- Article metrics
- Last updated: Sun, 12 Apr 2026 9:29:26 Z
Experimental evidence for lava-like mud flows under Martian surface conditions
Access & Citations
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- 3587
- Article Accesses
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- 49
- Citations
Citation counts are provided by Dimensions and depend on their data availability. Counts will update daily, once available.
Online attention
- 60 tweeters
- 16 blogs
- 5 Facebook pages
- 90 news outlets
- 64 Mendeley
This article is in the 99th percentile (ranked 1,480th) of the 441,480 tracked articles of a similar age in all journals and the 92nd percentile (ranked 3rd) of the 41 tracked articles of a similar age in Nature Geoscience
View more on Altmetric
Altmetric calculates a score based on the online attention an article receives. The donut visual summarises attention from different sources; a breakdown is shown in the legend. The number in the centre is the Altmetric score. Social media and mainstream news media are the main sources that calculate the score. Reference managers such as Mendeley are also tracked but do not contribute to the score. Older articles often score higher because they have had more time to get noticed. To account for this, Altmetric has included the context data for other articles of a similar age.
Mentions in news and blogs
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Mars: Where mud flows like lava
Bioengineer -
Mystery of lava-like flows on Mars is finally solved
Tech Explorist -
Mars may be covered in mud volcanoes disguised as lava flows
New Scientist TV -
Грязевые потоки на Марсе оказались похожи на земные потоки лавы
N+1: научные статьи, новости, открытия -
Planetary science: How mud might flow on Mars(Nature Geoscience)
Research Highlights -
Weird structures on Mars may be created by mud volcanoes
Gizmag Emerging Technology Magazine
This list highlights individual mainstream news articles and blogs that cite the article. Not all news and blogs link to articles in a way that Altmetric can pick up, so they are not representative of all media. Altmetric are responsible for the curation of this list and provide updates hourly.