139418236 -8.967202034056603, -46.67771652369315 -8.966267680627096, -46.67615993546327 -8.964766843700502, -46.675523586385324 -8.958874737830298, -46.67715208062697 -8.952435064019236, -46.67920428933901 -8.951224577755198, -46.68103120453679 -8.951626827366356, -46.683210114665805 -8.95370995861575, -46.685191943207734 -8.95414732826978, -46.68769157411299 -8.95381621609622, -46.690771967295824 -8.950179887887968, -46.6907885465102 -8.949497772030176, -46.68853344984577 -8.947981097066434, -46.68653585468207 -8.948128634066464))) |
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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_383d |
Folha |
SC23 |
Legenda_Completa |
323Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
323 |
Nome_Unidade |
Chapadões do Alto ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
17.69 |
the_geom |
MULTIPOLYGON (((-43.9418032999954 -8.395081715410788, -43.93860940691671 -8.395073838599414, -43.935795538477606 -8.393754847188712, -43.934485687347866 -8.392066843619459, -43.93373975469676 -8.389818058731883, -43.92998468141186 -8.389059097363408, -43.926791292797034 -8.389237747221907, -43.924157718251166 -8.390353962103818, -43.92392066108416 -8.390267982099115, -43.923631229594164 -8.390699911657816, -43.92334072863638 -8.390987133361552, -43.9231964138001 -8.391130330272974, -43.92290572978723 -8.391273768101586, -43.92247069688907 -8.391561293954563, -43.921890757835754 -8.392280441205752, -43.92145442771922 -8.392999250045197, -43.9204400347283 -8.393717490546285, -43.91971414212384 -8.394722653048968, -43.91840738818602 -8.395728036796928, -43.916958142038446 -8.39687667057199, -43.916377257689575 -8.397595770079063, -43.91623219493718 -8.397882712433438, -43.915652014395675 -8.398458951567253, -43.9141997747653 -8.400182566542746, -43.912894213963185 -8.40147640609377, 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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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_383e |
Folha |
SC23 |
Legenda_Completa |
329DEc33 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
217.564 |
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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_383f |
Folha |
SC23 |
Legenda_Completa |
323Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
323 |
Nome_Unidade |
Chapadões do Alto ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
4.08 |
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 SC.23 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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_3840 |
Folha |
SC23 |
Legenda_Completa |
323Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
323 |
Nome_Unidade |
Chapadões do Alto ParnaÃba |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
3.244 |
the_geom |
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