Deschutes Valley Water District Water Company 💧 3date ALERT Drinking Water

Jefferson County, Oregon | Drinking Water Utility Company

The neighborhood drinking water in Deschutes Valley Water District may be polluted with many pollutants such as Tetrachloroethylene (perchloroethylene), m-Xylene and Carbofuran, and may struggle with rising scores of water hardness. Deschutes Valley Water District supplies the area with drinking water that sources its water from Groundwater.

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Deschutes Valley Water District Details

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Jefferson County, Oregon

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881 Sw Culver Hwy, Madras, OR 97741

Oregon Dinking Water Utility


Contaminants Detected In Jefferson County, Oregon

Chromium (hexavalent); Chromium (hexavalent); Strontium; Vanadium… more

Madras Dinking Water Utility

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Deschutes Valley Water District

Annual Drinking Water Report

List of Drinking Water Contaminants Tested by Deschutes Valley Water District

But Not Detected:
1,1,1-Trichloroethane; 1,1,2-Trichloroethane; 1,1-Dichloroethane; 1,1-Dichloroethylene; 1,2,3-Trichloropropane; 1,2,4-Trichlorobenzene; 1,2-Dibromo-3-chloropropane (DBCP); 1,2-Dichloroethane; 1,2-Dichloropropane; 1,3-Butadiene; 1,4-Dioxane; 2,4,5-TP (Silvex); 2,4-D; Alachlor (Lasso); Atrazine; Benzene; Benzo[a]pyrene; Bromochloromethane; Bromomethane; Carbofuran; Carbon tetrachloride; Chlorate; Chlordane; Chlorodifluoromethane; Chloromethane; cis-1,2-Dichloroethylene; Cobalt; Dalapon; Di(2-ethylhexyl) adipate; Di(2-ethylhexyl) phthalate; Dichloromethane (methylene chloride); Dinoseb; Diquat; Endothall; Endrin; Ethylbenzene; Ethylene dibromide; Glyphosate; Heptachlor; Heptachlor epoxide; Hexachlorobenzene (HCB); Hexachlorocyclopentadiene; Lindane; Methoxychlor; Molybdenum; Monochlorobenzene (chlorobenzene); Nitrate; o-Dichlorobenzene; Oxamyl (Vydate); p-Dichlorobenzene; Pentachlorophenol; Perfluorobutane sulfonate (PFBS); Perfluoroheptanoic acid (PFHPA); Perfluorohexane sulfonate (PFHXS); Perfluorononanoic acid (PFNA); Perfluorooctane sulfonate (PFOS); Perfluorooctanoic acid (PFOA); Picloram; Polychlorinated biphenyls (PCBs); Radium; combined (-226 & -228); Simazine; Styrene; Tetrachloroethylene (perchloroethylene); Toluene; Toxaphene; trans-1,2-Dichloroethylene; Trichloroethylene; Vinyl chloride; Xylenes (total)

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Deschutes Valley Water District

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Is my water-secure? We are pleased to record that our drinking water is secure and meets government and state requirements. The purity of your water is of their education that the Environmental Protection Agency (EPA) would not require Deschutes Pit Water District to try for every contaminant annually. A waiver approved by the Oregon Well being Division (OHD) in 1996, stipulated the frequency and factors to be tested. A year ago, we conducted checks for over 80 impurities. We only discovered 3 of those impurities, and one such was at a good higher than the ENVIRONMENTAL PROTECTION AGENCY allows. This record is a snapshot of last year's normal water quality. Included happening to be details about where the water comes from, what contains, and how that compares to standards place by regulatory firms. We are committed to giving you information because educated customers are each of our best allies. Should I take special safeguards? Some people may be weaker to contaminants in drinking water than the standard population. Immuno-compromised people such as persons with cancer undergoing radiation treatment, persons who have been through organ transplants, people who have HIV/AIDS or various other immune system disorders, several elderly, and newborns can be particularly in danger from infections. These folks should seek suggestions about drinking water off their health care providers. EPA/Centers to get Disease Control (CDC) guidelines on best-suited means to lessen the chance of infection by Cryptosporidium and other microbial impurities are available from the Secure Water Drinking Servicenummer (800-426-4791). Where does my water is derived from? The Opal Suspension systems aquifer supplies the home water for Deschutes Valley Water District's approximately 4, 95 services. The artesian spring is located a few miles Southwest of Culver at the bottom in the 850 foot profound Crooked River Gosier, less than 150 feet from the river. The artesian wells are situated on the East aspect of the canyon starting from 300 to six-hundred feet South of Opal Springs. Opal Springs flows roughly 108, 000 gallons per minute at 53. 8 degrees Fahrenheit (f) with no seasonal variant. There has been no noticeable change in flow, temp, or pH considering that the spring was first analyzed in 1925. Good # 1 is 750 feet profound and produces three or more, 750 gallons each minute. Well, #2 is 513 feet deep and produces a few, 360 gallons each minute. Well, #3 is 661 feet profound and produces some, 000 gallons each minute. It has been determined the fact that wells and Opal Springs are provided from the same aquifer. Source water examination and its availability Moving water, including bottled water, may reasonably be expected to contain at least small amounts of several contaminants. The presence of impurities does not necessarily reveal that water postures a health risk. More information about impurities and potential well-being effects can be obtained by simply calling the Environmental Security Agency's (EPA) A safe drinking water supply Hotline (800-426-4791). At present, there is no filtration or perhaps treatment of Opal Suspension systems of any kind (nor is any needed). Historic and continuous water quality research indicates an absence of man-made contaminants in the captured Opal Springs normal water. The source is well protected because it is a huge selection of feet below the area and under pressure. It truly is unlikely that impurities introduced in the area would reach the deep aquifer. The spring and boreholes have yet to demonstrate radiation from the WWII-era nuclear testing (1953) placing the age of the from Opal Suspension systems at 65 years of age minimum. According to “USGS Report 97-197” and “USGS Record 97-4233”, studies show age the water could be that you four thousand years of age. An analysis to get waterborne particulates reveals conclusively that Opal Springs is a surface water source, certainly not influenced by floor water. The hardness of water is due to the presence of magnesium and calcium. Excessive solidity is undesirable as it causes difficulties when you are performing laundry or cleaning dishes. Domestic normal water should have hardness below 85 mg/l. The District's water testing at 42 mg/l and is considered incredibly soft. The ph level of water is measured on a size of 1 to 13. A low reading will indicate acidic normal water (which is corrosive) while high browsing connotes basic normal water. Neutral water (neither acidic nor basic) would have browsing of 7. The District's pH tested for 7. 67 this means our water is a little basic. How could I get involved? If you have virtually any questions about this record or concerning the utility, please speak to our General Administrator at (541) 475-3849. We want our respected customers to be educated about their water energy. If you want to learn more, make sure you attend any of each our regularly scheduled Panel Meetings. They are placed on the second Wednesday of each month for 7: 00 PM HOURS at the District business office at 881 SW Culver Hwy, Écharpe, Oregon..

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Opal Springs was an enormous, freezing spring that left the gully in such incredible power that it made a "bubbling" impact. There was such a lot of water that it made up a fourth of the Crooked River now. "Found" by Orla Hale, it was named Opal Springs in view of the "opal-like" stones that appeared to bubble and rise out of the water. The "opals" from Opal Springs were really agates that were normally cleaned by the water disturbance. The spring was one of the show places of Central Oregon and guests never tired of dunking down into the spring with an extemporized, since quite a while ago poled scoop, raising the gem like stones. Numerous individuals had them made into ring sets, and numerous homes had a few containers of "opal" keepsakes after numerous excursions to Opal Springs. The water from Opal Springs was first used in 1898 by Mr. Windom, Jim McMeen, and G. Springer. Alongside a few other stockmen and ranchers in that community, they introduced a water haggle to raise the water to the main seat, a separation of around 500 feet and utilized it to water steers About 1913, Mr. Mill operator had a property of 40 sections of land at the highest point of the ravine, running over the feign on the Crooked River above Opal Springs. Mill operator put in a water smash and ran an authority trough from a few springs at the foot of the precipice, 40 to 50 feet over the stream. This water ran the water smash. Drinking water was in rare stockpile since much of the surface water was debased, causing Typhoid fever episodes. Numerous homesteaders obtained little tracts of land in the east lower regions, where they burrowed wells to sell and take water. In the Culver area, water was given by a well 1,000 foot down, delivering just 12 gallons for each moment. Seeing a requirement for local water, Earl Thompson, a designer, procured an estate on Opal Springs. He structured the Thompson Water Engine that would lift the unadulterated, cold water 850 feet to the ravine edge. Funnels were laid beginning at the ravine edge, hence the household water circumstance was survived and water was first conveyed through these channels to Culver on August 22, 1916. To oblige the 24 hour supervision and support of the office he procured Burr Larkin. In 1928, a house was worked at the springs for the family, living there until 1956. The main access to this siphoning plant and home was a single direction earth street to the primary seat. From that point you either strolled down a trail or street a link bushel to the base. The Larkin kids, a child Chester and a little girl left the ravine day by day to go to class in Culver. Lamentably on one outing out of the ravine, their girl tumbled to her demise from the link bin. In later years, Earl Thompson got down to business for General Motors Corporation. He planned the Synchromesh Transmission and an accuracy machine. As indicated by Chester Larkin, Thompson had guarantees on different springs on the Crooked River too. The encompassing ranchers framed "The Jefferson Water Company" in 1915. The Directors of the company were: W.H. Peck, William Barber, Fred Degner, William Boglie, Art Wright, and Mr. Cockeran. These men, with the assistance of different ranchers, at that point fabricated a 100,000 gallon store. The supply was a concrete square tub assembled party in the ground, with a wooden shingled roof. It was situated at the highest point of the gully on the Miller residence. Four miles of 8 inch wood, wire-wrapped funnels were laid past the Limbaugh and Evans residences into Culver and the encompassing ranches. This system gave fundamental drinking water and some nursery water. Potatoes and grain were as yet dry land crops at that point. Erwin Horney reviewed that 100 sacks for every section of land of dry land potatoes could be raised at the time. The water system for Metolius was spread out by a railroad engineer, being given by a railroad well 700 feet down. Afterward, Metolius would be provided by water from Opal Springs also. On February 11, 1919 the community shaped a non-profit organization – Deschutes Valley Water District, purchasing out the Jefferson Water Company. Thompson still claimed Opal Springs, despite the fact that he had moved from the area, offering water to these organizations under Opal Water Company. At the time Deschutes Valley Water District was framed, another supply was constructed east of Metolius, and east of what is currently Highway 97..

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Deschutes Valley Water District provides drinking water services to the public of Madras and Jefferson County, Oregon.

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