No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology of northern Arizona with notes on archaeology and paleoclimate: Part I — Regional studies","largerWorkSubtype":{"id":15,"text":"Monograph"},"conferenceTitle":"27th Annual Meeting of the Rocky Mountain Section","conferenceDate":"1974","conferenceLocation":"Flagstaff, Arizona, United States","language":"English","publisher":"Geological Society of America","usgsCitation":"Shoemaker, E.M., Squires, R.L., and Abrams, M.J., 1974, The Bright Angel and Mesa Butte fault systems of northern Arizona, chap. of Geology of northern Arizona with notes on archaeology and paleoclimate: Part I — Regional studies, p. 355-392.","productDescription":"38 p.","startPage":"355","endPage":"392","costCenters":[],"links":[{"id":394200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Bright Angel fault system, Mesa Butte fault system","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.08203125,\n 37.020098201368114\n ],\n [\n -114.08203125,\n 36.1822249804225\n ],\n [\n -114.2578125,\n 36.06686213257888\n ],\n [\n -113.97216796875,\n 36.049098959065645\n ],\n [\n -113.97216796875,\n 35.15584570226544\n ],\n [\n -109.610595703125,\n 35.15584570226544\n ],\n [\n -109.654541015625,\n 37.00255267215955\n ],\n [\n -114.08203125,\n 37.020098201368114\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Karlstrom, Thor Nels Vincent","contributorId":35183,"corporation":false,"usgs":true,"family":"Karlstrom","given":"Thor","email":"","middleInitial":"Nels Vincent","affiliations":[],"preferred":false,"id":830626,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Swann, Gordon Alfred","contributorId":51834,"corporation":false,"usgs":true,"family":"Swann","given":"Gordon","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":830627,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Eastwood, Raymond L.","contributorId":271059,"corporation":false,"usgs":false,"family":"Eastwood","given":"Raymond","email":"","middleInitial":"L.","affiliations":[{"id":12698,"text":"Northern Arizona University","active":true,"usgs":false}],"preferred":false,"id":830628,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":830623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Squires, R. L.","contributorId":270733,"corporation":false,"usgs":false,"family":"Squires","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":830624,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abrams, M. J.","contributorId":29859,"corporation":false,"usgs":true,"family":"Abrams","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":830625,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70232380,"text":"70232380 - 1974 - Hydrogeology of Antietam Creek basin","interactions":[],"lastModifiedDate":"2022-06-29T16:56:36.980516","indexId":"70232380","displayToPublicDate":"1974-03-01T11:49:43","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Hydrogeology of Antietam Creek basin","docAbstract":"The Antictam Creek basin in the Great Valley of Maryland and Pennsylvania is underlain almost entirely by intensely folded and faulted lower Paleozoic carbonate rocks. The ground-water discharge of the basin is about 85 percent of the total discharge, in contrast with less than 70 percent of the total discharge in two small basins underlain by igneous and mctamorphic rocks in the Maryland Piedmont. Large quantities of ground water are stored in a thick residual mantle, which overlies the carbonate rocks in the valley and adjacent rnetamorphic rocks in mountain areas on the east edge of the basin. Streams that flow off the mountain areas are major sources of recharge to the carbonate-rock aquifers. Several streams lose a large part of their flow within a mile after reaching the carbonate rocks in the valley, and a few flow directly into swallow holes (sinkholes). The low density of perennial streams in the basin is a result of subsurface drainage through solution cavities along joints, faults, and bedding in the carbonate rocks. The major orientations of straight stream reaches along Antietam Creek and the strikes of major joint sets in quarries are nearly coincident, suggesting that the stream network throughout the basin is joint controlled.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Nutter, L.J., 1974, Hydrogeology of Antietam Creek basin: Journal of Research of the U.S. Geological Survey, v. 2, no. 2, p. 249-252.","productDescription":"4 p.","startPage":"249","endPage":"252","costCenters":[],"links":[{"id":402700,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402699,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland, Pennsylvania","otherGeospatial":"Antietam Creek basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.69805908203125,\n 39.403305486149264\n ],\n [\n -77.54287719726562,\n 39.77265852521458\n ],\n [\n -77.59368896484375,\n 39.85915479295669\n ],\n [\n -77.70355224609375,\n 39.7240885773337\n ],\n [\n -77.79556274414061,\n 39.53158493558714\n ],\n [\n -77.7227783203125,\n 39.39693836884292\n ],\n [\n -77.69805908203125,\n 39.403305486149264\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nutter, Larry J.","contributorId":292648,"corporation":false,"usgs":false,"family":"Nutter","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":845388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70232379,"text":"70232379 - 1974 - WATEQ, a computer program for calculating chemical equilibria of natural waters","interactions":[],"lastModifiedDate":"2022-06-29T16:47:32.05893","indexId":"70232379","displayToPublicDate":"1974-03-01T11:43:01","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"WATEQ, a computer program for calculating chemical equilibria of natural waters","docAbstract":"The computer program, WATEQ, calculates the equilibrium distribution of inorganic aqueous species of major and important minor elements in natural waters using the chemical analysis and in situ measurements of temperature, pH, and redox potential. From this model, the states of reaction of the water with solid and gaseous phases are calculated. Thermodynamic stabilities of aqueous species, minerals, and gases have been selected from a careful consideration of all available experimental data. The program is written in PL-1 for IBM 360 computers.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Truesdell, A.H., and Jones, B.F., 1974, WATEQ, a computer program for calculating chemical equilibria of natural waters: Journal of Research of the U.S. Geological Survey, v. 2, no. 2, p. 233-248.","productDescription":"16 p.","startPage":"233","endPage":"248","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":402697,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402696,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Truesdell, A. H.","contributorId":140646,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.","email":"","middleInitial":"H.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":845386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Blair F. bfjones@usgs.gov","contributorId":2784,"corporation":false,"usgs":true,"family":"Jones","given":"Blair","email":"bfjones@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":845387,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70247408,"text":"70247408 - 1974 - Interpretation of aeromagnetic anomalies bearing on the origin of upper Chesapeake Bay and river course changes in the Central Atlantic Seaboard Region: Speculations","interactions":[],"lastModifiedDate":"2023-08-02T16:58:58.88565","indexId":"70247408","displayToPublicDate":"1974-02-01T11:55:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation of aeromagnetic anomalies bearing on the origin of upper Chesapeake Bay and river course changes in the Central Atlantic Seaboard Region: Speculations","docAbstract":"On an aeromagnetic map of the Chesapeake Bay area, the northeastern part of the bay coincides well with a deep, “flat” magnetic low, and the upper part of the Delmarva Peninsula east of the bay coincides with detailed magnetic highs; the two areas are separated by a steep, straight gradient that matches the eastern shore of the bay. On the basis of magnetic and geologic evidence, we interpret the Chesapeake Bay magnetic low as a buried Baltimore Gneiss dome, bounded on the southeast by a normal or reverse fault marked by the steep, straight gradient; mafic and ultramafic plutonic rocks probably underlie the southeast side of the fault zone. The flatness of the Chesapeake Bay magnetic low, as opposed to the detail of the anomalies on either side, however, suggests that an abnormal thickness of nonmagnetic sedimentary rocks also coincides with the low. This could reflect a buried Triassic basin or, more probably, a thickened section of Coastal Plain sedimentary rocks deposited in the fault-bounded basin. The present course of the upper part of Chesapeake Bay is probably inherited from the pre-Pleistocene course of the Susquehanna River, but the river's course may have been determined by the fault zone. Thus, this zone and similar en echelon fault zones along strike may explain the sudden change in course of major rivers in the central Atlantic Seaboard region.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1974)2<73:IOAABO>2.0.CO;2","usgsCitation":"Higgins, M.W., Zietz, I., and Fisher, G.W., 1974, Interpretation of aeromagnetic anomalies bearing on the origin of upper Chesapeake Bay and river course changes in the Central Atlantic Seaboard Region: Speculations: Geology, v. 2, no. 2, p. 73-76, https://doi.org/10.1130/0091-7613(1974)2<73:IOAABO>2.0.CO;2.","productDescription":"4 p.","startPage":"73","endPage":"76","costCenters":[],"links":[{"id":419514,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Unites States","state":"Delaware, Maryland, Pennsylvania, Virginia","otherGeospatial":"Chesapeake Bay area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -77.62208413380793,\n 41.66470473029685\n ],\n [\n -77.62208413380793,\n 36.64779764868278\n ],\n [\n -74.36581028054306,\n 36.64779764868278\n ],\n [\n -74.36581028054306,\n 41.66470473029685\n ],\n [\n -77.62208413380793,\n 41.66470473029685\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Higgins, Michael W.","contributorId":12459,"corporation":false,"usgs":true,"family":"Higgins","given":"Michael","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":879477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":879478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, George Wescott","contributorId":51356,"corporation":false,"usgs":true,"family":"Fisher","given":"George","email":"","middleInitial":"Wescott","affiliations":[],"preferred":false,"id":879479,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70247302,"text":"70247302 - 1974 - Configuration of Precambrian rocks in southeastern New York and adjacent New England from aeromagnetic data","interactions":[],"lastModifiedDate":"2023-07-27T14:20:04.839255","indexId":"70247302","displayToPublicDate":"1974-02-01T09:16:16","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Configuration of Precambrian rocks in southeastern New York and adjacent New England from aeromagnetic data","docAbstract":"Two aeromagnetic anomalies of regional extent outline two previously unknown buried masses of highly magnetic, probably Precambrian, rocks in southeastern New York and adjacent Vermont, Massachusetts, and Connecticut. The northern mass extends northeastward from Albany, New York, to Bennington, Vermont, where it appears to be buried beneath weakly magnetic Precambrian rocks of the Green Mountains. The southern mass extends north-northeastward from Beacon, New York, through Stissing Mountain, to Copake, New York, and appears to be the buried northeast extension of the Reading Prong. The shape of the Beacon-Copake magnetic anomaly indicates that the source is near the surface and has a sharp boundary, probably a fault, on its northwestern side; the shape also indicates that the source becomes deeply buried to the southeast and thus supports a parautochthonous interpretation for the northern part of the Reading Prong. In southwestern Massachusetts, the highly magnetic Beacon-Copake mass appears to be overstepped on the east by a buried slice of weakly magnetic Precambrian rocks which, in turn, is overstepped on the east by imbricate slices of weakly magnetic Precambrian rocks exposed along the western front of the Berkshire Highlands.
Precambrian rocks exposed in the Green Mountains, the Berkshire and Housatonic Highlands, the eastern part of the Hudson Highlands, and the Manhattan Prong have a remarkably lower amplitude magnetic pattern than those in the Adirondack Mountains and the Reading Prong. This difference in magnetic character appears to represent more than different thicknesses of Precambrian rocks and may reflect a different sequence of Precambrian rocks to the east, a lower grade of Precambrian metamorphism to the east, or possibly a reduction in magnetite content in the eastern Precambrian rocks because of Paleozoic metamorphism.
","language":"English","publisher":"Geological Society of America","usgsCitation":"Harwood, D.S., and Zietz, I., 1974, Configuration of Precambrian rocks in southeastern New York and adjacent New England from aeromagnetic data: GSA Bulletin, v. 85, no. 2, p. 181-188.","productDescription":"8 p.","startPage":"181","endPage":"188","costCenters":[],"links":[{"id":419368,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Massachusetts, New York, Vermont","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.05826097754819,\n 41.10698859225988\n ],\n [\n -73.26750552005615,\n 41.11339495665467\n ],\n [\n -73.1824780515086,\n 41.90926188486546\n ],\n [\n -72.63830225280499,\n 41.896605081089206\n ],\n [\n -72.595788518531,\n 42.907440228552105\n ],\n [\n -74.05826097754819,\n 42.994568812271524\n ],\n [\n -74.05826097754819,\n 41.10698859225988\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"85","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harwood, David S.","contributorId":48153,"corporation":false,"usgs":true,"family":"Harwood","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":879159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, Isidore","contributorId":90825,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":879160,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70246985,"text":"70246985 - 1974 - Prehnite- and pumpellyite-bearing mineral assemblages, west side of the Appalachian metamorphic belt, Pennsylvania to Newfoundland","interactions":[],"lastModifiedDate":"2023-07-20T16:08:01.969843","indexId":"70246985","displayToPublicDate":"1974-01-01T11:04:17","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Prehnite- and pumpellyite-bearing mineral assemblages, west side of the Appalachian metamorphic belt, Pennsylvania to Newfoundland","docAbstract":"Prehnite- and/or pumpellyite-bearing meta-igneous rocks are found on the west side of the Appalachian metamorphic belt (1) near Jonestown, south-eastern Pennsylvania; (2) on Rensselaer Plateau, eastern New York; (3) near Quebec City, Quebec; and (4) at Little Port, Humber Arm, western Newfoundland. The assemblages critical to determining the conditions of metamorphism are (1) chlorite-epidote-hematite-pumpellyite-prehnite; actinolite-chlorite-hematite-pumpellyite-stilpnomelane; (2) actinolite-chlorite-epidote-stilpnomelane; chlorite-epidote-pumpellyite-stilpnomelane; chlorite-epidote-hematite-pumpellyite; (3) chlorite-epidote-hematite-pumpellyite-stilpnomelane; chlorite-epidote-pumpellyite-prehnite; and (4) chlorite-epidote-prehnite; chlorite-prehnite-stilpnomelane; chlorite-epidote-pumpellyite-prehnite. One pumpellyite-bearing rock from western Newfoundland shows a later vein of analcime-calcite. All the assemblages also include quartz, sphene, calcite, K-mica, and albite.
Analysis of the mineral assemblages by the Schreinemakers method for the phases actinolite-chlorite-epidote-hematite-prehnite-pumpellyite-stilpnomelane shows that the different localities can be assigned different metamorphic grades. Though the detailed results of the Schreinemakers analysis depend on the assumed source of ferric iron in epidote, the major conclusions are not affected. The thermodynamic role of calcite is more problematic, but it appears that CO2 did not behave as a boundary-value component during metamorphism. If calcite is treated as an excess phase, the Schreinemakers bundle decomposes to a net in a multisystem. Plotted on such a net, the various localities again occupy different parts signifying different metamorphic grades.
The occurrence of pumpellyite-bearing assemblages on the west flank of the northern Appalachian metamorphic belt might suggest that these assemblages, contrary to the ideas of Miyashiro and of others, do not indicate high-pressure and low-temperature type of metamorphism. These assemblages, however, are compatible with an alternative interpretation as remnants of a high-pressure, low-temperature Taconic metamorphic regime, whose imprint within most of the Appalachian metamorphic belt has been obliterated by later events. Such a reconstruction is compatible with the suggestion that this zone, lying near the margin of the early Paleozoic craton, was an active subduction zone during the Taconic orogeny.
","language":"English","publisher":"Oxford Academic","doi":"10.1093/petrology/15.2.197","usgsCitation":"Zen, E., 1974, Prehnite- and pumpellyite-bearing mineral assemblages, west side of the Appalachian metamorphic belt, Pennsylvania to Newfoundland: Journal of Petrology, v. 15, no. 2, p. 197-242, https://doi.org/10.1093/petrology/15.2.197.","productDescription":"46 p.","startPage":"197","endPage":"242","costCenters":[],"links":[{"id":419189,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Appalachian metamorphic belt","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.47423023405047,\n 39.69308703725781\n ],\n [\n -67.6920197700901,\n 44.79789616439686\n ],\n [\n -64.206384066307,\n 45.7962470849381\n ],\n [\n -53.4232657940356,\n 48.112138178866275\n ],\n [\n -55.99805109429077,\n 53.54319967895097\n ],\n [\n -65.79365836535626,\n 50.731908095598186\n ],\n [\n -70.79322235691728,\n 46.06624520636481\n ],\n [\n -80.44907525946763,\n 39.58813057959887\n ],\n [\n -76.47423023405047,\n 39.69308703725781\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zen, E-an","contributorId":38564,"corporation":false,"usgs":true,"family":"Zen","given":"E-an","affiliations":[],"preferred":false,"id":878471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162482,"text":"70162482 - 1974 - Earthquake history of Nevada","interactions":[],"lastModifiedDate":"2019-11-13T15:02:00","indexId":"70162482","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake history of Nevada","docAbstract":"Since 1852, more than 30 shocks of intensity VI or greater (Modified Mercalli scale) have occurred in western Nevada. At least three of these were classified as intensity X. In addition, seven earthquakes (intensity VI or greater) were centered in the eastern part of the State. Almost 2,000 other shocks have been cataloged in the nearly 125-year period of historical records. Thus, Nevada ranks among the most seismically active States.
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The densely settled Wasatch Front area has about 900,000 people, 80 percent of Utah's total population. This population is centered around Salt Lake City, a rapidly growing industrial and tourist center.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., 1974, Seismicity and earthquake hazards of the Wasatch Front, Utah: Earthquake Information Bulletin (USGS), v. 6, no. 4, p. 12-17.","productDescription":"6 p.","startPage":"12","endPage":"17","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Front","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.9451904296875,\n 39.63530729658601\n ],\n [\n -111.796875,\n 39.64799732373418\n ],\n [\n -111.7913818359375,\n 39.825413103424786\n ],\n [\n -111.7529296875,\n 40.01078714046552\n ],\n [\n -111.566162109375,\n 40.10328591293442\n ],\n [\n -111.676025390625,\n 40.333983227838104\n ],\n [\n -111.785888671875,\n 40.49291502689579\n ],\n [\n -111.829833984375,\n 40.826280356677124\n ],\n [\n -111.8792724609375,\n 41.17451935556443\n ],\n [\n -112.0001220703125,\n 41.35207214451295\n ],\n [\n -112.0660400390625,\n 41.6770148220322\n ],\n [\n -112.09899902343749,\n 41.75082413553287\n ],\n [\n -112.1759033203125,\n 42.00032514831621\n ],\n [\n -112.2747802734375,\n 42.00032514831621\n ],\n [\n -112.2308349609375,\n 41.49623534616764\n ],\n [\n -112.236328125,\n 41.19105625669688\n ],\n [\n -111.983642578125,\n 40.979898069620155\n ],\n [\n -112.1319580078125,\n 40.81380923056961\n ],\n [\n -112.03857421875,\n 40.48455955508278\n ],\n [\n -111.96716308593749,\n 39.787433886224406\n ],\n [\n -111.9451904296875,\n 39.63530729658601\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c84acce4b0b3c9ae3810a1","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":620950,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70230463,"text":"70230463 - 1973 - Salinity studies in East Glades Agricultural Area, southeastern Dade County, Florida","interactions":[],"lastModifiedDate":"2025-04-25T15:26:51.860646","indexId":"70230463","displayToPublicDate":"2022-04-13T08:43:50","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"FL 73-005","displayTitle":"Salinity Studies in East Glades Agricultural Area, Southeastern Dade County, Florida","title":"Salinity studies in East Glades Agricultural Area, southeastern Dade County, Florida","docAbstract":"Salinity studies in East Glades Agricultural Area, southeastern Dade County, Florida
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70230463","collaboration":"Prepared in cooperation with Central and Southern Florida Flood Control District","usgsCitation":"Hull, J., and Meyer, F., 1973, Salinity studies in East Glades Agricultural Area, southeastern Dade County, Florida: Open-File Report FL 73-005, 84 p., https://doi.org/10.3133/70230463.","productDescription":"84 p.","numberOfPages":"84","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":398639,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70230463/ofr-fl-73005.pdf","text":"Report","size":"2.21 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR FL 73-005"},{"id":398638,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70230463/coverthb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.57061091574482,\n 25.56455300026859\n ],\n [\n -80.57061091574482,\n 25.295388017649827\n ],\n [\n -80.28780387668424,\n 25.295388017649827\n ],\n [\n -80.28780387668424,\n 25.56455300026859\n ],\n [\n -80.57061091574482,\n 25.56455300026859\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Deep-well injection has been selected by the Dade County Water and Sewer Authority as a means of disposing treated waste water in southeast Dade County. Preliminary plans call for the construction of a county-owned sanitary sewage treatment plant and several 3,000-foot deep injection wells at 1,000-foot intervals on Levee 31E. As a first stage, drilling of seven wells, capable of accepting, in the aggregate, 30 mgd (million gallons per day) of treated liquid waste, is planned. The locations of the proposed sites (fig. 1) were selected by the consultants for the Authority.
A reconnaissance was made in the vicinity of the proposed well sites to determine the chloride content of surface and ground water because this information is needed to formulate plans for the safe disposal of salt water during drilling and testing of the injection wells. The reconnaissance was part of a cooperative program with the Dade County Water and Sewer Authority to investigate the hydrologic effects of injecting treated waste water into a deep-saline aquifer.
The area of investigation is near Cutler Ridge in southeast Dade County. It occupies about 51/2 square miles bounded on the east by S.W. 77th Avenue extended, on the west by S.W. 97th Avenue, on the south by Coconut Palm Drive, and on the north by Old Cutler Road (fig. 1). The area for the investigation was selected by the Authority and their consultants.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr7365","collaboration":"Prepared in cooperation with the Dade County Water and Sewer Authority","usgsCitation":"Earle, J., and Meyer, F., 1973, Reconnaissance of the water resources in the vicinity of proposed deep-well injection sites in southeast Dade County, Florida: U.S. Geological Survey Open-File Report 73-65, 20 p., https://doi.org/10.3133/ofr7365.","productDescription":"20 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":484522,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0065/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0065/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Dade 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\"}}]}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
VERIFICATIONS of tectonic concepts1 concerning seafloor spreading are emerging in a manner that has direct bearing on earthquake prediction. Although the gross pattern of worldwide seismicity contributed to the formulation of the plate tectonic hypothesis, it is the space-time characteristics of this seismicity that may contribute more toward understanding the kinematics and dynamics of the driving mechanism long speculated to originate in the mantle. If the lithosphere is composed of plates that move essentially as rigid bodies, then there should be seismic edge effects associated with this movement. It is these interplate effects, especially seismic migration patterns, that we discuss here. The unidirectional propagation at constant velocity (80 km yr−1 east to west) for earthquakes (M≥7.2) on the Antblian fault for the period 1939 to 1956 (ref. 2) is one of the earliest observations of such a phenomenon. Similar studies3,4 of the Alaska Aleutian seismic zone and certain regions of the west coast of South America suggest unidirectional and recurring migrations of earthquakes (M≥7.7) occur in these areas. Between these two regions along the great transform faults of the west coast of North America, there is some evidence5 for unidirectional, constant velocity and recurrent migration of great earthquakes. The small population of earthquakes (M>7.2) in Savage's investigation5 indicates a large spatial gap along the San Andreas system in central California from 1830 to 1970. Previous work on the seismicity of this gap in central California indicates that the recurrence curves remain relatively constant, independent of large earthquakes, for periods up to a century6. Recurrence intervals for earthquakes along the San Andreas Fault have been calculated empirically by Wallace7 on the basis of geological evidence, surface measurements and assumptions restricted to the surficial seismic layer. Here we examine the evidence for recurrence of seismic migrations along the San Andreas fault system of central California for earthquakes of magnitude M≥5.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i844G","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Map showing potential for copper deposits in the eastern three-quarters of the Nogales 2° quadrangle, Tucson area, Arizona: U.S. Geological Survey IMAP 844, 1 Plate: 39.61 × 28.47 inches, https://doi.org/10.3133/i844G.","productDescription":"1 Plate: 39.61 × 28.47 inches","costCenters":[],"links":[{"id":391244,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9679.htm"},{"id":255514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0844g/report-thumb.jpg"},{"id":255513,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0844g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255512,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0844g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona","otherGeospatial":"Nogales 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,31.25 ], [ -112,32 ], [ -110,32 ], [ -110,31.25 ], [ -112,31.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db65972a","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":534116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2406,"text":"wsp2006 - 1973 - The Pine-Popple River basin — Hydrology of a wild river area, northeastern Wisconsin","interactions":[],"lastModifiedDate":"2022-12-01T19:23:30.261504","indexId":"wsp2006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2006","title":"The Pine-Popple River basin — Hydrology of a wild river area, northeastern Wisconsin","docAbstract":"The Pine and Popple Rivers, virtually unaltered by man, flow through a semiprimitive area of forests, lakes, and glacial hills. White-water streams, natural lakes, fish and animal life, and abundant vegetation contribute to the unique recreational and aesthetic characteristics of the area. Resource planning or development should recognize the interrelationships within the hydrologic system and the possible effects of water and land-use changes upon the wild nature of the area. The basin covers about 563 square miles in northeastern Wisconsin. Swamps and wetlands cover nearly 110 square miles, and the 70 lakes cover about 11 square miles. The undulating topography is formed by glacial deposits overlying an irregular, resistant surface of bedrock. An annual average of 30 inches of precipitation, highest from late spring to early autumn, falls on the basin. Of this amount, evapotranspiration, highest in mid summer and late summer, averages 19 inches; the remaining 11 inches is runoff, which is highest in spring and early summer. Ground water from the glacial drift is the source of water for the minor withdrawal use in the basin. Ground-water movement is to streams and lakes and regionally follows the slope of topography and the bedrock surface, which is generally west to east. Ground water is of good quality, although locally high in iron. The major uses of water are for recreation and power generation. Domestic use is slight. No water is withdrawn from lakes or streams, and no sewage or industrial wastes are added to lakes or streams. Most of the flow of the Pine River is used for power generation. The main stems of the Pine and Popple Rivers contain 114 canoeable miles, of which 95 percent is without such major obstructions as falls or large rapids. In general streams support cold-water fish, and lakes support warm-water fish. Trout is the principal stream and game fish in the basin. The basin has no significant water problems. Future development between the Pine River power plant and the mouth of the Pine River should have little effect on the western two-thirds of the basin, already largely protected by public ownership or development planning agreements.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2006","usgsCitation":"Oakes, E.L., Field, S.J., and Seeger, L.P., 1973, The Pine-Popple River basin — Hydrology of a wild river area, northeastern Wisconsin: U.S. Geological Survey Water Supply Paper 2006, Report: iv, 57 p.; 2 Plates: 33.50 x 29.50 inches and 31.50 x 31.00 inches, https://doi.org/10.3133/wsp2006.","productDescription":"Report: iv, 57 p.; 2 Plates: 33.50 x 29.50 inches and 31.50 x 31.00 inches","numberOfPages":"64","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":28408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28407,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2006/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28406,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2006/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2006/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Florence County, Forest County, Marinette County","otherGeospatial":"Pine River, Popple River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.92951965332031,\n 45.874234183868346\n ],\n [\n -88.92951965332031,\n 46.08418564215268\n ],\n [\n -88.626708984375,\n 46.08418564215268\n ],\n [\n -88.626708984375,\n 45.874234183868346\n ],\n [\n -88.92951965332031,\n 45.874234183868346\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae0d","contributors":{"authors":[{"text":"Oakes, Edward L.","contributorId":79517,"corporation":false,"usgs":true,"family":"Oakes","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Field, Stephen J.","contributorId":53800,"corporation":false,"usgs":true,"family":"Field","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seeger, Lawrence P.","contributorId":17090,"corporation":false,"usgs":true,"family":"Seeger","given":"Lawrence","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":145150,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67404,"text":"i591O - 1973 - Map showing scenic features and recreation facilities in the Salina quadrangle, Utah","interactions":[{"subject":{"id":67404,"text":"i591O - 1973 - Map showing scenic features and recreation facilities in the Salina quadrangle, Utah","indexId":"i591O","publicationYear":"1973","noYear":false,"chapter":"O","title":"Map showing scenic features and recreation facilities in the Salina quadrangle, Utah"},"predicate":"IS_PART_OF","object":{"id":67401,"text":"i591 - 1971 - Geology, structure, and uranium deposits of the Salina quadrangle, Utah","indexId":"i591","publicationYear":"1971","noYear":false,"title":"Geology, structure, and uranium deposits of the Salina quadrangle, Utah"},"id":1}],"isPartOf":{"id":67401,"text":"i591 - 1971 - Geology, structure, and uranium deposits of the Salina quadrangle, Utah","indexId":"i591","publicationYear":"1971","noYear":false,"title":"Geology, structure, and uranium deposits of the Salina quadrangle, Utah"},"lastModifiedDate":"2025-08-04T21:27:53.586171","indexId":"i591O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"591","chapter":"O","title":"Map showing scenic features and recreation facilities in the Salina quadrangle, Utah","docAbstract":"This map is intended as a guide for those who enjoy outdoor recreation in magnificent scenic settings.
The Salina quadrangle lies in the heart of the Colorado Plateau, a sparsely populated land of unique and outstanding scenic beauty. The eastern half of the quadrangle is a great desert, partly blanketed by sand dunes, but mostly an area of badlands multicolored cliffs and benches of virtually barren rock, and deeply incised canyons. In the west half of the quadrangle, rugged tree-covered foothills flank high forested plateaus rimmed by cliffs. On these High Plateaus, dense coniferous forest is interspersed with wide grassy parks, grazed in summer by sheep and cattle. Valleys between the plateaus contain irrigated crop lands.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology, structure, and uranium deposits of the Salina quadrangle, Utah","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i591O","usgsCitation":"Williams, P., and Covington, H., 1973, Map showing scenic features and recreation facilities in the Salina quadrangle, Utah: U.S. Geological Survey IMAP 591, 1 Plate: 39.86 x 27.64 inches, https://doi.org/10.3133/i591O.","productDescription":"1 Plate: 39.86 x 27.64 inches","costCenters":[],"links":[{"id":493516,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9388.htm","linkFileType":{"id":5,"text":"html"}},{"id":256595,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0591o/report-thumb.jpg"},{"id":256593,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0591o/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256594,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0591o/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Salina quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,38 ], [ -112,39 ], [ -110,39 ], [ -110,38 ], [ -112,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a32ea","contributors":{"authors":[{"text":"Williams, Paul L.","contributorId":181839,"corporation":false,"usgs":false,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":276134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Covington, Harry R.","contributorId":101309,"corporation":false,"usgs":true,"family":"Covington","given":"Harry R.","affiliations":[],"preferred":false,"id":276135,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48166,"text":"ofr73161 - 1973 - Hydrology of the uppermost Cretaceous and the lowermost Paleocene rocks in the Hilight oil field, Campbell County, Wyoming","interactions":[],"lastModifiedDate":"2022-10-04T18:21:45.828655","indexId":"ofr73161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-161","title":"Hydrology of the uppermost Cretaceous and the lowermost Paleocene rocks in the Hilight oil field, Campbell County, Wyoming","docAbstract":"The lithologic equivalents of the Fox Hills Sandstone, Lance Formation, and the Tullock member of the Fort Union Formation, as mapped on the east side of the Powder River Basin, can be recognized throughout the basin; however, the formations are in hydraulic connection and cannot be treated as separate aquifers. \r\n\r\nRecharge to the Lance-Fox Hills aquifer in the Hilight oil field is largely by vertical movement; there is no recharge from the Lance and Fox Hills outcrops on the east side of the basin to the formations in the Hilight area. \r\n\r\nAt the and of the central Hilight water-flood project, the maximum possible drawdown resulting from the pumping of any one well at a distance of l0 miles from the pumped well, would be about 15 feet, if the projected pumping were evenly distributed among the project wells. \r\n\r\nWithin a few years after pumping has ceased, water in the project wells will approach the levels present before pumping began. The only irreversible effect of pumping will be the compaction of shale, with attendant subsidence, because the water derived from the shale probably will not be replaced.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73161","usgsCitation":"Lowry, M.E., 1973, Hydrology of the uppermost Cretaceous and the lowermost Paleocene rocks in the Hilight oil field, Campbell County, Wyoming: U.S. Geological Survey Open-File Report 73-161, Report: 60 p.; 5 Plates: 23.44 × 54.03 inches, https://doi.org/10.3133/ofr73161.","productDescription":"Report: 60 p.; 5 Plates: 23.44 × 54.03 inches","costCenters":[],"links":[{"id":84897,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0161/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84896,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0161/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84895,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0161/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84894,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0161/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84893,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0161/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84892,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0161/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0161/report-thumb.jpg"},{"id":110289,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51414.htm","linkFileType":{"id":5,"text":"html"},"description":"51414"}],"country":"United States","state":"Wyoming","county":"Campbell County","otherGeospatial":"Hilight oil field","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.5,\n 43.7\n ],\n [\n -105.2,\n 43.7\n ],\n [\n -105.2,\n 44\n ],\n [\n -105.5,\n 44\n ],\n [\n -105.5,\n 43.7\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc777","contributors":{"authors":[{"text":"Lowry, Marlin E.","contributorId":52552,"corporation":false,"usgs":true,"family":"Lowry","given":"Marlin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":236902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":204,"text":"wsp2092 - 1973 - Quality of surface waters of the United States, 1968, Part 2, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp2092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2092","title":"Quality of surface waters of the United States, 1968, Part 2, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp2092","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Quality of surface waters of the United States, 1968, Part 2, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 2092, x, 373 p. ;23 cm., https://doi.org/10.3133/wsp2092.","productDescription":"x, 373 p. ;23 cm.","costCenters":[],"links":[{"id":135999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2092/report-thumb.jpg"},{"id":24815,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651958","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":527233,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68651,"text":"ha437 - 1973 - Water resources of the Kettle River watershed, east-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:56:33","indexId":"ha437","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"437","title":"Water resources of the Kettle River watershed, east-central Minnesota","docAbstract":"The topography of the Kettle River watershed is formed primarily by glacial deposits that mantle the bedrock.
\nThe glacial deposits are generally less than 100 feet thick. Bedrock consists of several types and occasionally crops out at land surface. Topography ranges from gently rolling to steeply undulating. About 1,060 square miles is drained by the Kettle River and its tributaries, and about 510 square miles by smaller streams that are direct tributaries to the St. Croix River. Peat and swamp areas are common, particularly in the eastern part of the area. Most of the watershed is forested, mainly with hardwoods.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha437","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soil, and Minerals","usgsCitation":"Helgesen, J.O., Lindholm, G.F., Broussard, W., and Ericson, D., 1973, Water resources of the Kettle River watershed, east-central Minnesota: U.S. Geological Survey Hydrologic Atlas 437, 4 Plates: 47.0 X 36.5 inches or smaller, https://doi.org/10.3133/ha437.","productDescription":"4 Plates: 47.0 X 36.5 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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O.","contributorId":101630,"corporation":false,"usgs":true,"family":"Helgesen","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":278638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindholm, G. F.","contributorId":88763,"corporation":false,"usgs":true,"family":"Lindholm","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":628954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broussard, W.L.","contributorId":35334,"corporation":false,"usgs":true,"family":"Broussard","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":628955,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ericson, D.W.","contributorId":80295,"corporation":false,"usgs":true,"family":"Ericson","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":628956,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":66658,"text":"i766H - 1973 - Map showing thickness of saturated Quaternary deposits, Sugar House quadrangle, Salt Lake County, Utah, February 1972","interactions":[],"lastModifiedDate":"2025-08-05T18:46:48.121927","indexId":"i766H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"766","chapter":"H","title":"Map showing thickness of saturated Quaternary deposits, Sugar House quadrangle, Salt Lake County, Utah, February 1972","docAbstract":"Saturated Quaternary deposits in the Sugar Horse quadrangle supply significant quantities of water to wells from which water is withdrawn for domestic, municipal, industrial, and irrigation uses. The deposits consist of clay, silt, sand, and gravel; individual beds range from a few inches to several tens of feet thick. The principal aquifer, which is almost completely within the Quaternary deposits, supplied about 4 percent, or 9,000 acre-feet, of the municipal and industrial water used annually in Salt Lake County during 1964-68.
As a general rule, more water is stored and more water will be yielded to a well where aquifers are thicker. This map can be used as a general guide to those areas where greatest amounts of water are stored in the aquifer, and where yields to wells may be greater. Local variations in the ability of saturated deposits to transmit water can alter the general relationship between aquifer thickness and yield of wells.
The thickness of saturated Quaternary deposits within the area of the Sugar Horse quadrangle ranges from zero to about 650 feet, as shown on the map. The thickest section of these deposits is near the southwestern corner of the quadrangle, and the thinnest section is along the mountain front adjacent to the approximate eastern limit of saturated Quaternary deposits.
The thickness of saturated Quaternary deposits shown on this map is based on drillers’ logs for 55 deep wells (which show the thickness of the Quaternary deposits) and on water-level measurements made in February 1972 in wells in unconfined shallow aquifers.
Reports in the following list of selected references contain other information about the saturated Quaternary deposits in this and adjacent parts of Jordan Valley, Utah. The basic-data reports and releases contain well logs, water-level measurements, and other types of basic ground-water data. The interpretive repots contain discussions of the occurrence of ground water, tests to determine hydraulic properties of the aquifer, and related information. Ground-water terms used in this report have been defined by Lohman and others (1972).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i766H","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., 1973, Map showing thickness of saturated Quaternary deposits, Sugar House quadrangle, Salt Lake County, Utah, February 1972: U.S. Geological Survey IMAP 766, 1 Plate: 34.26 x 27.60 inches; Cover: 9.18 x 11.77 inches, https://doi.org/10.3133/i766H.","productDescription":"1 Plate: 34.26 x 27.60 inches; Cover: 9.18 x 11.77 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":493588,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9527.htm","linkFileType":{"id":5,"text":"html"}},{"id":256023,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0766h/plate-1.pdf","text":"Map I-766-H","linkFileType":{"id":1,"text":"pdf"}},{"id":256024,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0766h/report.pdf","text":"Folio Cover","linkFileType":{"id":1,"text":"pdf"}},{"id":256025,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0766h/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Utah","county":"Salt Lake County","otherGeospatial":"Sugar House quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.75,\n 40.625\n ],\n [\n -111.75,\n 40.75\n ],\n [\n -111.875,\n 40.75\n ],\n [\n -111.875,\n 40.625\n ],\n [\n -111.75,\n 40.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a241b","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":274868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24797,"text":"ofr73358 - 1973 - Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"ofr73358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-358","title":"Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California","docAbstract":"This is a study of the feasibility of recharging, in the Waterman Canyon-East Twin Creek area, imported water from northern California by way of the State Water Project beginning in 1972. \r\n\r\nThe feasibility of recharging 30,000 acre-feet of water a year in the Waterman Canyon-East Twin Creek area will depend on the effectiveness of fault K as a barrier to ground-water movement near the land surface. The results of test drilling and an infiltration test indicate that the subsurface material at the spreading grounds is permeable enough to allow recharged water to percolate to the water table. The data indicate that fault K extends into the Waterman Canyon-East Twin Creek area and may impede the lateral movement of recharged water. Fault K has no known surface expression and therefore probably does not affect the highly permeable younger alluvium. If that is so, fault K will be less effective as a barrier to ground-water movement as the recharge mound rises. Monitoring of the observation wells near the spreading grounds as the planned recharge operation proceeds should provide data about the hydrologic effects of fault K near the land surface.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr73358","issn":"0094-9140","usgsCitation":"Warner, J.W., and Moreland, J.A., 1973, Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California: U.S. Geological Survey Open-File Report 73-358, iv, 44 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr73358.","productDescription":"iv, 44 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":157510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0358/report-thumb.jpg"},{"id":53810,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0358/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c47","contributors":{"authors":[{"text":"Warner, J. W.","contributorId":42996,"corporation":false,"usgs":true,"family":"Warner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":192582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moreland, J. A.","contributorId":71994,"corporation":false,"usgs":true,"family":"Moreland","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}