With time and pressure from above, the many small ice grains joined and changed to larger crystals, and eventually the deeper crystals merged into a solid mass of ice.
在时间和压力的作用下,许多小冰粒结合到一起变成更大的 晶体,最终较底层的晶体合并成庞大而坚固的 冰块。
Formerly a solid mass that melted and refroze at its edges, it is now thinner, more fractured, and so more liable to melt.
以前的冰块坚固结实,只是在边缘发生融化和再次冻结。现在冰层变薄,变脆,更易融化。
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