They are not considered safe b/c of Reids Elastic Rebound Theory.
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.
to measure vertical movments-tilt meter to measure horizontil movments-creep meter
Four Instruments that are used to detect movement along faults are:1. Tiltmeter2. Creep meter3. Laser-ranging device4. Network of Earth-Orbiting satellites called GPS (global positioning system)
Soil creep is the slowest form of mass wasting.
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.++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.
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.
yes
to measure vertical movments-tilt meter to measure horizontil movments-creep meter
to monitor faults, geologists have developed instruments to measure changes in elevation, tiliting of the land surface, and ground movements along the faults. Geologists use tiltmeters, Creep Meters, Laser- Ranging Devices, and GPS Satellites.
four instruments that are used to detect faults are: creep meters, laser-ranging devices, tiltmeters, and satellites. how they work: a creep meter uses a wire stretched across a fault to measure sideways movement the ground. a laser-ranging device uses a laser beam bounced off a reflector to detect any fault movements
Geologists have created Creep Meters, GPS Satellites, Range/ Laser devices, and Tilt Meters. These instruments help keep track of changes in the land surface and elevation.- Polly T. Denver, CO
Four Instruments that are used to detect movement along faults are:1. Tiltmeter2. Creep meter3. Laser-ranging device4. Network of Earth-Orbiting satellites called GPS (global positioning system)
Four Instruments that are used to detect movement along faults are:1. Tiltmeter2. Creep meter3. Laser-ranging device4. Network of Earth-Orbiting satellites called GPS (global positioning system)
of Creep, of Creep, imp. & p. p. of Creep.
Yes, creep is a noun, as in "he was a creep". It can also be a verb, as in "he crept along".
Cause a Creep creep's up on someone slowly and a Creep is very slow
Yes, creep is a noun, as in "he was a creep". It can also be a verb, as in "he crept along".