Titlebook: Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries; Eystein S. Husebye Conference proceedings 2008 Springer Science+B

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The Karelian Regional Seismic Network in NW Russiaseismic observations which is incomplete regarding small earthquakes say below ML = 4.5. For the Karelia Region (north of St. Petersburg) most located seismic events are explosions in origin and further more recorded mainly by stations and arrays adjacent to Karelia that is in Kola, Finland and N. N

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Cossack Ranger II – A High Quality, Versatile and Affordable 3-Component Short-Period Seismographcal analysis center. National network operations are normally a government responsibility including the national tasks of monitoring earthquake activities and advising local authorities on earthquake hazards. Originally, seismographs were developed, deployed and operated by Academia but as stated no

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Accurate Location of Seismic Sources With and Without Travel Time Modelhe 3D seismic velocity structure of the Earth. Likewise, to collect associated ground truth (GT) event information that is event with focal parameter estimates within 1, 5 or 10 km for model validation tests. The accuracy of velocity models currently available are verified for limited areas only, as

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Data Driven Probabilistic Seismic Hazard Assessment Procedure for Regions with Uncertain Seimogenic (Cornell, 1968) and “historical” (Veneziano et al., 1984) procedures. The maximum regional magnitude .. is of paramount importance in this approach and the author present statistical technique that can be used for evaluation of this important parameter. The approach permits the utilization of incomp

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Seismicity and Seismic Hazard Assessment in Greecele seismic hazard assessments are important for sustaining the economical developments of a country like Greece. The objective of such studies and modeling efforts are to obtain long term probabilities of occurrences of seismic events of specified sizes in given time interval..Primary information fo

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Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Stuen up to present. Local shaking manifestations were most spectacular with rock, stone and mud avalanches, mast-high waves in nearby Rana fjord and even liquefaction was reported. Most surprisingly, at epicentral distances exceeding 100 km except for Stockholm 800 km away, very few macroseismic obser

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https://doi.org/10.1007/978-3-031-25859-6 Note that deployment and subsequent network operations are a costly undertakings but using the inexpensive and versatile Cossack Ranger II instrumentation a high quality and affordable network operation for Karelia has been achieved. These efforts are the topic of this article.

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