粒度分析表明，从冰水河流一直往湖泊，粒度特征正好与河流地貌特征和湖泊地貌特征一致。
Grain size analyses indicate that the grain size characteristics are consistent with the lake and river features from the glacial river to the lake.
成千上万条冰水河流自山上顺流而下，其中的一些来自于几千米高的山脉，它们可以流向海拔只有几百米的地区。
About one hundred thousand of these rivers of ice flow down mountains. Some start from thousands of meters up a mountain. They can flow to areas just a few hundred meters above sea level.
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