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Giz é uma rocha sedimentar porosa. Ele é constituído de carbonato de cálcio. É um tipo de calcário constituído por calcite. Forma-se em condições de águas relativamente profundas a partir da acumulação gradual de minúsculas placas de calcite largadas por microrganismos chamados cocolitóforos. É comum encontrar nódulos de cherte e sílex encravados no giz. As falésias brancas de Dover são constituídas por giz. O giz e xato More information...

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