{"pageNumber":"368","pageRowStart":"9175","pageSize":"25","recordCount":11004,"records":[{"id":11562,"text":"ofr80186 - 1980 - Seismic refraction data for shots recorded in the Coso Range, California, October 1976","interactions":[],"lastModifiedDate":"2022-10-24T19:10:14.089586","indexId":"ofr80186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-186","title":"Seismic refraction data for shots recorded in the Coso Range, California, October 1976","docAbstract":"
The Coso Range lies in the southwest corner of the Basin and Range province, east of the Sierra Nevada and north of the Garlock Fault. The range, circular in form, is covered by a thin sequence of late-cenozoic volcanics which overlie highly fractured crystalline basement, similar in composition to the nearby Sierra Nevada (Duffield et al., 1980). Thirty-eight rhyolite domes of Pleistocene age were emplaced near the center of the range and are aligned approximately parallel to the direction of Basin and Range faulting (Figure 1). Bacon et al. (1980), using both age-dates and chemical analyses, inferred that the domes originated from a magma source beneath the central and largest of the rhyolite domes, Sugarloaf Mountain (Figure 1). A shallow source was inferred because active fumeroles, hydrothermally altered zones, and high heat flow values (Combs, 1980) are presently observed in this vicinity.

In an effort to collect seismic data which could be used to identify a magma body beneath Sugarloaf Mountain, a 16 station seismograph array was operated in the Coso Range from September 1975 through September 1977. During the two years of network operation, over 4000 local earthquakes were located in the vicinity of the Coso Range (Walter and Weaver, 1980a, 1980b). In October of 1976, a seismic refraction experiment was conducted in the Coso Range in order to develop a crustal velocity model for use in interpreting the earthquake data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80186","usgsCitation":"Walter, A., and Weaver, C.S., 1980, Seismic refraction data for shots recorded in the Coso Range, California, October 1976: U.S. Geological Survey Open-File Report 80-186, 12 p., https://doi.org/10.3133/ofr80186.","productDescription":"12 p.","costCenters":[],"links":[{"id":145809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0186/report-thumb.jpg"},{"id":408669,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0186/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Coso Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.87207031250001,\n 34.71452466170392\n ],\n [\n -116.01562499999999,\n 34.71452466170392\n ],\n [\n -116.01562499999999,\n 36.74768773190056\n ],\n [\n -118.87207031250001,\n 36.74768773190056\n ],\n [\n -118.87207031250001,\n 34.71452466170392\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6b2","contributors":{"authors":[{"text":"Walter, A. W.","contributorId":67090,"corporation":false,"usgs":true,"family":"Walter","given":"A. W.","affiliations":[],"preferred":false,"id":163362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weaver, Craig S. craig@usgs.gov","contributorId":2690,"corporation":false,"usgs":true,"family":"Weaver","given":"Craig","email":"craig@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":163361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11295,"text":"ofr80312 - 1980 - Lemhi Pass drilling project, Montana","interactions":[],"lastModifiedDate":"2023-11-24T19:40:15.163633","indexId":"ofr80312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-312","title":"Lemhi Pass drilling project, Montana","docAbstract":"

The Lemhi Pass district has the largest thorium resources of any vein district in the United States (Staatz and others, 1979, p. 10). Most of the resources occur in veins that have an average grade of between 0.1 and 2.0 percent Th02. More than 200 thorium-bearing veins have been mapped in this district (Staatz, 1979, p. A34).

The Lemhi Pass thorium district lies astride the Continental Divide in the east-central part of the Beaverhead Mountains along the Idaho-Montana State line. Although the area in which thorium veins are found covers more than 150 square miles, the drilling project was confined to three veins in the northwestern part of this district on the Montana side of the Continental Divide (fig. 1). An unimproved dirt road that crosses the Continental Divide at Lemhi Pass furnishes access to the drilling area. This road connects Idaho State Highway 28 at Tendoy, Idaho, 13 miles west of Lemhi Pass, with Interstate Highway 15 at the Clark Canyon reservoir/dam, 31.5 miles east of Lemhi Pass. Salmon, Idaho, the principal town to the west, is 19 miles northwest of Tendoy; and Dillon, Mont., the principal town to the east, is 18 miles northeast of Clark Canyon Reservoir.

The drilling project was proposed by the Department of Energy headquarters personnel in Washington, D.C., during the spring of 1978. The purpose of the project was to demonstrate downward extension of the veins. Drilling was proposed to indicate whether several veins had a depth of 500 feet or more.

Little exploration has been carried out on thorium veins. The lack of a ready market for thorium has resulted in little economic incentive for exploration. Most veins in this district are covered by 50 feet of soil.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80312","usgsCitation":"Staatz, M.H., 1980, Lemhi Pass drilling project, Montana: U.S. Geological Survey Open-File Report 80-312, ii, 42 p., https://doi.org/10.3133/ofr80312.","productDescription":"ii, 42 p.","costCenters":[],"links":[{"id":422934,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142421,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0312/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Lemhi Pass","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.56438861291157,\n 45.05456729899308\n ],\n [\n -113.56438861291157,\n 44.751083170859914\n ],\n [\n -113.04253802697414,\n 44.751083170859914\n ],\n [\n -113.04253802697414,\n 45.05456729899308\n ],\n [\n -113.56438861291157,\n 45.05456729899308\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a64fb","contributors":{"authors":[{"text":"Staatz, Mortimer Hay","contributorId":39754,"corporation":false,"usgs":true,"family":"Staatz","given":"Mortimer","email":"","middleInitial":"Hay","affiliations":[],"preferred":false,"id":162883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10037,"text":"ofr801285 - 1980 - Ground-water appraisal of sand plains in Benton, Sherburne, Stearns, and Wright counties, central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T13:15:03","indexId":"ofr801285","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1285","title":"Ground-water appraisal of sand plains in Benton, Sherburne, Stearns, and Wright counties, central Minnesota","docAbstract":"

Surficial-sand aquifers in 960 square miles of central Minnesota have been studied to determine the occurrence, availability, and suitability of the surficial aquifer as a source of water. The aquifer is being increasingly developed for irrigation.

\n

During the drought of 1976, nearly 24,000 acre-feet of ground water was withdrawn for irrigation, more than double that of the previous year. The number of irrigation pumping centers more than doubled from 1975 to 1977. Nearly all water is pumped from drift aquifers, except in the eastern parts of Sherburne and Wright Counties, where Paleozoic sandstone beds are a reliable source.

\n

Physical and hydrologic properties of the surficial aquifer were determined by test augering, pumping tests, and laboratory sieve analyses. The aquifer is predominantly medium to coarse sand with lesser amounts of gravel in much of the study area. The Sauk River valley in Stearns County is nearly 50 percent poorly sorted gravel of irregular thickness. Saturated thickness of sand in the Maine Prairie area locally exceeds 100 feet, and transmissivity exceeds 40,000 feet squared per day. Similar deposits in Sherburne County exceed 80 feet in thickness, transmissivity exceeds 30,000 feet squared per day, and wells theoretically could yield 2,000 to 3,000 gallons per minute. Theoretical well yields of less than 100 gallons per minute can be expected where saturated thickness is less than 20 feet and transmissivity is less than 5,000 feet squared per day. Pumping tests indicate horizontal to vertical ratios of hydraulic conductivity ranging from 2-27:1.

\n

Average annual precipitation is 27 inches, about 8 of which is recharge to the surficial aquifer. Regional ground-water movement is toward the Mississippi River, which transects the area. Tributary streams and lakes act as controls for local flow systems. At extreme low flow in August 1976, mainstem gains in streamflow in the Elk, St. Francis, Sauk, and Mississippi Rivers averaged 0.4, 0.4, 0.2, and 2.5 cubic feet per second per river mile, respectively.

\n

Ground water is of the calcium bicarbonate type and is suitable for most uses. Relatively high nitrate and chloride concentrations occur in a heavily irrigated area in Sherburne County.

\n

Surficial aquifers in Sherburne County and the Maine Prairie area of Stearns County were simulated by two-dimensional digital ground-water-flow models. Calibration was achieved by matching calculated water-table heads and streamflow gains with observed field values. Aquifer responses to pumping stresses under present and hypothetically expanded development were determined for average and below average recharge conditions.

\n

Irrigation withdrawals for 1977 totaling 15.6 cubic feet per second from 96 pumping centers were included in the Sherburne steady-state model. Increasing withdrawals to 52.2 cubic feet per second from 153 pumping centers would lower regional water levels as much as 8 feet within a few years at normal recharge rates.

\n

Irrigation withdrawals in 1977, totaling 2.0 cubic feet per second from 19 pumping centers, were included in the Maine Prairie steady-state model. Increasing withdrawals to 10.8 cubic feet per second from 42 pumping centers would lower regional water levels as much as 18 feet at normal recharge rates.

\n

Both modeled areas will support additional withdrawals, but caution must be exercised because lowering ground-water levels will also lower lake levels and reduce streamflow. In some areas, aquifer dewatering will reduce individual well yields.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr801285","collaboration":"Prepared in cooperation with Minnesota Department of Natural Resources, Central Minnesota Regional Development Commission, Benton Sherburne, Stearns, and Wright County Boards","usgsCitation":"Lindholm, G.F., 1980, Ground-water appraisal of sand plains in Benton, Sherburne, Stearns, and Wright counties, central Minnesota: U.S. Geological Survey Open-File Report 80-1285, Document: viii, 103 p.; 4 Plates: 42.96 x 32.35 inches or smaller, https://doi.org/10.3133/ofr801285.","productDescription":"Document: viii, 103 p.; 4 Plates: 42.96 x 32.35 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":37882,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1285/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1285/report-thumb.jpg"},{"id":37883,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1285/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37884,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1285/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37885,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1285/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37881,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1285/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Benton County, Sherburne County, Stearns County, Wright County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.7641,45.8202],[-93.7598,45.5604],[-93.5106,45.5598],[-93.5093,45.4163],[-93.5138,45.2454],[-93.5158,45.2458],[-93.5197,45.2417],[-93.5242,45.2385],[-93.5332,45.2317],[-93.5371,45.2294],[-93.5462,45.2289],[-93.554,45.2298],[-93.5617,45.2289],[-93.5676,45.2225],[-93.5734,45.2202],[-93.5792,45.2189],[-93.5857,45.2189],[-93.5967,45.2134],[-93.6031,45.2111],[-93.6096,45.2111],[-93.6167,45.2115],[-93.6258,45.2092],[-93.6297,45.2074],[-93.6329,45.2056],[-93.6361,45.206],[-93.6387,45.2074],[-93.6471,45.2079],[-93.6562,45.201],[-93.6555,45.1969],[-93.6549,45.1905],[-93.6516,45.1841],[-93.6503,45.169],[-93.6529,45.1631],[-93.6554,45.1599],[-93.6574,45.1585],[-93.6716,45.1562],[-93.6793,45.1525],[-93.6852,45.1489],[-93.6929,45.1434],[-93.7019,45.1374],[-93.7155,45.1269],[-93.72,45.1205],[-93.7225,45.11],[-93.7257,45.1022],[-93.7322,45.0963],[-93.7341,45.0922],[-93.7399,45.0894],[-93.7534,45.0853],[-93.7631,45.0839],[-93.7663,45.077],[-93.7702,45.0734],[-93.7692,44.9789],[-94.0117,44.9796],[-94.2548,44.9812],[-94.2544,45.2268],[-94.2602,45.2268],[-94.2614,45.2784],[-94.2615,45.2844],[-94.382,45.2836],[-94.3819,45.327],[-94.7612,45.3272],[-94.7635,45.414],[-95.1322,45.4128],[-95.1319,45.5856],[-95.1384,45.5864],[-95.1388,45.7602],[-95.1398,45.7744],[-94.6438,45.7758],[-94.2782,45.777],[-94.2802,45.778],[-94.2841,45.7793],[-94.2894,45.7806],[-94.2972,45.7829],[-94.3018,45.7838],[-94.3051,45.7865],[-94.3077,45.7888],[-94.3091,45.792],[-94.3105,45.7965],[-94.3118,45.7983],[-94.3144,45.7992],[-94.3183,45.7997],[-94.3235,45.7992],[-94.3262,45.8001],[-94.3295,45.8014],[-94.3328,45.8042],[-94.338,45.8078],[-94.3426,45.811],[-94.3466,45.8141],[-94.3499,45.8173],[-94.3513,45.8228],[-94.0515,45.8262],[-93.9254,45.8216],[-93.7641,45.8202]]]},\"properties\":{\"name\":\"Benton\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3ed","contributors":{"authors":[{"text":"Lindholm, Gerald F.","contributorId":18374,"corporation":false,"usgs":true,"family":"Lindholm","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9745,"text":"ofr80160 - 1980 - Sediment transport model for the East Fork of the Carson River, Carson Valley, Nevada","interactions":[],"lastModifiedDate":"2019-08-20T12:31:12","indexId":"ofr80160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-160","title":"Sediment transport model for the East Fork of the Carson River, Carson Valley, Nevada","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80160","usgsCitation":"Katzer, T., and Bennett, J.P., 1980, Sediment transport model for the East Fork of the Carson River, Carson Valley, Nevada: U.S. Geological Survey Open-File Report 80-160, 40 p. , https://doi.org/10.3133/ofr80160.","productDescription":"40 p. ","costCenters":[],"links":[{"id":366727,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0160/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0160/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Douglas County","otherGeospatial":"Carson Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-119.5461,39.0859],[-119.5272,39.0858],[-119.316,39.0841],[-119.3155,38.9902],[-119.3356,38.9895],[-119.3366,38.9818],[-119.349,38.9816],[-119.4023,38.9826],[-119.4022,38.9558],[-119.4176,38.9547],[-119.4182,38.9098],[-119.4192,38.8817],[-119.4381,38.8823],[-119.4374,38.8533],[-119.419,38.8531],[-119.4192,38.835],[-119.4193,38.8164],[-119.4122,38.8165],[-119.4126,38.8093],[-119.4019,38.8099],[-119.4013,38.7863],[-119.4026,38.7654],[-119.4085,38.7658],[-119.4077,38.7354],[-119.4075,38.73],[-119.3887,38.7303],[-119.3888,38.7348],[-119.3788,38.735],[-119.3611,38.7352],[-119.3505,38.7354],[-119.3502,38.7263],[-119.349,38.6788],[-119.349,38.6769],[-119.3488,38.6466],[-119.3299,38.6469],[-119.3306,38.5364],[-119.4492,38.6196],[-119.4543,38.6231],[-119.5498,38.6895],[-119.5523,38.6912],[-119.5771,38.7084],[-119.5977,38.7226],[-119.6088,38.7303],[-119.6166,38.7357],[-119.678,38.7781],[-119.7033,38.7953],[-119.7285,38.8132],[-119.743,38.8235],[-119.752,38.8297],[-119.7873,38.8541],[-119.7899,38.8554],[-119.8223,38.8775],[-119.8261,38.8802],[-119.8471,38.8948],[-119.9025,38.9332],[-119.9151,38.942],[-119.9194,38.945],[-119.9508,38.9664],[-120.0009,39.0005],[-120.0023,39.0677],[-120.0031,39.1116],[-119.949,39.1122],[-119.9419,39.1123],[-119.8974,39.1123],[-119.8631,39.1129],[-119.8358,39.113],[-119.7611,39.1144],[-119.7612,39.099],[-119.7517,39.0987],[-119.7525,39.0851],[-119.6232,39.086],[-119.6042,39.0859],[-119.5657,39.0861],[-119.5461,39.0859]]]},\"properties\":{\"name\":\"Douglas\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbea3","contributors":{"authors":[{"text":"Katzer, Terry","contributorId":103679,"corporation":false,"usgs":true,"family":"Katzer","given":"Terry","email":"","affiliations":[],"preferred":false,"id":160222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, J. P.","contributorId":52103,"corporation":false,"usgs":true,"family":"Bennett","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7032,"text":"ofr80504 - 1980 - A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979","interactions":[{"subject":{"id":7032,"text":"ofr80504 - 1980 - A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979","indexId":"ofr80504","publicationYear":"1980","noYear":false,"title":"A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979"},"predicate":"SUPERSEDED_BY","object":{"id":16945,"text":"ofr84484 - 1984 - A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979","indexId":"ofr84484","publicationYear":"1984","noYear":false,"title":"A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979"},"id":1}],"supersededBy":{"id":16945,"text":"ofr84484 - 1984 - A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979","indexId":"ofr84484","publicationYear":"1984","noYear":false,"title":"A Catalogue of drill core recovered from Kilauea Iki lava lake from 1967 to 1979"},"lastModifiedDate":"2022-10-25T19:43:35.816708","indexId":"ofr80504","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-504","title":"A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979","docAbstract":"
The purpose of this report is to serve as a descriptive catalogue for drill core recovered from Kilauea Iki lava lake, from 1967 to 1979.

Kilauea Iki lava lake was formed when lavas of the 1959 summit eruption were ponded in Kilauea Iki pit crater, a large pit crater at the extreme upper end of Kilauea's east rift zone (Fig. 1). This eruption is one of the best documented of Kilauean eruptions: Murata and Richter (1966) and Richter and Murata (1966) presented data on the chemistry and petrography of the lavas, respectively, and Richter et al. (1970) described the complex filling of the pit crater in considerable detail.

Investigation of the lava lake began a few months after the crust stabilized, with the establishment of two perpendicular lines of levelling stations on the surface of the lake. In 1960-62, four holes were drilled through the upper crust in the center of the lake; the crust was 22-44 feet (6.7-13.4 m) thick at that time. Richter and Moore (1966) presented petrographic, modal, and chemical data on the core recovered from this early drilling.

The upper crust of Kilauea Iki was drilled again in 1967 by staff members of the Hawaiian Volcano Observatory, and core was recovered from three holes. In 1975, U.S. Geological Survey workers drilled three more holes, each a few feet away from one of the 1 967 holes. A summary of all work done on Kilauea Iki and other Hawaiian lava lakes through 1975 has been given by Wright et al. (1976).

The lake has been redrilled twice since 1975, by workers from Sandia Laboratories, as part of their Magma Energy Research program, in cooperation with the U.S. Geological Survey. In 1976, they drilled two holes near the center of the lake. In 1978-79, they drilled a total of six holes; one, commissioned by the U.S. Geological Survey, went completely through the lava lake near its north edge, into the pre-1959 lavas below.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80504","usgsCitation":"Helz, R.T., Banks, N.G., Casadevall, T.J., Fiske, R.S., and Moore, R.B., 1980, A catalogue of drill core recovered from Kilauea Iki lava lake, from 1967 to 1979: U.S. Geological Survey Open-File Report 80-504, 72 p., https://doi.org/10.3133/ofr80504.","productDescription":"72 p.","costCenters":[],"links":[{"id":140781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0504/report-thumb.jpg"},{"id":408713,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Iki lava lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.30925750732422,\n 19.39180098837034\n ],\n [\n -155.22171020507812,\n 19.39180098837034\n ],\n [\n -155.22171020507812,\n 19.43583809782748\n ],\n [\n -155.30925750732422,\n 19.43583809782748\n ],\n [\n -155.30925750732422,\n 19.39180098837034\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497ee4b0b290850ef3c7","contributors":{"authors":[{"text":"Helz, Rosalind Tuthill 0000-0003-1550-0684","orcid":"https://orcid.org/0000-0003-1550-0684","contributorId":85587,"corporation":false,"usgs":true,"family":"Helz","given":"Rosalind","email":"","middleInitial":"Tuthill","affiliations":[],"preferred":false,"id":154002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banks, Norman G.","contributorId":89524,"corporation":false,"usgs":true,"family":"Banks","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":154001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casadevall, Thomas J. 0000-0002-9447-6864 tcasadevall@usgs.gov","orcid":"https://orcid.org/0000-0002-9447-6864","contributorId":2734,"corporation":false,"usgs":true,"family":"Casadevall","given":"Thomas","email":"tcasadevall@usgs.gov","middleInitial":"J.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":154003,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fiske, Richard S.","contributorId":229675,"corporation":false,"usgs":false,"family":"Fiske","given":"Richard","email":"","middleInitial":"S.","affiliations":[{"id":36606,"text":"Smithsonian Institution","active":true,"usgs":false}],"preferred":false,"id":154000,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":154004,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":5878,"text":"pp1090 - 1980 - Ordovician and Silurian Phi Kappa and Trail Creek formations, Pioneer Mountains, central Idaho: Stratigraphic and structural revisions, and new data on graptolite faunas","interactions":[],"lastModifiedDate":"2023-08-29T20:47:29.939707","indexId":"pp1090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1090","title":"Ordovician and Silurian Phi Kappa and Trail Creek formations, Pioneer Mountains, central Idaho: Stratigraphic and structural revisions, and new data on graptolite faunas","docAbstract":"Recent geologic mapping in the northern Pioneer Mountains combined with the identification of graptolites from 116 new collections indicate that the Ordovician and Silurian Phi Kappa and Trail Creek Formations occur in a series of thrust-bounded slices within a broad zone of imbricate thrust faulting. Though confirming a deformational style first reported in a 1963 study by Michael Churkin, our data suggest that the complexity and regional extent of the thrust zone were not previously recognized. Most previously published sections of the Phi Kappa and Trail Creek Formations were measured across unrecognized thrust faults and therefore include not only structural repetitions of graptolitic Ordovician and Silurian rocks but also other tectonically juxtaposed lithostratigraphic units of diverse ages as well. Because of this discovery, the need to reconsider the stratigraphic validity of these formations and their lithology, nomenclature, structural distribution, facies relations, and graptolite faunas has arisen. \r\n\r\nThe Phi Kappa Formation in most thrust slices has internal stratigraphic continuity despite the intensity of deformation to which it was subjected. As revised herein, the Phi Kappa Formation is restricted to a structurally repeated succession of predominantly black, carbonaceous, graptolitic argillite and shale. Some limy, light-gray-weathering shale occurs in the middle part of the section, and fine-grained locally pebbly quartzite is present at the base. The basal quartzite is here named the Basin Gulch Quartzite Member of the Phi Kappa. The Phi Kappa redefined on a lithologic basis represents the span of Ordovician time from W. B. N. Berry's graptolite zones 2-4 through 15 and also includes approximately 17 m of lithologically identical shale of Early and Middle Silurian age at the top. The lower contact of the formation as revised is tectonic. The Phi Kappa is gradationally overlain by the Trail Creek Formation as restricted herein. Most of the coarser clastic rocks reported in previously measured sections of the Phi Kappa, as well as the sequence along Phi Kappa Creek from which the name originates, are excluded from the Phi Kappa as revised and are reassigned to two structural plates of Mississippian Copper Basin Formation; other strata now excluded from the formation are reassigned to the Trail Creek Formation and to an unnamed Silurian and Devonian unit. As redefined, the Phi Kappa Formation is only about 240 m thick, compared with the 3,860 m originally estimated, and it occupies only about 25 percent of the outcrop area previously mapped in 1930 by H. G. Westgate and C. P. Ross. Despite this drastic reduction in thickness and the exclusion of the rocks along Phi Kappa Creek, the name Phi Kappa is retained because of widely accepted prior usage to denote the Ordovician graptolitic shale facies of central Idaho, and because the Phi Kappa Formation as revised is present in thrust slices on Phi Kappa Mountain, at the head of Phi Kappa Creek. The lithic and faunal consistency of this unit throughout the area precludes the necessity for major facies telescoping along individual faults within the outcrop belt. However, tens of kilometers of tectonic shortening seems required to juxtapose the imbricated Phi Kappa shale facies with the Middle Ordovician part of the carbonate and quartzite shale sequence of east central Idaho. The shelf rocks are exposed in the Wildhorse structural window of the northeastern Pioneer Mountains, and attain a thickness of at least 1,500 m throughout the region north and east of the Pioneer Mountains. The Phi Kappa is in direct thrust contact on intensely deformed medium- to high-grade metamorphic equivalents of the same shelf sequence in the Pioneer window at the south end of the Phi Kappa-Trail Creek outcrop belt. Along East Pass, Big Lake, and Pine Creeks, north of the Pioneer Mountains, some rocks previously mapped as Ramshorn Slate are lithologically and faunally equivalent to the P","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1090","usgsCitation":"Dover, J.H., Berry, W.B., and Ross, R.J., 1980, Ordovician and Silurian Phi Kappa and Trail Creek formations, Pioneer Mountains, central Idaho: Stratigraphic and structural revisions, and new data on graptolite faunas: U.S. Geological Survey Professional Paper 1090, Report: vi, 54 p.; 1 Plate: 29.00 x 39.00 inches, https://doi.org/10.3133/pp1090.","productDescription":"Report: vi, 54 p.; 1 Plate: 29.00 x 39.00 inches","costCenters":[],"links":[{"id":104549,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4718.htm","linkFileType":{"id":5,"text":"html"},"description":"4718"},{"id":32698,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1090/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1090/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121437,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1090/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Pioneer Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -114.3333,\n 43.9297\n ],\n [\n -114.3333,\n 43.7728\n ],\n [\n -114.1667,\n 43.7728\n ],\n [\n -114.1667,\n 43.9297\n ],\n [\n -114.3333,\n 43.9297\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635245","contributors":{"authors":[{"text":"Dover, James H.","contributorId":43382,"corporation":false,"usgs":true,"family":"Dover","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":151728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, William B. N.","contributorId":76372,"corporation":false,"usgs":true,"family":"Berry","given":"William","email":"","middleInitial":"B. N.","affiliations":[],"preferred":false,"id":151729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Reuben James Jr.","contributorId":36911,"corporation":false,"usgs":true,"family":"Ross","given":"Reuben","suffix":"Jr.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":151727,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4300,"text":"cir833 - 1980 - Geological studies of the COST No. B-3 well, United States mid-Atlantic continental slope area","interactions":[],"lastModifiedDate":"2022-07-22T21:17:56.060978","indexId":"cir833","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"833","title":"Geological studies of the COST No. B-3 well, United States mid-Atlantic continental slope area","docAbstract":"The COST No. B-3 well is the first deep stratigraphic test to be drilled on the Continental Slope off the Eastern United States. The well was drilled in 2,686 ft (819 m) of water in the Baltimore Canyon trough area to a total depth of 15,820 ft (4,844 m) below the drill platform. It penetrated a section composed of mudstones, calcareous mudstones, and limestones of generally deep water origin to a depth of about 8.200 ft (2,500 m) below the drill floor. Light-colored, medium- to coarse-grained sandstones with intercalated gray and brown shales, micritic limestones, and minor coal and dolomite predominate from about 8,200 to 12,300 ft (2,500 to 3,750 m). From about 12,300 ft (3,750 m) to the bottom, the section consists of limestones (including oolitic and intraclastic grainstones) with interbedded fine-to medium-grained sandstones, dark-colored fissile shales, and numerous coal seams.\r\n\r\nBiostratigraphic examination has shown that the section down to approximately 6,000 ft (1,830 m) is Tertiary. The boundary between the Lower and Upper Cretaceous sections is placed between 8,600 and 9,200 ft (2,620 and 2,800 m) by various workers. Placement of the Jurassic-Cretaceous boundary shows an even greater range based on different organisms; it is placed variously between 12,250 and 13,450 ft (3,730 and 5,000 m). The oldest unit penetrated in the well is considered to be Upper Jurassic (Kimmeridgian) by some workers and Middle Jurassic (Callovian) by others. The Lower Cretaceous and Jurassic parts of the section represent nonmarine to shallow-marine shelf sedimentation. Upper Cretaceous and Tertiary units reflect generally deeper water conditions at the B-3 well site and show a general transition from deposition at shelf to slope water depths.\r\n\r\nExamination of cores, well cuttings, and electric logs indicates that potential hydrocarbon-reservoir units are present throughout the Jurassic and Cretaceous section. Porous and moderately permeable limestones and sandstones have been found in the Jurassic section, and significant thicknesses of sandstone with porosities as high as 30 percent and permeabilities in excess of 100 md have been encountered in the Cretaceous interval from about 7,000 to 12,000 ft (2,130 to 3,650 m).\r\n\r\nStudies of organic geochemistry, vitrinite reflectance, and color alteration of visible organic matter indicate that the Tertiary section, especially in its upper part, contains organic-carbon-rich sediments that are good potential oil source rocks. However, this part of the section is thermally immature and is unlikely to have acted as a source rock anywhere in the area of the B-3 well. The Cretaceous section is generally lean in organic carbon, the organic matter which is present is generally gas-prone, and the interval is thermally immature (although the lowest part of this section is approaching thermal maturity). The deepest part of the well, the Jurassic section, shows the onset of thermal maturity. The lower half of the Jurassic rocks has high organic-carbon contents with generally gas-prone organic matter. This interval is therefore considered to be an excellent possible gas source; it has a very high methane content.\r\n\r\nThe combination of gas-prone source rocks, thermal maturity, significant gas shows in the well at 15,750 ft (4,801 m) and porous reservoir rocks in the deepest parts of the well indicate a considerable potential for gas production from the Jurassic section in the area of the COST No. B-3 well. Wells drilled farther downslope from the B03 site may encounter more fully marine or deeper marine sections that may have a greater potential for oil (rather than gas) generation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir833","usgsCitation":"Scholle, P.A., 1980, Geological studies of the COST No. B-3 well, United States mid-Atlantic continental slope area: U.S. Geological Survey Circular 833, v, 132 p., https://doi.org/10.3133/cir833.","productDescription":"v, 132 p.","costCenters":[],"links":[{"id":404395,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22551.htm","linkFileType":{"id":5,"text":"html"}},{"id":31411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0833/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0833/report-thumb.jpg"}],"country":"United States","otherGeospatial":"mid-Atlantic continental slope area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72,\n 38.5\n ],\n [\n -74,\n 38.5\n ],\n [\n -74,\n 39.5\n ],\n [\n -72,\n 39.5\n ],\n [\n -72,\n 38.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687453","contributors":{"authors":[{"text":"Scholle, Peter A.","contributorId":48954,"corporation":false,"usgs":true,"family":"Scholle","given":"Peter","email":"","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":148767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56282,"text":"wdrWA792 - 1980 - Water resources data for Washington, water year 1979: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-14T20:34:55.644522","indexId":"wdrWA792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-79-2","title":"Water resources data for Washington, water year 1979: Vol. 2 - Eastern Washington","docAbstract":"

Water resources data for the 1979 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report, in two volumes, contains records for water discharge at 237 gaging stations; stage only at 5 gaging stations; stage and contents at 43 lakes and reservoirs; water quality at 135 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 88 crest-stage and 89 water-quality partial-record stations. Locations of sites in this volume are on figures 4, 5, and 19. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the national Water Data system operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Washington.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA792","collaboration":"Prepared in cooperation and with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Washington, water year 1979: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-79-2, x, 314 p., https://doi.org/10.3133/wdrWA792.","productDescription":"x, 314 p.","costCenters":[],"links":[{"id":410431,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1979/wa-79-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1979/wa-79-2/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aebb","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":532473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7548,"text":"ofr82398 - 1980 - Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56","interactions":[],"lastModifiedDate":"2022-09-26T19:10:40.19118","indexId":"ofr82398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"82-398","title":"Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56","docAbstract":"

This report summarizes our general knowledge of the petroleum potential, as well as problems and hazards associated with development of petroleum resources in the area proposed for nominations for lease sale number 56. This area includes the U.S. eastern continental margin from the North Carolina-Virginia border south to approximately Cape Canaveral, Florida and from three miles from shore, seaward to include the upper Continental Slope and inner Blake Plateau. The area for possible sales is shown in figure 1; major physiographic features of the region are shown in figure 2.

No wells have been drilled for petroleum within this proposed lease area and no significant commercial production has been obtained onshore in the Southeast Georgia Embayment. The COST GE-1 stratigraphic test well, drilled on the Continental Shelf off Jacksonville, Fla. (fig- 1), reached basement at 3,300 m. The bottom third of the section consists of dominantly continental rocks that are typically poor sources of petroleum (Scholle, 1979) and the rocks that contain organic carbon adequate for generation of petroleum at the well are seen in seismic profiles always at shallow subbottom depths, so they probably have not reached thermal maturity. However, seismic profiles indicate that the sedimentary deposits thicken markedly in a seaward direction where more of the section was deposited under marine conditions; therefore, commercial accumulations of petroleum offshore are more likely.

Several potential sources of environmental hazard exist. Among the most important are hurricanes, the Gulf Stream, and earthquakes. The potential danger from high wind, waves, storm surges, and storm-driven currents associated with hurricanes is obvious. Evidence for significant bottom scour by the Gulf Stream is abundant; such scour is a threat to the stability of bottom-mounted structures. The fast-flowing water also will hamper floating drill rigs and control of drill strings. A major earthquake of about magnitude 6.8 struck Charleston in 1886; it may have been associated with a zone of active seismicity that crosses South Carolina. The likelihood of a repetition of the 1886 event is presently not predictable but a seismic hazard must be assumed to exist.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82398","usgsCitation":"Dillon, W.P., Klitgord, K.D., Paull, C.K., Grow, J.A., Ball, M.M., Dolton, G., Powers, R.B., Khan, A.S., Popenoe, P., and Robb, J.M., 1980, Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56: U.S. Geological Survey Open-File Report 82-398, 61 p., https://doi.org/10.3133/ofr82398.","productDescription":"61 p.","costCenters":[],"links":[{"id":407344,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13718.htm","linkFileType":{"id":5,"text":"html"}},{"id":35009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0398/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":140845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0398/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.5,\n 29\n ],\n [\n -72,\n 29\n ],\n [\n -72,\n 38\n ],\n [\n -81.5,\n 38\n ],\n [\n -81.5,\n 29\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b9a","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paull, Charles K. 0000-0001-5940-3443","orcid":"https://orcid.org/0000-0001-5940-3443","contributorId":55825,"corporation":false,"usgs":false,"family":"Paull","given":"Charles","email":"","middleInitial":"K.","affiliations":[{"id":7043,"text":"University of North Carolina","active":true,"usgs":false}],"preferred":true,"id":704561,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grow, John A.","contributorId":25943,"corporation":false,"usgs":true,"family":"Grow","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":704562,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ball, Mahlon M.","contributorId":27472,"corporation":false,"usgs":true,"family":"Ball","given":"Mahlon","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704563,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dolton, Gordon","contributorId":50509,"corporation":false,"usgs":true,"family":"Dolton","given":"Gordon","email":"","affiliations":[],"preferred":false,"id":704564,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Powers, Richard B.","contributorId":52248,"corporation":false,"usgs":true,"family":"Powers","given":"Richard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":704565,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Khan, Abdul S.","contributorId":194534,"corporation":false,"usgs":false,"family":"Khan","given":"Abdul","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":704566,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704567,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704568,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":60712,"text":"mf1210 - 1980 - Maps showing kinds and sources of environmental geologic and geophysical data collected by the U.S. Geological Survey in the Baltimore Canyon trough area","interactions":[],"lastModifiedDate":"2016-08-23T09:17:15","indexId":"mf1210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1210","title":"Maps showing kinds and sources of environmental geologic and geophysical data collected by the U.S. Geological Survey in the Baltimore Canyon trough area","docAbstract":"

Exploration for petroleum on the Continental Shelf and Slope off the eastern United States has generated great interest in the quantity and quality of data available to evaluate the nature and magnitude of possible geological enveironmental hazards.  This set of maps presents a compilation of publicly available geological and geophysical data acquireed by the U.S. Geological Survey (USGS) in the Baltimore Canyon Trough area of the eastern United States Outer Continental Shelf and Slope.  Funding for the collection and analysis of much of the data indicated in this report was provided by the U.S. Bureau of Land Management.  Locations of blocks leased for petroleum development and locations of industry wells terminated or being drilled as of February 1980, as well as several other sampling sites, are included for comparison.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1210","usgsCitation":"Robb, J.M., and Kirby, J., 1980, Maps showing kinds and sources of environmental geologic and geophysical data collected by the U.S. Geological Survey in the Baltimore Canyon trough area: U.S. Geological Survey Miscellaneous Field Studies Map 1210, 4 Sheets: 41.82 x 36.40 inches or smaller, https://doi.org/10.3133/mf1210.","productDescription":"4 Sheets: 41.82 x 36.40 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":327465,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1210/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327466,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1210/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327467,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1210/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327468,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1210/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1210.PNG"}],"scale":"0","country":"United States","otherGeospatial":"Baltimore Canyon Trough","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75,37 ], [ -75,40 ], [ -72,40 ], [ -72,37 ], [ -75,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605b1a","contributors":{"authors":[{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":264272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirby, John R.","contributorId":91826,"corporation":false,"usgs":true,"family":"Kirby","given":"John R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":264271,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36728,"text":"fwsobs80_01_44 - 1980 - Selected vertebrate endangered species of the seacoast of the United States-the eastern cougar","interactions":[],"lastModifiedDate":"2012-02-02T00:09:52","indexId":"fwsobs80_01_44","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"80/01.44","title":"Selected vertebrate endangered species of the seacoast of the United States-the eastern cougar","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"National Fish And Wildlife Laboratory, 1980, Selected vertebrate endangered species of the seacoast of the United States-the eastern cougar: FWS/OBS 80/01.44, ca. 600 p. : ill., maps; 30 cm.","productDescription":"ca. 600 p. : ill., maps; 30 cm.","costCenters":[],"links":[{"id":165187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bea5","contributors":{"authors":[{"text":"National Fish And Wildlife Laboratory","contributorId":127936,"corporation":true,"usgs":false,"organization":"National Fish And Wildlife Laboratory","id":529555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46380,"text":"ofr801222 - 1980 - Map of the Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and water level contours for Spring 1979","interactions":[],"lastModifiedDate":"2022-09-28T18:14:51.364359","indexId":"ofr801222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1222","title":"Map of the Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and water level contours for Spring 1979","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801222","usgsCitation":"Lamb, C.E., 1980, Map of the Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and water level contours for Spring 1979: U.S. Geological Survey Open-File Report 80-1222, 1 Plate: 37.90 × 39.00 inches, https://doi.org/10.3133/ofr801222.","productDescription":"1 Plate: 37.90 × 39.00 inches","costCenters":[],"links":[{"id":168899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407523,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11498.htm","linkFileType":{"id":5,"text":"html"}},{"id":83347,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1222/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley-East Kern Water Agency area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.855,\n 34.3830\n ],\n [\n -117.628,\n 34.3830\n ],\n [\n -117.628,\n 35.361\n ],\n [\n -118.855,\n 35.361\n ],\n [\n -118.855,\n 34.3830\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658314","contributors":{"authors":[{"text":"Lamb, Charles Edwin","contributorId":33318,"corporation":false,"usgs":true,"family":"Lamb","given":"Charles","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":233189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24156,"text":"ofr80743 - 1980 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1977","interactions":[],"lastModifiedDate":"2022-12-27T21:41:38.499586","indexId":"ofr80743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-743","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1977","docAbstract":"

Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Dallas, Dallas County, Fort Worth, Houston, and San Antonio.

The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing gaging-station network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.

The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Salado Creek (lower station) at San Antonio are funded by the San Antonio River Authority in cooperation with the Texas Department of Water Resources and the U.S. Geological Survey.

 The operation and maintenance and collection of water-quality data at station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio are funded by the Edwards Underground Water District in cooperation with the Texas Department of Water Resources and the U.S. Geological Survey. These stations will provide hydrologic data on similar and adjacent drainage basins. One drainage basin is undergoing extensive urbanization while the other is undeveloped.

 The objective of the San Antonio urban-hydrology study are:

  1.  To provide data showing the effects of various stages of urbanization on flood discharge and runoff.
  2.  To provide water-quality data on surface-water runoff from floods of various magnitudes, during all seasons of the year from areas with different types of utilization.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr80743","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., and Harmsen, L., 1980, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1977: U.S. Geological Survey Open-File Report 80-743, 99 p., https://doi.org/10.3133/ofr80743.","productDescription":"99 p.","numberOfPages":"105","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1977-01-01","temporalEnd":"1977-12-31","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":286628,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411086,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75284.htm","linkFileType":{"id":5,"text":"html"}},{"id":286627,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0743/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.8165283203125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.123373210819224\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607b71","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":191417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harmsen, Lynn","contributorId":19941,"corporation":false,"usgs":true,"family":"Harmsen","given":"Lynn","email":"","affiliations":[],"preferred":false,"id":191416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21654,"text":"ofr80231 - 1980 - Chemical analyses, correlations, and ages of late Cenozoic tephra units of east-central and Southern California","interactions":[{"subject":{"id":21654,"text":"ofr80231 - 1980 - Chemical analyses, correlations, and ages of late Cenozoic tephra units of east-central and Southern California","indexId":"ofr80231","publicationYear":"1980","noYear":false,"title":"Chemical analyses, correlations, and ages of late Cenozoic tephra units of east-central and Southern California"},"predicate":"SUPERSEDED_BY","object":{"id":45716,"text":"pp1293 - 1984 - Chemical analyses, correlations, and ages of upper Pliocene and Pleistocene ash layers of east-central and Southern California","indexId":"pp1293","publicationYear":"1984","noYear":false,"title":"Chemical analyses, correlations, and ages of upper Pliocene and Pleistocene ash layers of east-central and Southern California"},"id":1}],"supersededBy":{"id":45716,"text":"pp1293 - 1984 - Chemical analyses, correlations, and ages of upper Pliocene and Pleistocene ash layers of east-central and Southern California","indexId":"pp1293","publicationYear":"1984","noYear":false,"title":"Chemical analyses, correlations, and ages of upper Pliocene and Pleistocene ash layers of east-central and Southern California"},"lastModifiedDate":"2025-04-15T16:38:56.520596","indexId":"ofr80231","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-231","title":"Chemical analyses, correlations, and ages of late Cenozoic tephra units of east-central and Southern California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80231","issn":"0566-8174","usgsCitation":"Sarna-Wojcicki, A.M., Bowman, H., Meyer, C., Russell, P., Asaro, F., Michael, H., Rowe, J., Baedecker, P.A., and McCoy, G., 1980, Chemical analyses, correlations, and ages of late Cenozoic tephra units of east-central and Southern California: U.S. Geological Survey Open-File Report 80-231, Report: iii, 57 p.; 1 Plate: 37.84 x 30.07 inches, https://doi.org/10.3133/ofr80231.","productDescription":"Report: iii, 57 p.; 1 Plate: 37.84 x 30.07 inches","costCenters":[],"links":[{"id":482567,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0231/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155182,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0231/report-thumb.jpg"},{"id":375165,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0231/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.67333984374999,\n 37.94419750075404\n ],\n [\n -122.32177734375,\n 36.98500309285596\n ],\n [\n -122.14599609375001,\n 36.10237644873644\n ],\n [\n -120.91552734375,\n 35.24561909420681\n ],\n [\n -120.58593749999999,\n 34.488447837809304\n ],\n [\n -120.30029296875,\n 34.30714385628804\n ],\n [\n -119.20166015625,\n 33.96158628979907\n ],\n [\n -118.10302734374999,\n 33.54139466898275\n ],\n [\n -117.53173828125,\n 33.211116472416855\n ],\n [\n -117.04833984375001,\n 32.52828936482526\n ],\n [\n -114.67529296874999,\n 32.731840896865684\n ],\n [\n -114.19189453125,\n 34.288991865037524\n ],\n [\n -114.58740234375,\n 34.994003757575776\n ],\n [\n -118.71826171875,\n 38.06539235133249\n ],\n [\n -122.67333984374999,\n 37.94419750075404\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e498e","contributors":{"authors":[{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":185081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowman, H.W.","contributorId":88770,"corporation":false,"usgs":true,"family":"Bowman","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":185085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, C.E.","contributorId":104023,"corporation":false,"usgs":true,"family":"Meyer","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":185088,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Russell, P.C.","contributorId":102856,"corporation":false,"usgs":true,"family":"Russell","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":185087,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Asaro, Frank","contributorId":65450,"corporation":false,"usgs":true,"family":"Asaro","given":"Frank","email":"","affiliations":[],"preferred":false,"id":185084,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Michael, Helen","contributorId":64627,"corporation":false,"usgs":true,"family":"Michael","given":"Helen","email":"","affiliations":[],"preferred":false,"id":185083,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":185082,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Baedecker, P. A.","contributorId":95444,"corporation":false,"usgs":true,"family":"Baedecker","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":185086,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McCoy, G.A.","contributorId":105757,"corporation":false,"usgs":true,"family":"McCoy","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":185089,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":24525,"text":"ofr80403 - 1980 - Hydrologic setting of Williams Lake, Hubbard County, Minnesota","interactions":[],"lastModifiedDate":"2022-09-15T18:12:26.459915","indexId":"ofr80403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-403","title":"Hydrologic setting of Williams Lake, Hubbard County, Minnesota","docAbstract":"

The hydrology and geology of Williams Lake watershed was studied to evaluate the accuracy of various methods used to determine precipitation and evaporation in lake water-balance studies and to define a lake and ground-water system according to approaches suggested by theoretical modeling studies. Regression analysis between estimated and measured precipitation at the lake showed that the accuracy of regionalization techniques is dependent on the closeness of the data network to the lake. For individual storms, the average-value method was found to be better than either the weighted average or isohyetal methods of determining precipitation, but it was least accurate in estimating 14-day average precipitation. The amount of evaporation calculated by the mass-transfer method ranged from 2 to 7 inches per month from July to October 1978, depending on the method used to determine the mass-transfer coefficient. Test drilling indicated that 30 to 150 feet of sand and gravel overlies till in the Williams Lake watershed. A sand lens about 50 feet thick occurs within the till.

\n

The configuration of the water table and vertical-head gradients measured from July to December 1978 indicate that ground water moves into the lake from the south and east and moves from the lake into the ground-water reservoir to the west. Preliminary numerical models indicate that the sand lens within the till is effectively isolated from the flow system interacting with the lake and that both inseepage and outseepage were about 1.4 inches from mid-July to mid-October 1978. When estimated as a residual in a water balance, ground water showed a net outseepage only of 1.47 inches.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr80403","collaboration":"Prepared in cooperation with Minnesota Department of Natural* Resources Division of Waters","usgsCitation":"Siegel, D., and Winter, T.C., 1980, Hydrologic setting of Williams Lake, Hubbard County, Minnesota: U.S. Geological Survey Open-File Report 80-403, vii, 56 p., https://doi.org/10.3133/ofr80403.","productDescription":"vii, 56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":53576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0403/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406774,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25793.htm"},{"id":156479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0403/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Hubbard County","otherGeospatial":"Williams Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.67845916748047,\n 46.948152929705195\n ],\n [\n -94.66163635253906,\n 46.948152929705195\n ],\n [\n -94.66163635253906,\n 46.959870280492964\n ],\n [\n -94.67845916748047,\n 46.959870280492964\n ],\n [\n -94.67845916748047,\n 46.948152929705195\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60547b","contributors":{"authors":[{"text":"Siegel, Donald I.","contributorId":97499,"corporation":false,"usgs":true,"family":"Siegel","given":"Donald I.","affiliations":[],"preferred":false,"id":192082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24572,"text":"ofr80568 - 1980 - Ground-water appraisal in northwestern Big Stone County, west-central Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:06:27","indexId":"ofr80568","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-568","title":"Ground-water appraisal in northwestern Big Stone County, west-central Minnesota","docAbstract":"

The development of ground water for irrigation in northwestern Big Stone County has not kept up with development in other irrigable areas of the State. This is due, in part, to the absence of extensive surficial aquifers and the difficulty in locating buried aquifers.

\n

Test augering south of Beardsley outlined a small surficial aquifer that consists of outwash deposits of sand and gravel. The aquifer is elongate, trending northeast-southwest, with a maximum saturated thickness of 42 feet and an areal extent of about 5 square miles.

\n

Deep test drilling showed that small buried outwash aquifers occur over much of the project area. The 2-mile spacing between test holes, however, was too great to permit correlation of the buried aquifers.

\n

A major buried outwash aquifer, east of Beardsley, consists of 130 feet of fine, uniform quartz sand, The aquifer lies in a steep-sided northwest-southeast trending valley eroded in bedrock and is overlain by 130 feet of clayey till. Pumping-test results indicate that its transmissivity ranges from 10,800 to 13,400 feet squared per day, and that the storage coefficient ranges from 0.0001 to 0.002. Recharge to the aquifer was negligible during 1979.

\n

Two Cretaceous aquifers, the Codell Sandstone Member of the Carlile Shale and the Greenhorn Formation, underlie the area, but little is known about these aquifers.

\n

Samples of water were collected for chemical analysis from wells in the surficial outwash, buried outwash, and Cretaceous aquifers. With the exception of nitrate, the greatest difference in chemical quality was between samples from the buried outwash and Cretaceous aquifers. Water from Cretaceous aquifers is softer than water from the outwash aquifers, but contains concentrations of sodium and boron that are high enough to damage soils and crops if used for irrigation. Nitrate concentrations exceeded the Minnesota Pollution Control Agency's recommended limits for drinking water in one sample from the surficial aquifer.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr80568","issn":"0094-9140","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, and Big Stone County Ground-Water Steering Committee","usgsCitation":"Soukup, W., 1980, Ground-water appraisal in northwestern Big Stone County, west-central Minnesota: U.S. Geological Survey Open-File Report 80-568, v, 41 p., https://doi.org/10.3133/ofr80568.","productDescription":"v, 41 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":95512,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0568/report.pdf","size":"3007","linkFileType":{"id":1,"text":"pdf"}},{"id":155096,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0568/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Big Stone County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.8363,45.5858],[-96.2535,45.5862],[-96.2425,45.5864],[-96.2412,45.4136],[-96.1185,45.4133],[-96.1176,45.241],[-96.1033,45.2408],[-96.1046,45.1896],[-96.1044,45.1859],[-96.105,45.1823],[-96.1049,45.18],[-96.1128,45.1839],[-96.1266,45.1896],[-96.1404,45.1944],[-96.148,45.191],[-96.1604,45.194],[-96.1748,45.1983],[-96.1827,45.2018],[-96.186,45.2031],[-96.2023,45.2046],[-96.2096,45.2108],[-96.2144,45.2171],[-96.2224,45.2211],[-96.2334,45.2222],[-96.2469,45.2206],[-96.258,45.2213],[-96.269,45.2224],[-96.2769,45.2245],[-96.2797,45.2309],[-96.2813,45.2359],[-96.2846,45.239],[-96.286,45.2417],[-96.2888,45.2453],[-96.2921,45.2471],[-96.2973,45.2483],[-96.3058,45.2495],[-96.3155,45.2502],[-96.3253,45.2514],[-96.3391,45.2548],[-96.3547,45.2567],[-96.3593,45.2575],[-96.3638,45.257],[-96.3826,45.2575],[-96.391,45.2573],[-96.4027,45.258],[-96.4091,45.2569],[-96.4144,45.2596],[-96.4277,45.2695],[-96.4536,45.2693],[-96.4536,45.2695],[-96.453,45.2802],[-96.4523,45.2941],[-96.4521,45.2978],[-96.4519,45.3022],[-96.4538,45.3074],[-96.4582,45.3116],[-96.4588,45.3121],[-96.4616,45.3142],[-96.4668,45.3179],[-96.4697,45.3239],[-96.4692,45.3265],[-96.47,45.3289],[-96.4728,45.3346],[-96.4736,45.3363],[-96.4752,45.3395],[-96.4772,45.3432],[-96.4793,45.3471],[-96.4839,45.3518],[-96.4874,45.3553],[-96.4946,45.3626],[-96.4981,45.3648],[-96.5017,45.3671],[-96.5059,45.3698],[-96.5121,45.3717],[-96.5181,45.3736],[-96.5232,45.3752],[-96.5301,45.3774],[-96.5372,45.3792],[-96.5443,45.381],[-96.5544,45.3836],[-96.5582,45.3852],[-96.5662,45.3886],[-96.5734,45.3918],[-96.5814,45.3952],[-96.5892,45.3985],[-96.5943,45.4007],[-96.6008,45.4046],[-96.6087,45.4094],[-96.6119,45.4096],[-96.6184,45.41],[-96.6301,45.41],[-96.6418,45.41],[-96.6457,45.41],[-96.6535,45.4104],[-96.6619,45.4109],[-96.6742,45.4115],[-96.6767,45.4123],[-96.6792,45.4133],[-96.6934,45.4229],[-96.6977,45.427],[-96.7013,45.4304],[-96.71,45.438],[-96.731,45.4587],[-96.7317,45.4593],[-96.7349,45.4642],[-96.7391,45.4715],[-96.7426,45.4777],[-96.7475,45.4838],[-96.7516,45.4984],[-96.7528,45.5011],[-96.7539,45.5035],[-96.7629,45.517],[-96.7642,45.5189],[-96.7734,45.5286],[-96.7757,45.5307],[-96.7848,45.5388],[-96.7921,45.5457],[-96.8002,45.5533],[-96.8043,45.5571],[-96.8144,45.5664],[-96.8245,45.575],[-96.829,45.5789],[-96.8363,45.5858]]]},\"properties\":{\"name\":\"Big Stone\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3e7","contributors":{"authors":[{"text":"Soukup, W.G.","contributorId":82732,"corporation":false,"usgs":true,"family":"Soukup","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":192175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8210,"text":"ofr801016 - 1980 - Technique for estimating magnitude and frequency of floods in Maryland","interactions":[],"lastModifiedDate":"2023-03-14T22:55:36.271712","indexId":"ofr801016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1016","title":"Technique for estimating magnitude and frequency of floods in Maryland","docAbstract":"

A method is presented for estimating flood magnitudes for natural drainage basins without urban development or regulated flow. The method was developed by multiple-regression techniques and applies to floods with recurrence intervals from 2 to 100 years.

The State is divided into three regions, and sets of equations for calculating peak discharges based on physical basin characteristics are provided for each region. In the northern region, flood-peak discharges are related to drainage area, forest cover, and 2-year 24-hour rainfall. In the southern region, flood peaks are related to drainage area alone. In the eastern region, peaks are related to drainage area, slope, storage, forest cover, and two composite soil categories. Standard errors of estimate for the regression equations in the northern region range from 38 to 49 percent. For the southern region, the standard errors of estimate vary from 52 to 86 percent, and for the eastern region they vary from 37 to 40 percent.

Maximum observed flood peaks, basin characteristics, and flood-frequency characteristics are tabulated for 234 gaged sites in Maryland and nearby in surrounding states. At 39 of these sites, a rainfall-runoff model was used to obtain synthetic flood-frequency data. These data were combined with observed flood-frequency data to determine the final flood-frequency distributions.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686205","contributors":{"authors":[{"text":"Carpenter, David H.","contributorId":49357,"corporation":false,"usgs":true,"family":"Carpenter","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24773,"text":"ofr801005 - 1980 - Floods of January and February 1980 in California","interactions":[],"lastModifiedDate":"2017-06-02T14:02:58","indexId":"ofr801005","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1005","title":"Floods of January and February 1980 in California","docAbstract":"

During January and February 1980, storms caused substantial rises in streamflow throughout much of California. In mid-January flooding occurred in the foothills of the Sierra Nevada and in the central coast area. In late January and mid-February, high floodflows in streams in coastal southern California caused much damage and several deaths. The Tijuana River in northern Baja California (Mexico) and southern San Diego County flooded many square miles of lowlands as its flow during two separate flooding episodes exceeded all records. Most reservoirs in San Diego County spilled, several for the first time since their completion. Lake Elsinore, in eastern Riverside County, caused much damage to lakeside property as it filled to an elevation not reached since 1916.

The February flooding in southern California was caused by a series of storms separated by short intervals. Some peaks of record were observed, and streamflow throughout the area remained high for a relatively long period. In many streams, the volumes of sustained flow for periods of 7 and 15 consecutive days were the greatest that have occurred during the period of record.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801005","issn":"0094-9140","usgsCitation":"Wahl, K.L., Crippen, J.R., and Knott, J.M., 1980, Floods of January and February 1980 in California: U.S. Geological Survey Open-File Report 80-1005, iv, 56 p., https://doi.org/10.3133/ofr801005.","productDescription":"iv, 56 p.","costCenters":[],"links":[{"id":156375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1005/report-thumb.jpg"},{"id":94490,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1005/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfcee","contributors":{"authors":[{"text":"Wahl, Kenneth L.","contributorId":61024,"corporation":false,"usgs":true,"family":"Wahl","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crippen, John R.","contributorId":13208,"corporation":false,"usgs":true,"family":"Crippen","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":192538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knott, J. M.","contributorId":77909,"corporation":false,"usgs":true,"family":"Knott","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192540,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25024,"text":"pp1064B - 1980 - Composition and properties of the Pierre Shale and equivalent rocks, northern Great Plains region","interactions":[],"lastModifiedDate":"2019-12-09T06:54:51","indexId":"pp1064B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1064","chapter":"B","title":"Composition and properties of the Pierre Shale and equivalent rocks, northern Great Plains region","docAbstract":"The Pierre Shale and equivalent rocks of Late Cretaceous age consist in the east-central Dakotas of several hundred feet of offshore-marine shale and minor marl; in west-central Montana near the sediment source the equivalents of the Pierre Shale consist of several thousand feet of volcanic-rich and mostly nonmarine sediments; and in the area between, both types of rock are separated by tongues of nearshore-marine siltstone and sandstone that mark three major transgressions of the sea across the area. The major-, minor-, and trace-element composition was determined for 226 samples of these rocks, and the mineralogical composition was determined for 1,350 samples. Slurry pH, Atterberg limits, and grain and bulk densities were determined on some samples. \r\n\r\nThe arithmetic mean, in percent, and standard deviation (in parentheses) of major and minor elements, mostly in shale and siltstone and excluding the 23 chemically analyzed bentonite samples, are as follows: \r\n\r\nSiO2 60.8 (7.9)\r\nAl2O3 14.4 (2.5)\r\nFe2O3 3.4 (1.4)\r\nFeO 1.1 (1.2)\r\nMgO 2.2 (1.0)\r\nCaO 2.7 (0.48)\r\nNa2O 1.1 (0.56)\r\nK2O 2.4 (0.57)\r\nH2O- 3.2 (1.3)\r\nH2O+ 4.3 (1.2)\r\nTiO2 0.58 (0.12)\r\nP2O5 0.14 (0.073)\r\nS 0.37 (1.1)\r\nF 0.71 (0.15)\r\nCl 0.16 (0.024)\r\nCO2 2.1 (7.0)\r\nC, organic 0.94 (1.8)\r\n\r\nThe mean and standard deviation of minerals as determined by X-ray methods, excluding bentonite samples, is as follows: clay minerals, 53 (20); quartz, 24 (13); cristobalite, 1 (5); potassium-feldspar, 1 (2); plagioclase, 6 (7); anorthite content from 20 to 40 percent; calcite, 5 (14); dolomite, 4 (7); organic matter, 1 (2); and sparsely scattered gypsum, jarosite, pyrite, zeolites, augite, siderite, and probably minor amounts of hydrated iron-manganese (Fe-Mn) oxides. The mean and standard deviation of the clay-mineral fraction is as follows: mixed-layer illite-smectite, 70 (20); illite, 16 (9); chlorite, 3 (6); and kaolinite, 9 (13). The mixed-layer clay, except in the Montana disturbed belt, is a random interlayering of 20 to 60 percent illite-type layers, about 35 percent beidelite-type layers, and the remainder montmorillonite-type layers; chlorite or vermiculite layers are rare. \r\n\r\nMost bentonite differs from shale in its small quartz content, rarely more than a few percent, in the more calcic composition and hightemperature thermal state of its plagioclase, and in its rare kaolinite, near absence of chlorite, and lack of illite-either free or mixed layered with smectite. Bentonite commonly consists of more than 90 percent smectite in which montmorillonite is interlayered with a smaller amount of beidellite. \r\n\r\nThe clay-mineral composition of marine rock, including proportions of layers in the dominant illite-smectite, averages about the same as in the nonmarine rock, though in the latter the composition is more variable. The average content of major chemical constituents also is closely similar, partly because the large clay content of fine-grained offshore-marine shale is balanced by the small clay content of nearshore-marine siltstone and sandstone. In addition, the alumina and alkalic elements in an average of 10 percent more clay in marine rock are partly balanced by these constituents in the 5 percent more feldspar in nonmarine rock. Much of the observed regional and stratigraphic variation in maj or constituents is the result of the three major east-west migrations of the depositional sites of nearshore-marine sandstone and siltstone. Dolomite is found almost exclusively in relatively coarse-grained rock, particularly in nearshore-marine siltstone where diagenetic dolomite is expected, but it is found almost as frequently in nonmarine siltstone. Amounts of minor constituents are nearly equal in marine and nonmarine rocks, except that pyrite and consequently sulfur are relatively sparse in nonmarine rock. Average amounts of organic matter found in marine and nonmarine rocks are nearly identical. However, organic matter in nonmarine rock occurs almost entirely in volumetric","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1064B","usgsCitation":"Schultz, L.G., Tourtelot, H.A., Gill, J.R., and Boerngen, J., 1980, Composition and properties of the Pierre Shale and equivalent rocks, northern Great Plains region: U.S. Geological Survey Professional Paper 1064, v. 1064 B, Report: 114 p.; 1 Plate: 25.50 x 40.25 inches, https://doi.org/10.3133/pp1064B.","productDescription":"Report: 114 p.; 1 Plate: 25.50 x 40.25 inches","startPage":"1","endPage":"114","costCenters":[],"links":[{"id":54030,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1064b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1064b/report-thumb.jpg"},{"id":54031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1064b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States ","state":"North Dakota, South Dakota, Montana 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\"}}]}","volume":"1064 B","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a822a","contributors":{"authors":[{"text":"Schultz, Leonard Gene","contributorId":19146,"corporation":false,"usgs":true,"family":"Schultz","given":"Leonard","email":"","middleInitial":"Gene","affiliations":[],"preferred":false,"id":193079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tourtelot, H. A.","contributorId":79140,"corporation":false,"usgs":true,"family":"Tourtelot","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gill, J. R.","contributorId":8125,"corporation":false,"usgs":true,"family":"Gill","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":193078,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boerngen, J.G.","contributorId":28974,"corporation":false,"usgs":true,"family":"Boerngen","given":"J.G.","affiliations":[],"preferred":false,"id":193080,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20811,"text":"ofr80327 - 1980 - Water-supply assessment of the Laramie-Fox Hills aquifer in parts of Adams, Boulder, Jefferson, and Weld Counties, Colorado","interactions":[],"lastModifiedDate":"2022-09-22T19:06:42.255253","indexId":"ofr80327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-327","title":"Water-supply assessment of the Laramie-Fox Hills aquifer in parts of Adams, Boulder, Jefferson, and Weld Counties, Colorado","docAbstract":"

Groundwater in the Laramie-Fox Hills aquifer is a potential source of supplemental municipal water supplies for the communities of Erie, Lafayette, Louisville, and Superior in Colorado. The present water supplies for these communities are not always adequate to meet current demands. The U.S. Geological Survey made a water-supply assessment of the Laramie-Fox Hills aquifer for the U.S. Bureau of Reclamation, which is investigating and evaluating alternative sources of water for the communities. Recharge to the aquifer is mostly in the western and southwestern parts of the study area. Groundwater movement is generally from the southwest to northeast. Groundwater discharge in the study area is primarily by pumping wells. Since 1961, this pumping has caused water-level declines of about 250 to 300 feet from Broomfield to east of Erie, Colorado. Generally, water levels in other parts of the area have remained the same. The aggregate sand thickness determined from well logs ranges from 42 to 360 feet and the mean thickness is 229 feet. The volume of groundwater in storage in the study area is about 5 million acre-feet. Reported yields from 93 wells ranged from 1 to 90 gallons per minute and averaged 22 gallons per minute. Well yields tended to be larger in the areas where aggregate sand thickness is the greatest. The water generally changes from a sodium calcium bicarbonate type to a sodium calcium sulfate type as it moves through the aquifer away from the recharge areas. The maximum limit established by the U.S. Environmental Protection Agency for nitrite plus nitrate in public-water supplies was exceeded in water from three wells, the maximum limit for fluoride was exceeded in water from two wells, and the maximum limit for selenium was exceeded in water from three wells.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80327","usgsCitation":"Schneider, P., 1980, Water-supply assessment of the Laramie-Fox Hills aquifer in parts of Adams, Boulder, Jefferson, and Weld Counties, Colorado (WRI/OFR): U.S. Geological Survey Open-File Report 80-327, Report: iv, 17 p.; 6 Plates: 21.00 × 28.00 inches, https://doi.org/10.3133/ofr80327.","productDescription":"Report: iv, 17 p.; 6 Plates: 21.00 × 28.00 inches","costCenters":[],"links":[{"id":108031,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11607.htm","linkFileType":{"id":5,"text":"html"},"description":"11607"},{"id":50361,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0327/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50360,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0327/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50359,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0327/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50358,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0327/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50357,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0327/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0327/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0327/report-thumb.jpg"},{"id":50356,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0327/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Adams County, Boulder County, Jefferson county, Weld County","otherGeospatial":"Laramie-Fox Hills aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.25,\n 39.875\n ],\n [\n -105,\n 39.875\n ],\n [\n -105,\n 40.125\n ],\n [\n -105.25,\n 40.125\n ],\n [\n -105.25,\n 39.875\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4813e4b07f02db4da29e","contributors":{"authors":[{"text":"Schneider, Paul A.","contributorId":32509,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul A.","affiliations":[],"preferred":false,"id":183293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48617,"text":"ofr801219 - 1980 - Water resources investigations in New York, 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:10:39","indexId":"ofr801219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1219","title":"Water resources investigations in New York, 1980","docAbstract":"This report describes the water-resources investigations conducted by the U.S. Geological Survey in New York in 1980; many of these studies will continue into 1981 or longer. The Geological Survey began its water-resources studies in New York State in 1895 with a stream-gaging program in the Catskill Mountain region and entered its first cooperative program, with the Office of the State Engineer, in 1900. Since 1910, the Survey has maintained a District office in Albany to direct its water investigations within the State. A Long Island subdistrict office was established in 1932 to monitor and study the ground-water situation in this area of increasing urbanization. Subdistrict offices are also maintained in Ithaca and Albany to collect and interpret data from western and eastern New York, respectively. A field station is maintained in Potsdam to collect records in the northernmost part of the State. A bibliography of reports published or released in 1980 by the New York District is included. (USGS)","language":"ENGLISH","doi":"10.3133/ofr801219","usgsCitation":"Finch, A.J., 1980, Water resources investigations in New York, 1980: U.S. Geological Survey Open-File Report 80-1219, v, 68 p. : ill., maps ; 28 cm., https://doi.org/10.3133/ofr801219.","productDescription":"v, 68 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":172403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94497,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015046045848?urlappend=%3Bseq=3"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08ac","contributors":{"authors":[{"text":"Finch, Anne J. (compiler)","contributorId":106189,"corporation":false,"usgs":true,"family":"Finch","given":"Anne","suffix":"(compiler)","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":237866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7744,"text":"ofr80362 - 1980 - Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington","interactions":[{"subject":{"id":7744,"text":"ofr80362 - 1980 - Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington","indexId":"ofr80362","publicationYear":"1980","noYear":false,"title":"Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington"},"predicate":"SUPERSEDED_BY","object":{"id":70047780,"text":"70047780 - 1980 - Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington","indexId":"70047780","publicationYear":"1980","noYear":false,"title":"Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington"},"id":1}],"supersededBy":{"id":70047780,"text":"70047780 - 1980 - Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington","indexId":"70047780","publicationYear":"1980","noYear":false,"title":"Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington"},"lastModifiedDate":"2024-02-28T22:28:27.903501","indexId":"ofr80362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-362","title":"Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington","docAbstract":"

This summary of southwestern Washington stratigraphy describes the principal Tertiary formations comprising the Cenozoic sequences. A field trip road log provides directions for access to type and/or reference localities for each formation discussed.

Tertiary rocks of southwestern Washington, measuring nearly 13,000 feet in thickness, are mapped as thirteen formational units. These units crop out within several structural basins formed along the tectonically active Pacific margin of the North American Plate. Thick Quaternary sands and gravels of glacial and fluvial origin and a heavy vegetational cover restrict exposures to stream and river banks, highway, road and railroad cuts, and occasional steep hillsides.

The Tertiary strata are predominantly marine sedimentary rocks with interbedded volcanics and eastwardly increasing amounts of nonmarine strata. Age equivalent and genetically similar sequences occur throughout the Coast Ranges of western Oregon and Washington.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80362","usgsCitation":"Armentrout, J.M., 1980, Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington: U.S. Geological Survey Open-File Report 80-362, 72 p., https://doi.org/10.3133/ofr80362.","productDescription":"72 p.","costCenters":[],"links":[{"id":426089,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0362/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142009,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0362/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"southwestern Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.20760160457772,\n 47.23490254061741\n ],\n [\n -124.20760160457772,\n 45.92227795638976\n ],\n [\n -122.06227461237941,\n 45.92227795638976\n ],\n [\n -122.06227461237941,\n 47.23490254061741\n ],\n [\n -124.20760160457772,\n 47.23490254061741\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea81","contributors":{"authors":[{"text":"Armentrout, John M.","contributorId":13980,"corporation":false,"usgs":true,"family":"Armentrout","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11255,"text":"ofr8068 - 1980 - Water-quality data for canals in eastern Broward County, Florida, 1975-78","interactions":[],"lastModifiedDate":"2022-05-17T18:25:27.193174","indexId":"ofr8068","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-68","title":"Water-quality data for canals in eastern Broward County, Florida, 1975-78","docAbstract":"

Increased urbanization in Broward County has contributed to canals being used as receptacles for urban wastes, sewage effluent, and stormwater runoff. The introduction of contaminants into the canals may affect the water quality. In 1969 the U.S. Geological Survey, in cooperation with the Broward County Pollution Control Board and the South Florida Water Management District, began to monitor the water-quality in canals of eastern Broward County. This report presents selected water-quality data collected from the canals, October 1974 through September 1978, in eastern Broward County. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8068","collaboration":"Prepared in cooperation with the Broward County Environmental Quality Control Board and the South Florida Water Management District","usgsCitation":"Sonntag, W.H., 1980, Water-quality data for canals in eastern Broward County, Florida, 1975-78: U.S. Geological Survey Open-File Report 80-68, iii, 161 p., https://doi.org/10.3133/ofr8068.","productDescription":"iii, 161 p.","costCenters":[],"links":[{"id":145792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0068/report-thumb.jpg"},{"id":400714,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Broward County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.37981,25.949959 ], [ -80.37981,26.37992 ], [ -80.060996,26.37992 ], [ -80.060996,25.949959 ], [ -80.37981,25.949959 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e7c","contributors":{"authors":[{"text":"Sonntag, W. H.","contributorId":106127,"corporation":false,"usgs":true,"family":"Sonntag","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6302,"text":"pp1146 - 1980 - Revised nomenclature and stratigraphic relationships of the Fredericksburg Complex and Quantico Formation of the Virginia Piedmont","interactions":[],"lastModifiedDate":"2019-09-10T09:37:04","indexId":"pp1146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1146","title":"Revised nomenclature and stratigraphic relationships of the Fredericksburg Complex and Quantico Formation of the Virginia Piedmont","docAbstract":"The Fredericksburg Complex, in part a migmatitic terrane in northeast Virginia, is subdivided on the basis of lithology, as well as aeromagnetic and aeroradiometric data, into two metamorphic suites. These suites are separated by the northeast-trending Spotsylvania lineament, a rectilinear geophysical feature that is probably the trace of an old fault zone. East of the lineament, the Po River Metamorphic Suite, of Proterozoic Z and (or) early Paleozoic age, consists dominantly of biotite gneiss, generally augen gneiss, and lesser amounts of hornblende gneiss and mica schist. West of the Spotsylvania lineament is the Ta River Metamorphic Suite, composed mostly of amphibolite and amphibole gneiss. However, to the southwest, along its strike belt, the Ta River contains abundant biotite gneiss and mica schist. Both the Ta River and Po River contain abundant foliated granitoid and pegmatoid bodies as concordant tabular masses and as crosscutting dikes; these rocks are considered part of the Ta River and Po River Metamorphic Suites. The amphibolitic Holly Corner Gneiss is interpreted to be a western allochthonous equivalent of the Ta River. Both the Ta River and Holly Corner are considered to be coeval, eastern, distal facies of the Lower Cambrian(?) Chopawamsic Formation. The Paleozoic Falls Run Granite Gneiss intrudes the Ta River Metamorphic Suite and the Holly Corner Gneiss; locally the Falls Run is interpreted to have been transported westward with the Holly Corner after intrusion. \r\n\r\nThe Quantico Formation, in the core of the Quantico-Columbia synclinorium, rests with angular unconformity along its northwest and southeast limbs, respectively, on the Chopawamsic Formation and the Ta River Metamorphic Suite. The Quantico Formation is assigned the same Late Ordovician age and similar stratigraphic position as the Arvonia Slate of the Arvonia syncline. \r\n\r\nThe youngest rocks of the area are the granitoid and pegmatoid bodies of the Falmouth Intrusive Suite. They consist of several generations of chiefly dikes and sills that are intrusive into the Fredericksburg Complex and into the Quantico Formation. Granitoid rocks also form small plutons. The Falmouth is isotopically dated as Carboniferous in age. \r\n\r\nSome of the metavolcanic rocks of the Evington Group and part of the amphibolite gneiss and amphibolite of the Hatcher Complex, named by W. B. Brown in 1969, are probably coeval with the Chopawamsic Formation and hence equivalents of the Ta River Metamorphic Suite and the Holly Corner Gneiss. The biotitic gneiss and granitoid rocks east of the Spotsylvania lineament in the Dillwyn area are considered to be coeval with the Po River Metamorphic Suite.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1146","usgsCitation":"Pavlides, L., 1980, Revised nomenclature and stratigraphic relationships of the Fredericksburg Complex and Quantico Formation of the Virginia Piedmont: U.S. Geological Survey Professional Paper 1146, Report: 29 p.; Plate; Companion Files, https://doi.org/10.3133/pp1146.","productDescription":"Report: 29 p.; Plate; Companion Files","costCenters":[],"links":[{"id":33590,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1146/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104558,"rank":700,"type":{"id":7,"text":"Companion Files"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4734.htm","linkFileType":{"id":5,"text":"html"},"description":"4734"},{"id":33591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1146/report-thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.6129150390625,\n 38.043765107439675\n ],\n [\n -76.92626953125,\n 38.043765107439675\n ],\n [\n -76.92626953125,\n 38.792626957868904\n ],\n [\n -77.6129150390625,\n 38.792626957868904\n ],\n [\n -77.6129150390625,\n 38.043765107439675\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ebc","contributors":{"authors":[{"text":"Pavlides, Louis","contributorId":79444,"corporation":false,"usgs":true,"family":"Pavlides","given":"Louis","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":152471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20088,"text":"ofr801190 - 1980 - Field data describing the movement and storage of sediment in the East Fork River, Wyoming: Part II, Bed elevations, 1979","interactions":[],"lastModifiedDate":"2022-06-08T15:52:44.5471","indexId":"ofr801190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1190","title":"Field data describing the movement and storage of sediment in the East Fork River, Wyoming: Part II, Bed elevations, 1979","docAbstract":"

At 39 cross sections in a 3.3-kilometer reach of East Fork River Wyo., bed elevations were measured daily during a month-long period that included the peak snowmelt runoff. Elevations were measured at less frequent intervals for a week before and several weeks after peak runoff. Considerable scour and fill was recorded at many of the cross sections.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801190","usgsCitation":"Meade, R.H., Myrick, R.M., and Emmett, W.W., 1980, Field data describing the movement and storage of sediment in the East Fork River, Wyoming: Part II, Bed elevations, 1979: U.S. Geological Survey Open-File Report 80-1190, v, 171 p., https://doi.org/10.3133/ofr801190.","productDescription":"v, 171 p.","costCenters":[],"links":[{"id":49639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1190/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1190/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"East Fork River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.74071502685547,\n 42.677135102723\n ],\n [\n -109.6281051635742,\n 42.677135102723\n ],\n [\n -109.6281051635742,\n 42.74575155146928\n ],\n [\n -109.74071502685547,\n 42.74575155146928\n ],\n [\n -109.74071502685547,\n 42.677135102723\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672bef","contributors":{"authors":[{"text":"Meade, Robert H. 0000-0002-4965-3040 rhmeade@usgs.gov","orcid":"https://orcid.org/0000-0002-4965-3040","contributorId":2744,"corporation":false,"usgs":true,"family":"Meade","given":"Robert","email":"rhmeade@usgs.gov","middleInitial":"H.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":182037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myrick, Robert M.","contributorId":24345,"corporation":false,"usgs":true,"family":"Myrick","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182038,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182039,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}