Eruption of Mount Vesuvius Pieces of Art

The volcanic eruption of "Vesuvius Eruption" (1835) of Vesuvius Pesce is a combination of the silver hydration of the moon and hot red lava flowing through the hillside. During Peter's generation he was not the only person to portray the famous Vesuvius Volcano, but Derby's Joseph Wright also painted 30 volcano paintings. This work is currently in the Nelson Atkins Museum of Art. This piece is oil on the panel, the frame is beautifully designed, and the edge is hung on one wall of the room with a one dimensional view.

The conical shape known as Vesuvio began to grow at the crater of Sonma Mountain Volcano that last erupted about 17000 years ago. Most of the rocks ejected from Mount Vesuvi are andesite, medium scale volcanic rock (about 53-63% silica). An andesite lava causes explosive eruption on various scales, making Mount Vesuvius a particularly dangerous and unpredictable volcano. Stromboli type volcanic eruption (magma burst of magma in volcano duct), lava flow and side crack are relatively small. The Prinny volcanic eruption (gas from a huge explosion, the pillars of ash and rock can rise up to tens of kilometers in the atmosphere) has a larger range, with an enormous ash and volcano, the entire ancient city near Mount Vesuvius Debris flow Vesuvius is now quiet, there are only small earthquakes (earthquakes) and volcanic holes in the crater of the summit but there is a possibility that the future will regain further violence in the future.

In the year 79 AD, the town of Rome of Pompeii and Herculaneum was buried beneath the layer of ash and volcanic ash with the eruption of Vesuvius Volcano. This is a model of the eruption of Plinim. Since then, Mount Vesuvius erupted several times. The last eruption was in 1944, when they advanced in Italy they brought problems to the Allies. It is a report of Pliny the Young that scientists led Vesuvius eruptions to be called "principals". The Phratomagmatic explosion is an eruption caused by the interaction between water and magma. When magma is in contact with water they are caused by thermal shrinkage (as opposed to magmatic eruptions caused by thermal expansion). The temperature difference between the two causes the interaction of fountains and lava that make up the volcanic eruption. Due to the difference of the eruption mechanism, the magmatic eruption product has a more uniform shape and finer grain size, it is thought to be finer than magmatic eruption products.