1986 Chalfant Valley earthquake

http://dbpedia.org/resource/1986_Chalfant_Valley_earthquake an entity of type: Thing

زلزال وادي شلفانت 1986 هو زلزالٌ وقعَ في كاليفورنيا في الولايات المتحدة بتاريخ 21 يوليو 1986. rdf:langString
The 1986 Chalfant Valley earthquake struck southern Mono County near Bishop and Chalfant, California at 07:42:28 Pacific Daylight Time on July 21. With a moment magnitude of 6.2 and a maximum Mercalli intensity of VI (Strong), the shock injured two people and caused property damage estimated at $2.7 million in the affected areas. There was a significant foreshock and aftershock sequence that included a few moderate events, and was the last in a series of three earthquakes that affected southern California and the northern Owens Valley in July 1986. rdf:langString
rdf:langString زلزال وادي شلفانت 1986
rdf:langString 1986 Chalfant Valley earthquake
xsd:float 37.54000091552734
xsd:float -118.4199981689453
xsd:integer 26453907
xsd:integer 1102596901
rdf:langString iscgem491308
xsd:gMonthDay --07-20
xsd:integer 2
rdf:langString United States
rdf:langString $2.7 million USD
xsd:date 1986-07-21
<second> 27748.0
xsd:double 6.2
xsd:date 1986-07-21
xsd:integer 1986
xsd:integer 491308
xsd:string 37.54 -118.42
<gram> 0.46
rdf:langString زلزال وادي شلفانت 1986 هو زلزالٌ وقعَ في كاليفورنيا في الولايات المتحدة بتاريخ 21 يوليو 1986.
rdf:langString The 1986 Chalfant Valley earthquake struck southern Mono County near Bishop and Chalfant, California at 07:42:28 Pacific Daylight Time on July 21. With a moment magnitude of 6.2 and a maximum Mercalli intensity of VI (Strong), the shock injured two people and caused property damage estimated at $2.7 million in the affected areas. There was a significant foreshock and aftershock sequence that included a few moderate events, and was the last in a series of three earthquakes that affected southern California and the northern Owens Valley in July 1986. Strong motion stations at the Long Valley Dam and an instrumented building in Bishop captured light to moderate readings from the event. The faulting reached the surface of the ground, but the maximum amount of measurable slip was limited to about 11 centimeters (4.3 in) of strike-slip motion along the White Mountain Fault Zone. Other destructive and surface-rupturing earthquakes, as well as large volume volcanic eruptions, have occurred in the area. Although the series of shocks occurred within the White Mountain seismic gap, the region continues to have potential for a very large earthquake.
xsd:nonNegativeInteger 19046
xsd:integer 2
<Geometry> POINT(-118.41999816895 37.540000915527)

data from the linked data cloud