Photographer at work, captured by his wife
Pam captured me at work on the north rim of Black Canyon, Colorado. That is a Manfrotto studio tripod and hydro-static ball head.
The header photograph is mine of a hot air balloon over our home last summer. I imagine us floating, the Black Canyon below us.
On viewing this photograph my wife, Pam, noticed the shapes eroded from the sedimentary rock of Taughannock gorge. These layers of shale, sandstone, siltstone formed at the bottom of a broad, shallow sea over 380 million years ago. Differential wearing of these rock layers, clearly visible in this photograph, resulted in these formations, including the three sisters and overhangs.
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.
Michael Stephen Wills Photography 