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Cold Springs, Washoe County, Nevada

Census-designated places in NevadaCensus-designated places in Washoe County, NevadaReno, NV Metropolitan Statistical AreaUse mdy dates from July 2023
Cold Springs in Winter
Cold Springs in Winter

Cold Springs is a census-designated place (CDP) in Washoe County, Nevada, United States. It is known as Eitse'ihpaa or Eitse'ippaa (literally "cold water" or "cold spring") in Shoshoni. It is located just off U.S. Route 395 in the northwestern part of the Reno–Sparks Metropolitan Statistical Area, adjacent to the California state line. The population was 8,544 at the 2010 census.

Excerpt from the Wikipedia article Cold Springs, Washoe County, Nevada (License: CC BY-SA 3.0, Authors, Images).

Cold Springs, Washoe County, Nevada
Cold Springs Drive,

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Geographical coordinates (GPS)

Latitude Longitude
N 39.676944444444 ° E -119.96777777778 °
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Address

Cold Springs Drive 17463
89508
Nevada, United States
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Cold Springs in Winter
Cold Springs in Winter
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Poeville, Nevada

Poeville, also known as Peavine until 1863, is the site of a historical mining town, established in 1864. John Poe, a professional promoter from Michigan allegedly related to Edgar Allan Poe, discovered rich gold and silver veins in 1862 on the slopes of Peavine Mountain. After the discovery of ore, Poe announced that the veins comprised the next Comstock Lode; he presented extracted ore at the state fair of 1864 as rich in content. As a result, the former mining camp, called Poe City (Poeville) or Podunk (Poedunk), grew to 200 people by 1864. Ore production in the mining district and population peaked around 1873-1874 with several hundred people living in town, supported by three hotels and a post office. The post office, named "Poeville", operated between September 1, 1874, and March 24, 1878.The smelting of the sulfide-rich ores with the primitive technology of the time directly at town was difficult, and also water resources were scarce. The situation improved in 1866, when the extracted ore was freighted to smelters by wagon to Cisco, California, and, after the completion of the Central Pacific Railroad, by rail to Sacramento, California. Income from the mines was low, for the extracted ore was rich not in gold, but in copper. Mining activity rapidly slowed, then ceased altogether in the late 1870s. By 1880, only 15 people remained in town. Nothing can be seen today of the former town. Several small mining claims were in operation near the town site since that time.

Swan Lake Nature Study Area
Swan Lake Nature Study Area

The Swan Lake Nature Study Area (formerly called Lemmon Valley Marsh) is a small conservation area in Lemmon Valley, Nevada. It contains marsh, alkali mud flats, and high desert. The Lahontan Audubon Society describes it as "a nearly unspoiled wetland in the midst of suburban housing and warehouses" and designates it a Nevada Important Bird Area. It is a notable location for birding; over 150 species have been observed there.The Swan Lake Nature Study Area consists of over 1,800 acres (7 km2) of land, with water supplied by the nearby Reno/Stead Sewage Treatment Plant. The size of the actual wetland varies seasonally and yearly, depending on the amount of precipitation, between 100 and 1,000 acres (4 km2). It was formally dedicated as a nature study area in 1999, following several years of planning by Reno-area environmentalist/writer/photographer Bob Goodman. The lead organization in planning and creating the conservation area was the Nevada Army National Guard, which contributed about 360 acres (1.5 km2) and performed preliminary ecological studies. Other sponsoring organizations include: the Bureau of Land Management; the City of Reno; the Lahontan Audubon Society; Nevada Division of Wildlife; the Nevada Land Conservancy; Washoe County Parks and Recreation Department; and Washoe County School District. Features include an observational boardwalk into the marsh and educational signs about the local ecology. Swan Lake is located in the midst of the rapidly developing suburbs of Stead and Lemmon Valley, near Peavine Peak north of Reno. According to a 1995 study, humans have lived in the area since as early as 400 AD; Native American artifacts attributed to the Washoe people have been found in the area, indicating it to have been a wintering site.

2008 Reno earthquakes

The Reno earthquakes of 2008, also known as the "Mogul-Somersett earthquake sequence", occurred in or near the western Reno, Nevada, suburbs of Mogul and Somersett. The earthquake swarm began in February 2008, but the first significant quake of the series occurred on April 15, 2008, registering a 3.6 magnitude. On April 24, 2008, two quakes in the same area registered 4.1 and 4.2. On April 25, 2008, the quake of largest magnitude occurred, registering 4.7 on the Richter scale and causing damage in the immediate area around the epicenter, including destroying 200 feet (61 m) of a wooden flume supplying water from the Highland Ditch, also known as the Highland Ditch flume. The flume carried up to 50 million US gallons (190,000 m3) a day from the Highland Ditch to Reno's Chalk Bluff Water Treatment Facility and another 5 million US gallons (19,000 m3) to area irrigation users. In addition to these significant quakes, hundreds of smaller events have also occurred in the same area. This swarm is significant because no known dominant fault line has been responsible for the earthquake swarm occurring in the region. It is also highly unusual because the quakes have, for the most part, been limited to a three-mile area. The United States Geological Survey (USGS) estimates that over 620 earthquakes have occurred in the general three mile vicinity since the swarm has been monitored. Seismologists with the USGS as well as the Nevada Seismological Laboratory expressed concern that the increasing magnitude of the felt quakes may indicate that a larger earthquake was imminent. As yet, they have not identified the particular tectonics involved with these earthquakes. However, they have stated categorically that volcanic activity is not involved. The last strong earthquake (M6.1) in the Reno area in occurred on April 24, 1914, and the state's most powerful quake to date was the M7.4 1915 Pleasant Valley earthquake south of Winnemucca.