I just learned by Eric Martindale’s comment to my Borg’s Woods post in February that the March 13 storm knocked down many of the trees in the old growth urban forest that was our neighborhood playground when I was a kid. For more here’s a post in the NJUrbanForest blog, and here are some pictures as well.
Storms are as much a part of nature as old growth forests, even when the former reduces the latter. Sad to read, however, that mosquito abatement has involved the draining of the woods’ pond, where generations of kids learned to skate in a beautiful setting.
For perspective perhaps it is helpful to note that the boggy parts of Borg’s Woods are among the few vernal remnants of glacial Lake Hackensack, which pooled over most of the Hackensack River watershed when the last ice age began to end around 15,000 years ago. The lake lasted several millennia, then drained around 11,500 years ago, when the terminal moraine near Perth Amboy broke. Back then the sea was still far outside the current borders of New York and New Jersey. Only when the rest of the ice cap melted did the oceans reach their current level — which, as we know, is still rising.
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