Gracchus
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- Dec 21, 2002
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It is true that my formal education in geology is somewhat deficient, consisting of two semesters in high school and two in college, but I did take field courses, with associated laboratory and cartographic work, have read a number of books since, and I can generally differentiate between aeolian, lacustrian, riparian, and marine sediments.I appreciate your answer very much, consider that you are not trained in geology.
The deposits are not "laminated" in the sense that they are cemented together. Because they are unweathered they do have a high angle of repose. Individual grains are angular and don't roll or even slide.But, exactly because the nature of pyroclastic flow as you described, we should not expect a fine laminated deposition like what we found on the ash/sand/pebble deposition.
And that is exactly what we observe. When wind (or water) flows over unsorted deposits, it carries away the finer sediment to be deposited down wind or down stream to present finer grained deposits over coarser grained ones that were left behind in the flow, producing ordered layering from unsorted sediments. Thus, the pyroclastic cloud deposits unsorted sediments vertically, with heavier grains falling out first, which are then further sorted by horizontal flow. This process can be observed and has been observed. And that is exactly what we see in the pyroclastic deposits around, for instance, Mt. St. Helens, but also in many other places.When later forceful flows ran over the earlier deposits, we should even expect frequent erosion and gouging of the loose sediments deposited slightly earlier.

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