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A Canal Through the Pines, Part 2
Submitted by Ben Ruset on Sun, 12/16/2007 - 10:32am.
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I set out yesterday to explore the Southern part of the canal through the pines, running from Mount Misery Brook to Bisphams Mill Creek. The day was heavy and ominous, the beginnings of the first Nor'easter of the Winter of 07-08 could be felt. Wisely, I stopped off and picked up a new pair of gloves and scarf. The best way to explore the Southern part of the canal is to park near the bridge at Lower Mill. Garbage is strewn through the area - it's remoteness lends itself well to being a dumping ground. A pile of computer monitors, old appliances, and vinyl siding litter the area. Recent rains have turned the road to muck, although fortunately the puddles are not deep. I crossed the bridge and headed towards the spot where I wanted to park. The little clearing off to the side of the road had already been claimed by two vehicles - hunters, no doubt - so I decided to turn around and try exploring the Northern part of the canal. Readers of the my last article will remember that the canal rises up from the remains of the trestle over Mount Misery Brook and continues on until it reaches a farm field. There the canal seems to angle along the side of the property, and presumably crosses Junction Road. I backtracked out to Four Mile Road, and drove on into New Lisbon. New Lisbon, once known only as Lisbon, was named by the Portuguese who came to cut lumber in the area. In 1834 Gordon mentions that the town contained a grist mill, saw mill, store, and ten to twelve dwellings. He also notes that a "railroad or Macadamized road, is about to be built from this village to the mouth of Craft's Creek, upon the Delaware, about 15 miles, in order to bring to market a quantity of excellent pine wood, which grows in the vacinity." This railroad would later be known as the Kinkora Railroad, now long abandoned. Interestingly, Gordon does not mention the iron furnace that was here, built around 1800, just thirty-four years before he published his Gazetteer. Boyer mentions that cinders and slag mark the location of the furnace, but sadly today even those are gone. I continued on up Junction Road, making a right turn at the diminutive New Lisbon Post Office. I followed the road up and down several times, becoming frustrated at the traffic backing up behind me as I slowed to take a look at spots that might be the canal. Unfortunately Brendan Byrne State Forest does not extend to this area, so any exploring must be done with the permission of the land owner. A lack of a shoulder to pull the Jeep on and no desire to trespass kept me from exploring this area further.
As the canal moved away from the brook, there's a substantial incline. Imagine the letter V stretched out, so that each top point in the letter was not at such an extreme angle. That's a rough example of the topography of the canal over Mount Misery Brook. The brook is in the low part of the V, and there is an incline on either side. This region of the canal is likely what made Beck conclude that this canal failed because water couldn't flow uphill.
Winding through the woods, it's hard to imagine how this canal worked. Early in my exploring the canal did a rather tight ninety degree bend. In other spots, it runs straight. Still others it curves gently. I couldn't help but compare this to the canal at Harrisville. While that canal is much shorter, it's also much deeper. This canal is - at most - four or five feet deep, but the length of it makes it an engineering marvel. It appears to me that the canal followed the shore of what used to be the lake that was created by damming Bisphams Mill Creek, used to power the sawmill at Lower Mill. The canal has steep banks on either side, and then along one side a drop off into a cedar swamp, which according to old maps was once the lake. It doesn't make sense, however, to dig a canal along the banks of a lake, unless for some reason the builder wanted to take water from before the dam.
The canal dipped down, and the sound of rushing water became more noticible. I emerged from the cedar swamp at Bisphams Mill Creek, flowing pretty rapidly. The sound of the water came from it flowing around several trees that fell into the water. In the 1930's, when Beck visited, he found the lake still in existance, with a waterfall nearby, and an "old footprint or two to betray humanity." Today the canal merely peters out, the cinders of an old campfire on a hill overlooking the stream serve as testament that few people venture here.
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Could you rephrase this?
Gabe, I think he means if you take the letter V and and pry it open you have a wider angle with still a sharp point at the bottom. Not like the letter U. This is certainly proof to me that it was never used. As water flows through a channel it wears the bottom out, but if water never flows the bottom will stay sharp like the letter V.
Guy
Jeff
I agree. The hills on either side of the banks are conspicuously man-made.
nevermind...
Guy