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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_3d16 |
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 |
10.835 |
the_geom |
MULTIPOLYGON (((-42.377540503679796 -11.394866232356682, -42.375891680136014 -11.394715951861102, -42.3741129561618 -11.395670061779255, -42.37295003631441 -11.393914408572401, -42.37315405183358 -11.393140037279021, -42.37238098595916 -11.391775994424112, -42.36982826335287 -11.391559391396765, -42.36863286850968 -11.393294234830744, -42.366426022529424 -11.398121433149596, -42.36580813890034 -11.401219660801567, -42.36383299280561 -11.402171232980916, -42.36286742193431 -11.400417164963619, -42.3627209382829 -11.39498556979197, -42.363150021840724 -11.391112476353511, -42.362967089363124 -11.389559805682977, -42.36139907558711 -11.389157771043372, -42.36079846532625 -11.390316491935085, -42.359800398552466 -11.392051144407624, -42.35840850730439 -11.39329329176239, -42.35729027430177 -11.394515148226782, -42.35681684547905 -11.395596046024597, -42.35593562256267 -11.396227551693018, -42.355567322559 -11.397160239107244, -42.35537248432748 -11.39868537472504, -42.35473841466376 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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_3d17 |
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 |
2.956 |
the_geom |
MULTIPOLYGON (((-42.7212590931137 -11.459905226186276, -42.72291456655154 -11.455778008338278, -42.72351219488325 -11.454832384971162, -42.724303540702536 -11.454062665918718, -42.72628277850683 -11.452526047205556, -42.727473723039445 -11.451178226396062, -42.72767420162297 -11.4505969046919, -42.72807524046901 -11.44963121028563, -42.728083515841995 -11.448661055738315, -42.72769473920917 -11.448075712768892, -42.72632364685886 -11.447290273559775, -42.72513937262894 -11.447861255662998, -42.724545125772345 -11.448439855568555, -42.72395091383862 -11.449017564454376, -42.723162022043354 -11.449397940484134, -42.721783605194055 -11.449581780873487, -42.7211967179597 -11.449190183575036, -42.720609907446764 -11.448796805626111, -42.72062220911067 -11.447245767888486, -42.72102023713065 -11.446860111725924, -42.7214253293731 -11.445312652177659, -42.72162670883045 -11.44473225923096, -42.722218357344396 -11.444347837842235, -42.72241733069847 -11.444155898299238, -42.72261537413777 -11.44396392272507, -42.723997753376224 -11.443199194212717, -42.72538345368585 -11.442046040533901, -42.72676914205943 -11.440892879896042, -42.72696791367002 -11.440506655987237, -42.72717020711422 -11.439926294275567, -42.72756964387454 -11.439153027535983, -42.72797472408072 -11.437604665697627, -42.72838072920474 -11.436056338458743, -42.728785762562545 -11.434508863801508, -42.72919179577403 -11.432959644302016, -42.72979326234908 -11.431412616385545, -42.73019264136574 -11.430640233837694, -42.73074764701138 -11.42982038421172, -42.72982200947511 -11.427922139302686, -42.7296279999717 -11.42753234428599, -42.72923758904806 -11.427141209851392, -42.72845693013298 -11.426554110887418, -42.727281688233774 -11.425962477570604, -42.72688702688312 -11.42595972431394, -42.72629050948485 -11.426925008187352, -42.726089887835094 -11.42731116143753, -42.72509064627986 -11.429437239908628, -42.72448822738724 -11.43098422317476, -42.723885801533626 -11.432531204489425, -42.723364652838036 -11.433541275389214, -42.72149025889742 -11.43716636024964, -42.718124326162226 -11.440146558487504, -42.71773020341166 -11.440240951379375, -42.717331514821026 -11.440819069549955, -42.7171336211846 -11.441206212487954, -42.716933716615024 -11.44139811269689, -42.71673400024736 -11.441784293776955, -42.716337832844125 -11.442170016486026, -42.71612244519295 -11.444495654862905, -42.71610770475488 -11.446435147458901, -42.715897325886026 -11.448178156304165, -42.715302166228675 -11.448755811746283, -42.715286527482355 -11.45069437627078, -42.715078108081315 -11.452147830933216, -42.71525279763886 -11.454960844586655, -42.715629930623976 -11.456903882188895, -42.716595195183466 -11.459143218098928, -42.7179543346987 -11.461383499877456, -42.71907893748201 -11.46169961850563, -42.7212590931137 -11.459905226186276))) |
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_3d18 |
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 |
14.382 |
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_3d19 |
Folha |
SC23 |
Legenda_Completa |
127Pgi |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
127 |
Nome_Unidade |
Serras Setentrionais do Espinhaço |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras Setentrionais do Espinhaço |
Area_Poligono_Km2 |
44.987 |
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_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 |
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