Talk:Rootless cone

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Misspelled?

So which is misspelled here? The title or the word in the single sentence? I presume the title is correct, but I will leave it to someone more knowledgeable to say. Unschool 03:56, 4 November 2005 (UTC)[reply]

Pseudocrater vs. Rootless cone

The following discussion is an archived discussion of a requested move. Please do not modify it. Subsequent comments should be made in a new section on the talk page. Editors desiring to contest the closing decision should consider a move review. No further edits should be made to this section.

The result of the move request was: Page moved: no objections Ground Zero | t 01:36, 9 September 2014 (UTC)[reply]

Pseudocrater → Rootless cone – Hi, I'd like to suggest to move/rename this article from Pseudocrater to Rootless cone. The reason for this is that in recent years, the term pseudocrater has been largely replaced by the term rootless cone in scientific literature. The reason for this is that the cones are real features and hence the prefix pseudo is misleading (see page 580).

What do you think? Best regards. Chmee2 (talk) 07:36, 20 August 2014 (UTC)[reply]

What proportion of pseudocraters make cones? Anthony Appleyard (talk) 14:28, 20 August 2014 (UTC)[reply]

Hi, if I am not wrong, the term is not size-dependent. To call them rootless cones, the important is mechanism of their formation - interaction of lava with water. Best regards --Chmee2 (talk) 17:03, 20 August 2014 (UTC)[reply]

Support pseudocraters are craters caused by explosions, so are still "craters" in a general non-volcanic sense. -- 65.94.169.222 (talk) 04:09, 21 August 2014 (UTC)[reply]
Support "Rootless cone" is a more accurate name. — Gorthian (talk) 20:43, 28 August 2014 (UTC)[reply]

The above discussion is preserved as an archive of a requested move. Please do not modify it. Subsequent comments should be made in a new section on this talk page or in a move review. No further edits should be made to this section.

Possible references to improve

Burr, Devon M.; Bruno, Barbara C.; Lanagan, Peter D.; Glaze, Lori S.; Jaeger, Windy L.; Soare, Richard J.; Wan Bun Tseung, Jean-Michel; Skinner, James A.; Baloga, Stephen M. (2009). "Mesoscale raised rim depressions (MRRDs) on Earth: A review of the characteristics, processes, and spatial distributions of analogs for Mars". Planetary and Space Science. 57 (5–6): 579–596. Bibcode:2009P&SS...57..579B. doi:10.1016/j.pss.2008.11.011.
Bruno, B.C., Fagents, S.A., Hamilton, C.W., Burr, D.M. and Baloga, S.M., 2006. Identification of volcanic rootless cones, ice mounds, and impact craters on Earth and Mars: Using spatial distribution as a remote sensing tool. Journal of Geophysical Research: Planets, 111(E6)
Fagents, S.A. and Thordarson, T., 2007. Rootless volcanic cones in Iceland and on Mars. The geology of Mars: Evidence from Earth-based analogs, pp.151-177.|Harvard doi:10.1017/CBO9780511536014.007
Boreham, F., Cashman, K., Rust, A. and Höskuldsson, Á., 2018. [Linking lava flow morphology, water availability and rootless cone formation on the Younger Laxá Lava, NE Iceland. https://www.sciencedirect.com/science/article/pii/S0377027318302063] Journal of Volcanology and Geothermal Research, 364, pp.1-19.https://doi.org/10.1016/j.jvolgeores.2018.08.019

ChaseKiwi (talk) 13:56, 10 February 2024 (UTC)[reply]