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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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f91 |
Folha |
SF21 |
Legenda_Completa |
485Dc51 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planalto da Bodoquena |
Identificacao_Unidade |
485 |
Nome_Unidade |
Alinhamentos Serranos da Bodoquena Oriental |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Alinhamentos Serranos da Bodoquena Oriental |
Area_Poligono_Km2 |
40.307 |
the_geom |
MULTIPOLYGON (((-56.39824628110536 -20.83560667471141, -56.39934955133093 -20.82818804655393, -56.397694092360645 -20.81904186861868, -56.40003281903164 -20.81567212385627, -56.400678351509214 -20.812693092508713, -56.40153354352307 -20.810709679574806, -56.40069260372252 -20.80931411132523, -56.4000638941936 -20.80772333239292, -56.400280446474554 -20.80653081587245, -56.40282549894236 -20.804751703149524, -56.40325773007337 -20.80217048425924, -56.40284098947777 -20.80077695131736, -56.40221556524491 -20.798389649350728, -56.39693077767156 -20.798372569843174, -56.396079764850604 -20.799760041741422, -56.3962820202205 -20.801946438059044, -56.39563763529645 -20.80452754100444, -56.39353460988192 -20.801737985241047, -56.39206370506928 -20.799546418567168, -56.39398351675978 -20.79518210011261, -56.390604108447 -20.79437475221773, -56.389339883306626 -20.793377702704106, -56.388287953318276 -20.791982047015306, -56.387448133153946 -20.790589202945387, -56.384914110463534 -20.789982968704358, -56.38385541321878 -20.790376602710563, -56.38278413816118 -20.794252536221794, -56.38257020393664 -20.794365841283014, -56.37876164422524 -20.79554454316111, -56.37621182501971 -20.798714906434597, -56.37451753684994 -20.799503274457482, -56.371549011388446 -20.80147988319105, -56.36987530277785 -20.797102719073937, -56.36690650221917 -20.79947528996324, -56.36605424441778 -20.801062499436334, -56.36434067930413 -20.806222526608593, -56.36221503351209 -20.8089970821341, -56.363031990662556 -20.815756491807427, -56.364290503274255 -20.818145288731547, -56.36314175103514 -20.825969888623504, -56.35336625555417 -20.83468703916259, -56.33974387949138 -20.85134740564045, -56.335864761816936 -20.86685184086405, -56.33327998011005 -20.876390846356415, -56.33616404513723 -20.894705527009855, -56.3391080525896 -20.8838137582445, -56.34038632878159 -20.881832248405455, -56.34294311050045 -20.877471340290494, -56.34421658872342 -20.876680883031927, -56.34633702623672 -20.875497595050078, -56.348887957842656 -20.872326838952173, -56.35491435832957 -20.868874035610645, -56.35232999538382 -20.878812961837365, -56.35824812678505 -20.8816192926019, -56.36801359572023 -20.876085970954488, -56.38033415467751 -20.86697809944351, -56.38799579090576 -20.857455208912896, -56.39777311480588 -20.848338512550054, -56.39813809577403 -20.842409883188246, -56.39739644959751 -20.83640018960209, -56.39824628110536 -20.83560667471141))) |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f90 |
Folha |
SF21 |
Legenda_Completa |
483Dc31 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
483 |
Nome_Unidade |
Planaltos Sul-Matogrossenses |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Planaltos Sul-Matogrossenses |
Area_Poligono_Km2 |
441.17 |
the_geom |
MULTIPOLYGON (((-54.65422965263345 -23.056022371322157, -54.633146592797274 -23.04289455306119, -54.60241130328935 -23.033560257303467, -54.57029849568616 -23.041940405307248, -54.529516549117496 -23.058063447186974, -54.49627503037313 -23.069368194974395, -54.48213216964476 -23.08491271330382, -54.484097483187 -23.093814808512168, -54.46647583140202 -23.12408510283968, -54.46492837348469 -23.14968547200137, -54.482479244788074 -23.180519756830183, -54.48540192197018 -23.19535071235557, -54.49786640543787 -23.213290240041367, -54.53203072180114 -23.211858919100855, -54.536242878192056 -23.214881563693265, -54.55506322575991 -23.23587334037755, -54.585909128514125 -23.241278883383192, -54.61247411752071 -23.247598731170033, -54.62453936557086 -23.229054128525824, -54.62069215076724 -23.20534019208346, -54.604940471698086 -23.191303147191075, -54.607354413194905 -23.175568926491252, -54.638138255588025 -23.183919025975086, -54.64331432644557 -23.192867969497385, -54.62917256425515 -23.20842605066695, -54.6459088699749 -23.227404901179565, -54.66509247601985 -23.228676866467023, -54.67395013484251 -23.210080553379825, -54.700666324674536 -23.20751606673556, -54.7358469598941 -23.209012217401852, -54.74676199733013 -23.19438367940218, -54.74284352838274 -23.17362787840537, -54.72814653979909 -23.159616163193082, -54.71337123248224 -23.150530412122684, -54.69971248561968 -23.13850380092638, -54.70322978329199 -23.119826933204145, -54.700418310360035 -23.097114776055772, -54.66787518625182 -23.068052184512187, -54.65422965263345 -23.056022371322157))) |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f8f |
Folha |
SF21 |
Legenda_Completa |
478Dc41 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
478 |
Nome_Unidade |
Planalto Dissecado da Borda Ocidental da Bacia do Paraná |
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 Dissecado da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
402.249 |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f8e |
Folha |
SF21 |
Legenda_Completa |
476Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies do Rio Paraná |
Identificacao_Unidade |
476 |
Nome_Unidade |
PlanÃcie do Rio Paraná |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
PlanÃcie do Rio Paraná |
Area_Poligono_Km2 |
1.532 |
the_geom |
MULTIPOLYGON (((-54.15442629461647 -23.98920596238919, -54.155953200221525 -23.988769651628058, -54.155974111767236 -23.98783950006552, -54.15371270111052 -23.987101465913714, -54.150470768928194 -23.984949164402845, -54.142459211837696 -23.98108165481476, -54.13215709204788 -23.977868713479523, -54.12585498072172 -23.97682130569729, -54.125808176835115 -23.978912468675894, -54.12802167500709 -23.981741876245305, -54.134045430103086 -23.983946808656356, -54.137560929305685 -23.985173568885937, -54.142841856606196 -23.986666770287563, -54.148118096532095 -23.98839083351612, -54.15442629461647 -23.98920596238919))) |
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 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 |
GeomorfologiaSF21.fid-6d9cbe3e_18e3b3f16e6_-4f8d |
Folha |
SF21 |
Legenda_Completa |
485Pri |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planalto da Bodoquena |
Identificacao_Unidade |
485 |
Nome_Unidade |
Alinhamentos Serranos da Bodoquena Oriental |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Alinhamentos Serranos da Bodoquena Oriental |
Area_Poligono_Km2 |
149.831 |
the_geom |
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