溃坝洪水
溃坝洪水
结合整个西部地区的冰川分布进行整合分析,发现冰川阻塞湖引起突发性洪水的发生规律。
Triggered by outburst flood, mudflow is a kind of debris flow and also a form of soil erosion, and it is an indicator of the most serious soil erosion process in the Loess Plateau.黄土泥流是黄土地区一类重要的灾害地貌过程,是泥石流的一个特殊类型,是水土流失的一种特殊形式,也是山地环境恶化、水土流失极严重的标志。
The outburst flood wave could have traveled as far as 1,250 miles downstream, breaking the river's natural banks, causing extensive flooding and even making the Yellow River switch course.溃坝洪水可能向下游奔涌了1250英里(约合2000公里)之远,冲毁了黄河的天然河岸,令许多地方被淹,甚至导致了黄河改道。