Rootless cones on Mars indicating the presence of shallow equatorial ground ice in recent times

By P. Lanagan, A. S. McEwen, L. Keszthelyi, T. Thordarson. 2001

154 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/f6fd139f77813cc609f8140d6fb83dacc7fcd29c

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. D. Kring
2. Hirise Team
3. Nicolas Gonzalez Thomas
4. A. S. McEwen
5. Oleg Abramov
6. Alberto G. Fairén
7. S. Byrne
8. E. Kite

In Atmospheric Science

1. D. Kring
2. Hirise Team
3. Nicolas Gonzalez Thomas
4. A. S. McEwen
5. Alberto G. Fairén

Citations in the corpus

• Impact‐induced hydrothermal activity on early Mars (2005, background): “, 1992; Barlow and Perez, 2003] and rootless cones [Lanagan et al., 2001] at lower latitudes.”
• Exploration of hydrothermal targets on Mars (2007, background): “, 1995), and phreatomagmatic explosions due to the emplacement of lava flow materials over a volatile-rich substrate to form rootless cones, among other possibilities (e.g., crater statistics of some of these lava surfaces in this region exhibit model ages of less than 10 Ma; Lanagan et al., 2001).”
• Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE) (2007, background): “[98] The other hydrovolcanic landform that has been claimed to exist on Mars are rootless cones [e.g., Allen, 1979; Greeley and Fagents, 2001; Lanagan et al., 2001].”