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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 SE.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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58c0 |
Folha |
SE23 |
Legenda_Completa |
514Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies do São Francisco |
Identificacao_Unidade |
514 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais do Rio São Francisco |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais do Rio São Francisco |
Area_Poligono_Km2 |
1.474 |
the_geom |
MULTIPOLYGON (((-44.51059632837838 -17.17892813421097, -44.50973411424594 -17.179256873705018, -44.508838499708666 -17.17976992644884, -44.50752724820915 -17.18028286505651, -44.506630864654205 -17.18108244620775, -44.50585499110722 -17.181824467882723, -44.50549659506235 -17.1822249270892, -44.505136650087714 -17.182854071689736, -44.50495570305684 -17.18371234468583, -44.50447714398528 -17.184741629989755, -44.50435665103883 -17.18514267105906, -44.50429527598408 -17.185944290409804, -44.50357569175983 -17.18743126408581, -44.50303754057951 -17.188231708829584, -44.50303479269794 -17.18926216151324, -44.5032719707243 -17.18989277224768, -44.50332953585719 -17.19052294046891, -44.503506379490055 -17.19121034875092, -44.50362413107248 -17.19184066499714, -44.50403874411322 -17.192586508219286, -44.504693746577615 -17.19275986123441, -44.505468790802134 -17.192703912983553, -44.506138141972635 -17.192431668011718, -44.50638616637629 -17.19216833298137, -44.5067555539604 -17.191885408423335, -44.50708751111249 -17.191531886538183, -44.50753052662341 -17.191143382710344, -44.50775226889272 -17.1908600956361, -44.50804717243205 -17.190648395826845, -44.50826881791033 -17.19040126439284, -44.50852797949726 -17.189835143070823, -44.50893393468502 -17.189233222294217, -44.50915651053256 -17.188631758353665, -44.509527004952524 -17.187923992136795, -44.51052237996549 -17.187394909278254, -44.51148050648384 -17.186723816817793, -44.51214495202642 -17.18615867134137, -44.51283051168233 -17.18578881978714, -44.513249962685435 -17.185771754017058, -44.51409704743218 -17.185845205247723, -44.514818900840254 -17.18634228715157, -44.51533339407152 -17.186662605330373, -44.51597043484241 -17.18723088858557, -44.516338876518205 -17.18730318148786, -44.516836283546105 -17.187324259598135, -44.517468737796754 -17.18712420075434, -44.518328570645544 -17.186634526656118, -44.51924971659131 -17.186069970042517, -44.52012109647142 -17.185109376351388, -44.52070304611963 -17.184798005496297, -44.521010610276136 -17.184407341118472, -44.5214917428753 -17.184171657303303, -44.52180921469303 -17.1839500471006, -44.52192035789348 -17.183879805179256, -44.52239972772605 -17.183597111402992, -44.52271043681496 -17.18344508512865, -44.52288937758072 -17.183338846448166, -44.52288561615569 -17.183338837553332, -44.522099774972794 -17.183221276656408, -44.521081855305525 -17.183029944916, -44.519931757701336 -17.18267920472751, -44.51940740552578 -17.182171764497703, -44.51773186508301 -17.181377745754183, -44.516385991101465 -17.18074178475702, -44.51487424783803 -17.180612511944982, -44.51382283081976 -17.180293611649528, -44.51247570740919 -17.17978416988905, -44.511327248429424 -17.179181193438012, -44.51059632837838 -17.17892813421097))) |
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 SE.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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58bf |
Folha |
SE23 |
Legenda_Completa |
149Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
149 |
Nome_Unidade |
Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
21.881 |
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 SE.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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58be |
Folha |
SE23 |
Legenda_Completa |
149Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
149 |
Nome_Unidade |
Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
3.372 |
the_geom |
MULTIPOLYGON (((-42.32942544986063 -17.15644011171253, -42.32926939203783 -17.160648422630025, -42.33026950948517 -17.163956259306435, -42.32824322915839 -17.165851295146087, -42.326023605221 -17.167927077094284, -42.32617096559753 -17.170949978803723, -42.32824368393093 -17.172441404481248, -42.32935572538208 -17.174561314937748, -42.33189294661738 -17.176883415629426, -42.335946378645254 -17.17968251092117, -42.33794139251273 -17.17998340864482, -42.33952984184062 -17.18210957041875, -42.34228056247628 -17.182786167855802, -42.34350038030246 -17.1840837894631, -42.345021810890564 -17.184195047229693, -42.344859803221624 -17.1821798276492, -42.34535561879978 -17.18081359154596, -42.3452842217052 -17.17916443086196, -42.346439501088554 -17.178264759707435, -42.348925465440445 -17.17747379346024, -42.34733786864986 -17.175347707892193, -42.34506904700135 -17.174219644799255, -42.34432420754916 -17.173019508584872, -42.34508729637217 -17.1729383364627, -42.347672905519225 -17.17187413500431, -42.34597261217034 -17.170936896857658, -42.34312754241793 -17.170167007442835, -42.342670875418456 -17.168788229758878, -42.34239706566354 -17.167960965495293, -42.34127837924895 -17.166298010209427, -42.339480690761036 -17.16554277982297, -42.33730690707429 -17.164415902114463, -42.33608426521464 -17.16339277684391, -42.33457479870722 -17.16245707419004, -42.334586565635306 -17.161633575576495, -42.33394453464877 -17.159886572691367, -42.33184702834915 -17.160133409783924, -42.33158637091219 -17.158390540152194, -42.32942544986063 -17.15644011171253))) |
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 SE.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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58bd |
Folha |
SE23 |
Legenda_Completa |
549Da51 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
549 |
Nome_Unidade |
Patamares das Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
39.996 |
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 SE.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 |
GeomorfologiaSE23.fid-6d9cbe3e_18e3b3f16e6_-58bc |
Folha |
SE23 |
Legenda_Completa |
524DEc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
68.215 |
the_geom |
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