Summary Shale rocks are known to be the primary troublesome formation that has plagued drillers for many years. Attempts have been made to investigate the characteristics of shales, but results are limited because of the scarcity of test samples. Rapid deterioration of cuttings and cores has made data collection limited at best and a complete failure in many cases. It now appears that the shales become unsaturated as they dry out because of poor storage conditions, which result in false test results owing to the incorporation of capillary pressure artifacts. This paper discusses results obtained with a specially preserved, highly reactive shale core obtained at a depth of 4,500 ft in the North Sea. A previously developed method was used for the evaluation of shale cores to determine their level of saturation. This study shows that shales must be preserved at their native water content if accurate physical measurements are to be made. Swelling data show that shales that are altered during handling (hydrated or dehydrated) do not respond properly even when restored to their native hydration conditions. They tend to experience excessive swelling compared to cores kept at their native water content. Results also showed that the North Sea core used in this study was maintained in a fully saturated condition during coring, retrieval, and storage. The technique used is discussed here.