The Hawaiian Ridge and Emperor Seamounts appear to form a single chain of tholeiitic shield volcanoes that erupted sequentially on the sea floor of the central Pacific Ocean during Tertiary and Quaternary time. The chain cuts obliquely across the older Cretaceous structural patterns of that sea floor. While the pattern of the chain as a whole is linear, the individual volcanoes lie on short, sigmoidal, en echelon loci that are subparallel with respect to each other and that may represent extensional features in the crust and upper mantle. In general, the order of eurption progressed from northwest to southeaśt along the chain, but the rate of progression of volcanism along individual loci is nonlinear where best studied in the southeastern part of the chain. Furthermore, simultaneous eruptions appear to have occurred within a distance along the chain of about 200 to 400 km. The available data are consistent with a genesis related to the motion of the Pacific crust over a melting spot in the mantle. This melting spot, which may be due to either excess heat or pressure release, appears to have a diameter of about 300 km and is presently centered slightly north of the island of Hawaii. We concur with the idea that the bend in the Hawaiian-Emperor chain probably reflects a significant change in the motion of the Pacific plate. Our best estimate of the age of the Hawaiian-Emperor bend, based on the existing radiometric data, is 24.6 ± 2.5 m.y., which correlates with a time of increased tectonic activity in the western Pacific island arcs and along the northern and eastern boundaries of the Pacific plate. The vector change in the motion of the Pacific plate (with respect to the melting spot) that is required to produce the bend is about 12 cm/yr in a west-southwest-ward direction. © 1972, The Geological Society of America, Inc.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[601:HCAIRT]2.0.CO;2","issn":"00167606","usgsCitation":"Jackson, E., Silver, E.A., and Dalrymple, G.B., 1972, Hawaiian-emperor chain and its relation to cenozoic circumpacific tectonics: Geological Society of America Bulletin, v. 83, no. 3, p. 601-618, https://doi.org/10.1130/0016-7606(1972)83[601:HCAIRT]2.0.CO;2.","productDescription":"18 p. 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\"}}]}","volume":"83","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jackson, E.D.","contributorId":99524,"corporation":false,"usgs":true,"family":"Jackson","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":775574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silver, E. A.","contributorId":18491,"corporation":false,"usgs":true,"family":"Silver","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":775575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":775576,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70197654,"text":"70197654 - 1972 - Paleomagnetic correlations and Potassium-Argon dating of Middle Tertiary ash-flow sheets in the eastern Great Basin, Nevada and Utah","interactions":[],"lastModifiedDate":"2018-06-15T11:38:42","indexId":"70197654","displayToPublicDate":"1972-12-31T00:00:00","publicationYear":"1972","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":"Paleomagnetic correlations and Potassium-Argon dating of Middle Tertiary ash-flow sheets in the eastern Great Basin, Nevada and Utah","docAbstract":"Directions of natural remanent magnetization are used to identify and correlate individual cooling units in the middle Tertiary ash-flow province in central and eastern Nevada and western Utah. Potassium-argon dating indicates that the minimum time between eruptions of individual but genetically related ash-flow cooling units is on the order of 0.8 m.y. As this interval is long in comparison with the secular variation of the direction of the geomagnetic field, in a given volcanic province the direction of natural thermoremanent magnetization is a unique characteristic of each cooling unit. Ash-flow sheets investigated include the Stone Cabin Formation, the tuff of Pancake Summit, the Windous Butte Formation, the Needles Range Formation, the Bates Mountain Tuff, and the tuff of Clipper Gap, of Oliogcene to early Miocene age. The original areas of individual ash-flow cooling units are as great as 8,000 km2; the volumes, 1,300 km3. The paleomagnetic correlations, made over distances up to 200 km, confirm most of the previously made lithologic correlations and allow more accurate delineation of single cooling units. These correlations are particularly useful in those parts of the Basin and Range province where the Tertiary stratigraphic section consists mainly of ash-flow sheets, and the outcrops are confined to mountain ranges that are separated by alluvium-filled valleys.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[1619:PCAPDO]2.0.CO;2","usgsCitation":"Grommé, C., McKee, E., and Blake, M.C., 1972, Paleomagnetic correlations and Potassium-Argon dating of Middle Tertiary ash-flow sheets in the eastern Great Basin, Nevada and Utah: GSA Bulletin, v. 83, no. 6, p. 1619-1638, https://doi.org/10.1130/0016-7606(1972)83[1619:PCAPDO]2.0.CO;2.","productDescription":"20 p.","startPage":"1619","endPage":"1638","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada, Utah","volume":"83","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grommé, C. S.","contributorId":38558,"corporation":false,"usgs":true,"family":"Grommé","given":"C. S.","affiliations":[],"preferred":false,"id":738084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, E.H.","contributorId":20736,"corporation":false,"usgs":true,"family":"McKee","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":738085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blake, M. Clark Jr.","contributorId":56675,"corporation":false,"usgs":true,"family":"Blake","given":"M.","suffix":"Jr.","email":"","middleInitial":"Clark","affiliations":[],"preferred":false,"id":738086,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5223308,"text":"5223308 - 1972 - Eastward migration of blue-winged teal","interactions":[],"lastModifiedDate":"2025-02-21T16:54:53.760943","indexId":"5223308","displayToPublicDate":"1972-10-06T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Eastward migration of blue-winged teal","docAbstract":"Of 3,789 recoveries of blue-winged teal (Anas discors) banded prior to the hunting season in the prairie pothole region, 183 (4.8 percent) were recovered, due east in New England, Ontario, Quebec, and the Maritime Provinces during the subsequent hunting season. Of 19 recoveries looked at in detail, all were banded as either hatching-year (flying young) or local (flightless young) birds. A blue-winged teal banded in Minnesota in September was retrapped in October in South Carolina, before being shot later that month in Colombia, South America.
","language":"English","publisher":"Wiley","doi":"10.2307/3799262","usgsCitation":"Sharp, B., 1972, Eastward migration of blue-winged teal: Journal of Wildlife Management, v. 36, no. 4, p. 1273-1277, https://doi.org/10.2307/3799262.","productDescription":"5 p.","startPage":"1273","endPage":"1277","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199687,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"North Dakota, Minnesota","otherGeospatial":"Alberta, Saskatchewan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.1520732984464,\n 59.92509917759563\n ],\n [\n -120.1690210759753,\n 53.861418873618376\n ],\n [\n -114.30334555422223,\n 49.729112484974586\n ],\n [\n -103.89236975427357,\n 45.747832694335045\n ],\n [\n -97.466221646018,\n 45.75362612194698\n ],\n [\n -96.3112252567795,\n 43.66239757659807\n ],\n [\n -90.47288416474126,\n 43.623425078704315\n ],\n [\n -92.64696983604352,\n 46.08348138659872\n ],\n [\n -89.99666740104907,\n 47.88552887744924\n ],\n [\n -94.73762141579002,\n 49.07380418744488\n ],\n [\n -101.43958666144323,\n 49.24157507682183\n ],\n [\n -102.70581818256466,\n 59.65559957942301\n ],\n [\n -120.1520732984464,\n 59.92509917759563\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f15","contributors":{"authors":[{"text":"Sharp, Brian","contributorId":34606,"corporation":false,"usgs":true,"family":"Sharp","given":"Brian","affiliations":[],"preferred":false,"id":338376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70197181,"text":"70197181 - 1972 - Paleomagnetism and potassium-argon ages of the Sonoma Volcanics, California","interactions":[],"lastModifiedDate":"2018-05-18T16:05:52","indexId":"70197181","displayToPublicDate":"1972-07-01T00:00:00","publicationYear":"1972","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":"Paleomagnetism and potassium-argon ages of the Sonoma Volcanics, California","docAbstract":"Paleomagnetic data and potassium-argon ages indicate that the Sonoma Volcanics was erupted during the Pliocene Gilbert reversed and Gauss normal polarity epochs. The Gilbert reversed epoch is represented in the Howell Mountains east of Napa and east of St. Helena, in the mountains immediately east of the Valley of the Moon, and on the hill just north of Santa Rosa. The Gauss normal epoch is represented by the rocks from Mount St. Helena and possibly by the flows from the upper part of Sonoma Mountain and the rhyolite flows north of Sonoma. The age of the volcanic rocks ranges from 5.3 m.y. to about 2.9 m.y. Volcanic rocks approximately 11.8 m.y. old occur at Burdell Mountain northwest of Novato. This volcanic sequence is probably part of the Tolay Volcanics of the Petaluma area.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[2063:PAPAOT]2.0.CO;2","usgsCitation":"Mankinen, E.A., 1972, Paleomagnetism and potassium-argon ages of the Sonoma Volcanics, California: GSA Bulletin, v. 83, no. 7, p. 2063-2072, https://doi.org/10.1130/0016-7606(1972)83[2063:PAPAOT]2.0.CO;2.","productDescription":"10 p.","startPage":"2063","endPage":"2072","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354349,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sonoma Volcanics","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122,\n 38.0833\n ],\n [\n -122.5,\n 38.0833\n ],\n [\n -122.5,\n 38.75\n ],\n [\n -122,\n 38.75\n ],\n [\n -122,\n 38.0833\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"83","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff592be4b0da30c1bfdd35","contributors":{"authors":[{"text":"Mankinen, Edward A. 0000-0001-7496-2681 emank@usgs.gov","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":1054,"corporation":false,"usgs":true,"family":"Mankinen","given":"Edward","email":"emank@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":735926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010193,"text":"70010193 - 1972 - Deuterium content of snow as an index to winter climate in the Sierra Nevada area","interactions":[],"lastModifiedDate":"2026-01-23T22:24:55.924746","indexId":"70010193","displayToPublicDate":"1972-05-19T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Deuterium content of snow as an index to winter climate in the Sierra Nevada area","docAbstract":"The winter of 1968-69 produced two to three times the amount of precipitation in the Sierra Nevada area, California and Nevada, as the winter of 1969-70. The deuterium content in snow cores collected at the end of each winter at the same sites, which represents the total snowfall of each interval, shows a depletion in 1968-69 of approximately 20 per mil. The higher snowfall in 1968-69 and the depletion of deuterium can be explained by an uncommonly strong westward flow of cold air over and down the western slopes of the Sierras, which interacted with an eastward flow of moist Pacific air that overrode and mixed with the cold air; this resulted in precipitation that occurred in greater than normal amounts and at a lower than normal temperature. Pluvial periods of the Pleistocene may have had the same shift in air-mass trajectory as the wet 1968-69 year. Snow cores collected in the normal 1970-71 winter have deuterium concentrations that resemble those of the normal 1969-70 winter. Small and nonsystematic differences in samples from these two normal winters are due to variations in climatic character as well as to factors inherent in the sampling sites.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.176.4036.790","issn":"00368075","usgsCitation":"Friedman, I., and Smith, G., 1972, Deuterium content of snow as an index to winter climate in the Sierra Nevada area: Science, v. 176, no. 4036, p. 790-793, https://doi.org/10.1126/science.176.4036.790.","productDescription":"4 p.","startPage":"790","endPage":"793","costCenters":[],"links":[{"id":218851,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.20332154938339,\n 38.685285646134076\n ],\n [\n -120.20332154938339,\n 37.7390228675344\n ],\n [\n -117.59050221328755,\n 37.7390228675344\n ],\n [\n -117.59050221328755,\n 38.685285646134076\n ],\n [\n -120.20332154938339,\n 38.685285646134076\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"176","issue":"4036","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0003e4b0c8380cd4f52e","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":358286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G.I.","contributorId":103694,"corporation":false,"usgs":true,"family":"Smith","given":"G.I.","email":"","affiliations":[],"preferred":false,"id":358287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001310,"text":"1001310 - 1972 - Red fox spatial characteristics in relation to waterfowl predation","interactions":[],"lastModifiedDate":"2025-02-21T17:30:39.304971","indexId":"1001310","displayToPublicDate":"1972-04-07T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Red fox spatial characteristics in relation to waterfowl predation","docAbstract":"Radio-equipped red foxes (Vulpes vulpes) on the Cedar Creek area in Minnesota were spatially distributed, with individual families occupying well defined, nonoverlapping, contiguous territories. Territory boundaries often conformed to natural physical boundaries and appeared to be maintained through some nonaggressive behavior mechanism. Individual foxes traveled extensively throughout the family territory each night. Fox territories appeared to range from approximately 1 to 3 square miles in size, dependent largely on population density. Red foxes used a sequence of dens to rear their pups, and the amount and location of food remains at individual dens changed as the pups matured. The denning season was divided into pre-emergence, confined-use, and dispersed-use periods of 4 to 5 weeks each. Remains of adult waterfowl were collected at rearing dens on six townships in three ecologically different regions of eastern North Dakota. Remains of 172 adult dabbling ducks and 16 adult American coots (Fulica americana) were found at 35 dens. No remains from diving ducks were found. The number of adult ducks per den averaged 1.6, 5.9, and 10.2 for paired townships in regions with relatively low, moderate and high duck populations, respectively. Eighty-four percent of the ducks were females. The species and sex composition of ducks found at dens during early and late sampling periods reflected the nesting chronology of prairie dabbling ducks. Occupied rearing dens were focal points of red fox travel, and the locations of dens may have had considerable influence on predation. Thirty-five of 38 dens found on the six township study areas were on pastured or idle lands. The distribution of rearing dens on the Sand Lake and Arrowwood national wildlife refuges suggested that, on these areas, fox dens were concentrated because of the topography and land-use practices.
","language":"English","publisher":"Wiley","doi":"10.2307/3799055","usgsCitation":"Sargeant, A., 1972, Red fox spatial characteristics in relation to waterfowl predation: Journal of Wildlife Management, v. 36, no. 2, p. 225-236, https://doi.org/10.2307/3799055.","productDescription":"12 p.","startPage":"225","endPage":"236","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133755,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Anoka County, Isanti County","otherGeospatial":"Cedar Creek Natural History Area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.0186,45.4131],[-93.0188,45.2984],[-93.0207,45.1258],[-93.2262,45.1255],[-93.2272,45.0373],[-93.2814,45.0374],[-93.2807,45.0498],[-93.2814,45.0539],[-93.2826,45.0584],[-93.2826,45.063],[-93.282,45.0666],[-93.282,45.0689],[-93.2813,45.0717],[-93.2794,45.0753],[-93.2781,45.0794],[-93.2787,45.0835],[-93.28,45.0867],[-93.28,45.0913],[-93.2799,45.0959],[-93.2786,45.1],[-93.2786,45.1036],[-93.2793,45.1064],[-93.2812,45.1077],[-93.2863,45.1119],[-93.2915,45.1155],[-93.2934,45.1187],[-93.2947,45.1215],[-93.296,45.1251],[-93.296,45.1274],[-93.296,45.1297],[-93.2985,45.1329],[-93.3011,45.1356],[-93.3024,45.1388],[-93.3056,45.1416],[-93.3076,45.1429],[-93.3127,45.1448],[-93.3179,45.1466],[-93.3211,45.1484],[-93.3257,45.1512],[-93.3302,45.1539],[-93.3328,45.1544],[-93.3347,45.1549],[-93.3373,45.1558],[-93.3399,45.1576],[-93.3431,45.1599],[-93.3463,45.1626],[-93.3495,45.1663],[-93.3528,45.1699],[-93.3553,45.1727],[-93.3579,45.1745],[-93.3618,45.1759],[-93.3663,45.1768],[-93.3709,45.1777],[-93.3767,45.1805],[-93.3812,45.1832],[-93.3838,45.1855],[-93.3864,45.1878],[-93.3889,45.1892],[-93.3928,45.1914],[-93.3967,45.1933],[-93.4025,45.1956],[-93.4084,45.1965],[-93.4116,45.1983],[-93.4142,45.2001],[-93.4161,45.2038],[-93.418,45.2088],[-93.4193,45.2116],[-93.4226,45.2134],[-93.4252,45.2152],[-93.4264,45.2157],[-93.4297,45.2161],[-93.4362,45.217],[-93.4426,45.2166],[-93.4472,45.2161],[-93.4517,45.2157],[-93.4543,45.2175],[-93.4575,45.2203],[-93.4614,45.2234],[-93.4653,45.2257],[-93.4698,45.2257],[-93.4763,45.2253],[-93.4821,45.2248],[-93.4847,45.2257],[-93.4879,45.2271],[-93.4912,45.2289],[-93.4964,45.2344],[-93.5022,45.239],[-93.5035,45.2399],[-93.5073,45.2417],[-93.5113,45.2431],[-93.5138,45.2454],[-93.5093,45.4163],[-93.5106,45.5598],[-93.5133,45.7335],[-93.1408,45.7312],[-93.1392,45.5602],[-93.0221,45.5576],[-93.0186,45.4131]]]},\"properties\":{\"name\":\"Anoka\",\"state\":\"MN\"}}]}","volume":"36","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63538a","contributors":{"authors":[{"text":"Sargeant, A.B.","contributorId":13171,"corporation":false,"usgs":true,"family":"Sargeant","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":310863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1001607,"text":"1001607 - 1972 - Techniques for establishing local breeding populations of wood ducks","interactions":[],"lastModifiedDate":"2025-02-21T17:19:35.493014","indexId":"1001607","displayToPublicDate":"1972-04-07T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Techniques for establishing local breeding populations of wood ducks","docAbstract":"A study was conducted on the Arrowwood National Wildlife Refuge in east-central North Dakota to further evaluate a technique for establishing nesting wood ducks (Aix sponsa) by releasing propagated birds and installing nest houses. No wood duck nesting had been recorded previously in the area. During May-July 1968, 253 ducklings, hand-reared at the Northern Prairie Wildlife Research Center near Jamestown, North Dakota, were released when 9 to 16 days old into a 0.5-acre enclosure on the refuge, where they grew to flight stage and departed. Seventy-eight nest houses were installed in August on the refuge. About 76 percent of the ducks survived until late September, when southward migration began. The first-year band recovery rate by hunters of 4.7 percent was comparable to that of wild immature wood ducks. Most recoveries occurred between North Dakota and Minnesota in the north and Texas and Louisiana in the south. There were 16 nesting attempts, which produced 175 ducklings, by homing female wood ducks in the boxes in 1969. The number of nesting attempts increased to 34 in 1970, with a production of 311 ducklings.
","language":"English","publisher":"Wiley","doi":"10.2307/3799073","usgsCitation":"Doty, H.A., and Kruse, A., 1972, Techniques for establishing local breeding populations of wood ducks: Journal of Wildlife Management, v. 36, no. 2, p. 428-435, https://doi.org/10.2307/3799073.","productDescription":"8 p.","startPage":"428","endPage":"435","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":134507,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Arrowwood National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.525390625,\n 47.37603463349758\n ],\n [\n -97.14111328125,\n 47.37603463349758\n ],\n [\n -97.14111328125,\n 47.98256841921405\n ],\n [\n -98.525390625,\n 47.98256841921405\n ],\n [\n -98.525390625,\n 47.37603463349758\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"36","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68618d","contributors":{"authors":[{"text":"Doty, Harold A.","contributorId":17565,"corporation":false,"usgs":true,"family":"Doty","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":311346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kruse, A.D.","contributorId":19900,"corporation":false,"usgs":true,"family":"Kruse","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":311347,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010248,"text":"70010248 - 1972 - Nimbus IV view of the major structural features of Alaska","interactions":[],"lastModifiedDate":"2026-01-23T22:32:08.618546","indexId":"70010248","displayToPublicDate":"1972-03-31T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Nimbus IV view of the major structural features of Alaska","docAbstract":"Notwithstanding the relatively low degree of ground resolution, many of the major structural features of Alaska can be identified on the Nimbus IV IDCS image, exposed at an altitude of 600 nautical miles (1100 km). In addition, linears of regional extent that may be structurally controlled can be seen, many of which have not yet been recognized in surface mapping. The synoptic view provided by the image brings into focus an orthogonal set of fractures trending north-northeast and east-southeast and not heretofore apparent in regional maps of Alaska. This orthogonal fracture set may reflect a conjugate set of fractures within the crust, which has exerted significant control over the geologic history of the state. Increased resolution in other images from space platforms, such as the resolution of 200 to 650 feet (60 to 200 m) planned for the satellite television cameras of the ERTS program, will permit the discernment of finer detail and a greater accuracy in identifying and locating geologic features.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4029.1423","issn":"00368075","usgsCitation":"Lathram, E., 1972, Nimbus IV view of the major structural features of Alaska: Science, v. 175, no. 4029, p. 1423-1427, https://doi.org/10.1126/science.175.4029.1423.","productDescription":"5 p.","startPage":"1423","endPage":"1427","costCenters":[],"links":[{"id":219601,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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H.","affiliations":[],"preferred":false,"id":358447,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70121227,"text":"70121227 - 1972 - Acoustic-reflection profiles, eastern Greater Antilles: Leg 3, 1971 cruise, UNITEDGEO I","interactions":[],"lastModifiedDate":"2018-06-21T10:13:22","indexId":"70121227","displayToPublicDate":"1972-01-01T10:17:57","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Acoustic-reflection profiles, eastern Greater Antilles: Leg 3, 1971 cruise, UNITEDGEO I","docAbstract":"As part of a cooperative marine research program designated the Internataional Decade of Ocean Exploration (IDOE), the United states Geological Survey is participating in an investigation of the geologic framework and resource potential of continental margins and small ocean basins in the Gulf of Mexico, Caribbean Sea, and west African continental shelf areas. These studies are funded through the National Science Foundation. Legs 1 and 2, completed June 22 and July 8, respectively, were concerned with subbottom features of the Bay of Campeche and with the tectonic framework of the continental margin east of the Yucatan Peninsula. Leg 3, described in this report was conducted in the Antilles region of the northeastern Caribbean between July 17 and August 4, 1971.
This report presents the unedited records of the approximately 5840 km of acoustic reflection profiling made during Leg 3. Magnetic and gravity data were collected also but are being reported elsewhere in conjunction with the results of the study.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70121227","collaboration":"USGS-GD-72-004, PB-207-596","usgsCitation":"Garrison, L.E., 1972, Acoustic-reflection profiles, eastern Greater Antilles: Leg 3, 1971 cruise, UNITEDGEO I, 19 p., https://doi.org/10.3133/70121227.","productDescription":"19 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":355152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/89839/report.pdf","text":"Report","size":"20.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Unumbered Series 89839"}],"otherGeospatial":"Caribbean Sea;Greater Antilles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.37,16.44 ], [ -79.37,23.38 ], [ -65.22,23.38 ], [ -65.22,16.44 ], [ -79.37,16.44 ] ] ] } } ] }","contact":"Coastal and Marine Geology Program
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1372B","usgsCitation":"Hayes, P.T., 1972, Stratigraphic nomenclature of Cambrian and Lower Ordovician rocks of easternmost southern Arizona and adjacent westernmost New Mexico: U.S. Geological Survey Bulletin 1372, iii, 21 p., https://doi.org/10.3133/b1372B.","productDescription":"iii, 21 p.","costCenters":[],"links":[{"id":416786,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92651.htm","linkFileType":{"id":5,"text":"html"}},{"id":62535,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1372b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167262,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1372b/report-thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111,\n 33.375\n ],\n [\n -111,\n 31.3322\n ],\n [\n -106.375,\n 31.3322\n ],\n [\n -106.375,\n 33.375\n ],\n [\n -111,\n 33.375\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebdd","contributors":{"authors":[{"text":"Hayes, Philip Thayer","contributorId":8071,"corporation":false,"usgs":true,"family":"Hayes","given":"Philip","email":"","middleInitial":"Thayer","affiliations":[],"preferred":false,"id":213326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17610,"text":"ofr72325 - 1972 - Reconnaissance geologic map of the Solomon D-6 quadrangle, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2022-08-11T13:04:59.96683","indexId":"ofr72325","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"72-325","title":"Reconnaissance geologic map of the Solomon D-6 quadrangle, Seward Peninsula, Alaska","docAbstract":"The Solomon D-6 15- by 30-minute quadrangle lies 20 miles northeast of Nome, Alaska, and adjoins on the east the Nome D-l quadrangle mapped by Hummel (1962b) and on the west the Solomon D-5 quadrangle mapped by Smith (1910).
Placer gold has been produced from Iron Creek and many of its tributaries, and a small amount of copper was shipped from the Wheeler mine. Many lode prospects contain small amounts of copper in silicified limestone within and near the base of thrust plates of carbonate rocks. Other lodes consist of well-defined veins containing gold and base-metal sulfide minerals, but none has been commercially productive.
Mapped rock units include the \"York Slate,\" of Precambrian age, which consists of a highly deformed and thick sequence of graphitic calcareous siltite, which contains thin limestone beds and intercalated(?) volcaniclastic rocks, and Paleozoic carbonate rocks, which have been converted largely to marble and schistose marble. Along and near the Kigluaik Mountains in the north part of the quadrangle, quartzo-feldspathic gneisses of Precambrian age are intruded by fine-grained granite. A very thick sequence of schistose thin-bedded argillaceous and dolomitic limestone overlies the York Slate and is correlative with a similar rock originally mapped in the York Mountains.
Surficial deposits, consisting principally of moraine and stream-reworked moraine, mantle large parts of the quadrangle.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72325","usgsCitation":"Sainsbury, C., Hudson, T., Ewing, R., and Richards, T., 1972, Reconnaissance geologic map of the Solomon D-6 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 72-325, Report: 17 p.; 1 Plate: 17.71 x 22.79 inches, https://doi.org/10.3133/ofr72325.","productDescription":"Report: 17 p.; 1 Plate: 17.71 x 22.79 inches","costCenters":[],"links":[{"id":150582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0325/report-thumb.jpg"},{"id":46804,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0325/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0325/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404229,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_113150.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"63360","country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula, Solomon D-6 quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -165,\n 64.75\n ],\n [\n -164.5,\n 64.75\n ],\n [\n -164.5,\n 65\n ],\n [\n -165,\n 65\n ],\n [\n -165,\n 64.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db6411dc","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":177092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":177091,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ewing, Rodney","contributorId":106914,"corporation":false,"usgs":true,"family":"Ewing","given":"Rodney","affiliations":[],"preferred":false,"id":177093,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richards, Thomas","contributorId":54622,"corporation":false,"usgs":true,"family":"Richards","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":177090,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70156919,"text":"70156919 - 1971 - Marine terraces of the western Aleutian Islands, Alaska","interactions":[],"lastModifiedDate":"2019-11-12T16:51:00","indexId":"70156919","displayToPublicDate":"2015-09-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Marine terraces of the western Aleutian Islands, Alaska","docAbstract":"The islands of the Rat Islands group, which includes Amchitka Island, have active sea cliffs, well-developed intertidal platforms, and a prominent submarine platform at -100 m. These features have not been disturbed by tectonic activity for the past 17,000 years. The islands of the Delarof Islands group, located east of Amchitka Pass, have inactive sea cliffs and emergent low terraces that indicate relatively recent uplift, possibly as much as 4 m. Higher and older marine terraces on the islands of both groups cannot be correlated, and some tectonic adjustment between the island groups is suggested.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70156919","usgsCitation":"Morris, R.H., 1971, Marine terraces of the western Aleutian Islands, Alaska, ii, 23 p., https://doi.org/10.3133/70156919.","productDescription":"ii, 23 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70156919.JPG"},{"id":308543,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156919/report.pdf","text":"Report"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Islands","tableOfContents":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i677","usgsCitation":"Moore, J., 1971, Bathymetry and geology— East cape of the island of Hawaii: U.S. Geological Survey IMAP 677, 1 Plate: 30.00 × 41.85 inches, https://doi.org/10.3133/i677.","productDescription":"1 Plate: 30.00 × 41.85 inches","costCenters":[],"links":[{"id":391832,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9454.htm"},{"id":260867,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0677/plate-1.pdf"},{"id":189504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","country":"United States","state":"Hawaii","otherGeospatial":"Island of Hawaii","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -154.875,\n 19.397\n ],\n [\n -154.5,\n 19.397\n ],\n [\n -154.5,\n 19.739\n ],\n [\n -154.875,\n 19.739\n ],\n [\n -154.875,\n 19.397\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ee4b07f02db640201","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":274801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47917,"text":"ofr7139 - 1971 - Chemical quality of ground water in the Dos Palos-Kettleman City area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2024-05-24T21:00:22.894001","indexId":"ofr7139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-39","title":"Chemical quality of ground water in the Dos Palos-Kettleman City area, San Joaquin Valley, California","docAbstract":"The Dos Palos-Kettleman City area of this report includes approximately 1,350 square miles on the central-western side of the San Joaquin Valley, California. Large-scale farming operations in the area have used ground water as the major source of irrigation water for nearly three quarters of a century. In 1968, completion of the San Luis Canal part of the California Aqueduct, made surface water available to farmers. In time the widespread use of this imported water may cause chemical-quality changes in the native ground water. To document conditions prior to any possible changes, 361 samples of ground water were taken before deliveries of surface water were begun. The data will serve as a base to which future investigations can be compared. To establish any trends, the results were compared to earlier chemical data for the area. The results indicated that only minor changes in chemical quality had occurred between 1951 and 1968.
Water from an upper water-bearing zone is markedly different from water in a lower water-bearing zone. Water in the upper zone is of various chemical types, and the concentration of dissolved solids increases from east to west across the area.
Water in the lower zone is a sodium sulfate type and is fairly consistent throughout the zone.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7139","collaboration":"Prepared in cooperation with the California Department of Water Resources U.S. Bureau of Reclamation, and Westlands Water District","usgsCitation":"Bertoldi, G., 1971, Chemical quality of ground water in the Dos Palos-Kettleman City area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 71-39, 45 p., https://doi.org/10.3133/ofr7139.","productDescription":"45 p.","costCenters":[],"links":[{"id":429283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0039/report-thumb.jpg"}],"country":"United States","state":"California","city":"Dos Palos, Kettleman City","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.68923886927595,\n 36.99619474770276\n ],\n [\n -120.68923886927595,\n 35.97967811304345\n ],\n [\n -119.91146897398625,\n 35.97967811304345\n ],\n [\n -119.91146897398625,\n 36.99619474770276\n ],\n [\n -120.68923886927595,\n 36.99619474770276\n ]\n ]\n ],\n \"type\": \"Polygon\"\n },\n \"id\": 0\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e399e","contributors":{"authors":[{"text":"Bertoldi, G.L.","contributorId":11605,"corporation":false,"usgs":true,"family":"Bertoldi","given":"G.L.","affiliations":[],"preferred":false,"id":236526,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6236,"text":"pp701A - 1971 - Hydrology of two small river basins in Pennsylvania before urbanization, with a section on observation of stream fauna","interactions":[],"lastModifiedDate":"2017-07-07T09:08:31","indexId":"pp701A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"701","chapter":"A","title":"Hydrology of two small river basins in Pennsylvania before urbanization, with a section on observation of stream fauna","docAbstract":"Basic data on water quantity, chemical quality, and suspended sediment are tabulated to record the conditions existing in two basins near Philadelphia, each about 32 square miles in area. The basins in 1970 are agricultural land for the most part, but urban and industrial development is imminent as the Philadelphia metropolitan area expands. Hopefully, as changes caused by urbanization occur in future years, data published herein will be useful as a base for comparison.
Pickering Creek basin has a higher population than the upper East Branch Brandywine Creek basin. The two are comparable in discharge characteristics and in shapes and sizes of channels, but the Pickering Creek basin is producing a considerably larger suspended-sediment load. Also the effects of urbanization are discernible in some chemical parameters.
During the study, a small subbasin, one-half square mile in area, was converted from agricultural use to an industrial park. This change resulted in a marked increase in sulfates, nitrates, chlorides, and dissolved solids in the streamflow.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp701A","usgsCitation":"Miller, R.A., Troxell, J., Leopold, L.B., Patrick, R., and Grant, R.R., 1971, Hydrology of two small river basins in Pennsylvania before urbanization, with a section on observation of stream fauna: U.S. Geological Survey Professional Paper 701, iv, 57 p., https://doi.org/10.3133/pp701A.","productDescription":"iv, 57 p.","numberOfPages":"68","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":117927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0701a/report-thumb.jpg"},{"id":33442,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0701a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Upper East Branch Brandywine Creek, Pickering Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.89355468749999,\n 39.96870074491696\n ],\n [\n -75.45135498046875,\n 39.96870074491696\n ],\n [\n -75.45135498046875,\n 40.16418235037417\n ],\n [\n -75.89355468749999,\n 40.16418235037417\n ],\n [\n -75.89355468749999,\n 39.96870074491696\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7cc","contributors":{"authors":[{"text":"Miller, R. Adam","contributorId":21540,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"Adam","affiliations":[],"preferred":false,"id":152357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troxell, John","contributorId":83517,"corporation":false,"usgs":true,"family":"Troxell","given":"John","email":"","affiliations":[],"preferred":false,"id":152359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":152360,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patrick, Ruth","contributorId":95055,"corporation":false,"usgs":true,"family":"Patrick","given":"Ruth","email":"","affiliations":[],"preferred":false,"id":152361,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grant, Robert R. Jr.","contributorId":75524,"corporation":false,"usgs":true,"family":"Grant","given":"Robert","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152358,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":41559,"text":"ofr71293 - 1971 - Aeromagnetic map of the Patterson and Leodore quadrangles, east-central Idaho","interactions":[{"subject":{"id":41559,"text":"ofr71293 - 1971 - Aeromagnetic map of the Patterson and Leodore quadrangles, east-central Idaho","indexId":"ofr71293","publicationYear":"1971","noYear":false,"title":"Aeromagnetic map of the Patterson and Leodore quadrangles, east-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"id":1}],"supersededBy":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"lastModifiedDate":"2022-06-06T19:37:48.060601","indexId":"ofr71293","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-293","title":"Aeromagnetic map of the Patterson and Leodore quadrangles, east-central Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71293","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the Patterson and Leodore quadrangles, east-central Idaho: U.S. Geological Survey Open-File Report 71-293, 1 Plate: 29.60 x 29.51 inches, https://doi.org/10.3133/ofr71293.","productDescription":"1 Plate: 29.60 x 29.51 inches","costCenters":[],"links":[{"id":171011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0293/report-thumb.jpg"},{"id":401809,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0293/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Idaho","otherGeospatial":"Leodore Quadrangle, Patterson Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.62060546875,\n 44.32384807250689\n ],\n [\n -113.0712890625,\n 44.32384807250689\n ],\n [\n -113.0712890625,\n 44.62175409623324\n ],\n [\n -113.62060546875,\n 44.62175409623324\n ],\n [\n -113.62060546875,\n 44.32384807250689\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b8b","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":530472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42087,"text":"ofr71291 - 1971 - Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","interactions":[{"subject":{"id":42087,"text":"ofr71291 - 1971 - Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","indexId":"ofr71291","publicationYear":"1971","noYear":false,"title":"Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"id":1}],"supersededBy":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"lastModifiedDate":"2022-06-06T19:51:44.388865","indexId":"ofr71291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-291","title":"Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71291","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho: U.S. Geological Survey Open-File Report 71-291, 1 Plate: 29.41 x 42.51 inches, https://doi.org/10.3133/ofr71291.","productDescription":"1 Plate: 29.41 x 42.51 inches","costCenters":[],"links":[{"id":175557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0291/report-thumb.jpg"},{"id":401700,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Idaho","otherGeospatial":"Challis Quadrangle, Doublespring Quadrangle, Lone Pine Peak Quadrangle, May Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.8895263671875,\n 44.209772586984485\n ],\n [\n -113.7579345703125,\n 44.209772586984485\n ],\n [\n -113.7579345703125,\n 44.67646564865964\n ],\n [\n -114.8895263671875,\n 44.67646564865964\n ],\n [\n -114.8895263671875,\n 44.209772586984485\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69704b","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":530820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1040,"text":"wsp1999D - 1971 - Underground storage of imported water in the San Gorgonio Pass area, southern California","interactions":[{"subject":{"id":55888,"text":"ofr6920 - 1969 - Underground storage of imported water in the San Gorgonio Pass area, California","indexId":"ofr6920","publicationYear":"1969","noYear":false,"title":"Underground storage of imported water in the San Gorgonio Pass area, California"},"predicate":"SUPERSEDED_BY","object":{"id":1040,"text":"wsp1999D - 1971 - Underground storage of imported water in the San Gorgonio Pass area, southern California","indexId":"wsp1999D","publicationYear":"1971","noYear":false,"chapter":"D","title":"Underground storage of imported water in the San Gorgonio Pass area, southern California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1999D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1999","chapter":"D","title":"Underground storage of imported water in the San Gorgonio Pass area, southern California","docAbstract":"The San Gorgonio Pass ground-water basin is divided into the Beaumont, Banning, Cabazon, San Timoteo, South Beaumont, Banning Bench, and Singleton storage units. The Beaumont storage unit, centrally located in the agency area, is the largest in volume of the storage units. \r\n\r\nEstimated long-term average annual precipitation in the San Gorgonio Pass Water Agency drainage area is 332,000 acre-feet, and estimated average annual recoverable water is 24,000 acre-feet, less than 10 percent of the total precipitation. Estimated average annual surface outflow is 1,700 acre-feet, and estimated average annual ground-water recharge is 22,000 acre-feet. Projecting tack to probable steady-state conditions, of the 22.000 acre-feet of recharge, 16,003 acre-feet per year became subsurface outflow into Coachella Valley, 6,000 acre-feet into the Redlands area, and 220 acre-feet into Potrero Canyon. \r\n\r\nAfter extensive development, estimated subsurface outflow from the area in 1967 was 6,000 acre-feet into the Redlands area, 220 acre-feet into Potrero Canyon, and 800 acre-feet into the fault systems south of the Banning storage unit, unwatered during construction of a tunnel. Subsurface outflow into Coachella Valley in 1967 is probably less than 50 percent of the steady-state flow. An anticipated 17,000 .acre-feet of water per year will be imported by 1980. Information developed in this study indicates it is technically feasible to store imported water in the eastern part of the Beaumont storage unit without causing waterlogging in the storage area and without losing any significant quantity of stored water.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1999D","usgsCitation":"Bloyd, R.M., 1971, Underground storage of imported water in the San Gorgonio Pass area, southern California: U.S. Geological Survey Water Supply Paper 1999, iv, 37 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1999D.","productDescription":"iv, 37 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999d/report-thumb.jpg"},{"id":25684,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25685,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e479fe4b07f02db49307c","contributors":{"authors":[{"text":"Bloyd, Richard M.","contributorId":55802,"corporation":false,"usgs":true,"family":"Bloyd","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42025,"text":"ofr71292 - 1971 - Aeromagnetic map of the Custer, Elevenmile Creek, Sunbeam, Thompson Creek, and Clayton quadrangles, east-central Idaho","interactions":[{"subject":{"id":42025,"text":"ofr71292 - 1971 - Aeromagnetic map of the Custer, Elevenmile Creek, Sunbeam, Thompson Creek, and Clayton quadrangles, east-central Idaho","indexId":"ofr71292","publicationYear":"1971","noYear":false,"title":"Aeromagnetic map of the Custer, Elevenmile Creek, Sunbeam, Thompson Creek, and Clayton quadrangles, east-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"id":1}],"supersededBy":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"lastModifiedDate":"2022-06-06T19:49:25.510987","indexId":"ofr71292","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-292","title":"Aeromagnetic map of the Custer, Elevenmile Creek, Sunbeam, Thompson Creek, and Clayton quadrangles, east-central Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71292","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the Custer, Elevenmile Creek, Sunbeam, Thompson Creek, and Clayton quadrangles, east-central Idaho: U.S. Geological Survey Open-File Report 71-292, 1 Plate: 29.59 x 30.97 inches, https://doi.org/10.3133/ofr71292.","productDescription":"1 Plate: 29.59 x 30.97 inches","costCenters":[],"links":[{"id":175436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0292/report-thumb.jpg"},{"id":401811,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0292/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Idaho","otherGeospatial":"Clayton Quadrangle, Custer Quadrangle, Elevenmile Creek Quadrangle, Sunbeam Quadrangle, Thompson Creek Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.103759765625,\n 44.762336674810996\n ],\n [\n -113.675537109375,\n 44.762336674810996\n ],\n [\n -113.675537109375,\n 45.30580259943578\n ],\n [\n -115.103759765625,\n 45.30580259943578\n ],\n [\n -115.103759765625,\n 44.762336674810996\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691c8f","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":530776,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68326,"text":"ha354 - 1971 - Reconnaissance of the Black River, a cold-water river in the northcentral part of Michigan's southern peninsula","interactions":[],"lastModifiedDate":"2021-10-21T15:11:14.56474","indexId":"ha354","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"354","title":"Reconnaissance of the Black River, a cold-water river in the northcentral part of Michigan's southern peninsula","docAbstract":"The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, trout fishing) but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of the water resource for recreation and other demands, an analysis of the hydrologic factors related to recreational values is essential.
The Black River north of Johannesburg in Otsego County has been rated by many fisherman as the number one brook-trout stream in the north-central part of the southern peninsula of Michigan. Headwaters are a few miles north of Johannesburg, and the Black flows northward to join the Cheboygan river a few miles south of Cheyboygan. Only the part of the Black upstream from the impoundment at Tower is included in this report.
The headwaters of the Black can be reached by driving east and north from Gaylord, or east from Vanderbilt. The lower reaches included in this study can be reached from Tower or Onaway.
The recreational value of a river depends on the characteristics of streamflow, water-quality, and its bed and banks. The purpose of this atlas is to describe these characteristics and to show how they relate to recreational uses.
Some of the information presented here was derived from basic records of the U.S. Geological Survey's Water-Resources Division. Additional information was obtained in field reconnaissance surveys in 1966 and 1968. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Advice and assistance were also obtained from other sections of the Michigan Conservation Department.
Sheet 1 of this atlas presents information on streamflow characteristics and water quality. Sheet 2 describes the physical character of the stream channel, bed and banks, and shows how it relates to streamflow, water quality, and recreational use.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha354","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1971, Reconnaissance of the Black River, a cold-water river in the northcentral part of Michigan's southern peninsula: U.S. Geological Survey Hydrologic Atlas 354, 2 Plates: 34.0 x 33.8 inches and 34.5 x 34.0 inches, https://doi.org/10.3133/ha354.","productDescription":"2 Plates: 34.0 x 33.8 inches and 34.5 x 34.0 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha354.JPG"},{"id":390725,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15731.htm"},{"id":89788,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/354/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89787,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/354/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Michigan","otherGeospatial":"Black River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.26994323730469,\n 45.33090957287155\n ],\n [\n -84.25689697265625,\n 45.3386325573467\n ],\n [\n -84.24247741699219,\n 45.33332311865989\n ],\n [\n -84.23492431640624,\n 45.32028874948921\n ],\n [\n -84.2376708984375,\n 45.313046137311275\n ],\n [\n -84.25003051757812,\n 45.31352900692258\n ],\n [\n -84.254150390625,\n 45.2995241178219\n ],\n [\n -84.24316406249999,\n 45.287448160456634\n ],\n [\n -84.23492431640624,\n 45.27343682845453\n ],\n [\n -84.25209045410156,\n 45.26377182487572\n ],\n [\n -84.26994323730469,\n 45.2574886900362\n ],\n [\n -84.28573608398438,\n 45.25265503624703\n ],\n [\n -84.29122924804688,\n 45.24250302408533\n ],\n [\n -84.29878234863281,\n 45.23863511362128\n ],\n [\n -84.31320190429686,\n 45.2352504759637\n ],\n [\n -84.31732177734375,\n 45.230414929592946\n ],\n [\n -84.32418823242188,\n 45.222677199620094\n ],\n [\n -84.32418823242188,\n 45.21010114198755\n ],\n [\n -84.31800842285156,\n 45.19752230305682\n ],\n [\n -84.31732177734375,\n 45.18687649773411\n ],\n [\n -84.31251525878906,\n 45.15395869129108\n ],\n [\n -84.30152893066406,\n 45.12053735276011\n ],\n [\n -84.31388854980469,\n 45.101638366018676\n ],\n [\n -84.36882019042969,\n 45.09485258791474\n ],\n [\n -84.40658569335936,\n 45.101638366018676\n ],\n [\n -84.41482543945311,\n 45.119083806728156\n ],\n [\n -84.42512512207031,\n 45.1433047394883\n ],\n [\n -84.42100524902344,\n 45.16315822892636\n ],\n [\n -84.40933227539062,\n 45.17671273501559\n ],\n [\n -84.34684753417969,\n 45.188812246819055\n ],\n [\n -84.34272766113281,\n 45.19897384949407\n ],\n [\n -84.34066772460938,\n 45.20864987944066\n ],\n [\n -84.342041015625,\n 45.222677199620094\n ],\n [\n -84.33448791503906,\n 45.23138207178167\n ],\n [\n -84.32281494140625,\n 45.24588722974015\n ],\n [\n -84.30427551269531,\n 45.25458854713424\n ],\n [\n -84.29878234863281,\n 45.26280523400372\n ],\n [\n -84.27886962890625,\n 45.27053750018046\n ],\n [\n -84.25209045410156,\n 45.27778554315248\n ],\n [\n -84.25827026367188,\n 45.284549548064156\n ],\n [\n -84.27337646484375,\n 45.29855813586017\n ],\n [\n -84.26513671875,\n 45.31352900692258\n ],\n [\n -84.26170349121094,\n 45.32559941008895\n ],\n [\n -84.26994323730469,\n 45.33090957287155\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afcc","contributors":{"authors":[{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":925,"text":"wsp1999C - 1971 - Water resources of the upper White River basin, east-central Indiana","interactions":[],"lastModifiedDate":"2022-11-07T16:50:28.66113","indexId":"wsp1999C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1999","chapter":"C","title":"Water resources of the upper White River basin, east-central Indiana","docAbstract":"Ground-water discharge to the streams sustains year-round streamflow in the upper White River basin. This discharge, referred to as ground-water runoff or base runoff, is considered to be an index to the amount of g ound water available for development. A comparison of the variations of groundwater runoff and aquifer distribution in the basin shows that the areas of best development potential are areas where thick sand and gravel aquifers are adjacent to the streams. The average ground-water runoff for these areas is between 400,000 and 500,000 gallons per day per square mile.
\nThe most permeable aquifers in the basin are the sand and gravel deposits of Quaternary age. These aquifers occur mainly as relatively thick elongate bodies along bedrock valleys and as relatively thin sheetlike deposits at or near land surface. The representative hydraulic conductivity of these aquifers ranges from 1,500 to 2,500 gallons per day per square foot. The limestone and dolomite formations of the bedrock are a source of moderate quar tities of water.
\nThe long-term average streamflow in the basin is approximately 0.9 cubic feet per second per square mile. The yearly average discharge varies from about one-fourth to twice the long-term average. The 7-day 10-year low flow ranges from about 0.01 to 0.3 cubic feet per second per square mile; the main-stem flow ranges from 0.10 to 0.13 cubic feet per second per square mile.
\nThe water in the aquifers is predominately a very hard calcium bicarbonate type; it is generally high in iron and contains a moderate amount of dissolved solids. Fresh water (1,000 milligrams per liter dissolved solids or less) is present to depths of approximately 400 feet below land surface. In the tributaries and in the headwaters region of the White River, the composition of surface water is very similar to that of ground water. The quality cf the water in the White River deteriorates in the downstream direction owing to the cumulative effects of sewage effluent.
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