Author
Listed:
- J. W. Holt
(Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin 78758, Texas, USA)
- K. E. Fishbaugh
(Smithsonian National Air and Space Museum, Washington 20560, District of Columbia, USA)
- S. Byrne
(Lunar and Planetary Laboratory, University of Arizona, Tucson 85721, Arizona, USA)
- S. Christian
(Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin 78758, Texas, USA
Bryn Mawr College, Bryn Mawr 19010, Pennsylvania, USA)
- K. Tanaka
(Astrogeology Science Center, US Geological Survey, Flagstaff 86001, Arizona, USA)
- P. S. Russell
(Planetary Science Institute, Tucson 85719, Arizona, USA)
- K. E. Herkenhoff
(Astrogeology Science Center, US Geological Survey, Flagstaff 86001, Arizona, USA)
- A. Safaeinili
(Jet Propulsion Laboratory, Pasadena 91109, California, USA)
- N. E. Putzig
(Southwest Research Institute, Boulder 80302, Colorado, USA)
- R. J. Phillips
(Southwest Research Institute, Boulder 80302, Colorado, USA)
Abstract
Martian landmarks on the radar The northern polar cap of Mars, containing enough water to cover the entire planet to a depth of several metres, features two major landforms that stand above all others. These are the enormous canyon, Chasma Boreale, and a series of spiral troughs. The processes leading to their formation have remained unclear. Now two papers in this issue present detailed histories of both systems. John Holt and colleagues use penetrating radar imagery from Mars Reconnaissance Orbiter's radar sounder to show that depositional processes — rather than a catastrophic event — formed the Chasma Boreale. Isaac Smith and John Holt use Mars Reconnaissance Orbiter data to rule out erosional cutting of polar ice as the cause of the central troughs, and instead conclude that they too are largely depositional, having migrated polewards and upwards in elevation in the past two million years.
Suggested Citation
J. W. Holt & K. E. Fishbaugh & S. Byrne & S. Christian & K. Tanaka & P. S. Russell & K. E. Herkenhoff & A. Safaeinili & N. E. Putzig & R. J. Phillips, 2010.
"The construction of Chasma Boreale on Mars,"
Nature, Nature, vol. 465(7297), pages 446-449, May.
Handle:
RePEc:nat:nature:v:465:y:2010:i:7297:d:10.1038_nature09050
DOI: 10.1038/nature09050
Download full text from publisher
As the access to this document is restricted, you may want to search for a different version of it.
Corrections
All material on this site has been provided by the respective publishers and authors. You can help correct errors and omissions. When requesting a correction, please mention this item's handle: RePEc:nat:nature:v:465:y:2010:i:7297:d:10.1038_nature09050. See general information about how to correct material in RePEc.
If you have authored this item and are not yet registered with RePEc, we encourage you to do it here. This allows to link your profile to this item. It also allows you to accept potential citations to this item that we are uncertain about.
We have no bibliographic references for this item. You can help adding them by using this form .
If you know of missing items citing this one, you can help us creating those links by adding the relevant references in the same way as above, for each refering item. If you are a registered author of this item, you may also want to check the "citations" tab in your RePEc Author Service profile, as there may be some citations waiting for confirmation.
For technical questions regarding this item, or to correct its authors, title, abstract, bibliographic or download information, contact: Sonal Shukla or Springer Nature Abstracting and Indexing (email available below). General contact details of provider: http://www.nature.com .
Please note that corrections may take a couple of weeks to filter through
the various RePEc services.