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No description available.

The Smithfield 7.5' quadrangle is located about 13.8 kilometers (8.6 miles) south of the Utah-Idaho State Line and occupies the central portion of the eastern side of Cache Valley, Utah. The mapped area contains more than 55 square miles. The Bear River Range on the eastern side of the quadrangle contains stratigraphic units ranging from Precambrian to Quaternary age. Cache Valley contains deposits of Tertiary and Quaternary age. Quaternary units in the Smithfield quadrangle are subdivided into thirty-two map units based on age and genesis. Five ages of Quaternary units are identified, and these units are assigned to one of fourteen genetic types. The East Cache fault zone is mapped along the western edge of the Bear River Range. Early Quaternary time was principally a period of pediment formation, followed by normal faulting, erosion, and alluvial-fan deposition. Cache Valley was later occupied by a pre-Bonneville cycle lake which is tentatively correlated with the Little Valley lake cycle. This lacustrine cycle was followed by more erosion and alluvial-fan deposition. The current Cache Valley landscape is dominated by the sediments and geomorphic features of Pleistocene Lake Bonneville. Alluvial-fan deposition has been the principal geologic process in post-Lake Bonneville time. Geologic hazards in the Smithfield quadrangle include flooding, landslides, debris flows, rock fall, problem soils, shallow ground water, earthquake ground shaking, surface fault rupture, and liquefaction. Some of the areas affected by these hazards and measures for mitigating the hazards are identified. Bonneville lake cycle fine-grained offshore deposits and the Tertiary Salt Lake Formation are the primary geologic units susceptible to landsliding.

Difficult human childbirth is often explained to be the outcome of long term evolutionary hanges in the genus Homo resulting in an‘obstetrical dilemma,’defined as the compromise between the need for a large pelvis in birthing large brained babies and a narrow pelvis for the mechanics of bipedal locomotion (Washburn, 1960). The ‘obstetrical dilemma’ is argued to result in the risk of cephalopelvic disproportion and injury (Washburn, 1960). Current research challenges the premise of the obstetrical dilemma by considering the effects ecological factors have on the growth of the bony human pelvis (Wells et al., 2012; Wells, 2015, Stone, 2016; Wells, 2017). This thesis tests Wells et al.’s (2012) assertion that environmental factors, such as agricultural diets, compromise pelvic size and morphology and potentially affect human childbirth. The skeletal samples examined in this study are from medieval English populations with long established agricultural diets. Bony pelvic metrics analyzed are from the St. Mary Spital assemblage, and demographic and pathological data from St. Mary Spital were compared to the East Smithfield Black Death cemetery assemblage. The results show that there is some evidence for a relationship between chronic stress and compromised pelvic shape and size in both men and women, however the evidence is not conclusive that younger women with compromised pelvic dimensions were at an increased risk of obstructed labour and maternal mortality during childbirth. This suggests that childbirth was not likely a significantly elevated cause of death among younger women in medieval London as a result of cephalopelvic disproportion. The concept of a single obstetrical dilemma is flawed, as multiple obstetrical dilemmas other than cephalopelvic disproportion through pelvic capacity constrains are present, including ecological and nutritional stressors, childbirth practices and technologies, sanitation ractices, and social and gender inequality / Graduate