The frozen waterfall of the Juncalito River is a 7-meter vertical ice wall at 3,900 m (12,795 ft) in the Diego de Almagro municipality, 220 km from Copiapó and 150 km from Diego de Almagro. It is a winter phenomenon visible strictly between June and August, when sub-zero Andean temperatures freeze the river into a massive curtain of ice and icicles. Reaching the site requires high-clearance 4x4 transport followed by a gentle 1 km hike through the canyon, alongside technical mountaineering layers designed for daytime temperatures near 0 °C (32 °F) and nights plunging below -15 °C (5 °F).
What Is the Frozen Waterfall of the Juncalito River and Where Is It Located
The frozen waterfall forms in a narrow rocky gorge carved by the Juncalito River in the high Andes of Chile's Atacama Region. Unlike alpine cascades in central Chile, this watercourse flows through an arid, wind-scoured canyon fed by high-altitude glacial springs and permafrost runoff.
When the coldest months of the southern hemisphere winter settle over the Puna, the continuous flow freezes layer upon layer. The result is a solid vertical ice wall standing 7 meters tall against volcanic bedrock, draped with thick icicles reaching down to the canyon floor.
| Technical Parameter | Specification |
|---|---|
| Administrative location | Diego de Almagro Municipality, Atacama Region, Chile |
| Altitude | 3,900 m.a.s.l. (12,795 ft) |
| Ice wall height | Approx. 7 vertical meters (23 ft) |
| Freezing season | June to August (austral winter) |
| Distance from Copiapó | 220 km / 137 mi (approx. 3.5 to 4 hours driving) |
| Distance from Diego de Almagro | 150 km / 93 mi (approx. 2.5 hours driving) |
| Vehicle required | True 4x4 with low-range transfer case (4L) and high clearance |
| Hike length | 1 km round-trip (flat trail along the canyon bed) |
| Hiking time | 20 to 30 minutes each way |
| Average temperatures | 0 °C (32 °F) daytime with wind chill; below -15 °C (5 °F) at night |
| Mobile cellular reception | None throughout the cordillera and access tracks |
When to Go: The Seasonal Ice Window from June to August
The complete freezing of the waterfall is strictly seasonal. During spring and summer, water flows freely through the gorge, swelling as snow melts from surrounding peaks, leaving only the bare rock face behind the current.
Solid ice begins to consolidate by mid-June, when polar air masses lock into the Atacama Andes. Throughout July and early August, the structure reaches its greatest thickness and structural integrity. By late August, increasing solar radiation begins fracturing the outer icicles, and running water begins seeping behind the ice sheet.
If you plan a winter trip, always check regional road reports and weather alerts for whiteout conditions (viento blanco). Although Atacama is the driest desert on Earth, winter frontal storms can deposit heavy snow on high mountain passes, temporarily cutting off unpaved access roads.

How to Get to the Juncalito Canyon: 4x4 Routes
Reaching the trailhead requires a dependable 4x4 vehicle in solid mechanical condition. The route runs over dirt tracks and harsh mining gravel where standard highway tires face high risk of puncture from sharp volcanic stones.
Two primary overland routes lead into the area:
- From Copiapó (220 km): Take International Route 31-CH eastward toward Paso San Francisco. Past the historic mining ruins of Puquios and before climbing toward Salar de Maricunga, branch northward onto secondary mountain tracks that skirt the pre-cordillera to reach the Juncalito river basin.
- From Diego de Almagro (150 km): Drive up Route C-13 toward Llanta and the outskirts of Potrerillos, taking cordilleran detours toward Tranque Juncal and the canyon entrance.
The final stretches follow unmaintained mining tracks with severe washboard (calamina), deep sand patches, and morning black ice in shaded gullies. If you are traveling without your own vehicle from Copiapó, consult our guide on mountain gear and 4x4 rental in Copiapó (in Spanish) to confirm the exact vehicle specifications needed for high Puna terrain, or review day outings like the Laguna Verde hot springs tour and the Pedernales salt flat and turquoise lagoon tour.

Driving precaution: Leave Copiapó or Diego de Almagro with a full fuel tank plus at least one certified 20-liter spare canister. There are zero gas stations anywhere in the Andes.
Hiking the Canyon and Spotting Andean Wildlife
Where the vehicle track ends due to the narrowing rock walls, park on a wide, stable shoulder clear of any seasonal flood channels. From there, an easy 1 km hike follows the dry riverbed into the gorge.
The path weaves between sheer volcanic cliffs that channel the mountain wind. There is virtually no elevation gain, though the ground consists of loose talus, hard-packed sand, and slippery patches of frozen crust. Sturdy mid-cut hiking boots and trekking poles are strongly recommended.
During morning walks, hikers regularly encounter native Andean fauna well-adapted to winter extremes:
- Vicuñas (Vicugna vicugna): Graze in small family herds across nearby wetlands (vegas) where sub-surface springs remain active. Maintain a respectful distance to avoid disrupting their grazing patterns.
- Culpeo Fox (Lycalopex culpaeus andinus): Often scavenges among canyon boulders hunting mountain rodents. Its winter coat is thick, plush, and rust-colored.
- High-Andean Birds: Look for ground-tyrants, Andean geese (piuquenes), and buff-necked ibises sheltering on leeward slopes.
The walk to the base of the frozen waterfall takes 20 to 30 minutes at an unhurried pace. At 3,900 m (12,795 ft), the reduced partial pressure of oxygen demands steady, deliberate movement to avoid premature breathlessness.
Weather, Thermal Warnings, and Required Winter Gear
Winter temperatures in the Juncalito Canyon offer zero margin for poor preparation. Under direct midday sunlight, ambient temperatures hover between 0 °C and 4 °C (32 °F to 39 °F), but wind chill inside the shaded gorge immediately drops conditions well below freezing. By late afternoon or during wind events, temperatures plummet below -15 °C (5 °F).

To explore the canyon safely, dress using a strict three-layer technical system:
- Moisture-wicking base layer: Merino wool or synthetic thermal top and bottoms. Never wear cotton, which traps perspiration and induces rapid hypothermia.
- Insulating mid layer: Heavyweight fleece or Polartec jacket, paired with a lightweight down jacket or synthetic puffy.
- Weatherproof outer shell: A breathable hardshell jacket with windproof membrane to block high-velocity mountain gusts.
- Extremity protection: Thermal beanie covering the ears, thin liner gloves paired with insulated outer gloves, neck gaiter, and heavyweight wool socks.
- Footwear: Waterproof trekking boots with aggressive lug soles. Near the frozen waterfall base, flexible trail microspikes provide reliable grip over slick ice.
- Sun protection: At 3,900 m UV radiation is severe, intensified by reflections off snow and ice. Use Category 3 or 4 sunglasses and broad-spectrum SPF 50+ sunscreen.
To calculate the real cooling impact of canyon winds, use our wind chill calculator. Carry at least 2 liters of drinking water in insulated flasks or thermal bottle covers, as uninsulated bottles will freeze inside your pack. Dry mountain air accelerates dehydration; estimate your fluid needs with our high-altitude respiratory water loss calculator. To visualize the Juncalito basin within the broader Seismiles region, inspect the interactive Seismiles map.
Connecting with High-Altitude Expeditions in Copiapó
Visiting the frozen waterfall of the Juncalito River serves as an outstanding active acclimatization outing for mountaineers preparing for larger peaks in the Atacama Andes. Spending several hours active at 3,900 m triggers red blood cell production without accumulating muscular fatigue from steep ascents.
This sector provides natural access to major summits in the region:
- The Volcán Copiapó ascent (6,052 m / 19,856 ft), located within the same Andean massif and crowned by historic Inca ceremonial ruins.
- The Nevado San Francisco ascent (6,018 m / 19,744 ft), the most accessible 6,000 m peak in the region on the border with Argentina.
- The ultimate high-desert climb on the Ojos del Salado volcano ascent (6,893 m / 22,615 ft), the highest active volcano on Earth.
- The full network of shelters and salt lakes detailed in our guide on the Seismiles Route in Chile and 4x4 logistics and mountain shelters (in Spanish).
¿Listo para poner a prueba tu equipo en la alta montaña?
Acompáñanos en nuestras expediciones guiadas con logística integral, grupos reducidos y guías certificados UIAGM / WFR.
Frequently Asked Questions About the Juncalito Frozen Waterfall
Can you visit the frozen waterfall during summer?
Not as an ice formation. During spring and summer, water runs freely as liquid streamflow and no ice walls remain. The frozen waterfall phenomenon occurs strictly between June and August when Andean temperatures remain continuously below freezing.
Do I need a professional guide to visit the waterfall?
If you have verified experience driving low-range 4x4 vehicles on remote gravel tracks, satellite GPS navigation, and certified cold-weather gear, autonomous access is feasible. However, given the absence of mobile signal, zero mechanical recovery services, and real altitude sickness risks near 4,000 m, booking an authorized local operator or certified guide equipped with satellite communication and emergency medical oxygen is strongly recommended.
Is there an admission fee for the Juncalito River?
There is no entrance fee or checkpoint, as the canyon is situated on open public land. Visitors must practice strict Leave No Trace principles, carry all waste back to town, and refrain from breaking the icicles to preserve the fragile winter structure.
Is ice climbing permitted on the frozen waterfall?
The waterfall forms a 7-meter vertical ice wall with dense consistency in mid-winter. Experienced local climbers occasionally use it for short beginner ice climbing lines. It requires specialized technical gear (ice tools, rigid crampons, ice screws) and careful on-site inspection, as temperature fluctuations can cause sudden detachment of hanging ice pillars.


