What can lithostratigraphic sequences help interpret?

Lithostratigraphic sequences are essentially layers of rock that are categorized based on their physical and mineralogical characteristics. These sequences help geologists interpret the geologic history of an area by providing insights into the processes that formed the different layers over time. By studying the arrangement, composition, and age of these rock layers, geologists can reconstruct past environments, including changes in sea level, sedimentation rates, and tectonic activities. This historical perspective allows for a better understanding of the geological events that have shaped the landscape.

While mineral composition, soil fertility, and groundwater levels are important aspects of geology, they do not directly relate to the primary purpose of lithostratigraphy. Lithostratigraphic sequences focus on the interpretation of rock layers and their histories, making the understanding of geologic history the most relevant interpretation derived from this method.