Prepared in cooperation with White Sands Missile Range

Compilation of Hydrologic Data for White Sands Habitat and Nonhabitat Areas, Northern Tularosa Basin, White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008

Data Series 810

U.S. Department of the Interior U.S. Geological Survey

Compilation of Hydrologic Data for Habitat and Nonhabitat Areas, Northern Tularosa Basin, White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008

By C.A. Naus, R.G. Myers, D.K. Saleh, and N.C. Myers

Prepared in cooperation with White Sands Missile Range

Data Series 810

U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director

U.S. Geological Survey, Reston, Virginia: 2014

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Suggested citation: Naus, C.A., Myers, R.G., Saleh, D.K., and Myers, N.C., 2014, Compilation of hydrologic data for White Sands pupfish habitat and nonhabitat areas, northern Tularosa Basin, White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008: U.S. Geological Survey Data Series 810, 35 p., http://dx.doi.org/10.3133/ds810.

ISSN 2327-638X (online) iii

Contents

Abstract ...... 1 Introduction ...... 1 Purpose and Scope ...... 3 Site-Numbering Systems ...... 3 Acknowledgments ...... 8 Description of Study Area ...... 8 White Sands Pupfish Habitat ...... 12 Hydrologic Data ...... 13 Quality Assurance and Quality Control ...... 13 Salt Creek ...... 17 Malpais Spring and Malpais Salt Marsh ...... 26 Main Mound Spring ...... 31 Lost River ...... 31 Sites Located in Pupfish Nonhabitat Areas ...... 31 Summary ...... 32 References ...... 33 Appendixes (available at http://pubs.usgs.gov/ds/810/) 1. Photographs of Pupfish Habitat Areas Within the Tularosa Basin, New Mexico 2. Hydrologic Data Compiled for 67 Sites Located in the Northern Tularosa Basin, New Mexico, on White Sands Missile Range and Holloman Air Force Base

Figures

1. Map showing location of study area in White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 2 2. Diagram showing system for identifying site locations according to the Public Land Survey system of subdivision of sectionized land in New Mexico ...... 8 3. Map showing locations of White Sands pupfish habitat areas and sites in and near pupfish habitat areas, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 9 4. Map showing locations of sites in the White Sands pupfish Malpais Spring and Malpais Salt Marsh, Main Mound Spring, and northern Salt Creek habitat areas and surrounding areas, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 10 5. Map showing locations of sites in the White Sands pupfish southern Salt Creek and Lost River habitat areas and surrounding areas, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 11 6. Stiff diagrams showing major-ion chemistry (averaged for sites with more than one sample) of water samples collected from sites in White Sands pupfish habitat and nonhabitat areas, 1983–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 14 7. Piper diagram showing major-ion chemistry of water samples collected from sites in the White Sands pupfish Salt Creek habitat area, 1983–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 15 iv

8. Piper diagram showing major-ion chemistry of water samples collected from sites in the White Sands pupfish Malpais Spring and Malpais Salt Marsh habitat area, 1982–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 15 9. Piper diagram showing major-ion chemistry of water samples collected from sites in the White Sands pupfish Main Mound Spring and Lost River habitat areas, 1982–2006, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 16 10. Piper diagram showing major-ion chemistry of water samples collected from sites in White Sands pupfish nonhabitat areas, 1954–2006, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 16 11. Piper diagram showing major-ion chemistry of water samples collected from White Sands pupfish habitat and nonhabitat areas, 1954–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico ...... 17 12. Graphs showing daily mean streamflow at U.S. Geological Survey streamflow- gaging station Salt Creek near Tularosa, New Mexico, for water years 1995–2008...... 18 13. Graph showing daily mean and instantaneous streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico, calendar years 1995–2008 ...... 23 14. Graphs showing instantaneous streamflow, dissolved-solids concentration, and pH at Salt Creek surface-water sites ...... 24 15. Graph showing dissolved-solids concentrations and streamflow during a seepage (gain-loss) study along a 24.5-mile reach of Salt Creek, New Mexico, August 12–13, 2002 ...... 26 16. Graphs showing daily mean streamflow at U.S. Geological Survey streamflow- gaging station Malpais Spring near Oscura, New Mexico, for water years 2004–8 ...... 27 17. Graph showing daily mean and instantaneous streamflow at U.S. Geological Survey streamflow-gaging station Malpais Spring near Oscura, New Mexico, calendar years 2003–8 ...... 29

Tables

1. Site names and descriptions, identification numbers, locations, and land-surface altitudes of water-sampling sites on White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008 ...... 4 2. Water types of samples collected from sites on White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008 ...... 30 v

Conversion Factors, Datums, and Abbreviations

Inch/Pound to SI

Multiply By To obtain Length inch (in.) 2.54 centimeter (cm) inch (in.) 25.4 millimeter (mm) foot (ft) 0.3048 meter (m) mile (mi) 1.609 kilometer (km) Area acre 0.004047 square kilometer (km2) square mile (mi2) 2.590 square kilometer (km2) Volume acre-foot (acre-ft) 1,233 cubic meter (m3) Flow rate cubic foot per second (ft3/s) 0.02832 cubic meter per second (m3/s) gallon per minute (gal/min) 0.06309 liter per second (L/s)

SI to Inch/Pound

Multiply By To obtain Length meter (m) 3.281 foot (ft) Area square kilometer (km2) 247.1 acre Mass gram (g) 0.03527 ounce, avoirdupois (oz)

Temperature in degrees Celsius (°C) may be converted to degrees Fahrenheit (°F) as follows: °F=(1.8×°C)+32 Vertical coordinate information is referenced to the North American Vertical Datum of 1988 (NAVD 88). Horizontal coordinate information is referenced to the North American Datum of 1983 (NAD 83). Altitude, as used in this report, refers to distance above the vertical datum. Concentrations of chemical constituents in water are given in either milligrams per liter (mg/L) or micrograms per liter (µg/L).

Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin, White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008

By C.A. Naus, R.G. Myers, D.K. Saleh, and N.C. Myers

Abstract Main Mound Spring water sample collected in 1982 indicated that the water was about 19,600 years old. Dissolved-solids concentrations of Lost River samples The White Sands pupfish Cyprinodon( tularosa), listed collected from 1984 to 1999 ranged from 8,930 to 118,000 as threatened by the State of New Mexico and as a Federal (estimated) mg/L. species of concern, is endemic to the Tularosa Basin, New Dissolved-solids concentrations in samples from Mexico. Because water quality can affect pupfish and the nonhabitat area sites ranged from 1,740 to 54,200 (estimated) environmental conditions of their habitat, a comprehensive mg/L. In general, water collected from pupfish nonhabitat compilation of hydrologic data for pupfish habitat and area sites tends to have larger proportions of calcium, nonhabitat areas in the northern Tularosa Basin was magnesium, and sulfate than water from pupfish habitat area undertaken by the U.S. Geological Survey in cooperation with sites. Water from springs associated with mounds in pupfish White Sands Missile Range. nonhabitat areas was of a similar type (calcium-sulfate) to The four locations within the Tularosa Basin that are water associated with mounds in pupfish habitat areas. Alkali known pupfish habitat areas are the Salt Creek, Malpais Spring had a sodium-chloride water type, but the proportions Spring and Malpais Salt Marsh, Main Mound Spring, and Lost of sodium-chloride and magnesium-sulfate are unique as River habitat areas. Streamflow data from the Salt Creek near compared to samples from other sites. Tularosa streamflow-gaging station indicated that the average annual mean streamflow and average annual total streamflow for water years 1995–2008 were 1.35 cubic feet per second Introduction (ft3/s) and 983 acre-feet, respectively. Periods of no flow were observed in water years 2002 through 2006. Dissolved-solids The White Sands pupfish Cyprinodon( tularosa) is the concentrations in Salt Creek samples collected from 1911 only endemic fish species of the Tularosa Basin in south- through 2007 ranged from 2,290 to 66,700 milligrams per central New Mexico (fig. 1). The species is listed as threatened liter (mg/L). by the State of New Mexico (19 NMAC 33.1) and as a Federal The average annual mean streamflow and average species of concern (50CFR 17:64481-64485) (Pittenger and annual total streamflow at the Malpais Spring near Oscura Springer, 1999). A cooperative agreement among White streamflow-gaging station for water years 2003–8 were Sands Missile Range, Holloman Air Force Base, New Mexico 6.81 ft3/s and 584 acre-feet, respectively. Dissolved-solids Department of Game and Fish, U.S. Fish and Wildlife Service, concentrations for 16 Malpais Spring samples ranged from and White Sands National Monument was signed in 1994 3,882 to 5,500 mg/L. Isotopic data for a Malpais Spring near (Pittenger and Springer, 1996) to establish an interagency Oscura water sample collected in 1982 indicated that the water team to develop and implement conservation measures for the was more than 27,900 years old. White Sands pupfish (Pittenger and Springer, 1999). Because Streamflow from Main Mound Spring was estimated water quality can affect pupfish and the environmental at 0.007 ft3/s in 1955 and 1957 and ranged from 0.02 to conditions of their habitat, a comprehensive compilation 0.07 ft3/s from 1996 to 2001. Dissolved-solids concentrations of hydrologic data for pupfish habitat and nonhabitat areas in samples collected between 1955 and 2007 ranged from in the northern Tularosa Basin was undertaken by the U.S. an estimated 3,760 to 4,240 mg/L in the upper pond and Geological Survey (USGS) in cooperation with White Sands 4,840 to 5,120 mg/L in the lower pond. Isotopic data for a Missile Range. 2 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

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Base modified from U.S. Geological Survey digital data, 1:100,000, 0 10 20 30 40 50 MILES and White Sands Missile Range (2003) Universal Transverse Mercator projection, Zone 13 0 10 20 30 40 50 KILOMETERS North American Datum of 1983

Figure 1. Location of study area in White Sands Missile Range and Holloman Air Force Base, New Mexico. Introduction 3

Purpose and Scope quarters. The first digit of the fourth segment of the location number denotes the 160-acre quarter section. Then, the 160- This report presents a compilation of hydrologic data for acre quarter section is divided into four quarters numbered springs, streams, and ponds of White Sands pupfish habitat in the same manner, and the second digit in the fourth and nonhabitat areas on White Sands Missile Range and segment of the location number denotes the 40-acre tract. Holloman Air Force Base in the northern Tularosa Basin. Finally, the 40-acre tract is divided into four quarters, and Data compiled include daily and instantaneous streamflow, the third digit in the fourth segment of the location number suspended-sediment concentrations, streamflow and water- denotes the 10-acre tract. For example, site 14S.08E.35.144 quality data collected during a seepage (gain-loss) study, is located in the southeast quarter of the southeast quarter of and physical and chemical water-quality data. Data were the northwest quarter of section 35, Range 08 East, Township collected by the USGS and the Department of Fishery and 14 South (fig. 2). If more than one site has the same location Wildlife Sciences at New Mexico State University between number, then the letter “a” is appended to the fourth segment 1911 and 2008 and compiled from the USGS National Water of the location number of the second site, the letter “b” is Information System database (U.S. Geological Survey, 2013), appended to the location number of the third site, and so on. other published (Meinzer and Hare, 1915; Weir, 1965) and Where sections are irregularly shaped, the site is located by unpublished USGS data (data on file with the U.S. Geological superimposing a regular square section grid on the irregular Survey, New Mexico Water Science Center, Albuquerque, section with the southeastern corners and eastern section lines New Mexico), and a New Mexico State University report of the grid and irregular section matching. The site is then (Turner, 1987). numbered by its location in the superimposed square grid. Documentation of water-quality and streamflow Location numbers for sites identified according to the conditions in White Sands pupfish habitat areas in the grid system of latitude and longitude (USGS location number northern Tularosa Basin in White Sands Missile Range will in table 1) consist of three parts: a latitude value, a longitude aid in the evaluation of current and future management and value, and a two-digit sequence number. The latitude and research activities, the assessment of cumulative effects of longitude values (denoted in degrees [°], minutes [′], and military activities, and adherence to National Environmental seconds [″]) are based on an initial determination of site Policy Act documentation with regard to White Sands pupfish location rounded to the nearest second. The third part of the habitat conservation. USGS location number is a two-digit sequence number that is used to uniquely identify sites that have the same latitude Site-Numbering Systems and longitude. The first site generally is assigned a sequence number of “01,” the second site with the same latitude and Three systems of identifying site locations are used in longitude is assigned a sequence number of “02,” and so on. this report: one based on the Public Land Survey (PLS) system This type of USGS location number consists of 15 digits. of subdivision of sectionized land, one based on the grid For example, the site for which the PLS location number system of latitude and longitude, and one based on the order of was described above (14S.08E.35.144) is located at latitude sites along streams. Unless otherwise noted, site locations are 33o 03′ 23″ North and longitude 106o 09′ 38″ West and has a presented as they appear in data sources. In some instances, it USGS location number of 330323106093801. Once a USGS was not possible to locate the site for which data are presented location number is established it is never changed even if in this report, and so no location information is given herein. the latitude and longitude of the site is refined or corrected Sites are shown on maps in this report only if latitude and through subsequent measurements. Even though the 15-digit longitude were available or if sites were depicted on maps USGS location number is based on latitude and longitude it with identifiable landmarks in the source publication. should never be used as a substitute for the actual latitude and Location numbers for sites identified according to the longitude of a site. PLS system of subdivision of sectionized land (PLS location The downstream-order system is used to assign USGS number in table 1) consist of four segments separated by location numbers to some surface-water sites (usually periods and define the location of the site to the nearest streamflow-gaging stations) in river basins. Numbers are 10-acre tract of land, when possible. The four segments assigned, from lowest to highest (upstream to downstream), denote, from left to right, the township south (S.) of the New along the primary (main) stream in a river basin. Downstream Mexico base line, the range east (E.) of the New Mexico order numbers for tributaries also are assigned location principal meridian, the section, and the particular 10-acre tract numbers in downstream order, but the sites on tributaries within the section. The fourth segment of the number, which are numbered such that their values fall between those of consists of three digits, denotes from left to right the 160-, sites on the main stream that are upstream and downstream 40-, and 10-acre tracts within the section in which the site is of the tributary. Sites numbered according to this system located. To delineate the fourth segment of the number, the have location numbers that consist of eight digits: the first section is divided into four quarters, numbered 1, 2, 3, and two digits identify the major river basin (for example, “08” 4, in the normal reading order (from left to right from top to designates the Rio Grande Basin), and the six subsequent bottom), for the northwest, northeast, southwest, and southeast digits designate the downstream order of the sites. 4 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin Source Hare (1915). Hare (1915). Meinzer and Meinzer and USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. (1987). Turner (1987). Turner USGS NWIS. (1987). Turner (1987). Turner (1987). Turner (1987). Turner (1987). Turner (1987). Turner ------4,118 4,125 4,125 3,940 4,135 (feet) Land- surface altitude

------(west) Longitude 106° 29′ 46″ 106° 09′ 38″ 106° 09′ 36″ 106° 22′ 03″ 09″ 106° 11′ 106° 17′ 12″ 106° 09′ 13″

------(north) Latitude 33° 05′ 34″ 33° 03′ 23″ 33° 03′ 23″ 33° 04′ 44″ 33° 04′ 50″ 33° 25′ 01″ 33° 03′ 31″ b b b b b c

------number 12S.06E.12.3 12S.06E.14.2 PLS location 14S.08E.35.144 14S.08E.35.144 14S.06E.23.342 14S.08E.21.424 10S.06E.26.242 14S.08E.35.223 16S.08E.28.322

AFB, Air Force Base; HAFB, Holloman Air Force Base; mi, mile; NE, northeast; NM, New Air Force Base; HAFB, Holloman AFB, AFB, Air Force Base; HAFB, Holloman Air Force Base; mi, mile; NE, northeast; NM, New Air Force Base; HAFB, Holloman AFB, ------number USGS location 330534106294610 330323106093810 330323106093601 330444106220310 330450106110910 332501106171201 330328106091401

used in this report) (if different from that database or publication Site name or description in source WSMR Range Road 9 downstream from the dirt road that crosses Malone Draw channel less than about 0.3 mi down the drainage and upstream from where a power line crosses Lost River WSMR Range Road 9 culvert under WSMR Range Road 9 downstream from Water immediately below surface of Alkali Flat immediately below surface of Water Alkali Flat immediately below surface of Water WSMR Alkali Spring on NM Tularosa, Pond north of Barrel Spring near 14S.08E.35.144 Barrel Spring-South Pond NM Tularosa, Big Salt Lake near NM Tularosa, WSMR Road 6 near Brazel Lake at Dead Oryx Mound Spring near Oscura, NM --- Upper Pond at Double Mound Spring --- upstream from culverts under Lost River-just pool containing pupfish Lost River-first water at the head of an eroded Lost River-flowing WSMR Range Road 9 from Lost River-upstream below the west end of north Lost River-just fishless reach about 0.9 mi Lost River-shallow,

a a a a a a a Site names and descriptions, identification numbers, locations, and land-surface altitudes of water-sampling sites on White Sands Missile Range and Holloman Air Site names and descriptions, identification numbers, locations, land-surface altitudes of water-sampling Site names and descriptions, identification numbers, locations, and land-surface altitudes of water-sampling sites on White Sands Missile Range and Holloman Air Site names and descriptions, identification numbers, locations, land-surface altitudes of water-sampling a a

shown on figures) (site names in bold are Pond Pond and (or) tables in this report Site name as shown on maps Alkali Flat 1 Alkali Flat 2 Alkali Spring Spring-North Pond Barrel Spring-South Pond Barrel Big Salt Lake Brazel Lake Dead Oryx Mound Spring Double Mound Springs-Lower Double Mound Springs-Upper Guilez Spring (Turner) Lost River Lost River 1 Lost River 2 Lost River 3 Lost River 4 Lost River 5 Table 1. Table Force Base, New Mexico, 1911–2008.—Continued [Location information as published in source database or publication unless otherwise indicated. ---, no data; White Sands Missile Range] WSMR, Information System; PLS, Public Land Survey; USGS, U.S. Geological Water northwest; NWIS, National Mexico; NMSU, New Mexico State University; NW, Table 1. Table Force Base, New Mexico, 1911–2008. [Location information as published in source database or publication unless otherwise indicated. ---, no data; White Sands Missile Range] WSMR, Information System; PLS, Public Land Survey; USGS, U.S. Geological Water northwest; NWIS, National Mexico; NMSU, New Mexico State University; NW, Introduction 5 Source Hare (1915). Hare (1915). Turner (1987). Turner (1987). Turner (1987). Turner USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. Meinzer and (1987). Turner (1965). Weir (1987). Turner (1987). Turner (1987). Turner (1987). Turner (1987). Turner (1987). Turner Meinzer and ------4,047 4,150 4,160 4,350 (feet) Land- surface altitude

------(west) Longitude 106° 09′ 55″ 106° 17′ 07″ 106° 17′ 05″ 106° 18′ 50″ 106° 19′ 11″ 106° 18′ 33″

------(north) Latitude 32° 52′ 51″ 33° 25′ 28″ 33° 25′ 35″ 33° 16′ 57″ 33° 16′ 22″ 33° 17′ 15″ b b b b c

------number PLS location 10S.06E.23.442 10S.06E.24.313 12S.07E.08.434 12S.07E.08.424 12S.07E.9.3 12S.07E.08.422 12S.07E.21.332 10S.06E.26

AFB, Air Force Base; HAFB, Holloman Air Force Base; mi, mile; NE, northeast; NM, New Air Force Base; HAFB, Holloman AFB, ------number USGS location 325251106095310 332528106170710 332535106170501 331657106185010 331622106191110 08480594

used in this report) (if different from that database or publication Site name or description in source between Holloman AFB and White Sands AFB and between Holloman National Monument National Monument south of the springhead near Road 316 from the spring Spring Lost River-ponded area near HAFB Building 1176 Lost River-ponded upstream from the boundary Lost River-just White Sands western pool on Lost River-most Air Force Base, NM Lost River on Holloman Lower Mound Spring Pond near Oscura, NM Mound Spring (Upper Pond) near Oscura, NM Malpais Marsh near Oscura, NM WSMR, NM Salt Marsh Lower Lake, Site 8 on Malpais Spring near Oscura, NM ------Manmade pond that is located approximately 2 mi ------Middle of the marsh that received outflow Near the upper end of study site on Malpais ------a d

a

a a a a a a a a Site names and descriptions, identification numbers, locations, and land-surface altitudes of water-sampling sites on White Sands Missile Range and Holloman Air Site names and descriptions, identification numbers, locations, land-surface altitudes of water-sampling a a

shown on figures) (site names in bold are Pond Pond Lake Hare) marsh and (or) tables in this report Site name as shown on maps Lost River 6 Lost River 7 Lost River 8 AFB on Holloman Lost River Main Mound Spring-Lower Main Mound Spring-Upper Malpais Salt Marsh Malpais Salt Marsh Lower Oscura Malpais Spring near Malpais Spring (Meinzer and Malpais Spring (Turner) Malpais Spring (Wier) Malpais Spring Pond Malpais Spring-at springhead Malpais Spring-edge of marsh Malpais Spring-middle of Malpais Spring-upper end Mound Spring (Turner) Mound Spring 25 Table 1. Table Force Base, New Mexico, 1911–2008.—Continued [Location information as published in source database or publication unless otherwise indicated. ---, no data; White Sands Missile Range] WSMR, Information System; PLS, Public Land Survey; USGS, U.S. Geological Water northwest; NWIS, National Mexico; NMSU, New Mexico State University; NW, 6 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin Source Hare (1915). Hare (1915). Hare (1915). Meinzer and (1987). Turner (1987). Turner (1987). Turner USGS NWIS. Meinzer and Meinzer and USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. (1987). Turner USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. USGS NWIS. ------4,350 3,960 3,950 3,990 4,000 4,050 4,040 4,050 4,050 4,100 (feet) Land- surface altitude

------(west) Longitude 106° 17′ 20″ 106° 23′ 45″ 106° 21′ 13″ 106° 22′ 57″ 106° 22′ 25″ 106° 24′ 38″ 106° 25′ 35″ 106° 26′ 07″ 106° 26′ 14″ 106° 25′ 01″ 106° 23′ 19″ 106° 22′ 02″

------(north) Latitude 33° 26′ 06″ 33° 07′ 16″ 33° 20′ 57″ 33° 06′ 08″ 33° 05′ 12″ 33° 08′ 47″ 33° 09′ 44″ 33° 10′ 42″ 33° 13′ 46″ 33° 14′ 54″ 33° 17′ 22″ 33° 18′ 45″

c b b b b b b b b c b b b b

------number PLS location 10S.06E.23 12S.06E.31.322 11S.06E.24.322 10S.06E.23.221 12S.06E.15.2 13S.06E.19.2 14S.06E.04.441 11S.06E.24.144 14S.06E.15.213 14S.06E.23.113 13S.06E.32.224 13S.06E.29.111 13S.06E.18.433 12S.06E.31.234 12S.06E.29.223 12S.06E.10.144 11S.06E.35.434

AFB, Air Force Base; HAFB, Holloman Air Force Base; mi, mile; NE, northeast; NM, New Air Force Base; HAFB, Holloman AFB, ------number USGS location 332606106172001 330716106234510 332057106211310 330608106225710 330512106222510 330847106243810 330944106253510 331042106260710 331346106264410 331454106250110 331722106231910 331845106220210

used in this report) (if different from that database or publication Site name or description in source Double Mound Springs 12 S., R.6 E. T. 1/4 Sec. 15, 13 S., R.6 E. T. 1/4 Sec. 19, WSMR, NM --- Single Mound Spring located northwest of the ------North Mound Spring near Oscura, NM Salt Creek-sample taken at road crossing in NE Salt Creek-sample taken at road crossing in NE WSMR, NM Salt Creek 3 at Range Road 6 on WSMR, NM Salt Creek 4 at Range Road 7 on Salt Creek above Big Lake at mile 1.2 on WSMR, NM Salt Creek at Big Lake on --- WSMR, NM Salt Creek at stream mile 5.8 on WSMR, NM Salt Creek at stream mile 6.4 on WSMR, NM Salt Creek at stream mile 8.4 on WSMR, NM Salt Creek at stream mile 12.5 on WSMR, NM Salt Creek at stream mile 14.5 on WSMR, NM Salt Creek at stream mile 18.1 on WSMR, NM Salt Creek at stream mile 21.1 on

a a a a a Site names and descriptions, identification numbers, locations, and land-surface altitudes of water-sampling sites on White Sands Missile Range and Holloman Air Site names and descriptions, identification numbers, locations, land-surface altitudes of water-sampling

shown on figures) (site names in bold are Mound Springs 6 7 Lake at mile 1.2 12.5 14.5 18.1 21.1 and (or) tables in this report Site name as shown on maps Mound Spring 7 of Double Mound Spring, NW study site NMSU lower study site NMSU upper North Mound Spring Salt Creek 1 Salt Creek 2 3 at Range Road Salt Creek 4 at Range Road Salt Creek above Big Salt Salt Creek at Big Salt Lake Salt Creek Salt Creek at Road 6 mile 5.8 at stream Salt Creek mile 6.4 at stream Salt Creek mile 8.4 at stream Salt Creek mile at stream Salt Creek mile at stream Salt Creek mile at stream Salt Creek mile at stream Salt Creek Table 1. Table Force Base, New Mexico, 1911–2008.—Continued [Location information as published in source database or publication unless otherwise indicated. ---, no data; White Sands Missile Range] WSMR, Information System; PLS, Public Land Survey; USGS, U.S. Geological Water northwest; NWIS, National Mexico; NMSU, New Mexico State University; NW, Introduction 7 Source Turner (1987). Turner USGS NWIS. USGS NWIS. USGS NWIS. (1987). Turner (1987). Turner (1987). Turner (1987). Turner (1987). Turner USGS NWIS. USGS NWIS. USGS NWIS. ------4,175 (feet) Land- surface altitude

------(west) Longitude 106° 21′ 02″ 106° 23′ 50″ 106° 26′ 57″ 106° 17′ 39″ 106° 08′ 59″ 106° 17′ 34″

------(north) Latitude 33° 21′ 39″ 33° 16′ 32″ 58″ 33° 11′ 33° 24′ 20″ 33° 05′ 08″ 33° 25′ 08″ b b c b b b b c

------number PLS location 11S.06E.13.414 12S.06E.16.244 13S.05E.12.422 11S.06E.13.234 12S.06E.03.422 10S.06E.35.122 14S.08E.24.133 10S.06E.26.213

AFB, Air Force Base; HAFB, Holloman Air Force Base; mi, mile; NE, northeast; NM, New Air Force Base; HAFB, Holloman AFB, ------number USGS location 332139106210210 08480595 331158106265710 332420106173901 330508106085910 332508106173401

used in this report) (if different from that database or publication Site name or description in source Salt Creek at Range Road 316) NM --- WSMR, NM Salt Creek below Spring on NM (formerly named Tularosa, Salt Creek near WSMR, NM on Salt Creek near NW-50 ------South Mound Spring near Oscura, NM Tularosa, WSMR Road 9, near Creek at Tularosa Mound Spring near Oscura, NM West a

a a a Site names and descriptions, identification numbers, locations, and land-surface altitudes of water-sampling sites on White Sands Missile Range and Holloman Air Site names and descriptions, identification numbers, locations, land-surface altitudes of water-sampling

shown on figures) (site names in bold are Derived from location plotted by using latitude and longitude published in NWIS. Previously USGS site number 331715106183301. Not shown on maps because of insufficient location information. Derived from location approximated by using maps in source publication. and (or) tables in this report a b c d Site name as shown on maps Salt Creek at Wit Road Bridge Wit Salt Creek at below Salt Spring Salt Creek Tularosa near Salt Creek NW-50 near Salt Creek Salt Creek-Road 6 bridge Road Salt Creek-Wit Salt Creek-Road 6 of drainage Salt Creek-top Salt Creek-waterfall South Mound Spring Creek Tularosa Mound Spring West Table 1. Table Force Base, New Mexico, 1911–2008.—Continued [Location information as published in source database or publication unless otherwise indicated. ---, no data; White Sands Missile Range] WSMR, Information System; PLS, Public Land Survey; USGS, U.S. Geological Water northwest; NWIS, National Mexico; NMSU, New Mexico State University; NW, 8 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

Sierra Counties, New Mexico. Surface water and springs in the study area are located in alluvium of Quaternary and Tertiary age on the floor of the Tularosa Basin (Hawley, 1983, 1993). The Tularosa Basin is contained within a large structural basin in the Mexican Highland section of the Basin and Range physiographic province (Fenneman and Johnson, 1946). The combined thickness of Tertiary- and Quaternary-age bolson- fill sedimentary deposits in the basin is as great as 10,000 feet (ft) (Risser, 1988; Orr and Risser, 1992). The present basin- and-range configuration of the Tularosa Basin developed in response to late Tertiary crustal extension associated with the Rio Grande rift. The Tularosa Basin is a closed surface-water drainage system, separated from the Hueco Bolson (a through-flowing basin) by a subtle high that forms a surface divide near the New Mexico-Texas State line (fig. 1 inset map; Basabilvazo and others, 1994). Much of the surface-water runoff from the mountains bordering the Tularosa Basin infiltrates before reaching the basin floor (Naus, 2002), but surface-water Site 14S.08E.35.144 flow during summer thunderstorms may reach depressions and playas on the basin floor, forming ephemeral lakes that eventually evaporate and develop into alkali flats (Basabilvazo and others, 1994). During the last glacial-pluvial time toward the end of Figure 2. Diagram showing system for identifying site locations the Pleistocene Epoch, a large ephemeral lake now called according to the Public Land Survey (PLS) system of subdivision Lake Otero was present in Tularosa Basin. Lucas and Hawley of sectionized land in New Mexico. (2002) indicated that Lake Otero might have covered about 810 square miles. A large stream, the ancestral Salt Creek, which drained the northern portion of the basin, formed the Acknowledgments main tributary to Lake Otero (Weir, 1965; Hawley, 1993). Dating of organic sediment associated with Lake Otero The authors wish to acknowledge White Sands Missile indicates that the lake persisted in the Tularosa Basin until Range personnel for their support of the long-term data- about 10,000 years ago, when a change of climate to more arid collection efforts that provided the basic data included in this conditions resulted in the recession and drying of Lake Otero report. We also wish to acknowledge the field data collection (Pittenger and Springer, 1999). Lake Lucero (fig. 1) is a small efforts of the many USGS and non-USGS personnel who remnant of Lake Otero (White Sands National Monument, labored in sometimes inclement conditions to obtain the n.d.). Pittenger and Springer (1999) postulated that White field data. Sands pupfish inhabited Lake Otero and its tributaries such as The White Sands Missile Range Operational Security the ancestral Salt Creek. review of this report was completed on June 22, 2012, and Four locations within the Tularosa Basin are known the information contained in this report has been approved for pupfish habitat areas: Salt Creek, Malpais Spring and Malpais public release by White Sands Missile Range. Salt Marsh, Main Mound Spring, and Lost River (figs. 3, 4, and 5). The pupfish habitat areas are on property under the jurisdiction of the Department of Defense. The Salt Creek, Malpais Spring and Malpais Salt Marsh, and Main Mound Description of Study Area Spring habitat areas are within the boundaries of White Sands Missile Range, and Lost River flows through Holloman Air The study area (fig. 1) is located in the northern part of Force Base. Photographs of springs, streams, and ponds the Tularosa Basin on the White Sands Missile Range and in pupfish habitat and nonhabitat areas are included in Holloman Air Force Base, in Doña Ana, Lincoln, Otero, and appendix 1. Description of Study Area 9

106°45’ 106°30’ 106°15’ 106°00’ EXPLANATION T08S Water-quality site (lake-reservoir) Oscura Mountains LINCOLN Water-quality site (spring) T09S 33°30’ COUNTY Water-quality site (stream) SOCORRO COUNTY Area shown in figure 4 Seepage study site (stream) SIERRA COUNTY Water-quality and seepage site (stream) Mound Spring habitat area Sacramento T10S Mountains New Mexico State University (NMSU) study site

Carrizozo NMSU upper study site lava flow s T11S in ta n u o M

s e r Malpais Spring and d T12S 33°15’ n Malpais Salt Marsh A

n NMSU lower study site habitat area a

S Salt Creek Salt Creek habitat area T13S 54 White Sands Alkali Missile Range Spring Big Salt Lake boundary T14S

33°00’ Lost River T15S Area shown SIERRA COUNTY habitat in figure 5 area

Study area Malone HOLLOMAN Draw T16S AIR FORCE BASE Lost River Ritas SAN ANDRES Draw NATIONAL WILDLIFE 70 WHITE SANDS T17S REFUGE NATIONAL MONUMENT

COUNTY

DOÑA ANA DOÑA 32°45’

OTERO COUNTY T18S Lake Lucero

T19S

R02E R03E R04E R05E R06E R07E R08E R09E

Base modified from U.S. Geological Survey digital data, 1:100,000, 0 5 10 MILES and White Sands Missile Range (2003) Universal Transverse Mercator projection, Zone 13 0 5 10 KILOMETERS North American Datum of 1983

Figure 3. Locations of White Sands pupfish( Cyprinodon tularosa) habitat areas and sites in and near pupfish habitat areas, White Sands Missile Range and Holloman Air Force Base, New Mexico. 10 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

106°30’ 106°25’ 106°20’ 106°15’ 4 3 2 1 6 5 4 3 2 1 2 1 6 5 6 5 4 3 2 11 12 7 8 9 10 11 12 7 8 9 10 7 8 11 12 9 10 11 7

16 15 14 13 18 17 16 15 14 13 8 14 13 18 17 17 16 15 s SIERRA 14 in North Mound Spring ta n COUNTY u Main Mound Spring-Upper Pond T10S o 21 22 23 24 19 20 21 22 23 24 19 23 24 19 20 20 21 22 M 23

Main Mound Spring-Lower Pond 33°25’ s West Mound Spring e r 26 25 d 30 29 28 27 26 25 30 29 28 27 26 Dead25 Oryx30 Mound 29Spring n 28 27 26 A

n South Mound Spring

a S 33 34 35 36 31 32 33 34 35 36 31 32 35 36 31 32 33 34 LINCOLN COUNTY 35 4 3 2 1 6 5 4 3 2 1 6 5 4 3 2 1 6 5 4 3 OTERO COUNTY 9 10 11 11 12 7 8 9 12 7 8 9 10 10 11 12 7 8 9 10 Salt Creek-top of drainage 16 15 14 14 13 18 17 13 18 17 16 15 Salt Creek below Salt16 Spring15 14 13 18 17 16 15 Salt Creek 4 at Range Road 7 21 22 23 24 23 24 19 T11S 19 20 21 22 20 21 22 23 24 19 20 21 7 NMSU upper study site 22

33°20’ 28 27 26 25 30 29 28 27 26 25 30 29 28 27 26 Carrizozo25 30 29 28 27 lava 33 34 35 36 31 32 33 34 35 36 31 32 33 34 flow Salt Creek at stream mile 21.1 35 36 31 32 33 34

4 3 2 1 5 4 3 Salt2 Creek-waterfall1 6 5 3166 4 3 2 1 6 5 4 3 Salt Creek at stream mile 18.1 Malpais Spring near Oscura 99 10 7 11 12 7 8 9 10 11 12 8 9 10 11 12 7 11 Malpais12 Salt Marsh 8 9 10 Salt Creek near Tularosa Malpais Salt Marsh 14 13 16 15 14 13 13 18 17 18 17 16 15 14 16 15 14 13 18 17 16 15 7 Malpais Salt Marsh T12S Lower Lake 21 22 24 19 23 24 19 20 Salt 21Creek 22 23 20 21 22 23 24 19 20 Malpais Spring Pond 21 22 33°15’ Salt Creek at stream mile 14.5 316 28 27 26 25 28 27 26 25 30 29 30 29 28 27 26 25 30 29 28 27 NMSU lower study site Salt Creek at stream mile 12.5 33 34 35 36 31 32 33 34 35 36 31 32 33 34 35 36 31 32 33 34

R05E R06E R07E R08E Base modified from U.S. Geological Survey digital data, 1:100,000, 0 5 MILES and White Sands Missile Range (2003) Universal Transverse Mercator projection, Zone 13 0 5 KILOMETERS North American Datum of 1983

EXPLANATION Water-quality site (lake-reservoir) State highway Water-quality site (spring) Paved two-lane road Water-quality site (stream) Gravel road Seepage study site (stream) Water-quality and seepage site (stream) New Mexico State University (NMSU) study site

Figure 4. Locations of sites in the White Sands pupfish( Cyprinodon tularosa) Malpais Spring and Malpais Salt Marsh, Main Mound Spring, and northern Salt Creek habitat areas and surrounding areas, White Sands Missile Range and Holloman Air Force Base, New Mexico. Description of Study Area 11

106°25’ 106°20’ 106°15’ 106°10’ T12S 1 6 5 4 6 5 4 3 2 1 3 2 1 6 5 4 3 2 1 6

12 7 8 9 7 8 9 10 11 12 10 11 12 7 8 9 10 11 12 7 Salt Creek near NW-50

18 17 16 13 18 17 16 15 14 13 15 14 13 18 17 16 15 14 13 18 Salt Creek at stream mile 8.4 Salt Creek 2 T13S 19 20 24 19 20 21 22 23 24 21 22 23 24 19 20 21 22 23 24 19 33°10’ Salt Creek at stream mile 6.4 Salt Creek 30 29 25 30 29 28 27 26 25 28 27 26 25 30 29 28 27 26 25 30

31 36 31 32 33 34 35 36 32 33 34 35 36 31 32 33 34 35 36 31 Salt Creek at stream mile 5.8 Three Rivers

1 6 5 4 Salt3 Creek 23 at Range1 Road6 6 5 4 3 2 1 6 5 4 3 2 1 6 6 12 7 8 9 10 11 12 7 8 9 10 11 12 7 8 9 10 11 12 7 Salt Creek above Big Salt Lake at mile 1.2 Tularosa Creek 13 18 17 16 15 14 13Big Salt18 Lake17 16 15 14 13 18 17 16 15 14 13 18 Salt Creek at T14S Big Salt Lake 33°05’ 24 19 20 21 22 23 24 19 20 21 22 23 24 19 20 21 22 23 24 19 Big Salt Lake Brazel Lake 6 25 30 29 28 27 26 25 30 29 28 27 26 25 30 29 28 27 26 25 30 Guilez Spring

36 31 32 33 34 35 36 31 32 33 34 35 36 Barrel31 Spring-South32 33 Pond34 35 36 31

1 6 5 4 Barrel Spring-North Pond 3 2 1 6 5 4 3 2 1 6 5 4 3 2 1 6 SIERRA COUNTY 12 7 8 9 10 11 12 7 8 9 10 11 12 7 8 9 10 11 12 7

13 18 17 16 15 14 13 18 17 16 15 14 13 18 17 16 15 14 13 18

33°00’ OTERO COUNTY T15S

24 19 20 21 22 23 24 COUNTYANA DOÑA 19 20 21 22 23 24 19 20 21 22 23 24 19

25 30 29 28 27 25 30 29 28 27 26 25 30 29 28 27 26 25 30

36 31 32 33 34 36 31 32 33 34 35 36 31 32 33 34 35 36 31

5 4 3 2 1 6 5 4 3 2 1 6 5 4 3 2 1 6 5 4

12 7 8 9 10 11 12 7 8 9 10 11 12 7 8 9 10 11 8 9 HOLLOMAN AIR FORCE BASE 17 16 15 14 13 18 17 16 15 14 13 18 17 16 15 14 13 18 17 16 32°55’ T16S 19 20 21 19 20 21 22 23 24 19 20 21 20 21 22 23 24 22 23 24 Lost River (Turner) 30 29 28 28 27 Lost26 River25 on 30 29 28 29 28 27 26 25 27 26 25 30 29 Holloman AFB er 34 35 36 31 32 33 34 35 36 31 32 33 34 35 36iv 31 32 33 32 33 R st Lo 5 4 3 2 1 6 5 WHITE4 SANDS3 2NATIONAL1 6MONUMENT5 4 3 2 1 6 5 4 T17S R05E R06E R07E R08E Base modified from U.S. Geological Survey digital data, 1:100,000, 0 5 MILES and White Sands Missile Range (2003) Universal Transverse Mercator projection, Zone 13 0 5 KILOMETERS North American Datum of 1983 EXPLANATION Water-quality site (lake-reservoir) State highway Water-quality site (spring) Paved two-lane road Water-quality site (stream) Gravel road Seepage study site (stream) Water-quality and seepage site (stream) New Mexico State University (NMSU) study site

Figure 5. Locations of sites in the White Sands pupfish( Cyprinodon tularosa) southern Salt Creek and Lost River habitat areas and surrounding areas, White Sands Missile Range and Holloman Air Force Base, New Mexico. 12 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

Salt Creek is a perennial stream in the northern Tularosa basalt as an aquifer and was the first to suggest that stream Basin (fig. 3) and is one of two endemic habitat areas of sediment buried beneath the basalt was an additional source the White Sands pupfish. The lower reach of the stream, of water. The Main Mound Spring habitat area (fig. 3), which which drains into Big Salt Lake (fig. 5), is intermittent and includes an upper pond and a lower pond, is part of a group of ephemeral. The Salt Creek drainage basin includes parts of the springs associated with mounds between Salt Creek and the northern San Andres and Oscura Mountains (fig. 1) that are Carrizozo lava flow. The mounds were formed by deposition west of the Quaternary Carrizozo lava flow (figs. 1, 3, and 4), of windborne sediments in and around vegetation supported a 5,000-year-old olivine basalt (Salyards, 1991; Dunbar, by water from the springs. The mounds are typically low, 1999). Much of the ancestral Salt Creek stream channel in flat, symmetrical domes that can be as large as 600 ft in the northern Tularosa Basin was buried by the Carrizozo diameter and 15–20 ft high (Meinzer and Hare, 1915). Mound lava flow (Hawley, 1983). Lava occupying the ancestral Salt composition can include silt, plant matter that has been Creek stream channel probably blocked tributary outlets partially converted to peat, and gypsum precipitated from to the ancestral channel and caused shallow depressions to springwater and deposited by wind. When Meinzer and Hare form at the tributary terminuses along the margins of the lava (1915) mapped 29 mounds in Township 10 South, Range 7 flow (Meinzer and Hare, 1915). Surface-water runoff from East (fig. 4), there were more inactive than active (water- the Sacramento Mountains now drains to playas east of the bearing) mounds. lava flow, and surface-water runoff from the Oscura and San The Lost River (figs. 3 and 5) originates in the Andres Mountains drains to playas or Salt Creek on the west Sacramento Mountains (fig. 1) and extends onto White Sands side of Tularosa Basin. Much of the runoff from the Oscura National Monument (figs. 3 and 5). Many sections of the Mountains is diverted southwestward by the western edge stream channel on Holloman Air Force Base and White Sands of the lava flow and flows to Salt Creek by way of a major National Monument are ephemeral and (or) intermittent. intermittent and ephemeral stream channel. Salt Creek is now the major perennial stream of the Tularosa Basin floor. The Malpais Spring and Malpais Salt Marsh habitat area, located at the southwestern edge of the Carrizozo lava White Sands Pupfish Habitat flow (fig. 3), is the other endemic habitat area of the White Sands pupfish. As noted by Pittenger and Springer (1999), The White Sands pupfish Cyprinodon( tularosa) was first reports of fish in the Malpais Spring area were published as described as a distinct species by Miller and Echelle (1975). early as 1900 (Herrick) and 1913 (Ligon). The first White Other papers of interest are Suminski (1977), Jester and Sands pupfish specimens were collected in July 1927 during Suminski (1982), and Turner (1987). Pittenger and Springer the University of Michigan-Walker-Harris expedition to New (1999) determined through a record, literature, and oral history Mexico (Bradley and others, 1927) and currently reside in the search that White Sands pupfish were endemic to the Salt University of Michigan Museum of Zoology (Cody Thompson Creek and Malpais Spring habitat areas and that White Sands and Douglas Nelson, University of Michigan Museum of pupfish were introduced to Lost River in 1970 and Main Zoology, written commun., 2013). Groundwater discharges Mound Spring between 1967 and 1973. Stockwell and others from several springs and seeps that issue from the base of the (1998) confirmed the genetic relations of the Main Mound terminus of the Carrizozo lava flow in the Malpais Spring Spring and Lost River pupfish populations to pupfish in Salt area. The accumulated groundwater discharges form a stream Creek. Stockwell and others (1998) also established genetic that flows to wetlands, identified as the Malpais Salt Marsh evidence of two evolutionarily significant units. (fig. 4), which encompassed approximately 1,188 acres in Water-quality characteristics of the White Sands pupfish 1997 (Lichvar and Sprecher, 1997) and have a salt marsh habitats can affect pupfish and the environmental conditions ecosystem. Dominant species of marsh vegetation in the area of their habitats. Results from genetic studies by Stockwell include saltgrass (Distichlis spicata), iodinebush (Allenrolfea and others (1998) illustrated the ability of White Sands occidentalis), and spikerush (Eleocharis palustris). Some pupfish to survive in water-quality conditions that may change areas of the wetland are seasonally inundated by water. At one rapidly because of precipitation and runoff events. Water- time, the water from the spring area was diverted to a ditch for quality characteristics also are important in regard to the body stock water and, later, military use. morphology of White Sands pupfish and populations of fish The aquifer that discharges at Malpais Spring was parasites and aquatic snails that can be associated with fish described by Meinzer and Hare (1915) as consisting of basalt parasites (Collyer, 2003; Harstad, 2003). of the Carrizozo lava flow. Weir (1965) also recognized the Hydrologic Data 13

Hydrologic Data percent (106 samples from 28 sites). Ion charge imbalances (C.I.) were calculated by using the following equation: Hydrologic data were compiled for 67 sites (table 1) located in the northern Tularosa Basin on White Sands  sum cations − sum anions  Missile Range and Holloman Air Force Base. Compiled C.I. (percent) =  ×100, (1)  sum cations + sum anions  data (app. 2) include streamflow measurements (tables 2–1 and 2–2), selected field water-quality characteristics where including suspended-sediment concentrations (table 2–2), sum cations is the sum of the cations, in measurements from a seepage (gain-loss) study (table 2–3) milliequivalents per liter, and at Salt Creek, and other physical and chemical water-quality sum anions is the sum of the anions, in characteristics of surface water and springs in the Quaternary milliequivalents per liter. and Tertiary alluvial fill. In addition to the general chemistry and trace elements (tables 2–4 and 2–5), some samples were Quality Assurance and Quality Control analyzed for nutrients and anthropogenic constituents such as perchlorate, pesticides, herbicides, organic compounds, To ensure that measurements made in the laboratory and others (tables 2–6, 2–7, and 2–8). The data also include also represent the actual environmental concentrations isotopic values in water samples collected by the USGS at of constituents, the USGS follows prescribed procedures Malpais Spring and Main Mound Spring in 1982 as part of for onsite measurements and for collecting, treating, and a regional hydrochronological study (Cruz, 1983) and from shipping water-quality samples (U.S. Geological Survey, Alkali Spring, Malpais Spring, Main Mound Spring, and Salt variously dated; Wood, 1976). Quality-assurance and quality- Creek in 2006 (table 2–9). Data sources include the USGS control procedures also have been prescribed for streamflow National Water Information System database (U.S. Geological measurements (Benson and Dalrymple, 1967; Matthai, 1967; Survey, 2013), other published (Meinzer and Hare, 1915; Bodhaine, 1968; Rantz and others, 1982). Data generated from Weir, 1965) and unpublished USGS data (data on file with quality-control samples are used to evaluate the quality of the the U.S. Geological Survey, New Mexico Water Science sampling and processing techniques, as well as to evaluate Center, Albuquerque, New Mexico), and a New Mexico State the data from the environmental samples. Quality-control data University report (Turner, 1987). Unless otherwise indicated, for water samples are identified and stored so that they can be dissolved concentrations were determined from analyses related to corresponding environmental samples. The various of filtered samples. Some constituent concentrations were types of quality-control samples typically collected include determined from unfiltered samples, and in these cases, total blank samples, reference samples, replicate samples, and concentrations are reported and denoted with a capital letter T spike samples (U.S. Geological Survey, variously dated). The in parentheses after the constituent abbreviations (app. 2). USGS National Water Information System database includes For example, cadmium (Cd) concentrations may be reported information about types of quality-assurance and quality- as dissolved concentrations, Cd, or as total concentrations, control procedures associated with water-quality samples, Cd (T). when available. This section of the report summarizes streamflow and Very little quality-assurance and quality-control water-quality characteristics and constituents of water samples information is available for data compiled for this study from collected at sites located in White Sands pupfish habitat areas, USGS reports published prior to 1970 (Meinzer and Hare, as well as at sites in pupfish nonhabitat areas. Throughout the 1915; Weir, 1965) and from non-USGS reports. Turner (1987) section, dissolved-solids concentrations are presented as the cited Orth (1983) for methods used in the New Mexico State sum of constituents (unless otherwise noted) because results of University study for streamflow measurements. In that study, determination by residue on evaporation are not available for water-quality samples collected by the New Mexico State all samples. Discussions of minor and trace elements refer to University Department of Fishery and Wildlife Sciences were dissolved concentrations unless otherwise specified. Stiff and analyzed by the Soil and Water Testing Laboratory at New piper diagrams (figs. 6–11) illustrate the major-ion chemistry Mexico State University (Turner, 1987). of water samples with ion charge imbalances less than ±10 14 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

EXPLANATION Na Cl Ca HCO Mg SO 3 4 Sampling site and number of samples (n)

Lost River on Holloman AFB (n=1) Lost River habitat area Lost River (n=1)

Malpais Salt Marsh (n=2) Malpais Spring and Malpais Spring (U.S. Geological Survey) (n=8) Malpais Salt Marsh habitat area Malpais Spring (Turner) (n=2)

Main Mound Spring-Lower Pond (n=2) Mound Spring Main Mound Spring-Upper Pond (n=5) habitat area Mound Spring (Turner)

Salt Creek 3 at Range Road 6 (n=9)

Salt Creek 4 at Range Road 7 (n=14)

Salt Creek at stream mile 18.1 (n=1) Salt Creek Salt Creek at stream mile 21.1 (n=1) habitat area Salt Creek below Salt Spring (n=1)

Salt Creek near Tularosa (n=18)

Salt Creek near NW-50 (n=9)

Alkali Spring (n=1)

Barrel Spring-North Pond (n=1)

Barrel Spring-South Pond (n=2) Pupfish Big Salt Lake (n=1) nonhabitat areas Brazel Lake (n=1)

Guilez Spring (n=1)

Tularosa Creek (n=1)

West Mound Spring (n=1)

14 12 10 8 6 4 2 0 2 4 6 8 10 12 14 16 18 Milliequivalents per liter, times 100

Figure 6. Stiff diagrams showing major-ion chemistry (averaged for sites with more than one sample) of water samples collected from sites in White Sands pupfish( Cyprinodon tularosa) habitat and nonhabitat areas, 1983–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico. Hydrologic Data 15

EXPLANATION Salt Creek 3 at Range Road 6 80 80 Calcium plus magnesium Salt Creek 4 at Range Road 7

Salt Creek at stream mile 18.1 60 60 Salt Creek at stream mile 21.1

Sulfate plus40 chloride 40 Salt Creek below Salt Spring Salt Creek near NW-50

20 20 Salt Creek near Tularosa

Salt Creek-Road 6 bridge

Salt Creek-Wit Road Magnesium Sulfate

80 Sodium plus potassium 80

Sulfate 60 60

Magnesium Bicarbonate 40 40

20 20

80 60 40 20 20 40 60 80

Calcium Chloride Percent of total milliequivalents per liter

Figure 7. Piper diagram showing major-ion chemistry of water samples collected from sites in the White Sands pupfish( Cyprinodon tularosa) Salt Creek habitat area, 1983–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico.

EXPLANATION Malpais Spring (U.S. Geological Survey) 80 80 Calcium plus magnesium Malpais Spring (Turner)

Malpais Salt Marsh 60 60

Sulfate plus40 chloride 40

20 20

Magnesium Sulfate

80 Sodium plus potassium 80

Sulfate 60 60

Magnesium Bicarbonate 40 40

20 20

80 60 40 20 20 40 60 80

Calcium Chloride Percent of total milliequivalents per liter

Figure 8. Piper diagram showing major-ion chemistry of water samples collected from sites in the White Sands pupfish( Cyprinodon tularosa) Malpais Spring and Malpais Salt Marsh habitat area, 1982–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico. 16 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

EXPLANATION Main Mound Spring-Upper Pond 80 80 Calcium plus magnesium Main Mound Spring-Lower Pond

Mound Spring (Turner) 60 60 Lost River on Holloman AFB

Sulfate plus40 chloride 40 Lost River

20 20

Magnesium Sulfate

80 Sodium plus potassium 80

Sulfate 60 60

Magnesium Bicarbonate 40 40

20 20

80 60 40 20 20 40 60 80

Calcium Chloride Percent of total milliequivalents per liter

Figure 9. Piper diagram showing major-ion chemistry of water samples collected from sites in the White Sands pupfish( Cyprinodon tularosa) Main Mound Spring and Lost River habitat areas, 1982–2006, White Sands Missile Range and Holloman Air Force Base, New Mexico.

EXPLANATION Guilez Spring 80 80 Calcium plus magnesium Brazel Lake

Big Salt Lake 60 60 Barrel Spring-South Pond

Sulfate plus40 chloride 40 Barrel Spring-North Pond Alkali Spring

20 20 West Mound Spring

Tularosa Creek

Magnesium Sulfate

80 Sodium plus potassium 80

Sulfate 60 60

Magnesium Bicarbonate 40 40

20 20

80 60 40 20 20 40 60 80

Calcium Chloride Percent of total milliequivalents per liter

Figure 10. Piper diagram showing major-ion chemistry of water samples collected from sites in White Sands pupfish( Cyprinodon tularosa) nonhabitat areas, 1954–2006, White Sands Missile Range and Holloman Air Force Base, New Mexico. Hydrologic Data 17

EXPLANATION Pupfish habitat areas 80 80 Calcium plus magnesium Pupfish nonhabitat areas

60 60

Sulfate plus40 chloride 40

20 20

Magnesium Sulfate

80 Sodium plus potassium 80

Sulfate 60 60

Magnesium Bicarbonate 40 40

20 20

80 60 40 20 20 40 60 80

Calcium Chloride Percent of total milliequivalents per liter

Figure 11. Piper diagram showing major-ion chemistry of water samples collected from White Sands pupfish( Cyprinodon tularosa) habitat and nonhabitat areas, 1954–2007, White Sands Missile Range and Holloman Air Force Base, New Mexico.

Salt Creek The average annual mean streamflow and average annual total streamflow at the Salt Creek near Tularosa gaging As part of the hydrologic monitoring program for station for water years 1995–2008 were 1.35 cubic feet per pupfish habitats in White Sands Missile Range, streamflow second (ft3/s) and 983 acre-feet, respectively (table 2–1). The measurements and water samples were collected at seven sites maximum instantaneous streamflow (376 ft3/s) for the period on Salt Creek from 1995 through 2008. USGS streamflow- occurred on May 7, 2007. Periods of no flow at the gaging gaging station 08480595 (Salt Creek near Tularosa [formerly station were observed in water years 2002 through 2006, named “Salt Creek at Range Road 316”]; fig. 4), funded by but small pools of water allowed the White Sands pupfish to the U.S. Army, White Sands Missile Range, is part of the maintain their population. USGS National Streamflow Information Program, a program From 1995 to 2008, the USGS periodically collected designed to ensure the availability of critical information water-quality data, including field measurements and needed to protect and manage rivers in the United States water samples for chemical analysis, in conjunction with (Hirsch and Norris, 2001). Streamflow data for the Salt Creek instantaneous streamflow measurements. Beginning in 1998, near Tularosa gaging station were collected by using both samples were collected for determination of suspended- discrete (instantaneous) measurements and a continuous stage- sediment concentrations (table 2–2). At the Salt Creek near recording device through which either instantaneous or daily Tularosa gaging station, suspended-sediment concentrations mean streamflow may be computed for any time, or any period ranged from 4 to 1,570 milligrams per liter (mg/L) from 1999 of time, during the period of record (figs. 12, 13, and 14; through 2008 (table 2–2). Suspended-sediment concentrations tables 2–1 and 2–2). At the six other streamflow-measurement in water collected from the other six Salt Creek sites during sites on Salt Creek, streamflow data (table 2–2) were obtained the same time period ranged from 17 mg/L at the Salt Creek through instantaneous measurements without using a near NW-50 site to 3,430 mg/L at the Salt Creek 4 at Range continuous stage-recording device. Methods of data collection Road 7 site (table 2–2). and computation are described in Byrd and others (2003). 18 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

A 500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 1994 1995 Water year 1995

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 1995 1996 Water year 1996

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 1996 1997 Water year 1997

Figure 12. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico (08480595), for water years 1995–2008 (see fig. 4 for location of station).A , 1995–1997. B, 1998–2000. C, 2001–3. D, 2004–6. E, 2007–8. Hydrologic Data 19

B 500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 1997 1998 Water year 1998

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 1998 1999 Water year 1999

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 1999 2000 Water year 2000

Figure 12. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico (08480595), for water years 1995–2008 (see fig. 4 for location of station).A , 1995–1997. B, 1998–2000. C, 2001–3. D, 2004–6. E, 2007–8. —Continued 20 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

C 500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2000 2001 Water year 2001

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2001 2002 Water year 2002

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2002 2003 Water year 2003

EXPLANATION

Period of zero flow

Figure 12. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico (08480595), for water years 1995–2008 (see fig. 4 for location of station).A , 1995–1997. B, 1998–2000. C, 2001–3. D, 2004–6. E, 2007–8. —Continued Hydrologic Data 21

D 500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2003 2004 Water year 2004

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2004 2005 Water year 2005

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2005 2006 Water year 2006

EXPLANATION

Period of zero flow

Figure 12. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico (08480595), for water years 1995–2008 (see fig. 4 for location of station).A , 1995–1997. B, 1998–2000. C, 2001–3. D, 2004–6. E, 2007–8. —Continued 22 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

E 500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2006 2007 Water year 2007

500

100

10

1

0.1 Streamflow, in cubic feet per second Streamflow,

0.01 Oct. Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. 2007 2008 Water year 2008

Figure 12. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico (08480595), for water years 1995–2008 (see fig. 4 for location of station).A , 1995–1997. B, 1998–2000. C, 2001–3. D, 2004–6. E, 2007–8. —Continued Hydrologic Data 23

200

100

40

10

4

1

0.4 Streamflow, in cubic feet per second Streamflow,

0.1

EXPLANATION 0.04 Daily mean streamflow Instantaneous streamflow

0.01 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 Calendar year

Figure 13. Daily mean and instantaneous streamflow at U.S. Geological Survey streamflow-gaging station Salt Creek near Tularosa, New Mexico (08480595), calendar years 1995–2008 (see fig. 4 for location of station).

The magnitude of the dissolved-solids concentrations indicate a net seepage loss of 0.07 ft3/s from the Salt Creek in Salt Creek varies throughout the length of the stream below Salt Spring site at stream mile 24.5 to the Salt Creek channel. Dissolved-solids concentrations and other chemical near Tularosa gaging station at stream mile 17.6. Ponded, and physical characteristics of the water also can vary no-flow conditions at stream mile 14.5 were noted, and dry temporally because of precipitation, surface-water runoff, and conditions were observed from stream mile 12.5 to the mouth changes in bank storage of groundwater. In samples collected of Salt Creek at stream mile 0. No tributary inflow or outflow from Salt Creek from 1911 through 2007, dissolved-solids (diversions) was observed during the study. Channel gain or concentrations ranged from 2,290 to 66,700 mg/L (solids, sum loss values incorporate seepage to or from the unlined channel, of constituents in table 2–4). Salt Creek base flow generally evaporation from the water surface, and evapotranspiration is saline (defined for this report as 10,000–100,000 mg/L by vegetation along the channel banks. Individual streamflow dissolved solids), but during low and high flow, the dissolved- measurements, made by using a 3-inch Parshall flume, solids concentrations can vary from brackish (defined for this were rated excellent (error of 5 percent or less) throughout report as 1,000–10,000 mg/L dissolved solids) to saline. the stream reach (Byrd and others, 2003). The overall A seepage (gain-loss) study was conducted on August investigation was rated fair (error of 15 percent or less) on 12–13, 2002, along the 24.5-mile reach from the Salt Creek the basis of unsteady streamflow conditions (Byrd and others, below Salt Spring site (fig. 4) to the mouth of the creek at 2003). During the seepage investigation, dissolved-solids Big Salt Lake (fig. 5). Stream miles are referenced upstream concentrations of samples collected from five sites (between from the mouth of the creek, which is designated as stream stream mile 24.5 and stream mile 17.6) ranged from 12,700 to mile 0. Streamflow measurements (fig. 15; table 2–3) 38,100 mg/L (fig. 15; table 2–3). 24 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

A 15 45,000

14 Salt Creek 4 at Range Road 7 40,000 13

12 35,000 11

10 30,000

9 25,000 8

7 20,000 6

5 15,000

4 10,000 3

2 5,000 1

0 0

15 45,000

14 Salt Creek near Tularosa pH, in standard units 40,000 13 Streamflow, in cubic feet per second Streamflow,

12 Dissolved solids, in milligrams per liter 35,000 11

10 30,000

9 25,000 8

7 20,000 6

5 15,000

4 10,000 3

2 5,000 1

0 0 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 Year

EXPLANATION Instantaneous streamflow

pH

Dissolved-solids concentration (table 2–2; solids, residue on evaporation at 180 degrees Celsius, dissolved)

Figure 14. Instantaneous streamflow, dissolved-solids concentration, and pH at Salt Creek surface-water sites (see fig. 4 for locations of sites). A, Salt Creek 4 at Range Road 7 and Salt Creek near Tularosa. B, Salt Creek near NW-50 and Salt Creek 3 at Range Road 6. Hydrologic Data 25

B 15 70,000

14 Salt Creek near NW-50

13 60,000

12

11 50,000 10

9 40,000 8

7 30,000 6

5 20,000 4

3

2 10,000

1

0 0

30 45,000

Salt Creek 3 at Range Road 6 pH, in standard units 40,000

25 Streamflow, in cubic feet per second Streamflow, 35,000 Dissolved solids, in milligrams per liter

20 30,000

25,000

15 20,000

10 15,000

10,000

5 5,000

0 0 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 Year

EXPLANATION Instantaneous streamflow

pH

Dissolved-solids concentration (table 2–2; solids, residue on evaporation at 180 degrees Celsius, dissolved)

Figure 14. Instantaneous streamflow, dissolved-solids concentration, and pH at Salt Creek surface-water sites (see fig. 4 for locations of sites). A, Salt Creek 4 at Range Road 7 and Salt Creek near Tularosa. B, Salt Creek near NW-50 and Salt Creek 3 at Range Road 6. —Continued 26 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

45,000 0.30

40,000 EXPLANATION Dissolved-solids concentration, 0.25 residue on evaporation at 35,000 180 degrees Celsius

30,000 Streamflow 0.20

25,000 0.15 20,000

15,000 0.10

10,000 in cubic feet per second Streamflow, Dissolved solids, in milligrams per liter 0.05 5,000

0 0.00 24.5 23.5 21.1 18.1 17.6 Stream mile

Figure 15. Dissolved-solids concentrations and streamflow during a seepage (gain-loss) study along a 24.5-mile reach of Salt Creek, New Mexico, August 12–13, 2002.

Most Salt Creek samples were sodium-chloride-sulfate collected in the study area. One sample collected in 2000 from type water (figs. 6 and 7); a few samples were sodium-chloride Salt Creek 4 at Range Road 7 had a perchlorate concentration or sodium-calcium-chloride-sulfate type water. Concentrations of 16 µg/L; however, this was the only sample collected with of sodium and chloride exceeded those of seawater (10,500 detectable perchlorate. In subsequent samples, perchlorate was and 19,000 mg/L, respectively) in some samples (table 2–4). not detected. The herbicide 2,4-D was detected in 2 of 38 Salt Concentrations of trace elements (table 2–5), when detected, Creek samples collected between 1995 and 2001 (table 2–8). generally were higher in Salt Creek samples than in most Concentrations in these samples were 0.020 and 0.030 µg/L, samples from other areas. Dissolved chromium was detected less than the maximum contaminant level for drinking water only once in Salt Creek samples at 1.6 micrograms per liter of 70 µg/L set by the U.S. Environmental Protection Agency (µg/L) in a sample from the Salt Creek near Tularosa gaging (U.S. Environmental Protection Agency, no date). station. Salt Creek dissolved selenium concentrations (ranging from 1 to 10 µg/L) and dissolved strontium concentrations Malpais Spring and Malpais Salt Marsh (ranging from 7,110 to 44,500 µg/L) were similar to selenium and strontium concentrations in samples from other sites. The Malpais Spring near Oscura streamflow-gaging Nitrate (as N) concentrations in Salt Creek samples station (08480594) (fig. 4), funded by the U.S. Army, White generally were less than 0.70 mg/L (table 2–6), but in two Sands Missile Range, was installed in July 2003 on the main Salt Creek samples nitrate (as N) concentrations were 1.98 and channel that flows from Malpais Spring to the Malpais Salt 1.29 mg/L. In these two samples nitrite (as N) concentrations Marsh wetlands. Streamflow data for the Malpais Spring near (0.332 and 0.310 mg/L) were higher than in all other samples Oscura gaging station were obtained by using both discrete except one from Big Salt Lake (0.500 mg/L). Total phosphorus (instantaneous) measurements and a continuous stage- (as P) concentrations were generally similar in Salt Creek recording device through which either instantaneous or daily samples to concentrations in samples from other locations mean streamflow may be computed for any time, or any period (generally not more than 0.05 mg/L), but three samples from of time, during the period of record (figs. 16 and 17; tables 2–1 Salt Creek had concentrations of 0.102, 0.14, and 1.17 mg/L. and 2–2). In samples collected between 1995 and 2001, total The average annual mean streamflow and average annual bromide concentrations in Salt Creek samples were highly total streamflow at the Malpais Spring near Oscura gaging variable, ranging from 0.55 to 84.8 mg/L (table 2–7). The station for water years 2003–8 were 6.81 ft3/s and 584 acre- Salt Creek near NW-50 sample collected in May 2003 had the feet, respectively (table 2–1). The maximum instantaneous highest dissolved bromide concentration (6.62 mg/L) of any streamflow of 4.3 ft3/s for the period occurred on both sample. Triethyl phosphate was not detected in any samples January 9, 2004, and August 19, 2006. Hydrologic Data 27

A 4

3

2

1 Streamflow, in cubic feet per second Streamflow,

0 Oct. 1, Nov. 1, Dec. 1, Jan. 1, Feb. 1, Mar. 1, Apr. 1, May 1, June 1, July 1, Aug. 1, Sept. 1, Oct. 1, 2003 2003 2003 2004 2004 2004 2004 2004 2004 2004 2004 2004 2004 Water year 2004

4

3

2

1 Streamflow, in cubic feet per second Streamflow,

0 Oct. 1, Nov. 1, Dec. 1, Jan. 1, Feb. 1, Mar. 1, Apr. 1, May 1, June 1, July 1, Aug. 1, Sept. 1, Oct. 1, 2004 2004 2004 2005 2005 2005 2005 2005 2005 2005 2005 2005 2005 Water year 2005

4

3

2

1 Streamflow, in cubic feet per second Streamflow,

0 Oct. 1, Nov. 1, Dec. 1, Jan. 1, Feb. 1, Mar. 1, Apr. 1, May 1, June 1, July 1, Aug. 1, Sept. 1, Oct. 1, 2005 2005 2005 2006 2006 2006 2006 2006 2006 2006 2006 2006 2006 Water year 2006

Figure 16. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Malpais Spring near Oscura, New Mexico (08480594), for water years 2004–8 (see fig. 4 for location of station).A , 2004–6. B, 2007–8. 28 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

B 4

3

2

1 Streamflow, in cubic feet per second Streamflow,

0 Oct. 1, Nov. 1, Dec. 1, Jan. 1, Feb. 1, Mar. 1, Apr. 1, May 1, June 1, July 1, Aug. 1, Sept. 1, Oct. 1, 2006 2006 2006 2007 2007 2007 2007 2007 2007 2007 2007 2007 2007 Water year 2007

4

3

2

1 Streamflow, in cubic feet per second Streamflow,

0 Oct. 1, Nov. 1, Dec. 1, Jan. 1, Feb. 1, Mar. 1, Apr. 1, May 1, June 1, July 1, Aug. 1, Sept. 1, Oct. 1, 2007 2007 2007 2008 2008 2008 2008 2008 2008 2008 2008 2008 2008 Water year 2008

Figure 16. Daily mean streamflow at U.S. Geological Survey streamflow-gaging station Malpais Spring near Oscura, New Mexico (08480594), for water years 2004–8 (see fig. 4 for location of station).A , 2004–6. B, 2007–8.—Continued

Meinzer and Hare (1915) estimated the flow of Malpais in table 2–4), the dissolved-solids concentrations ranged Spring to be about 4.46 ft3/s in 1911, and Weir (1965) from 3,882 to 5,500 mg/L. Excluding the lowest (3,882 estimated the flow to be about 3.34 ft3/s in 1955 (table 2–2). mg/L) and highest (5,500 mg/L) concentrations, dissolved- Flow rates measured near the upper end of the stream solids concentrations fell within a relatively narrow range of channel in 1984 were 1.3 (March 3, 1984), 1.1 (June 2, 4,360 (estimated) to 4,800 mg/L (solids, sum of constituents, 1984), and 1.1 (August 12, 1984) ft3/s (Malpais Spring-Upper dissolved in table 2–4). Dissolved-solids concentrations in End in table 2–2). From 1996 to 2008, instantaneous flow water samples from Malpais Salt Marsh generally were higher measurements in the channel near Malpais Spring made by than were concentrations in the Malpais Spring samples, the USGS ranged from 0.74 (December 26, 2006) to 2.6 ft3/s particularly at the lower end of the marsh (Malpais Salt Marsh (March 29, 2004) (table 2–2). Lower Lake in table 2–4) where one concentration was an For the 16 Malpais Spring samples (Malpais Spring near estimated 12,600 mg/L. The two highest dissolved-solids Oscura, Malpais Spring [Meinzer and Hare], Malpais Spring (residue on evaporation) concentrations (8,780 and 7,080 [Turner], and Malpais Spring [Weir]) that have dissolved- mg/L) in water from any pupfish habitat area springs were solids concentrations (solids, sum of constituents, dissolved measured in samples from Malpais Spring Pond, a manmade Hydrologic Data 29

4

EXPLANATION 3.5 Daily mean streamflow Instantaneous streamflow

3

2.5

2

1.5 Streamflow, in cubic feet per second Streamflow,

1

0.5

0 2003 2004 2005 2006 2007 2008 Calendar year

Figure 17. Daily mean and instantaneous streamflow at U.S. Geological Survey streamflow-gaging station Malpais Spring near Oscura, New Mexico (08480594), calendar years 2003–8 (see fig. 4 for location of station)

pond about 2 miles south of the Malpais Spring springhead In samples collected from Malpais Spring near Oscura (fig. 4), and from Malpais Spring-Edge of Marsh, respectively and Malpais Spring (Weir) nitrate (as N) and nitrate plus (table 2–4). nitrite (as N) concentrations generally were higher than The water type of samples from the Malpais Spring and concentrations in samples from other sites (table 2–6). Malpais Salt Marsh habitat area has been consistently calcium- Orthophosphate (as P) concentrations generally were similar sulfate (fig. 8; table 2), with the exception of one sample in Malpais Spring near Oscura samples and samples from collected in 1983 for which the water type was sodium-sulfate other sites, but the highest concentration (0.24 mg/L) at any (table 2). Although some of the later detection limits were site was detected in a sample collected from Malpais Spring higher than were concentrations of chromium, copper, iron, near Oscura on May 15, 2001 (table 2–6). Total bromide lead, manganese, and zinc in the 1982 Malpais Spring near concentrations (table 2–7) measured in two Malpais Spring Oscura sample (table 2–5), some of the 1982 values appear near Oscura samples (collected in 2000 and 2001) were 0.57 to be anomalously high as compared with concentrations and 8.5 mg/L, respectively. Herbicides and pesticides included in the other 12 Malpais Spring samples (with analytical in this data compilation were not detected (table 2–8). results) from Malpais Spring near Oscura collected from Carbon 14 isotopic data for a Malpais Spring near Oscura 1996 through 2007. In samples collected from the Malpais water sample collected by the USGS in 1982 indicated that Spring and Malpais Salt Marsh habitat area from 1996 through the water was greater than 27,900 years old (Cruz, 1983; 2007, concentrations of most trace elements, when detected, table 2–9). Before recharging the aquifer, the carbon 14 were similar to or lower than concentrations at most other composition of water can be affected by carbon dioxide gas sites (table 2–5). Exceptions include chromium, which was and dissolution of carbonate minerals in the unsaturated zone detected in 10 (including four estimated values) samples at (Anderholm and Heywood, 2003). For groundwater samples concentrations of 2.0–14.5 (estimated) µg/L, and selenium, from the Hueco Bolson (fig. 1) south of Tularosa Basin, which was detected in 13 samples (one estimated value) at Anderholm and Heywood (2003) assumed that at the time concentrations of 1–7 µg/L in samples from Malpais Spring the water in their samples recharged the aquifer the carbon near Oscura and Malpais Salt Marsh (table 2–5). 14 composition of that water was 100 percent modern. A 30 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

Table 2. Water types of samples collected from sites on White Sands Missile Range and Holloman Air Force Base, New Mexico, 1911–2008.

[Pupfish nonhabitat areas shaded grey. AFB, Air Force Base]

Site name from table 1 and data source Number of samples Pupfish habitat area for multiple sites with same name with sufficient data to (habitat areas shown on fig. 3) (site locations shown in figs. 4 and 5) determine water type Calcium-sulfate water type Barrel Spring-South Pond 2 Nonhabitat. Dead Oryx Mound Spring 1 Nonhabitat. Guilez Spring 1 Nonhabitat. Main Mound Spring-Lower Pond 3 Mound Spring. Main Mound Spring (unknown if from Upper or Lower Pond) 1 Mound Spring. Main Mound Spring-Upper Pond 8 Mound Spring. Malpais Salt Marsh 4 Malpais Spring and Malpais Salt Marsh. Malpais Spring near Oscura 12 Malpais Spring and Malpais Salt Marsh. Malpais Spring (Meinzer and Hare) 1 Malpais Spring and Malpais Salt Marsh. Malpais Spring (Turner)a 1 Malpais Spring and Malpais Salt Marsh. North Mound Spring 1 Nonhabitat. South Mound Spring 1 Nonhabitat. Tularosa Creek 1 Nonhabitat. West Mound Spring 2 Nonhabitat. Magnesium-sulfate water type Barrel Spring-North Pond 1 Nonhabitat. Brazel Lake 1 Nonhabitat. Sodium-chloride water type Alkali Spring 1 Nonhabitat. Big Salt Lake 1 Nonhabitat. Lost River on Holloman AFB 1 Lost River. Lost River 1 Lost River. Salt Creek 3 at Range Road 6 9 Salt Creek. Salt Creek 4 at Range Road 7 15 Salt Creek. Salt Creek at stream mile 18.1 1 Salt Creek. Salt Creek at stream mile 21.1 1 Salt Creek. Salt Creek below Salt Spring 1 Salt Creek. Salt Creek near Tularosa 18 Salt Creek. Salt Creek near NW-50 11 Salt Creek. Salt Creek-Road 6 Bridge 1 Salt Creek. Salt Creek-Wit Road 2 Salt Creek. Sodium-sulfate water type Malpais Spring (Turner)b 1 Malpais Spring and Malpais Salt Marsh. Mound Spring (Turner) 1 Mound Spring. aSample collected on June 8, 1986. bSample collected on December 3, 1983. Hydrologic Data 31 smaller percentage of modern carbon would cause calculated Lost River apparent age to be less. Although Cruz (1983) does not discuss assumptions used to estimate the carbon 14 apparent The hydrologic characteristics of Lost River are the least age for the Malpais Spring near Oscura sample, the apparent studied of the four pupfish habitat areas. Lost River water age is similar to the high end of the range of groundwater usually ranges from brackish to briny (briny is defined in ages (12,100–25,500 years) estimated by Anderholm and this report as greater than 100,000 mg/L dissolved solids). Heywood (2003). Dissolved-solids concentrations of Lost River (Lost River on Holloman AFB, Lost River, and Lost River 1–8) samples Main Mound Spring collected from 1984 to 1999 ranged from 8,930 to 118,000 (estimated) mg/L (solids, sum of constituents, dissolved, At the Main Mound Spring-Upper Pond in 1955 and table 2–4). The water type of samples collected in 1984 and 1957, streamflow was estimated to be about 0.007 ft3/s 1999 was sodium-chloride (figs. 6 and 9; table 2). Data are (table 2–2). From 1996 to 2001 measured streamflow available for only three trace elements analyzed in one sample ranged from 0.02 to 0.07 ft3/s (table 2–2). Dissolved-solids (Lost River on Holloman AFB); of these, the concentration of concentrations of samples collected by the USGS annually dissolved bromide (6.55 mg/L on March 17, 1999; table 2–5) between 1955 and 2007 ranged from 3,760 (estimated) to was the second highest of any sample documented in this 4,240 (estimated) mg/L in the Main Mound Spring-Upper study. Little nutrient data are available for Lost River, and Pond and from 4,840 to 5,120 (estimated) mg/L in the Main there are no total bromide, triethyl phosphate, perchlorate, Mound Spring-Lower Pond (solids, sum of constituents, pesticide, or herbicide data. dissolved in table 2–4). Water from the Main Mound Spring-Upper Pond and Main Mound Spring-Lower Pond has consistently been a Sites Located in Pupfish Nonhabitat Areas calcium-sulfate type (figs. 6 and 9; table 2). Concentrations Sites located in pupfish nonhabitat areas for which of chromium, copper, iron, lead, manganese, and zinc in streamflow and (or) water-quality data are available include a sample collected from Main Mound Spring (unknown if Alkali Spring (fig. 3), springs near the Main Mound Spring from upper or lower pond) in 1982 appear to be anomalously habitat area (Dead Oryx Mound Spring, North Mound high compared to concentrations in other samples collected Spring, South Mound Spring, and West Mound Spring) from that site (table 2–5). In all other Main Mound Spring- (fig. 4), Big Salt Lake (fig. 5), and several sites near the Upper Pond and Main Mound Spring-Lower Pond samples, northern boundary of Holloman Air Force Base (Tularosa concentrations of most trace elements, when detected, were Creek, Brazel Lake, Guilez Spring, Barrel Spring-North Pond, similar to or lower than concentrations at other sites. Nutrient and Barrel Spring-South Pond) (fig. 5). Data also are available concentrations (table 2–6) observed in Main Mound Spring for a few sites for which exact locations are uncertain (table upper and lower pond samples were generally lower than 1) and thus are not shown on any maps (Alkali Flat 1 and those for Malpais Spring near Oscura samples. No pesticides 2, Double Mound Springs-Lower and Upper Ponds, Mound or herbicides (table 2–8) were detected in Main Mound Springs 7 and 25, and Mound Spring, NW of Double Mound Spring-Upper Pond or Main Mound Spring-Lower Pond Springs). samples. In Main Mound Spring-Upper Pond, total bromide Flow data are available for some of these sites. The flow concentrations were 0.60 and 5.3 mg/L in 2000 and 2001, of Alkali Spring was measured at 0.13 ft3/s on November 15, respectively (table 2–7). 2006 (table 2–2). The flow of Guilez Spring ranged from 0.07 Carbon 14 isotopic data for a Main Mound Spring to 0.13 ft3/s in 1957 (table 2–2). Measured flow rates for South water sample (unknown if from upper or lower pond) Mound Spring and Tularosa Creek were 0.02 and 0.06 ft3/s in collected by the USGS in 1982 indicated that the water was 1996 and 1997, respectively (table 2–2). Streamflows at the about 19,600 years old (Cruz, 1983; table 2–9). Although Mound Spring 7 and 25 sites were estimated to be 0.011 and Cruz (1983) does not discuss assumptions used to estimate 0.004 ft3/s, respectively (table 2–2). the carbon 14 apparent age for the Main Mound Spring In samples from springs located in pupfish nonhabitat sample, the apparent age within the range of ages (12,100– areas, dissolved-solids concentrations (solids, sum of 25,500 years) estimated by Anderholm and Heywood (2003) constituents, dissolved in table 2–4) ranged from 1,740 mg/L for groundwater samples collected from wells in the Hueco in Barrel Spring-South Pond to 54,200 (estimated) mg/L in Bolson (fig. 1) south of Tularosa Basin. A sample collected Alkali Spring. Dissolved-solids concentrations in samples in 2006 from Main Mound Spring-Upper Pond had a carbon collected from Dead Oryx Mound Spring, North Mound 14 (percent modern carbon) value of 8.58 percent (table Spring, South Mound Spring, and West Mound Spring ranged 2–9). This value is similar to that of the Main Mound Spring from 3,650 to 4,460 mg/L and were consistently higher (unknown if from upper or lower pond) (8.80 percent; table than in samples from Barrel Spring-South Pond and Guilez 2–9), so the age apparent ages of the two samples would be Spring, which ranged from 1,740 to 1,790 mg/L. The highest about the same. 32 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin dissolved-solids concentrations in samples from pupfish analysis. The pesticides and herbicides included in this nonhabitat areas were 54,200 (estimated) mg/L (Alkali report (table 2–8) were not detected in samples from pupfish Spring), 24,200 mg/L (Big Salt Lake), 12,600 (estimated) nonhabitat area springs. mg/L (Malpais Salt Marsh Lower Lake), 10,600 mg/L (Brazel Lake), and 10,000 mg/L (Barrel Spring-North Pond). A dissolved-solids concentration of 3,940 mg/L was measured in a sample from Tularosa Creek. Summary Water types of samples collected from sites in pupfish The White Sands pupfish Cyprinodon( tularosa), listed nonhabitat areas are calcium-sulfate, magnesium-sulfate, as threatened by the State of New Mexico and as a Federal and sodium-chloride (figs. 6 and 10; table 2). In general, species of concern, is endemic to the Tularosa Basin, New water collected from pupfish nonhabitat area sites tends to Mexico. Because water quality can affect pupfish and the have larger proportions of calcium, magnesium, and sulfate environmental conditions of their habitat, a comprehensive than water from pupfish habitat area sites (fig. 11).Water compilation of hydrologic data for pupfish habitat and from springs associated with mounds in pupfish nonhabitat nonhabitat areas in the northern Tularosa Basin was areas (Dead Oryx Mound Spring, North Mound Spring, undertaken by the U.S. Geological Survey in cooperation with South Mound Spring, and West Mound Spring) was of White Sands Missile Range. a similar type (calcium-sulfate) to water associated with The four locations within the Tularosa Basin that are mounds in pupfish habitat areas (Main Mound Spring and known pupfish habitat areas are the Salt Creek, Malpais Spring Malpais Spring and Malpais Salt Marsh) (table 2). Big Salt and Malpais Salt Marsh, and Main Mound Spring habitat areas Lake and Salt Creek water samples were all of similar type on White Sands Missile Range and the Lost River habitat (sodium-chloride; figs. 6 and 10; table 2), Barrel Spring-North area on Holloman Air Force Base. Results of genetic studies Pond and Brazel Lake water samples were of a similar type illustrate the ability of the White Sands pupfish to survive in (magnesium-sulfate; figs. 6 and 10; table 2;), and Guilez rapidly changing water-quality conditions. Spring and Barrel Spring-South Pond water samples were Streamflow data from the Salt Creek near Tularosa of a similar type (calcium-sulfate; figs. 6 and 10; table 2). streamflow-gaging station indicate that the average annual Alkali Spring had a sodium-chloride water type (table 2), mean streamflow and average annual total streamflow for but the proportions of sodium-chloride and magnesium-sulfate water years 1995–2008 were 1.35 cubic feet per second (ft3/s) are unique as compared to samples from other sites (figs. 6 and 983 acre-feet, respectively. The maximum instantaneous and 10). streamflow of 376 ft3/s occurred on May 7, 2007, whereas Concentrations of trace elements, when detected, were periods of no flow were observed at the gaging station in water higher in samples from Alkali Spring, Barrel Spring-North years 2002 through 2006. Suspended-sediment concentrations Pond, Big Salt Lake, and Brazel Lake than in samples in samples from Salt Creek at the Salt Creek near Tularosa from other sites except Salt Creek (table 2–5). Otherwise, gaging station ranged from 4 to 1,570 milligrams per liter concentrations of trace elements in samples collected from (mg/L) from 1999 through 2008. Suspended-sediment sites in pupfish nonhabitat areas were generally in the same concentrations ranged from 17 to 3,430 mg/L at other Salt range as concentrations in other samples. An exception is one Creek sites. sample from South Mound Spring in which the dissolved iron Dissolved-solids concentrations in Salt Creek samples concentration (120 µg/L) was high relative to concentrations collected from 1911 through 2007 ranged from 2,290 to detected in other samples. 66,700 mg/L. Concentrations of trace elements generally In the one sample collected from Big Salt Lake in were higher in most Salt Creek samples than in most samples 1998, the ammonia (as N) concentration (2.72 mg/L) was from other areas. Nitrate (as N) concentrations in Salt Creek about one order of magnitude higher than in all other samples generally were less than 0.70 mg/L but were 1.98 samples for which ammonia concentrations were determined and 1.29 mg/L in two samples. Perchlorate was detected at 16 (table 2–6). The nitrite (as N) concentration was higher in micrograms per liter (µg/L) in one sample collected in 2000 this sample (0.5 mg/L) than in any other sample presented from the Salt Creek 4 at Range Road 7 site; this was the only in this report. In two of the three Barrel Spring samples, the sample collected with a detectable perchlorate. nitrate (as N) concentrations (1.19 and 1.28 mg/L) were The Malpais Spring near Oscura streamflow-gaging higher than in samples from all other locations except station was installed in July 2003 on the main channel that selected samples from Guilez Spring, Malpais Spring, Salt flows from Malpais Spring to the salt marsh wetlands. For Creek, and Malpais Salt Marsh Lower Lake (table 2–6). West water years 2003–8, the average annual mean streamflow Mound Spring was another site for which the orthophosphate and average annual total streamflow at the Malpais Spring (as P) concentration (0.04 mg/L in one sample) exceeded near Oscura gaging station were 6.81 ft3/s and 584 acre-feet, the range for other sites (generally equal to or less than 0.02 respectively. A maximum instantaneous streamflow of 4.3 ft3/s mg/L). Total bromide and perchlorate data (table 2–7) are occurred on both January 9, 2004, and August 19, 2006. not available for pupfish nonhabitat area sites, and triethyl Dissolved-solids concentrations for 16 Malpais Spring phosphate was not detected in any samples submitted for samples ranged from 3,882 to 5,500 mg/L. Dissolved-solids References 33 concentrations in water from Malpais Salt Marsh generally are unique as compared to samples from other sites. were higher than concentrations in water from Malpais Concentrations of trace elements, when detected, were higher Spring. The water type of samples from the Malpais Spring in samples from Alkali Spring, Barrel Spring-North Pond, Big and Malpais Salt Marsh habitat area has been consistently Salt Lake, and Brazel Lake than in samples from other sites calcium-sulfate except for one sample for which the water except Salt Creek. In one sample collected from Big Salt Lake type was sodium-sulfate. Concentrations of chromium, copper, in 1998, the ammonia (as N) concentration was about one iron, lead, manganese, and zinc appear to be anomalously high order of magnitude higher than in all other samples. in a 1982 Malpais Spring sample. In samples collected from the Malpais Spring and Malpais Salt Marsh habitat area from 1996 to 2007, concentrations of most trace elements, when References detected, were similar to or lower than concentrations at most other sites. The nitrate (as N) and nitrate plus nitrite (as N) Anderholm, S.K., and Heywood, C.E., 2003, Chemistry and concentrations generally were higher than concentrations in age of groundwater in the southwestern Hueco Bolson, samples from other sites. Isotopic data for a Malpais Spring New Mexico and Texas: U.S. Geological Survey Water- near Oscura water sample collected in 1982 indicated that Resources Investigations Report 02–4237, 16 p. the water was more than 27,900 years old, which is similar to the high end of the range of ages estimated for groundwater Basabilvazo, G.T., Myers, R.G., and Nickerson, E.L., 1994, samples from the Hueco Bolson. Geohydrology of the High Energy Laser System Test Streamflow from Main Mound Spring was estimated at Facility site, White Sands Missile Range, Tularosa Basin, 0.007 ft3/s in 1955 and 1957. From 1996 to 2001 measured south-central New Mexico: U.S. Geological Survey Water- streamflow ranged from 0.02 to 0.07 ft3/s. Dissolved-solids Resources Investigations Report 93–4192, 59 p. concentrations in samples collected between 1955 and 2007 Benson, M.A., and Dalrymple, Tate, 1967, General field and ranged from an estimated 3,760 to 4,240 mg/L in the upper office procedures for indirect discharge measurements: pond and 4,840 to 5,120 mg/L in the lower pond. Water from U.S. Geological Survey Techniques of Water-Resources the upper and lower ponds has consistently been a calcium- Investigations, book 3, chap. A1, 30 p. sulfate type. Isotopic data for a Main Mound Spring water sample collected in 1982 indicated that the water was about Bodhaine, G.L., 1968, Measurement of peak discharge at 19,600 years old and is within the range of ages estimated for culverts by indirect methods: U.S. Geological Survey groundwater samples from the Hueco Bolson. Techniques of Water-Resources Investigations, book 3, Dissolved-solids concentrations of Lost River samples chap. A3, 60 p. collected from 1984 to 1999 ranged from 8,930 to 118,000 Bradley, Robert, Bradt, G.W., Whitlock, S.G., and Dice, L.R., (estimated) mg/L. The water type of samples collected in 1984 1927, Field notes—University of Michigan-Walker-Harris and 1999 was sodium-chloride. The concentration of dissolved expedition to New Mexico: Ann Arbor, University of bromide (6.55 mg/L) was the second highest of any sample Michigan Museum of Zoology, Division of Mammals. documented in this study. Sites located in pupfish nonhabitat areas include Alkali Byrd, David, Lange, Kathy, and Beal, Linda, 2003, Water Spring, Dead Oryx Mound Spring, North Mound Spring, resources data, New Mexico, water year 2002: U.S. South Mound Spring, West Mound Spring, Big Salt Lake, Geological Survey Water-Data Report NM–02–1, 433 p. Tularosa Creek, Brazel Lake, Guilez Spring, Barrel Spring- Collyer, M.L., 2003, Ecological morphology of the White North Pond, and Barrel Spring-South Pond. Other sites for Sands pupfish (Cyprinodon tularosa): Fargo, North Dakota which the exact locations are uncertain include Alkali Flat State University, Ph.D. dissertation, 206 p. 1 and 2, Double Mound Springs-Lower and Upper Ponds, Mound Springs 7 and 25, and Mound Spring, NW of Double Cruz, R.R., 1983, Annual water-resources review, White Sands Mound Springs. Missile Range, New Mexico, 1982: U.S. Geological Survey Dissolved-solids concentrations in samples from pupfish Open-File Report 83–695, 32 p. nonhabitat area sites ranged from 1,740 mg/L to 54,200 Dunbar, N.W., 1999, Cosmogenic 36Cl-determined age of (estimated) mg/L. Water types of samples from pupfish the Carrizozo lava flows, south-central New Mexico: New nonhabitat area sites are calcium-sulfate, magnesium-sulfate, Mexico Geology, v. 21, no. 2, p. 25–29. and sodium-chloride. In general, water collected from pupfish nonhabitat area sites tends to have larger proportions of Fenneman, N.M., and Johnson, D.W., 1946, Physiographic calcium, magnesium, and sulfate than water from pupfish divisions of the conterminous United States: U.S. habitat area sites. Water from springs associated with mounds Geological Survey map, scale 1:7,000,000. in pupfish nonhabitat areas was of a similar type (calcium- Harstad, D.L., 2003, Effects of digenetic trematode sulfate) to water associated with mounds in pupfish habitat (Diplostomatidae) infection on life history traits of male areas. Alkali Spring had a sodium-chloride water type, but White Sands pupfish Cyprinodon( tularosa): Fargo, North the proportions of sodium-chloride and magnesium-sulfate Dakota State University, M.S. thesis, 96 p. 34 Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin

Hawley, J.W., 1983, Quaternary geology of Rhodes Canyon Orth, D.J., 1983, Aquatic habitat measurements, in Nielsen, (RATSCAT) Site, in Eidenbach, P.L., ed., The prehistory L.A., and Johnson, D.L., eds., Fisheries techniques: of Rhodes Canyon, New Mexico: Tularosa, New Mexico, Bethesda, Maryland, American Fisheries Society, Human Systems Research, Inc., Report 8302, p. 17–32. p. 61–84. Hawley, J.W., 1993, Geomorphic setting and late Quaternary Pittenger, J.S., and Springer, C.L., 1996, White Sands pupfish history of pluvial-lake basins in the southern New Mexico status report—1995: Report prepared for the White Sands region: New Mexico Bureau of Mines and Mineral Pupfish Conservation Team, 31 p. Resources Open-File Report 391, 28 p. Pittenger, J.S., and Springer, C.L., 1999, Native range and Herrick, C.L., 1900, The geology of the White Sands of New conservation of the White Sands pupfish Cyprinodon( Mexico: Journal of Geology, v. 8, p. 112–128. tularosa): Southwestern Naturalist, v. 44, no. 2, Hirsch, R.M., and Norris, J.M., 2001, National Streamflow p. 157–165. Information Program—Implementation plan and progress Rantz, S.E., and others, 1982, Measurement and computation report: U.S. Geological Survey Fact Sheet 048–01. of streamflow: U.S. Geological Survey Water-Supply Paper Jester, D.B., and Suminski, R.R., 1982, Age and growth, 2175, 2 v., 631 p. fecundity, abundance, and biomass production of the White Risser, D.W., 1988, Simulated water-level and water-quality Sands pupfish, Cyprinodon tularosa (Cyprinodontidae) in a changes in the bolson-fill aquifer, Post Headquarters area, desert pond: The Southwestern Naturalist, v. 27, p. 43–54. White Sands Missile Range, New Mexico: U.S. Geological Lichvar, Robert, and Sprecher, Steven, 1997, Draft report of Survey Water-Resources Investigations Report 87–4152, the delineation of waters of the United States, White Sands 71 p. Missile Range-Malpais Spring wetland: U.S. Army Corps of Salyards, S.L., 1991, A possible Mid-Holocene Age of the Engineers, Waterways Experiment Station, 10 p. Carrizozo malpais from paleomagnetics using secular Ligon, J.S., 1913, Physiography, 1913—Field reports of variation magnetostratigraphy, in Barker, J.M., Kues, the U.S. Fish and Wildlife Service: Archives and Special B.S., Austin, G.S., and Lucas, S.G., eds., Geology of the Collections of the Smithsonian Institution, Record Unit Sierra Blanca, Sacramento and Capitan Ranges, New 7176, Box 74, Folder 24. Mexico: New Mexico Geological Society, 42d annual field conference, Guidebook, p. 153–157. Lucas, S.G., and Hawley, J.W., 2002, The Otero Formation, Pleistocene lacustrine strata in the Tularosa Basin, southern Stockwell, C.A., Mulvey, Margaret, and Jones, A.G., 1998, New Mexico: New Mexico Geological Society, 53d field Genetic evidence for two evolutionarily significant units conference, Guidebook, p. 277–283. of White Sands pupfish: Conservation, v. 1, p. 213–225. Matthai, H.F., 1967, Measurement of peak discharge at width contractions by indirect methods: U.S. Geological Survey Suminski, R.R., 1977, Life history of the White Sands pupfish Techniques of Water-Resources Investigations, book 3, and distribution of Cyprinodon in New Mexico: Las Cruces, chap. A4, 44 p. New Mexico State University, M.S. thesis, 80 p. Meinzer, O.E., and Hare, R.F., 1915, Geology and water Turner, P.R., 1987, Ecology and management needs of the resources of Tularosa Basin, New Mexico: U.S. Geological White Sands pupfish in the Tularosa Basin of New Mexico: Survey Water-Supply Paper 343, 317 p. Las Cruces, New Mexico State University, Department of Fishery and Wildlife Sciences, 127 p. Miller, R.R., and Echelle, A.A., 1975, Cyprinodon tularosa, a new cyprinodontid fish from the Tularosa Basin, New U.S. Environmental Protection Agency [n.d.], Drinking Mexico: Southwestern Naturalist, v. 19, no. 4. p. 365–377. water contaminants—National primary drinking water Naus, C.A., 2002, Conceptual model of the bolson-fill aquifer, regulations: Accessed September 21, 2004, at http://www. Soledad Canyon area, Doña Ana County, New Mexico: epa.gov/safewater/mcl.html. New Mexico Geology Society, 53d field conference, U.S. Geological Survey, variously dated, National field manual Guidebook, p. 309–318. for the collection of water-quality data: U.S. Geological Orr, B.R., and Risser, D.W., 1992, Geohydrology and potential Survey Techniques of Water-Resources Investigations, effects of development of freshwater resources in the book 9, chaps. A1–9. (Also available at http://pubs.water. northern part of the Hueco Bolson, Doña Ana and Otero usgs.gov/twri9A/.) Counties, New Mexico, and El Paso County, Texas: U.S. U.S. Geological Survey, 2013, National Water Information Geological Survey Water-Resources Investigations Report System—Web interface: Accessed December 12, 2013, at 91–4082, 92 p. http://waterdata.usgs.gov/nwis. References 35

Weir, J.E., Jr., 1965, Geology and availability of ground water White Sands National Monument [n.d.], White Sands in the northern part of the White Sands Missile Range and National Monument—Nature and science: Accessed August vicinity, New Mexico: U.S. Geological Survey Water- 5, 2004, at http://whitesands.areaparks.com/parkinfo. Supply Paper 1801, 78 p. html?pid=28369. Wood, W.W., 1976, Guidelines for collection and field analysis White Sands Missile Range, 2003, GIS data—White Sands of ground-water samples for selected unstable constituents: Missile Range: Directorate of Environment and Safety, U.S. Geological Survey Techniques of Water-Resources White Sands Missile Range, CD-ROM (3 disks). Investigations, book 9, chap. D2, 24 p.

Publishing support provided by Lafayette and Rolla Publishing Service Centers Naus and others—Compilation of Hydrologic Data for White Sands Pupfish Habitat and Nonhabitat Areas, Northern Tularosa Basin—DS 810 ISSN 2327-638X (online) http://dx.doi.org/10.3133/ds810