Standing on the South Rim trail where the gorge bends almost 90 degrees, changing from a northern to eastern flow. The creek is flowing toward the camera, the falls out of view, upper left. Lower left two people walk the 3/4 mile trail of the falls.
The sun, in its wander south, casts long midday shadows
The sun, in its wander south, casts long midday shadows
The elements come into focus, revealing Ludlowville Falls, near Lansing, New York. On the eastern side of Cayuga Lake, Salmon Creek plunges 35 feet over this limestone shelf. Pioneers constructed a grist mill at this site.
Here we see The Fang hanging over the entrance to The Cave. There is falling water overall, but especially the center section (can you see it?). The weight of accumulated ice fractured a portion of the frozen cascade.
Flowing water eroded away until this durable limestone strata. The majority of sedimentary rock is shale, only 6% is limestone. Throughout the Finger Lakes and elsewhere, this is why when flowing water exposed the edge of a limestone strata, the underlying, soft shales are worn away to reveal a waterfall, ever deepening. Eventually, the support of the limestone washes away to form this ledge. Here it is an ephemeral cave behind a curtain of ice.
See “The Fang?” for the first post of this series.
Amid the crystallized water, super-cooled, flowing water seeps through the structure to fall free.
See “The Fang” for the first post of this series.
Michael Stephen Wills Photography 