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The Hawaii water resource region is one of 21 major geographic areas, or regions, in the first level of classification used by the United States Geological Survey to divide and sub-divide the United States into successively smaller hydrologic units. These geographic areas contain either the drainage area of a major river, or the combined ...
Following is a list of dams and reservoirs in Hawaii. 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 ).
Rank Name Population (2020) County 1 Honolulu †† 350,964 Honolulu: 2 East Honolulu: 50,922 Honolulu: 3 Pearl City: 45,295 Honolulu: 4 Hilo † 44,186
Category: Bodies of water of Hawaii by island. ... Bodies of water of Oahu (1 C, 8 P) This page was last edited on 15 July 2017, at 03:49 (UTC). Text ...
Captain Cook is located on the west side of the island of Hawaii at (19.498211, −155.904275 It is bordered to the north by Kealakekua and to the south by Honaunau-Napoopoo . Hawaii Route 11 , part of the Hawaii Belt Road , passes through the community, leading north 12 miles (19 km) to Kailua-Kona and south 47 miles (76 km) to Naalehu .
The word skookum means "strong", and chuck means "water". [6] The Quinault Indian Nation , by way of the 1856 Treaty of Olympia, hold fishing rights on the river. Beginning in 2021, the river is allowed to be used as a year-round water bank and is the largest in the state, allowing a draw of 28,000 acre-feet of water per year.
In the rainy winter season, high water levels enlarge the freshwater pond to more than 400 acres (1.6 km 2). [7] [8] By spring, water levels begin dropping [9] and by summer, the pond shrinks to half its winter size, leaving a salty residue behind: this accounts for its name, "Kealia", meaning "salt encrusted place"; [7] Coastal salt pans once produced the mineral from seawater. [4]
The surrounding topography of a catchment zone influences the flow vectors and direction that the water flows. [1] Water flows from areas of high potential energy to low potential energy under the influence of gravity. The geometry of the slope leading to the catchment area influences the amount of water the catchment will contain. [1]