January 23, 1986 - Ice to Follow January Thaw?January 23, 1986
The Suffolk Times
Ice to Follow January Thaw?
By PAUL STOUTENBURGH
Ice and winter are pretty synonymous
here in the northeast. Young and old
alike know ice means winter sports. Of
course, ice here is nothing like ice in
Maine or upstate New York, but
nevertheless we get our share here on
the island. Nowadays, we always get
breaks in the weather, such as we have
just experienced, and then our winter's
ice disappears. It's an on- again, off -
again thing of late, but it wasn't always
so. It seems to me as a kid our bays and
creeks would freeze over in December
and stay that way until March.
There were always thick manholes of
ice scattered on the surface of the creek
ice where men and boys had chopped
holes so their long - handled spears could
probe the bottom for the sleeping eels
below. It was cold but rewarding work.
You could usually tell a good spot by
the parked cars down by one of the
creeks. Usually it took a lot of exploring
and chopping to find a good spot. Of
course, being like a beacon out on the
ice would draw attention, particularly
if you had started to bring up eels. It
wouldn't be long before others would be
out there with their ax, bag and spear
-- ready to get their share.
I remember an old friend of mine from
the city who came out weekends and
was always looking for something to do.
One day he followed me out on the ice
in Eugene's Creek to see how we
speared eels. It had snowed a bit that
night and a new layer covered up every-
thing, including the thin new ice that
covered our previous eeling holes. We
were talking about this and that and
not paying too much attention to any-
thing when, to and behold, Herb disap-
peared. Right up to his crotch he went!
He had fallen into one of the newly -fro-
zen -over holes. There he sat on the ice.
What could we do but laugh? Herb
promptly returned home to dry off, but
he was soon back for more.
Home Ice Advantage
We always skated on the creek ice
because it was always the closest to
home. It never seemed to be as smooth
and fast as the ice in the ponds and
lakes, but it would do. From the creek
side, the first thing you learned was to
watch out for the edge. It was here the
tide went up and down and kept a
slushy area between the solid ice and
the shore. If you didn't know this, and
you happened to step in this slushy
area, you were in for a muddy retrieval.
Nothing dangerous, but it sure put a
hold on skating until you got back with
dry socks.
There is something spectacular about
ice when it starts to move. In a small
way, it gives you the idea of a miniature
glacier on the move. Put wind or tide
behind a huge mass of ice and some-
thing has to give. Often I've seen great
chunks of creek or bay beach literally
planed level by this moving ice. In many
places, huge walls of ice are formed as
the ice piles up and under itself. A good
northwest wind when there is ice in the
Sound will give you this effect and is
also responsible for building up the wall
of sand and gravel that's characteristic
of that shore.
Trying to relate this to the great
Focus on
Nature
glaciers that helped form our island
boggles the mind. Imagine an ice sheet
thousands of feet thick, stretching from
Wisconsin to Cape Cod, moving south-
ward ever so slowly, grinding, planing,
smoothing, polishing everything in its
way. The rounded stones and boulders
we see along the north shore and scat-
tered throughout our island vouch for
its work. Depressions, some dry, some
wet like Marratooka Lake, Laurel
Lake, Lake Ronkonkoma and Lake Suc-
cess, are reverse monuments to these
glaciers passing. Here huge chunks of
the glacial ice broke off and were plowed
under as the glacier moved on. Later,
after the glacier retreated because of
the warming of our climate, these
buried chunks of ice started to melt,
leaving the depressions that in some in-
stances created our lakes and in other
instances dry kettle holes.
The glaciers formed our land in many
ways, some hardly recognized today.
Each of our creeks is a direct result of
glacier melt water running off to the
sea. If you follow the creek ends north-
ward, you will find their depressions in
the dry land as they continue on the
upland.
Besides ice being a factor in glaciers,
we also find ice playing its part in chip-
ping away the solid rock that once made
our entire world. Wherever moisture
can get in and freezing can take place,
we'll have this chipping away. We all
know the power of ice when it's con-
fined. Years ago when milk was deliv-
ered to our homes, we often saw the
milk rise out of the bottle when it was
left on the porch to freeze. My cows'
water pails, if left out to freeze, will
burst their bottoms. So it is if moisture
finds its way into the slightest niche or
rock. Sometimes these cracks can split
huge boulders. We've all seen them
along the Sound. It was the freezing
that did it. All this process of picking
away at the solid mass eventually made
our sand and soils. Without ice and tem-
perature changes, we'd not have the
world we have today. Each day the pro-
cess still goes on, supported by the
grinding sea, the howling winds, the
roots of plants and the many other fac-
tors that make our world what it is.
With the recent cold snap we had, the
ice boats of Orient almost came into
play. Here is about the only place you
will find ice boating on the East End.
It's nice to see Orient's heirlooms
coming out from the old barns and cel-
lars. They have a majesty all their own
and seeing them scoot along the frozen
bay, with their bundled up crew, brings
to mind a Currier & Ives scene of yes-
teryear.
Although we've seen a January thaw,
don't count on spring being just around
the corner. The end of January and all
of February still have much to offer the
ice enthusiasts. Perhaps we'll still get
skating and ice boating here on the East
End.
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Page 13A
Photo by Paul Stoutenburgh
WINTER'S ICE - -If you own ice skates or an ice boat, you probably
can't wait for a good freeze. But if you have work outside or on the
bay, ice can really slow you down.
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