While examining how the orientation of particles and droplets in the air subject to static electric fields during atmospheric transport affect sedimentation processes, an important point that has been overlooked throughout the history of electricity was realized. The type of lightning and its refraction angle with respect to the pathway of the electrical discharges seen in the air column, which is pushed by a buffer area of atmospheric fronts, or in the lower stable air flows moving from upper unstable air layers are the same in a given geographical region. The similarity seen in the refraction angles within the whole column of a lightning strike during grounding is quite impressive, as is the similarity in the shape of different lightning strikes at different times in history. When historical lightning photographs taken in the same geological region are examined, we can see that this shape has not changed in 100 years. The shape of lightning strikes seen at different times in the same region and relevant visual evidence have been collected.
The characteristic atmospheric features that create stable erosion and transportation properties are more important than geological stratigraphy and have a greater effect on our findings. The geological lithography of these areas is the second most impactful feature. The different types of suspended material involved in float laminarization processing during transportation is the reason a separated laminar column flow occurs under the same atmospheric conditions. The physical multi-layered separation these materials experience is the result of their varying physical properties, such as their static electric field, humidity, or internal relative displacements. Multi-laminar volumetric leakages of the same air density by the same type of suspended material occur at different heights in the main air column, with an increased number of layers occurring due to static electricity. The pathway of a lightning strike always hasthe same refraction shape, making this a regional marker of constant atmospheric conditions in a stable climate.
