
They look like something from a fever dream. Hollow pillars of lava rock stand scattered through a tropical forest near Pahoa on Hawaii's Big Island, some rising six or eight feet, others broken and toppled, their interiors coated with moss and ferns. These are not natural rock formations. They are molds, the stone impressions of living trees that were engulfed by a lava flow in 1790. When the molten rock swept through the forest, it wrapped around the trunks, cooled against the wet bark, and solidified. The trees themselves burned away, but their shapes remained, preserved in basalt like plaster casts of something vanished.
The process that created these formations is straightforward but the results are eerie. When pahoehoe lava, the smooth, ropy variety, encounters a standing tree, the molten rock flows around the trunk and begins to cool against the moisture in the bark. The outer layer of lava solidifies while the interior of the tree burns, leaving a hollow cylinder of stone. Some molds preserve the texture of the bark. Others show the knots where branches once grew. The lava in this area came from Kilauea's east rift zone during a 1790 eruption, the same event that killed a party of warriors near the summit caldera and left their footprints preserved in volcanic ash at what is now Hawai'i Volcanoes National Park. Ancient Hawaiians recognized the molds as remnants of trees, but one of the first Western observers to formally propose this explanation was Rufus Anderson Lyman, a local resident and judge.
What makes Lava Tree State Monument striking is not just the lava formations but the lush tropical forest that has grown up around them. Two hundred years of rain, warmth, and isolation have turned the site into a dense garden. Orchids bloom wild. Moss and ferns colonize every crack in the rock. Tree roots snake across the paved loop trail, lifting and separating the pavement in places, a slow-motion reminder that the forest is still in the process of reclaiming what the eruption took. The 0.7-mile footpath that winds through the park passes formations in every state of preservation, from intact pillars with clearly visible trunk textures to collapsed mounds that reveal their hollow interiors. Inside some of the larger molds, rainwater collects and supports tiny ecosystems of moss and lichens, worlds within worlds contained by walls of cooled basalt.
The land was once part of the extensive ranch holdings of William Herbert Shipman, whose family had deep roots in the Big Island's ranching and conservation history. Shipman was the same landowner who worked with Lorrin Thurston to establish the boundaries of what would become Hawai'i Volcanoes National Park. Today the monument is a state park, free to enter like all Hawaii state parks, with restrooms, picnic tables, and three covered shelters. It is open only during daylight hours since the trail has no lighting. In May 2018, the monument closed when Kilauea's lower Puna eruption sent lava flows dangerously close to the park, a reminder that the same volcanic forces that created the lava trees in 1790 remain very much active. The eruption reshaped entire neighborhoods in nearby Pahoa, adding a modern chapter to the ongoing story of life on an active volcanic landscape.
There is something inherently uncanny about the lava trees. They are negative space made solid, the absence of something preserved in stone. Each pillar marks the exact spot where a living tree stood on a particular day in 1790, its height, its diameter, even its lean captured with a precision no sculptor could match. The forest around them has regenerated completely, so the molds stand among living trees that are themselves descendants, in a sense, of the ones that were destroyed. Wild orchids and morning glories drape across the formations. Deep fissures in the ground, created by the same volcanic forces, drop away beside the trail, their depths filled with ferns. Walking the loop in early morning, with dew on the vegetation and mist filtering through the canopy, the monument feels less like a geological curiosity and more like a memorial, a place where the forest remembers what it lost and shows what it has rebuilt.
Located at 19.48N, 154.90W in the Puna District on Hawaii's Big Island, approximately 2.7 miles southeast of Pahoa. The park is surrounded by dense tropical forest and is not easily distinguishable from the air, but the surrounding Puna District lava flows from the 2018 eruption create dramatic contrast between black lava and green vegetation. Nearest airport: Hilo International (PHTO, approximately 20 miles northwest). Best viewed at low altitude (1,000-2,000 feet AGL) to see the contrast between lava fields and forest. The windward location means frequent cloud cover and rain.