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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_-5db8 |
Folha |
SE23 |
Legenda_Completa |
548Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
548 |
Nome_Unidade |
Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
4.063 |
the_geom |
MULTIPOLYGON (((-46.11132532395059 -18.528915168740564, -46.11407249225276 -18.5262629636943, -46.119095705624744 -18.52575434029523, -46.121845208759545 -18.52334149000745, -46.125366520857256 -18.523800412209614, -46.12764589372862 -18.526422850544773, -46.13317205257164 -18.525909949682678, -46.137428460937016 -18.523488746505507, -46.13791402604397 -18.52084980926868, -46.13865218181302 -18.518448823330534, -46.14189695818194 -18.5150748219519, -46.141882648031725 -18.512917840817142, -46.13962230103197 -18.513171851554187, -46.13637276180647 -18.515826518888577, -46.133366255000745 -18.51728230869077, -46.1303502512546 -18.51730036182204, -46.126078204843836 -18.51732585102344, -46.12354953774405 -18.51494524398406, -46.11927598247508 -18.51473111084081, -46.115251890004 -18.514275030814556, -46.11347799545266 -18.512129302396772, -46.10996003685029 -18.512149980418418, -46.10471136318813 -18.51673346078451, -46.104978712411366 -18.51912755931906, -46.10599145310156 -18.5203199196486, -46.108019466722745 -18.522944082159125, -46.10753806027747 -18.526301365584562, -46.11132532395059 -18.528915168740564))) |
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_-5db7 |
Folha |
SE23 |
Legenda_Completa |
555Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
555 |
Nome_Unidade |
Planalto Dissecado do Centro - sudeste Goiano |
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 |
Planalto Dissecado do Centro - sudeste Goiano |
Area_Poligono_Km2 |
19.045 |
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_-5db6 |
Folha |
SE23 |
Legenda_Completa |
548Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
548 |
Nome_Unidade |
Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
1.277 |
the_geom |
MULTIPOLYGON (((-46.553074443609376 -18.34635391473033, -46.55251184041121 -18.346291634885596, -46.55067765672174 -18.345500586972513, -46.548987360942085 -18.3452459730856, -46.54828677408227 -18.345520025157274, -46.54617903480937 -18.34567176805889, -46.54505884862711 -18.346217572074966, -46.543939601153866 -18.346763362330517, -46.542121174942785 -18.34785152551465, -46.542137853408086 -18.349730813596395, -46.54215095703538 -18.351207138675097, -46.54145867118665 -18.35242081204686, -46.54133530335009 -18.354300329347634, -46.541908060903964 -18.355503765323366, -46.5438820994257 -18.356158224061193, -46.544869475227905 -18.356418578505465, -46.546406002937104 -18.35533267376831, -46.54724283318177 -18.354520801050604, -46.54878650606883 -18.35423989830047, -46.55075430931421 -18.354089259065447, -46.55258378221429 -18.35434271695851, -46.554397397337716 -18.352717776469486, -46.554528772461836 -18.351643270290687, -46.55437218524951 -18.349899764975873, -46.55463878855334 -18.348287438135728, -46.554348173739484 -18.347215470438382, -46.553637993214856 -18.34641618516988, -46.553074443609376 -18.34635391473033))) |
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_-5db5 |
Folha |
SE23 |
Legenda_Completa |
548Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas do São Francisco |
Identificacao_Unidade |
548 |
Nome_Unidade |
Chapadas do Alto Rio São Francisco |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Alto Rio São Francisco |
Area_Poligono_Km2 |
3.408 |
the_geom |
MULTIPOLYGON (((-46.00174185797684 -18.35314921764157, -46.00451697312071 -18.35221010182166, -46.006573829553034 -18.352429696443746, -46.008023954088706 -18.352307258312774, -46.00922267370733 -18.350450999237275, -46.00921260250572 -18.34871681431348, -46.01150361870686 -18.347548811642547, -46.013197032785904 -18.34777116906847, -46.015134066519806 -18.348223565777648, -46.017069347921236 -18.348213248008406, -46.01924228666266 -18.347738936327072, -46.01971840866139 -18.346464858822934, -46.01922331038828 -18.344502824213244, -46.019214499232596 -18.34299998818808, -46.0219875737211 -18.341597935489148, -46.0247623825872 -18.340658538026734, -46.02717703492984 -18.339951489763255, -46.027410833885966 -18.338679604494494, -46.025231632160505 -18.33822863114923, -46.022818615502004 -18.339050417556628, -46.01967027581156 -18.33825845238401, -46.017491364229755 -18.337691711823027, -46.01470549684151 -18.336897727947186, -46.012403476505916 -18.33598545786117, -46.0107085601885 -18.335647419815146, -46.00804722211221 -18.335430153632327, -46.00562680406833 -18.334981130639697, -46.0037026122444 -18.33672460683744, -46.00310660221152 -18.338230633122755, -46.0033599118415 -18.340309668487052, -46.00457330385876 -18.340997337262536, -46.00458265062001 -18.342614949554708, -46.002411447938876 -18.343551789722493, -45.99998693435419 -18.34240866238308, -45.99817112634901 -18.34195547225438, -45.99612300608997 -18.34323772348086, -45.99541306024631 -18.346015862429457, -45.99663176047399 -18.347627158005945, -45.99881899702799 -18.349465627551456, -45.999068958944456 -18.350967206997364, -45.99943873123647 -18.35223680457657, -46.00174185797684 -18.35314921764157))) |
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_-5db4 |
Folha |
SE23 |
Legenda_Completa |
533Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
533 |
Nome_Unidade |
Planalto Dissecado Suaçuà Grande |
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 |
Planalto Dissecado Suaçuà Grande |
Area_Poligono_Km2 |
125.909 |
the_geom |
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