Landslides are caused by water making the ground on a hill loose and wet, allowing it to slide down the hill and crush everything in its path. Volcanoes erupt when magma from deep underground pushes its way up towards the surface, which explodes through the vent(s) releasing toxic gases, ash, and lava, which can burn and bury everything in the vicinity. Crustal plate movement is when tectonic plates in the lithosphere move around. It doesn't do that much damage. Tsunamis are formed when 2 oceanic plates collide, forcing a giant wave to occur that can stretch for miles, destroying everything in its path except for taller and sturdier buildings. Mountains are formed when 2 tectonic plates converge at their boundaries and push against each other, thus forcing one of them to rise upward. This causes the crust to rise, which will grow very high to form mountains. Natural earthquakes occur mainly along faults, large cracks in the crust. They form at the focus deep underground which produces several seismic waves which are picked up by seismographs. Directly above the focus is the epicenter, which is on the surface directly above the focus. The seismic waves are the shaking that is felt during an earthquake, and they can do different amounts of damage depending on the magnitude of the quake(s). Man-made earthquakes are not destructive unless caused by explosives. Otherwise, they are just caused by lots of people in an area clapping or stomping or yelling, etc. and are not destructive in any way.
The eruption that caused Mount St. Helens to lose its top occurred on May 18, 1980. The eruption was the result of a massive landslide and subsequent volcanic explosion, which caused the top 1,300 feet (400 meters) of the mountain to collapse and disintegrate.
If there is an earthquake near a mountain, the shaking can trigger landslides, rockfalls, and avalanches on the mountain slopes. The earthquake can also cause the formation of cracks or fractures in the mountain, potentially leading to increased instability in the area.
The eruption caused the top 1,300 feet (400 meters) of Mount St. Helens to be removed by the lateral blast and resulting landslide. This drastically altered the shape and height of the mountain, creating a large crater at the summit.
Yes, you can feel an earthquake on top of a mountain. However, the intensity of the shaking may vary depending on the distance from the epicenter of the earthquake and the height of the mountain. Generally, higher elevations can amplify the shaking during an earthquake.
A tall building on a mountain of granite is less likely to be damaged by an earthquake compared to a valley of sediment. Granite is a more stable and solid foundation that can help dissipate the seismic waves, whereas sediment in the valley is more prone to liquefaction and amplification of seismic waves, making it more vulnerable to damage.
mountain of granite
Earthquakes cause shaking that causes soil, rocks to slide down a mountain side. The longer the earthquake the more likely there will be large landslides. Volcanoes can also cause landslides when they erupt.
Earthquakes occur at that moment
The eruption that caused Mount St. Helens to lose its top occurred on May 18, 1980. The eruption was the result of a massive landslide and subsequent volcanic explosion, which caused the top 1,300 feet (400 meters) of the mountain to collapse and disintegrate.
If there is an earthquake near a mountain, the shaking can trigger landslides, rockfalls, and avalanches on the mountain slopes. The earthquake can also cause the formation of cracks or fractures in the mountain, potentially leading to increased instability in the area.
There are no benefits to a landslide. In mountain country they injure and even kill many people.
slump
When that happens a earthquake is produced.
Landslide
Signs of an imminent volcanic eruption include increased earthquake activity, swelling of the volcanic cone, increased gas emissions, and changes in the composition of gas emissions. Monitoring these signs can help predict and warn of an eruption.
whats the most famous eruption
Well, if an earthquake hits into a building, the building shows some cracks and starts deforming but it does not collapse, then the building is ductile structure. now consider a building to be a natural thing like a mountain, then you have a proper application of a ductile structure.