冰碛（qì）岩全称为冰碛砾泥岩，是世界稀有的石种之一。其色为灰褐，暗褐，质量重，坚而脆，内夹杂有砂石或其他小生物化石。
冰碛岩屑 morainic debris
类冰碛岩 paratillite ; [岩] tilloid
准冰碛岩 para-tillite
带状冰碛岩 banded tillite
德怀卡冰碛岩 [岩] Dwyka tillite
块状冰碛岩 massive tillite or Unstratified Diamicts
亿年冰碛岩西施壶 hundreds of millions of years moraine rock xishi pot
亿年冰碛岩原石茶具 hundreds of millions of years of moraine rock original stone tea set
兰皮诺认为某些冰碛岩是由流星撞击而产生的，而不是冰川。
Rampino thinks that certain tillites were produced by meteor impacts, not glaciers.
宜昌莲沱地区早震旦世南沱冰碛岩，位于鄂中古岛陆西部冰川前缘地区。
The Nantuo Formation of Early Sinian Epoch in Liantuo area, Yichang is situated in glacier frontland of western palaeo—island continent of central Hubei.
此外，现代冰碛物的组构特征，对于研究古冰碛和冰碛岩也有着重要的意义。
In addition, the fabric characteristics of modern till are also of importance to the study of the ancient till and tillite.
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