The Scale of Iceberg Glacier

Why is the glacier face blue?

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Glacier ScaleA glacier is more than ice; not alive, it crawls; not feeling, it groans, cackles, shouts; passive, it is dangerous to approach closely backed as it is by the southern ice field, over a mile high. The ship nudged as close as a half mile from the massed ice, navigating using the bow thrusters to face first port, then starboard and back to port. I was lucky enough to be on the 11th deck, pictured above, when we caught sigh of the fast ship’s launch, manned by ship’s crew.

Iceberg Glacier Scale
Three person ship launch and glacier base at head of Tempanos Fjord

The crew prepared for a run to the rock face, almost 100 feet high, beneath 500 feet of glacier. Enjoy the views! Click any photograph to visit my online gallery. Purchase a photograph from this newly published series or any of my other popular works.

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Ice Bells

Noticing small miracles, taking the time and effort to capture them…..

These icicles were formed along Fall Creek during the coldest months of February in the Finger Lakes Region of New York State.

The transient nature of these forms is suggested by the thinness of the pedicle joining each bell to the ice lobe of the ledge. Note the golden crystals in the ice lobe.

A visualization of the symbolic power of the numeral three, reflected on itself.  Question: what do “threes” mean to you?

Captured with the Sony DSLR-A700, DT 16-105mm F3.5-5.6 lens, hoya circular polarizing filter, mounted on the Manfrotto tripod with ball head.

Click the photograph for my online gallery Ice Bells listing.

Red Sun over Cornell University

On this spring equinox morning a huge sun, filtered by morning clouds, hangs over East Hill and Cornell University. Taken from our home on West Hill, looking across the valley and Ithaca, New York.

The temperature is a balmy 18 degrees F.

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Red Sunrise Over Cornell– CLICK ME!!!!


Red Sunrise Over Cornell– CLICK ME!!!!


Can you pick out these Cornell landmarks?
— Jenny McGraw Tower
— Lib Slope still covered in snow from last week’s storm.
— the looming fortress shape of Bradford Hall.

Red Sunrise Over Cornell– CLICK ME!!!!


Copyright 2021 All Rights Reserved Michael Stephen Wills

Glacier!!!

experience a glacier of Patagonia

Two person ship launch against glacier base.
Summer was the season for our visit to the edge of eternal, for now, Patagonian ice fields.  Remnants from the last ice age, larger than some (small) countries.  The site is surprisingly noisy with sharp, explosive, ice crackles.
More amazing even than the sounds, the dark shading on the ice is volcanic dust from recent eruptions of many cones. 

Click this link for my series of posts about Chilean fjords and glaciers we visited February 2016.

Copyright 2021 All Rights Reserved Michael Stephen Wills

Ice Bells

Noticing small miracles, taking the time and effort to capture them…..

These icicles were formed along Fall Creek during the coldest months of February in the Finger Lakes Region of New York State.

The transient nature of these forms is suggested by the thinness of the pedicle joining each bell to the ice lobe of the ledge. Note the golden crystals in the ice lobe.

A visualization of the symbolic power of the numeral three, reflected on itself.  Question: what do “threes” mean to you?

Captured with the Sony DSLR-A700, DT 16-105mm F3.5-5.6 lens, hoya circular polarizing filter, mounted on the Manfrotto tripod with ball head.

Click the photograph for my online gallery Ice Bells listing.

Fresh Snow

In Dawn’s Light, Untouched

Here is a story of a local man’s narrow escape from this week’s snowstorm.

Copyright 2020 Michael Stephen Wills All Rights Reserved

The path beckons

just around the corner

What is there, just beyond?

Click image for a larger version.

Click Me for another Malloryville post, “Formed By Water.”

Copyright 2020 Michael Stephen Wills All Rights Reserved

Kame = Pile

Kettle and Kame Topography

Hard on the defunct gravel pit of the northwest side of the preserve is the deposit of glacial rocks washed to some extent by melting ice the former owners of the pit were turning over for profit with the averted result of destroying the water sources for the ecosystems of the future preserve.

The deposit is called a kame. Kames are the obverse of kettles, formed with an enormous remnant of glacial ice melts in place leaving a substantial depression. A kame is formed when earth gathers in a depression formed by meltwater running over a glacial surface. When the glacier melts (in this area the ice wash a mile high), the washed earth is left as a steeply sided pile we experience as a hill.

Water flowing beneath glaciers forms the long, ridged hills, eskers, we explored in yesterday’s post.

The forested land of this video the kame, upper left, shown in the header, an IPhone7 photograph of GoogleEarth. Also marked is a path for the primary esker, the bog formed by a kettle and another kettle that is now a pond. Click me to view a pdf file saved from GoogleEarth. It provides a clearer view of the header image.

Click me for better experience viewing the following video. To do this from WordPress Reader, you need to first click the title of this post to open a new page. Note the replay icon (an arrow circling counter-clockwise.

Click Me for the first post of this series.

Thank You for visiting. Here is a recapitulation of Malloryville Preserve.

Copyright 2020 Michael Stephen Wills All Rights Reserved