“…They sometimes depend on the purpose of the study [14] or are neutral, and combine the widest range of the abiotic components [15]. Two widely used methods of geodiversity assessment [4,16]-which have also been modified for geodiversity evaluation on micro- [17], mid-and large-scale [18] study areas [17,19] or evaluation purposes [12,20,21]-are the one developed by Pereira et al [22], which equals the G value to the sum of geological, geomorphological, paleontological, pedological and mineral occurrence sub-indices, and the second one by Serrano and Ruiz-Flaño [3], which divides the multiplication of all geodiversity elements in an area and the terrain ruggedness index (R) of that area with the value of the natural logarithm of the area. The second method, which is to be discussed in greater detail in this article, has been extensively used and applied at various levels-ranging from local [23] to landscape [10] ones-and geographic environments, for example karst [17,24,25] and even the seabed [19], among others.…”