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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 SC.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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_39b9 |
Folha |
SC23 |
Legenda_Completa |
207Kd |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
207 |
Nome_Unidade |
Baixadas dos Rios Jacaré e Salitre |
Letra_Simbolo |
Kd |
Categoria |
Carste descoberto |
Natureza |
dissolução |
Caracteristica |
carste descoberto |
Forma |
carste |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Baixadas dos Rios Jacaré e Salitre |
Area_Poligono_Km2 |
17.786 |
the_geom |
MULTIPOLYGON (((-42.62765802390048 -10.896843501661266, -42.62864370588 -10.898909791171361, -42.63015581022908 -10.90125064458201, -42.63037054261349 -10.90381364105896, -42.63011792201723 -10.906024148545823, -42.62786336954522 -10.908218064875927, -42.62619100285463 -10.911233329701007, -42.62499059072293 -10.91425095441462, -42.62414497338475 -10.916922311554863, -42.623771571436514 -10.91948106366816, -42.624935271586104 -10.921120203343435, -42.627640410288336 -10.921606349878934, -42.62893423940251 -10.921733475651125, -42.631995705059055 -10.921640734580325, -42.63318767235338 -10.919785971455823, -42.63438077710811 -10.917816263092215, -42.63532701917319 -10.917241689193483, -42.63720623470985 -10.91772139820687, -42.63767000274116 -10.918773437063033, -42.63730365555083 -10.920401017973942, -42.63728979879039 -10.922263390382424, -42.63787401237727 -10.922973387879624, -42.64106012649074 -10.922066263615205, -42.64179614316881 -10.921803471270545, -42.64400688038618 -10.921500079526126, -42.64588309935545 -10.922446677608333, -42.647995927087344 -10.923160922307405, -42.64940897942526 -10.923172267706004, -42.65188952837589 -10.922027197162713, -42.65437885615288 -10.919949210411882, -42.65522001140885 -10.917859655150826, -42.656645284494964 -10.916241172363938, -42.659007467968316 -10.915211767212167, -42.66171970434306 -10.914650544641654, -42.664074768061326 -10.914668152590691, -42.66525274512463 -10.914677412412685, -42.667957213457115 -10.915047285305715, -42.67208486295827 -10.914263777220146, -42.674910307374304 -10.9141676570637, -42.67761958848311 -10.914071454565054, -42.67950915559068 -10.913272214192816, -42.68069127993485 -10.912698634346645, -42.682462681891955 -10.912012444078323, -42.684584386610986 -10.91167944282506, -42.68646836533656 -10.911694628871468, -42.68869947294366 -10.912292840401475, -42.689641205793265 -10.912416731812128, -42.69234688907638 -10.912669659845855, -42.69387930838423 -10.912449216513496, -42.69600368221083 -10.911765938841853, -42.698013597134505 -10.910733258942907, -42.69944124954348 -10.90876436795261, -42.69992634357623 -10.907021878960805, -42.69993980231783 -10.905158601005297, -42.699600919303 -10.903409125035113, -42.69819728738954 -10.902118412179037, -42.69480157923632 -10.899763718254862, -42.692575203992604 -10.898350147030255, -42.690115558432815 -10.896585228314448, -42.68918634052058 -10.895064185402408, -42.68825620542428 -10.89354310247813, -42.686858952979016 -10.891552862113064, -42.68593294684145 -10.889449875695306, -42.68511812367982 -10.888279989569382, -42.68418300012257 -10.887340747292095, -42.68230419406933 -10.886744577923793, -42.68006201585666 -10.887426747604632, -42.6780487309072 -10.889158000833552, -42.67709108479728 -10.891129911659588, -42.67566510311373 -10.892749366535634, -42.67471661037105 -10.89355751771725, -42.67459543959585 -10.894138428005824, -42.67446533003534 -10.895767219998993, -42.67551243883976 -10.8972893271559, -42.6771459030781 -10.899164005411121, -42.67760765739345 -10.900332673187563, -42.67771347347198 -10.901964385764831, -42.67722557766514 -10.904056146424058, -42.67615587715343 -10.905445206508137, -42.67485583691076 -10.906016861912994, -42.67214635100832 -10.906229794497989, -42.66967824085992 -10.905744354088268, -42.66839003750646 -10.904803823746336, -42.6671033831754 -10.903628922432498, -42.66570473151075 -10.901872065026618, -42.66537143998961 -10.899423936326691, -42.665388998486534 -10.897095518107768, -42.66492844371508 -10.895811889183157, -42.66387535617155 -10.894872452790006, -42.66175468636572 -10.895205342009323, -42.660917848580716 -10.896712156167844, -42.659131570043925 -10.899377332682029, -42.65759470257384 -10.900297130904239, -42.65559279473049 -10.900281622325016, -42.65348100664554 -10.89921715807102, -42.65184774506715 -10.897341457440055, -42.6505681248299 -10.895585585921957, -42.649751324588884 -10.894531398131809, -42.64905735471461 -10.893012246199687, -42.64878020482299 -10.892622627268212, -42.648475026284224 -10.89219269677438, -42.64683943247367 -10.890549512406052, -42.64519692088981 -10.88983840733485, -42.64355323044458 -10.889243123028878, -42.641670264116335 -10.889229475554082, -42.6413106343462 -10.890041750236605, -42.64129706780878 -10.891788282064342, -42.64152122667564 -10.893187533584891, -42.64134362353581 -10.894726224378934, -42.64067557915644 -10.895974830051545, -42.637329864592786 -10.89615996878195, -42.6371818199353 -10.896013363547949, -42.63629189584699 -10.89600630334339, -42.63585382641292 -10.895269900474585, -42.634079315676516 -10.894669464461957, -42.631417332974706 -10.893916746206854, -42.62875005894163 -10.893749418593915, -42.62771175057244 -10.893888965431636, -42.62713832393916 -10.89575359694231, -42.62765802390048 -10.896843501661266))) |
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 SC.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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_39ba |
Folha |
SC23 |
Legenda_Completa |
216Pru |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
216 |
Nome_Unidade |
Blocos Planálticos Setentrionais da Chapada Diamantina |
Letra_Simbolo |
Pru |
Categoria |
Pediplano retocado desnudado |
Natureza |
aplanamento |
Caracteristica |
retocado desnudado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Blocos Planálticos Setentrionais da Chapada Diamantina |
Area_Poligono_Km2 |
60.41 |
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 SC.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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_39bb |
Folha |
SC23 |
Legenda_Completa |
399Pgi |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
399 |
Nome_Unidade |
Cuesta de Bom Jesus do Gurguéia |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Cuesta de Bom Jesus do Gurguéia |
Area_Poligono_Km2 |
3.626 |
the_geom |
MULTIPOLYGON (((-44.45553962153467 -9.919749204712225, -44.45318559500011 -9.919646836370028, -44.451029074307094 -9.91935210546963, -44.45034202113442 -9.919253714974214, -44.44887197672186 -9.918473302512687, -44.446912461936634 -9.917400360774593, -44.44495187825016 -9.91661894249641, -44.442893369158455 -9.915545387913792, -44.4408360228178 -9.914569938562973, -44.439268684374106 -9.913011413397436, -44.437604138553674 -9.91106269260141, -44.435745178080836 -9.909115578470253, -44.433786550475794 -9.907265031270075, -44.432414496200025 -9.906386995328536, -44.43055258668351 -9.905410770819342, -44.42868913043895 -9.904921334481017, -44.42672833109223 -9.904722927063215, -44.424767471320436 -9.904526287631269, -44.422805753209765 -9.904327823174853, -44.420844870682004 -9.903741495529601, -44.4203561244899 -9.903351756445614, -44.41927776872854 -9.902571621462878, -44.41771130421503 -9.900915796004748, -44.41624319630612 -9.899357724315058, -44.41369711311035 -9.897504567688413, -44.4134016368247 -9.897406533652147, -44.41340179918919 -9.89711585218583, -44.41183349923068 -9.896917819418636, -44.40987249661426 -9.896622986720788, -44.4069826283114 -9.896264453334693, -44.40541479908279 -9.89792465887661, -44.40686312786697 -9.900478138073444, -44.40864727401278 -9.902699405562139, -44.410206101300176 -9.90514059063331, -44.41024953661075 -9.90537653536537, -44.411327619986906 -9.905669840896397, -44.41201330861787 -9.906351434520229, -44.413580432708976 -9.907520453882162, -44.41514884759782 -9.908107245551598, -44.416913004050976 -9.90849986439511, -44.41867898936407 -9.908502873143368, -44.42044358602819 -9.908701100861613, -44.42221031390156 -9.908605137349072, -44.42289612653301 -9.908607255247793, -44.42309216714374 -9.90889905669698, -44.423974483900984 -9.908997713151113, -44.42573915492373 -9.909584678088631, -44.427502054308164 -9.910560340262242, -44.42779687428199 -9.910755528402323, -44.42838534206334 -9.911048673350939, -44.429168509564356 -9.911827952474061, -44.43083316302154 -9.913094602360015, -44.43230255993117 -9.914360155888131, -44.43357559954344 -9.915238489692795, -44.43514460556561 -9.916019569045572, -44.43671138240341 -9.916994056360943, -44.43828018687581 -9.91767702775927, -44.439848430006 -9.918167372897491, -44.4414174130204 -9.918558759278678, -44.44298544441651 -9.918950997252926, -44.44455472287934 -9.919438675095895, -44.44612219131569 -9.92031683104676, -44.447690594554196 -9.92119500839076, -44.44925808342537 -9.922073146279233, -44.45082653867726 -9.922950414933121, -44.452394457435 -9.923634167292521, -44.453963717072796 -9.924123573845307, -44.45553241791023 -9.924028027551254, -44.45710311362141 -9.923640967166602, -44.45720254601359 -9.92344717974273, -44.45788842823604 -9.923448324365634, -44.45847768369249 -9.922963014462825, -44.45916573454088 -9.922380192955538, -44.459347394531136 -9.920857864042716, -44.45553962153467 -9.919749204712225))) |
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 SC.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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_39bc |
Folha |
SC23 |
Legenda_Completa |
216Dt33 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
216 |
Nome_Unidade |
Blocos Planálticos Setentrionais da Chapada Diamantina |
Letra_Simbolo |
Dt |
Categoria |
Homogênea tabular |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo tabular |
Densidade_Drenagem |
média |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Blocos Planálticos Setentrionais da Chapada Diamantina |
Area_Poligono_Km2 |
52.209 |
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 SC.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 |
GeomorfologiaSC23.fid-6d9cbe3e_18e3b294723_39bd |
Folha |
SC23 |
Legenda_Completa |
207Kd |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
207 |
Nome_Unidade |
Baixadas dos Rios Jacaré e Salitre |
Letra_Simbolo |
Kd |
Categoria |
Carste descoberto |
Natureza |
dissolução |
Caracteristica |
carste descoberto |
Forma |
carste |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Baixadas dos Rios Jacaré e Salitre |
Area_Poligono_Km2 |
12.032 |
the_geom |
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