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Old 07-20-2015, 08:01 PM   #1
Boardwalk Bluesboy
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Quote:
Originally Posted by ApS View Post
This site seems to be very comprehensive, disclosing that the Lake Winnipesaukee water level had been raised from 5 to 12 feet. (Which is consistent with what I'd heard from my Dad, and some other longtime residents).

http://www.weirsbeach.com/topten/reason9frame.html

At the original (low) level, the range of boats on the lake would have to have been very small. Rocks Ahead!

BTW: Is this a legal matter?



.
Here's an updated link to the WeirsBeach.com page referenced above. Scroll all the way down to see a map of the lake showing the original shoreline "...before THE INVADING COLONISTS DAMMED THE FALLS".
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Old 07-21-2015, 10:03 AM   #2
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If you want to PM me your email address I will scan and email you copies of testimony I have from proceedings in the late 40's early 50's on this issue. They indicate that while Paugus Bay might have been raised the Lake itself was not raised by damming. The channel was dredged to allow the old mill companies to draw the lake down further than it naturally could have been. More drawdown capacity meant more hydropower for the mills. As the mills became less of an economic power and tourism became more of one the deep drawdowns became an issue and in the 40's the legislature stepped in and passed a law limiting the level to which the mill could lower the lake during the summer.
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Old 07-21-2015, 10:19 AM   #3
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Default Makes sense

That makes much more sense, Shore Things. The claim of 5-12' lower in the earlier article definitely conflicts with the description and existence of a natural waterfall at the Weirs and the later need for dredging of the channel.
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Old 07-23-2015, 06:24 AM   #4
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Question Amiright?

Quote:
Originally Posted by Boardwalk Bluesboy View Post
Here's an updated link to the WeirsBeach.com page referenced above. Scroll all the way down to see a map of the lake showing the original shoreline "...before THE INVADING COLONISTS DAMMED THE FALLS".
Another thread here on the subject:

Raised, apparently, two hundred-plus years ago.

That might explain the present day shoreline's slow, but continuous "rain" of falling trees from relatively steeper shores.

Two hundred years of rocks and boulders being moved against the shoreline by centuries of thick ice—a relatively short time of geological history.

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