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Modelado cársico

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O modelado cársico é um exemplo de uma paisagem sedimentar, onde predomina o calcário. A água da chuva reage com a rocha dissolvendo-a e esculpindo-a, abrindo fendas cada vez maiores e mais profundas. Estas fendas acabam por formar grutas subterrâneas e poços capazes de fazer desaparecer rios.

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