Template:Did you know nominations/Meers Fault
Appearance
- 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 Yoninah (talk) 00:55, 4 August 2019 (UTC)
DYK toolbox |
---|
Meers Fault
[edit]- ... that the Meers Fault in Oklahoma was active during the last 3,000 years and features a scarp that reaches 5 metres (16 ft) height? Most recent prehistoric deformation: latest Quaternary (<15 ka) Comments: Two late Holocene events are documented—one between 1,100–1,300 yrs ago (Luza and others, 1987 #669; Luza and others, 1987 #544; Madole, 1988 #662; Crone and Luza, 1990 #661; Kelson and Swan, 1990 #659), and a preceding event between 2,000-2,900 yrs ago (Kelson and Swan, 1990 #659; Swan and others, written commun. 1993 #675)A 26-km-long linear fault scarp as much as 5m high along the Meers fault, first brought to public attention by Gilbert (1983a, 1983b) and Donovan et al. (1983), indicates recent reactivation of the Meers fault.
Moved to mainspace by Jo-Jo Eumerus (talk). Self-nominated at 09:34, 23 June 2019 (UTC).
- This article is new enough and long enough. The hook facts are cited inline, the article is neutral and I detected no copyright or plagiarism issues. A QPQ has been done. Cwmhiraeth (talk) 05:40, 12 July 2019 (UTC)