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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 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_-5a9a |
Folha |
SE23 |
Legenda_Completa |
512Kd |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
512 |
Nome_Unidade |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Letra_Simbolo |
Kd |
Categoria |
Carste descoberto |
Natureza |
dissolução |
Caracteristica |
carste descoberto |
Forma |
carste |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Area_Poligono_Km2 |
41.711 |
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_-5a99 |
Folha |
SE23 |
Legenda_Completa |
512Da43 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Serras e Patamares do São Francisco |
Identificacao_Unidade |
512 |
Nome_Unidade |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Patamares das Chapadas dos Rios Urucuia - Paracatu |
Area_Poligono_Km2 |
66.479 |
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_-5a98 |
Folha |
SE23 |
Legenda_Completa |
195Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
195 |
Nome_Unidade |
Maciços de Pedra Azul |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Maciços de Pedra Azul |
Area_Poligono_Km2 |
0.851 |
the_geom |
MULTIPOLYGON (((-42.02070513329482 -16.381162834500632, -42.02118955570279 -16.38116969797815, -42.021918808275224 -16.38094615703968, -42.022483656049566 -16.380954156545414, -42.02280984534347 -16.38072490410233, -42.023139586008774 -16.38026182992284, -42.02322593558391 -16.379872965702642, -42.023230666791925 -16.379561505119604, -42.02363964965377 -16.379177207574532, -42.02404506653317 -16.37902763306777, -42.02477406565213 -16.378881733118032, -42.025097878186045 -16.3788086580329, -42.02534482865544 -16.378499720375302, -42.02575143528597 -16.37827159969698, -42.02591701076871 -16.377962413172146, -42.02609180837586 -16.377107053600803, -42.02610599920849 -16.3761717663445, -42.02611191634849 -16.375781762364074, -42.02604332695549 -16.375000617235838, -42.0254855905157 -16.374524986655814, -42.02517006016966 -16.374052780594017, -42.024536646975584 -16.373263646925245, -42.02413621418928 -16.373024110653507, -42.023740267219004 -16.372550765607194, -42.02359007226514 -16.371847025722197, -42.02360072080844 -16.371145561539997, -42.02352409232976 -16.370832949563724, -42.02353120481322 -16.37036440397952, -42.0235406603569 -16.369741482067344, -42.02354658014078 -16.369351478761857, -42.02355604872018 -16.368727653995723, -42.02372964895335 -16.36795083843915, -42.02389995585681 -16.367329288415455, -42.02398959873945 -16.36678425352579, -42.023997872603566 -16.366238970745584, -42.02368235606812 -16.365766764914575, -42.02344608176097 -16.365373335897925, -42.02296524618782 -16.3651326626394, -42.02240492825922 -16.364890863875484, -42.022082318094775 -16.364886299037057, -42.02167835420725 -16.36488058237035, -42.02151751677829 -16.364878306074953, -42.021194906895914 -16.364873739880764, -42.02111448821651 -16.364872601564226, -42.02087111793655 -16.364946812585266, -42.02070816622137 -16.36502216180604, -42.020547328818914 -16.36501988475064, -42.020143107130416 -16.365092720457444, -42.01909274433546 -16.36515550082336, -42.01884817960484 -16.36530825134404, -42.01852438966219 -16.36538132016664, -42.01811780650844 -16.365609430115956, -42.018111877368774 -16.36599943162571, -42.017863755762214 -16.36638600098005, -42.01785427052387 -16.367009822640572, -42.01809172807055 -16.36732471441029, -42.018731025594704 -16.367723858808077, -42.01905363943472 -16.367728429548997, -42.01937387967178 -16.367889181107326, -42.019614894260165 -16.36797025109588, -42.01985471554856 -16.368129862918913, -42.02008980450719 -16.368600934554664, -42.02000489611123 -16.368833603009392, -42.01967517292778 -16.369296674649412, -42.01943060278794 -16.369449425018633, -42.019186981140784 -16.369601285505112, -42.01886198978478 -16.36975289567032, -42.01869428408859 -16.370140604879094, -42.01877114977185 -16.3703755648672, -42.01876996934205 -16.370453204069236, -42.01892937158468 -16.37061167767342, -42.019652655972926 -16.37077814022094, -42.01989130030581 -16.3710153918134, -42.02028842786516 -16.371410200047713, -42.02028132087961 -16.371877841415575, -42.02035675042466 -16.37226899584684, -42.020751494091655 -16.37282088795087, -42.020988962273954 -16.373135778224132, -42.021464131560904 -16.37368880849083, -42.0216164473136 -16.374314019847997, -42.02161289476671 -16.37454784075395, -42.02159749058403 -16.37556166646765, -42.02158683184458 -16.37626312907315, -42.02125827626718 -16.376648562137554, -42.02084600031496 -16.37718812057659, -42.020599980857774 -16.377497065328633, -42.01978700722514 -16.37787563189596, -42.01905420912502 -16.37833298724399, -42.0189704880061 -16.37848711225888, -42.018797774280834 -16.37926483460027, -42.019261097335324 -16.380596970973013, -42.01990256613543 -16.38091759017894, -42.02070513329482 -16.381162834500632))) |
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_-5a97 |
Folha |
SE23 |
Legenda_Completa |
177Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
177 |
Nome_Unidade |
Patamares da Borda Ocidental do Espinhaço |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Patamares da Borda Ocidental do Espinhaço |
Area_Poligono_Km2 |
16.948 |
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_-5a96 |
Folha |
SE23 |
Legenda_Completa |
177Dc21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
177 |
Nome_Unidade |
Patamares da Borda Ocidental do Espinhaço |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Patamares da Borda Ocidental do Espinhaço |
Area_Poligono_Km2 |
0.153 |
the_geom |
MULTIPOLYGON (((-43.66400400164892 -16.766680173086094, -43.66368914769985 -16.765958730293608, -43.66188173897841 -16.76484169398057, -43.660352018297715 -16.76519959330702, -43.657578073434856 -16.765734654747927, -43.65547259765606 -16.766457504087803, -43.655369303546856 -16.76647219437087, -43.655451515845535 -16.76652063037974, -43.6559048366311 -16.766623001379273, -43.65621425573148 -16.766644901680216, -43.656586099595614 -16.76672776089618, -43.656977091111244 -16.76688937212788, -43.65736919958579 -16.766891926558866, -43.65774091143204 -16.766993762047587, -43.65798688547492 -16.76723395876472, -43.65794365182051 -16.76751294199588, -43.65771538534484 -16.767690401916717, -43.6577966794167 -16.767869877617493, -43.65804307298936 -16.768050428285484, -43.6583710152949 -16.767973031476977, -43.658828346118156 -16.767637997993916, -43.65947298746142 -16.76694538503783, -43.65985125285932 -16.76611185749125, -43.66016234917157 -16.76589426365962, -43.660490867783416 -16.766135897797188, -43.660632683890356 -16.766514595264535, -43.66058875831839 -16.76689298955736, -43.66075173294255 -16.76733147328924, -43.6611219469292 -16.767513728669798, -43.661348958217644 -16.767515203130877, -43.66165963814194 -16.76735725325048, -43.66205532827158 -16.766982045966802, -43.66259176017021 -16.767005410173347, -43.66279218630094 -16.767186560907735, -43.6628798146189 -16.76726575743693, -43.66287842499627 -16.76746457800923, -43.663124678090654 -16.767665908703663, -43.66343410053718 -16.76768779834197, -43.66372427442486 -16.767510733091267, -43.66386744957015 -16.76729294863024, -43.663932876495075 -16.767193054132147, -43.66400400164892 -16.766680173086094))) |
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