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Anna Ruby Falls Has Ice-Sheathed For The First Time In Eleven Years. Ranger Pope: 'It Is Beautiful And Also Not A Destination You Should Currently Visit.'

Anna Ruby Falls — the tandem waterfall pair at the terminus of the Smith Creek hiking trail in the Chattahoochee-Oconee National Forest, approximately 4.2 miles northeast of downtown Helen — has, following the seven-day sub-freezing cold snap of January 4 through January 10, 2026, developed a partial ice sheath across approximately 70% of its two falling columns. Curtis Creek (the 153-foot column, on the left from the viewing deck) and York Creek (the 50-foot column, on the right) are both encased in what U.S. Forest Service Ranger Calvin Pope describes as 'translucent blue-white ice, with intermittent flowing channels behind.' The ice formation is the first since January 2015.

Garrett "Buck" Pendergrass
Garrett "Buck" Pendergrass
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Anna Ruby Falls, photographed Monday, January 12, at approximately 10:40 a.m., from the public viewing deck at the end of the Smith Creek trail. Curtis Creek (the taller, left-side column) is visibly ice-sheathed from the upper lip down to approximately 100 feet; the remaining 53 feet of the column remains in visible liquid flow. (Photo: Bavarian Brainrot / Garrett 'Buck' Pendergrass)

The cold snap of Sunday, January 4 through Saturday, January 10, 2026 — a seven-day period in which temperatures in the upper Smith Creek drainage, elevation 2,040 feet, averaged 18°F and dropped to a low of 6°F at approximately 4:47 a.m. Wednesday, January 7 — produced the first substantial ice-sheathing of Anna Ruby Falls since January 2015, when a comparable but shorter cold snap produced a similar, slightly smaller, formation.

I hiked up the Smith Creek trail Monday morning, January 12, with Ranger Calvin Pope of the U.S. Forest Service's Anna Ruby Falls Visitor Center, to document the formation. The hike, ordinarily a moderate 0.4-mile walk from the Visitor Center parking lot on a paved ADA-accessible surface, required the use of ice cleats above the trail's midpoint. The Visitor Center has, per Ranger Pope, advised all visitors against attempting the hike without appropriate traction. I had borrowed a pair of Ranger-issue Yaktrax from the Center's loaner supply.

The formation

Curtis Creek, the 153-foot-high northern column of the tandem formation, is, as of Monday morning, sheathed in ice from its upper lip (elevation 2,178 feet, the top of the rock face) to a clear horizontal demarcation line at approximately 100 feet above the lower pool (elevation 2,078 feet). The ice is, per my visual inspection from the public viewing deck, approximately 3 to 5 inches thick at its most built-up sections, and is translucent — a pale, milky blue-white with the suggestion of channels of liquid water flowing behind and occasionally through its mass.

Below the demarcation line, the remaining 50 feet of Curtis Creek's column flows in visible liquid form, striking the lower pool in its usual arrangement.

York Creek, the 50-foot southern column, is, per Ranger Pope, approximately 80% ice-sheathed — slightly more extensively covered than Curtis Creek's 70%. This is, Ranger Pope explained, a consequence of York Creek's substantially lower volume of flow: less water is moving through the column, so more of the water's mass has had time to freeze against the rock face.

The two falls, from the public viewing deck at 10:40 a.m. Monday, were producing a continuous, low-register, percussive sound — water flowing behind ice, occasional ice chunks breaking loose and striking the lower pool, and the wind moving through the exposed lip of each column. I have visited Anna Ruby Falls approximately forty times over the past twenty-eight years. I have not before heard this sound.

The advisory

Ranger Pope's standing advisory, as of Monday afternoon, is that the formation is "beautiful and also not a destination you should currently visit" — specifically for members of the general public without prior winter-hiking experience or proper traction equipment. The advisory cites the following reasons:

  1. The Smith Creek trail, above its midpoint, is substantially ice- covered. A hiker without traction has an elevated fall risk.
  2. Ice chunks are, under current daytime-warming conditions, falling from both columns. The observation deck is within the estimated fall shadow of occasional such chunks.
  3. The Center's ambulance-access from the public parking lot to the trailhead is, per current road conditions, estimated at 20-30 minutes longer than under normal conditions.
  4. The Center, which is ordinarily staffed by three rangers in peak season, is presently staffed by Ranger Pope alone.

The Center recommends, per Ranger Pope's advisory, that visitors wishing to view the ice formation do so via the webcam feed maintained at the USFS website (linked from anna-ruby-falls-live-cam on this publication), which offers a continuously updated image from a fixed camera on the Center's roof.

Expected duration

Per the National Weather Service's extended forecast for the Helen upper-slope region, temperatures are expected to moderate into the mid-40s°F range during the daytime through the end of January, with continued sub-freezing nighttime lows. Ranger Pope estimates, based on his own observation of the 2015 formation's dissipation curve, that the 2026 ice sheath will persist, in visible form, through the end of the month.

"It will be what it is for about two weeks," Ranger Pope said, standing at the observation deck at approximately 11:14 a.m. "Then it will stop."

He paused.

"I wanted to see this again," he said.

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