Major Tributaries of the Huang He (Yellow River)

The Huang He (Yellow River) drains a vast basin across northern China. Its major tributaries, ordered roughly west to east:

Right-Bank (Northern) Tributaries

• Tao River (洮河) – Rises in Gansu, joins near Lanzhou. Major sediment contributor.
• Zuli River (祖厉河) – Inner Mongolia/Shanxi border.
• Kuye River (库耶河) – Shaanxi/Inner Mongolia, coal country.
• Wuding River (无定河) – "Unstable River," high sediment, Loess Plateau.
• Fen River (汾河) – Shanxi's mother river, joins near Hejin. Industrial basin (Taiyuan).
• Qin River (沁河) – Shanxi/Henan, joins near Wuzhi.
• Hui River (浑河) – Not to be confused with Huai River. Joins in Henan.

Left-Bank (Southern) Tributaries

• Wei River (渭河) – Largest tributary by discharge & basin (135,000 km²). Xi'an basin. "Mother River of Guanzhong." Joins near Tongguan.
• Luo River (洛河) – Luoyang basin, historic capital region. Joins near Gongyi.
• Yi River (伊河) – Often grouped with Luo system.
• Jialu River (贾鲁河) – Zhengzhou flood diversion channel.
• Dahei River (大黑河) – Lower plain, flood management.

Critical Notes

• "Yellow River" listed as tributary in source is an error—it's the main stem.
• Sediment load: Wei River contributes ~30% of water but <10% of sediment; Loess Plateau tributaries (Wuding, Kuye) contribute disproportionate silt.
• Many smaller tributaries are now seasonal or diverted; the river often fails to reach the sea (Bohai) naturally.
• South-North Water Transfer Project (Middle Route) draws from Han River (Yangtze tributary) to Beijing/Tianjin—relieves Yellow River pressure.

The Huang He's tributaries write the story of North China's water crisis—and its civilization.