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The dates of spring tides and neap tides, approximately seven days apart, can be determined by the heights of the tides on the classic tide tables: a small range indicates neaps and large indicates springs. This cycle of tides is linked to the phases of the moon, with the highest tides (spring tides) occurring near full moon and new moon.
The Wilson River, about 33 miles (53 km) long, flows from the Northern Oregon Coast Range to Tillamook Bay in the U.S. state of Oregon.Formed by the confluence of its Devil's Lake Fork and its South Fork, it runs generally west through the Tillamook State Forest to its mouth near the city of Tillamook.
Summers in Tillamook are brief and mild with average daytime temperatures in the upper 60s, although daytime temperatures can occasionally soar into the 80s and 90s for days at a time. Summer is by far the driest season in Tillamook with only 1.35 inches and 1.33 inches of rain (34 mm in either case) falling in July and August, respectively.
The Tillamook River is a stream, about 17 miles (27 km) long, near the coast of northwest Oregon in the United States. It drains an oceanside valley in the foothills of the Northern Oregon Coast Range west of Portland and empties into the Pacific Ocean via Tillamook Bay . [ 3 ]
Tillamook Bay is a small inlet of the Pacific Ocean, approximately 6 mi (10 km) long and 2 mi (3 km) wide, on the northwest coast of the U.S. state of Oregon. It is located just north of Cape Meares in western Tillamook County approximately 75 mi (120 km) west of Portland .
Sometimes known as "the town that fell into the sea", it was a planned resort community founded in 1906 on Tillamook Spit, a small stretch of land that forms one wall of Tillamook Bay. [ 1 ] [ 2 ] Bayocean's post office was established on February 4, 1909, and by 1914, the town's population was 2,000. [ 2 ]
The shellfish in question include oysters and bay clams from Netarts Bay and Tillamook Bay, Oregon, harvested on or after May 28, and all shellfish species from the area of Willapa Bay, Washington ...
A bore in Morecambe Bay, in the United Kingdom Video of the Arnside Bore, in the United Kingdom The tidal bore in Upper Cook Inlet, in Alaska. A tidal bore, [1] often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current.