For the first time, the issue of the consequences of an earthquake on the state of the fractured environment of mountainous regions is investigated using a rigorous mechanical and mathematical approach. It is known that Earthquakes in mountainous areas are characterized by the repetition of high-magnitude aftershocks compared to the cases of lowland earthquakes. For this purpose, in order to approach reality, for the first time, a dynamic mixed problem on the unsteady impact on the shores of the semi-infinite Griffiths crack, as one of the objects of the mountain environment, is considered. It is assumed that the crack is located in a half-space parallel to its boundary. It is assumed that the fractured rock environment is an anisotropic composite and is described by the corresponding equations. The mechanical effects on the crack banks are described by a function that continuously depends on the time parameter and the geometric parameters of the coordinate system, which makes it possible to take into account the real non-stationary effect on the crack caused by an earthquake. It is assumed that the impact is carried out over a semi-infinite time interval, starting from zero initial conditions. The problem under consideration is related not only to the problem of seismic processes occurring in the Earth's crust of complex structure, including mountainous territories, but also to the engineering practice of composite materials of anisotropic structure. The case of a three-dimensional problem in which geometric and temporal parameters are equally included is studied. The mixed problem is reduced to the two-dimensional Wiener–Hopf integral equation, for which the authors have recently developed a rigorous mathematical method. The obtained solution, depending on the geometric and temporal parameters, made it possible to identify a previously undescribed surge effect at the initial moment of the stress intensity coefficient at the crack tip. It is established that the time-dependent stress intensity coefficient at the crack tip as a result of unsteady action can grow indefinitely at the initial moment, destroying the crack. The result explains the appearance of aftershocks after the main earthquake, as a result of its impact on existing cracks in the environment. Such a phenomenon in seismology as a swarm of earthquakes, consisting in the occurrence of more than ten small earthquakes within one hour, is also explained by the result obtained in the article.
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