— — a brow above the city's edge.
“A tuff cone at the east end of Waikīkī, looking like someone scooped out one side of a hill and left the rest standing. Hawaiians call it Lēʻahi, the brow of the tuna. The trail to the rim is short, switchbacks then a steep tunnel, then a concrete bunker overlooking the channel. The view at the top is half ocean, half hotels, all light.
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Diamond Head, known in Hawaiian as Lēʻahi, is a tuff cone on the south-east shore of Oʻahu, just east of Waikīkī in Honolulu. It formed during a single explosive eruption of the Honolulu Volcanics roughly 300,000 years ago, when superheated steam shaped the broad saucer-rim still visible from offshore. The summit reaches 762 feet (232 metres). The crater and surrounding 475 acres are managed as a Hawaiʻi State Monument, with a 0.8-mile trail from the floor to the rim. British sailors named it Diamond Head in the 1820s, mistaking calcite crystals on the slope for gemstones.
The rim runs roughly east-west, so morning light flares off the trade-wind chop in the channel and afternoon light lays a long shadow inside the crater. Most hikers go up at sunrise; gates open at 6 a.m. and the parking lot fills quickly. Late afternoon, around 4 p.m., is quieter and the angle softens the brown lava and the white hotel ranks along Waikīkī into something closer to ochre and bone. The trail itself climbs 560 feet through switchbacks, a lit tunnel, and a concrete observation bunker built in 1911.
The trail requires a reservation for out-of-state visitors, booked through the Hawaiʻi State Parks site up to thirty days in advance; Hawaiʻi residents enter without one. Parking inside the crater costs ten dollars per vehicle, walk-in entry five dollars per person. The gate opens at 6 a.m. and last entry is 4 p.m. Plan an hour and a half round trip with photos. The trail is paved early, then becomes uneven rock, narrow stairs, and the dark Battery Birkhimer tunnel. Closed-toe shoes and water are essential.