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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_3909 |
Folha |
SC23 |
Legenda_Completa |
066Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
66 |
Nome_Unidade |
Planalto Dissecado do Tocantins |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Tocantins |
Area_Poligono_Km2 |
20.496 |
the_geom |
MULTIPOLYGON (((-47.852905016739484 -11.00061146733653, -47.85350655624229 -10.999498176835532, -47.85169700057962 -10.993691247002037, -47.85013007595762 -10.993715229524083, -47.84719597142964 -10.99558550012815, -47.84483284393604 -10.99520427280677, -47.84492212244332 -10.991233196170922, -47.84396806012074 -10.98839724686257, -47.839735592751005 -10.988307899004765, -47.83733452780694 -10.989580914392855, -47.83376379199265 -10.99016643281989, -47.83245371640759 -10.988152252345486, -47.83249556674821 -10.98633233905303, -47.83151213155042 -10.984820342478702, -47.82828321530583 -10.985249114158965, -47.82626675680996 -10.984543687894673, -47.82637348886971 -10.979745405102667, -47.82435616872171 -10.979039053947272, -47.822493504874906 -10.978999613678086, -47.82019652930197 -10.98325443799126, -47.81865371853172 -10.98404841563745, -47.81712140276802 -10.984346429938652, -47.81453116265271 -10.978994792151676, -47.811995411914985 -10.978775321558475, -47.81110846295816 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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_390a |
Folha |
SC23 |
Legenda_Completa |
294Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Formas Agradacionais Atuais e Subatuais Interioranas |
Identificacao_Unidade |
294 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais |
Area_Poligono_Km2 |
0.829 |
the_geom |
MULTIPOLYGON (((-43.27548969004627 -11.521497565056595, -43.275399281814366 -11.520337633364852, -43.275306678444224 -11.519371874923987, -43.275118182823974 -11.518405270412774, -43.27492786432064 -11.517437707505898, -43.274737475853485 -11.516471923753498, -43.27435158520567 -11.515504311058075, -43.27406441438866 -11.514536756391847, -43.27377535008838 -11.513570022692745, -43.27319489561624 -11.512600612756335, -43.27271219570506 -11.511632116292688, -43.27222763942082 -11.510663550503176, -43.27164619556849 -11.509695882122331, -43.270771543732664 -11.50872457616633, -43.26924878950413 -11.507054923968552, -43.26885865579307 -11.508306820169938, -43.27024480646657 -11.510572935359745, -43.27150077808086 -11.51309000171326, -43.272627776079524 -11.516106674726894, -43.27346462219939 -11.524641805020991, -43.273946166167875 -11.5292868191317, -43.27387638310908 -11.529308317041902, -43.27416250634727 -11.530372064806038, -43.27454934775249 -11.53133970800623, -43.274836538350925 -11.532307257819001, -43.27512376669659 -11.533273917337588, -43.275608374395446 -11.534242472424635, -43.2761888845443 -11.535211871923778, -43.27677129460861 -11.536180448502762, -43.27735400775684 -11.536955672461367, -43.278231100979845 -11.537636547933678, -43.278328860853364 -11.537637460930432, -43.278917780261125 -11.537351645027684, -43.279117018328996 -11.53677262947348, -43.27902396719579 -11.53609645848493, -43.278829771806244 -11.535805974776792, -43.27873227481221 -11.535612600427436, -43.27863939185275 -11.534839308565086, -43.278446294677835 -11.534451738068249, -43.27825346061698 -11.533871705795674, -43.27786753217163 -11.532904102267628, -43.277482572187125 -11.531935642337562, -43.27729219985223 -11.530968974252337, -43.27690627906745 -11.530001368706442, -43.276715910189694 -11.529034699746664, -43.276526472681084 -11.528068064535463, -43.27623831486532 -11.52710137092616, -43.27614663611497 -11.526135648633902, -43.27585948306999 -11.525167208745371, -43.27576687636845 -11.524201451707626, -43.275674270335195 -11.523235694389594, -43.27548969004627 -11.521497565056595))) |
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_390b |
Folha |
SC23 |
Legenda_Completa |
066Pgu |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
66 |
Nome_Unidade |
Planalto Dissecado do Tocantins |
Letra_Simbolo |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Tocantins |
Area_Poligono_Km2 |
171.115 |
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.
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FID |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_390c |
Folha |
SC23 |
Legenda_Completa |
399Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
399 |
Nome_Unidade |
Cuesta de Bom Jesus do Gurguéia |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Cuesta de Bom Jesus do Gurguéia |
Area_Poligono_Km2 |
2.541 |
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_390d |
Folha |
SC23 |
Legenda_Completa |
066Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Região não identificada - domÃnio 2 |
Identificacao_Unidade |
66 |
Nome_Unidade |
Planalto Dissecado do Tocantins |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Tocantins |
Area_Poligono_Km2 |
41.674 |
the_geom |
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