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The Pithlachascotee River, often called the Cotee or "Cootie" River, [1] [2] [3] is a blackwater river in Pasco County, Florida . Originating near Crews Lake, the river flows for over 23 miles (37 km) [4] to the south and west, flowing through the Starkey Wilderness Park before turning northwest through downtown New Port Richey, entering the ...
As it paralleled the coastline, Alma produced a storm tide of 10 ft (3.0 m) in New Port Richey. The high tides caused significant flooding in Cedar Key. In northern Florida where Alma moved ashore, wind gusts reached 100 mph (160 km/h) in Crawfordville; the high winds damaged the local tobacco crop.
12-48500 [3] GNIS feature ID. 0287669 [4] Website. City of New Port Richey. New Port Richey is a city in Pasco County, Florida, United States. It is a suburban city included in the Tampa-St. Petersburg-Clearwater, Florida Metropolitan Statistical Area. The population was counted at 16,728 in the 2020 census.
Get the New Port Richey, FL local weather forecast by the hour and the next 10 days.
Gulf High School. / 28.235328; -82.717220. Gulf High School Buccaneers. Gulf High School is a four-year public high school in New Port Richey, Florida. It is part of the Pasco County School System in Pasco County, Florida. It is the first high school in western Pasco County and the second school in Pasco County to offer the International ...
The Tampa Bay hurricane of 1921 (also known as the 1921 Tarpon Springs hurricane) was a destructive and deadly major hurricane which made landfall in the Tampa Bay area of Florida in late October 1921. The eleventh tropical cyclone, sixth tropical storm, and fifth hurricane of the season, the storm developed from a trough in the southwestern ...
12-58600 [4] GNIS feature ID. 0289237 [5] Website. cityofportrichey .com. Port Richey is a city in Pasco County, Florida, United States. It is a suburban city included in the Tampa-St. Petersburg-Clearwater, Florida Metropolitan Statistical Area. As of 2020, the city had a population of 3,052.
Tide. Simplified schematic of only the lunar portion of Earth's tides, showing (exaggerated) high tides at the sublunar point and its antipode for the hypothetical case of an ocean of constant depth without land, and on the assumption that Earth is not rotating; otherwise there is a lag angle. Solar tides not shown.