Answers are grounded in this paper and cite their sources.
Secular earth-strain measurements have been made in the central Aleutian Islands during the years 1970 and 1971. An annual variation of about 3 × 10−6 is evident on all records. A residual deformation of less than 3 × 10−6 per year is detected on most records. The state of strain near Amchitka Island, Alaska, at the time of CANNIKIN, November 6, 1971, differed from the state of strain at the time of the MILROW test, October 2, 1969, by less than 1 × 10−5. The strain records also contain novel episodes of large size (1-3 × 10−6) and high strain rate (1 × 10−7 / hr).
No takes yet. Share an insight, caveat, or question.
Butler et al. (1972) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: