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La depresión intermedia presenta rasgos de relieve que determinan una serie de cuencas. La más septentrional de ellas corresponde a la del río Maipo, que ha sido modelada por el depósito de sedimentos glaciales, aluviales y fluviales, y por potentes capas de cenizas provenientes sobre todo de las erupciones del volcán Maipo, ubicado en el lím