42.6921, -76.3900

Fillmore Glen is the gorge park that Watkins Glen takes all the regional press from, which means Fillmore has the visitor load it deserves for the quality it delivers. This is not a criticism of Watkins Glen, which earns its reputation, but an observation about what that reputation displacement has done for Fillmore: kept it manageable. The crowds are present on summer weekends but not overwhelming in the way that Watkins Glen is overwhelming in July and August, and in off-season months the gorge is often nearly empty, which is the correct condition for doing anything useful with it.

The gorge trail drops into the canyon fast from the parking area. The microclimate shift happens within a few hundred yards of the trailhead: cooler, distinctly damper, with the sound of the creek amplified against the Tully limestone walls. If you have been in Taughannock or Watkins Glen gorges you know the acoustic quality I am describing. The stone walls contain and reflect sound in a way that changes how you experience the space, and in the narrow sections of the Fillmore gorge that effect is pronounced.

The falls sequence runs through four or five distinct drops depending on where you are counting and what the water level is doing. In a wet spring the drops are full and loud and the spray radius makes tripod work complicated without protection on the gear. In a dry September, as this visit was, they narrow to ribbons in some places and threads in others, which reveals the plunge pool and channel geometry that the higher flows obscure. From a geological reading standpoint, low water in a gorge is more informative than high. You can see what the water has done over ten thousand years without the water being in the way.

The September afternoon light threads into the upper gorge at a specific angle that exists for perhaps ninety minutes if you position correctly relative to the gorge orientation. I spent that ninety minutes working the upper section. The limestone takes the low light differently than it takes overhead light, and the color shift in the wet rock from the angle is worth being there for specifically.

We were on the same circuit as the Fairgrounds and Labrador Hollow that day, which made for a full morning of documentation across three distinctly different photographic subjects. Coming from the south, Fillmore serves as the geological anchor of the sequence, the oldest and most dramatic of the three, the place that reminds you what water and time and uplift do when given sufficient distance to work.

Five stars in the right conditions. Rate this particular September visit as what it was: a productive working afternoon in a gorge that rewards repeated visits across different seasons and flow conditions. Spring runoff is being scheduled. The Schoharie Creek gorge comparison trip is also being planned, which will give me a better frame for where Fillmore sits in the regional gorge hierarchy.