Sequestered glacial ice contribution to the global Martian water budget: Geometric constraints on the volume of remnant, midlatitude debris-covered glaciersJ. S. Levy, J. L. Watters, C. I. Fassett et al.|Journal of Geophysical Research Planets|2014Cited by 123
Distribution and Characteristics of Boulder Halos at High Latitudes on Mars: Ground Ice and Surface Processes Drive Surface ReworkingJ. S. Levy, M. D. Dyar, C. I. Fassett et al.|Journal of Geophysical Research Planets|2018Cited by 11
Estimating the Volume of Non-Polar Ice on Mars: Geometric Constraints on the Volume of Midlatitude Debris Covered GlaciersJ. S. Levy, J. W. Head, C. I. Fassett et al.|Lunar and Planetary Science Conference|2014Cited by 1