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Shine Tidelands State Park is a 249-acre (101 ha) Washington state park located in Jefferson County, seven miles (11 km) south of Port Ludlow.The park has 5,000 feet (1,500 m) of shoreline on Bywater Bay adjacent to the west end of the Hood Canal Bridge and offers activities including picnicking, fishing, shellfish harvesting, beachcombing, birdwatching, windsurfing, and wildlife viewing. [1]
Tide tables, sometimes called tide charts, are used for tidal prediction and show the daily times and levels of high and low tides, usually for a particular location. [1] Tide heights at intermediate times (between high and low water) can be approximated by using the rule of twelfths or more accurately calculated by using a published tidal ...
Leadbetter Point State Park is a nature preserve and public recreation area located sixteen miles (26 km) north of the city of Long Beach, Washington, at the northern tip of the Long Beach Peninsula. The state park is bounded by the Pacific Ocean to the west and Willapa Bay to the east and shares a border with the Willapa National Wildlife Refuge.
The Long Beach Peninsula is known for its continuous sand beach 28 miles (45 km) in extent on the Pacific Ocean side, claimed to be the longest beach in the United States. It is a popular vacation destination for people from Seattle, Washington (165 miles (266 km) distant) and Portland, Oregon (115 miles (185 km) distant).
Willapa Bay is fairly shallow: more than half of its surface area lies in the intertidal zone, and half of the volume of water inside it enters and leaves with every tide. The bay is an estuary formed when the Long Beach Peninsula, a long sand spit from the Columbia River to the south, partially enclosed the estuaries of several smaller rivers.
Cape Disappointment State Park (formerly Fort Canby State Park) is a public recreation area on Cape Disappointment, located southwest of Ilwaco, Washington, on the bottom end of Long Beach Peninsula, the northern headlands where the Columbia River meets the Pacific Ocean.
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range").
Seaview's history began in 1859 when Jonathan Stout, a cooper from Ohio, arrived on the Long Beach Peninsula. [3] In 1880 he purchased 153 acres along the ocean front with plans for a summer resort. [4] He ran through several names for the resort—Stout's, Ocean View, North Pacific Beach, and finally Sea View.
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