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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_-543c |
Folha |
SE23 |
Legenda_Completa |
557Dt21 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores São Francisco - ParanaÃba |
Identificacao_Unidade |
557 |
Nome_Unidade |
SuperfÃcie de Catalão |
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 |
SuperfÃcie de Catalão |
Area_Poligono_Km2 |
20.062 |
the_geom |
MULTIPOLYGON (((-47.99172194391003 -18.29007368023583, -47.990598630797045 -18.289643374321347, -47.9880784797228 -18.287745320241626, -47.98729715231444 -18.28511581635961, -47.98879486231593 -18.281129797742, -47.989868622360994 -18.279263969244333, -47.991026453529486 -18.276956233358817, -47.992173681106365 -18.27403201782906, -47.993603754177045 -18.271456381144, -47.99142215381055 -18.267792489665887, -47.98718731982139 -18.267946291770464, -47.98279834074512 -18.269863866764062, -47.98072827123934 -18.27271395980707, -47.97865062994297 -18.275124467249537, -47.9770315547555 -18.27743933484587, -47.97714833297406 -18.284775905269452, -47.97838344462912 -18.291402541601588, -47.975534318169274 -18.295306660146164, -47.972898038284725 -18.29856370071157, -47.96911805545571 -18.300551941714613, -47.96599502524391 -18.30365667730193, -47.966080151325514 -18.30648942787052, -47.9662476421537 -18.31204662595059, -47.96212483974168 -18.318128256507396, -47.95870040598447 -18.32332231529132, -47.958767722024696 -18.32405620054545, -47.958902341890294 -18.32552306796969, -47.9578920125633 -18.327427535332756, -47.956915064871026 -18.328071987883078, -47.95550665149792 -18.32919532477373, -47.95407683801944 -18.32906039136435, -47.95301386215282 -18.327869731158355, -47.95139734449171 -18.326425802616143, -47.94848979511553 -18.327564169927008, -47.947918655004244 -18.333577081705148, -47.95197819595199 -18.33479992211277, -47.95295164788423 -18.339287428177883, -47.945813876609726 -18.341757126349442, -47.944069782228446 -18.344785230766313, -47.94725278658471 -18.34687941381578, -47.95095319145715 -18.347702407276422, -47.95372454033863 -18.34810004176321, -47.95530522191279 -18.34886823210608, -47.95705129274376 -18.348576588249273, -47.95858154262628 -18.346439223297992, -47.96083852443818 -18.343674804674098, -47.96310744533752 -18.34161441140407, -47.96501670448606 -18.340087766758458, -47.966939446452606 -18.339352701590325, -47.96813698077958 -18.339334048225407, -47.969230800465844 -18.33861277741154, -47.969460160135704 -18.335879874178197, -47.96989731582685 -18.33446370567546, -47.971439345407084 -18.33303121535656, -47.97308751159463 -18.332388861325082, -47.97398848615044 -18.331229987528516, -47.97449017039493 -18.328228302769965, -47.97684229427497 -18.32563742052864, -47.97966667890894 -18.32374426220041, -47.982328410290904 -18.323174478518723, -47.98352827905941 -18.323244184817646, -47.98435710673969 -18.323231212891347, -47.98535510014496 -18.32233441207124, -47.98660278535442 -18.3198492049471, -47.98832278097962 -18.3180617138831, -47.98922755246159 -18.317078783751345, -47.99124915497416 -18.316782553587245, -47.99263325464472 -18.316849317899102, -47.99409746690308 -18.316298174954053, -47.99491355664195 -18.315492668700852, -47.99615708595976 -18.31283143308063, -47.99801567626151 -18.308399093253882, -47.99890215052001 -18.30636009815931, -47.99941989308068 -18.305797618385007, -47.99980680373348 -18.305377134100567, -48.00044915509382 -18.30529932183756, -48.000449896929915 -18.290913514336513, -48.00044959536526 -18.286175429996664, -48.000449410521 -18.27825860952302, -47.99816213395226 -18.28001023224159, -47.99656304695796 -18.282542121686028, -47.99616327563598 -18.284540981527776, -47.994963960671264 -18.28733938548887, -47.993897902480846 -18.288405444314407, -47.99172194391003 -18.29007368023583))) |
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_-543b |
Folha |
SE23 |
Legenda_Completa |
555Dc42 |
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 |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Centro - sudeste Goiano |
Area_Poligono_Km2 |
38.313 |
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_-543a |
Folha |
SE23 |
Legenda_Completa |
555Dc21 |
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 |
baixa |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planalto Dissecado do Centro - sudeste Goiano |
Area_Poligono_Km2 |
24.061 |
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_-5439 |
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 |
0.328 |
the_geom |
MULTIPOLYGON (((-42.51723920237111 -19.872258701548393, -42.51790769662415 -19.87174697489973, -42.51847198215055 -19.870816594327557, -42.518876984731385 -19.86957154437866, -42.51922743228578 -19.868274260210526, -42.52006585346737 -19.86745244215528, -42.52051793797337 -19.866676713769138, -42.52057961949596 -19.866208900404718, -42.52004130604609 -19.86547175821391, -42.51950447317287 -19.864578411470028, -42.51918660336674 -19.863844337332676, -42.518810805449476 -19.863214207242613, -42.51826020081235 -19.863206536688114, -42.517974019731085 -19.863932195749538, -42.517576478932796 -19.864760150207175, -42.517119383743825 -19.86579587242541, -42.51656729206821 -19.86594439873994, -42.51589963667334 -19.86640375864193, -42.51565971283624 -19.867651103651347, -42.515190558799155 -19.86952014346427, -42.51483924475781 -19.870870682617568, -42.5151580580407 -19.8716047766707, -42.516414542875275 -19.872194825285373, -42.51723920237111 -19.872258701548393))) |
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_-5438 |
Folha |
SE23 |
Legenda_Completa |
149Pgi |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planaltos e Chapadas do Jequitinhonha |
Identificacao_Unidade |
149 |
Nome_Unidade |
Chapadas do Jequitinhonha |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapadas do Jequitinhonha |
Area_Poligono_Km2 |
2.514 |
the_geom |
MULTIPOLYGON (((-42.01245945690867 -17.346751210870934, -42.01322796630414 -17.34510134028426, -42.01356974546806 -17.34431549669482, -42.01528384461792 -17.345290051482866, -42.01595424364489 -17.34458856423886, -42.01663137851359 -17.34341224276387, -42.01664418440799 -17.342620579927896, -42.016338242612115 -17.341192122943177, -42.01618910579264 -17.340240937282775, -42.01688122994358 -17.338194428102124, -42.01853175834144 -17.33798157310738, -42.01992997545542 -17.338081867746784, -42.0221847341919 -17.336138064236483, -42.019923909314436 -17.33333515425151, -42.018295139912695 -17.332203912388678, -42.016401318820094 -17.332175678467106, -42.014836121544334 -17.33223088359633, -42.014191358286794 -17.331350855650488, -42.01207562790753 -17.32981682820212, -42.01115169687321 -17.330909995618022, -42.01002761963443 -17.329153295853697, -42.00838998952141 -17.328575336115758, -42.00761256240377 -17.330778542054535, -42.00602812991112 -17.332020712494984, -42.005467074706786 -17.333781468522304, -42.00493761776311 -17.33475214013739, -42.004717010680004 -17.335060990208497, -42.00281978940802 -17.336252269289414, -42.001849117921765 -17.336296390939474, -42.00156267198945 -17.336173628474395, -42.00041738190924 -17.33771072455378, -42.000407827148905 -17.338298370023455, -42.00039827238851 -17.33888601549337, -42.00158439011372 -17.340840898023327, -42.00237857630358 -17.342561633678677, -42.00365809818825 -17.344061762066477, -42.00395282339557 -17.344533322147324, -42.00558071156547 -17.344354017337242, -42.00814122254478 -17.34391741988204, -42.00862568689395 -17.344479053150096, -42.01002651166332 -17.344420550661038, -42.01124234015035 -17.34562515034224, -42.01245945690867 -17.346751210870934))) |
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