place

Waianae High School

1957 establishments in HawaiiEducational institutions established in 1957Public high schools in Honolulu County, HawaiiUse mdy dates from October 2020
Waiʻanae High School 08
Waiʻanae High School 08

Waiʻanae High School is a public, coeducational secondary school in the City and County of Honolulu, Hawaii, United States, on the leeward (western) coast of the island of Oʻahu. The school about 40 miles (64 km) northwest of central Honolulu CDP. Waiʻanae High School is part of the Leeward School District, under the Hawaii State Department of Education.

Excerpt from the Wikipedia article Waianae High School (License: CC BY-SA 3.0, Authors, Images).

Waianae High School
Farrington Highway,

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Waianae High SchoolContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 21.455173 ° E -158.199925 °
placeShow on map

Address

Farrington Highway (State Highway 93)

Farrington Highway
96792
Hawaii, United States
mapOpen on Google Maps

Waiʻanae High School 08
Waiʻanae High School 08
Share experience

Nearby Places

Mākaha, Hawaii
Mākaha, Hawaii

Mākaha (Hawaiian for "fierce", or "savage", pronounced [maːˈkɐhə]) is a census-designated place (CDP) in Honolulu County, Hawaiʻi, United States. It is a town located along the Pacific coast, west of the Mākaha Valley, and at the foot of Mt. Ka'ala in the Wai’anae Mountain Range. It is the last of the leeward towns on O'ahu. North of Mākaha there is no development, i.e. no towns, no gas stations, or restaurants. The population of Mākaha was 8,278 at the 2010 census. It is located 35 miles northwest of Honolulu, but is a part of Honolulu County. In the Hawaiian language its name means “fierce” or “savage”, which refers to the group of bandits who were based in the Mākaha Valley. They would hide and wait for unsuspecting passersby to show up, and then plunder and pillage them. Mākaha has a higher percentage of Native Hawaiians and other Pacific islanders than most settlements on O’ahu; 26.2% of the population were Pacific Islanders in 2010. Mākaha Resort stages weekend traditional Hawaiian arts and crafts fairs and other Hawaiian cultural programs in order to preserve the Native Hawaiian traditions in Mākaha.The town is particularly known for its surfing waves and surfing history, the Hawaiian temple Kāne’āki Heiau, and Mākaha Beach Park, which is a nesting place for several species of sea turtles. Aside from surfing, other water activities include diving, canoe-surfing, fishing, tandem surfing, bodysurfing, and other recreational water sports. Kāne’āki Heiau is Hawaii's most thoroughly restored ancient heiau, it was excavated by Bishop Museum archeologists in 1970 and can now be visited Tuesdays-Sundays. It originated as an agricultural temple to the god Lono in the 15th century. 200 years later, it was converted into a luakini, where human sacrifices were dedicated to the god Kū – a typical progression indicating Mākaha now supported a large enough population to have its own chief.

Māʻili, Hawaii
Māʻili, Hawaii

Māʻili (Hawaiian pronunciation: [maːˈʔili]) is a census-designated place (CDP) in the Waiʻanae District on the island of Oʻahu, City & County of Honolulu, Hawaiʻi, United States. In Hawaiian, māʻili means "pebbly", referring to rounded stones at the shore. Māʻili is located along Farrington Highway on Oʻahu's Leeward Coast, between Māʻili Beach Park to the west and Lualualei Valley to the east. It is located 1.4 miles south of the town of Waianae, separated by the Māʻiliʻili Stream, and 1.5 miles north of Nanakuli. As of the 2020 census, the town population was 11,535. Māʻili has one 7-Eleven, a gas station, and a few residential developments. The town is also home to several dairy farms and vegetable plots. Two tall, red antennae near the mouth of the Lualualei Valley are parts of the Navcom Radio Transmitting Facility, and were the tallest man-made structures in the Western Hemisphere at 1,503 feet when they were built in 1972. The town has an elevation of 20 feet (6.1 m).Māʻili has among the highest percentage of Native Hawaiians in Hawai’i, with 48.8% of the population in 2009. Māʻili and its waterfront park, Māʻili Beach Park, is a popular destination for surfing, snorkeling, swimming, boogieboarding, and bodyboarding. Māʻili Beach Park has a total area of forty acres, and is located immediately south of Lualualei Beach Park. The park is home to two popular Hawaiian surf spots: Green Lanterns by the mouth of the Māʻiliʻili Stream, and Tumbleland in the center of the beach park. The water conditions are treacherous during winter-time, but usually calm during summer. The beach park has a lifeguard station, a playground, beach facilities, restrooms, picnic tables, and showers.

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.