The Dahan River (, also spelled Tahan) is a river in northern Taiwan. It originates in Hsinchu County and then flows through Taoyuan City and New Taipei City for 135 km, before it joins Xindian River in Taipei to form the Tamshui River. The upper reaches of the Dahan are also known as Takekan Creek () or Taigang Creek (泰崗溪). An alternative historical name for the Dahan is the Shihmen River (石門溪).
The Dahan River once flowed north through the area of Taoyuan City to empty into the Taiwan Strait about west of the mouth of the Tamsui River. The Taoyuan Plateau is the ancient alluvial fan of the Dahan River, created by sediments eroded from the mountains. About 30,000 years ago, tectonic movement caused the Taipei Basin to drop in elevation, and the Tamsui River system Stream piracy the Dahan River and caused it to flow northeast. As a result the Dahan River cut a canyon through the alluvial sediments for more than to reach the new lower elevation. The former channels of the Dahan River remain as "beheaded" streams that flow only seasonally across the plateau.
The Shihmen Dam, one of Taiwan's first multi-purpose water projects, was completed in 1964. It provides flood control, irrigation, domestic water supply and hydroelectricity for much of Taoyuan and New Taipei City. The dam has had problems with silt build-up since its construction, due to the high rate of erosion caused by typhoon storms and earthquakes in the upper Dahan River drainage. About 123 "sabo dams" () have been built along the Dahan River upstream in order to block silt and extend the useful life of the Shihmen reservoir. Chief among these is the Junghua Dam, upstream. The second largest dam, the Baling dam, failed during Typhoon Wipha in 2007, destroying Baling village and washing of silt into the Dahan River.
The Taiwanese government has proposed the construction of a mega-dam on the Takekan Creek known as Gaotai Dam (高台壩) to trap silt and provide additional water storage. This plan has been criticized due to its potential environmental damage, and its limited useful life, because the new reservoir would also eventually fill with silt.
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