An earthquake create a hazard of collapsing buildings and falling objects, which are the greatest threats. So it is quite possible to survive. A pyroclastic flow produces searing temperaturesthat can be well over 1,000 degrees Fahrenheit. You can survive the collapse of a building, but you cannot survive a pyroclastic flow.
A lava flow is simply a flow of liquid rock down a slope that usually results from an effusive eruption. A pyroclastic flow is an avalanche-like flow of hot ash, rock and gas that moves down a volcano during an explosive eruption, The move much faster than lava flows and are far more dangerous.
A pyrcoclastic flow is is much denser than a pyroclastic surge, as a large portion of it is composed of ash and rock. A pyrcolastic surge is composed more of gas.
In general, composite volcanoes are the most dangerous volcanoes because they are more explosive than the other types.
In addition to suffocating ash and flowing lava, pyroclastic flows are probably the most dangerous feature of some volcanoes. Pyroclastic flows are currents of extremely hot gases and rocks that flow down and away from the slopes of volcanoes. They travel at speeds has high as 450 mph, and the temperature of the gas and rock can reach more than 1800° F (1000° C).
No. Most pyroclastic flows don't go for more than a few miles.
Pyroclastic flow.
A lava flow is simply a flow of liquid rock down a slope that usually results from an effusive eruption. A pyroclastic flow is an avalanche-like flow of hot ash, rock and gas that moves down a volcano during an explosive eruption, The move much faster than lava flows and are far more dangerous.
A pyrcoclastic flow is is much denser than a pyroclastic surge, as a large portion of it is composed of ash and rock. A pyrcolastic surge is composed more of gas.
In general, composite volcanoes are the most dangerous volcanoes because they are more explosive than the other types.
No. Most pyroclastic flows don't go for more than a few miles.
In addition to suffocating ash and flowing lava, pyroclastic flows are probably the most dangerous feature of some volcanoes. Pyroclastic flows are currents of extremely hot gases and rocks that flow down and away from the slopes of volcanoes. They travel at speeds has high as 450 mph, and the temperature of the gas and rock can reach more than 1800° F (1000° C).
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.
Pyroclastic flows move much faster than lava flows and carry much more momentum. This means there is little time tog et out of the way, and that they can pass over barriers that would stop or deflect lava flows. They can also carry more material. A single pyroclastic flow can bury an area to several meters thick in a matter of seconds.
a tsunami
They destroy homes and bury and kill people.
An earthquake in the ocean is dangerous than on land because in the ocean if it occurs it can generate an earthquake which can cause more destruction than an earthaquake on land
In a pyroclastic flow, the magma would almost always be considered high-velocity. The velocity and strength of the magma is a result of its chemical composition.