季风性降雨使杰赫勒姆河、奇纳布河、拉维河和萨特累季河涨满,来自这些河流的急流与印度河在旁遮普南部的拉詹普尔地区汇合。
Massive torrents of water from the Jhelum, Chenab, Ravi and Sutlej rivers fed by these monsoon rains eventually met the Indus at Rajanpur district in southern Punjab.
这条河的水流量是泰晤士河的350倍,它有自己的河道、急流甚至瀑布
Watershed discovery: The river - with 350 times the flow of the Thames - has channels, rapids and waterfalls
台伯河已不再是漫溢平原的泛起泡沫的急流。
The river tiber was no longer a foaming torrent overflowing the plains.
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