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Mokulēia, Hawaii

Census-designated places in Honolulu County, HawaiiPages with Hawaiian IPAPopulated coastal places in HawaiiPopulated places on Oahu
Honolulu County Hawaii Incorporated and Unincorporated areas Mokuleia Highlighted
Honolulu County Hawaii Incorporated and Unincorporated areas Mokuleia Highlighted

Mokulēʻia (Hawaiian pronunciation: [mokuleːˈʔijə]) is a North Shore community and census-designated place (CDP) in the Waialua District on the island of Oʻahu, City & County of Honolulu, Hawaiʻi, United States. Mokulēʻia means "isle [of] abundance" in Hawaiian. As of the 2020 census, the CDP had a population of 1,816. Features of interest here include Mokulēʻia Beach, Mokulēʻia Polo Field, and Dillingham Airfield, west of the town. At the western end of Farrington Highway, approximately 1-mile (1.6 km) beyond Dillingham Airfield entrance, begins the track (trail) to Kaʻena Point, the westernmost tip of Oʻahu. The U.S. postal code for Mokulēʻia is 96791.

Excerpt from the Wikipedia article Mokulēia, Hawaii (License: CC BY-SA 3.0, Authors, Images).

Mokulēia, Hawaii
Mahinaai Street,

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Geographical coordinates (GPS)

Latitude Longitude
N 21.577222222222 ° E -158.15888888889 °
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Address

Mahinaai Street

Mahinaai Street
96791
Hawaii, United States
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Honolulu County Hawaii Incorporated and Unincorporated areas Mokuleia Highlighted
Honolulu County Hawaii Incorporated and Unincorporated areas Mokuleia Highlighted
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Nearby Places

Waiʻanae Range
Waiʻanae Range

Waiʻanae Range (sometimes referred to as the Waianae Mountains) is the eroded remains of an ancient shield volcano that comprises the western half of the Hawaiian Island of Oʻahu. Its crest, at Kaʻala, is the highest peak on Oʻahu at 4,025 feet (1,227 m). Like the neighboring Koʻolau, the Waiʻanae Range is not a mountain range in the sense most people are familiar with, as the mountain range as a whole was created from a single volcano rather than plate tectonics. The oldest lava dated from the volcano are about 3.9 million years old. About 3.2 million years ago, the volcano's activity changed, the rate of eruption started to decrease and the composition of the lava erupted from the volcano changed. The volcano is thought to have last erupted about 2.5 million years ago. When active, the Waiʻanae volcano's center of activity was at present-day Lualualei Valley. Intense erosion on the western flank of the mountain has destroyed much of those flanks. Thus, the mountain today is much smaller than it was when the volcano was active. While the western part of the mountain has been destroyed by erosion, the eastern part is still in a youthful stage of erosion. This is considered somewhat strange by some geologists since the western part of the volcano is on the leeward side of the island; thus, most rain falls on the eastern side of the volcano. Given this information, more erosion would be expected on the eastern portion of the mountain. One theory to explain this erosion pattern is that a large landslide cut away the western portion of the volcano. The faults from this huge landslide weakened the rock, making the western part of the mountain much more susceptible to erosion than the eastern side.