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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_-53bf |
Folha |
SE23 |
Legenda_Completa |
532Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos do Leste de Minas |
Identificacao_Unidade |
532 |
Nome_Unidade |
Planalto dos Campos das Vertentes |
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 dos Campos das Vertentes |
Area_Poligono_Km2 |
115.754 |
the_geom |
MULTIPOLYGON (((-44.8942092554668 -19.859455736555624, -44.89354906685129 -19.859745425958724, -44.885126914975665 -19.863439876375516, -44.881714145016744 -19.867309020678434, -44.8783007176211 -19.87182242199052, -44.881416766606606 -19.87801293532357, -44.88362954076765 -19.883959712808167, -44.88140973995978 -19.887456395974, -44.880670509051434 -19.888505074966112, -44.87993153195813 -19.889204026663293, -44.87881869465702 -19.894099410524024, -44.878814968302386 -19.898996446787706, -44.87585538295158 -19.9049397097087, -44.874004035066044 -19.909485717104452, -44.87252374423513 -19.912282448968178, -44.866982662261734 -19.910529775332517, -44.86512921727108 -19.917173118855736, -44.86254062905752 -19.91962010082439, -44.862536699378005 -19.924166493763597, -44.86142525131447 -19.92766285687204, -44.85574277985948 -19.928585507251483, -44.85437176092296 -19.935681853631465, -44.84344688175034 -19.944060466373674, -44.83252193876816 -19.95050182250461, -44.83660542257599 -19.960829177094197, -44.841385730728646 -19.958252625928637, -44.846846680347554 -19.956321754929668, -44.85093973106126 -19.957615682807045, -44.862540799218806 -19.956979821797734, -44.87072883915062 -19.9576311950927, -44.87686328082509 -19.966668668231463, -44.883681827653376 -19.974415930211613, -44.88777199627893 -19.980870778545484, -44.892543258564544 -19.989906825955597, -44.890489891843636 -19.998293432501285, -44.8904329278643 -20.00048750622203, -44.93920411090422 -20.000477512701913, -44.98189720084345 -20.000487016298944, -44.98048439751908 -19.999393425138386, -44.97706717498971 -19.99675881610804, -44.97566307794226 -19.995430232813213, -44.97504180351677 -19.99484276034776, -44.97446831420022 -19.99435831104974, -44.9714976957758 -19.99184836371977, -44.96884052326529 -19.990291794684723, -44.96795460501377 -19.989214460469686, -44.96592982643728 -19.985501799921952, -44.96542344015818 -19.98442452504537, -44.96276667703669 -19.981909067887, -44.9617548465547 -19.980113255843435, -44.95530139837525 -19.974962620807815, -44.95163329226961 -19.967537983842156, -44.951633949333235 -19.96538272241885, -44.95163431433147 -19.9641853547351, -44.95074917893592 -19.961431616675664, -44.94996606178742 -19.959550851616633, -44.950266650860755 -19.95799029039971, -44.94996807329046 -19.95316910188246, -44.95176885165415 -19.94919885138095, -44.951469377899905 -19.947213394758116, -44.949371656377856 -19.944376171140995, -44.94817288178934 -19.942674203655997, -44.948173899444214 -19.939554713809006, -44.944878246193504 -19.93331383490348, -44.944279498791 -19.932178629896768, -44.94248214626603 -19.929342318371077, -44.94218292856592 -19.927073087304763, -44.93918725293482 -19.922250063307597, -44.93678960404954 -19.92054760131649, -44.934991820764964 -19.919412837037715, -44.93499298003828 -19.91657619109255, -44.935593439939225 -19.913173155644667, -44.93739389788061 -19.909770543177594, -44.93739490212014 -19.90721764934682, -44.93679568814092 -19.905232053440777, -44.935897907402016 -19.90211222949133, -44.9341009255639 -19.89955867683202, -44.93230448337634 -19.895870986600915, -44.93080689552061 -19.89275000125135, -44.92901224865113 -19.885375255956912, -44.92961429787288 -19.88055435233016, -44.93320988796154 -19.88055573696884, -44.93440978655401 -19.87800418412119, -44.93321250215509 -19.874315810608284, -44.938156447958875 -19.875026986428992, -44.9395041624112 -19.875311205574665, -44.94100369984735 -19.873184438981653, -44.941603345923205 -19.871199244773262, -44.94145426397086 -19.86878907243931, -44.94040620996926 -19.86680333230871, -44.937860596020045 -19.864533313069018, -44.936512189770276 -19.863823446023673, -44.93576357471287 -19.86325566429983, -44.92962129106147 -19.862544856623877, -44.928571584182684 -19.864671710692733, -44.926622833967514 -19.867222921290274, -44.92272473334284 -19.87317744842949, -44.92167521219138 -19.874595771860797, -44.91837801601645 -19.876012169468922, -44.91448205515563 -19.877002584889023, -44.910287616159835 -19.875298888264485, -44.90714242419132 -19.873028130257076, -44.897914278483356 -19.8668093601851, -44.89412795726565 -19.85962467711463, -44.8942092554668 -19.859455736555624))) |
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_-53be |
Folha |
SE23 |
Legenda_Completa |
521Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos da Bacia do Alto Rio Paraná |
Identificacao_Unidade |
521 |
Nome_Unidade |
Planalto do Triângulo Mineiro |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto do Triângulo Mineiro |
Area_Poligono_Km2 |
25.803 |
the_geom |
MULTIPOLYGON (((-47.59371715078932 -20.000479546337626, -47.593789215828956 -19.999456344134025, -47.59116784658718 -19.99879943870492, -47.589484130431366 -19.997476849348317, -47.59050586366706 -19.994654610272665, -47.59222158240132 -19.990699838100955, -47.59310277088785 -19.98653243410993, -47.59411433064337 -19.98303762983885, -47.59169087521359 -19.980040949817706, -47.58942357931815 -19.97928851199222, -47.59069768124293 -19.977361037135758, -47.59373689743884 -19.97451019888348, -47.59181960093084 -19.97337161498234, -47.59094668800162 -19.970801907170273, -47.59173516532704 -19.96820791824706, -47.59587839828877 -19.96758567658034, -47.59788300903136 -19.966770749195504, -47.5973661818629 -19.964195861495465, -47.59483196936728 -19.961650492888637, -47.59384070919477 -19.959082526165947, -47.593077094715426 -19.95595048476869, -47.589724438095075 -19.954090590224126, -47.58519115401422 -19.95988239507537, -47.57797122484308 -19.96685814881034, -47.57636460414781 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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_-53bd |
Folha |
SE23 |
Legenda_Completa |
000Magua |
Nome_Dominio |
|
Nome_Regiao |
|
Identificacao_Unidade |
0 |
Nome_Unidade |
|
Letra_Simbolo |
|
Categoria |
|
Natureza |
|
Caracteristica |
|
Forma |
|
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Corpo d´água continental |
Area_Poligono_Km2 |
3.999 |
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_-53bc |
Folha |
SE23 |
Legenda_Completa |
555DEc43 |
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 |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Centro - sudeste Goiano |
Area_Poligono_Km2 |
8.638 |
the_geom |
MULTIPOLYGON (((-48.00034306115171 -18.454765437118684, -47.9996742257232 -18.454531468481886, -47.99878425226821 -18.454545554865934, -47.997707629900674 -18.45405339520291, -47.99645855722547 -18.453817650326158, -47.995215918861476 -18.454007027599303, -47.9936147209898 -18.454032329788344, -47.99130134961964 -18.45406886188376, -47.98969720590794 -18.45392444490935, -47.988539048285276 -18.453857847291655, -47.98685040690838 -18.453969337548504, -47.986149470641 -18.454575352793334, -47.98518087087641 -18.455185583007033, -47.98483847694978 -18.455955678844873, -47.98458351801925 -18.456639530555403, -47.985408766341 -18.458515261198873, -47.9857283558737 -18.458996853072208, -47.98680796616314 -18.460426176256316, -47.98717486967216 -18.46101716442146, -47.98709482405057 -18.461530333547834, -47.98760727899293 -18.462221948144588, -47.98779696796481 -18.462850036890938, -47.98773748251785 -18.46356692214408, -47.98821223829524 -18.464157108427642, -47.98833897031878 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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_-53bb |
Folha |
SE23 |
Legenda_Completa |
555Dc53 |
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 |
muito alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Centro - sudeste Goiano |
Area_Poligono_Km2 |
0 |
the_geom |
MULTIPOLYGON (((-48.00034306115171 -18.454765437118684, -48.000343108274464 -18.454765501959653, -48.00034329412743 -18.454765518617023, -48.00034306115171 -18.454765437118684))) |
|
PWG РPowering Growth ̩ um projeto para facilitar o |
Sobre nós |
Privacidade |