I am fascinated by this vantage from the South Rim trail. It is possible because the gorge bends almost 90 degrees, the gorge walls fall away to reveal the 215 foot waterfall.
Tag: Finger Lakes Region
Three Sisters
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.
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Three Sisters, Taughannock Falls gorge wall.
Three Views from The Bend
Taughannock Gorge, November 
Into the Gorge Three Sisters, Taughannock Falls gorge wall.
Copyright 2019 All Rights Reserved Michael Stephen Wills
Zoom In
View from The Bend
Oaks are the last to release leaves, seen here on an early November afternoon.
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Into the Gorge
Views from The Bend
Taughannock Gorge, November Into the Gorge
Copyright 2019 All Rights Reserved Michael Stephen Wills
The Bend
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.
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Taughannock Gorge, November
Copyright 2019 All Rights Reserved Michael Stephen Wills
Hemlock Shadows
The sun, in its wander south, casts long midday shadows
The sun, in its wander south, casts long midday shadows
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Copyright 2019 All Rights Reserved Michael Stephen Wills
Reveal
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.
The Cave?
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.
Falling Water
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.
Fracture
Second element of the same object from last week, see “The Fang?”
The Fang?
Michael Stephen Wills Photography 