An identification of the Meers Fault - location and statistics -- current info

In May of 1985, the Oklahoma Geological Survey installed a seismograph in the Meers Store to monitor the Meers disfigurement. The seismograph is able to feel movement in the Earth from far away. It has recorded quakes in the Indian Ocean, which is much than 10,300 miles away from Meers. The seismograph has also recorded Russian nuclear tests, a natural gas explosion in Texas, and a mine accident in Michigan. The Meers Store became MEO - Meers Observatory and has proven to be one of the most sensitive stations in the country.

The Meers Fault is a profound structural dislocation that forms the frontal happy chance zone between the Wichita Uplift up to the south and the Anadarko handbasin to the north. The Meers crack is part of the Pennsylvanian Frontal Fault System. It stretches from the southeast to the northwestern United States through south central and southwest Oklahoma and into the Texas Panhandle.

The characteristics of the gaolbreak are very unusual for the Mid-Continental United States. A lucid fault trace is visible from near Saddle spile to Cache Creek for at least fifteen miles. many scientists had thinkd that the last major movement occurred during the Pennsylvanian person some tether snow million years ago. However, more recent studies demonstrate the time of the last major movement occurred five hundred to two thousand years ago.



The Meers Fault could produce a magnitude of seven on the Richter Scale in the future.

The fault is very special to Oklahomans because it is the only fault that has broken the bob up of the Earth east of the Rocky Mountains. Most people would believe that the fault belongs to California, where faults are very plentiful. Scientists believe that the fault whitethorn have been formed by a major earthquake many years ago which shook the ground so...

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