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1 language. Português; Edit links. Article; Talk; English. Read; ... Fluid feeders are organisms that feed on the fluid of other organisms. It can refer to ...
Dry Creek is a stream in Boone and Kenton counties, Kentucky, in the United States. [1] It is a tributary of the Ohio River. Dry Creek was so named from low water levels during dry weather. [2] [3] A large wastewater treatment plant has operated on Dry Creek since 1979. [4]
Metropolitan Area Population Five Years and Over Percentage Speaking Spanish at Home Population Speaking Spanish at Home (in thousands) New York-Newark-Jersey City, NY-NJ-PA 18,066,122 20.24 3656 Los Angeles-Long Beach-Anaheim, CA 12,450,222 36.0128 4483 Chicago-Naperville-Elgin, IL-IN-WI 8,898,149 17.3754 1546 Dallas-Fort Worth-Arlington, TX
The motion of the head may induce a bow wave in the fluid which pushes the prey away from the jaws, but this can be avoided by allowing water to flow through the jaw. This can be accomplished by means of a swept-back mouth, as in balaenid whales, [ 21 ] or by allowing water to flow out through the gills, as in sharks and herring .
Following is a list of dams and reservoirs in Kentucky. All major dams are linked below. The National Inventory of Dams defines any "major dam" as being 50 feet (15 m) tall with a storage capacity of at least 5,000 acre-feet (6,200,000 m 3 ), or of any height with a storage capacity of 25,000 acre-feet (31,000,000 m 3 ).
Cherokee State Park was the third blacks-only state park in the United States. It was the first such state park in Kentucky, as well as the Southern United States. The park was opened in 1951 as the companion to the whites-only Kentucky Lake State Park, and it was publicized as "the finest colored vacation site in the South".
The Beech Fork, [1] or Beech Fork River, [2] [3] is a 112-mile-long (180 km) [4] river in central Kentucky in the United States.It is a tributary of the Rolling Fork of the Salt River, with its waters flowing eventually to the Ohio River and ultimately the Mississippi River.
The Camp Nelson Limestone along the Kentucky River gorge between Frankfort and Boonesboro dates to the Middle Ordovician and is the oldest rock exposed at the surface in the state. Additional mudstone and shale formation from the Late Ordovician indicates a shift to a shallower sea, which supported extensive marine life.