Time Crawls On

There’s a crevice at the top of a ridge, about 18.5 miles from my house as the crow flies. And as time flies, it’s been in my life for 36 or 37 years.

The crevice is locally known as The Snow Hole because it retains snow late into the year. Decades ago it had snow through August and sometimes beyond. Unfortunately the time for that is long past due the overall temperatures increasing a day or two.

I first visited this in the Spring of ’84 or ’85. I honestly can’t recall which year. As part of the Outdoor Education club or “OE” as we called it in high school, we did an overnight trip. The instructor liked to challenge us and in this particular case we literally arrived at a random parking lot at the base of a ridge and were purposely given a vague map and told to find a particular peak to camp on. With some bushwhacking we made it to the top of the ridge, struck south and arrived at the peak with a gorgeous view. We camped there and then the next day headed north, crossed a road, and eventually arrived at a crack in the ground full of snow. We explored the crack and I’m sure threw a few snowballs at each other. The crack has sheer walls on three sides and a walkable slope on the west side. At the very top of that slope there is a hole in the ground. Alas, no hobbit lived in it, but it was large enough to wiggle into and with some effort find oneself completely underground. It wasn’t much of a cave, but it was there. (Arguably, by some definitions, because one never got beyond what’s known as the twilight zone, it’s not really a cave, but to us, it was a cave.)

We hiked back to the road and in the parking lot there, not the one we started at, we packed up the vehicles and headed home. At the time, I honestly had no clue where we had gone. But I knew it was fun.

It was a couple of years later, I was now in college, when I joined the Rensselaer Outing Club on a day hike to Berlin Mountain. We drove east from campus and arrived at a parking lot. We unloaded and hiked south. I was having a mild sense of deja vu, but I wasn’t sure why. Several miles later, we arrived at the top of Berlin Mountain and I instantly recognized the view. I had camped there. To our east was Mount Greylock, the highest point in Massachusetts. I had returned.

On a later hike, we headed north to the Snowhole. This was the first of many return trips to both locations, the most recent being a hike this past weekend to the Snowhole with my wife.

As we headed north, I was trying to remember my last time there and I want to say close to a decade ago. As I move on in my years and I revisit locations from the past, I try to recall what they were like years ago. In some cases my memories are clouded and faded, in others though, I know my memories are accurate but the places have changed. Both were true on the hike in. In this case, there are two rather open spots about 2/3rds of the way in where one has gorgeous views. Or, more accurately had. The areas themselves are open, but the trees just downhill have continued to grow over the decades and now block much of the view.

View north of Berlin Mountain in the distance, but numerous trees in the foreground blocking much of the view. Taken from the Taconic Crest Trail on the way to the Snowhole.
Decades ago, you could see far more!

And as I mentioned above, the snow doesn’t persist as long in the Snowhole as it used it. But the Snowhole itself hasn’t changed much. Oh, I’m sure a rock or two has fallen since then, more leaves have filled the bottom and decade and I think there’s a bit of a subsistence at the bottom that’s opened up a bit, but overall it’s the same.

And one thing waiting there was that cave. For whatever reason I had not reentered that cave since my first time. This time I decided to do so. I’ve talked about in the past how sometimes we remember caves being bigger than they actually are. Well, in this case I swear the entrance was larger than I remember. I do think in fact the rock had shifted a bit, so perhaps it had been smaller in the past, but in any event, in this case I was able to crawl in without much effort. And the cave itself was deeper and far larger than I recall. Unlike most caves in New York, this is not a solutional cave formed by the breakdown of limestone. Instead, it’s really more of a breakdown cave, where as other stuff erodes away or shifts the layers of rock shift, break, or otherwise move. In my memory, the cave was about 6′ long and just enough to turn around in and peep out a much smaller window near the entrance. Now, it was probably a good 12′-15′ feet long and it dropped down about 6′. Technically I could probably have crawled over a ledge and down just enough to get out of the twilight zone. It truly is a cave, at least now. And it’s one of those rare cases where it’s far larger than I remember. I don’t know in this case if it’s just my memory, or if the cave had changed. It didn’t matter.

After a few minutes I crawled back out and started to do the math. That’s when I realized it had been nearly 40 years since I had last crawled in there. I do hope it’s not another 40 before I crawl in again.

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