Daniel M. Davis

Daniel M. Davis serves as a Research Professor in the Department of Geosciences at Stony Brook University, where he has maintained faculty status since 1986. His academic foundation includes an A.B. from Princeton University (1978), a Ph.D. from MIT (1983), and postdoctoral research at Lamont-Doherty Geological Observatory (1983-86).

His scholarly career centers on two interconnected domains: tectonics and field geophysics. Within tectonics, Davis pioneers analog scale modeling to investigate thin-skinned mountain belts and accretionary wedges, examining how stratigraphic thickness, basement structures, and pore fluid pressures govern deformation. His Pakistan-focused research on oblique plate convergence reveals critical mechanics of forearc slivers and mountain-building processes. Concurrently, his field geophysics work employs ground-penetrating radar and resistivity surveys to decode Quaternary features on Long Island, including glaciotectonic folds in push moraines, kettle hole sedimentology, and active parabolic dunes—providing terrestrial analogs for ancient tectonic and glacial systems.

Publication analysis shows consistent innovation in experimental methodologies since 2000, with recent work emphasizing quantitative strain measurement in analog models and high-resolution geophysical mapping of surface processes. His research bridges structural geology, geophysics, and Quaternary science through rigorous field-experimental integration.

Professor Davis actively mentors graduate students in research projects, as evidenced by frequent student co-authorship. His laboratory operations feature a specialized analog modeling apparatus for simulating tectonic convergence and portable geophysical systems deployed across Long Island's glacial landscapes to capture real-time deformation signatures.