1986 North Palm Springs earthquake, on which they migrated to Australia, arriving 9 February 1872. The present dam was first proposed in 1928 but was not built until 1954 by the Stanthorpe Shire Council. It had filled by February 1954. Following local government area amalgamations in 2008, the dam is currently operated by the Southern Downs Regional Council. It supplies water both to residents of Stanthorpe and to irrigators. In the 1980s, the Memorial School of Arts was relocated from Amiens to the dam to expand the recreation centre in the youth camp. It opened in Amiens in 1926. During drought periods, the dam has 	Storm King Dam
8595082	proved inadequate to meet the needs of the community it serves. In 2007, Storm King Dam was carrying as little as two months supply. In August 2019, the dam was almost dry and plans were being made to bring drinking water to the community by truck. The shire council delivered water by truck from approximately January 2020 to March 2021. Following heavy rain on the eastern seaboard in mid-late March 2021, the dam filled and started to spill. Amenities. Storm King Dam is available for recreational use, including fishing, water sports, bird watching and picnics. Fish in the dam 	Storm King Dam
8595083	include Murray cod, yellowbelly and silver perch. The lake attracts many water birds including pelicans. Barbeques and other picnic facilities are available. Boating is permitted on the lake, but motor boats require a permit. There is a boat ramp and jetty off Eukey Road (). It is managed by the Southern Downs Regional Council. Storm King Dam Storm King Dam is a reservoir created by the dam of the same name in the locality of Storm King in the Southern Downs Region, Queensland, Australia. It provides water for the town of Stanthorpe. Geography. Storm King Dam was created from Quart Pot 	Storm King Dam
8595084	1986 North Palm Springs earthquake 1986 North Palm Springs earthquake The 1986 North Palm Springs earthquake occurred on July 8 at with a moment magnitude of 6.0 and a maximum Mercalli Intensity of VII (Very strong"). The shock occurred in a complex setting along the San Andreas Fault Zone where it bisects San Gorgonio Mountain and San Jacinto Peak at the San Gorgonio Pass and was the first in a series of three earthquakes that affected southern California and the northern Owens Valley in July 1986. Numerous strong motion instruments recorded the event, one of which showed relatively high accelerations. Between 29 and 40 people  were injured, and financial losses were estimated to be in the range of $4.5 to 6 million. Preface. July 1986 was an unusually active month for moderate to strong earthquakes in California, with three events occurring in less than two weeks. Each had mild to moderate effects and began on July 8 with the event near Palm Springs. The second event was a M5.8 shock that occurred off the coast of Oceanside on July 13. While the earthquake off the southern California coast occurred in an area thought to be capable of generating a tsunami, the earthquake near Palm  Springs occurred on a portion of the southern San Andreas Fault system that has been designated a seismic gap and is a likely location for a very large future earthquake. The Chalfant Valley earthquake occurred on July 21 along the White Mountains Fault Zone near Bishop. Tectonic setting. The San Andreas Fault (SAF) spans nearly the length of California, where much of its length the fault is clearly identifiable, especially from San Francisco to near Cajon Pass. There, the fault splays into several branches. Several unusual characteristics are displayed further to the southeast in the area of the San Gorgonio  Pass. There are no lateral stream offsets (that are associated with strike-slip faulting) near the pass like there are along other segments (one researcher indicated that thrust faulting was the dominant type of fault displacement at the pass). There are no great earthquakes that are known to have occurred at the pass, where the main trace of the SAF is marked by numerous sag ponds and north-facing scarps. The Banning Fault lies about two miles to the south of these features. Earthquake. Early research indicated that the Banning Fault comprises three segments and that the nearly-parallel Garnet  Hill Fault lies just to the south. The epicenter of the July 8 earthquake was located in this convoluted area of faults between two segments of the Banning Fault and the Mission Creek strand of the San Andreas Fault, about northwest of where these two faults converge to form the Coachella Valley segment of the SAF. The focal mechanism (as defined by first motions) showed pure right-lateral strike-slip on a fault trending west-northwest that dipped to the north at 45°. As many of the aftershocks and previous events in the area showed oblique-reverse motion, researchers  did not exclude the possibility that the rupture started as horizontal motion, then transitioned into movement that included some vertical motion. Damage. In North Palm Springs, four homes and sixteen businesses were destroyed, and an additional 100 mobile homes and 100 businesses were damaged. In Whitewater Canyon, chimneys fell and three homes were destroyed, and ceramic columns were broken and a transformer was displaced at the Devers electrical substation. The Windy Point Bridge was displaced on the I-10 northwest of Palm Springs and was considered major damage. Other temporary roadway closures included State Route 111, which was closed until the  following evening, and State Route 74 and State Route 243 that were reopened later in the day. State Route 62, which crosses the Banning and Mission Creek Faults, was not immediately reopened due to buckled pavement. The California Aqueduct was damaged at several locations and water had to be diverted into a lake bed, and up to 80,000 people lost power for a portion of the day. Two fires in Riverside County caused serious damage, including a glass company that sustained $45,000 in damage, and several other brush fires. Strong motion. The shock was captured by strong motion stations  that were operated by the United States Geological Survey, the California Division of Mines and Geology and a private company. Altogether, the networks comprised about seventy-five stations, mainly including ground response stations, but also included seventeen buildings, nine dams, a power plant, and a freeway interchange. The stations were triggered at distances of up to , with a strong motion duration of greater than three seconds at five of the closest stations. The strongest acceleration (0.778 "g") occurred at the North Palm Springs Post Office on the vertical axis. Intensity. The maximum intensity for the event was VII ("Very strong ). At Desert Hot Springs, effects aligned with this rating were broken underground pipes (including a 5-inch water main) and filing cabinets that were knocked over at city hall. At the Devers substation near North Palm Springs, 75% of the ceramic lightning arrestors and circuit breakers were damaged, and a 650,000 lb. transformer was dislocated 10 inches. A building collapsed at a drug and alcohol recovery facility and the White Water overpass was damaged due to lateral movement at its south abutment in Palm Springs. Broken glass and cracks in walls and concrete columns (some severe) were also widespread there	1986 North Palm Springs earthquake
8595093	. Intensity VI (Strong") effects were widespread, from La Jolla and Pacific Beach area near San Diego to Seal Beach in the Los Angeles area that were deemed to qualify. The effects at this level included cracked walls and windows and small landslides, and were more prevalent in the Banning Pass and Coachella Valley areas. The area of perceptibility for the mainshock was large (130,500 km), from Malibu and Ridgecrest in California, to Bullhead City and Yuma in Arizona, and Las Vegas in southern Nevada. 1986 North Palm Springs earthquake The 1986 North Palm Springs earthquake occurred on July 8 at