{"pageNumber":"6221","pageRowStart":"155500","pageSize":"25","recordCount":184934,"records":[{"id":24979,"text":"pp850 - 1973 - Geological Survey research 1973","interactions":[],"lastModifiedDate":"2025-01-07T17:39:30.968268","indexId":"pp850","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"850","title":"Geological Survey research 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp850","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Geological Survey research 1973: U.S. Geological Survey Professional Paper 850, viii, 366 p., https://doi.org/10.3133/pp850.","productDescription":"viii, 366 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":421216,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92939.htm","text":"Biostratigraphic record extended to Early Silurian or Ordovician in western Brooks Range","linkFileType":{"id":5,"text":"html"}},{"id":53964,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0850/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118859,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0850/report-thumb.jpg"},{"id":465772,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92944.htm","text":"Upper Lower Permian rocks discovered in northeastern Alaska","linkFileType":{"id":5,"text":"html"}},{"id":465773,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92945.htm","text":"New evidence bearing on age of Wales Group","linkFileType":{"id":5,"text":"html"}},{"id":465774,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92947.htm","text":"Late Ordovician (Ashgillian) age of volcanic rocks, north-central Maine","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6876ee","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23312,"text":"ofr73102 - 1973 - Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr73102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-102","title":"Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington","docAbstract":"A model of the circulation and quality of water in the Duwamish River estuary has been sufficiently developed to allow prediction of the effects of a proposed widening and deepening of waterways on residence time and dissolved oxygen in the estuary's salt wedge. For a low river-discharge period in August 1970, use of the model yielded an estimated residence time of wedge water to be 6.3 days in the present waterways estuary and 8.6 days in the wider and deeper proposed-waterways estuary--a 37-percent increase. June-September 1970 and for the estuary about 4 miles upstream from its mouth, the model estimates indicate that dissolved-oxygen values in the wedge of the proposed-waterways estuary would be as much as 1.4 milligrams per liter lower and would average 0.4 milligram per liter lower than (average difference significant at 95-percent confidence level) dissolved-oxygen values in the wedge of the present-waterways estuary. \r\n\r\nExtrapolation to low dissolved-oxygen values of a regression between the predicted dissolved oxygen for both the proposed and present-waterways estuaries suggests that 4 miles upstream of the estuary mouth oxygen would be completely depleted from the proposed-waterways estuary wedge whereas there still would be 0.2 milligram of oxygen per liter of water in the wedge of the present-waterways estuary.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr73102","issn":"0094-9140","usgsCitation":"Haushild, W., and Stoner, J., 1973, Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington: U.S. Geological Survey Open-File Report 73-102, 13 p. :ill., map ;27 cm., https://doi.org/10.3133/ofr73102.","productDescription":"13 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":155134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0102/report-thumb.jpg"},{"id":52612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fde2","contributors":{"authors":[{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":189874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":189875,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2898,"text":"wsp2029C - 1973 - Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp2029C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2029","chapter":"C","title":"Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado","docAbstract":"A method to determine evapotranspiration from ground water was tested at four sites in the flood plain of the Arkansas River in Colorado. Approximate ground-water budgets were obtained by analyzing water-level data from observation wells installed in five-point arrays. The analyses were based on finite difference approximations of the differential equation describing ground-water flow. \r\n\r\nData from the sites were divided into two groups by season. It was assumed that water levels during the dormant season were unaffected by evapotranspiration of ground water or by recharge, collectively termed 'accretion.' Regression analyses of these data were made to provide an equation for separating the effects of changes in aquifer storage and of aquifer heterogeneity from those due to accretion during the growing season. The data collected during the growing season were thus analyzed to determine accretion.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2029C","usgsCitation":"Weeks, E.P., and Sorey, M., 1973, Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado: U.S. Geological Survey Water Supply Paper 2029, iii, 27 p. ;24 cm., https://doi.org/10.3133/wsp2029C.","productDescription":"iii, 27 p. ;24 cm.","costCenters":[],"links":[{"id":138379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2029c/report-thumb.jpg"},{"id":29564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2029c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046a9","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":145977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2858,"text":"wsp1969 - 1973 - Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T11:55:59","indexId":"wsp1969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1969","title":"Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan","docAbstract":"<p>The Tri-County region, consisting of Clinton, Eaton, and Ingham Counties, is an area of 1,697 square miles in Michigan's Lower Peninsula and has as its hub the Lansing metropolitan area. The land surface ranges in altitude from about 700 to about 1,000 feet. The region receives an average of about 31 inches of precipitation each year. </p><p>The population is nearing 400,000 and by 1990 will be near 600,000. Average daily water use is slightly more than 30 million gallons today; by 1980 it will be about 50 million gallons, and by 1990 it will probably be about 70 million gallons. </p><p>The Tri-County region is drained by seven river systems. The median annual 7 -day mean low flows of the principal streams in these systems were measured at the point farthest downstream within the region. These values, in cubic feet per second, are as follows: Grand River, 180; Maple River, 34; Looking Glass River, 28; Red Cedar River, 30; Portage Creek, 15; Battle Creek, 20; and Thornapple River, 24-a total of 331 cubic feet per second or about 220 million gallons per day. The areal variance in 7-day low-flow runoff ranges from 0 to 0.15 cubic foot per second per square mile. </p><p>The principal source of ground water in the Tri-County region is a complex aquifer system composed of the Saginaw and Grand River Formations and some of the overlying glacial sediments. This aquifer yields between 300 and 700 gallons per minute to individual wells in much of the western half of Ingham County, in the eastern half of Clinton County, in a small area in southeastern Clinton County, and in northeastern Eaton County. In some parts of the region, the glacial sediments are favorable for development of moderate to large supplies of water. Minor aquifers in the region are the Bayport, Michigan, and Marshall Formations. </p><p>Providing water supplies in the future requires complete and comprehensive water-management programs. Such management programs involve determining which of several alternative water-development systems is the best. Some of the chief factors and methods that must be considered when planning these systems are combined use of ground and surface water, artificial recharge, treatment of wastes, use of storage reservoirs, and importation of water from the Great Lakes.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1969","usgsCitation":"Vanlier, K.E., Wood, W., and Brunett, J.O., 1973, Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan: U.S. Geological Survey Water Supply Paper 1969, Document: vii, 111 p.; 3 Plates: 35.70 x 31.97 inches or smaller, https://doi.org/10.3133/wsp1969.","productDescription":"Document: vii, 111 p.; 3 Plates: 35.70 x 31.97 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":139081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1969/report-thumb.jpg"},{"id":247253,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-1.pdf","size":"5337","linkFileType":{"id":1,"text":"pdf"}},{"id":247254,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-2.pdf","size":"10148","linkFileType":{"id":1,"text":"pdf"}},{"id":247255,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-3.pdf","size":"13282","linkFileType":{"id":1,"text":"pdf"}},{"id":29452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1969/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Clinton County, Eaton County, Ingham County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.3681,43.1172],[-84.3675,42.9561],[-84.3679,42.9439],[-84.3666,42.861],[-84.3668,42.8561],[-84.3649,42.7746],[-84.1593,42.7779],[-84.1519,42.685],[-84.146,42.5999],[-84.1402,42.4239],[-84.2539,42.4236],[-84.2607,42.4242],[-84.3676,42.4242],[-84.3677,42.4224],[-84.4864,42.4215],[-84.6026,42.4215],[-84.7207,42.4209],[-84.83,42.421],[-84.8375,42.4215],[-84.9561,42.4221],[-85.0667,42.4215],[-85.0736,42.4211],[-85.0738,42.5956],[-85.0745,42.7707],[-84.9577,42.7712],[-84.8391,42.7706],[-84.8376,42.857],[-84.8393,42.9434],[-84.8382,43.1199],[-84.6022,43.1185],[-84.3681,43.1172]]]},\"properties\":{\"name\":\"Clinton\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99fe","contributors":{"authors":[{"text":"Vanlier, Kenneth Eugene","contributorId":6840,"corporation":false,"usgs":true,"family":"Vanlier","given":"Kenneth","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":145916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brunett, Jilann O.","contributorId":92230,"corporation":false,"usgs":true,"family":"Brunett","given":"Jilann","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":145917,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2861,"text":"wsp1974 - 1973 - Water resources of the New Jersey part of the Ramapo River basin","interactions":[{"subject":{"id":56068,"text":"ofr70352 - 1970 - Water resources of the New Jersey part of the Ramapo River basin","indexId":"ofr70352","publicationYear":"1970","noYear":false,"title":"Water resources of the New Jersey part of the Ramapo River basin"},"predicate":"SUPERSEDED_BY","object":{"id":2861,"text":"wsp1974 - 1973 - Water resources of the New Jersey part of the Ramapo River basin","indexId":"wsp1974","publicationYear":"1973","noYear":false,"title":"Water resources of the New Jersey part of the Ramapo River basin"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1974","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1974","title":"Water resources of the New Jersey part of the Ramapo River basin","docAbstract":"The Ramapo River, a major stream in the Passaic River basin, drains an area of 161 square miles, 70 percent of which is in Orange and Rockland Counties, N.Y., and 30 percent is in Bergen and Passaic Counties, N.J. This report describes the hydrology of the New Jersey part of the basin and evaluates the feasibility of developing large ground-water supplies from the stratified drift in the Ramapo River valley by inducing recharge to the aquifer from the river. The ground water and surface water of the basin are considered as a single resource because the development of either ground water or surface water affects the availability of the other. \r\n\r\nPrecambrian gneiss, sparsely mantled with Pleistocene glacial drift, underlies the basin west of the Ramapo River in New Jersey. To the east, bedrock consists of the Watchung Basalt and of shale, sandstone, and conglomerate of the Brunswick Formation of Triassic age. Glacial drift occurs nearly everywhere in the eastern part of the basin, and deposits of stratified drift more than 100 feet thick occur in the Ramapo valley. Average annual runoff at Pompton Lakes accounts for 25 inches of the 45 inches of annual precipitation in the New Jersey part of the basin, and the remaining 20 inches is accounted for by evapotranspiration. Streamflow is highly variable--particularly in the area underlain by gneissic rocks-because of the low storage capacity of the rocks and the rough topography. \r\n\r\nMany of the small tributaries go dry during extended periods of no precipitation. Small domestic supplies of ground water can be obtained nearly everywhere, but the Brunswick Formation is the only consolidated-rock aquifer in the basin that can be depended upon to yield 100-200 gallons per minute to wells. Supplies of more than 1,000 gallons per minute are available from wells tapping the stratified drift in the Ramapo valley. The drift supplies 75 percent of the ground water pumped for public supply in the basin. Sustained ground-water yield in upland areas, based on stream base-flow recession, is estimated to be 200,000-300,000 gallons per day per square mile for the drift-covered Brunswick Formation and about 100,000-200,000 gallons per day per square mile for the gneiss and basalt. Potential sustained yield of the stratified drift in the valley depends on the availability of the streamflow and on the induced rate of infiltration. \r\n\r\nPumping from the stratified drift results in a reduction in streamflow, which may be undesirable, mainly because of prior downstream water rights. On the basis of the storage available in the stratified drift and an analysis of daily flow during the drought period of October 1964 to September 1967 at Pompton Lakes, 20-25 million gallons per day of Ramapo River water are available for development after existing downstream water requirements are supplied. However, some low-flow augmentation will be. necessary to insure downstream rights. Rates of infiltration computed from seepage losses observed near Mahwah indicate that at least 11 million gallons per day, on an average basis, can be infiltrated from the river by the pumping of wells tapping the stratified drift. The use of recharge pits and spreading areas would increase the rate of infiltration. Losses from the Ramapo River could be minimized by returning treated sewage effluent directly to the river or, preferably, by recharging the stratified-drift aquifer with the treated effluent. \r\n\r\nGround-water quality and surface-water quality at times of low-flow vary according to the type of rock from which the water is obtained. Water from the gneiss is low in dissolved solids--less than 127 mg/l (milligrams per liter)--and soft to moderately hard--less than 94 rag/l. Water from the Brunswick Formation is more mineralized--total dissolved-solids content is as much as 278 mg/1 and hardness as much as 188 mg/1. Water from the stratified drift is generally intermediate in quality--that is, total dissolved-solids content is as ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1974","usgsCitation":"Vecchioli, J., and Miller, E., 1973, Water resources of the New Jersey part of the Ramapo River basin: U.S. Geological Survey Water Supply Paper 1974, vi, 77 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1974.","productDescription":"vi, 77 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1974/report-thumb.jpg"},{"id":29456,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29457,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29458,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29459,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1974/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef13d","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":145920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, E.G.","contributorId":44132,"corporation":false,"usgs":true,"family":"Miller","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":145921,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2193,"text":"wsp2009C - 1973 - Chemical quality of surface water in the Flaming Gorge Reservoir area, Wyoming and Utah","interactions":[],"lastModifiedDate":"2017-09-04T11:04:36","indexId":"wsp2009C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2009","chapter":"C","title":"Chemical quality of surface water in the Flaming Gorge Reservoir area, Wyoming and Utah","docAbstract":"<p>Construction of Flaming Gorge Dam on the Green River by the U.S. Bureau of Reclamation started in 1959, and storage began in November 1962. A reconnaissance study was made during the period 1966-68 to determine the effects of the reservoir on the chemical quality of the effluent water and to describe the quality of the impounded water and inflowing water.</p><p>The major inflow to the reservoir is from the Green River, which contributes an average of 81 percent of the water and 59 percent of the inflow load of dissolved solids. Together, Blacks Fork and Henrys Fork contribute an average of about 16 percent of the water and about 23 percent of the dissolved-solids load, whereas minor tributaries contribute approximately 3 percent of the total inflow water to the reservoir, but about 18 percent of the total incoming load of dissolved solids.</p><p>The concentration of dissolved solids in the reservoir in October 1966 was about 150 mg/l (milligrams per liter) greater than the concentration of the 1962-66 inflow and in September 1968 about 95 mg/l greater than the concentration of the 1962-68 inflow. The increased concentration is due. mostly to leaching of minerals from the reservoir bottom. For the 1963-68 water years, about 1.2 million tons of dissolved solids was leached from inundated areas. The major observable difference between the chemical composition of the inflow during 1963-66 and that of the reservoir in 1966 is an increase in the percentage of sulfate and a decrease in the percentage of bicarbonate. Impoundment of water in Flaming Gorge Reservoir during the 1963-68 water years caused the concentration of dissolved solids in the river system to increase by 130 mg/l, or about 32 percent over what would have occurred without the reservoir. Evaporation accounted for an increase of 15 mg/l, and leaching accounted for an increase of 115 mg/l.</p>","language":"English","publisher":"U.S. Goverment Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2009C","usgsCitation":"Madison, R.J., and Waddell, K.M., 1973, Chemical quality of surface water in the Flaming Gorge Reservoir area, Wyoming and Utah: U.S. Geological Survey Water Supply Paper 2009, Report: iv, 18 p.; Plate: 22.00 in. x 20.00 in., https://doi.org/10.3133/wsp2009C.","productDescription":"Report: iv, 18 p.; Plate: 22.00 in. x 20.00 in.","numberOfPages":"24","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2009c/report-thumb.jpg"},{"id":27834,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2009c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2009c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah, Wyoming","otherGeospatial":"Flaming Gorge Reservoir","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47b3e4b07f02db49ee49","contributors":{"authors":[{"text":"Madison, R. J.","contributorId":84734,"corporation":false,"usgs":true,"family":"Madison","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":144802,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3001,"text":"wsp2029A - 1973 - Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:05:48","indexId":"wsp2029A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2029","chapter":"A","title":"Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota","docAbstract":"<p>Stratified fluvial sediments occur within the glacial drift at many places in the Mesabi Iron Range area. These sediments, which are important aquifers, occur extensively between the three main till units. The thickest and most extensive aquifer consists of glaciofluvial sediments that lie between the surficial till and the middle till unit, the bouldery till. Thickness of the glaciofluvial sediments at this stratigraphic interval is greater than 50 feet in much of the area, and transmissivity is greater than 100,000 gallons per day per foot in some places.</p>\n<p>Glaciofluvial sediments underlying the bouldery till occur largely in the western half of the area. These sediments are generally less than 50 feet thick, and transmissivity is generally less than 50,000 gallons per day per foot.</p>\n<p>Surficial glaciofluvial sediments are a source of ground water for high-yield wells only in the eastern part of the area in the vicinity of the Biwabik bedrock valley. Thickness of these sediments is greater than 100 feet in some places, but transmissivity is generally less than 50,000 gallons per day per foot.</p>\n<p>Practical sustained yield of aquifers in glacial drift is estimated to be as much as 40 million gallons per day from known aquifers. Assuming that the ratio of area underlain by aquifer to total area is constant for the study area (about 20 percent where mapped in detail), as much as 80 million gallons per day could be developed from glacial-drift aquifers.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2029A","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Winter, T.C., 1973, Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 2029, Document: iv, 23 p.; 3 Plates: 28.00 x 28.17 inches or smaller, https://doi.org/10.3133/wsp2029A.","productDescription":"Document: iv, 23 p.; 3 Plates: 28.00 x 28.17 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":29794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2029a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2029a/report-thumb.jpg"},{"id":29791,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2029a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29792,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2029a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29793,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2029a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi Iron Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.8,\n              47.625\n            ],\n            [\n              -93.8,\n              47\n            ],\n            [\n              -91.75,\n              47\n            ],\n            [\n              -91.75,\n              47.625\n            ],\n            [\n              -93.8,\n              47.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624639","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":146127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3834,"text":"cir689 - 1973 - Effects of the May 5-6, 1973, storm in the Greater Denver area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"cir689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"689","title":"Effects of the May 5-6, 1973, storm in the Greater Denver area, Colorado","docAbstract":"Rain began falling on the Greater Denver area the evening of Saturday, May 5, 1973, and continued through most of Sunday, May 6. Below about 7,000 feet altitude, the precipitation was mostly rain; above that altitude, it was mostly snow. Although the rate of fall was moderate, at least 4 inches of rain or as much as 4 feet of snow accumulated in some places. Sustained precipitation falling at a moderate rate thoroughly saturated the ground and by midday Sunday sent most of the smaller streams into flood stage. The South Platte River and its major tributaries began to flood by late Sunday evening and early Monday morning. \r\n\r\nGeologic and hydrologic processes activated by the May 5-6 storm caused extensive damage to lands and to manmade structures in the Greater Denver area. Damage was generally most intense in areas where man had modified the landscape--by channel constrictions, paving, stripping of vegetation and topsoil, and oversteepening of hillslopes. Roads, bridges, culverts, dams, canals, and the like were damaged or destroyed by erosion and sedimentation. Streambanks and structures along them were scoured. Thousands of acres of croplands, pasture, and developed urban lands were coated with mud and sand. Flooding was intensified by inadequate storm sewers, blocked drains, and obstructed drainage courses. Saturation of hillslopes along the Front Range caused rockfalls, landslides, and mudflows as far west as Berthoud Pass. Greater attention to geologic conditions in land-use planning, design, and construction would minimize storm damage in the future.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/cir689","usgsCitation":"Hansen, W.R., 1973, Effects of the May 5-6, 1973, storm in the Greater Denver area, Colorado: U.S. Geological Survey Circular 689, iii, 20 p. :illus. ;26 cm., https://doi.org/10.3133/cir689.","productDescription":"iii, 20 p. :illus. ;26 cm.","costCenters":[],"links":[{"id":124696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1973/0689/report-thumb.jpg"},{"id":30907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1973/0689/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610541","contributors":{"authors":[{"text":"Hansen, Wallace R.","contributorId":90273,"corporation":false,"usgs":true,"family":"Hansen","given":"Wallace","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38677,"text":"pp758A - 1973 - Geology and mineral deposits of the Chulitna-Yentna mineral belt, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"pp758A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"758","chapter":"A","title":"Geology and mineral deposits of the Chulitna-Yentna mineral belt, Alaska","language":"ENGLISH","doi":"10.3133/pp758A","usgsCitation":"Hawley, C.C., and Clark, A.L., 1973, Geology and mineral deposits of the Chulitna-Yentna mineral belt, Alaska: U.S. Geological Survey Professional Paper 758, 9 p., https://doi.org/10.3133/pp758A.","productDescription":"9 p.","costCenters":[],"links":[{"id":104735,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5034.htm","linkFileType":{"id":5,"text":"html"},"description":"5034"},{"id":120104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0758a/report-thumb.jpg"},{"id":65514,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0758a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65515,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0758a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65516,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0758a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6851d5","contributors":{"authors":[{"text":"Hawley, C. C.","contributorId":102070,"corporation":false,"usgs":true,"family":"Hawley","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, A. L.","contributorId":89502,"corporation":false,"usgs":true,"family":"Clark","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220268,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61690,"text":"gq1092 - 1973 - Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming","interactions":[{"subject":{"id":40824,"text":"ofr71250 - 1971 - Preliminary geologic map of the Clause Peak Quadrangle, Lincoln, Sublette, and Teton counties, Wyoming","indexId":"ofr71250","publicationYear":"1971","noYear":false,"title":"Preliminary geologic map of the Clause Peak Quadrangle, Lincoln, Sublette, and Teton counties, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":61690,"text":"gq1092 - 1973 - Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming","indexId":"gq1092","publicationYear":"1973","noYear":false,"title":"Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming"},"id":1}],"lastModifiedDate":"2022-09-29T19:32:43.982602","indexId":"gq1092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1092","title":"Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1092","usgsCitation":"Schroeder, M.L., 1973, Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming: U.S. Geological Survey Geologic Quadrangle 1092, Report: 1 p.; 1 Plate: 33.57 x 32.58 inches, https://doi.org/10.3133/gq1092.","productDescription":"Report: 1 p.; 1 Plate: 33.57 x 32.58 inches","costCenters":[],"links":[{"id":107533,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10636.htm","linkFileType":{"id":5,"text":"html"},"description":"10636"},{"id":252569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1092/report-thumb.jpg"},{"id":247992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Wyoming","county":"Lincoln County, Sublette County, Teton County","otherGeospatial":"Clause Peak quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.625,\n              43.125\n            ],\n            [\n              -110.5,\n              43.125\n            ],\n            [\n              -110.5,\n              43.25\n            ],\n            [\n              -110.625,\n              43.25\n            ],\n            [\n              -110.625,\n              43.125\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69cad8","contributors":{"authors":[{"text":"Schroeder, Marvin L.","contributorId":91104,"corporation":false,"usgs":true,"family":"Schroeder","given":"Marvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61393,"text":"mf471 - 1973 - Map showing landslides in the Pacific Palisades area, city of Los Angeles, California","interactions":[],"lastModifiedDate":"2025-03-26T20:41:44.095674","indexId":"mf471","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"471","title":"Map showing landslides in the Pacific Palisades area, city of Los Angeles, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf471","isbn":"0607798653","usgsCitation":"McGill, J., 1973, Map showing landslides in the Pacific Palisades area, city of Los Angeles, California: U.S. Geological Survey Miscellaneous Field Studies Map 471, 1 Plate: 54.99 inches x 34.62 inches, https://doi.org/10.3133/mf471.","productDescription":"1 Plate: 54.99 inches x 34.62 inches","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":483901,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2910.htm","linkFileType":{"id":5,"text":"html"}},{"id":278779,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0471/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183466,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0471/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"California","city":"Los Angeles","otherGeospatial":"Pacific Palisades","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119,\n              34.15\n            ],\n            [\n              -119,\n              34\n            ],\n            [\n              -118.5167,\n              34\n            ],\n            [\n              -118.5167,\n              34.15\n            ],\n            [\n              -119,\n              34.15\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c45","contributors":{"authors":[{"text":"McGill, J.T.","contributorId":32988,"corporation":false,"usgs":true,"family":"McGill","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":265570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68307,"text":"ha465 - 1973 - Water resources of the Powder River basin and adjacent areas, northeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha465","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"465","title":"Water resources of the Powder River basin and adjacent areas, northeastern Wyoming","language":"ENGLISH","doi":"10.3133/ha465","usgsCitation":"Hodson, W.G., Pearl, R.H., and Druse, S.A., 1973, Water resources of the Powder River basin and adjacent areas, northeastern Wyoming: U.S. Geological Survey Hydrologic Atlas 465, 4 col. maps on 4 sheets ;105 x 144 cm. or smaller fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha465.","productDescription":"4 col. maps on 4 sheets ;105 x 144 cm. or smaller fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89747,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/465/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89748,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/465/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89749,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/465/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89750,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/465/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"75000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -11.234722222222222,43 ], [ -11.234722222222222,45 ], [ -10.666666666666666,45 ], [ -10.666666666666666,43 ], [ -11.234722222222222,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b7e","contributors":{"authors":[{"text":"Hodson, Warren Gayler","contributorId":49337,"corporation":false,"usgs":true,"family":"Hodson","given":"Warren","email":"","middleInitial":"Gayler","affiliations":[],"preferred":false,"id":278000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearl, Richard Howard","contributorId":50974,"corporation":false,"usgs":true,"family":"Pearl","given":"Richard","email":"","middleInitial":"Howard","affiliations":[],"preferred":false,"id":278001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Druse, Stanley A.","contributorId":7252,"corporation":false,"usgs":true,"family":"Druse","given":"Stanley","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277999,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66265,"text":"i743 - 1973 - Geologic map of parts of the Masontown and Morgantown North quadrangles, Greene County, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-10T00:11:19","indexId":"i743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"743","subseriesTitle":"NONE","title":"Geologic map of parts of the Masontown and Morgantown North quadrangles, Greene County, Pennsylvania","language":"ENGLISH","doi":"10.3133/i743","usgsCitation":"Kent, B., 1973, Geologic map of parts of the Masontown and Morgantown North quadrangles, Greene County, Pennsylvania: U.S. Geological Survey IMAP 743, 1 map., https://doi.org/10.3133/i743.","productDescription":"1 map.","costCenters":[],"links":[{"id":106944,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9497.htm","linkFileType":{"id":5,"text":"html"},"description":"9497"},{"id":188399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80,39.75 ], [ -80,39.8675 ], [ -79.86749999999999,39.8675 ], [ -79.86749999999999,39.75 ], [ -80,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2740","contributors":{"authors":[{"text":"Kent, B.H.","contributorId":30278,"corporation":false,"usgs":true,"family":"Kent","given":"B.H.","affiliations":[],"preferred":false,"id":274270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3871,"text":"cir679 - 1973 - Occurrence and distribution of selected metals in streams near Huntsville, Alabama","interactions":[],"lastModifiedDate":"2017-06-18T21:59:54","indexId":"cir679","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"679","title":"Occurrence and distribution of selected metals in streams near Huntsville, Alabama","docAbstract":"Arsenic, cadmium, chromium, cobalt, lead, mercury, and zinc are widely distributed around Huntsville, Ala. However, concentrations of these metals in streamflow in the vicinity of the Huntsville municipal water intake during June, August, and September 1971 did not exceed the limits recommended for a public drinking water supply. The occurrence of these metals in general is related to man's activities. \r\n\r\nInformation gained during this study suggests that cadmium and the other metals are associated with and transported with suspended sediment, bed material, and airborne dust particles. Lead and zinc were the most abundant of the selected metals in streamflow, bed material, and rainwater samples. The highest concentration of cadmium was detected downstream from an industrial park in the Flint River basin; rainwater samples also contained a relatively high level of cadmium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir679","usgsCitation":"German, E.R., and Knight, A.L., 1973, Occurrence and distribution of selected metals in streams near Huntsville, Alabama: U.S. Geological Survey Circular 679, iii, 13 p. :maps. ;26 cm., https://doi.org/10.3133/cir679.","productDescription":"iii, 13 p. :maps. ;26 cm.","costCenters":[],"links":[{"id":30962,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1973/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1973/0679/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a5e","contributors":{"authors":[{"text":"German, E. R.","contributorId":86315,"corporation":false,"usgs":true,"family":"German","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knight, Alfred L.","contributorId":34906,"corporation":false,"usgs":true,"family":"Knight","given":"Alfred","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147763,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67139,"text":"i761C - 1973 - Map showing areas of potential rockfalls in the Golden Quadrangle, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"i761C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"761","subseriesTitle":"NONE","chapter":"C","title":"Map showing areas of potential rockfalls in the Golden Quadrangle, Jefferson County, Colorado","language":"ENGLISH","doi":"10.3133/i761C","usgsCitation":"Simpson, H.E., 1973, Map showing areas of potential rockfalls in the Golden Quadrangle, Jefferson County, Colorado: U.S. Geological Survey IMAP 761, 1 map :col. ;58 x 45 cm. on sheet 73 x 107 cm. folded to 27 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i761C.","productDescription":"1 map :col. ;58 x 45 cm. on sheet 73 x 107 cm. folded to 27 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":256479,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0761c/plate-1.pdf","size":"5334","linkFileType":{"id":1,"text":"pdf"}},{"id":256480,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0761c/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":256481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0761c/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.25,39.75 ], [ -105.25,39.8675 ], [ -105.11749999999999,39.8675 ], [ -105.11749999999999,39.75 ], [ -105.25,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db6593d8","contributors":{"authors":[{"text":"Simpson, H. E.","contributorId":96702,"corporation":false,"usgs":true,"family":"Simpson","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":275662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27912,"text":"wri733 - 1973 - Effects of Urbanization on Floods in the Houston, Texas Metropolitan Area","interactions":[],"lastModifiedDate":"2016-08-22T14:17:30","indexId":"wri733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-3","title":"Effects of Urbanization on Floods in the Houston, Texas Metropolitan Area","docAbstract":"<p>Rainfall and runoff data from drainage basins in the Houston metropolitan area and a 60-year rainfall record for the National Weather Service station, Houston-City, were used to simulate 60 annual flood peaks at 26 sites. Selected frequency characteristics, based on these simulated annual peaks, are related to drainage area and percentage of impervious area. These relations, which may be used to estimate the flood characteristics at ungaged sites, indicate that in the Houston metropolitan area, complete urbanization increases the magnitude of a 2-year flood nine times and increases the magnitude of a 50-year flood five times.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri733","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Johnson, S.L., and Sayre, D.M., 1973, Effects of Urbanization on Floods in the Houston, Texas Metropolitan Area: U.S. Geological Survey Water-Resources Investigations Report 73-3, iv, 50 p., https://doi.org/10.3133/wri733.","productDescription":"iv, 50 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":120076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_73_3.jpg"},{"id":13938,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri3-73/","linkFileType":{"id":5,"text":"html"}},{"id":327295,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri3-73/pdf/wri3-73.pdf","size":"4.1 MB","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624df8","contributors":{"authors":[{"text":"Johnson, Steven L.","contributorId":8140,"corporation":false,"usgs":true,"family":"Johnson","given":"Steven","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayre, Douglas M.","contributorId":67929,"corporation":false,"usgs":true,"family":"Sayre","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":198887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14989,"text":"ofr73186 - 1973 - Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia","interactions":[{"subject":{"id":14989,"text":"ofr73186 - 1973 - Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia","indexId":"ofr73186","publicationYear":"1973","noYear":false,"title":"Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":62498,"text":"gq1350 - 1977 - Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia","indexId":"gq1350","publicationYear":"1977","noYear":false,"title":"Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia"},"id":1}],"supersededBy":{"id":62498,"text":"gq1350 - 1977 - Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia","indexId":"gq1350","publicationYear":"1977","noYear":false,"title":"Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia"},"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr73186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-186","title":"Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr73186","usgsCitation":"Miller, R.L., and Meissner, C.R., 1973, Geologic map of the Big A Mountain quadrangle, Buchanan and Russell Counties, Virginia: U.S. Geological Survey Open-File Report 73-186, 1 v. (various pagings) :ill., folded map ;27 cm.; 28 p., 7 sheets, scale 1:24,000, https://doi.org/10.3133/ofr73186.","productDescription":"1 v. (various pagings) :ill., folded map ;27 cm.; 28 p., 7 sheets, scale 1:24,000","costCenters":[],"links":[{"id":147914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0de4b07f02db69f42e","contributors":{"authors":[{"text":"Miller, Ralph L.","contributorId":74737,"corporation":false,"usgs":true,"family":"Miller","given":"Ralph","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":170372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meissner, Charles R. Jr.","contributorId":28970,"corporation":false,"usgs":true,"family":"Meissner","given":"Charles","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":170371,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15079,"text":"ofr73197 - 1973 - Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah","interactions":[{"subject":{"id":15079,"text":"ofr73197 - 1973 - Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah","indexId":"ofr73197","publicationYear":"1973","noYear":false,"title":"Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66652,"text":"i883 - 1975 - Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah","indexId":"i883","publicationYear":"1975","noYear":false,"title":"Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah"},"id":1}],"supersededBy":{"id":66652,"text":"i883 - 1975 - Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah","indexId":"i883","publicationYear":"1975","noYear":false,"title":"Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah"},"lastModifiedDate":"2012-02-02T00:07:04","indexId":"ofr73197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-197","title":"Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah","language":"ENGLISH","publisher":"U.S Geological Survey,","doi":"10.3133/ofr73197","usgsCitation":"Morris, H.T., 1973, Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah: U.S. Geological Survey Open-File Report 73-197, 6 p. :ill., 2 folded maps ;27 cm., https://doi.org/10.3133/ofr73197.","productDescription":"6 p. :ill., 2 folded maps ;27 cm.","costCenters":[],"links":[{"id":148727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c1e9","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":170531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15249,"text":"ofr73209 - 1973 - Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts","interactions":[{"subject":{"id":15249,"text":"ofr73209 - 1973 - Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts","indexId":"ofr73209","publicationYear":"1973","noYear":false,"title":"Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":62361,"text":"gq1158 - 1974 - Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts","indexId":"gq1158","publicationYear":"1974","noYear":false,"title":"Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts"},"id":1}],"supersededBy":{"id":62361,"text":"gq1158 - 1974 - Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts","indexId":"gq1158","publicationYear":"1974","noYear":false,"title":"Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr73209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-209","title":"Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr73209","usgsCitation":"Oldale, R.N., 1973, Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts: U.S. Geological Survey Open-File Report 73-209, 15 p. :ill. (some folded), folded map ;29 cm.; 1 sheet, scale 1:24,000, https://doi.org/10.3133/ofr73209.","productDescription":"15 p. :ill. (some folded), folded map ;29 cm.; 1 sheet, scale 1:24,000","costCenters":[],"links":[{"id":147156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f5c","contributors":{"authors":[{"text":"Oldale, Robert N.","contributorId":38953,"corporation":false,"usgs":true,"family":"Oldale","given":"Robert","email":"","middleInitial":"N.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":170816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14999,"text":"ofr73188 - 1973 - Geologic setting and chemical characteristics of hot springs in central and western Alaska","interactions":[],"lastModifiedDate":"2016-02-03T14:33:40","indexId":"ofr73188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-188","title":"Geologic setting and chemical characteristics of hot springs in central and western Alaska","docAbstract":"<p>Numerous hot springs occur in a variety of geologic provinces in central and western Alaska. Granitic plutons are common to all the provinces and the hot springs are spatially associated with the contacts of these plutons. Of 23 hot springs whose bedrock geology is known, all occur within 3 miles of a granitic pluton. The occurrence of hot springs, however, appears to be independent of the age, composition, or magmatic history of the pluton.</p>\n<p>Preliminary chemical and isotopic analyses suggest the hot springs waters belong to two groups. Most of the analyzed hot springs appear to have chemical and Isotopic compositions indicating they were derived from deeply circulating meteoric water. About 25 percent of the analyzed hot springs show a distinct saline character with high concentrations of chloride, sodium, potassium, and calcium indicating either much more complex water rock reactions than occurred in the other hot springs or the addition of another type of water. The present chemical and isotopic data are insufficient to determine the source of the constituents of the saline hot springs.</p>\n<p>Chemical geothermometers suggest subsurface temperatures in the general range of 100&deg;C to 160&deg;C. If the hot spring waters have derived their heat solely from deep circulation, the waters must have reached depths of 9,000 to 15,000 feet, assuming geothermal gradients of 30&deg;C to 50&deg;C/km. If hot magmatic water has been added to the geothermal systems or if dilution or mixing has occurred, temperatures of 100&deg;C to 160&deg;C may be reached at shallower depths.</p>\n<p>The geologic and chemical data are too preliminary to make an estimate of the potential of the hot springs as a geothermal resource. The data suggest, however, that most of the hot springs of central and western Alaska have relatively low subsurface temperatures and limited reservoir capacities in comparison with geothermal areas presently being utilized for electrical power generation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73188","usgsCitation":"Miller, T.P., Barnes, I., and Pattan, W.W., 1973, Geologic setting and chemical characteristics of hot springs in central and western Alaska: U.S. Geological Survey Open-File Report 73-188, Report: 19 p.; 1 Figure; 1 Table (in 2 parts), https://doi.org/10.3133/ofr73188.","productDescription":"Report: 19 p.; 1 Figure; 1 Table (in 2 parts)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":43825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-1.pdf","text":"Figure 1","size":"688.14 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 1"},{"id":43826,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-2.pdf","text":"Table 1","size":"1.21 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1"},{"id":43827,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-3.pdf","text":"Table 1, Part 2","size":"1.29 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1, Part 2"},{"id":43828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0188/report.pdf","text":"Report","size":"589.73 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":148931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0188/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -165,\n              64\n            ],\n            [\n              -165,\n              66\n            ],\n            [\n              -150,\n              66\n            ],\n            [\n              -150,\n              64\n            ],\n            [\n              -165,\n              64\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881be","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":170388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":170389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pattan, William Wallace Jr.","contributorId":61297,"corporation":false,"usgs":true,"family":"Pattan","given":"William","suffix":"Jr.","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":170390,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14997,"text":"ofr73187 - 1973 - Distribution and chemical analyses of thermal springs in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:06","indexId":"ofr73187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-187","title":"Distribution and chemical analyses of thermal springs in Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr73187","usgsCitation":"Miller, T.P., 1973, Distribution and chemical analyses of thermal springs in Alaska: U.S. Geological Survey Open-File Report 73-187, 5 p. :folded map ;27 cm., https://doi.org/10.3133/ofr73187.","productDescription":"5 p. :folded map ;27 cm.","costCenters":[],"links":[{"id":148800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":43822,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fad","contributors":{"authors":[{"text":"Miller, T. P.","contributorId":49345,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":170385,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14941,"text":"ofr73182 - 1973 - Phospatic rock in the Nizampur area of the Kala Chitta Hills, Pakistan","interactions":[],"lastModifiedDate":"2021-02-22T19:04:48.899139","indexId":"ofr73182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-182","title":"Phospatic rock in the Nizampur area of the Kala Chitta Hills, Pakistan","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73182","usgsCitation":"Meissner, C.R., 1973, Phospatic rock in the Nizampur area of the Kala Chitta Hills, Pakistan: U.S. Geological Survey Open-File Report 73-182, Report: 15 p. 2 Plates: 9.96 x 6.10 inches and 7.65 x 9.99 inches, https://doi.org/10.3133/ofr73182.","productDescription":"Report: 15 p. 2 Plates: 9.96 x 6.10 inches and 7.65 x 9.99 inches","costCenters":[],"links":[{"id":383458,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1973/0182/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383457,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1973/0182/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383456,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0182/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0182/report-thumb.jpg"}],"country":"Pakistan","city":"Nizampur","otherGeospatial":"Kala Chitta Hills","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              73.927001953125,\n              31.914867503276223\n            ],\n            [\n              74.718017578125,\n              31.914867503276223\n            ],\n            [\n              74.718017578125,\n              32.37996146435729\n            ],\n            [\n              73.927001953125,\n              32.37996146435729\n            ],\n            [\n              73.927001953125,\n              31.914867503276223\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687878","contributors":{"authors":[{"text":"Meissner, Charles R. Jr.","contributorId":28970,"corporation":false,"usgs":true,"family":"Meissner","given":"Charles","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":170287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13959,"text":"ofr7397 - 1973 - Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr7397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-97","title":"Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia","docAbstract":"This report summarizes the geology of an area of some 6000 square kilometers in the northern part of the Central Cordillera of the Colombian Andes. The area, in north-central Department of Antioquia, was mapped between 1964 and 1968 as part of the Inventario Minero Nacional (IMN) project. Mineral resources are summarized within a larger area, designated as subzone ILK of IMN Zone If, which comprises almost 22,000 sq. kin, including the area mapped geologically by IMN and additional areas mapped by other agencies. \r\n\r\nThe oldest formation is a micaceous paragneiss of early Paleozoic or possibly late Precambrian age. A thick geosynclinal sedimentary series accumulated during the Paleozoic Era and became regionally metamorphosed to greenschist (locally amphibolite) facies during the Permian or early Triassic; these schists and gneisses are designated collectively as the Valdivia Group. The Permian(?) orogenic episode included intrusion of concordant syntectonic plutons, mostly of tonalitic composition. Rocks of unequivocal Triassic or Jurassic age are not recognized.\r\n\r\nThe Cretaceous is well represented by both igneous and sedimentary assemblages. Eugeosynclinal alpine ophiolites comprising submarine basalt flows and numerous intrusions of gabbro and serpentinite are prominent in the Lower Cretaceous, together with flysch composed of marine shale and lesser sandstone and conglomerate. The Upper Cretaceous is represented along the west border of the mapped area by submarine basalt flows and pyroclastic rocks, locally Interbedded with fine-grained clastic sedimentary beds, and lenses of dark laminated chert, at least part of which is radiolarian. The Late Cretaceous was marked by an orogenic event that profoundly folded and faulted all rocks and in the Central Cordillera caused low-grade metamorphism, the overprint of which is hardly observable in pre-Cretaceous rocks elsewhere. The Late Cretaceous orogeny culminated with discordant intrusion of the epizonal tonalitic Antioquian batholith. Displacement along the great Romeral wrench fault may have begun in the Cretaceous. \r\n\r\nPlutonism continued into the Cenozoic, exemplified by the hornblende-diorite Sabanalarga pluton. Intermontane basins were filled with molasse derived from the erosion of adjacent highlands; Tertiary sedimentation in marshy areas included organic carboniferous matter subsequently converted to lignite or subbituminous coal. The Sabanalarga fault system originated in the Late Tertiary; intermittent displacement continued on the older wrench faults such as the Romeral. Epeirogenic uplift, which probably began in the Pliocene and continued through the Pleistocene and Holocene, brought on renewed erosion which has sculptured the mountains into their present form.\r\n\r\nMineral resources in subzone IIA are varied but not of outstanding importance. Gold and silver mining, significant in past centuries, is minor today. Ferruginous laterite on serpentinite once considered as a potential source of iron ore is not economically exploitable. IMN has explored nickeliferous laterite at the extreme northwest corner of subzone IIA; this is a potential resource, exploitable only after exhaustion of the larger and richer nickel laterite deposit at Cerro Matoso, farther to the north and outside the boundaries of Zone If. Known deposits of mercury, chromium, manganese, and copper are small, with limited economic potential. Nonmetallic resources include raw materials for cement, including portland cement. Saprolite clay is widely used in making common red brick and tile, still a dominant construction material in all but the most modern multistory buildings. Aggregate materials are varied and abundant. Kaolin of good quality near La Union is important as a ceramic raw mineral filler. Tertiary subbituminous coal beds are an important energy resource in western subzone IIA, and have a good potential for greater development. Deposits of sodic feldspar, talc, decorative stone, and silica a","language":"ENGLISH","publisher":"U.S. Geological Survey]","doi":"10.3133/ofr7397","usgsCitation":"Hall, R., Alvarez A., J., and Rico H., H., 1973, Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia: U.S. Geological Survey Open-File Report 73-97, x, 174 p. :maps (3 folded, 1 col.) ;27 cm.; 1 map, scale 1:100,000, https://doi.org/10.3133/ofr7397.","productDescription":"x, 174 p. :maps (3 folded, 1 col.) ;27 cm.; 1 map, scale 1:100,000","costCenters":[],"links":[{"id":95182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0097/plate-1.pdf","size":"12413","linkFileType":{"id":1,"text":"pdf"}},{"id":147401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0097/report-thumb.jpg"},{"id":42615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46fd","contributors":{"authors":[{"text":"Hall, R.B.","contributorId":17214,"corporation":false,"usgs":true,"family":"Hall","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":168699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alvarez A., Jairo","contributorId":44411,"corporation":false,"usgs":true,"family":"Alvarez A.","given":"Jairo","email":"","affiliations":[],"preferred":false,"id":168701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rico H., Hector","contributorId":42481,"corporation":false,"usgs":true,"family":"Rico H.","given":"Hector","email":"","affiliations":[],"preferred":false,"id":168700,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13762,"text":"ofr73314 - 1973 - Preliminary report on the geology and field petrology at the Apollo 17 landing site","interactions":[],"lastModifiedDate":"2018-10-23T08:29:35","indexId":"ofr73314","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-314","title":"Preliminary report on the geology and field petrology at the Apollo 17 landing site","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73314","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Apollo Lunar Geology Investigation Team, 1973, Preliminary report on the geology and field petrology at the Apollo 17 landing site: U.S. Geological Survey Open-File Report 73-314, Report: iii, 60 p.; Maps (2 folded, col.): 27 cm., https://doi.org/10.3133/ofr73314.","productDescription":"Report: iii, 60 p.; Maps (2 folded, col.): 27 cm.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":145488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c912","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Apollo Lunar Geology Investigation Team","contributorId":127892,"corporation":true,"usgs":false,"organization":"Apollo Lunar Geology Investigation Team","id":528959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13675,"text":"ofr7374 - 1973 - The isotopic analysis of water from the Henderson mine, Clear Creek County, Colorado","interactions":[],"lastModifiedDate":"2025-08-05T13:43:05.705247","indexId":"ofr7374","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-74","title":"The isotopic analysis of water from the Henderson mine, Clear Creek County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7374","usgsCitation":"Friedman, I., 1973, The isotopic analysis of water from the Henderson mine, Clear Creek County, Colorado: U.S. Geological Survey Open-File Report 73-74, 4 p., 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