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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_3c09 |
Folha |
SC23 |
Legenda_Completa |
117Pgi |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
117 |
Nome_Unidade |
Serras da Borda Ocidental da Chapada Diamantina |
Letra_Simbolo |
Pgi |
Categoria |
Pediplano degradado inumado |
Natureza |
aplanamento |
Caracteristica |
degradado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Serras da Borda Ocidental da Chapada Diamantina |
Area_Poligono_Km2 |
3.781 |
the_geom |
MULTIPOLYGON (((-42.45761920584499 -11.835382840275548, -42.458134460057494 -11.833601330824276, -42.4580038905006 -11.833105175690482, -42.45821357777009 -11.831748258288954, -42.45802979173097 -11.830195813787794, -42.45586993193882 -11.829594648209337, -42.45507580959174 -11.830362646263145, -42.45468059102611 -11.830552899438684, -42.45310060644329 -11.831120569827211, -42.45211805451806 -11.830918718095855, -42.45252629272884 -11.829370029315603, -42.45293351838963 -11.827823081996828, -42.45353836398162 -11.826277694906185, -42.45434086452944 -11.824732977218922, -42.45435472816224 -11.82318208900572, -42.454167317569194 -11.822210504277985, -42.453188526709745 -11.821620275598402, -42.45162247110118 -11.820637050048246, -42.4502503902893 -11.820041980493638, -42.44936857771366 -11.819646265846854, -42.446930911513725 -11.817104788181103, -42.44693464965489 -11.816716407709032, -42.44596057330572 -11.815543546691526, -42.445568132629596 -11.815540524162119, -42.443996565573755 -11.815138938028737, -42.44379434303781 -11.815718198734253, -42.443198708506436 -11.816295286364198, -42.44299831681755 -11.816681245780398, -42.44279792455008 -11.817067205032382, -42.44178619641654 -11.820063283622748, -42.44158439792378 -11.820546318456962, -42.441381185357606 -11.821320693348923, -42.44117431348153 -11.822287405252215, -42.441364480978365 -11.823064845079392, -42.441554649581235 -11.82384228467377, -42.44194428782552 -11.8242337292594, -42.44213816568406 -11.824623678058028, -42.443696723835764 -11.826383713218526, -42.44427382302635 -11.827744965958146, -42.44387302500926 -11.828516884498844, -42.44347499860588 -11.828901275640153, -42.44327459786659 -11.829287234365504, -42.44248227416366 -11.829861898143058, -42.44208048756172 -11.8308289300308, -42.44127052016183 -11.833147702209448, -42.4408019329036 -11.83492568344179, -42.44065813158528 -11.835468930704543, -42.44064602314476 -11.836826514961137, -42.44122960342 -11.837607018748914, -42.44162206528825 -11.837804310110242, -42.44318445080883 -11.838981702045203, -42.44356759626298 -11.84014904825529, -42.44395448787282 -11.840928014973949, -42.44434134326061 -11.841707870670803, -42.44433300470952 -11.842482812090795, -42.4459065645494 -11.842691094716962, -42.446303677011386 -11.84230666444768, -42.44709229112817 -11.842120370329908, -42.44729736490988 -11.841346067860632, -42.44829198294357 -11.840191241553134, -42.44848864841216 -11.840193659024921, -42.448700219018086 -11.838643450251741, -42.44969201747681 -11.837877034438131, -42.45047878798066 -11.837884030982005, -42.45024964489837 -11.841372614008492, -42.450085015210185 -11.84239802685539, -42.45093433430503 -11.843655051287708, -42.451398301604954 -11.844873694868976, -42.452173581811934 -11.844499726709127, -42.45430146583067 -11.84368545375266, -42.45544088508832 -11.8417904554005, -42.45632328714691 -11.840728307208433, -42.45633464528496 -11.83953733520625, -42.4571030310046 -11.837401348762292, -42.45761920584499 -11.835382840275548))) |
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_3c0a |
Folha |
SC23 |
Legenda_Completa |
197Pri |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
197 |
Nome_Unidade |
Vãos da Bacia do Alto ParnaÃba |
Letra_Simbolo |
Pri |
Categoria |
Pediplano retocado inumado |
Natureza |
aplanamento |
Caracteristica |
retocado inumado |
Forma |
pediplano |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
20.82 |
the_geom |
MULTIPOLYGON (((-46.70695350968909 -9.117306455332674, -46.71022695513227 -9.114988442108626, -46.71261085688231 -9.113082412891028, -46.714104931233045 -9.111154844127752, -46.716348646720085 -9.11044328255136, -46.71738836450608 -9.108940469900073, -46.71873138093296 -9.108645998453307, -46.72105617515865 -9.109137152068014, -46.722176104334 -9.1088352673235, -46.723654324701634 -9.10756201697902, -46.72446704736606 -9.10619530401718, -46.73596413358821 -9.100357543015887, -46.7356627312501 -9.099041313783273, -46.734672179100606 -9.098582000612305, -46.73504620090899 -9.09695445028383, -46.73596539034727 -9.095776809501896, -46.73730050473238 -9.095807657064695, -46.73915628958855 -9.097269956555898, -46.742307132557805 -9.095925286351717, -46.74407879234651 -9.09629444406731, -46.74532294759294 -9.095451422172754, -46.745561754025125 -9.094803524616948, -46.7413931293957 -9.09230463377189, -46.74064143114865 -9.09119654995209, -46.74379521848696 -9.089636049562653, -46.74826440446205 -9.088976481780602, -46.74975318215582 -9.087266227040605, -46.75176450203281 -9.08698745776551, -46.754421822355205 -9.087527724494713, -46.75879992073919 -9.085995046844998, -46.75982069965302 -9.085256089803238, -46.75967285067469 -9.082197914874653, -46.761593160031076 -9.081043453096791, -46.763380413437936 -9.080758103468206, -46.76554528371309 -9.078737277519764, -46.76570182759107 -9.07688566142677, -46.76432551449976 -9.074018866608903, -46.76490201313263 -9.073159935397937, -46.7642589134574 -9.072163444415382, -46.76323128566684 -9.073229649548882, -46.762589258532415 -9.072124346920873, -46.76250596090314 -9.07103123882115, -46.76078814902644 -9.06848326100202, -46.75968029344432 -9.068238752262706, -46.75920660370963 -9.069426756245667, -46.75770534557608 -9.06802605427292, -46.75621671583738 -9.065155488143775, -46.7545988700554 -9.063046195275588, -46.75242222168363 -9.061032614069862, -46.74976810560384 -9.051262691166297, -46.75058136347851 -9.049864626583783, -46.751926988816436 -9.04946032831661, -46.75041993733633 -9.047351968704566, -46.7492690575263 -9.044380039938206, -46.74947854031324 -9.040350256125699, -46.750622566900105 -9.039068416045684, -46.74988266312089 -9.037524344879383, -46.7486750696646 -9.036841928204009, -46.744248958395765 -9.035755823501749, -46.7446275603268 -9.038491640978911, -46.74414802169601 -9.03989718552619, -46.74312826899609 -9.040637034935294, -46.744965106665134 -9.042861668256407, -46.74482308523322 -9.044132936728868, -46.744239804053194 -9.045210250065093, -46.74257999456882 -9.044844765396405, -46.741090507065344 -9.046554139962595, -46.7408389340546 -9.047747715313909, -46.73957539862557 -9.049354803942798, -46.73921429571493 -9.050435895743933, -46.736852677754534 -9.051471213074516, -46.73379323615078 -9.053689754801812, -46.73194724668505 -9.056372320034358, -46.72992328911679 -9.057197496612053, -46.72718571954221 -9.059860287269569, -46.727495858025996 -9.060848504772508, -46.72601788701223 -9.062122724457614, -46.726319225266685 -9.063438119854865, -46.72869917774576 -9.066221534520102, -46.72821455683928 -9.067845452808005, -46.72710670934515 -9.06760171066921, -46.72724080483203 -9.06673172161607, -46.72363450480031 -9.064029850598407, -46.72025482786982 -9.065695100398994, -46.71922027383611 -9.066978656773452, -46.71804150483716 -9.06967789895419, -46.71723881173145 -9.070640775341797, -46.716006586857134 -9.070938928327227, -46.7147895313423 -9.073105497864578, -46.71589739027675 -9.073349285852453, -46.71903384432842 -9.074041121889678, -46.72134869218704 -9.075919244228295, -46.72322462197612 -9.07977921996594, -46.72429402679841 -9.081385109207009, -46.72460172323128 -9.081195698441935, -46.72550013813995 -9.089810799513355, -46.72467928689836 -9.090384277181181, -46.7200996555041 -9.09195597037186, -46.71916327636318 -9.093118860720429, -46.7177761932114 -9.09614910287741, -46.71654704167573 -9.096911207407151, -46.716724224250676 -9.097903189356087, -46.72140794717533 -9.100284252819693, -46.721774699658944 -9.1017752018868, -46.72074573696439 -9.102640484191133, -46.7191215103213 -9.102997469274513, -46.715593618105515 -9.102815879470757, -46.71343129585174 -9.10869274444817, -46.71260507653663 -9.109462297237028, -46.70975959242179 -9.11028355447463, -46.7090250084757 -9.111452371278581, -46.70787234738546 -9.113685574990656, -46.70695350968909 -9.117306455332674))) |
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_3c0b |
Folha |
SC23 |
Legenda_Completa |
197Dt21 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Chapadas e Vales da Bacia do Alto Rio ParnaÃba |
Identificacao_Unidade |
197 |
Nome_Unidade |
Vãos da Bacia do Alto ParnaÃba |
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 |
Vãos da Bacia do Alto ParnaÃba |
Area_Poligono_Km2 |
29.716 |
the_geom |
MULTIPOLYGON (((-46.097441121230126 -9.036944726783933, -46.09716053370388 -9.038276214272562, -46.095251696646805 -9.041788275766539, -46.09355929578599 -9.042785850645421, -46.0916847368593 -9.04496501972311, -46.09202396430756 -9.049422643232228, -46.09132425482422 -9.051993462392714, -46.09331618182398 -9.053501261057367, -46.096907022006185 -9.053993746706025, -46.09794736105439 -9.054760883438355, -46.098935326901525 -9.057605314371067, -46.09981243806342 -9.058813167950778, -46.10305561886467 -9.062305312496273, -46.10425585225693 -9.0627796979613, -46.108813460519 -9.06229920870282, -46.11014693425777 -9.063519475172306, -46.11097777144872 -9.0665058619586, -46.11214619892953 -9.068166792892514, -46.11335757590581 -9.06819715148605, -46.11473741849958 -9.067638820184804, -46.11706459436251 -9.065470996054286, -46.1187184346017 -9.06595678999237, -46.12006311356437 -9.066731236214919, -46.123744656726245 -9.069977225016581, -46.12989841473502 -9.073205682025868, 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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_3c0c |
Folha |
SC23 |
Legenda_Completa |
139Dc23 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
139 |
Nome_Unidade |
Chapada da Tabatinga |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
baixa |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Chapada da Tabatinga |
Area_Poligono_Km2 |
10.521 |
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_3c0d |
Folha |
SC23 |
Legenda_Completa |
139DEc31 |
Nome_Dominio |
Crátons Neoproterozóicos |
Nome_Regiao |
Região não identificada - domÃnio 4 |
Identificacao_Unidade |
139 |
Nome_Unidade |
Chapada da Tabatinga |
Letra_Simbolo |
DEc |
Categoria |
Estrutural convexa |
Natureza |
dissecação |
Caracteristica |
dissecação estrutural |
Forma |
topo convexo |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Chapada da Tabatinga |
Area_Poligono_Km2 |
87.002 |
the_geom |
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