Hello! I’m a geomorphologist and geochemist interested in how we can use rare nuclides produced in situ within near-surface rock and sediment by cosmic ray bombardment, known as in situ cosmogenic nuclides. My main focus has been working to advance applications of radiocarbon (14C) produced in this manner (in situ 14C). In situ 14C is unique among the commonly measured cosmogenic nuclides in that its 5.7 ky half-life renders it dominantly sensitive to 1) post-30 ka exposure histories and 2) rapid surficial process rates, enabling unique perspectives in late Pleistocene and Holocene paleoclimatic and geomorphic studies often not available using long-lived cosmogenic nuclides. My recent work has focused largely on in situ 14C applications to glacial environments, but I have also started expanding into using in situ 14C to study disequilibrium landscape evolution processes over the last ca. 20 ka.