Frozen Fall Creek II

Natural Ice Sculpture

My last post, “Frozen Fall Creek I”, ended with macros of Ice Crystals on a bed of frost over creek ice within sight of our former home, a restored water mill. I continued on the ice, following the creek to this spot were the stream bed turns 90 degrees, changing from a southerly to a western flow.

Here I encountered an open course where constant water motion resisted freezing. A few frigid days later, the course had an amazing transformation.

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Last To Freeze, Fall Creek

The transparent ice of the now frozen space retained the impression of movement, the surface rippled by current. In the following photograph, motionless ice crystals reveal the truth.

Ice Crystals on Water Frozen while Supercooled

In the intervening days, the constant motion resisted freezing while the water temperature dropped well past freezing to achieve a supercooled state. As the water temperature continued to drop, a fast transition from fluid to solid happened so quickly the movement of the water surface was preserved.

Ice Crystals on Water Frozen while Supercooled

Here is the matching “after” photograph to the “before” that started this post.

Channel of Water Frozen while Supercooled
Click me for “Fall Creek Winter,” another stunning scene.
Copyright 2019 All Rights Reserved Michael Stephen Wills

Frozen Fall Creek I

Ice Crystals

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Winter Shadows
Ice Crystals
Ice Crystal Macro I
Ice Crystal Macro II
Ice Crystal Macro III
Click me for the next post in this series, “Frozen Fall Creek II.”
Click me for another Winter Series starting with “The Fang?”
Copyright 2019 All Rights Reserved Michael Stephen Wills

Reveal

SONY DSC

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?

The Object Comes Into View

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

SONY DSC

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.