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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 SD.22 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.
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FID |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_466e |
Folha |
SD22 |
Legenda_Completa |
410Dt11 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
SuperfÃcie do Araguaia |
Identificacao_Unidade |
410 |
Nome_Unidade |
SuperfÃcie Central do Médio Araguaia |
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 Central do Médio Araguaia |
Area_Poligono_Km2 |
188.771 |
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 SD.22 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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_466f |
Folha |
SD22 |
Legenda_Completa |
421Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
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 |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
6.152 |
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 SD.22 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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4670 |
Folha |
SD22 |
Legenda_Completa |
294Atf1 |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Formas Agradacionais Atuais e Subatuais Interioranas |
Identificacao_Unidade |
294 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais |
Letra_Simbolo |
Atf |
Categoria |
Terraço fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
terraço |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
nÃvel 1 (mais baixo) |
Legenda |
PlanÃcies e Terraços Fluviais |
Area_Poligono_Km2 |
10.661 |
the_geom |
MULTIPOLYGON (((-49.96459267668274 -13.7508236625356, -49.9624540755283 -13.75218084213061, -49.96156849906475 -13.752513242401024, -49.95626503030461 -13.753302154734317, -49.954964793439764 -13.753744011674454, -49.94942319082568 -13.754758503092793, -49.94545412872673 -13.756176070155036, -49.94387579926465 -13.756233559083157, -49.94033042990367 -13.757563713844654, -49.9396231454392 -13.757611337989557, -49.93897120712688 -13.758004547476773, -49.93803010947123 -13.758048433288, -49.933345485172445 -13.760914973080455, -49.931306729376544 -13.763932808411703, -49.93123426844549 -13.764909479163684, -49.93074556606135 -13.76628222866732, -49.93049143437542 -13.77214161345647, -49.93104008619415 -13.77513838980236, -49.931560576353775 -13.775778082302288, -49.931608132728535 -13.776641474730345, -49.93200503151551 -13.777738203504402, -49.93343128920501 -13.78109370279729, -49.93510057372468 -13.78376015613394, -49.936374978571465 -13.785272753648687, -49.938154170021896 -13.78857493705893, -49.938963663801324 -13.789679116647374, -49.94050826318506 -13.792919494604215, -49.94265828529418 -13.79490415862456, -49.9434686503126 -13.795097347010175, -49.94406891513686 -13.7949820546144, -49.94525726358315 -13.794078582831544, -49.94727110415399 -13.793015031475889, -49.949894909749005 -13.790292204690333, -49.95244949867462 -13.788372837316519, -49.95502657823004 -13.784730306291962, -49.95807295594918 -13.781207758503298, -49.960425147389564 -13.776814154072065, -49.960730124303176 -13.775956368173906, -49.96080825258211 -13.774462735075762, -49.96032476127525 -13.771007169263068, -49.95963985691813 -13.769387097773786, -49.959591936600035 -13.768639776785914, -49.95884583153639 -13.767192838458843, -49.95665492676981 -13.76388510570513, -49.95648928678613 -13.76307787390312, -49.956632046416345 -13.761126244001803, -49.956995961407365 -13.760268514673013, -49.958482165119825 -13.759081282069435, -49.96069823188857 -13.756066045792812, -49.96397792242558 -13.752547097786007, -49.96459267668274 -13.7508236625356))) |
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 SD.22 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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4671 |
Folha |
SD22 |
Legenda_Completa |
421Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
7.172 |
the_geom |
MULTIPOLYGON (((-48.03623639908759 -13.747385390283048, -48.03481420726882 -13.746716148621829, -48.02862164116165 -13.745387858183115, -48.02689807299059 -13.744545266498937, -48.02672070403756 -13.744009879522737, -48.028525639487285 -13.740225554437574, -48.02837188887699 -13.739002949271876, -48.027918747188295 -13.738295737444142, -48.025715221397135 -13.73793262384561, -48.023329945587385 -13.737955719325067, -48.02168866990864 -13.738480895670708, -48.02045238930076 -13.73983792469221, -48.020437496809166 -13.741382865536073, -48.0214755641003 -13.743432776154112, -48.02319766893494 -13.74578108129761, -48.027779994931215 -13.749272200499567, -48.02859064178057 -13.75005024954945, -48.02909660743572 -13.751016390115188, -48.02914209915856 -13.752719291527349, -48.02874506292499 -13.753534938657946, -48.027880537891434 -13.754337846285969, -48.024871438825606 -13.755706013807167, -48.02413927441898 -13.756812807460555, -48.02395194133979 -13.75805905188136, -48.02406498493307 -13.758582371681758, -48.025015272332304 -13.760127993787206, -48.025067777687894 -13.762509146779124, -48.02538695542466 -13.763836770546181, -48.02650957374339 -13.76509883679603, -48.02706898889206 -13.76536615187986, -48.0282312885598 -13.765425992138795, -48.031331409274046 -13.764903360494085, -48.03371367172494 -13.763822079931716, -48.035055223223154 -13.76393358771667, -48.03550024658707 -13.764454133829242, -48.035739078646 -13.76593992530689, -48.03539510314091 -13.76728276010341, -48.03434393708972 -13.769134061412098, -48.03284144940739 -13.770346809149467, -48.030138502653784 -13.771155824600182, -48.029742654247315 -13.771615300855066, -48.030784871829205 -13.772517501477603, -48.033078768914166 -13.77379383139384, -48.03299171873006 -13.775025715272495, -48.032141550184235 -13.777105109570915, -48.03169176042722 -13.777624006788928, -48.03041385674784 -13.77841281712502, -48.02896321998174 -13.77821869263352, -48.02494126817969 -13.776461106357008, -48.02367785744798 -13.776410309877615, -48.02285944817336 -13.776707691834096, -48.02230560550044 -13.777516997934617, -48.021616038382405 -13.780219293869042, -48.02088967860496 -13.781145909886332, -48.01802990014482 -13.781910653179757, -48.01736297342766 -13.782473668691857, -48.01716418707438 -13.782993168018255, -48.01720606871967 -13.783959832861191, -48.0196318354797 -13.787324645885134, -48.020212204315364 -13.788941598922829, -48.02030647876677 -13.789940274443897, -48.019600551584496 -13.792889303078875, -48.02007901600336 -13.79333589934118, -48.020526461286806 -13.795464220262593, -48.02099209410354 -13.795928102147577, -48.0210921510839 -13.797650725612527, -48.02230002662329 -13.800245451031694, -48.02299956266609 -13.800712187058787, -48.023344206676185 -13.801460810567116, -48.02438963701812 -13.802561861667757, -48.02521147538055 -13.802627782321444, -48.0272715710366 -13.802246103654758, -48.028098096017466 -13.801794989855358, -48.03048374223695 -13.798145737486376, -48.03096531896793 -13.797059445801107, -48.03103082820216 -13.796370588895313, -48.031623699095896 -13.795803164314167, -48.03204533840472 -13.79471722212632, -48.03211552161347 -13.793684595686626, -48.03247635148758 -13.792769603993932, -48.032827034813806 -13.781236327746655, -48.03356546753226 -13.777857065515766, -48.034413991883575 -13.775282475432734, -48.035906178614084 -13.77288568319303, -48.03638267148413 -13.772259226673746, -48.03726580329979 -13.77192374197744, -48.037824836553234 -13.771338795219481, -48.03858540972546 -13.769437574224117, -48.038203598102584 -13.76820612759727, -48.038154884520175 -13.766722159346005, -48.03755936692124 -13.76607144275737, -48.0374846760734 -13.761823489758626, -48.037728190009744 -13.761022702008038, -48.03826202849678 -13.760453871903252, -48.040060387741214 -13.75725420499005, -48.03906203790799 -13.756730368527986, -48.03802108680842 -13.755228406734764, -48.037419414938164 -13.750744683862427, -48.03623639908759 -13.747385390283048))) |
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 SD.22 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 |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_4672 |
Folha |
SD22 |
Legenda_Completa |
322Da52 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planalto dos Parecis |
Identificacao_Unidade |
322 |
Nome_Unidade |
Planalto do Alto Xingu |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Planalto do Alto Xingu |
Area_Poligono_Km2 |
14.702 |
the_geom |
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