No breakthroughs

The water breaks through because upstream – far enough up that there isn’t any stream – there’s a drip, drip, drip.

Enough drips to puddle, to pool and start to trickle and then to run: a rivulet, a stream to cool your feet in.

Further on* lakes, rivers, waterfalls, floods, torrents to burst banks and blow your socks off.

All it takes is gravity, time, and enough drips.

*in no particular hydrological order

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