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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_3819 |
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 |
7.245 |
the_geom |
MULTIPOLYGON (((-46.79885914145983 -8.061914169837216, -46.79747619656096 -8.05781058834117, -46.79758068142552 -8.053520924914148, -46.798490870024665 -8.048861107257592, -46.80091307104712 -8.047454312934764, -46.80289383396534 -8.047793220555441, -46.805008999766 -8.046769898394336, -46.80629356556751 -8.042994638579426, -46.806457822077164 -8.040364923192435, -46.80587885283848 -8.039669890059612, -46.805134744723226 -8.037505997784113, -46.80506890110763 -8.036139650530119, -46.805532428119776 -8.033418256346451, -46.80603960071317 -8.033040635330355, -46.80719078522973 -8.030725824059, -46.807323326208426 -8.029363530763865, -46.80696068182225 -8.027891506540016, -46.805027086551675 -8.025602281450764, -46.804681567404806 -8.023449206118192, -46.804760307183656 -8.020231382719857, -46.80516738018285 -8.01985036149941, -46.805643728587626 -8.016643357019285, -46.80471070851807 -8.014085259692436, -46.80484327743484 -8.012722045893058, -46.806093516783356 -8.010411443620066, -46.8101999267094 -8.009239533713876, -46.81302802220503 -8.007548867351773, -46.81346576750776 -8.005902089786076, -46.81290884992089 -8.003888384127151, -46.807765338640934 -8.003036405424083, -46.806386774665384 -8.002419599949862, -46.80634401386595 -8.002438180655098, -46.80538120931853 -8.002882129470853, -46.80364960518498 -8.004598368385524, -46.80261817538229 -8.006037363045133, -46.800856427549895 -8.013019787771753, -46.80023220060983 -8.014175098172801, -46.797059357974575 -8.01780764448984, -46.79710206268466 -8.020149659854713, -46.79809471630001 -8.024270472816736, -46.796244039215246 -8.026762464291973, -46.7943240432907 -8.027985336478139, -46.78918402537988 -8.030693203162881, -46.788772871597615 -8.031503693958996, -46.787617082330996 -8.033778126850654, -46.788492783972856 -8.034578883636227, -46.790108968671994 -8.037640839297842, -46.791082216334736 -8.038541378401986, -46.79364786645805 -8.03938265268328, -46.79478866860413 -8.041555609963986, -46.79493054750877 -8.043900037616368, -46.79399404915325 -8.045633360523434, -46.79372789798093 -8.0483578527565, -46.79246790733506 -8.051060128958595, -46.78968348552362 -8.059189133817107, -46.78963547078056 -8.061137576486395, -46.790097262512425 -8.062612044841224, -46.790781493168836 -8.06311592285003, -46.79104564283463 -8.064488087778104, -46.79211818755833 -8.065391076959196, -46.79318802326437 -8.06580725536707, -46.79453356535822 -8.066328571914918, -46.79627245533717 -8.066365844111706, -46.79697386033235 -8.066187809017046, -46.79891552298668 -8.06408759899683, -46.79886855903655 -8.061940305376472, -46.79885914145983 -8.061914169837216))) |
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_381a |
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 |
3.555 |
the_geom |
MULTIPOLYGON (((-45.57952962016381 -8.031945677180742, -45.58025482980133 -8.031944565630893, -45.581371583714194 -8.031943294876273, -45.582053041384974 -8.031633622975862, -45.582795777277 -8.030829097810443, -45.58347716028302 -8.030581053952087, -45.58372439602035 -8.030581138940201, -45.58465548794675 -8.030579785007768, -45.58527437105145 -8.030331695648554, -45.58558462017571 -8.029899504390727, -45.586327452462264 -8.028972596814162, -45.58669869232753 -8.028292077721565, -45.58694554921013 -8.027858923856634, -45.5873786450807 -8.027674177716912, -45.58762590579667 -8.027673366913998, -45.588060795838715 -8.027549413047378, -45.58868011097408 -8.0269306301967, -45.58905090063422 -8.026620791820607, -45.589484737202426 -8.025817935276015, -45.590101771624134 -8.024767641405079, -45.590784215818914 -8.024395448039797, -45.59183759256225 -8.02433243765217, -45.59264231134223 -8.023899498423907, -45.59276657679079 -8.023774500756693, -45.59301396459596 -8.022848279609272, -45.592950804662436 -8.02185938918192, -45.59232912137748 -8.02136690733176, -45.59183287092247 -8.0213059581238, -45.59108932491752 -8.02130656219398, -45.590221268929035 -8.020875656236761, -45.58978642215981 -8.020196578334224, -45.58978516384106 -8.019702570655653, -45.58984544495377 -8.018467170741832, -45.58948937514316 -8.01696502072794, -45.5885215050164 -8.016196216490814, -45.587555509555855 -8.015812458715489, -45.58716878039755 -8.015717185611152, -45.58552706094428 -8.015429787850927, -45.585140276078846 -8.01495040740651, -45.58330176564536 -8.012737616231078, -45.58158720273238 -8.010203282820358, -45.57916801678046 -8.008847972447064, -45.57788824487325 -8.009664482270328, -45.576539125530324 -8.011206076074238, -45.57619679597369 -8.011754346597089, -45.57619781388232 -8.012433259257612, -45.576447473561636 -8.01342226733906, -45.57712986932551 -8.014593661453487, -45.57762748358195 -8.015025381316459, -45.5777518001574 -8.015581056649, -45.577753008942395 -8.01607595944652, -45.57744343886969 -8.016693968122613, -45.57713347861073 -8.016879626226752, -45.57670036531768 -8.017065251960556, -45.57639016023706 -8.01669529350547, -45.57576748522796 -8.01558371138277, -45.57520986432776 -8.01459730134496, -45.57446373114188 -8.013733105948614, -45.5735336875655 -8.013672820648212, -45.57198411580135 -8.013674780888161, -45.57136511250154 -8.014046113296873, -45.57111833036102 -8.015158144879102, -45.57062297148494 -8.015839486302815, -45.57012706802588 -8.016271590139777, -45.56926053934386 -8.016889351880295, -45.568659381764654 -8.01721832355745, -45.569234956805644 -8.01904761381133, -45.570228673894896 -8.020404109281316, -45.571345541042575 -8.021020123043414, -45.57153147012976 -8.021515073816461, -45.57278744848897 -8.022476379086143, -45.573368807565274 -8.023438467652994, -45.573852068332755 -8.024303889668397, -45.575302930691976 -8.025264633640713, -45.57559290967982 -8.025457133015777, -45.575786842909324 -8.025842442346145, -45.57598077668849 -8.026227751355451, -45.57742950618533 -8.027435849353582, -45.577555767651546 -8.0286704413112, -45.57805440330466 -8.029781942622312, -45.57941951712743 -8.03113853552301, -45.57954363130696 -8.03187909387066, -45.57952962016381 -8.031945677180742))) |
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_381b |
Folha |
SC23 |
Legenda_Completa |
323Dt32 |
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 |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
184.218 |
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_381c |
Folha |
SC23 |
Legenda_Completa |
329Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressão do Rio Tocantins |
Identificacao_Unidade |
329 |
Nome_Unidade |
Depressão do Médio Tocantins |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Depressão do Médio Tocantins |
Area_Poligono_Km2 |
3.073 |
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_381d |
Folha |
SC23 |
Legenda_Completa |
323Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadões do Alto ParnaÃba |
Area_Poligono_Km2 |
146.653 |
the_geom |
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