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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1731","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of the United States, October 1950 to September 1960, part 7. Lower Mississippi basin: U.S. Geological Survey Water Supply Paper 1731, Report: xiii, 552 p.; 1 Plate: 39.79 × 30.88 inches, https://doi.org/10.3133/wsp1731.","productDescription":"Report: xiii, 552 p.; 1 Plate: 39.79 × 30.88 inches","costCenters":[],"links":[{"id":138477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1731/report-thumb.jpg"},{"id":27070,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1731/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264375,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1731/plate-1.pdf","size":"8506","linkFileType":{"id":1,"text":"pdf"}},{"id":395104,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24915.htm"}],"country":"United States","otherGeospatial":"lower Mississippi River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.501953125,\n 29.878755346037977\n ],\n [\n -86.044921875,\n 29.878755346037977\n ],\n [\n -86.044921875,\n 39.605688178320804\n ],\n [\n -104.501953125,\n 39.605688178320804\n ],\n [\n -104.501953125,\n 29.878755346037977\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a97fa","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1853,"text":"wsp1750B - 1964 - Summary of floods in the United States during 1959","interactions":[],"lastModifiedDate":"2017-09-06T17:51:01","indexId":"wsp1750B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1750","chapter":"B","title":"Summary of floods in the United States during 1959","docAbstract":"

This report describes the most outstanding floods that occurred in the United States during 1959.

The floods of January-February in Ohio and adjacent States were the most outstanding floods of the year 1959 with respect to area affected, number of streams having maximum discharge of record, rare occurrence of peaks, and great amount of damage caused.

Floods in the Rock River basin in southern Wisconsin and northern Illinois during late March and early April produced maximum stages and discharges on many streams. The Rock River at Watertown, Wisc., was the highest in 40 years and Lake Mendota at Madison, Wisc., reached its maximum stage since 1916. Many towns were flooded and thousands of persons were forced from their homes.

What is possibly the greatest 24-hour rainfall ever to be noted in Iowa fell August 5-6. The resulting floods inundated an 80-block area in Fort Madison, Iowa, and caused damage estimated at $600,000 in the city. A total of 130,000 acres of land was inundated.

Major floods occurred in Texas in the upper Trinity, middle Brazos, middle Colorado, upper Guadalupe, and upper Nueces River basins in early October, following heavy general rains that covered most of Texas. The peak stage on North Bosque River near Clifton was the highest known since 1887. More than \\$1 million in damage was reported for Houston.

In addition to the 4 floods mentioned above, 22 others of lesser magnitude are considered important enough to report in this annual summary.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1750B","usgsCitation":"Hendricks, E.L., 1964, Summary of floods in the United States during 1959: U.S. Geological Survey Water Supply Paper 1750, vi, 101 p., https://doi.org/10.3133/wsp1750B.","productDescription":"vi, 101 p.","numberOfPages":"101","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1750b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1750b/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69927b","contributors":{"authors":[{"text":"Hendricks, E. 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D1-D32, https://doi.org/10.3133/pp462D.","productDescription":"p. D1-D32","costCenters":[],"links":[{"id":123283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0462d/report-thumb.jpg"},{"id":65972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0462d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdcf","contributors":{"authors":[{"text":"Colby, B. 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E1-E46, https://doi.org/10.3133/pp462E.","productDescription":"p. E1-E46","costCenters":[],"links":[{"id":120516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0462e/report-thumb.jpg"},{"id":65973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0462e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685878","contributors":{"authors":[{"text":"Guy, H.P.","contributorId":73571,"corporation":false,"usgs":true,"family":"Guy","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":220685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32795,"text":"pp372B - 1964 - General effects of drought on water resources of the southwest","interactions":[],"lastModifiedDate":"2022-02-16T22:32:18.53445","indexId":"pp372B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"372","chapter":"B","title":"General effects of drought on water resources of the southwest","docAbstract":"

The effects of drought are most pronounced on soil moisture, because soil is the prime recipient of the water from precipitation, and upon streamflow, because it is the residual water that is not accepted by or that flows out from the soil and groundwater reservoirs. Studies by statistical correlation of records of natural streamflow and of dendrochronology indicate patterns of regional runoff that reflect precipitation trends in the principal meteorologic regions in the Southwest. By contrast, the effects of drought upon ground water vary with the natural characteristics and degree of utilization of individual aquifers.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Drought in the Southwest, 1942-56 (Professional Paper 372)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp372B","usgsCitation":"Gatewood, J.S., Wilson, A., Thomas, H.E., and Kister, L., 1964, General effects of drought on water resources of the southwest: U.S. Geological Survey Professional Paper 372, Report: iii, 55 p.; 1 Plate: 16.99 x 20.10 inches, https://doi.org/10.3133/pp372B.","productDescription":"Report: iii, 55 p.; 1 Plate: 16.99 x 20.10 inches","numberOfPages":"59","costCenters":[],"links":[{"id":336002,"rank":7,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372D","text":"Chapter D: Effects of drought in the Rio Grande basin"},{"id":336000,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372A","text":"Chapter A: The meteorologic phenomenon of drought in the Southwest"},{"id":336001,"rank":6,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372C","text":"Chapter C: Effects of drought in central and south Texas"},{"id":336003,"rank":8,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372E","text":"Chapter E: Effects of drought in basins of interior drainage"},{"id":336004,"rank":9,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372F","text":"Chapter F: Effects of drought in the Colorado River basin"},{"id":336005,"rank":10,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372G","text":"Chapter G: Effects of drought along Pacific Coast in California"},{"id":336006,"rank":11,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp372H","text":"Chapter H: General summary of effects of the drought in the Southwest"},{"id":60777,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0372b/plate-1.pdf","text":"Plate 1","size":"3.43 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Areas where annual runoff was less than the median, 1942-57"},{"id":60778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0372b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104445,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4368.htm","size":"7.73 MB","linkFileType":{"id":5,"text":"html"},"description":"4368"},{"id":119888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0372b/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Southwestern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.32226562500001,\n 31.50362930577303\n ],\n [\n -99.49218749999999,\n 31.50362930577303\n ],\n [\n -99.49218749999999,\n 38.95940879245423\n ],\n [\n -120.32226562500001,\n 38.95940879245423\n ],\n [\n -120.32226562500001,\n 31.50362930577303\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0fb6","contributors":{"authors":[{"text":"Gatewood, J. 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R.","affiliations":[],"preferred":false,"id":209188,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20,"text":"wsp1722 - 1964 - Compilation of records of surface waters of the United States, October 1950 to September 1960, part 1–B. North Atlantic Slope Basins, New York to York River","interactions":[],"lastModifiedDate":"2022-01-28T21:47:58.436514","indexId":"wsp1722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1722","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960, part 1–B. North Atlantic Slope Basins, New York to York River","docAbstract":"

No abstract available.

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An investigation of the chemical quality of surface waters and of the sedimentation in the Grand River drainage basin by the U.S. Geological Survey began in 1946. The chemical quality of the water was studied to obtain information on the nature and amounts of dissolved solids in the streams and on the suitability of the water for domestic, industrial, and irrigation uses. Sedimentation was studied to determine the quantity of sediment that is transported by the streams, the particle sizes of the sediment, and the probable specific weight of the sediment when deposited in a reservoir.

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The basin is underlain by consolidated sedimentary rocks of Cretaceous and Tertiary age; along the Grand River and its tributaries thefe rocks are mantled by alluvium of Quaternary age. The Hell Creek and Fort Union Formations underlie about 4,700 of the 5,680 square miles of drainage area. The climate of the basin is semiarid and is characterized by tot summers and cold winters. Mean annual runoff is about 53 acre-feet per square mile of drainage area and is equal to about 7 percent of the mean annual precipitation. The highest streamflows on the Grand River and major- tributaries are caused by melting of snow in March and April. Streamflow is extremely variable from year to year.

\n

Most of the surface waters in the basin are of the sodium sulfate or sodium bicarbonate type. High percent sodium is typical of almost all the surface water's. The streamflow-quality patterns of the Grand River and its two forks are very similar; dissolved-solids concentration, which usually c'oes not exceed 3,000 ppm, is maximum during low-flow periods.

\n

The water in Shadehill Reservoir became stratified during the flood inflow of 1952; about 75 percent of the flood water, which was of good qutlity, passed through the reservoir. The quality of the water became almost uniform throughout the reservoir the latter part of July 1952. After the specific conductance became relatively stable in 1956, it fluctuated from abrut 1,300 to 1,600 micromhos per centimeter and was between 1,400 and 1,500 rnicromhos per centimeter most of the time.

\n

During the representative period July 1937 to June 1950 the quantity of dissolved solids passing the station near Wakpala was estimated to have been about 140,000 tons per year. Yields computed for different parts of the basin ranged from about 22 to 32 tons per square mile.

\n

Except for sulfate, concentrations of chemical constituents usually do not exceed the maximum concentrations recommended for domestic supplies. The rather high dissolved solids and hardness of most of the surface waters prevent the use of these waters for most industrial purposes unless the quality is improved by treatment.

\n

Classified for irrigation use according to its specific conductance and sodiumadsorption-ratio, the water stored in Shadehill Reservoir has a high salinity hazard and a medium sodium hazard. The water can be used safely forsustained irrigation on soils of the proposed irrigation unit if adequate teaching is practiced and if gypsum or some other calcium compound is added to the water or land during the high sodium cycle.

\n

 

","language":"English","publisher":"U.S. Government Print Office","doi":"10.3133/wsp1769","usgsCitation":"Hembree, C.H., Krieger, R.A., and Jordan, P.R., 1964, Chemical quality of surface waters, and sedimentation in the Grand River drainage basin, North and South Dakota: U.S. Geological Survey Water Supply Paper 1769, Report: viii, 78 p.; 4 Plates: 18.50 x 24.00 inches or smaller, https://doi.org/10.3133/wsp1769.","productDescription":"Report: viii, 78 p.; 4 Plates: 18.50 x 24.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":27028,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1769/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27030,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1769/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1769/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1769/report-thumb.jpg"},{"id":27029,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1769/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27027,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1769/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota, South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.04052734375,\n 45.537136680398596\n ],\n [\n -104.04052734375,\n 46.240651955001695\n ],\n [\n -100.37109375,\n 46.240651955001695\n ],\n [\n -100.37109375,\n 45.537136680398596\n ],\n [\n -104.04052734375,\n 45.537136680398596\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3286","contributors":{"authors":[{"text":"Hembree, Charles Herbert","contributorId":63784,"corporation":false,"usgs":true,"family":"Hembree","given":"Charles","email":"","middleInitial":"Herbert","affiliations":[],"preferred":false,"id":144223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krieger, Robert A.","contributorId":99954,"corporation":false,"usgs":true,"family":"Krieger","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jordan, Paul Robert","contributorId":57819,"corporation":false,"usgs":true,"family":"Jordan","given":"Paul","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":144222,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3181,"text":"wsp1369E - 1964 - Stream gaging control structure for the Rio Grande Conveyance Channel near Bernardo New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1369E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1369","chapter":"E","title":"Stream gaging control structure for the Rio Grande Conveyance Channel near Bernardo New Mexico","language":"ENGLISH","publisher":"U.S. Govt. 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