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An active fault is a fault that has displayed recent seismic activity, while an inactive fault has not displayed recent seismic activity.

Do not be fooled by the word "recent," however, as we are talking about "recent" from a geological perspective, which is much different from a non-geologic perspective. Because of the fickle nature of plate tectonics, an active fault could have earthquakes as often as once every few years or once every one thousand years. Conversely, it's very hard to call a fault inactive if we don't know it's quake history, and for some faults, geologists will wait ten thousand years in between quakes to call them inactive.

There are a variety of techniques that geologists can use to help them determine the frequency of earthquakes among faults, however. If a history of quakes coming from the fault are available, scientists can look at the average period of time in between quakes to determine whether a fault is presently "active" or "inactive." Scientists can also measure creep among fault lines to check for seismic activity.

There really is no way to concretely define a fault as "active" or "inactive" (especially because inactive faults can suddenly become active again), but it's more or less safe to say that if a fault hasn't shown tectonic activity for about 5,600 years, it's probably inactive.

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Just to add to that explanation, if movement occurs on long-quiescent fault in a new phase of tectonic activity, the fault is described as 're-activated', and the new movement can be the opposite to the original.

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What are active faults and inactive?

Most geologist consider a particular fault to be an active fault if it has moved during the past 10,000 years of the Holocene Epoch. An inactive fault is one that hasn't moved during the past 10,000 years of the Holocene Epoch.


What is differentiate active and inactive faults?

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.


What is inactive fault?

According to the book Natural Hazards, most geologist consider a particular fault to be an active fault if it has not moved during the past 10,000 years of the Holocene Epoch.


What are the examples of inactive faults in the Philippines?

Oh honey, let me tell you, the Philippines has more inactive faults than I have ex-husbands! Some examples include the West Valley Fault, Manila Trench, and the Central Philippine Fault. These bad boys may be dormant now, but don't let them fool you - they can still shake things up when they feel like it.


Why don't all faults cause earthquakes?

Faults are the boundaries between tectonic plates and are not the cause of earthquakes. The motion of one plate against another or the subduction of one plate by another can eventually cause a slippage, and it is this slippage that causes earthquakes.

Related Questions

What are the similarities of active and inactive faults?

Active and inactive faults are both types of fractures in the Earth's crust where movement has occurred in the past. They both have the potential to generate earthquakes when stress is released along the fault line. Additionally, both types of faults can be identified through geological mapping, remote sensing techniques, and geophysical surveys. The main difference between active and inactive faults is that active faults are currently experiencing tectonic movement, while inactive faults have not shown any recent movement but still have the potential to generate earthquakes in the future.


What are active faults and inactive?

Most geologist consider a particular fault to be an active fault if it has moved during the past 10,000 years of the Holocene Epoch. An inactive fault is one that hasn't moved during the past 10,000 years of the Holocene Epoch.


What is differentiate active and inactive faults?

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.


What is active and inactive faults?

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.


What is inactive fault?

According to the book Natural Hazards, most geologist consider a particular fault to be an active fault if it has not moved during the past 10,000 years of the Holocene Epoch.


What is a passive fault?

A passive fault is a fault that is not currently experiencing movement or does not have the potential to generate seismic activity. These faults may have been active in the past but are now considered inactive or dormant.


How many faults does the US have?

OK!over 99 active faults!


What are the examples of inactive faults in the Philippines?

Oh honey, let me tell you, the Philippines has more inactive faults than I have ex-husbands! Some examples include the West Valley Fault, Manila Trench, and the Central Philippine Fault. These bad boys may be dormant now, but don't let them fool you - they can still shake things up when they feel like it.


Why don't all faults cause earthquakes?

Faults are the boundaries between tectonic plates and are not the cause of earthquakes. The motion of one plate against another or the subduction of one plate by another can eventually cause a slippage, and it is this slippage that causes earthquakes.


What is an inactive fault?

An inactive fault is a fault line that is currently not experiencing significant seismic activity. These faults may have a history of movement but have not shown recent signs of movement, making them less of a concern for potential earthquakes.


What two factors do geologists consider when determining earthquake risk for a region?

By locating where faults are active and where past earthquake have occurred.


Are faults with no active creep safe?

No, they are not safe. No active creep, that is acting over hundreds of years slowly deforms the crustal rock on both sides of the fault. Ultimately, it leads to the elastic rebound of the rock, that causes big scale earthquakes.