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The Quadrangles Av-11 and Av-12 on Vesta are located at the northern rim of the giant Rheasilvia south polar impact basin. The primary geologic units in Av-11 and Av-12 include…

The Quadrangles Av-11 and Av-12 on Vesta are located at the northern rim of the giant Rheasilvia south polar impact basin. The primary geologic units in Av-11 and Av-12 include material from the Rheasilvia impact basin formation, smooth material and different types of impact crater structures (such as bimodal craters, dark and bright crater ray material and dark ejecta material). Av-11 and Av-12 exhibit almost the full range of mass wasting features observed on Vesta, such as slump blocks, spur-and-gully morphologies and landslides within craters.

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    • 2014-12-01
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    • NOTICE: this is the author's version of a work that was accepted for publication in ICARUS. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in ICARUS, 244, 120-132. DOI: 10.1016/j.icarus.2014.03.013

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    Krohn, K., Jaumann, R., Otto, K., Hoogenboom, T., Wagner, R., Buczkowski, D. L., Garry, B., Williams, D. A., Yingst, R. A., Scully, J., De Sanctis, M. C., Kneissl, T., Schmedemann, N., Kersten, E., Stephan, K., Matz, K-D., Pieters, C. M., Preusker, F., Roatsch, T., Schenk, P., Russell, C. T., & Raymond, C. A. (2014). Mass movement on Vesta at steep scarps and crater rims. ICARUS, 244, 120-132. http://dx.doi.org/10.1016/j.icarus.2014.03.013

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