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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_3d1a |
Folha |
SC23 |
Legenda_Completa |
117Pgu |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
117 |
Nome_Unidade |
Serras da Borda Ocidental da Chapada Diamantina |
Letra_Simbolo |
Pgu |
Categoria |
Pediplano degradado desnudado |
Natureza |
aplanamento |
Caracteristica |
degradado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras da Borda Ocidental da Chapada Diamantina |
Area_Poligono_Km2 |
6.221 |
the_geom |
MULTIPOLYGON (((-42.72939298686341 -11.464837977328127, -42.729317481758144 -11.464530289221917, -42.729050784367686 -11.463323177823018, -42.72895640522246 -11.462734046942568, -42.728485804055104 -11.46245478322874, -42.7273868002332 -11.462392777736438, -42.72661212746255 -11.4629653103365, -42.72622437826701 -11.463592873120202, -42.72583652955138 -11.46395754019737, -42.72500569902153 -11.464735541173418, -42.724596337971406 -11.46667137683569, -42.723204846629145 -11.46859960605672, -42.72240256158036 -11.47053363926106, -42.72160030244215 -11.47246677949038, -42.72119183468074 -11.474402642005787, -42.72117712932207 -11.47634211816262, -42.720968352854904 -11.477892687888843, -42.72115152484562 -11.479445910605659, -42.721138295010874 -11.48099689815587, -42.72132666499097 -11.482161777249022, -42.7213110304142 -11.484101213276016, -42.72129535810562 -11.486041537950099, -42.721083314002506 -11.48797873746096, -42.7210710131384 -11.48952975718252, -42.72145060503947 -11.49108520904763, -42.722225965762426 -11.49264167625726, -42.72319581454584 -11.49420208148674, -42.72377710679765 -11.495369641122121, -42.72376974418525 -11.496339818547282, -42.72435646950246 -11.49653890686946, -42.724360725329724 -11.497255554828538, -42.72522876573901 -11.498602601824544, -42.72658798836716 -11.500294755359501, -42.72679850881775 -11.501398988586367, -42.72794230051786 -11.502722799228307, -42.729309557096094 -11.503495583374885, -42.73029317050367 -11.504134151764964, -42.73094861792748 -11.504559553604816, -42.73276462068289 -11.504076177833422, -42.733050947594954 -11.502607023843794, -42.733502389406496 -11.501087201821433, -42.734825888587736 -11.500466302257827, -42.73581958000799 -11.499870111878147, -42.73927750501793 -11.499563159851707, -42.739879268282415 -11.498210418562946, -42.74028432921253 -11.496662955487952, -42.74088357237466 -11.495502602175714, -42.741716123679254 -11.494463521075412, -42.743066690246586 -11.492998820202764, -42.743665153984594 -11.492033592103644, -42.74367405845879 -11.490870096098034, -42.743110715002885 -11.49015953689623, -42.740926745016104 -11.490072719703537, -42.740669648319894 -11.489100372694953, -42.74173222316776 -11.487751122480384, -42.74342069878142 -11.485934957786638, -42.743919256591795 -11.484665561784748, -42.744916429794586 -11.483121291859039, -42.7457143602004 -11.481575582278271, -42.74631910215993 -11.479641017313286, -42.74672180390686 -11.478480208339386, -42.74673560485928 -11.476734975312956, -42.74615027123192 -11.476149223721416, -42.74536455658287 -11.476143021249117, -42.744771086400235 -11.476525634919637, -42.74378800265096 -11.476518063476847, -42.74221632689364 -11.476312254376499, -42.74163031835258 -11.475919847222487, -42.74064630717391 -11.475912229389227, -42.739466787984504 -11.475903311722874, -42.738477123344225 -11.47667166232488, -42.73827834148593 -11.477057890032889, -42.73788291626119 -11.47724850513948, -42.73709064865102 -11.478017330297785, -42.73668552256587 -11.479566576432685, -42.736278569725755 -11.481114859939128, -42.73548062366944 -11.482659654258581, -42.73428792111433 -11.484201702511678, -42.733890057657135 -11.48478165122733, -42.73349388880771 -11.485166502722574, -42.73309613459444 -11.48574378108272, -42.73269895846776 -11.486130374957247, -42.73269004391775 -11.4872929824628, -42.733075570055675 -11.488266725678717, -42.73359117061923 -11.489203599274722, -42.73345384658199 -11.490208868034891, -42.73316810648574 -11.490669268583975, -42.7316750709722 -11.491358479353336, -42.73048300155965 -11.492707155720531, -42.73008446058419 -11.493479560751434, -42.729883062792794 -11.494059951456233, -42.729490198107115 -11.49405638378801, -42.72870678878702 -11.493662577638833, -42.72811723964869 -11.493464279990064, -42.72793162156013 -11.492299516561214, -42.72794302797624 -11.490746682474601, -42.72834911388153 -11.489198378888963, -42.72816403389254 -11.487645093204865, -42.72817718586806 -11.486094997939675, -42.72838592697738 -11.484544426648556, -42.728401547805575 -11.482604100779412, -42.72821736434884 -11.481051737828292, -42.727826839953465 -11.480661497279891, -42.727833491730316 -11.47988466880507, -42.72803979669554 -11.478723435055137, -42.728638123026755 -11.477563065147363, -42.729041790577945 -11.476403205421098, -42.729443632629945 -11.47524238332233, -42.73004847785892 -11.473307848552553, -42.73103815425429 -11.472539525750948, -42.73164225145906 -11.470799229719939, -42.732046625896025 -11.469445120029523, -42.73186080788057 -11.468086071693328, -42.73147033455639 -11.467694944866272, -42.73030151220434 -11.466327388957168, -42.72998435493078 -11.465898094507844, -42.72959554911105 -11.465312756980596, -42.72939298686341 -11.464837977328127))) |
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_3d1b |
Folha |
SC23 |
Legenda_Completa |
117Pgi |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
117 |
Nome_Unidade |
Serras da Borda Ocidental da Chapada Diamantina |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras da Borda Ocidental da Chapada Diamantina |
Area_Poligono_Km2 |
45.505 |
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_3d1c |
Folha |
SC23 |
Legenda_Completa |
127DEa32 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
127 |
Nome_Unidade |
Serras Setentrionais do Espinhaço |
Letra_Simbolo |
DEa |
Categoria |
Estrututral aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo aguçado |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras Setentrionais do Espinhaço |
Area_Poligono_Km2 |
58.101 |
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_3d1d |
Folha |
SC23 |
Legenda_Completa |
197Dt32 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
197 |
Nome_Unidade |
Vãos da Bacia 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 |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
32.586 |
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_3d1e |
Folha |
SC23 |
Legenda_Completa |
197Dt31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
197 |
Nome_Unidade |
Vãos da Bacia do Alto ParnaÃba |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
48.189 |
the_geom |
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