Access HonoluluA royal palace downtown, and a crater at the end of the beach.
Diamond Head (Lēʻahi)
THE CRATER AT THE END OF THE BEACH

Diamond Head (Lēʻahi)

A volcanic tuff cone some 400,000 to 500,000 years old, named for a tuna's fin in Hawaiian and for diamonds that were never there in English, with a steep army trail of 1908 to its summit.

Photo: Farragutful, Wikimedia Commons, CC BY-SA 4.0

Home · Sights · Diamond Head (Lēʻahi)

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What you are looking at

Diamond Head (Lēʻahi)

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    The crater floorA wide grassy bowl inside the rim, with the visitor center, where the trail begins.
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    The switchbacksThe first part of the trail, a paved and then rocky path zigzagging up the inside of the crater wall.
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    The stairs and the tunnelSteep flights of steps and a lighted tunnel about 225 feet long near the top.
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    The fire control stationA concrete bunker on the summit, built to direct coastal artillery, now the lookout.
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    The summit viewWaikīkī, downtown and the Koʻolau ridge to the west, the reef and the ocean below.
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    The lighthouseA navigational lighthouse of 1917 on the seaward slope, seen from the trail and the coast road.
The grassy floor inside Diamond Head crater
The grassy floor inside Diamond Head craterFarragutful, Wikimedia Commons, CC BY-SA 4.0
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The sight in full

Reading the place

Why it matters

Diamond Head is the shape everyone knows from Honolulu: the broad, ridged cone at the east end of Waikīkī Beach, seen behind the hotels, the surfers and the palms in countless photographs and films. It is a State Monument, and since 1968 a National Natural Landmark. Climbing it is the most popular walk in the city, and the view from the top explains Honolulu's layout better than any map: the reef, the beach, the towers, and the green ridges of the Koʻolau behind.

Kiawe trees on the crater floor, the rim behind
Kiawe trees on the crater floor, the rim behindFarragutful, Wikimedia Commons, CC BY-SA 4.0

It is also a reminder that the city stands on volcanoes. Diamond Head belongs to the Honolulu Volcanic Series, a set of younger cones and vents that also made Punchbowl and other landmarks on the island.

Two names

In Hawaiian the mountain is Lēʻahi, most likely from lae, a brow or promontory, and ʻahi, the tuna: the ridgeline was said to look like the dorsal fin of a tuna. The English name came in 1825, when British sailors found sparkling calcite crystals in the sand on its slopes, took them for diamonds and called the place Diamond Hill. The hill became Diamond Head, from headland. The Hawaiian rendering Kaimana Hila, “Diamond Hill,” is the title of a well-known song of 1916 by Charles King.

How the crater formed

Waikīkī and the city spread below the Diamond Head summit
Waikīkī and the city spread below the Diamond Head summitFarragutful, Wikimedia Commons, CC BY-SA 4.0

Diamond Head is a tuff cone: a crater made when rising magma met water and exploded, throwing out ash that settled and hardened into the rock called tuff. It formed long after the Koʻolau volcano, which built this side of Oʻahu, had gone quiet; the Koʻolau range is about 2.6 million years old, and Diamond Head only some 400,000 to 500,000. The whole landmark, crater and outer slopes together, covers more than 475 acres.

A fort in a volcano

The crater was the first military reservation of the United States in Hawaiʻi, Fort Ruger, and the summit was a strategic lookout in the early 1900s because of its view over Waikīkī and the south shore. The trail you walk was built in 1908 as part of the Army's coastal defense system, to reach a fire control station at the summit that would direct the fire of the coastal guns in case of war. Bunkers and pillboxes still stand on the rim.

The reef and the Kāhala shore seen from the summit
The reef and the Kāhala shore seen from the summitFarragutful, Wikimedia Commons, CC BY-SA 4.0

Parts of the crater are still used by the government and closed to the public. A National Guard emergency operations center and the state's civil defense headquarters remain inside, and antennas stand on the rim. In the 1960s and 1970s the crater floor also held a series of large music festivals, sometimes called Hawaiian Woodstock.

The trail

The hike runs 0.8 mile from the trailhead on the crater floor to the summit and climbs 560 feet. It starts gently, on a paved path, then turns into a rocky trail of switchbacks up the inside of the crater wall. Near the top come steep stairs and a lighted tunnel about 225 feet long, and then the last climb to the fire control station, where you come out onto the lookout.

The switchback trail climbing the inside of the crater wall
The switchback trail climbing the inside of the crater wallPrayitno / Thank you for (12 millions +) view from Los Angeles, USA, Wikimedia Commons, CC BY 2.0

From the summit you look west over the whole of Waikīkī and downtown to the harbor, north over Kapahulu and Kaimukī to the Koʻolau ridge and Mānoa valley, and down onto the reef and the lighthouse of 1917 on the seaward slope.

The mountain in song

Diamond Head has been sung about for more than a century. Charles King's Kaimana Hila of 1916 is a Hawaiian-language classic. In 1964 the instrumental “Diamond Head,” written by Danny Hamilton and recorded by The Ventures, became an international hit, and in Japan it was the first single to sell a million copies. The Beach Boys recorded a song of the same name.

Diamond Head from the air, the crater open toward the city
Diamond Head from the air, the crater open toward the cityMiguel Teixeira, Wikimedia Commons, CC BY-SA 3.0

In 1952 the crater appeared on an air mail stamp issued for sending orchids to the mainland, and television kept it in the background for decades, as the scenic backdrop of shows set in Hawaiʻi.

At the foot of the mountain

The dry plain below the western slope was chosen by King Kalākaua in the 1870s for a horse-racing course, and in 1877 it became Kapiʻolani Park. On the seaward side, the road curves around the base of the cone past the lighthouse of 1917 and the cliffs above the reef, with lookouts over the surf; the photographs of the lighthouse and the rocky shore on this page were taken there.

The Diamond Head lighthouse, built in 1917, on the seaward slope
The Diamond Head lighthouse, built in 1917, on the seaward slopeAnna, Wikimedia Commons, CC BY-SA 3.0

From the park you can walk to the crater entrance, so a morning can join the two: the climb while it is cool, and then the shade of the park's trees and a swim at the Diamond Head end of Waikīkī.

How to visit

You need a reservation. Visitors who are not Hawaiʻi residents must book an entry time, and a parking reservation if they drive in, in advance through the state parks reservation site; residents with valid identification are exempt. See booking ahead. Walk-up entry cannot be counted on.

The start of the trail, the green crater wall above
The start of the trail, the green crater wall aboveCliff from Arlington, Virginia, USA, Wikimedia Commons, CC BY 2.0

State Parks advises good walking shoes, water, a hat and sunscreen, and planning about an hour and a half to two hours for the round trip. The trail is exposed, hot for most of the day and steep near the top, and the summit is not accessible to people with limited mobility, though the crater floor facilities are. Go early in the day, when it is cooler.

From Waikīkī the crater entrance is a walk of some distance or a short bus ride; getting around explains TheBus.

Honest notes

Dry grass on the seaward slope, the lighthouse below
Dry grass on the seaward slope, the lighthouse belowJason Jacobs from Honolulu, USA, Wikimedia Commons, CC BY 2.0

There were never any diamonds. And the Diamond Head on film, from the 1963 film of that name to two versions each of Hawaii Five-O and Magnum, P.I., is almost always the view from Waikīkī. The mountain itself, from inside the crater, looks nothing like that famous profile; it is a dry, grassy bowl ringed by rock.