its only been around for 120 years wow :) your welcome for answering my uncle was a seismologist
Ancient Greeks are credited with being the first to study and document earthquakes, with Thales of Miletus being one of the first to speculate about the causes of earthquakes around 585 BCE. However, the Chinese also have a long history of recording and studying earthquakes, with historical texts dating back to 780 BCE documenting seismic events.
3 around 1984
Pi have been studied for over 10 centuries!!!
because they like to learn about it
The local or Richter magnitude scale is named after Charles Francis Richter an American seismologist and geophysicist. Some people use the title Richter-Gutenberg scale to acknowledge the contribution to the scale of Charles Richter's colleague, Beno Gutenberg a fellow geophysicist at the California Institute of Technology. it is worth noting however that geophysicists / seismologists use the moment magnitude scale in place of the Richter magnitude scale when possible as it is more reliable for large magnitude earthquakes (greater than 6.9) and for earthquakes that occur a long distance away from the nearest seismometer station (greater than 600 km).
they learn how long that rocs been there ,what encoutered it and how old it is
Yes, earthquake activity has affected Earth in the distant past. Over millions of years, earthquakes have shaped the Earth's surface by creating mountains, shifting continents, and causing tsunamis. Studying the geological record helps us understand how earthquakes have influenced the planet's history.
The earthquakes will be 90%-81% of the largest 40,000km long.
They never "started", earthquakes have been going on for as long as the earth has been around.
There have been many earthquakes in Turkey that lasted for varied periods. Most of the earthquakes have lasted for about 30 seconds leaving so many fatalities and so much damage.
How long the seismologist wants the paper to last before it runs out and he has to go and install a new roll.
Long-term earthquakes refer to seismic activity that occurs over an extended period of time, potentially lasting for years or decades, while short-term earthquakes occur within a brief timeframe, often minutes or hours. Long-term earthquakes may involve slow-slip events or aftershocks, while short-term earthquakes are typically caused by sudden release of tectonic stress along fault lines.