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Yes. Earthquakes and volcanic eruptions can cause debris flows. Volcanic eruptions can mudflows called lahars.
As for I only know, there's only earthquakes and volcanic eruptions...please help!
Six types of classification of volcanic eruptions in the Philippines are Hawaiian, Straombolian, Vulcanian, Plinian, Ultra-Plinian, and Phreatic. Plinian eruptions are explosive eruptions that produce a large ash cloud.
What happens to the atmosphere when they erupt?
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Yes. Earthquakes and volcanic eruptions can cause debris flows. Volcanic eruptions can mudflows called lahars.
Yes. Large explosive eruptions can release large amounts of sulfur dioxide. This gas forms tiny droplets of sulfuric acid in the upper atmosphere, which reflect a portion of the sun's light back into space and reduce global temperatures.
As for I only know, there's only earthquakes and volcanic eruptions...please help!
Six types of classification of volcanic eruptions in the Philippines are Hawaiian, Straombolian, Vulcanian, Plinian, Ultra-Plinian, and Phreatic. Plinian eruptions are explosive eruptions that produce a large ash cloud.
What happens to the atmosphere when they erupt?
Tsunami are waves caused by sudden movement of the ocean due to earthquakes, landslides on the sea floor, land slumping into the ocean, large volcanic eruptions or meteorite impact in the ocean.
A significant impact to the planet from a large enough asteroid could cause volcanic eruptions.
Volcanic eruptions.
Both a typhoon and a volcanic eruption are natural disasters that can release large amounts of energy. Beyond that they are completely different.
It is captured during sedimentation through carbon capture which is one of the processes involving limestone formation. It is released in large quantities during volcanic eruptions.
No. Volcanic eruptions produce ash. Earthquakes and volcanic eruptions get clustered. A volcanic eruption can cause vibrations, while a large temblor can rattle a magma chamber under a volcano, causing towers of ash and rivers of lava to gush forth.