Fairview Peak (Churchill County, Nevada)
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Fairview Peak is a
summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for ...
in the
Clan Alpine Mountains The Clan Alpine Mountains are a mountain range located in west-central Nevada in the United States. The range lies in a southwest-northeasterly direction in Churchill County, and contains Mount Augusta, at above sea level. The mountains lie to ...
of the
U.S. state In the United States, a state is a constituent political entity, of which there are 50. Bound together in a political union, each state holds governmental jurisdiction over a separate and defined geographic territory where it shares its so ...
of
Nevada Nevada ( ; ) is a landlocked state in the Western United States. It borders Oregon to the northwest, Idaho to the northeast, California to the west, Arizona to the southeast, and Utah to the east. Nevada is the seventh-most extensive, th ...
. The elevation is . Fairview Peak was so named on account of the scenic views it affords. Variant names were "Fairview Cairn" and "Fairview Mountain". The ghost town of
Fairview, Nevada Fairview is a ghost town in Churchill County, Nevada, in the United States. History Discovery of silver in the area in 1905 led to several claims and the creation of a boom town in 1906. Some of the first mining claims were bought by George N ...
takes its name from the nearby peak.


1954 earthquakes

A very large
earthquake doublet __NOTOC__ In seismology, doublet earthquakes – and more generally, multiplet earthquakes – were originally identified as multiple earthquakes with nearly identical waveforms originating from the same Epicenter, location. They are now characteri ...
occurred on December 16, 1954. The Dixie Valley/Fairview earthquakes occurred four minutes apart, each with a maximum Mercalli intensity of X (''Extreme''). The initial shock measured 7.3 and the second shock measured 6.9 . Damage to man-made structures was minimal because the region was sparsely populated at the time, but oblique-slip motion on a normal fault resulted in the appearance of large
fault scarp A fault scarp is a small step-like offset of the ground surface in which one side of a fault has shifted vertically in relation to the other. The topographic expression of fault scarps results from the differential erosion of rocks of contrastin ...
s.


References

Mountains of Churchill County, Nevada {{ChurchillCountyNV-geo-stub