There is a scientific use of these clean, unstable rocks, and …

The precariously balanced rocks are not only some of nature’s most dramatic and eye-catching features, but they are extremely helpful in identifying earthquake hazards in an area.

The instability that gives PBRs – an official term used by geologists – their name tells experts about tremors and tremors in a specific area in the past. Every movement is very difficult, and these rocks or rocks will fall off their corners.

By analyzing the vulnerability and lifetime of some California breeders’ rights, the researchers determined the upper limit of earthquake intensity that has occurred since the rock structures formed and used this information to reduce the uncertainty in current major earthquake risk models by 49 percent.

“Our new approach can help us figure out which areas are most likely to have a major earthquake,” says geologist Anna Rudd of Imperial College London in the United Kingdom.

“Breeder’s rights work like reverse seismometers, capturing regional seismic history that we haven’t seen and informing us of previous highs of earthquakes by non-inversion. Using these, we provide uniquely valuable data on rare rates of high-strength earthquakes.”

The new research consists of two phases. First, the researchers determined the age of the PBR formations through cosmic surface exposure, and counted the number of rare beryllium atoms in rocks (which consist of long-term exposure to cosmic rays).

Second, the researchers used 3D simulation models to calculate the amount of vibration these rocks could withstand before they capsized. One of the findings of the study was that plant breeders’ rights to the landscape could be reserved twice as long than previously assumed.

This information is an invaluable addition to earthquake risk models because it bridges some of our knowledge gaps prior to the existence of modern monitoring equipment – an indication of earthquake activity up to a million years ago.

Risk models consist of a bewildering number of different factors and data points, from fault-line location to seismic activity over time. Solid records, such as those emerging from the new study, help fine-tune these other factors.

Color stickers were used to support the 3D modeling. (Anna Rudd and Dylan Rudd, Imperial College London)

“We are now looking at breeder rights near major earthquake faults like the San Andreas Fault near Los Angeles,” says Anna Rudd. “We are also investigating how precisely how data – whether they relate to error rates or choice of equations of soil vibration – deform the results in the original risk models.”

Breeder rights can arise when soft rocks erode to leave more rigid rocks, or when receding glaciers leave rocks in unnatural locations. There are many examples around the world, from the Briham Rocks in Yorkshire in the United Kingdom to the Chericahua National Monument in Arizona, USA.

This broad coverage in terms of location means that researchers can feed plant breeders’ rights into many seismic risk models. Models can help determine future earthquake risks in residential areas and sites with major structures such as dams and nuclear power plants.

Thanks to new research, we now have a better idea of ​​how long the PBR can last and how much vibration it will take to remove it. All this information is useful for risk modeling, especially in cases where other data sources are lacking, for example B. Marine fault lines that are not easily monitored.

“We are on the verge of a breakthrough in the science of earthquake prediction,” says geologist Dylan Rudd of Imperial College London.

Our “rock clock” technologies have the potential to save enormous costs in seismic engineering and can be used to test and update site-specific risk estimates for seismic regions – particularly in coastal areas where controlled seismic sources are marine faults whose movement is more difficult to study. ”

The research has been published in Advanced Advances at AGU.

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