Sevy, Jonathon; Radebaugh, Jani; McDougall, Dylan; Kerber, Laura; Rabinovitch, Jason (Brigham Young University)
Faculty Advisor: Radebaugh, Jani (Brigham Young University, Geology)
Yardangs are wind-carved linear ridges that are found selectively on Earth and extensively on Mars. The history of the morphologic development of yardangs is not well known. In the Puna high plateau of Argentina there are ignimbrite deposits, many of which have been eroded into yardang fields, commonly called fleets. Yarding fleets are evenly spaced forms, facing into the wind, that resemble a fleet of boats sailing. A prominent fleet, known as Campo de las Piedras Pomez (CCP) was studied to more fully understand their formation and morphology, including field research in December 2018 and 2019. Some physical characteristics looked at in the field included: dedos direction and lengths; heights and lengths of yardangs; structural features; wind and gravel ripple direction. In addition, relationships between yardang organization and structural control have been analyzed. The dedos on the fronts of yardangs averaged 4.0cm in length, while the reverse dedos were 3.3cm. From this it was determined that: Two wind directions, with one dominant, are present; Structural features can shape morphology of yardangs.