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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_-55ae |
Folha |
SE23 |
Legenda_Completa |
519Dc41 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Depressões do São Francisco |
Identificacao_Unidade |
519 |
Nome_Unidade |
Depressão do Alto Rio São Francisco |
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 |
Depressão do Alto Rio São Francisco |
Area_Poligono_Km2 |
399.298 |
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_-55ad |
Folha |
SE23 |
Legenda_Completa |
000Magua |
Nome_Dominio |
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Nome_Regiao |
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Identificacao_Unidade |
0 |
Nome_Unidade |
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Letra_Simbolo |
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Categoria |
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Aprofundamento_Incisoes |
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Nivel_Altimetrico |
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Corpo d´água continental |
Area_Poligono_Km2 |
0.244 |
the_geom |
MULTIPOLYGON (((-42.46730662225355 -19.668425505910502, -42.4678316698638 -19.668377825674934, -42.4684217890115 -19.667889485676277, -42.46918371901228 -19.66756881679232, -42.46970616997613 -19.66768634645014, -42.471048685197594 -19.667484016307046, -42.471863637242116 -19.667550574162167, -42.473085531955796 -19.667623757521056, -42.473498635093875 -19.667298160998932, -42.47462070936557 -19.666319716329824, -42.47545113794301 -19.66533716426792, -42.475523102613316 -19.66445502077302, -42.47512220676711 -19.664062892837013, -42.47454164020247 -19.66394365959765, -42.47383864458748 -19.66415501440354, -42.47307501171176 -19.664585850146995, -42.47248491813594 -19.665074208516092, -42.471669114039884 -19.665062726845473, -42.470973990943385 -19.664832604092044, -42.469812848766324 -19.664595011886192, -42.46923140754447 -19.664531736434196, -42.468585763402984 -19.664854045906527, -42.468401814313985 -19.66545918416867, -42.46821604545454 -19.666119380484364, -42.467564321459825 -19.66682809098518, -42.467030609400716 -19.667427391907825, -42.466962923344006 -19.668034167434683, -42.46730662225355 -19.668425505910502))) |
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_-55ac |
Folha |
SE23 |
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525Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Quadrilátero FerrÃfero |
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525 |
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aplanamento |
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degradado inumado |
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Nivel_Altimetrico |
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Serras do Quadrilátero FerrÃfero - Pará de Minas |
Area_Poligono_Km2 |
2.663 |
the_geom |
MULTIPOLYGON (((-44.70191113281651 -19.687706032987986, -44.70429439585206 -19.686708682034475, -44.70562275606418 -19.683954600776417, -44.70668086580977 -19.684457881837346, -44.7093287830235 -19.683209668094165, -44.709858292145846 -19.68321052431798, -44.713836124669406 -19.678205923172335, -44.71357274496309 -19.67770485676038, -44.7109253453151 -19.678201262566347, -44.708014113299804 -19.67844687727342, -44.70316531364596 -19.677597591424508, -44.700313682773924 -19.68016657544264, -44.699594899957354 -19.67934662866198, -44.69729179017481 -19.67784082403347, -44.695274594662806 -19.677018667441544, -44.69397840578974 -19.67633417568825, -44.69095432106829 -19.675237337580583, -44.68893587476565 -19.675097396429756, -44.685764976657566 -19.674955420602135, -44.68259381630889 -19.674949845991414, -44.68057714748385 -19.67440044149307, -44.67899347545889 -19.67344241595136, -44.67668954930292 -19.67248308198985, -44.67546126124416 -19.67319568821943, -44.67437104347398 -19.6716709941554, -44.67369967274976 -19.67060613029517, -44.672579720749226 -19.66964708283866, -44.671458699476446 -19.66921939765835, -44.67022315539233 -19.66974940925857, -44.669772386499 -19.670917959114156, -44.67001832464257 -19.67101239490869, -44.67104403020025 -19.671402863246897, -44.671209800874344 -19.67151341709789, -44.673257187888005 -19.67287630492132, -44.674184383344084 -19.67764677127801, -44.67775307976959 -19.678781016094813, -44.68251272566168 -19.679792589996122, -44.68277674966407 -19.67991866968175, -44.68957506067476 -19.680056160717314, -44.69578738587268 -19.68182176129629, -44.69591976502894 -19.68194669507463, -44.69829334200422 -19.68558625394505, -44.699035487381956 -19.685657987318105, -44.70191113281651 -19.687706032987986))) |
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_-55ab |
Folha |
SE23 |
Legenda_Completa |
566Dc21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Patamares Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
566 |
Nome_Unidade |
Patamares Dissecados do Planalto de Cristalina |
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 Dissecados do Planalto de Cristalina |
Area_Poligono_Km2 |
45.861 |
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_-55aa |
Folha |
SE23 |
Legenda_Completa |
523Dt11 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco-ParanaÃba |
Identificacao_Unidade |
523 |
Nome_Unidade |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
muito baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
54.56 |
the_geom |
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