The Chelan River is a tributary of the Columbia River, in the U.S. state of Washington. Just long, it is the shortest river in Washington. Lake Chelan Dam is located at the river's source: the outlet of Lake Chelan. Nearly the entire river's flow is diverted to the Lake Chelan Powerhouse, downstream near the river's mouth. Thus the Chelan River is almost always dry. Statistics on the streamflow are taken at the tailrace of the powerhouse, measuring the water that would flow through the river were it not diverted, although not including small tributaries, including Daybreak Canyon, that join the Chelan riverbed from the Lake Chelan Dam to the canal outlet. Course The Chelan River originates at the outlet of Lake Chelan, in the city of Chelan at the southern end of the lake. Lake Chelan Dam, also in the city of Chelan, blocks the river. The dry riverbed runs through a steep and rocky gorge, dropping before reaching the Columbia River near the community of Chelan Falls. Only the first short section of the river between Lake Chelan and Lake Chelan Dam is filled with water. The rest is called the "bypassed reach". The Lake Chelan Powerhouse is located adjacent to the river's former mouth. Diverted water is dropped through hydroelectric turbines and released into the Columbia River at Columbia river mile 503.3 (810 km). The tailrace is essentially an arm of the Columbia River with no gradient due to the impoundment of the Columbia by Rocky Reach Dam. River modifications Although Lake Chelan is a natural lake its water level and discharge via the Chelan River has been controlled by Lake Chelan Dam since construction was completed in 1927. Due to the dam, the river is nearly always dry, although sometimes water is spilled over the dam, temporarily recreating a small streamflow in the old Chelan River. The river's water is used not only for hydroelectric power but also irrigation and drinking water. In addition, during the summer the water level of Lake Chelan is maintained at a relatively high elevation for scenic and recreational purposes. Normally water flow in the dry bypassed reach occurs in spring and early summer, when snow melt raises Lake Chelan to levels requiring spill for flood control. The river's water is diverted through a long power tunnel, which ends with a drop through turbines at the powerhouse. Most of the Chelan River's