Gray instead of white.
I rode up to Mount Hope Pond with a bucket of shiners and fatheads, hoping for nice trout, pickerel, and bass. With 280 trout stocked into 18 surface acres of water, it's a possibility. Of course I knew I might find the ice unsafe, but I really expected it wouldn't be just yet. Again, I pulled into the large parking lot as I did once earlier in the ice season, and within seconds the pond came into view. It didn't look good. That gray off-color, rather than white, signaled to me that I probably wasn't staying here long. I quickly decided to first approach the pond with just my splitting bar. That no one else fished it, and Fridays might draw more anglers than other weekdays do, was also a definite sign that things weren't good.
Of course, I had to check it out. And I stepped out on the ice a couple of feet from the beach, my feet getting moist because my waterproof boots aren't living up to that description, and I need to try to repair or replace them. Then I reached forward and whacked my way through the ice with two thrusts of my splitting bar. I did this repeatedly out of curiosity, but there was no hope. Three inches on top was slush, and maybe three or four inches underneath rotted out.
I'm getting older and forgetful, it's true. How many times I've walked a plank to get onto a lake over the melt at the edge late in the ice season, I don't recall, but if I had had a plank, I might have walked it, and then tested the ice, say, eight feet from the edge of the beach. Then, I might have found hope existed yet. But while I was at Mount Hope, it didn't occur to me to think of the possibility.
It's interesting to me how, quite apparently, the ice melts from underneath. I noticed what clearly seemed to be the phenomenon at Lake Aeroflex two days ago, when, by all we could judge, the ice had melted about four inches from underneath, having been a foot thick Thursday the week before. I only hedge from certain judgment because I want some peer review to back up what I've seen. Here, too. With three inches of slush and four inches of striated rot underneath, that's a total of seven inches. Oliver Round was up here a week ago when it was 15 inches thick.
That rot is a curiosity. I always refer to the striations, but most people speak of honeycombing. I recall once being out on Lake Hopatcong with my son when things began to get sketchy. This was almost two decades ago. The surface was soft, there was about four inches of striated ice, and three or four inches of hard ice underneath that rot, so I considered the ice safe and we fished. But if it melts from underneath, as it clearly seems to, why wasn't it striated all the way through? And besides, how do warmer temps permeate cold, hard ice to rot it down towards that surface underneath?
I've paid attention to many ice conditions over the decades, but I've never noticed until two days ago that ice seems to thin out from underneath. I've seen plenty of that striated rot--which proves much of the whole mass is affected by the melt--but I've never had the opportunity to measure such differences as a foot and eight inches, 15 inches and about seven inches, as these recent outings have afforded me.
My splitting bar head was welded onto the iron shaft, a cut having accommodated that chisel head.










