Fan Creek is a small, steep tributary that joins Horsethief Creek in the Columbia Valley, one of a cluster of minor streams, alongside Red Line Creek, Paulding Creek and others, draining toward Horsethief Creek and on to the Columbia River in the Radium-Invermere corridor.
The water
Fan Creek's mouth sits at 50.54984, -116.47655. It runs stream order 3 (low on the 1-to-6+ scale where 1 is a headwater trickle and 6+ a river), a narrow channel with a median width of roughly 2.6 m, dropping at a very steep median gradient near 38.55%, with a peak mean-annual discharge of about 0.077 m³/s (very low flow). That combination, narrow, steep, low-volume, reads as a classic headwater tributary rather than a stream built for a day of fishing.
The fishing
No fish records turn up for Fan Creek in the provincial stream data covering the Horsethief Creek watershed, and no guide, report or online log names it specifically. That is not proof of an empty creek, small steep headwater tributaries are routinely under-surveyed, but it does mean Fan Creek is honestly a regulation-and-access check rather than a confirmed fishery. If it does hold coldwater fish, the character of the wider Horsethief system points toward small-stream basics: caddis, mayfly and stonefly imitations with summer terrestrials, but that is a hypothesis carried over from the surrounding watershed, not a record from Fan Creek itself.
An unconfirmed water
Conditions
- Navigability: narrow and very steep (median width ~2.6 m, narrow; gradient ~38.55%, very steep; peak mean-annual discharge ~0.077 m³/s, very low flow), consistent with a small, technical headwater tributary rather than a stream built for wading any distance.
- Stocking: no stocking record. Nothing suggests Fan Creek is on any hatchery program; it runs, if it holds fish at all, on wild fish only.
Access and the rules
No named trailhead, road access point or put-in has been confirmed specifically for Fan Creek. It sits within the wider Horsethief Creek drainage in the Columbia Valley, part of the tributary network feeding the upper Columbia system around the Radium-Invermere corridor, but the exact route in remains unconfirmed.
