Seismic work in Mount Spor Berkano

The past few weeks have seen a remarkable rise in attention to the possibility of Mount Spurr Volcano about the explosion, partly due to the escalation of the earthquake. The Alaska earthquake center tracks a variety of seismic activity throughout the state, with a focus on earthquakes that are likely to be harmful. While we discover and determine the location of the earthquakes associated with volcanoes, our priorities are somewhat different from those in the Alaska Berkane Observatory (AVO).

The AVO component in Alaska's seismic monitoring system focuses on volcanoes. The main goal of the earthquake center is to accurately trace the earthquake – including those in volcanoes – appointed via Alaska on a state level.

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Mount Spurr Oarmquakes gradually increased in April 2024, and AVO raised the level of alert to the yellow/consultant in October 2024. In March 2025, the signs began to indicate a possible eruption.

Mount Spurr is 78 miles northwest of Marina, a prominent peak in the Aleutian chain (Figure 1). Over the past century, she gained attention due to many important explosions and ongoing periods of volcanic activity, with the last explosion in 1992 (to obtain a full volcanic history, prefer to visit AVO on the Mount Spurr activity.)

Since we are watching observation earthquakes, we notice the earthquakes that often accompany (but not always!) The explosions. Southwest Alaska also produces the major earthquakes in the state, along the same part of the famous Pacific Ring, which generates magma that nourishes the volcanic arc in Alaska. The distinction between the earthquakes of the integration area and the volcanic earthquakes is an important part of assessing the various risks.

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The increase in seismic activity often indicates the volcanoes to the movement of magma or gas below the surface. The magma and gas also accumulate and expand, as it causes the volcano to swell and break. This cracking is picked up by seismic sensors, and the earthquake center analyzes are known to put these events as volcanic because they are shallow and occur near volcanoes (Forms 2 and 3). How much and what is the type of activity that differs from the volcano and the earthquake center.

The data of each station is shared within the seismic Alaska networks through the institutions that decline all types of seismic events. Last year, the AVO seismic data analysts dealt with nearly 3,700 earthquakes near Mount Spor. This high number is partially caused by the very low threshold that AVO has identified for the seismic activity that they discover and achieve, providing a level of details for scientists to examine internal business and the stage of disturbances of active volcanoes known.

At the Alaska earthquake center, seismic data analysts show about 45,000 seismic event every year, the vast majority of which are earthquakes. We have a somewhat higher threshold for the events we review, but again, we also have our eyes on the entire state. We focus on capturing the events that I also felt insightful on other types of seismic information that improves the clearest discoveries of our earthquake.

While the earthquake center and the volcanic Observatory focus on various aspects of seismic activity, the enhanced understanding of geological risks in Alaska is at the heart of everything.

For more information about the last activity in Mount Spurr, check the AVO website on the Mount Spurr activity.

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