Kingston High School (Washington)

Spectrum Community School was an alternative high school in Kingston, Washington, United States. It was a part of the North Kitsap School District. The school had been running for over 20 years, and earned two awards of Special Merit from the Grammy Foundation in Los Angeles. The school was designed for students searching for a nontraditional learning environment that embraced diversity, inclusion, different learning styles and preferences, tools, and a student empowered curriculum. The school sponsored exchange programs with Russia and Mexico. The school promoted social responsibility, respect for cultural diversity and appreciation for lifelong learning, and was founded with the support of North Kitsap School District and Chris Wendelyn in 1986. Courses met all requirements for a formal STEM education and graduation with a high school diploma. Course design enabled students to integrate areas of interest to strengthen engagement and learning in critical areas of study. School leadership and faculty engaged local communities, traditions, and partnerships to strengthen student inclusion, engagement, and respect. Courses also supported onsite and distance learning objectives. Spectrum Community School was located on the same campus as the future Kingston High School.

Kingston (formerly Appletree Cove) is an unincorporated community and census-designated place (CDP) in Kitsap County, Washington, United States. The population was 2,099 at the 2010 census. Kingston is along the shores of Appletree Cove and Puget Sound, and is home to a major Washington State Ferry terminal linking it to Edmonds.

Appletree Cove is a bay and estuary of Puget Sound on the Kitsap Peninsula in the U.S. state of Washington. The cove is fed by Carpenter Creek; its estuary is a tidal flood zone that fills and empties at high and low tides. Appletree Cove was named "from the numbers of that tree which were in blossom around its shores" by Charles Wilkes who surveyed the area on April 9, 1841, on the Wilkes expedition. Reportedly these Pacific crabapple trees were cleared by Benjamin Bannister after settling at the bay in 1874. Another source says Wilkes mistook flowering dogwoods for apple trees.Appletree Cove is the site of the Kingston ferry terminal for the Washington State Ferries. Appletree Cove is also the former name of the town of Kingston, Washington which is to the north and west of the cove. To the south is an area known by the locals as "Jefferson Beach".

Heronswood is a botanical garden located in Kingston, Washington, in the Northwestern United States. It is also the name for a now defunct mail order specialty plant nursery business that originated at the gardens.

Indianola is a census-designated place (CDP) in Kitsap County, Washington, United States, located on the north shore of Port Madison on the Port Madison Indian Reservation, home of the Suquamish Indian Tribe. The population was 3,500 at the 2010 census. It was originally established as a summer community and was a stop for Mosquito Fleet ferries until the 1950s.

Eglon is an unincorporated community in Kitsap County, Washington, United States. The town has a community center, a church, a cemetery, a boat launch, a beach, and a picnic area. Its Fire Protection services are provided by North Kitsap Fire and Rescue.

Port Madison, sometimes called Port Madison Bay, is a deep water bay located on the west shore of Puget Sound in western Washington. It is bounded on the north by Indianola, on the west by Suquamish, and on the south by Bainbridge Island. Port Madison connects to Bainbridge Island via the Agate Pass Bridge to the southwest. Two small bays open off Port Madison: Miller Bay to the northwest, and another small bay to the south which, confusingly, is also called Port Madison Bay (or, locally, as the "Inner Harbor"). The inner harbor, which indents into Bainbridge Island is where the Port Madison Yacht Club and a Seattle Yacht Club outstation are located. The Port Madison Indian Reservation is located on the west and north shores of Port Madison. According to various sources, the native name of the bay was either Tu-che-kup or Noo-sohk-um. On Nov. 8 1824, John Work of the Hudson's Bay Company, while looking for potential sites for a trading post, recorded it as Soquamis Bay - a variation on the name of the Suquamish tribe which made its home on the western shore. The Wilkes Expedition surveyed the bay on May 10, 1841 and named it for James Madison, the 4th president of the United States. George A. Meigs built a lumber mill on the Bainbridge Island shore of the bay in 1854, and Port Madison was soon a booming mill town. The town of Port Madison became Kitsap County's first county seat, but after the economic depression of the 1890s closed the mill, the seat was relocated and Port Madison became a ghost town. Today, Port Madison is a residential area and a popular destination for boaters.

Little Boston is a community in Kitsap County, Washington, United States. It is located on the east side of Port Gamble, an inlet or bay of Hood Canal, and is direct across the bay from the unincorporated community of Port Gamble. Little Boston is within the Port Gamble Indian Reservation, which houses the Port Gamble band of the S'Klallam tribe. The Port Gamble S'Klallam Reservation consists of 1,340 acres (5 km2) of land held in trust by the federal government. There is no private land ownership on the reservation. Most of the land is in the forest with residential, business, and office areas. The land is listed by the U.S. Census Bureau as the Port Gamble Tribal Community census-designated place, with a population of 916 as of the 2010 census.The reservation receives approximately 20 inches (510 mm) of rain per year due to its location in the Olympic Mountain rain shadow. The reservation lands rise from the beach to gently rolling terrain. Port Gamble Bay is the last bay in Kitsap County that is still open for commercial shellfish harvest. The Tribe has a hatchery on Middle Creek. Bear, deer, and other wildlife also live on the reservation.

The Suquamish Indian Tribe of the Port Madison Reservation is a federally recognized tribe and Indian reservation in the U.S. state of Washington. The tribe includes Suquamish, Duwamish, and Sammamish peoples, all Lushootseed-speaking Indigenous peoples of the Pacific Northwest, and was a signatory to the Treaty of Point Elliott of 1855. They had 950 enrolled tribal citizens in 2012.

The House of Awakened Culture (Lushootseed: sgwәdzadad qәɫ ʔaltxw) is a community house in Suquamish, Washington State, on the Port Madison Indian Reservation. Built by the Suquamish tribe in 2008, it acts as a spiritual successor to the historic Old Man House, which was burnt by the local Indian agent in 1870 in an attempt to disperse the tribe. Since its opening in 2009, the house has served as a community center for the Suquamish tribe and the community.

Suquamish is a census-designated place (CDP) in Kitsap County, Washington, United States. The population was 4,140 at the 2010 census. Comprising the Port Madison Indian Reservation, it is the burial site of Chief Seattle and the site of the Suquamish tribe winter longhouse known as Old Man House.

Haleets (also called Figurehead Rock) is a sandstone glacial erratic boulder with inscribed petroglyphs on Bainbridge Island, Washington. The Native American Suquamish Tribe claims the rock, on a public beach at Agate Point on the shore of Agate Passage, as part of their heritage. The exact date the petroglyphs were carved is unknown but is estimated to be around 1000 BCE to 400 or 500 CE, the latest date being when labrets (worn by one of the petroglyph figures) were no longer used by Coast Salish peoples.Haleets is the Coast Salish name of the rock, also transcribed as Halelos, Xalelos and Xalilc, meaning "marked face". It is known in English as Figurehead Rock. Its purpose is unknown but the Suquamish Museum curator and archivist Charlie Sigo has stated that it may have been a boundary marker. An amateur astronomer has proposed a theory that it has a calendrical function (see Archaeoastronomy). The rock is 5 feet (1.5 m) tall and 7 feet (2.1 m) long. It sits about 100 feet (30 m) offshore, and has been marked with chiseled and drilled Coast Survey features since 1856, and a bronze geodetic mark was placed on it in 1934. Some sources say that the rock is one of three prominent Salish Sea petroglyphs that were always on the shoreline, but tectonic activity around the Seattle Fault may have put Haleets in the intertidal zone.