Geologia de Alberta e sul das Montanhas Rochosas - IGEO- Unicamp
Geologia de Alberta e sul das Montanhas Rochosas - IGEO- Unicamp
Geologia de Alberta e sul das Montanhas Rochosas - IGEO- Unicamp
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<strong>Geologia</strong> <strong>de</strong> <strong>Alberta</strong> e <strong>sul</strong><strong>das</strong> <strong>Montanhas</strong> <strong>Rochosas</strong>DESENVOLVENDO O CICLODAS ROCHASPedro Wagner GonçalvesInstituto <strong>de</strong> Geociências – UNICAMPCx. P. 6152 Barão Geraldo 13083-970 Campinas-SPe.Mail: pedrog@ige.unicamp.brCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
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eleira <strong>de</strong> Athabasca, Parque Nacional <strong>de</strong> JaspeAltitu<strong>de</strong>: 2700mÁrea: 6 km 2Espessuramédia: 300 mVelocida<strong>de</strong>:125 m/ano(cabeceira), 25na baseNo verãocerca <strong>de</strong>10.000 turistaspasseiam nageleira por diaCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Geleira <strong>de</strong> AthabascaNotar: recuoda geleiraLocal <strong>de</strong>visitaçãocoberto em1980Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
leira <strong>de</strong> Athabasca, vales suspensoCorrenteCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
ocha moutonée e <strong>de</strong>pósitos <strong>de</strong> morena lateral,Geleira <strong>de</strong> AthabascaMorenalateralEstriasCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
OkotokisCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
xo <strong>de</strong> geleira da Cordilheira e Norte-AmericanCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Franksli<strong>de</strong>, escorregamentoCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Lake MoraineCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Lago PeytoCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Lago Peyto: foz <strong>de</strong> material <strong>de</strong> <strong>de</strong>geloCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Franksli<strong>de</strong>Como seformou estevale?E o materialem primeiroplano?Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Calgary, down town (Rio Bow)Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
TilCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
TilCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Canmore TilCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Lago PeytoCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Head Smashed, <strong>sul</strong> <strong>de</strong> <strong>Alberta</strong> (pradarias)Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
<strong>Montanhas</strong> <strong>Rochosas</strong>Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
<strong>Montanhas</strong> <strong>Rochosas</strong>Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
CanmoreCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Mo<strong>de</strong>lagens...Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Mapa geológico: <strong>Rochosas</strong> às pradariasCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Monte Cathedral, calcáriosEscorregamentosCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
nanaskis, cama<strong>das</strong> <strong>de</strong> arenito e carvãCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Kananaskis, siltito finoCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Relação entre grãos e matrizchas Clásticass visíveis anuGrãos maiores visíveis aolho nu ou com lupa 10X(parte fina)PartículaMatrizCimentoCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
ssificação <strong>de</strong> rochas sedimentares clásticxosm,esmCascalhoG r o s saF i n aG r o s saAreiaF i n aSilteArgila60 mmM ádia2062 mm0.6M édia0.20.06 mm0.002 mmãos visíveis ao nuaentos angulosos)lomeradoentos arredondados)Grãos maiores visíveis aolho nu ou com lupa 10X(parte fina)ArenitoGrãos não visíveiscom lupa 10XLamitosSiltitoArgilitoFolhelhCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Rochas Sedimentares Clásticasificação <strong>de</strong> arenitos pelo conteúdo mineral/litológicoenito Quartzoso Arcósio Arenito Lítico GrauvacaCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
Rochas Sedimentares Químicashas Químicasento Rocha Composição Mineraisrito Evaporito Cloreto <strong>de</strong> Sódio HalitaSulfato <strong>de</strong> Cálcio AnidritaGipsitaento Formação Óxido <strong>de</strong> Ferro Hematitaro Ferrífera LimonitaCarbonato <strong>de</strong> Ferro Si<strong>de</strong>ritado Dolomito Carbonato <strong>de</strong> DolomitaagêneseCálcio-magnésioFosforito Fosfato <strong>de</strong> Cálcio ApatitaCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
EvaporitosCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
ochas Sedimentares Bioquímicaschas Bioquímicasimento Rocha Composição Mineraisia e lama Calcário, CaCO 3 Calcitaimento Chert SiO 2 Opala,osoCalcedônia,Quartzofa, matéria Linhito, Compostos (Carvão)ânica Carvão <strong>de</strong> Carbono (Óleo)(Gás)Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
ue idéias centrais po<strong>de</strong>m ser explora<strong>das</strong>a partir da interpretação <strong>das</strong> rochas?Habilida<strong>de</strong> <strong>de</strong> pensar hipoteticamente e construir enarrar a história do que po<strong>de</strong> ter ocorrido com aamostra ou com o local visitadoCapacida<strong>de</strong> para investigar um certo fenômeno apartir <strong>de</strong> vestígios do que ocorreu e alcançarconclusões com base em pequeno número <strong>de</strong>dados (aos mol<strong>de</strong>s do conto policial)Habilida<strong>de</strong> para resolver problemas <strong>de</strong>safiadores ecompreen<strong>de</strong>r processos ocorridos no passado(eventos históricos)Create PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
O que as geociências informam sobre aTerra?Uma idéia central fornecida pelas geociências é a noção <strong>de</strong>tempo geológico: uma escala <strong>de</strong> tempo que combinaeventos <strong>de</strong> diferentes duraçãoA idéia <strong>de</strong> tempo geológico é central para compreen<strong>de</strong>rque o ambiente terrestre mudou e continua mudando aolongo <strong>das</strong> erasO ambiente atual é, portanto, somente um <strong>de</strong> um estado <strong>de</strong>uma série <strong>de</strong> estados que dominaram a TerraSabemos que o ambiente muda ao longo do tempo porqueparte <strong>de</strong>ssas transformações são registra<strong>das</strong> nascaracterísticas <strong>das</strong> rochasCreate PDF with PDF4U. If you wish to remove this line, please click here to purchase the full version
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