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A fourth awakening

Since 2005 the ground of Campi Flegrei has risen by 0.4 to eight inches per year. This rate of inflation is lower than what was observed during the past three periods of unrest, but it has been happening for almost two decades now. Volcanologists have begun to wonder what happens if the crust is stretched beyond its breaking point.Hentai Sex Doll

There has also been a jump in the frequency and intensity of quakes in the area since the summer. The number has dropped off in the past few weeks, but potent temblors are still rocking the region, including a magnitude-4.0 event on October 2. What could explain this perturbing activity?Fucking A Sex Doll

In June a group of scientists published a paper that attempted to decode the behavior of the volcano over the past 70 years. If this study’s interpretation is correct, it could also explain what’s happening in today.

Here’s what they think is going on: At a depth of five to six miles, there is a persistent magma reservoir that is continually loosing noxious gas. Some of that gas is trapped at a barrier of rock roughly two miles below the surface, and some escapes out of small volcanic maws at places like the malodorous Solfatara crater.

The researchers hypothesize that, in the 1950s, a magma batch intruded close to that rock barrier, fracturing it a little and elevating the crust. Once the magma cooled down and the extra gas escaped to the surface, the uplift stopped and the ground subsided—although it never returned to levels measured before the uplift.

The team believes the same process happened again in the 1970s and 1980s. By the time of the 1980s unrest, the repeated fracturing of the crust had created new pathways for trapped gas to escape, which led to a significant period of subsidence afterwards.Elden Ring Sex Doll

Many of those fractures have since healed up. Those past three injections of magma have cooled and frozen, creating a “magma seal, which is also a barrier to the gas’s escape,” says study co-author Nicola Alessandro Pino, senior researcher at the INGV’s Vesuvius Observatory in Naples. But gas has continued to come from the deep magma reservoir, and much of it has accumulated again at the rocky barrier about two miles down, causing the ground to inflate.

Magmatic gas rising from deep below and getting stuck is sufficient to explain the uplift that has been happening since 2005—and the recent and occasionally strong quakes may be coming from the aggressive merging of newly formed fractures.