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.
Yes, they are longer. Longer wavelengths are lower energy.
Although quakes on the moon are much weaker (and rarer) than those on Earth, they can last for much longer. We live in far damper environment than is on the moon and the seismic vibrations of our earthquakes will eventually be calmed by the moisture in the atmosphere. While an earthquake typically lasts for just a few seconds (10-30 for most moderate earthquakes), moonquakes can last up to an hour.
Tornadoes are both much larger than tornadoes and last much longer.
Longer faults have a larger area of rupture, which allows more accumulated stress to be released during an earthquake. Additionally, longer faults tend to involve greater amounts of energy release due to the larger fault surface area, resulting in larger earthquakes.
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.
Not necessarily. Impulse depends on both the force applied and the time over which it acts. A smaller force acting for a longer time can produce the same impulse as a larger force acting for a shorter time.
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
an act is longer
centisecond is longer