In 1981, James F. Cherry embarked on what evolved into a passionate, personal quest to identify and document all the known headpots of Mississippian Indian culture from northeast Arkansas and the bootheel region of southeast Missouri. Produced by two groups the Spanish called the Casqui and Pacaha and dating circa AD 1400–1700, headpots occur, with few exceptions, only in a small region of Arkansas and Missouri. Relatively little is known about these headpots: did they portray kinsmen or enemies, the living or the dead or were they used in ceremonies, in everyday life, or exclusively for the sepulcher? Cherry’s decades of research have culminated in the lavishly illustrated The Headpots of Northeast Arkansas and Southern Pemiscot County, Missouri, a fascinating, comprehensive catalog of 138 identified classical style headpots and an invaluable resource for understanding the meaning of these remarkable ceramic vessels.

Pinson Mounds: Middle Woodland Ceremonialism in the Midsouth is a comprehensive overview and reinterpretation of the largest Middle Woodland mound complex in the Southeast. Located in west Tennessee about ten miles south of Jackson, the Pinson Mounds complex includes at least thirteen mounds, a geometric earthen embankment, and contemporary short-term occupation areas within an area of about four hundred acres. A unique feature of Pinson Mounds is the presence of five large, rectangular platform mounds from eight to seventy-two feet in height. Around A.D. 100, Pinson Mounds was a pilgrimage center that drew visitors from well beyond the local population and accommodated many distinct cultural groups and people of varied social stations. Stylistically nonlocal ceramics have been found in virtually every excavated locality, all together representing a large portion of the Southeast. Along with an overview of this important and unique mound complex, Pinson Mounds also provides a reassessment of roughly contemporary centers in the greater Midsouth and Lower Mississippi Valley and challenges past interpretations of the Hopewell phenomenon in the region.