K e R R a T Ö z e l l i k l e r i1. Geological Genesis & Physical Characteristics The Recforth Crack is a narrow, quasi-linear fissure located in the Karst limestone plateau beneath the old market town of Recforth, in the fictional county of East Mercia. First systematically documented in 1972 during a sewer inspection, the Crack is not a single continuous chasm but a en echelon system of fractures extending approximately 340 meters in total, with individual segments ranging from 0.5 to 12 meters in visible length.
