Major Ridge Path Configuration
Major ridge path formations are sometimes referred to as 1) Ridge endings (ridges that end abruptly) 2) Bifurcations (ridges that appear to split apart and continue on as two ridges) 3) Enclosures (ridges that appear to split in two and then rejoin) 4) Short ridges (consist of at least two ridge units) and 5) Ridge dots (only one ridge unit). Others have been known to disagree with this and have stated that only two major ridge path formations actually extist - ridge 'endings' and 'bifurcations'. Everything else is just a derivative of these.
As David Ashbaugh explains in his book entitled "Quantitative-Qualitative Friction Ridge Analysis"..."A major ridge path deviation does not develop in isolation. Other ridge formations must develop around it and in concert with it. Therefore all major ridge path deviations display interaction with surrounding ridges." (An extremely important point for the Friction Ridge Identification Specialist to remember when analyzing friction ridge prints.) |