What does WVF mean in GEOLOGY
WVF stands for Washita Valley Fault, which is a major fault system located in the Washita Valley of Oklahoma. It is one of the most active fault systems in the United States and has been studied extensively by seismologists and geologists. The fault system consists of two branches, the Northeastern Branch and the Southern Branch, which are connected by a series of smaller faults. The WVF is known to produce earthquakes up to magnitude 7 on the Richter scale.
WVF meaning in Geology in Academic & Science
WVF mostly used in an acronym Geology in Category Academic & Science that means Washita Valley Fault
Shorthand: WVF,
Full Form: Washita Valley Fault
For more information of "Washita Valley Fault", see the section below.
What does WVF Stand for?
The full form of WVF is Washita Valley Fault. This is a major fault system in Oklahoma that has been studied extensively by seismologists and geologists. The fault consists of two branches, the Northeastern Branch and the Southern Branch, which are connected by a number of smaller faults. It is known to have produced earthquakes up to magnitude 7 on the Richter Scale.
Meaning in SCIENCE
In science, WVF stands for Washita Valley Fault, an active fault system found in Oklahoma in the United States. The fault consists of two branches, namely Northeastern Branch and Southern Branch which are connected by smaller associated faults. This active seismic zone has caused numerous quakes in its history with recorded magnitude up to 7 on the Richter Scale. Geologists and seismologists have conducted various studies into this area due to its high activity rate which could pose a risk to life if an earthquake were to strike nearby population centres.
Essential Questions and Answers on Washita Valley Fault in "SCIENCE»GEOLOGY"
What is the Washita Valley Fault?
The Washita Valley Fault (WVF) is a northeast-dipping reverse fault in Oklahoma that runs along the northern boundary of the Washita River Valley. This fault is considered to be part of the western boundary of the Ouachita Mountain fold belt, and it has been instrumental in creating the basins and canyons visible today.
How long is the Washita Valley Fault?
The length of the Washita Valley Fault runs for roughly 70 miles, beginning near Healdton in southern Oklahoma and extending to just north of McAlester.
What type of activity takes place at the Washita Valley Fault?
The activity associated with this fault includes seismic events such as earthquakes, as well as geyser eruptions erupting from underground pools or ponds caused by surface fracturing in acceptable areas.
How frequently does seismic activity occur on the Washita Valley Fault?
Seismic activity associated with this fault occurs at low frequency and magnitude, typically below M2 on the Richter scale.
Is there a danger to humans living near or on top of this fault line?
As seismic activity associated with WVF remains relatively low in magnitude, there is no immediate danger to humans residing near or above it. However, caution should still be taken when constructing buildings or structures on or across faults lines due to potential unknown hazards associated with geologic processes occurring beneath one's feet.
When was the last major earthquake experienced along this Fault Line?
The most recent major earthquake experienced along WVF was a M4.0 event that occurred in 2002 south of McAlester near Corbet Field Airport.
Are there any interesting geological features created by forces attributed to WVF?
Yes; several interesting geological features have been created by forces attributed to WVF including McCurtain County’s Caney Springs recreation area – an expansive sinkhole filled with crystal clear water accessed through a deep canyon walled by sandstone cliffs - as well as Poteau Mountain – an ancient ridge formed by multiple folds over time lifted its summit several hundred feet above its base.
Does research suggest evidence that indicates past seismic events along this fault line?
Yes; research conducted shows evidence indicating strong seismic events throughout history due to stresses under which many faults lay dormant until some sort of trigger triggers movement along them such as sudden changes in pressure or temperature.
Final Words:
In conclusion, WVF stands for Washita Valley Fault, an active seismic zone found in Oklahoma in the United States that has seen numerous earthquakes up to magnitude 7 occur along its length throughout history. Despite its location away from any large population centres it still represents a significant potential hazard due to its activity level and as such has been subject to extensive study by geologists and seismologists alike.
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