Thanks for the reply. Obviously the Seattle PI map of
Tena Bar is wrong. I attached a few correct which show the outline of the river from Washougal out beyond Tena Bar. I will assume the area opposite Tena Bar was searched, for some distance up and down stream.
Tena Bar sits on the right hand side of the river and even juts out (in dry periods) into a free flow field following the rather sharp right hand curve in the Columbia, prior to the channel involving Tena Bar.
(Fast deeper water flows to the outside of an arc, Slow more shallow water to the inside of an arc). These
remarks must be interpreted in the context of the Columbia being a wide river; during flood even wider.
But the the principles of flow and deposition are the same.
Debris in this situation would collect on the inside of the curve, then wash into the channel or even to the
opposte side depending on velocity and volume of flow, then be conveyed downstream some conveying to the sides (shorelines), again depending on time of year and velocity and flow.
The problem is "entry point" (above, from sides
proximate to Tena Bar, or further upstream as in the
Washougal hypothesis.) There may also be a fourth
option, as I read the maps, which is the Vancouver Lake area upstream and not too far behind Tena Bar.
If Tena Bar is affected by overflow from Vancouver Lake then that is a possible entry point, also.
I seriously doubt Tena Bar was the original deposit site
unless by accident money was dropped or buried further inland and it washed or eroded to that location,
apparently after dredging operations.
Only two things come to mind which might shed light on this matter.
I notice what appear to be 'worm holes' in the money?
I wonder if these holes penetrated the total stacks of
bills or were just superficial. Different worms leave different (hole) tracks and patterns, which might help
distinguish if money spent its time on land vs in the water.
BTW, the outer areas of the bills show relative
uniform wear in terms of erosion, rolling, and decay.
Notice the curved wear patterns at both ends of each bill. This is consistent with uniform wear from burying
vs one specific side of the bills being subject to directional wear (as bills sitting in stream wash). I tend
to agree with the poster who points to the lack of staining from water - in fact colour in several bills is still very bright. But the wear patterns suggest a uniform state of decay consistent with burying, unless
I am missing something.
Lastly, had it been me, I would have had some of these bills analysed under a microscope simply on the chance some clue in pollen, bacteria, or mineral deposits might turn up. In addition, I would have taken samples of some of these bills (outisde of stack vs inside protected in stack) and run some mass spectroscopy on the samples, just to see what turned up. You never know. Clues like this might shed light on their history.
That's enough for now - and thank you. I wish you all great luck in this quest.
George