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Craters of the Moon Sacred Lava Fields exterior
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Craters of the Moon Sacred Lava Fields

An ancestral volcanic landscape where Shoshone and Bannock sacred oral traditions meet monumental basalt fissures.

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Visitor Insights

Visiting Craters of the Moon Sacred Lava Fields

Visitors experience a dramatic open-air sanctuary defined by stark volcanic formations, ancient basalt plains, and quiet cave chambers. Walking along the trails offers profound reflection on the living relationship between geological forces and indigenous cultural memory.

Highlights

  • Walking through the colossal subterranean archways of Indian Tunnel.
  • Ascending Inferno Cone for sweeping vistas across the 52-mile Great Rift volcanic fissure.
  • Viewing pristine kipukas preserving untouched native sagebrush-steppe ecology.
  • Gazing into the dark volcanic night skies recognized as an International Dark Sky Park.

Things to Know

  • Basalt terrain is abrasive and requires sturdy, closed-toe hiking boots.
  • Free self-service cave permits are mandatory before entering any lava tube to protect bat habitats.
  • All ancient stone hunting blinds and archaeological artifacts are strictly protected by federal law.
  • Summer surface heat on dark basalt can exceed 150 degrees Fahrenheit, requiring ample water.

Location

1266 Craters Loop Road, Arco, ID 83213

Hours: Open 24 hours daily year-round; Visitor Center open 8:30 AM to 4:30 PM daily.

Getting There: Located along US Highway 20/26/93, roughly 18 miles southwest of Arco and 24 miles northeast of Carey, Idaho.

Get Directions (opens in a new tab)

Tips for Your Visit

Footwear and Hydration

Wear thick-soled hiking shoes to navigate sharp aa lava safely and carry at least two liters of water.

Cave Etiquette

Obtain a free cave permit at the visitor center and carry a reliable headlamp with extra batteries.

Stay on Marked Paths

Protect delicate cryptobiotic soil crusts and fragile cinder slopes by remaining strictly on designated routes.

About

The Craters of the Moon Sacred Lava Fields encompass an expansive volcanic landscape within the ancestral homelands of the Shoshone and Bannock peoples (Newenee). Shaped across millennia by deep subterranean fissures along the Great Rift, this open-air natural cathedral features vast basalt flows, towering cinder mounds, and subterranean lava tubes that served as sites of shelter, vision seeking, and spiritual encounter.

Rather than a barren wilderness, indigenous traditions understand this geomorphic terrain as an enduring spiritual sanctuary. Oral narratives recount the cosmic movements of the Great Serpent, whose immense coils squeezed the mountains until molten rock poured across the Snake River Plain, creating physical landmarks that remain central to tribal history and cultural continuity.

Today, the landscape operates both as an active ancestral sanctuary and a protected National Monument and Preserve. Tribal stewardship and federal partnerships continue to honor the geological, ecological, and sacred heritage of this monumental volcanic domain.

Tradition
Indigenous (Northern Shoshone & Bannock)
Status
Operating Sacred Landscape
Total Area
753,401 acres
Base Elevation
5,910 feet
Primary Geological Feature
The Great Rift Volcanic Fissure
Federal Designation
May 2, 1924
753,401 acres
Protected Monument & Preserve
52 miles
Great Rift Fissure Length
2100 years BP
Youngest Volcanic Flow
500+
Protected Ecological Kipukas

Common Questions

Why is Craters of the Moon sacred to indigenous tribes?

It is the ancestral homeland of the Shoshone and Bannock peoples, holding physical records of the Great Serpent cosmogony.

Did native people live inside the lava fields?

They traversed the flows seasonally, using lava tubes for shelter and constructing stone blinds for hunting.

What is a kipuka?

A kipuka is an island of ancient soil and vegetation entirely surrounded by younger lava flows.

Are the lava fields permanently extinct?

The volcanic rift is considered dormant, with future basaltic eruptions geologically expected along the Great Rift.

Can visitors enter the lava tube caves?

Yes, visitors can enter designated caves after obtaining a free permit at the visitor center.

Timeline

10000 BCE

Paleo-Indian Habitation

Ancestral indigenous bands begin seasonal use of the Snake River Plain volcanic margins.

Milestone
2100 BCE

Great Rift Eruptive Period

Major fissure eruptions pour fresh basalt across central Idaho hunting corridors.

Event
100 BCE

Youngest Volcanic Outpouring

Final fissure eruptions at North Crater give rise to Shoshone oral traditions of the cosmic serpent.

Milestone
1200

Stone Blind Construction

Hunters construct semicircular basalt walls along crater rims to intercept game.

Milestone
1750

Equestrian Transhumance

Shoshone bands use pack horses along trails skirting the northern lava margins.

Event
1862

Goodale's Cutoff Established

Emigrant wagon trains begin utilizing northern lava corridors during westward migration.

Event
July 3, 1868

Fort Bridger Treaty

Treaty sets aside ancestral lands and precedes forced relocation to Fort Hall.

Event
May 2, 1924

National Monument Proclaimed

President Calvin Coolidge designates the volcanic field as a national monument.

Dedication
August 22, 1969

Apollo 14 Lunar Training

NASA astronauts explore the monument's lava tubes and craters to study volcanic geology.

Milestone
November 9, 2000

Presidential Preserve Expansion

President Bill Clinton vastly expands the protected area tenfold through Proclamation 7373.

Milestone
August 21, 2002

National Preserve Designation

Congress formally designates the expanded acreage as a National Preserve under joint federal management.

Milestone
May 2, 2024

Centennial of Protected Status

Centennial events highlight ongoing tribal cooperative stewardship and cultural preservation.

Milestone

History by Decade

10,000 BCE — Paleo-Indian Era

Following the retreat of Pleistocene glaciers, ancestral indigenous peoples inhabited the Snake River Plain. Semi-nomadic bands utilized the edge of cooling volcanic fields, hunting megafauna and establishing sacred paths across the emerging basalt landscape.

100 BCE — The Youngest Eruptions

The final major eruptive phase of the Great Rift occurred at North Crater and Sheep Trail Butte. Ancestral Shoshone witnessed fountains of fire and spreading pahoehoe flows, embedding these geological spectacles directly into enduring oral histories.

1700s — The Horse Era

The acquisition of the horse expanded the seasonal mobility of Shoshone and Bannock bands. Seasonal hunting parties navigated established trails across the lava fields while traveling between western camas prairies and eastern bison hunting grounds.

1860s — Emigrant Encroachment and Treaties

The creation of Goodale's Cutoff in 1862 brought emigrant wagon trains along the northern fringe of the volcanic fields. The Fort Bridger Treaty of 1868 subsequently led to forced tribal relocation to the Fort Hall Reservation, disrupting seasonal access while spiritual bonds persisted.

1920s — National Monument Establishment

Explorer Robert Limbert completed extensive expeditions across the volcanic field, publicizing the region's remarkable geology. On May 2, 1924, President Calvin Coolidge officially proclaimed Craters of the Moon National Monument to preserve its unusual geological formations.

2000s — Preserve Expansion and Collaborative Stewardship

President Bill Clinton signed Proclamation 7373 in November 2000, vastly expanding the protected monument area. Federal agencies expanded formal consultation with the Shoshone-Bannock Tribes, integrating traditional ecological knowledge into modern site interpretation.

Architecture & Facilities

The site functions as an open-air natural temple shaped by continental basaltic fissure volcanism along the Great Rift. Undulating pahoehoe terraces, jagged aa ridges, and towering spatter chimneys form monumental natural architecture recognized by indigenous traditions as living spirit ground.

Building Materials

Basaltic Pahoehoe

Smooth, ropy lava formations featuring subtle metallic blue and bronze iridescent crusts.

Aa Basalt

Dense, fractured scoria clinkers that formed natural defensive barriers and defined ancient trails.

Obsidian and Vitrophyre

Dark volcanic glass quarried by ancestral artisans for sharp projectile points and tools.

Pyroclastic Cinder Tuff

Charcoal-black volcanic gravel forming monumental cinder cones like Big Cinder Butte.

Interior Features

Indian Tunnel

A colossal lava tube chamber over eight hundred feet long illuminated by natural skylights.

Dewdrop Cave

A sheltered basalt cavern displaying delicate layered lava benches and breakdown blocks.

Boy Scout Cave

A frigid subterranean chamber that houses a perennial ice floor even through hot summers.

Beauty Cave

A deep lava tube terminus demonstrating pristine flow textures and smooth basalt ceilings.

Temple Grounds

Over seven hundred thousand acres of protected volcanic tableland featuring undisturbed sagebrush kipukas, ancient stone blinds, and fragile cinder ecosystems.

Additional Facilities

The Robert Limbert Visitor Center offers educational exhibits, tribal cultural panels, and backcountry permit facilities.

Religious Significance

To the Shoshone and Bannock peoples, the volcanic expanse is a living, conscious relative rather than an inanimate desert.

The landscape serves as a perpetual sanctuary for reflection, spiritual renewal, and honoring cosmic forces of earth renewal.

Sacred Ordinances

Vision Seeking and Fasting

Solitary contemplation undertaken within secluded lava caverns and remote cinder cones to seek spiritual direction.

Seasonal Harvesting

Ceremonial gathering of wild medicinal roots, sweetgrass, and minerals from protected kipukas.

Oral Remembrance Rites

The retelling of the Great Serpent cosmology to transmit sacred geography and ethical responsibility to younger generations.

Kinship with Volcanic Forces

Indigenous cosmologies view volcanic eruptions as physical expressions of earth transformation and spiritual purification.

The Sanctuary of the Kipukas

Surrounded by impassable fields of sharp aa lava, kipukas preserve native desert plants in their pristine ancestral state.

Sources & Research

Every fact on Temples.org is backed by verified Sources & Research. Each piece of information is rated by source tier and confidence level.

Tier A
Official Primary source from official institution
Tier B
Academic Peer-reviewed or encyclopedic source
Tier C
Secondary News articles, travel sites, or general reference
Tier D
Commercial Tour operators, booking agencies, or promotional content
View All Sources (7)
Field Source Tier Retrieved
About & Historical Background National Park Service (opens in a new tab) A 2026-02-18
Indigenous Cultural Heritage & Treaties Shoshone-Bannock Tribes (opens in a new tab) A 2026-02-18
Timeline & Geologic Eruptions National Park Service (opens in a new tab) A 2026-02-18
Archaeological Records & Pioneer Trails National Park Service History Electronic Library (opens in a new tab) B 2026-02-18
Geographic Terrain & Rift Systems PeakVisor Topographic Database (opens in a new tab) B 2026-02-18
Cosmology & Symbolic Elements Armchair Explorer Travel Guide (opens in a new tab) C 2026-02-18
Visitor Insights & Regulations South Idaho News Archive (opens in a new tab) C 2026-02-18