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Mount Washington (Cascades)

King County, Washington geography stubsMountains of King County, WashingtonMountains of Washington (state)
Mount Washington Cascades
Mount Washington Cascades

Mount Washington is a small mountain in the US state of Washington roughly 30 miles (48 km) east-southeast of Seattle, Washington along Interstate 90. It lies on the western margin of the Cascade Range just above the coastal plains around Puget Sound, and is southeast of nearby town of North Bend. Once known as Profile Mountain, Mount Washington was named due to a cliff resembling a profile of George Washington when viewed from an angle.The hike to the top of Mt. Washington is known for its view. Cedar Butte lies at the west end of the mountain.

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Mount Washington (Cascades)
Mount Washington Trail,

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N 47.425938 ° E -121.7001055 °
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Mount Washington Trail

Mount Washington Trail

Washington, United States
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Mount Washington Cascades
Mount Washington Cascades
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Chester Morse Lake
Chester Morse Lake

Chester Morse Lake (originally Cedar Lake) is a lake in the upper region of the Cedar River watershed in the U.S. state of Washington. The original lake surface was 1,530 feet (466 m) above sea level, but when the river was dammed in 1900, the elevation was raised to 1,560 feet (475 m). Chester Morse Lake is more than four miles (6 km) long, and is primarily fed from the east by the north and south forks of the Cedar River, and from the south by the Rex River. The lake is part of the Seattle area water supply. Located in the upper watershed, Chester Morse Lake is impounded by the masonry dam and a secondary control structure called the Overflow Dike. The lake now functions as a water supply storage reservoir and powers a 30-megawatt hydroelectric facility. Chester Morse Lake was previously a natural lake called Cedar Lake. Cedar Lake was formed about 14,000 years ago by the terminal moraine of an alpine glacier descending the Cedar River valley from the upper elevations of the Cascade Mountains. Because upstream fish passage to Chester Morse Lake is naturally blocked by Cedar Falls, the fish populations in the lake are isolated from those downstream. Bull trout and pygmy whitefish populations in Chester Morse Lake have thus been separated from other populations for at least 13,000 years, and represent unique genetic stocks of these species. Both of these species spend most of their time in deeper portions of the lake. The surface of Chester Morse Lake has an average annual fluctuation of about 20 feet in elevation. Inundation of the Cedar and Rex river deltas strongly affects their aquatic and wetland habitats. Changes in lake level management toward higher lake levels in the past 15 years have resulted in a retreat upslope of sedge and willow communities on the delta. Inundation of the Cedar and Rex river channels within and upstream of the delta causes sedimentation that can negatively affect bull trout eggs. Studies are underway to examine these effects.