Depth, features, etc all play into this and there is no answer that applies across the board. In most cases the current speed is one of the larger factors so the comment about that (I forget who made it) is probably right on target. More food for thought: I am not sure how constricted of an area you are talking about, so the following may or may not be relevent. In whitewater paddling we look at flow and gradient. Basically the more flow the less gradient you can handle and vice versa. In extremely low volume conditions (< 100cfs) a skilled creeker might be able to paddle a 600 ft per mile or greater gradient. In a high volume situation it would be possible for a 30 ft per mile run to be unrunnable. Of course all this is an over simplification, since there are many other factors. Another thing that happens is that a rapid may wash out at a given level and then reappear with a vengance at a still higher level. There are places where there is a waterfall flowing one way at one tide state, a waterfall flowing the other way at another, and flat water at yet another. I have never witnessed this first hand but have seen som impressive pictures of such a "reversing falls". Sorry if all of this just muddies the water, but the point is that there is no one correct answer except, "it depends". Pete __________________________________________________ Do you Yahoo!? Yahoo! Mail Plus - Powerful. Affordable. Sign up now. http://mailplus.yahoo.com *************************************************************************** PaddleWise Paddling Mailing List - Any opinions or suggestions expressed here are solely those of the writer(s). You must assume the entire responsibility for reliance upon them. All postings copyright the author. Submissions: PaddleWise_at_PaddleWise.net Subscriptions: PaddleWise-request_at_PaddleWise.net Website: http://www.paddlewise.net/ ***************************************************************************Received on Sat Dec 21 2002 - 08:26:25 PST
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