Understanding the natural processes that have taphonomic effects on bone is an important part of accurately determining the postmortem interval (PMI). Ultraviolet radiation is one of these various natural processes that weather bone. The present study quantifies the degree to which differential exposure to sunlight affects bone bleaching and weathering. In this study, 140 Sus scrofa long bones were placed in two different microenvironments (grassland and woodland) within a New England setting. Upon the completion of a one-year observation period, 100% of the bones had reached bleaching level 4, and 9.85% (n = 13) of the bones had reached weathering stage 1, with the majority (n = 11) being from the woodland sample. The results indicated that the microhabitat that each sub-sample was deposited within played a statistically significant role in the degree and rate of bleaching and weathering on the bone, with chi-square tests all indicating a p value of < 0.001. In addition, results indicated that environmental variables that led to the more rapid decomposition of soft tissue, such as temperature, humidity, and the type of plant coverage, may play a greater role in the level of bleaching and weathering achieved by the bones, rather than simply the degree of exposure to UV radiation and light intensity.