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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_375b |
Folha |
SC23 |
Legenda_Completa |
352Dc41 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
352 |
Nome_Unidade |
Patamares do Chapadão Ocidental Baiano |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares do Chapadão Ocidental Baiano |
Area_Poligono_Km2 |
25.529 |
the_geom |
MULTIPOLYGON (((-47.41675161350207 -9.34882912653225, -47.41147424862592 -9.345725141044083, -47.4107516165539 -9.344686690282973, -47.410524666466706 -9.341611921786088, -47.41086984115759 -9.339574853683523, -47.41264769532272 -9.333767676053558, -47.41178271808736 -9.332433462158708, -47.41089992271875 -9.331830129163738, -47.40851340843304 -9.331776711924519, -47.406461408906175 -9.330123834086608, -47.40617665690244 -9.329533208859294, -47.40670515651863 -9.326038600793979, -47.40843761262306 -9.322129934305504, -47.40833615946065 -9.32008177496514, -47.40762074192735 -9.318750934906847, -47.40612140721419 -9.319010209916499, -47.4043453933186 -9.318386507936347, -47.40467014846734 -9.31079460330897, -47.404249282764695 -9.30961582065583, -47.4033710706485 -9.308866293254912, -47.401577301155584 -9.308972577038247, -47.398547546508716 -9.310804917004893, -47.39640135009426 -9.313241525008552, -47.39527569171048 -9.316722538039171, -47.39390534840179 -9.31786136179698, -47.39152424472826 -9.317516295837232, -47.38970989804383 -9.318498706386437, -47.3878785946102 -9.320211125832293, -47.38724762436492 -9.321658424538729, -47.38136862559304 -9.321287781634643, -47.377643045563005 -9.330212716084583, -47.375064979840445 -9.331908854179622, -47.373666735017906 -9.334216106557452, -47.37336865241602 -9.33420928601034, -47.372750203262 -9.341502671386996, -47.372146871033934 -9.341780487265119, -47.36738792013001 -9.347373775266632, -47.36628680820731 -9.349834023797596, -47.36595016444284 -9.351434238806789, -47.36621518058724 -9.35290108498403, -47.368696783328076 -9.355295329797988, -47.37003968745929 -9.355324289981679, -47.370789923771575 -9.355195207322355, -47.37109786809782 -9.354763489013761, -47.37199402966217 -9.354783998606013, -47.37476496464481 -9.357620896880038, -47.37834600269486 -9.357701006022983, -47.38172754035596 -9.359968551775344, -47.38336948152315 -9.36000517421675, -47.38519394589553 -9.358584299965605, -47.38700590070055 -9.35774903901373, -47.391354157698025 -9.356968082087326, -47.39326653317605 -9.358179966818085, -47.39355221009144 -9.35877061049022, -47.393917796717474 -9.362286381951055, -47.39357957188005 -9.364032825738802, -47.39218226368935 -9.366339230338037, -47.387443843393065 -9.371055673996887, -47.387385798212655 -9.37353975881234, -47.388199003262095 -9.377064818820052, -47.38842572902674 -9.380139506761743, -47.390325836539745 -9.381934325837834, -47.39283915713396 -9.383013642627489, -47.39673654269837 -9.38236947256236, -47.39874804714919 -9.379344924505437, -47.3988157399586 -9.376424099106988, -47.397965007901384 -9.374504319314475, -47.39503077935387 -9.372248092116761, -47.395214179289006 -9.370790635443047, -47.39627234645454 -9.370230641605875, -47.396434339947824 -9.369648430101211, -47.39897070908563 -9.369705352656458, -47.402583967877256 -9.37490028262703, -47.40390737913359 -9.375807045423688, -47.40924291073755 -9.377531920740182, -47.41105399526275 -9.376696502577397, -47.411692075755056 -9.374957772671427, -47.411773889124774 -9.371452245905179, -47.412742031914206 -9.368258481512433, -47.41410634626927 -9.367411986215176, -47.41764761384062 -9.36924306418299, -47.41927985529687 -9.369718020015982, -47.420667191000355 -9.367850029791551, -47.42302699131824 -9.362642063280456, -47.42325726978488 -9.359138977426172, -47.42242944528608 -9.356197763541408, -47.42096813477492 -9.354850063348826, -47.42083191648907 -9.354262841018466, -47.41775657033583 -9.353365375674345, -47.41606849737029 -9.3510555899493, -47.41675161350207 -9.34882912653225))) |
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_375c |
Folha |
SC23 |
Legenda_Completa |
352Dc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
352 |
Nome_Unidade |
Patamares do Chapadão Ocidental Baiano |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares do Chapadão Ocidental Baiano |
Area_Poligono_Km2 |
19.653 |
the_geom |
MULTIPOLYGON (((-44.77921409260608 -11.801745702873884, -44.77962809950715 -11.800525817532979, -44.77839575910317 -11.794016762856405, -44.777572443174805 -11.78954013872076, -44.77716071097872 -11.78791205300167, -44.77468434229892 -11.787096364076572, -44.77138221471063 -11.78587421748909, -44.77138229012409 -11.785467101613753, -44.76890926540291 -11.781398082409588, -44.76849653856999 -11.780583295313347, -44.76725793397077 -11.780175401570858, -44.76643323106664 -11.779360973691295, -44.764781721868964 -11.778953401148454, -44.76271718922165 -11.779358599409761, -44.76230100812921 -11.781799755628764, -44.76312544628876 -11.784239989322053, -44.76394992472682 -11.786274883496922, -44.76436174616742 -11.787088756844254, -44.76477227314274 -11.789936398442533, -44.76394519586636 -11.791563709487253, -44.76394496639877 -11.792784165712854, -44.766007298561256 -11.79481981286265, -44.766417937909075 -11.797260333011996, -44.768068600834255 -11.797668755398513, -44.76806724841357 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-11.801745702873884))) |
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_375d |
Folha |
SC23 |
Legenda_Completa |
352DEc42 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
352 |
Nome_Unidade |
Patamares do Chapadão Ocidental Baiano |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares do Chapadão Ocidental Baiano |
Area_Poligono_Km2 |
7.343 |
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_375e |
Folha |
SC23 |
Legenda_Completa |
353Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
353 |
Nome_Unidade |
Chapadão Ocidental Baiano |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadão Ocidental Baiano |
Area_Poligono_Km2 |
1.619 |
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_375f |
Folha |
SC23 |
Legenda_Completa |
352DEt32 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
352 |
Nome_Unidade |
Patamares do Chapadão Ocidental Baiano |
Letra_Simbolo |
DEt |
Categoria |
Estrutural tabular |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo tabular |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares do Chapadão Ocidental Baiano |
Area_Poligono_Km2 |
102.387 |
the_geom |
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