When a longer fault ruptures, you have movement along a longer section of the crust, and so more rock is moving.
Active faults can generate earthquakes and represent sources of seismic energy. Inactive faults can no longer generate earthquakes but did so in the past. +++ They can, but really the earthquake is the effect of the movement on the fault, so not the defining mechanism. ' An active fault is one still moving (albeit usually in small, irregular steps over millions of years); an inactive fault is stable. If a new phase of tectonic stresses arrive, an inactive fault can be 're-activated', in many cases with the movement in the opposite direction. A fault is a fracture with displacement, and that movement is of the rock on one side of the fault-plane across the other.
The size of the wick dertermines how large the flame is.
Moonquakes typically last longer than earthquakes. This is due to the structure of the Moon, which lacks tectonic plates like Earth. Moonquakes can last up to several minutes whereas earthquakes on Earth typically last for only a few seconds.
Yes, they are longer. Longer wavelengths are lower energy.
Tornadoes are both much larger than tornadoes and last much longer.
Because it is stronger!
Because it is stronger!
yes it is
Active faults can generate earthquakes and represent sources of seismic energy. Inactive faults can no longer generate earthquakes but did so in the past. +++ They can, but really the earthquake is the effect of the movement on the fault, so not the defining mechanism. ' An active fault is one still moving (albeit usually in small, irregular steps over millions of years); an inactive fault is stable. If a new phase of tectonic stresses arrive, an inactive fault can be 're-activated', in many cases with the movement in the opposite direction. A fault is a fracture with displacement, and that movement is of the rock on one side of the fault-plane across the other.
Active faults can generate earthquakes and represent sources of seismic energy. Inactive faults can no longer generate earthquakes but did so in the past. +++ They can, but really the earthquake is the effect of the movement on the fault, so not the defining mechanism. ' An active fault is one still moving (albeit usually in small, irregular steps over millions of years); an inactive fault is stable. If a new phase of tectonic stresses arrive, an inactive fault can be 're-activated', in many cases with the movement in the opposite direction. A fault is a fracture with displacement, and that movement is of the rock on one side of the fault-plane across the other.
The larger batteries are able to produce more current, and will last longer before they die.
alligators live longer because they are larger and longer and has a larger part of everything than a crocodile
The size of the wick dertermines how large the flame is.
It is no longer in existence, destroyed by earthquakes but was situated on the island of Pharos
If there is little or no earthquake activity on a fault, or a section of a fault then it may be: Inactive (no longer moving) Locked (If it is known to be building up strain for a future large earthquake, i.e. San Andreas) or It may be releasing nearly all it's stress by creeping, rather than in large quakes.
an act is longer
centisecond is longer