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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.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSD22.fid-6d9cbe3e_18e3b294723_54dc |
Folha |
SD22 |
Legenda_Completa |
421Dt32 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Depressões Intermontanas do Alto Tocantins - Maranhão |
Identificacao_Unidade |
421 |
Nome_Unidade |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
SuperfÃcies Intermontanas Uruaçu - Ceres |
Area_Poligono_Km2 |
136.868 |
the_geom |
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-14.340869254948649, -48.631317285559085 -14.338053967255771, -48.63146310157607 -14.335013013069892, -48.631315245678955 -14.332088971566415, -48.630246531806755 -14.330664036113395, -48.627764556047154 -14.328563062752345, -48.625751772292965 -14.32645788354836, -48.62457213795882 -14.3256645372401, -48.62397940608568 -14.324924005603354, -48.619085997855265 -14.321810167727225, -48.61807990781684 -14.320786565037253, -48.615250661838104 -14.319089629453217, -48.61400665015805 -14.317667070477928, -48.610523798783596 -14.31499962263102, -48.60892466534537 -14.313292558365532, -48.60751301315848 -14.312787899816765, -48.606097048523154 -14.311651822325059))) |
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_54dd |
Folha |
SD22 |
Legenda_Completa |
294Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
Formas Agradacionais Atuais e Subatuais Interioranas |
Identificacao_Unidade |
294 |
Nome_Unidade |
PlanÃcies e Terraços Fluviais |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcies e Terraços Fluviais |
Area_Poligono_Km2 |
1.161 |
the_geom |
MULTIPOLYGON (((-51.26869629888002 -15.038255895298699, -51.266057156530145 -15.037785576827485, -51.26215429451567 -15.036144949167213, -51.26040394185865 -15.035645403253012, -51.25851205014909 -15.035675245533978, -51.25793785127856 -15.036011024866019, -51.2578238790455 -15.036401837997865, -51.25819785902623 -15.037376262062919, -51.26063927407729 -15.03971417967447, -51.26345098767024 -15.041133082736234, -51.267525487690875 -15.042215598716536, -51.26916130487609 -15.042854512833012, -51.2714564304899 -15.043158515769914, -51.2764459281289 -15.042288715375255, -51.281461394694446 -15.03957846869871, -51.28378329779868 -15.038739067299126, -51.28404138317758 -15.03798674581171, -51.28340913655764 -15.037541414105993, -51.278505961861455 -15.038021991094201, -51.27397314396691 -15.03772059373995, -51.26961520159831 -15.038338658145408, -51.26869629888002 -15.038255895298699))) |
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_54de |
Folha |
SD22 |
Legenda_Completa |
443Dt11 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Planaltos Divisores do Araguaia-Tocatins |
Identificacao_Unidade |
443 |
Nome_Unidade |
SuperfÃcie Oriental 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 Oriental do Médio Araguaia |
Area_Poligono_Km2 |
15.287 |
the_geom |
MULTIPOLYGON (((-50.434063752538975 -14.438228970923618, -50.43427813532881 -14.436907136928205, -50.434047245669596 -14.436217319478743, -50.43252603468712 -14.434368369570468, -50.432236028329214 -14.433504537118331, -50.43070550783809 -14.433265989863372, -50.42887189070384 -14.434059672235632, -50.42608859748292 -14.435998719557968, -50.4235435999154 -14.437306353279565, -50.42289516971738 -14.437359681278092, -50.42135520289948 -14.438327975097923, -50.41662926769076 -14.439795712275545, -50.41509492469172 -14.439959654499324, -50.41326780635924 -14.439834638081974, -50.41085991304415 -14.438440784342342, -50.40991681057644 -14.438262242724031, -50.40932938805758 -14.437913758311733, -50.405557914190375 -14.437489670312202, -50.40343520256284 -14.437478220900537, -50.402253718257306 -14.437930135598103, -50.401133238324945 -14.43792400506361, -50.40024639177269 -14.438321164945775, -50.39936144965164 -14.438373733911858, -50.39663888974603 -14.439909803947018, -50.39302270719853 -14.44281958497758, -50.3894770686483 -14.44400724015614, -50.38575983398821 -14.444387143178291, -50.38256796401673 -14.445403010453518, -50.380135966315684 -14.447745658973686, -50.37917828930054 -14.44975228567968, -50.37927620832896 -14.452740917245647, -50.38020093819914 -14.455621716366172, -50.38195645485395 -14.457701107462158, -50.384302342698774 -14.459555005594256, -50.387299666995276 -14.461182500913532, -50.3877669452461 -14.461759661390364, -50.39035135739961 -14.4634428123149, -50.39198231417787 -14.464190266655116, -50.3971283856774 -14.46411440022274, -50.39819273789494 -14.463717999048544, -50.39889944037817 -14.463721818535994, -50.39984647824411 -14.463267491736948, -50.406395551642724 -14.46278925291076, -50.40858143358996 -14.462226622688009, -50.411596987666655 -14.460979383327935, -50.41626050694388 -14.46020184648755, -50.418735379862504 -14.460560103553048, -50.42026323885204 -14.461317358204521, -50.42114828002859 -14.461321859542736, -50.42203330673638 -14.46132723672189, -50.42280288253357 -14.460814953000362, -50.42646592503013 -14.459742766850608, -50.42912003467112 -14.459700799075122, -50.4394915895993 -14.46073713619586, -50.443267226675424 -14.460528690191932, -50.4439203797215 -14.45984241476363, -50.44463820477792 -14.458236607796014, -50.44453662604857 -14.45570686385922, -50.44424657643818 -14.454957334482314, -50.440268903736005 -14.449934005440248, -50.437449628254775 -14.448078410044886, -50.431989584180776 -14.44506148183693, -50.43113873464324 -14.443737062858238, -50.43146595586668 -14.441065608366188, -50.431842149153496 -14.440227796028292, -50.43207858982397 -14.439826708369454, -50.43293859937507 -14.439492360000907, -50.434063752538975 -14.438228970923618))) |
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_54df |
Folha |
SD22 |
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 |
0.225 |
the_geom |
MULTIPOLYGON (((-49.099400123921555 -14.441161407553832, -49.098828919869796 -14.439257503699388, -49.0980798687568 -14.43893451235531, -49.09682493255342 -14.438923587547473, -49.09581334900454 -14.439707741455265, -49.09506081945726 -14.439622939538788, -49.09413748213933 -14.440089631054269, -49.0945495415219 -14.440805315260649, -49.09466039915114 -14.442102518324226, -49.095951182869484 -14.44327029903349, -49.0974529079693 -14.443757224139208, -49.09845530166486 -14.443844181037406, -49.099387109342715 -14.442665479818672, -49.099400123921555 -14.441161407553832))) |
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_54e0 |
Folha |
SD22 |
Legenda_Completa |
196Da52 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Complexos Serranos dos Planaltos do Alto Paraguai |
Identificacao_Unidade |
196 |
Nome_Unidade |
ProvÃncia Serrana |
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 |
ProvÃncia Serrana |
Area_Poligono_Km2 |
45.304 |
the_geom |
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