A systematic study of the waters likely to be utilized on the Reclamation Service projects was made in order to determine the influence of the salinity of the waters on the growth of vegetation and the effect of suspended matter in silting canals and reservoirs. The work was begun early in 1905, under the direction of Thomas H. Means, engineer, and was continued during 1906 and until May, 1907, under the direction of W. H. Heileman, engineer. The analyses were made in a laboratory established at quarters provided by the University of California at Berkeley, Cal., by C. H. Stone, P. L. McCreary, F. M. Eaton, O. J. Hawley, W. C. Riddell, F. T. Berry, H. A. Burns, J. H. Hampson, J. A. Pearce, and M. Vaygouny, the greater part of the work being that of the first five named. C. H. Stone was chemist in charge at the beginning of the investigations and is chiefly responsible for the plan of the analytical work and the methods of analysis.
The results of the investigations were prepared for publication under instructions from F. H. Newell, Director of the United States Reclamation Service, by Herman Stabler, assistant engineer, who assembled and checked- the analyses, compiled the accompanying stream-flow data from records of the United States Geological Survey, and computed daily discharge of suspended matter and dissolved solids, under the supervision of D. W. Murphy, engineer in charge of Washington office engineering.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp274","usgsCitation":"Stabler, H., 1911, Some stream waters of the Western United States, with chapters on sediment carried by the Rio Grande and the industrial application of water analyses: U.S. Geological Survey Water Supply Paper 274, 188 p., https://doi.org/10.3133/wsp274.","productDescription":"188 p.","numberOfPages":"187","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0274/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0274/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7813","contributors":{"authors":[{"text":"Stabler, Herman","contributorId":83498,"corporation":false,"usgs":true,"family":"Stabler","given":"Herman","email":"","affiliations":[],"preferred":false,"id":145696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2098,"text":"wsp217 - 1908 - Water resources of Beaver Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-12T07:54:00","indexId":"wsp217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1908","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"217","title":"Water resources of Beaver Valley, Utah","docAbstract":"Location and extent of area examined. Beaver Valley is located in Beaver County, in southwestern Utah, about 175 miles south of Salt Lake. It lies between the Tushar Mountains on the east and the Beaver Mountains on the west. The principal town of the valley is Beaver, which is most conveniently reached from Milford, a station on the San Pedro, Los Angeles and Salt Lake Railroad. The valley, together with its neighboring highlands, occupies the eastern third of Beaver County, an area of about 1,200 square miles. A large part of this area, however, is rocky upland and unproductive desert, the tillable land comprising a comparatively small area in the immediate vicinity of the streams.
Purpose and scope of work. The purpose of this paper is to present information concerning the waters of Beaver Valley and to point out ways and means of increasing their usefulness. The presence of a large amount of water in Beaver Valley results from local topograhic conditions, the water being supplied by precipitation in the highland to the east. Its conservation and distribution result from geologic conditions, the water being held in loose gravel and sand, which are more or less confined between ridges of consolidated rocks. The rock basins were formed partly by erosion and partly by faulting and surface deformation. In order to accomplish the purpose in view it is therefore necessary to describe the geographic and geologic conditions in Beaver Valley and neighboring regions.
The investigation included the determination of the flow of streams and springs, of the manner of occurrence and quantity of the underground waters as shown by the geologic and geographic conditions of the region and by the distribution of springs and wells, and of the chemical character of the waters with reference to their adaptability to domestic use and to irrigation. The chemical data were obtained (a) by field assays, which are approximately correct and probably of sufficient accuracy to be of value in comparing the various waters; (b) by more exact analyses, some of which were made in the laboratory of the United States Geological Survey by W. M. Barr, and others by Herman Harms, State chemist of Utah, for the San Pedro, Los Angeles and Salt Lake Railroad; and (c) by sanitary analyses, made also by Herman Harms.
Cooperation. The work was done during the summer of 1906, the United States Geological Survey cooperating with the State of Utah through Caleb Tanner, State engineer, and with the county of Beaver through the supervisors of the county. In collecting the information the writer was assisted by J. F. Hoyt, of Nephi, Utah.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp217","usgsCitation":"Lee, W.T., 1908, Water resources of Beaver Valley, Utah: U.S. Geological Survey Water Supply Paper 217, 57 p., https://doi.org/10.3133/wsp217.","productDescription":"57 p.","numberOfPages":"60","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0217/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.13034057617188,\n 38.06539235133249\n ],\n [\n -113.13034057617188,\n 38.68014968334624\n ],\n [\n -112.39837646484375,\n 38.68014968334624\n ],\n [\n -112.39837646484375,\n 38.06539235133249\n ],\n [\n -113.13034057617188,\n 38.06539235133249\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b11f2","contributors":{"authors":[{"text":"Lee, Willis Thomas","contributorId":52949,"corporation":false,"usgs":true,"family":"Lee","given":"Willis","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":144670,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2115,"text":"wsp183 - 1907 - Flowing wells and municipal water supplies in the middle and northern portions of the southern peninsula of Michigan","interactions":[],"lastModifiedDate":"2017-01-11T14:20:29","indexId":"wsp183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1907","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"183","title":"Flowing wells and municipal water supplies in the middle and northern portions of the southern peninsula of Michigan","docAbstract":"A large amount of data on water supplies was collected by the writer in the course of glacial investigations made under the direction of Prof. T. C. Chamberlin in the last five years in the Southern Peninsula of Michigan. These investigations resulted in a partial acquaintance with conditions in about 200 separate flowing-well districts and brought out matters of such exceptional importance that arrangements were made to extend them by examining each of the flowing-well districts in the State sufficiently to determine its essential characteristics, present state of development, and probable capacity for future development. It was arranged also that the quality of various classes of water, both surface and underground, as well as water supplies of, cities and villages, should be given attention. As the mineral waters of the State had already been discussed in some detail by the State geologist, Dr. A. C. Lane, in Water-Supply Paper No. 31 of the United States Geological Survey, it was deemed unnecessary to prepare another report on that subject, but arrangements were made with Doctor Lane for embodying in this report the large amount of material which had accumulated at his office relative to other classes of water supply, and also for furnishing reports on certain counties in which special investigations had been carried on by the State survey. The results of all these studies, so far as they apply to the middle- and northern counties (see fig. 1, on next page), are embodied in the present report; the remainder appears in a companion report on the southern counties of the Southern Peninsula of Michigan.
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Frank","contributorId":77512,"corporation":false,"usgs":true,"family":"Leverett","given":"Frank","email":"","affiliations":[],"preferred":false,"id":144695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2116,"text":"wsp182 - 1906 - Flowing wells and municipal water supplies in the southern portion of the southern peninsula of Michigan","interactions":[],"lastModifiedDate":"2017-01-11T14:35:15","indexId":"wsp182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"182","title":"Flowing wells and municipal water supplies in the southern portion of the southern peninsula of Michigan","docAbstract":"A large amount of data on water supplies was collected by the writer in the course of glacial investigations made under the direction of Prof. T. C. Chamberlin in the last five years in the Southern Peninsula of Michigan. These investigations resulted in a partial acquaintance with conditions in about 200 separate flowing-well districts and brought out matters of such exceptional importance that arrangements were made to extend them by examining each of the flowing-well districts in the State sufficiently to determine its essential characteristics, present state of development, and probable capacity for future development. It was arranged also that the quality of various classes of waters, both surface and underground, as well as water supplies of the cities and villages, should be given attention. As the mineral waters of the State had already been discussed in some detail by the State geologist, Dr. A. C. Lane, in Water-Supply Paper No. 31 of the United States Geological Survey, it was deemed unnecessary to prepare another report on that subject, but arrangements were made with Doctor Lane for embodying in this report the large amount of material which had accumulated at his office relative to other classes of water supply, and also for furnishing reports on certain counties in which special investigations had been carried on by the State survey. The results of all these studies, so far as they apply to the southern counties (see fig. 1), are embodied in the present report; the remainder will appear in a companion report on the middle and northern counties of the Southern Peninsula of Michigan.
","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp182","usgsCitation":"Leverett, F., 1906, Flowing wells and municipal water supplies in the southern portion of the southern peninsula of Michigan: U.S. Geological Survey Water Supply Paper 182, xi, 292, iii p., https://doi.org/10.3133/wsp182.","productDescription":"xi, 292, iii p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":27704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0182/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0182/report-thumb.jpg"}],"country":"United 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Frank","contributorId":77512,"corporation":false,"usgs":true,"family":"Leverett","given":"Frank","email":"","affiliations":[],"preferred":false,"id":144696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32886,"text":"pp52 - 1906 - Geology and underground waters of the Arkansas Valley in eastern Colorado","interactions":[],"lastModifiedDate":"2017-04-25T14:37:34","indexId":"pp52","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"52","title":"Geology and underground waters of the Arkansas Valley in eastern Colorado","docAbstract":"In the valley of Arkansas River in southeastern Colorado there is an area of considerable extent in which artesian flows are available. During the last ten years numerous wells have been sunk to develop this important resource and, in most cases in the lower lands, abundant water supplies have been obtained. The principal water-bearing bed is the \"Dakota\" formation, which consists of two sheets of porous sandstone separated by a small body of clay and overlain in the greater portion of the area by a mass of impervious shales. The sandstones receive their waters from, rainfall and from the sinking of streams along the foothills of the Rocky Mountains and on some of the higher slopes south of the Arkansas Valley. In the passage of this sandstone underground, the waters which it contains are held down by the overlying shales, but, as some of the sandstone outcrops are at relatively low levels to the east only a moderate head or pressure is sustained. On account of this low head, artesian flows are available only in the lower lands, and one of the principal objects of this investigation has been the determination of the area in which flows are to be expected. The \"Dakota\" sandstone and associated formations do not lie level, or even slope regularly to the east, but are flexed into low arches and shallow troughs of considerable complexity of configuration. Accordingly, in investigating this source of water supply, it has been necessary to ascertain the structure and distribution of the various formations in order to indicate the variations in depth to the water-bearing stratum. The principal results of these investigations are set forth: (1) In the geologic map (Pl. VI), which shows the distribution of the formations on the surface; (2) in the map, Pl. XXV, which shows the depth to the water-bearing horizon, the area in which flows are expected, the head of the underground waters, and other features, and (3) in the cross sections (Pls. VII and XXIII), which show the principal underground features. The investigation has been in progress for several years and is an extension of the preliminary examination of the region by G. K. Gilbert in 1894 and 1895.
For the western portion of the area the maps and texts of the Pueblo, Elmoro, Walsenburg, Spanish Peaks, and Pikes Peak folios have been utilized as far as practicable. For the central and eastern portions the larger features of the geology have been specially mapped, and considerable detailed mapping has been done in the region south and southeast of Canyon and Colorado Springs. In the field work I have been assisted by Mr. C. A. Fisher, who has examined in detail the Nepesta quadrangle and contributed numerous other data. Dr. W. S. Tangier Smith and Messrs. C. E. Sicbenthal and W. T. Lee have made observations in certain areas. Much valuable information respecting wells has been furnished by Mr. William Archer, of the Atchison, Topeka and Santa Fe Railway Company, and Mr. C. H. McVay, well driller at Rocky Ford.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp52","usgsCitation":"Darton, N.H., 1906, Geology and underground waters of the Arkansas Valley in eastern Colorado: U.S. Geological Survey Professional Paper 52, Report: iv, 90 p.; 2 Plates: 33.18 x 27.43 inches and 32.29 x 27.27 inches, https://doi.org/10.3133/pp52.","productDescription":"Report: iv, 90 p.; 2 Plates: 33.18 x 27.43 inches and 32.29 x 27.27 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":340321,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0052/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0052/report-thumb.jpg"},{"id":340322,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0052/plate-25.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0052/report.pdf","text":"Report","size":"7.41 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.5,\n 39.5\n ],\n [\n -102,\n 39.5\n ],\n [\n -102,\n 37\n ],\n [\n -105.5,\n 37\n ],\n [\n -105.5,\n 39.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6841c9","contributors":{"authors":[{"text":"Darton, N. H.","contributorId":71523,"corporation":false,"usgs":true,"family":"Darton","given":"N.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1248,"text":"wsp149 - 1905 - Preliminary list of deep borings in the United States","interactions":[],"lastModifiedDate":"2017-09-12T07:57:57","indexId":"wsp149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"149","title":"Preliminary list of deep borings in the United States","docAbstract":"The first preliminary list of deep borings in the United States was issued as Water-Supply Papers Nos. 57 and 61. The present publication includes all of the wells listed in these two papers, together with many additional borings, mostly of recent date. Messrs. M. L. Fuller and A. C. Veatch, of the eastern section of hydrology, and other geologists of the Survey have contributed many new data. Descriptions of borings published in reports issued since 1901 have been incorporated as far as practicable. All the entries are by counties. The wells and borings reported in the paper are all more than 400 feet in depth. The information concerning them has been obtained partly from replies to circular letters sent to all parts of the United States and partly from geological reports and other published sources. Owing to the difficulty of obtaining replies to the circulars, to lack of knowledge on the part of correspondents, and to the incompleteness of published records, doubtless there are borings which have not been reported. In regions of oil and gas wells, where borings are numerous, the individual wells can not be listed here, but representative wells are given. References to logs or records of the wells or extended descriptions of them are given in footnotes, and after the list of wells in each State there is added a list of the principal publications relating to deep borings in that State.
The bearing of the information given in the columns of the lists probably is apparent unless, perhaps, in the one headed \"Height to which the water rises.\" In this column an entry such as \"-45\" indicates that the water rises to within 45 feet of the surface; \"+45\" indicates that it is a flowing well and has sufficient head to raise the water 45 feet above the surface in an open pipe 45 feet or more in height. The yield in gallons per minute usually is estimated. Depths and diameters often have been reported from memory and different sources of publication sometimes give different figures. Most wells which are not stated to be \"for oil,\" \"for gas,\" \"brine,\" \"abandoned,\" etc., in the remarks column, or \"not any\" in the yield column, generally afford more or less water. Many of the gas and oil wells, active or abandoned, yield salt water.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp149","usgsCitation":"Darton, N.H., 1905, Preliminary list of deep borings in the United States (2d ed. with additions.): U.S. Geological Survey Water Supply Paper 149, 175 p., https://doi.org/10.3133/wsp149.","productDescription":"175 p.","numberOfPages":"180","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0149/report-thumb.jpg"}],"country":"United States","edition":"2d ed. with additions.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d96f","contributors":{"authors":[{"text":"Darton, Nelson Horatio","contributorId":78307,"corporation":false,"usgs":true,"family":"Darton","given":"Nelson","email":"","middleInitial":"Horatio","affiliations":[],"preferred":false,"id":143436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70273254,"text":"70273254 - null - An empirical algorithm for estimating agricultural and riparian evapotranspiration using MODIS Enhanced Vegetation Index and ground measurements of ET. II. Application to the lower Colorado River, U.S.","interactions":[],"lastModifiedDate":"2025-12-23T16:00:36.737075","indexId":"70273254","displayToPublicDate":"2009-11-20T09:55:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3250,"text":"Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"An empirical algorithm for estimating agricultural and riparian evapotranspiration using MODIS Enhanced Vegetation Index and ground measurements of ET. II. Application to the lower Colorado River, U.S.","docAbstract":"Large quantities of water are consumed by irrigated crops and riparian vegetation in western U.S. irrigation districts. Remote sensing methods for estimating evaporative water losses by soil and vegetation (evapotranspiration, ET) over wide river stretches are needed to allocate water for agricultural and environmental needs. We used the Enhanced Vegetation Index (EVI) from MODIS sensors on the Terra satellite to scale ET over agricultural and riparian areas along the Lower Colorado River in the southwestern U.S., using a linear regression equation between ET of riparian plants and alfalfa measured on the ground, and meteorological and remote sensing data, with an error or uncertainty of about 20%. The algorithm was applied to irrigation districts and riparian areas from Lake Mead to the U.S./Mexico border. The results for agricultural crops were similar to results produced by crop coefficients developed for the irrigation districts along the river. However, riparian ET was only half as great as crop coefficient estimates set by expert opinion, equal to about 40% of reference crop evapotranspiration. Based on reported acreages in 2007, agricultural crops (146,473 ha) consumed 2.2 × 109 m3 yr−1 of water. All riparian shrubs and trees (47,014 ha) consumed 3.8 × 108 m3 yr−1, of which saltcedar, the dominant riparian shrub (25,044 ha), consumed 1.8 × 108 m3 yr−1, about 1% of the annual flow of the river. This method could supplement existing protocols for estimating ET by providing an estimate based on the actual state of the canopy as determined by frequent-return satellite data.
","language":"English","publisher":"MDPI","doi":"10.3390/rs1041125","usgsCitation":"Murray, R.S., Nagler, P.L., Morino, K., and Glenn, E., An empirical algorithm for estimating agricultural and riparian evapotranspiration using MODIS Enhanced Vegetation Index and ground measurements of ET. II. Application to the lower Colorado River, U.S.: Remote Sensing, v. 1, no. 4, p. 1125-1138, https://doi.org/10.3390/rs1041125.","productDescription":"14 p.","startPage":"1125","endPage":"1138","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":498057,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/rs1041125","text":"Publisher Index Page"},{"id":497940,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Nevada","otherGeospatial":"lower Colorado River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.8813192791255,\n 36.97080066185404\n ],\n [\n -116.96456312629869,\n 36.97080066185404\n ],\n [\n -116.96456312629869,\n 32.699643980926254\n ],\n [\n -110.8813192791255,\n 32.699643980926254\n ],\n [\n -110.8813192791255,\n 36.97080066185404\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2009-11-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Murray, R. Scott","contributorId":64468,"corporation":false,"usgs":true,"family":"Murray","given":"R.","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":952887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nagler, Pamela L. 0000-0003-0674-103X pnagler@usgs.gov","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":1398,"corporation":false,"usgs":true,"family":"Nagler","given":"Pamela","email":"pnagler@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":952888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morino, Kiyomi","contributorId":78210,"corporation":false,"usgs":true,"family":"Morino","given":"Kiyomi","email":"","affiliations":[],"preferred":false,"id":952889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glenn, Edward P.","contributorId":56542,"corporation":false,"usgs":false,"family":"Glenn","given":"Edward P.","affiliations":[{"id":13060,"text":"Department of Soil, Water and Environmental Science, University of Arizona","active":true,"usgs":false}],"preferred":false,"id":952890,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}