Over geologic time, the continental slopes are temporary depositional sites for sediments. During lowstands of sea level, rivers may dump their sedimentary burden directly on them. Sediments build up until the mass becomes unstable and sloughs off to the lower slope and the continental rise.
Here are the answers of the question given above. The methods that scientists do use to predict volcanic eruptions are the following: the same methods used to predict earthquakes, measurements from seismograph and tiltmeters, and <span>tracking sulfur dioxide gas emissions with cospec. Hope this is the answer that you are looking for. Thanks for posting!</span>
It’s always depends on the mass/weight of the rock heavier goes faster and the lighter goes slower (but if they are roughly the same size there is no dramatic change in speed)
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