- The following is an archived discussion of the DYK nomination of the article below. Please do not modify this page. Subsequent comments should be made on the appropriate discussion page (such as this nomination's talk page, the article's talk page or Wikipedia talk:Did you know), unless there is consensus to re-open the discussion at this page. No further edits should be made to this page.
The result was: promoted by Theleekycauldron (talk) 11:37, 11 February 2022 (UTC)
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Louth (crater)
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A simulated surface-level view of Louth's ice dome using HiRISE data
- ... that the mound at the center of Louth crater is the warmest permanent body of water, in the form of ice, on the Martian surface? Source: "This ice mound, although a common feature in northern plains’ polar craters, represents the most equatorward (70°N) example (i.e., on average, it is the warmest perennial surface ice on the planet)." Bapst, Jonathan; Byrne, Brendan (2016). "LOUTH CRATER WATER ICE AS A MARTIAN CLIMATE PROXY" (PDF). Lunar and Planetary Science Conference. 47. Retrieved 14 November 2021.
- Reviewed: Shaylee Mansfield
- Comment: I was busy with school for the past few days so apologies for the lack of review on the last nomination, I'll get to it ASAP! Thank you in advance to whoever reviews this article!
Converted from a redirect by Ornithoptera (talk). Self-nominated at 01:35, 29 January 2022 (UTC).
Hi Ornithoptera, review follows; article moved to mainspace 24 January; exceeds minimum length and is well written; sources used appear to mainly be articles from reliable scientific journals; I didn't find any overly close paraphrasing from a (smallish) sample of the many sources cited; hook fact is mentioned in the article and checks out to the source cited; image looks good and is freely and appropriately licensed; a QPQ has been carried out. Can't see any issues here - Dumelow (talk) 09:36, 29 January 2022 (UTC)
- Thank you so much for the review Dumelow! Enjoy your day and I hope you enjoyed the article! Ornithoptera (talk) 00:52, 30 January 2022 (UTC)
To T:DYK/P6