In my article (G. S. Shteinberg, “The mechanism of generation of volcanic tremors and long-range prediction of eruptions”), published in *DAN*, vol. 165, no. 6, 1965, p. 1297, line 6, one should read: *Oscillations with such a period correspond to eigen-oscillations in a channel 60–80 km long.
G. S. Shteinberg
Submitted 1967-01-01 | RussiaRxiv: ru-196701.39988 | Translated from Russian

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ERRATA

In my article (G. S. Shteinberg, “The mechanism of generation of volcanic tremors and long-range prediction of eruptions”), published in DAN, vol. 165, no. 6, 1965, p. 1297, line 6, one should read: Oscillations with such a period correspond to eigen-oscillations in a channel 60–80 km long.

In the article (G. S. Shteinberg, “The structure of the Earth’s crust of Southern Kamchatka and the structural-tectonic position of Quaternary volcanoes”), published in DAN, vol. 166, no. 2, 1966, p. 443, line 24 from the bottom, one should read:

  1. The local distribution of volcanoes (within the volcanic group) is controlled by comparatively shallow-seated disturbances that cut through deep faults.

G. S. Shteinberg

Submission history

In my article (G. S. Shteinberg, “The mechanism of generation of volcanic tremors and long-range prediction of eruptions”), published in *DAN*, vol. 165, no. 6, 1965, p. 1297, line 6, one should read: *Oscillations with such a period correspond to eigen-oscillations in a channel 60–80 km long.