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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_3c06 |
Folha |
SC23 |
Legenda_Completa |
197DEc41 |
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 |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
42.412 |
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_3c07 |
Folha |
SC23 |
Legenda_Completa |
197DEc41 |
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 |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
6.539 |
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_3c08 |
Folha |
SC23 |
Legenda_Completa |
197Dt21 |
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 |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
36.504 |
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_3c09 |
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 |
3.781 |
the_geom |
MULTIPOLYGON (((-42.45761920584499 -11.835382840275548, -42.458134460057494 -11.833601330824276, -42.4580038905006 -11.833105175690482, -42.45821357777009 -11.831748258288954, -42.45802979173097 -11.830195813787794, -42.45586993193882 -11.829594648209337, -42.45507580959174 -11.830362646263145, -42.45468059102611 -11.830552899438684, -42.45310060644329 -11.831120569827211, -42.45211805451806 -11.830918718095855, -42.45252629272884 -11.829370029315603, -42.45293351838963 -11.827823081996828, -42.45353836398162 -11.826277694906185, -42.45434086452944 -11.824732977218922, -42.45435472816224 -11.82318208900572, -42.454167317569194 -11.822210504277985, -42.453188526709745 -11.821620275598402, -42.45162247110118 -11.820637050048246, -42.4502503902893 -11.820041980493638, -42.44936857771366 -11.819646265846854, -42.446930911513725 -11.817104788181103, -42.44693464965489 -11.816716407709032, -42.44596057330572 -11.815543546691526, -42.445568132629596 -11.815540524162119, -42.443996565573755 -11.815138938028737, -42.44379434303781 -11.815718198734253, -42.443198708506436 -11.816295286364198, -42.44299831681755 -11.816681245780398, -42.44279792455008 -11.817067205032382, -42.44178619641654 -11.820063283622748, -42.44158439792378 -11.820546318456962, -42.441381185357606 -11.821320693348923, -42.44117431348153 -11.822287405252215, -42.441364480978365 -11.823064845079392, -42.441554649581235 -11.82384228467377, -42.44194428782552 -11.8242337292594, -42.44213816568406 -11.824623678058028, -42.443696723835764 -11.826383713218526, -42.44427382302635 -11.827744965958146, -42.44387302500926 -11.828516884498844, -42.44347499860588 -11.828901275640153, -42.44327459786659 -11.829287234365504, -42.44248227416366 -11.829861898143058, -42.44208048756172 -11.8308289300308, -42.44127052016183 -11.833147702209448, -42.4408019329036 -11.83492568344179, -42.44065813158528 -11.835468930704543, -42.44064602314476 -11.836826514961137, -42.44122960342 -11.837607018748914, -42.44162206528825 -11.837804310110242, -42.44318445080883 -11.838981702045203, -42.44356759626298 -11.84014904825529, -42.44395448787282 -11.840928014973949, -42.44434134326061 -11.841707870670803, -42.44433300470952 -11.842482812090795, -42.4459065645494 -11.842691094716962, -42.446303677011386 -11.84230666444768, -42.44709229112817 -11.842120370329908, -42.44729736490988 -11.841346067860632, -42.44829198294357 -11.840191241553134, -42.44848864841216 -11.840193659024921, -42.448700219018086 -11.838643450251741, -42.44969201747681 -11.837877034438131, -42.45047878798066 -11.837884030982005, -42.45024964489837 -11.841372614008492, -42.450085015210185 -11.84239802685539, -42.45093433430503 -11.843655051287708, -42.451398301604954 -11.844873694868976, -42.452173581811934 -11.844499726709127, -42.45430146583067 -11.84368545375266, -42.45544088508832 -11.8417904554005, -42.45632328714691 -11.840728307208433, -42.45633464528496 -11.83953733520625, -42.4571030310046 -11.837401348762292, -42.45761920584499 -11.835382840275548))) |
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_3c0a |
Folha |
SC23 |
Legenda_Completa |
197Pri |
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 |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
20.82 |
the_geom |
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