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Tabernacle Hill Lava Tubes

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Tabernacle Hill Lava Tubes - Fillmore, Utah
Tabernacle Hill Lava Tubes
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Explore the Tabernacle Hill Lava Tubes in Utah, a captivating natural wonder located near Leeds. This unique geological formation offers adventure seekers a chance to hike, explore underground lava tubes, and take in scenic desert landscapes. Ideal for outdoor enthusiasts, photographers, and campers, the lava tubes are a must-see for those seeking an off-the-beaten-path experience in Southern Utah.

Caves

Caves

Exploring

Exploring

Camping: Dispersed camping allowed up to 14 consecutive days.

Water: No potable water; pack your own supply.

More Info

Plants Foraged

Nearby Locations

Meadow Hot Springs

Meadow Hot Springs - Utah

Tabernacle Hill Lava Tubes

West of Fillmore in the high desert of Millard County, Utah, Tabernacle Hill rises from a landscape of ancient volcanic drama — lava flows, cinder cones, and a network of lava tubes formed thousands of years ago when flowing basalt cooled on the outside while still-liquid rock drained from within, leaving hollow tunnels beneath the hardened surface. The result is an accessible and genuinely remarkable underground exploration destination on BLM land with no entrance fee and no crowds.


The tubes themselves are the destination — dark, cathedral-quiet corridors of basalt with rough walls and ceilings that reflect the violent geology of their formation. A headlamp is essential — some sections receive natural light but the deeper sections are genuinely dark. Above ground the landscape is classic Utah high desert — lava rock, sagebrush, juniper, and the open sky that this part of the Colorado Plateau delivers in every direction. Desert lizards work the warm rock. Ravens and golden eagles are the common birds of prey overhead. The approach road passes through white sand dunes that sit in striking contrast against the dark volcanic rock — worth slowing down for on both the way in and the way out.


The Geology

Tabernacle Hill is part of the Black Rock Desert volcanic field — a geologically recent and volcanically active region of western Utah where basaltic eruptions occurred as recently as 1,000 years ago. The lava tubes at Tabernacle Hill formed during a period of active basalt flow when the outer surface of a lava river cooled and solidified while molten rock continued flowing inside — eventually draining out and leaving the hollow tube behind. The ceiling skylights formed where the roof section was thinner and eventually collapsed — creating natural light wells that make exploration of the tubes practical without complete reliance on artificial light.


Our Visit — September 20, 2017

A stop during our month-long trip that began in Utah — we had come from the south and were heading north, with Meadow Hot Springs as our next stop just a short distance away.


On the way in a group of cows at a cattle guard had decided the road was theirs — a welcome and completely unhurried blockade that reminded us whose country this actually is. Eventually they moved.


Luca, Alexis, and I explored one full tunnel and part of a second. The skylights were the highlight — sections where the ceiling has opened to the sky above, sending natural light down into the dark tube in columns that make the whole experience more visually interesting than a uniformly dark cave. The contrast between the deep dark of the unexplored sections and the dramatic shafts of light at the skylight openings is something photographs don't fully capture. We used flashlights throughout and would not have wanted to be without them in the darker sections.


On the way out we played on the white sand dunes along the approach road — a completely different textural and visual world from the dark basalt of the tubes, sitting alongside each other in the same high desert landscape.

Dispersed Camping

Dispersed Camping
Utah

Tabernacle Hill Lava Tubes, Leeds, UT, USA

Washington County

38°54'47.4"N 112°31'52.8"W

Elevation: 5,200 feet



Directions

From Interstate 15, take exit 158 to Meadow and turn south onto Main Street (State Road 133.) Follow Main street to Center and turn west (right) at the sign for White Mountain. It is a well-graded road that passes under the freeway. Continue onto 4000 S, 4000 S turns right and becomes 4600 W, for 0.2 miles, then turns west becoming 3900 S. 3900 S continues to turn northwest, as the road turns north, becoming 6400 West, to a T-junction with 2300 South. Take 2300 South west and then northwest for 1.8 miles to a signed junction with Lava Tubes Road. Turn Left. The road winds a rough 2.1 miles south to a loop parking area. Sounds confusing... I suppose. Google it.

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Best Seasons & Temperatures

Feb-April

Oct-Dec

Spring and fall are the ideal seasons — May through early June and September through October when temperatures at 5,200 feet are comfortable for both the above-ground hike and the below-ground exploration. September as we experienced is excellent — the high desert cooling after summer, the tubes at a comfortable temperature underground, and the surrounding landscape still showing some color. Summer heat at this elevation is significant — the tubes themselves remain cool underground making them a reasonable heat escape, but the exposed approach road and surrounding terrain can be uncomfortable in July and August. Winter visits are possible in dry conditions but the dirt access road can become impassable after snow or rain — verify road conditions before the drive in.

Tabernacle Hill Lava Tubes - Fillmore, Utah

September 20, 2017

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