{"id":319,"date":"2014-08-13T07:33:54","date_gmt":"2014-08-13T07:33:54","guid":{"rendered":"https:\/\/www.closdecaille.com\/le-terroir\/la-geologie\/"},"modified":"2022-02-11T15:08:40","modified_gmt":"2022-02-11T14:08:40","slug":"geology","status":"publish","type":"page","link":"https:\/\/www.closdecaille.com\/en\/le-terroir\/geology\/","title":{"rendered":"Geology"},"content":{"rendered":"<p>The Clos de Caille terroir consists of two geological classes:<\/p>\n<ul>\n<li><strong>Limestone<\/strong>\u00a0Deposited over 3 million years ago on top of a layer of sediment, the proportion of limestone varies between 40-60 % depending on the parcel.<\/li>\n<li><strong>Clay<\/strong>\u00a0Of a more recent origin, approximately one hundred thousand years old, clay occurs on gently sloping hillsides.<\/li>\n<\/ul>\n<p>The Clos de Caille has been\u00a0drained ever since the 19<sup>th<\/sup> century, and benefits from a fast water run off which protects the quality of the grapes.<\/p>\n<p>The complexity of a limestone-clay geology gives our terroir optimum conditions to produce distinguished wines.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Our terroir, limestone-clay geology.<\/p>\n","protected":false},"author":1,"featured_media":1892,"parent":311,"menu_order":1,"comment_status":"open","ping_status":"open","template":"","meta":{"_acf_changed":false,"footnotes":""},"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v22.4 - 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