Dacite, a volcanic rock with about 65% silica. This amount of silica in dacite is a lot higher than the basalts of Hawaii which have less than 50% silica. The high silica content makes the magma "sticky" and can cause more pressure to build up. With so much pressure, eruptions from Mount St. Helens can be very violent like the famous 1980 eruption.
Dacite, a volcanic rock with about 65% silica. This amount of silica in dacite is a lot higher than the basalts of Hawaii which have less than 50% silica. The high silica content makes the magma "sticky" and can cause more pressure to build up. With so much pressure, eruptions from Mount St. Helens can be very violent like the famous 1980 eruption.
The eruption of 1980 was Plinian in nature, however, the collapse of the Northern flank removed the confining pressure rapidly, causing volatiles to exsolve explosively and leading to a lateral debris avalanche (pyroclastic flow), more typical of the Pelean eruption style (and Nuee Ardentes). The eruption was also accompanied by a hydrothermal blast.
Sources: Own knowledge. Use link for reference: http://www.geology.sdsu.edu/how_volcanoes_work/Sthelens.html
The 1980 eruption of Mount St. Helens did not produce lava flows. It was a highly explosive Plinian eruption that produced a massive plume of ash and pyrolastic flows. These are not lava flows but rather avalanche-like masses of hot ash, rock, and gas. Some time after that eruption Mount St. Helens produced a lava dome, which consists of lava so viscous that it piles up at the vent rather than flowing away.
Mount St. Helens consists of lava rock interlayered with ash, pumice and deposits, together with layers of basalt and andesite.
As Mount St. Helens is a volcano the slopes would be covered in layers of volcanic dust and lava.
The rock type you're looking for is basalt -- St. Helens contains basalt, andesite, and dacite in the form of lava flows and pyroclastic deposits.
the type of material it is, is a composite which has high eruptive forces, has high silica content, and has high gas content. which makes it an eruption product of gas and ash.
Mount St Helens erupts dacitic lava, which forms dacite when it cools. Because of the high gas content and high viscosity much of the material gets erupted as ash and pumice rather than lava.
a pyroclastic flow
Mount St. Helens consists of lava rock interlayered with ash, pumice and deposits, together with layers of basalt and andesite.
it has pyroclastic flow and has small eruptions of ash.
As Mount St. Helens is a volcano the slopes would be covered in layers of volcanic dust and lava.
Hot lava
The rock type you're looking for is basalt -- St. Helens contains basalt, andesite, and dacite in the form of lava flows and pyroclastic deposits.
the type of material it is, is a composite which has high eruptive forces, has high silica content, and has high gas content. which makes it an eruption product of gas and ash.
The 1980 eruption of Mount St. Helens did not produce lava flows. It was a plinian eruption that produced aolumn of ash and pyroclastic flows. Pyroclastic flows are avalanche-like masses of hot ash, rock, and gas that rase away from an erupting volcano at speeds that can reachinto the hundreds of miles per hour.
Mount St Helens erupts dacitic lava, which forms dacite when it cools. Because of the high gas content and high viscosity much of the material gets erupted as ash and pumice rather than lava.
Mount St. Helens has produced lava flows in the past. However, the famous eruption in 1980 produced something much more dangerous: pyroclastic flows. These are avalanche-like currents of hot ash, rock, and gas that race out of a volcano. The initial pyroclastic flow from the lateral blast may have briefly been supersonic.
No, a dike is not a type of Lava flow.
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.