While we are at this stage of dredging, and rubber bands on the money. if we dismiss the dredge theory. how is it fragments were found in the dredge material according to Palmer's layer's? they say it was above the dredge material, but the chart shows fragments in the dredge material.
If the money was believed to have been placed there, or got there through natural means. how did pieces get several feet below the area it was found in?
How did up to 3' of new material arrive on the beach after 1974?
These are problems that cause me to continue to search for answers to this part of the problem. is the fragments found at 3' verified?
How did up to 3' of new material arrive on the beach after 1974?Nobody has worked up a historical record of the geology of Tina Bar, so far as I know. You are asking for data that does not exist for Tina Bar. The events of deposition and erosion or movement of sands, was not covered in the Palmer report (or even mentioned). Did Tom work up a record? We all know the natural forces that build and change Tina Bar - Tom added another force: large wakes by passing ships. But beyond Palmer's strata he found and the 1974 Dredging report, there is no historical record for the geology of Tina Bar, that I know of.
I mentioned on DZ years ago that we needed some elevation profiles for the area encompassing Tina Bar. Sluggo took this seriously because of his interest in geology-paleontology and he produced a number of elevation profiles. I will attach one. At the top of Sluggo's profile I have inserted Palmer's trench. His trench is tiny by comparison to the whole of Tina Bar, but, 'all of the data we have about formation strata at Tina Bar' comes from this (almost microscopic!) trench Palmer dug. In contrast to that, see Tom's photo on his website which gives a broader view of strata in the vicinity of the Ingram find. Tom's photo presents a much broader view when compared to Palmer's singular trench!
Can Tom's wider perspective and Palmer's smaller perspective be reconciled? Of course Palmer's view is from 1980 ... Tom's view is much later, 2008? But I see some similarity. One similarity may be in Palmer's Layer 'B', a layer of cross bedded sand. Cross bedded sand layers are pretty easy to identify because of their recognizable morphology. Palmer's cross bedded Layer 'B' is clearly visible in several of Palmer's trench photos, and in one photo Palmer is pointing to the line between Layer 'B' and his Layer 'C', the clay lump layer below. In Tom's photo from 2008 there is a large deep layer of cross bedded sand clearly visible. Is the cross bedded layer in Tom's photo the same cross bedded layer Palmer found in 1980? I don't know, but some part of these cross bedded layers could be the same! The lower part of Tom's cross bedded layer may be the cross bedded layer Palmer found in 1980? I sure would like to know what Tom thinks about this?
If, and it's a big "if", the lower part of the cross bedded formation in Tom's photo is the same cross bedded layer Palmer found in 1980, then of course the Ingram money came from a layer just above that which at the time in 1980 would have been Palmer's "upper active layer" Layer A. I really would like to know what Tom thinks about this
The goal is to know when and how the Ingram money came to be on Tina Bar. Identifying the strata the money was in or next to helps answer that question, but we have to resolve the issue of the strata which has emerged (Kaye vs. Palmer). And since there was no core samples or chemistry for anything at Tina Bar ... we are lacking guidance.
Maybe someone at the USGS or at Portland State could offer assistance in resolving these issues over strata at Tina Bar?
[edit] Look at Sluggo's profile for Tina Bar stretching back to River Road (501). What we have always needed is chart of the strata formations which comprise Tina Bar ... at various dates. That was something Sluggo and I discussed and wished we could have!