nõlvadel paiknevate allikate või koobaste suudmete juurde tekkivad allikalubjast terrassilaadsed pinnavormid; kujunevad temperatuurimuutusest tingitud kiirel kaltsium karbonaadi sadestumisel
terrace like landform made of tufa and formed by a process of rapid precipitation of calcium carbonate at the mouth of a spring or a limestone cave
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