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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_3907 |
Folha |
SC23 |
Legenda_Completa |
244Dc42 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
244 |
Nome_Unidade |
Tabuleiros de Formosa do Rio Preto -- Parnaguá |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Tabuleiros de Formosa do Rio Preto -- Parnaguá |
Area_Poligono_Km2 |
5.611 |
the_geom |
MULTIPOLYGON (((-44.83867150381981 -10.99334652695338, -44.83621015138546 -10.994802719125717, -44.83414055304391 -10.995726764304157, -44.8331602813294 -10.995830506951991, -44.83098069470496 -10.995730809250789, -44.83010830737593 -10.995424481148534, -44.82858182925438 -10.995222331756953, -44.82738400292951 -10.995736230395753, -44.825182104814765 -10.996533085788071, -44.82411592706986 -10.996865771671215, -44.82234488475412 -10.996586393045174, -44.82057590610624 -10.99616538974063, -44.81874969368163 -10.996466115702855, -44.81744837402794 -10.997233341845682, -44.81703388177185 -10.997477808832341, -44.81726607390946 -10.997753328486903, -44.81867427062554 -10.999455923409915, -44.81881913377614 -11.000897762998768, -44.818819452859614 -11.001919818186154, -44.818684494864435 -11.002848508848244, -44.81841566058593 -11.003642890345722, -44.81734198066131 -11.004437774838701, -44.81653639588295 -11.005762365380994, -44.816938734101946 -11.006822916589734, -44.8186828158686 -11.00762007151087, -44.81881566225215 -11.00868015551498, -44.81854579945771 -11.010535750925548, -44.81854471218361 -11.012657320121361, -44.818543920389416 -11.0139831849952, -44.818811144126315 -11.01570598485264, -44.820555289220714 -11.016503125609914, -44.822566822929005 -11.016901456938815, -44.8244448298728 -11.017698329797383, -44.825517161471765 -11.01968702783713, -44.8255154085974 -11.02207409947561, -44.82551347843638 -11.024194739171119, -44.825513551834874 -11.024328399005372, -44.82578155624525 -11.024726216921525, -44.82792756171589 -11.025787222492898, -44.82926952605058 -11.026715117712246, -44.82953729627201 -11.026848282694731, -44.831014260409034 -11.02592168568633, -44.832624064059374 -11.02380079454869, -44.833968009310574 -11.021680450026421, -44.833968836151364 -11.019427008877706, -44.833835354253296 -11.017703976226327, -44.83383654029958 -11.014787599378245, -44.83450932460316 -11.012533881629365, -44.83518089265664 -11.011076724812455, -44.83571867169963 -11.008557680365096, -44.836658226555926 -11.007498329124125, -44.839745729981104 -11.005045998998698, -44.840014301109115 -11.00504641392844, -44.839880737186114 -11.002726364137478, -44.83867443747241 -11.001665544140803, -44.8384121325877 -11.000856244558728, -44.83792172244423 -10.997420958503604, -44.83830227398614 -10.994986954469647, -44.83867150381981 -10.99334652695338))) |
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_3908 |
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 |
94.044 |
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_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 |
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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 |
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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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