The anatomy of a shear zone: Evidence for constrictional deformation and crustal thickening within the Nevadan-age Condrey Mountain Shear Zone
Katie Gates, Texas Tech University

Accessible and inclusive: An evolution of universally-designed teaching and learning in geoscience field courses
Christopher Atchison, University of Cincinnati-Main Campus

Chronology of Andean Orogenesis from the Sedimentary Archive: Opportunities and Challenges Using Detrital Thermochronology
Julie Fosdick, University of Connecticut

Deducing Deformation from Quartz Crystallographic Preferred Orientation Data
Joshua Davis, Carleton College

Velocity influence on restraining bend evolution
Hanna Elston, University of Massachusetts-Amherst

Can Anisotropic Rocks Influence Stress Directions from Boreholes?
Sarah Titus, Carleton College

Paleostress Analysis of Normal faults and Early Cretaceous Sheet Intrusions in Northern New England: Evidence for a Dynamic Extensional Setting During the Early Cretaceous
Jennifer Cooper Boemmels, Southern Connecticut State University

Ductile and Brittle Fault Rocks in the Upper and Lower Crust, Respectively.
Robert Wintsch, Indiana University-Bloomington

Acadian-age Inverted Metamorphism Below the Embreeville Thrust in the Central Appalachian Piedmont of Pennsylvania
Howell Bosbyshell, West Chester University of Pennsylvania

Off-fault damage at the base of the seismogenic zone and implications for crustal rheology