A millennial-scale record of Holocene tsunamis on the Kronotskiy Bay coast, Kamchatka, Russia

2003 ◽  
Vol 59 (1) ◽  
pp. 36-47 ◽  
Author(s):  
Tatiana K. Pinegina ◽  
Joanne Bourgeois ◽  
Lilia I. Bazanova ◽  
Ivan V. Melekestsev ◽  
Olga A. Braitseva

AbstractDeposits from as many as 50 large tsunamis during the last 7000 years are preserved on the Pacific coast of the Kamchatka Peninsula near the mouth of the Zhupanova River, southern Kronotskiy Bay. These deposits are dated and correlated using Holocene marker tephra layers. The combined, preserved record of tsunami deposits and of numerous marker tephras on Kamchatka offers an unprecedented opportunity to study tsunami frequency. For example, from the stratigraphy along southern Kronotskiy Bay, we estimate frequency of large tsunamis (>5 m runup). In the last 3000 years, the minimum frequency is about one large tsunami per 100 years, and the maximum about one large tsunami per 30 years; the latter frequency occurred from about 0 to 1000 A.D. This time interval corresponds to a period of increased seismicity and volcanic activity that appears to be recorded in many places on the Kamchatka Peninsula.

2014 ◽  
Vol 123 (6) ◽  
pp. 835-853 ◽  
Author(s):  
Takahiro WATANABE ◽  
Noriyoshi TSUCHIYA ◽  
Shin-ichi YAMASAKI ◽  
Ryoichi YAMADA ◽  
Nobuo HIRANO ◽  
...  

2004 ◽  
Vol 4 (5/6) ◽  
pp. 703-709 ◽  
Author(s):  
A. Ramírez-Rojas ◽  
A. Muñoz-Diosdado ◽  
C. G. Pavía-Miller ◽  
F. Angulo-Brown

Abstract. In this work we present a spectral and multifractal study of the electric self-potential fluctuations registered in an electroseismic station located at 100km from the epicenter of an earthquake (EQ) with Mw=6.5 in the Pacific coast of Mexico. Our study suggests that in general the time series analyzed displays a persistent behavior. Our results show an anticorrelation between the spectral exponent β and the width of the multifractal spectrum Δα, when they are calculated during a time interval of five months (four months before the EQ and one month after the EQ). In addition, we also calculate the time evolution of the correlation coefficient finding that it has a very similar behavior that the time evolution of Δα.


2014 ◽  
Vol 358 ◽  
pp. 120-127 ◽  
Author(s):  
Ken Ikehara ◽  
Tomohisa Irino ◽  
Kazuko Usami ◽  
Robert Jenkins ◽  
Akiko Omura ◽  
...  

2014 ◽  
Vol 29 (2) ◽  
pp. 200-208 ◽  
Author(s):  
KOICHIRO TANIGAWA ◽  
YUKI SAWAI ◽  
MASANOBU SHISHIKURA ◽  
YUICHI NAMEGAYA ◽  
DAN MATSUMOTO

2014 ◽  
Vol 349 ◽  
pp. 91 ◽  
Author(s):  
Ken Ikehara ◽  
Tomohisa Irino ◽  
Kazuko Usami ◽  
Robert Jenkins ◽  
Akiko Omura ◽  
...  

2020 ◽  
Author(s):  
Paulina Bittner ◽  
Jane Gore ◽  
David Applbaum ◽  
Aaron Jimenez ◽  
Marcela Villarroel ◽  
...  

<p>International Monitoring System (IMS) is designed to detect and locate nuclear test explosions as part of Comprehensive Nuclear Test-Ban Treaty (CTBT) verification regime. This network can be also used for civil applications, such as the remote monitoring of volcanic activity.</p><p>Events related to volcanic eruptions, which are listed in the International Data Centre (IDC) bulletins, are typically detected by infrasound stations of the IMS network. Infrasound station IS44 and primary seismic station PS36 are situated in Kamchatka, Russian Federation, in the vicinity of several active volcanoes. These two stations recorded seismo-acoustic events generated by volcanic eruptions. In addition to atmospheric events, the IMS network has the potential of detecting underwater volcanic activity. Under favourable conditions, the hydroacoustic stations located in the Pacific Ocean and PS36 may detect underwater events close to the shore of Kamchatka Peninsula.</p><p>The aim of this presentation is to show examples of volcanic eruptions at Kamchatka Peninsula recorded by the IMS network. Supplementary information obtained by other observing networks can be found in reports issued by Kamchatkan Volcanic Eruption Response Team (KVERT) or Tokyo Volcanic Ash Advisory Center (VAAC). Such information can be compared with events listed in IDC bulletins.</p>


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