As with many stratovolcanoes, the type of activity at Mount St Helens varies. In its famous 1980 eruption it produce massive clouds of ash and pumice and later built a lava dome. The rock formed was dacite. However, other material has erupted in the volcano's past, including basaltic lava flows.
Volcanic fragments are small pieces of rock that come from a volcano. Fragments are usually thrown in the air during a volcanic eruption.
Lassen Peak erupts mainly dacite and andesite lava, which results in volcanic fragments such as pumice, ash, and tephra being expelled during its eruptions. These fragments can vary in size and are often carried by the eruption plume and deposited around the volcano.
Mount Fuji primarily erupts and produces basaltic to andesitic volcanic rock fragments, including tephra, pumice, and volcanic ash. The lava flows from its eruptions are typically fluid, allowing for extensive lava flow development. These materials reflect the stratovolcano's explosive and effusive eruption styles, contributing to its iconic conical shape. The volcanic activity at Mount Fuji has created a diverse range of volcanic products over its history.
Mount St. Helens is predominantly composed of andesite, which is an intermediate volcanic rock that forms from the partial melting of the Earth's crust. This type of rock gives Mount St. Helens its characteristic gray color and is related to the volcanic activity in the area.
Interesting question. After the explosive eruption, the gas content of the rhyolitic magma should have decreased enough to allow obsidian to form. It is the right kind of lava. However, most of the lava dome in the Mount St. Helens caldera is dacite, which is "grainier" than obsidian, indicating that it cooled too slowly to have a "glassy" appearance. Obsidian flows must cool quickly to prevent crystal formation. It is possible that some obsidian was formed, but subsequently covered by dacite. I have not been able to find any reports that mention obsidian recovered from the Mount St Helens lava dome.So the answer is a qualified no, we don't have any evidence of obsidian flows from Mount St Helens.Incidentally, there are individuals and companies selling products they call "helenite" or "St Helens Obsidian", which is a synthetic material created by fusing volcanic ash (which may or may not have come from Mount St Helens).
it was created by magma in the earth's core and when all the volcanic gasse come out it exploded and is now what it is
Igneous Rock
Volcanic fragments are small pieces of rock that come from a volcano. Fragments are usually thrown in the air during a volcanic eruption.
Lassen Peak erupts mainly dacite and andesite lava, which results in volcanic fragments such as pumice, ash, and tephra being expelled during its eruptions. These fragments can vary in size and are often carried by the eruption plume and deposited around the volcano.
Mount Fuji primarily erupts and produces basaltic to andesitic volcanic rock fragments, including tephra, pumice, and volcanic ash. The lava flows from its eruptions are typically fluid, allowing for extensive lava flow development. These materials reflect the stratovolcano's explosive and effusive eruption styles, contributing to its iconic conical shape. The volcanic activity at Mount Fuji has created a diverse range of volcanic products over its history.
Meteorites are formed from fragments of asteroids, planets, or moons that collide in space. These fragments are flung into space due to impacts, volcanic eruptions, or other geological events. Some meteorites come from the Moon or Mars, ejected by asteroid impacts. Once these fragments enter Earth's atmosphere without burning up, they are called meteorites.
Mount St. Helens is predominantly composed of andesite, which is an intermediate volcanic rock that forms from the partial melting of the Earth's crust. This type of rock gives Mount St. Helens its characteristic gray color and is related to the volcanic activity in the area.
Interesting question. After the explosive eruption, the gas content of the rhyolitic magma should have decreased enough to allow obsidian to form. It is the right kind of lava. However, most of the lava dome in the Mount St. Helens caldera is dacite, which is "grainier" than obsidian, indicating that it cooled too slowly to have a "glassy" appearance. Obsidian flows must cool quickly to prevent crystal formation. It is possible that some obsidian was formed, but subsequently covered by dacite. I have not been able to find any reports that mention obsidian recovered from the Mount St Helens lava dome.So the answer is a qualified no, we don't have any evidence of obsidian flows from Mount St Helens.Incidentally, there are individuals and companies selling products they call "helenite" or "St Helens Obsidian", which is a synthetic material created by fusing volcanic ash (which may or may not have come from Mount St Helens).
Analysis of deposits suggets that many of Pinatubo's eruptions are similar to the one that occurred in 1991. This eruption produced enormous clouds of ash and pumice.
Kilauea generally produces lava flows and lava fountains. Its current activity has also involved the formation of lava lakes. All of the lava involved is basaltic.
im not sure but im doing a project on st.helens mountain and i have to due it in 4 days time and i only have written half a page so i reaaly need help so plz help meee!!! im so anoyed !!!
Volcanic ash forms when magma is explosively ejected from a volcano. The explosive force of expanding gasses in the magma blasts it apart into small particles, which then solidify to form tiny shards of glass.