Abstract Geology has been part of the curriculum at Wheaton College, Illinois, since it was established in 1860 as a non-denominational, Christian liberal arts college. The school continues to maintain a strong identity with evangelical Christian theology and subculture. The first president Jonathan Blanchard recruited George Frederick Barker to teach geology and natural history on the personal recommendations of the renowned geologists Agassiz, Silliman and Hitchcock. Barker taught at Wheaton for only one year, and was followed by a succession of other young scientists who kept geology in the curriculum to the end of the nineteenth century. These teachers respected the geological evidence for an ancient Earth and interpreted the creation days in Genesis 1 as representing extended epochs of God's creative activity. In the early twentieth century, Professors James Bole and L. Allen Higley harmonized mainstream geological history and the Bible through the gap or ruin–restoration interpretation, wherein eons of geological time preceded six days of Edenic re-creation only thousands of years ago. Higley's background in geology, his role in recruiting additional science faculty staff, and his influence among fundamentalists set the stage for the acceptance by subsequent Wheaton geologists of mainstream geology and their rejection of emerging popular fundamentalist ideas about a six day creation and Flood geology. Geology was established as a major subject in 1935 and an independent Geology Department was established in 1958. Geology education at Wheaton College was profoundly influenced by the tension over creation issues in the evangelical subculture, and different models for understanding the relationship between science and Christian theology have been employed by teachers and students.

Abstract The quarry at Hamilton Mound is in the NE¼, Sec.36, T.-20N., R.6E., Coloma NW 7½-minute Quadrangle. It can be reached by turning east from Wisconsin 13 on Archer Drive, just north of Dorro Couche Lake, and proceeding about 4 mi (6 km) to a turnoff leading south into the quarry in the middle of Hamilton Mound.The turnoff from Wisconsin 13 is about 15 mi (24 km) south of Wisconsin Rapids (Fig.1).