Recent (Late Amazonian) enhanced backweathering rates on Mars: Paracratering evidence from gully alcoves

Tjalling De Haas, Susan J. Conway, Michael Krautblatter

Research output: Contribution to journalArticlepeer-review

28 Scopus citations

Abstract

Mars is believed to have been exposed to low planet-wide weathering and denudation since the Noachian. However, the widespread occurrence of alcoves at the rim of pristine impact craters suggests locally enhanced recent backweathering rates. Here we derive Late Amazonian backweathering rates from the alcoves of 10 young equatorial and midlatitude craters. The enhanced Late Amazonian Martian backweathering rates (10-4-10-1 mm yr-1) are approximately 1 order of magnitude higher than previously reported erosion rates and are similar to terrestrial rates inferred from Meteor crater and various Arctic and Alpine rock faces. Alcoves on initially highly fractured and oversteepened crater rims following impact show enhanced backweathering rates that decline over at least 101-102 Myr as the crater wall stabilizes. This "paracratering" backweathering decline with time is analogous to the paraglacial effect observed in rock slopes after deglaciation, but the relaxation timescale of 101-102 Myr compared to 10 kyr of the Milankovitch-controlled interglacial duration questions whether a paraglacial steady state is reached on Earth. The backweathering rates on the gullied pole-facing alcoves of the studied midlatitude craters are much higher (∼2-60 times) than those on slopes with other azimuths and those in equatorial craters. The enhanced backweathering rates on gullied crater slopes may result from liquid water acting as a catalyst for backweathering. The decrease in backweathering rates over time might explain the similar size of gullies in young (<1 Ma) and much older craters, as alcove growth and sediment supply decrease to low-background rates over time.

Original languageEnglish
Pages (from-to)2169-2189
Number of pages21
JournalJournal of Geophysical Research: Planets
Volume120
Issue number12
DOIs
StatePublished - Dec 2015

Keywords

  • Late Amazonian
  • Mars
  • alcoves
  • erosion
  • gullies
  • weathering

Fingerprint

Dive into the research topics of 'Recent (Late Amazonian) enhanced backweathering rates on Mars: Paracratering evidence from gully alcoves'. Together they form a unique fingerprint.

Cite this