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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_-5b9e |
Folha |
SE23 |
Legenda_Completa |
523Dt21 |
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 |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
5.307 |
the_geom |
MULTIPOLYGON (((-47.363688089640846 -19.099870751688474, -47.3640596950895 -19.100214596667136, -47.36147248219754 -19.10274231253688, -47.36169248021569 -19.103047465147302, -47.36381167202186 -19.10295162270709, -47.36370969738337 -19.103397283000316, -47.360913803961445 -19.10387751768717, -47.36087819474727 -19.103912294266657, -47.35942331631757 -19.105229685357642, -47.35938816962999 -19.105230135920415, -47.35873038805977 -19.107015974658335, -47.35785162048263 -19.10842802830607, -47.35797444614842 -19.10945153476328, -47.35793883519521 -19.10948631094869, -47.35688342888673 -19.11110654430183, -47.35686482553593 -19.11180492122705, -47.35716623148745 -19.112758403967337, -47.35789504255127 -19.113432752959422, -47.35872442543959 -19.113694874178112, -47.35969723175844 -19.11381967893059, -47.35970256407358 -19.114195322228625, -47.358916565478694 -19.11451337725783, -47.358388131976135 -19.115305895847197, -47.359027579831064 -19.117314438453665, -47.35965054480942 -19.11816083088533, -47.36109320675959 -19.118518029771863, -47.36167814934752 -19.119228525984735, -47.3620508372548 -19.120180177732077, -47.36348915348449 -19.120230340162774, -47.36431369458284 -19.120082463935237, -47.36621503249084 -19.119819581695104, -47.367293269667144 -19.11980570719053, -47.36708881280291 -19.120594078033502, -47.36724004441865 -19.121138536558412, -47.36846320587693 -19.121225747850367, -47.36939314982264 -19.12094011609433, -47.36946534931321 -19.12093918595042, -47.37059092776403 -19.121779058459346, -47.37107149557022 -19.1226958792264, -47.37186969597166 -19.123231989763784, -47.37251177500186 -19.122882318288333, -47.372583485183306 -19.122847073613066, -47.37278351958047 -19.12175078338339, -47.373055781414806 -19.120722200246114, -47.37296016596978 -19.11908332114539, -47.3729333227683 -19.11720331758057, -47.373651951468624 -19.114630918258392, -47.37347974884959 -19.112685054002583, -47.37412666010049 -19.112676707511365, -47.37455307629184 -19.114858622947935, -47.37618702041849 -19.118494357375855, -47.37692035053374 -19.119544270193654, -47.378114234197994 -19.120109558857585, -47.378943174879076 -19.120270436084795, -47.379422798136304 -19.12111860453182, -47.37947993657522 -19.122587277760992, -47.380238152561525 -19.122851117893276, -47.38080996329618 -19.12263870299257, -47.38047569687061 -19.12185639363091, -47.380534708142456 -19.12100125770313, -47.381571950318005 -19.120646441880154, -47.381887592837465 -19.120129370219832, -47.38162260155077 -19.11914205570729, -47.381537670442 -19.118254464210462, -47.381142974661195 -19.11829389343382, -47.38024968271879 -19.118681162254838, -47.37942317341405 -19.118623217072646, -47.3791997085833 -19.118079706358472, -47.379261661818084 -19.117429545403496, -47.38022913304249 -19.117246335234025, -47.3802149342778 -19.11625486871649, -47.379953879087836 -19.11554115117724, -47.38001925579352 -19.115130278674076, -47.38012755040665 -19.11512887760323, -47.381458487021696 -19.11524802769959, -47.383575347753506 -19.114981280070886, -47.384650633904194 -19.114830970757545, -47.384823765605255 -19.114315742917718, -47.384280764647144 -19.114083448817386, -47.383377681612984 -19.113719443842133, -47.38297075242304 -19.112904662898824, -47.383280009651784 -19.111943327589728, -47.383157016837586 -19.11138316688242, -47.382032464318215 -19.11067973115195, -47.37984391714817 -19.11091306386639, -47.37778072120032 -19.109880349522754, -47.37687281151608 -19.109242718413796, -47.37790364034501 -19.10844366511365, -47.377842623480795 -19.106701385115297, -47.377375238406216 -19.106638784441117, -47.37632635244768 -19.106173664081773, -47.37674492364932 -19.105280467457238, -47.376731735884086 -19.104357623498956, -47.3769005165726 -19.103603124087556, -47.37646146153429 -19.103062390476904, -47.37523600009475 -19.102804555133517, -47.37420325065548 -19.100938430952073, -47.37417788984969 -19.09916136518158, -47.37429693931436 -19.09745107597833, -47.37521355133356 -19.096174847909474, -47.37495550082537 -19.095733828479087, -47.37391351979674 -19.09574726568402, -47.373835972801515 -19.095372556195695, -47.375330645409385 -19.094328208874835, -47.3754902023555 -19.093193604688288, -47.3755062933062 -19.091791713425476, -47.37484727573083 -19.09094583598294, -47.374060439652396 -19.091195314918615, -47.372739441058954 -19.09175964725162, -47.37200502558149 -19.091888323853972, -47.370884218671776 -19.092768876897097, -47.369376501318236 -19.093365395061742, -47.36858908709777 -19.093375525012352, -47.36793201572932 -19.094133590474872, -47.36667070830256 -19.094957223088556, -47.366022776159895 -19.09629227925487, -47.364284262761906 -19.097699143857902, -47.36442633868255 -19.099139652950836, -47.363887526551345 -19.099664981637513, -47.363688089640846 -19.099870751688474))) |
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_-5b9d |
Folha |
SE23 |
Legenda_Completa |
547Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
547 |
Nome_Unidade |
Planalto de PatrocÃnio |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto de PatrocÃnio |
Area_Poligono_Km2 |
1.648 |
the_geom |
MULTIPOLYGON (((-46.95346840480947 -19.109676377451176, -46.95653123474643 -19.109352063157022, -46.95896496911025 -19.107577305142787, -46.96016759983775 -19.10552385305073, -46.962927821263285 -19.10549444005024, -46.96382348979448 -19.103444241397213, -46.9631718580995 -19.100244332008923, -46.961004891533065 -19.09851765113377, -46.96096368270013 -19.095020349465848, -46.9597199354983 -19.0935755932547, -46.95967533113801 -19.089786543685022, -46.955310053494216 -19.083710056884073, -46.95442804400192 -19.08692629232871, -46.954778458733884 -19.090713011909568, -46.95482638041804 -19.094793816251713, -46.955177777869636 -19.098579616426427, -46.95521545551684 -19.101786088386415, -46.95374012636123 -19.106758401560192, -46.95345813487759 -19.10880204927448, -46.95346840480947 -19.109676377451176))) |
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_-5b9c |
Folha |
SE23 |
Legenda_Completa |
547Dc32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
547 |
Nome_Unidade |
Planalto de PatrocÃnio |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto de PatrocÃnio |
Area_Poligono_Km2 |
65.128 |
the_geom |
MULTIPOLYGON (((-46.92458845297283 -18.77702529098316, -46.924560883594516 -18.774597275564844, -46.92306791222597 -18.771490546542935, -46.92377652537129 -18.769748751310996, -46.92560606123854 -18.77042370785487, -46.92852109962468 -18.770393646420395, -46.93068715273493 -18.768636783816742, -46.93065160167767 -18.76551415475072, -46.93027562705053 -18.764477339943646, -46.933530959668914 -18.76236230070165, -46.9367862080426 -18.7602472116006, -46.94041738664916 -18.75916886436002, -46.944412625295165 -18.7580866643255, -46.94620230791683 -18.75529286759415, -46.948003878053335 -18.75353962439835, -46.95014160312139 -18.749353682275377, -46.94938553717532 -18.74693328620924, -46.94574276114466 -18.74697121201091, -46.9439293130267 -18.74768386119494, -46.94249184743489 -18.749433283464125, -46.94177858159238 -18.7508282813881, -46.939232911351475 -18.751201591842392, -46.93778348690319 -18.75191041195178, -46.9348687819725 -18.751940589210122, -46.93342423976473 -18.75299712949713, 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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_-5b9b |
Folha |
SE23 |
Legenda_Completa |
524Pru |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Serras do Espinhaço |
Identificacao_Unidade |
524 |
Nome_Unidade |
Serras do Espinhaço Meridional |
Letra_Simbolo |
Pru |
Categoria |
Pediplano retocado desnudado |
Natureza |
aplanamento |
Caracteristica |
retocado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras do Espinhaço Meridional |
Area_Poligono_Km2 |
15.545 |
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_-5b9a |
Folha |
SE23 |
Legenda_Completa |
523Dc52 |
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 |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto Rebaixado do ParanaÃba / Quebra-Anzol |
Area_Poligono_Km2 |
57.69 |
the_geom |
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