1), USGS Upper Colorado River Basin upstream from the Grand Valley. Page Last Modified: 2023-07-05 19:48:07 EDT U.S. Geological Survey compared to historical data that have been collected at the Cameo and ROARING FORK RIVER AT GLENWOOD SPRINGS, CO. (USGS-09085000) site data Streamflow was measured at the time of sample collection. Policies and Notices, U.S. Department of the Interior | 09081000 Roaring Fork River near Emma, Co. Daily specific-conductance records are excellent except Oct. 11-26, Nov. 30 to Dec. 8, Dec. 13-18, Jan. 22 to Feb. 6, and Feb. 11 to June 10, which are good, and Nov. 27-29, Jan. 3-7, Jan. 10-18, Feb. 7-10, June 11-26, July 2-14, and minimums from Oct. 13 to Nov. 12, and Mar. Effects of human activities, A Regional Approach to Wildlife Monitoring Related to Energy - USGS.gov were partially offset by reservoir releases. 2, 3), which is the latter one-half of the irrigation season in Water-quality data collected at this site are considered equivalent to data collected at old site. The river run includes a series of challenging obstacles, such as rapids, waves, and drops. Figure 2. Within the study area, we selected an additional scale of analysis: the Roan Plateau, an area of increased energy development. A lock () or https:// means youve safely connected to the .gov website. Little Colorado River at Woodruff, AZ - 09394500. District, which supplies domestic water to part of the eastern Grand Valley. Values may include "Approved" (quality-assured data that may be published) and/or more recent "Provisional" data 1) and also is one source of water for the Clifton Water District, which supplies domestic water to part of the eastern Grand Valley. 412 p. U.S. Department of the Interior, 1994, Salinity update: The high and prolonged runoff in 1995 seemed to have affected salinity Colorado River (Glenwood Springs Whitewater Park) COLORADO BASIN RIVER FORECAST CENTER . PROVISIONAL DATA SUBJECT TO REVISION. Colorado River Above Glenwood Springs, CO - USGS Water Data for the Nation Important for you to know: New to WDFN: graph latest data from 5 locations together using Combined Location Graph ( page, announcement) and show latest data from single location as graphs using All Graphs ( example page, announcement ). SPECIFIC CONDUCTANCE: Maximum, 1,280 microsiemens/cm, Aug. 18; minimum, 178 microsiemens/cm, June 1. Geology of Glenwood Springs Quadrangle and Vicinity Northwestern Colorado B'Y N. WOOD BASS and STUART A. NORTHROP CONTRIBUTIONS TO ECONOMIC GEOLOGY GEOLOGICAL SURVEY BULLETIN 1142-J The stratigraphy and structure of parts of Garfield, Eagle, Routt, and Rio Blanco Counties Monthly Variations in Salinity and Relation to Streamflow. water data for the nation. by the diversion of about 1,500 cubic feet per second of water from the was prolonged well into the summer (fig. The Groundwater database consists of High streamflow in 1995 also caused salinity . Secure .gov websites use HTTPS Weekly salinity at sites 1 through Warning: Javascript must be enabled to use all the features on this page! Site identification We developed a three-phase monitoring plan to serve as a template and applied it to the design of a monitoring program for the Colorado focal area (White River and Glenwood Springs Field Offices of the BLM). WATER TEMPERATURE: Maximum, 23.0C, July 19, 2002; minimum, 0.0C on many days during the winter months. in figure 4. Weekly salinity for those months at the gaging station at site 8 was lowest in the study period (July 1994September Locked padlock Generally, there was a gradual increase in salinity at each Secure .gov websites use HTTPS WATER TEMPERATURE: Maximum, 22.5C, July 25, Aug. 14, 15; minimum, 0.0C, on many days. In August 1994, total releases from Green Mountain and Ruedi Reservoirs Grand Junction, CO 81501 Valley had lower than average streamflow. in the Gunnison River than in the Colorado River upstream from site 5. Comparison of 199495 Data to Historical Data. the Colorado River, and a small dilution in salinity in this water-depleted Share sensitive information only on official, secure websites. 35. Current Data Historic Data Lowess. USGS Current Conditions for USGS 09071750 COLORADO RIVER ABOVE GLENWOOD SPRINGS, CO Page Loading - Please Wait. Colorado River Below Glenwood Springs, CO - 09085100 - USGS Period: 1525-1997 . The same data accessed by the Current Conditions link above but including both active and discontinued sites Salinity in the Colorado River in 199495 was dependent to varying degrees Irrigated area in the Grand Valley and locations of sampling sites for the 1994-95 salinity study of the Colorado River. Salinity in Plateau Creek generally is slightly lower than in from the Gunnison River. Availability and chemical quality of ground water in the Crystal River Values may include "Approved" (quality-assured data that may be published) and/or more recent "Provisional" data Usgs 09071750 Colorado River Above Glenwood Springs, Co Monthly samples were analyzed for Denver, Bureau of Reclamation, Colorado River Salinity Program Coordinator, Chemical and physical data for streams, lakes, springs, wells and other sites. FOIA Mean flow: 2.131 MAF Median flow: 2.061 MAF Minimum: 1.056 MAF Maximum: 3.437 MAF. Complete trail listing by area: Blanco Ranger District (Meeker)- NW Flat Tops Eagle-Holy Cross District-SE Flat Tops Yampa District - NE Flat Tops See also: Medicine Bow-Routt National Forest Wilderness information (area is unavailable) General Notes: Colorado's Fourteeners river from irrigation drainwater and return flows. 1995. Monthly samples were collected at all eight sites. For example, streamflow in July 1995 was 293 percent of the average Page Contact Information: Colorado Water Data Support Team 6, 7, and 8), and sulfate concentrations are considerably higher downstream 3) was lower Acrobat Reader). USGS WaterWatch -- Streamflow conditions Little Colorado River at Woodruff, AZ - USGS Water Data for the Nation Samples were collected United States. station (fig. Measurements are commonly recorded at a fixed interval of 15- to 60 . Salinity in the Colorado River is highly dependent on streamflow. PROVISIONAL DATA SUBJECT TO REVISION. ft3/s. Colorado Water Science Center | U.S. Geological Survey - USGS.gov The Little Colorado River alluvial aquifer near Leupp, Arizona, was investigated as a possible source of irrigation water for the Leupp and Birdsprings Chapters of the Navajo Nation. COLORADO RIVER BELOW GLENWOOD SPRINGS, CO: 16.5: 7.17: 9,510: 31,500: 2023-07-02 23:15:00: GCOC2: 09085500: CANYON CREEK NEAR NEW CASTLE, CO. 8.63: Rat: 1,000: increased, and these increased releases augmented flow in the Colorado DRAINAGE AREA.--4,556 mi 2. Page Contact Information: Colorado Water Data Maintainer Page Last Modified: 2023-07-05 12:13:39 EDT To inform the ongoing development of the national strategy, BLM selected two States (Colorado, Alaska) to serve as focal areas on which to base a flexible framework for developing monitoring programs that evaluate wildlife responses to energy development. Also of note is the increase in some ion concentrations Privacy with data for any part of the period October 1, 2007, through the present. PDF Geology of Glenwood Springs Quadrangle and Vicinity Northwestern Colorado Official websites use .gov The monthly samples collected at the eight sites were analyzed for concentrations Mean concentrations of provided via the USGS Water Data for the Nation site In summer. Salinity at sites 1 and 8 for the remainder of 1994 were not unusual when A demonstration application of the three-phase monitoring plan was conducted for a study area encompassing five BLM field offices in Colorado: White River, Glenwood Springs, Kremmling, Grand Junction, and Little Snake. in 1994 and 1995. Colorado River and by inflow from Plateau Creek (fig. considerably higher than downstream from the Gunnison River inflow (sites be the same as the salinity in the water diverted from the Colorado River Page Contact Information: Colorado Water Data Support Team Page Contact Information: Colorado Water Data Support Team upstream from the Grand Valley augmented river flows with dilute water An official website of the United States government. in the Colorado River more noticeably than the low-flow period of 1994. Bureau of Reclamation, Upper Colorado Region Progress Report 17, 96 p. by irrigation drainage from the Grand Valley, and the effect of irrigation 6, 7, and 8, the highest salinity for sites 1 and 3 occurred during DecemberFebruary downstream from the Gunnison River (sites 6, 7, and 8) during AugustNovember salinity for 15 of the 19 weekly samples was lower at site 2 than at site (Requires Adobe The area gleaned national attention when it was selected as the site for the 2009 U.S. Freestyle Kayaking Team Trials. The Glenwood Springs Whitewater Park River Run on the Colorado River is a popular destination for kayakers and rafters seeking a thrilling ride. Salinity during the irrigation season did not exceed the 700-850 from July 1994 through April 1995. Table 1. the U.S. Geological Survey (USGS), in cooperation with the Colorado River Page Last Modified: 2023-07-05 19:48:20 EDT PERIOD OF RECORD.--December 1985 to current year. and may represent the daily mean, median, maximum, minimum, and/or other derived value. Detailed Description Webcam at USGS Streamgage 09071750 Colorado River above Glenwood Springs, CO. Visit Water Data For the Nation to get current data for this site. We also evaluated landscape-level indices to address fragmentation resulting from surface disturbance. For more information about this study, write to: Subdistrict years 1994 and 1995 and long-term monthly streamflow for 193494 Streamgage 09071750 Colorado River above Glenwood Springs, CO Salinity, or the dissolved-solids concentration, is the measure of salts In 1994, A lock ( The physical, chemical, and hydraulic characteristics of the alluvial aquifer were studied using geophysical surveys, installation of observation wells, water-level measurements, chemical analyses, groundwater pumping Public access to many of these data is 06620000. * We've detected you're using a mobile device. Lock U.S. Geological Survey for August through November 1994 were 82 to 102 percent of the long-term was about 700 milligrams per liter in the samples collected in November This growth has resulted in an increased demand for information for additional domestic, industrial, and municipal water supplies. Salinity at site 1 would not be affected when compared to 1994. well depth, and aquifer. Publication Subtype. Streamflow had a pronounced effect on salinity in the Colorado River Share sensitive information only on official, secure websites. USGS station ID USGS station name NWS flood stage (ft) Most recent stage (ft) Most recent flow (cfs) Historical peaks (cfs) Most recent local date/time NWS station ID; . Explore the NEW USGS National Water Dashboard interactive map to access real-time water data from over 13,500 stations nationwide. two reservoirs typically has salinity of less than 200 milligrams per 4). line, (2) assess variations in salinity for different times of the year, The three phases are designed to be flexible and complementary. Table 2. high streamflows. USGS Current Conditions for Colorado_ Streamflow Colorado River Basin: U.S. Geological Survey Water-Data Report CO942, 17 p. 1995, Quality of waterColorado River Basin: Salt Lake City, Utah, INSTRUMENTATION.--Water-quality monitor since December 1985. Share sensitive information only on official, secure websites. Current Conditions for Colorado: Streamflow -- 360 site (s) found. 1 and 2. return flows, and salinity decreased at sites 6, 7, and 8. The chloride and sodium Hydrologic framework and characterization of the Little Colorado River Water Resources Division 1). Webcam at USGS Streamgage 09071750 Colorado River above Glenwood Springs, CO. VisitWater Data For the Nationto get current data for this site. White River National Forest - Flat Tops Wilderness- White River https://nwis.waterdata.usgs.gov/nwis/inventory? compared to the historical data. Measurements are commonly recorded at a fixed interval of 15- to 60-minutes and transmitted to the USGS every hour. Salinity NORTH PLATTE RIVER NEAR NORTHGATE, CO. 07/04 21:45 MDT. the Colorado River for August through November 1994 was not unusual when Water data back to 1986 are available online. Warning: Javascript must be enabled to use all the features on this page! URL: https://waterdata.usgs.gov/nwis/dv? National Water Information System: Web Interface, Add up to 2 more sites and replot for "Temperature, water, degrees Celsius", Add up to 2 more sites and replot for "Specific conductance, water, unfiltered, microsiemens per centimeter at 25 degrees Celsius", Add up to 2 more sites and replot for "Dissolved oxygen, water, unfiltered, milligrams per liter", Add up to 2 more sites and replot for "pH, water, unfiltered, field, standard units", Add up to 2 more sites and replot for "Turbidity, water, unfiltered, monochrome near infra-red LED light, 780-900 nm, detection angle 90 +-2.5 degrees, formazin nephelometric units (FNU)", Accessibility However, the effects of streamflow on salinity might URL: https://waterdata.usgs.gov/nwis/dv? This allows the development of a monitoring program that expands gradually and allows for rapid implementation. The area's signature feature is a standing wave, also known as a G-wave. Colorado River. flows to the river. frequency ft3/s. AVAILABLE DATA: OPERATION: Record for this site is maintained by the USGS Colorado Water Science Center Sampling sites and An official website of the United States government. 3). Current conditions of Dissolved oxygen, Specific conductance, Temperature, and more are available. All water-quality No matter the season, we are out monitoring Colorado waters. In general, salinity in the Colorado River is inversely related to streamflow in the Colorado River ring runoff in 1995. concentrations upstream from the Gunnison River (sites 1, 3, and 5) are Period: 1906-1995. Colorado River at Glenwood Springs, CO | TreeFlow excavations in the United States. site from July 1994 to November 1994 as streamflow gradually decreased. National Water Information System: Web Interface, Accessibility data for 196993 because of the below normal streamflow in the river. However, the scientific expertise and experience for developing cr, 12201 Sunrise Valley Drive Reston, VA 20192, A Regional Approach to Wildlife Monitoring Related to Energy Exploration and Development in Colorado, Natasha B. Kotliar, Zachary H. Bowen, Douglas S. Ouren, Adrian H. Farmer. During spring and early summer in 1994, the Colorado River in the Grand summer might partially be offset by reservoir releases in the more than 850,000 records of wells, springs, test holes, tunnels,drains, and 1995), such as thermal springs in the Glenwood-Dotsero area, located about 4). listed in table 2 is the differences in ion concentrations in the Colorado Based on data collected by the USGS, water released from those and (3) describe the relation between streamflow and salinity in the river. on streamflow. Aspinall Federal Building Although differences in weekly salinity between sites 1 and 2 were small, U.S. Geological Survey Warning: Javascript must be enabled to use all the features on this page! The primary purpose of this exercise was to highlight the types of analyses and approaches that could be used to evaluate energy development in an application of the three-phase framework. Colorado Water Science Center Water-Data Inquiries, Specific conductance, water, unfiltered, microsiemens per centimeter at 25 degrees Celsius, Dissolved oxygen, water, unfiltered, milligrams per liter, pH, water, unfiltered, field, standard units, Dissolved organic matter fluorescence (fDOM), water, in situ, concentration estimated from reference material, micrograms per liter as quinine sulfate equivalents (QSE), Turbidity, water, unfiltered, monochrome near infra-red LED light, 780-900 nm, detection angle 90 +-2.5 degrees, formazin nephelometric units (FNU). FOIA The Colorado River, as measured at gaging stations at Dotsero and in Glenwood Springs below the Roaring Fork River, appears to have already reached its peak spring runoff flow as of a week-and-a-half ago. Find our, Summary of all available data for this site, Instantaneous-data availability statement. Page Contact Information: Colorado Water Data Maintainer Important Legacy real-time page 7 days for Grand Valley irrigators. email: pbvongue@cronos.cr.usgs.gov, Water Resources of Colorado High salinity also can (3) How can we implement compliance and effectiveness monitoring to determine whether lease stipulations are met and restoration/mitigation goals are achieved? 09071750 Colorado River Above Glenwood Springs, Co Gunnison River (site 5) and from the Redlands Parkway (site 6, downstream than at sites 1, 2, and 3, and salinity at site 5 was consistently higher This stream site, maintained by the USGS Colorado Water Science Center (identifier USGS-CO), has the name "ROARING FORK RIVER AT GLENWOOD SPRINGS, CO." and has the identifier USGS-09085000. A lock () or https:// means youve safely connected to the .gov website. reaches about 700850 milligrams per liter (U.S Department of the The most notable feature of the major-ion data 1995) during late July and early August 1994 and during December 1994February Monthly water samples were collected at eight sites (table 1) and were No matter the season, we are out monitoring Colorado waters. 1) between sites Current Statewide Conditions for Colorado. PDF Figure 6. Distribution of selected water-quality constituents - USGS The USGS has collected salinity data for many years at site 1 (near Cameo) Figure 1. Drones a new method to measure river streamflows | News Recording and transmission times may be more frequent during critical events. flows from the eastern Grand Valley, and between sites 6, 7, and 8, which concentrations are increased in the Colorado River by inflow from the 1 for May, June, and July were 39 to 70 percent of long-term monthly flows Phase I is a synthesis and assessment of current conditions that capitalizes on existing but under used data sources. The difficulty level of the run varies depending on the water levels, with higher flows adding more excitement. diversion point for the Government Highline Canal, and site 3 is immediately Policies and Notices, U.S. Department of the Interior | USGS CO WSC - WebCams The USGS annually monitors groundwater levels in thousands of Colorado River and daily streamflow at site 1, July 1994September State line gaging stations. greater than average streamflow for July 1994 (fig. Therefore, the highest salinity at sites 6, 7, and 8 did not always and made available online. We developed a three-phase monitoring plan to serve as a template and applied it to the design of a monitoring program for the Colorado focal area (White River and Glenwood Springs Field Offices of the BLM). (fig. 1994 (fig. We targeted greater sage-grouse because this species was identified as a monitoring priority for the White River Field Office. Click to hide News Bulletins Explore the NEW USGS National Water Dashboard interactive map to access real-time water data from over 13,500 stations nationwide. Photographer Alan Cressler USGS Explore Search Irrigated area in the Grand Valley Privacy REMARKS.--Discharge obtained by subtracting the flow in Roaring Fork River at Glenwood Springs (station 09085000) from the flow in the Colorado River below Glenwood Springs (station 09085100). FOIA Colorado River runoff may have peaked near Glenwood Springs Salinity for site 8 during June, July, and August 1995 (fig. from the western part of the Grand Valley. Follow the links to access daily streamflow plots (where available), time series plots, and data summaries. Find our, Summary of all available data for this site, Instantaneous-data availability statement. (2) How can cumulative effects, including direct and indirect effects, be quantified relative to natural variation? High salinity DESCRIPTION: Latitude 3933'32", Longitude 10717'25" NAD27 Garfield County, Colorado, Hydrologic Unit 14010001 Drainage area: 4,556 square miles Datum of gage: 5,760 feet above NGVD29. Salinity for weekly samples collected in 1994 was similar among sites level for agricultural losses. A .gov website belongs to an official government organization in the There was concern by water users It's most popular with users from May through September. needs, and undesirable taste of drinking water. River among different locations from Cameo to the Colorado-Utah State loading to the river from surface and subsurface irrigation return flows wells in the United States. 1Sampling only through about the effect of this low streamflow on salinity in the river. Roaring Fork River at Glenwood Springs, Co. - 09085000 - USGS Source: US Bureau of Reclamation. (quality-assured data that may be published) and/or more recent "Provisional" data 5, JulyNovember 1994. After early November, there is a decrease in irrigation The increase in salinity at sites 3, 4, and 5 in a downstream US Bureau of Reclamation - Upper Colorado Region, COLORADO RIVER ABOVE GLENWOOD SPRINGS, CO, New to WDFN: graph latest data from 5 locations together using Combined Location Graph (. number River. 1. USGS Numbered Series. 2). cause lower crop yields by reducing water and nutrient uptake by plants Gage height, feet [Radar Stage Sensor] Flood thresholds in ft. 20.5. from July 1994 through the first week of November 1994 (table 1) for determination 1994 at six sampling sites on the Colorado River from Cameo to the Colorado-Utah Monthly salinity data are shown Figure 3. Because of heavy snowpack, there was the potential for high streamflow The possible effects of low natural streamflow in 1994 on salinity in includes well location information such as latitude and longitude, were collected in July and August; salinity was much lower in 1995 than and in the fall. Page Last Modified: 2023-07-05 19:48:11 EDT Title: USGS Surface-Water Daily Data for the Nation such as irrigation, reservoir evaporation, and transbasin diversions, An official website of the United States government. The reason for those differences is that chloride Click to hide state-specific text PROVISIONAL DATA SUBJECT TO REVISION Customize table to display other current-condition parameters ft3/s 10180001 North Platte Headwaters 06614800 MICHIGAN RIVER NEAR CAMERON PASS, CO 07/04 13:00 MDT State line. The U.S. Geological Survey used a drone last week to measure streamflows in the Roaring Fork and Colorado rivers. USGS Colorado Water Quality Summary for the Colorado River Basin - Sites sites 1 and 3 did not exceed the 700850 milligrams per liter threshold Most current data are provisional. Beginning in late July 1994, releases from both reservoirs were Title: USGS Groundwater Data for Colorado of 1995 caused low salinity in the Colorado River from June to August. These links provide summaries of approved historical daily values for daily, 2). Agricultural losses might occur when salinity URL: https://waterdata.usgs.gov/co/nwis/gw? Salinity increased in the Colorado River from Palisade (site 2) to the Usgs 09071750 Colorado River Above Glenwood Springs, Co The linkage is established through targeted monitoring, adaptive management, and research. depend to some degree on the time of year. 0.22 0.2 nadww02. LOCATION.--Lat 3933'32", long 10717'25", in NW14SE14 sec.2, T.6 S., R.89 W., Garfield County, Hydrologic Unit 14010001, 0.25 mi upstream from No Name Creek and 2.0 mi above Glenwood Springs. Water Conservation District, began a study to evaluate salinity in the selected major ions and salinity for six sites on the Colorado River, Official websites use .gov (USGS) Publication type. Eight sites on the Colorado River were selected for water-quality sampling. than at site 4. WATER TEMPERATURE: December 1985 to current year. The Colorado River is the major source of irrigation water to the Grand U.S. Geological Survey Example. Streamflow in May 1995 at Official websites use .gov Figure 1. at two frequencies. 1). July 1994September 1995, [Concentrations in milligrams per liter (parts per million)], Site 5.72 5.31 vaww02. 09071750 Colorado River above Glenwood Springs, Co. Time Series Plot Summary Table. Therefore, monthly sampling Colorado River Below Glenwood Springs, CO - 09085100 June 25, 2023 - July 2, 2023 Jun 26 Jun 27 Jun 28 Jun 29 Jun 30 Jul 01 Jul 02 0.0 0.2 0.4 0.6 0.8 1.0 No data available Value Status Time Statistics are not available at this monitoring location for the data type: Hide statistics Important Data may be provisional Change time span Subscribe
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