clockwise around Lake Washington
eastbound on Tolt Pipeline Trail
only memories will remain
- Dream argument (Wikipedia)
The dream argument is the postulation that the act of dreaming provides preliminary evidence that the senses we trust to distinguish reality from illusion should not be fully trusted, and therefore, any state that is dependent on our senses should at the very least be carefully examined and rigorously tested to determine whether it is in fact reality.
Washington State Route 520
Washington Trails Association
- Blyth Park (wta.org)
Blyth Park lies along the Sammamish River in the City of Bothell. Near the park entrance are all the amenities you would expect: a large parking lot, restrooms, plenty of picnic tables and a playground. One of the main attractions here is the 10-hole disc golf course (watch out for flying discs, some of the holes run across the trail!).
- Marymoor Park (wta.org)
With a handful of trails to explore, including a wetland marsh boardwalk that runs along the Sammamish River, Marymoor Park is a perfect place to spot wildlife.
- Sammamish River Trail (wta.org)
The Sammamish River Trail is a 9.5-mile trail with one end at Marymoor Park in Redmond, passing through Woodinville, and the other end at Blythe Park in Bothell. At Blyth Park, it connects with the Burke-Gilman Trail and continues another 18.8 miles ending at Golden Gardens in Seattle.
- Sammamish River (Wikipedia)
The Sammamish River runs for about 13.7 miles (22.0 km) through portions of King County, Washington, draining Lake Sammamish into Lake Washington. It flows out of Lake Sammamish at Marymoor Park in Redmond, before continuing through suburban residential areas in Redmond, Woodinville, Bothell, and Kenmore. About 32% of the river’s riparian habitat is forested, with the invasive reed canarygrass found across its course. The river hosts fish such as salmon as they migrate between the lakes. It has four major tributary streams: Bear Creek, North Creek, Swamp Creek, and Little Bear Creek. The floodplain was carved out by a glacial meltwater channel during the Vashon Glaciation, about 15,000 years ago, resulting in a geology dominated by glacial deposits and alluvium.
