E-mail a Wiley Online Library Link

David K. Weiss and James W. Head Formation of double-layered ejecta craters on Mars: A glacial substrate model Geophysical Research Letters 40

Article first published online: 7 AUG 2013 | DOI: 10.1002/grl.50778

Key Points

  • Features of double-layered ejecta craters point to impact into an ice sheet.
  • Inner ejecta facies is formed in a landslide mode of the outer rim ejecta.
  • Landslide is controlled by structural uplift angle and ice sheet lubrication.

Complete the form below and we will send an e-mail message containing a link to the selected article on your behalf

Required = Required Field