{"pageNumber":"658","pageRowStart":"16425","pageSize":"25","recordCount":16493,"records":[{"id":70212914,"text":"70212914 - 1936 - Report of the Committee on Underground Waters, 1935–36","interactions":[],"lastModifiedDate":"2020-09-01T17:53:58.343522","indexId":"70212914","displayToPublicDate":"1936-09-01T12:51:48","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the Committee on Underground Waters, 1935–36","docAbstract":"

Interest in problems of ground‐water hydrology continues unabated. As proof of this statement it is only necessary to state that of 57 papers listed for presentation at the present annual meeting of the Section of Hydrology and of the Pacific Coast meeting of the Section on January 31 and February 1, 26 papers, or 45 per cent, related to some phase of ground‐water hydrology. In this connection, attention may be called especially to the papers on ground‐water presented at the Pacific Coast meeting and published in the present Transactions.

At this early point in his report, the Chairman should state that at about the time he usually takes the preliminary steps in compiling data for his annual report, his official duties somewhat unexpectedly took him to field‐work in New Mexico and Colorado. Without the usual office facilities it has not been possible for him to make all desired contacts, and the present report of current ground‐water studies is necessarily somewhat incomplete.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00326","usgsCitation":"Thompson, D., 1936, Report of the Committee on Underground Waters, 1935–36: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 326-329, https://doi.org/10.1029/TR017i002p00326.","productDescription":"4 p.","startPage":"326","endPage":"329","costCenters":[],"links":[{"id":378064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David G.","contributorId":8443,"corporation":false,"usgs":true,"family":"Thompson","given":"David G.","affiliations":[],"preferred":false,"id":797808,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221656,"text":"70221656 - 1935 - Further tests of permeability with low hydraulic gradients","interactions":[],"lastModifiedDate":"2021-06-27T15:08:10.582045","indexId":"70221656","displayToPublicDate":"1935-08-01T10:04:26","publicationYear":"1935","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Further tests of permeability with low hydraulic gradients","docAbstract":"

Many of the water‐bearing formations in the United States have hydraulic gradients of much less than 20 feet to the mile, and some may have gradients of less than one foot to the mile, whereas most laboratory‐tests of permeability are made with much higher gradients. An investigation was therefore undertaken by the writer, under the direction of 0. E. Meinzer, in the Hydrologic Laboratory of the United States Geological Survey, to determine whether Darcy's law is valid for very low hydraulic gradients—that is, whether under such low gradients the rate of flow remains proportional to the gradient. In a previous paper by Meinzer and the writer (Amer. Geophysical Union,15th annual meeting, pp.405–409, 1934), it was shown that for the sand tested the rate of flow varies directly with the hydraulic gradient down to a gradient of about one foot to the mile. More recently six additional tests have been made on this sand with the same apparatus, and these tests give evidence of the validity of Darcy's law for still lower gradients.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR016i002p00499","usgsCitation":"Fishel, V., 1935, Further tests of permeability with low hydraulic gradients: Eos, Transactions, American Geophysical Union, v. 16, no. 2, p. 499-503, https://doi.org/10.1029/TR016i002p00499.","productDescription":"5 p.","startPage":"499","endPage":"503","costCenters":[],"links":[{"id":386779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":818359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221655,"text":"70221655 - 1935 - The Piezometric surface of artesian water in the Florida peninsula","interactions":[],"lastModifiedDate":"2021-06-27T15:02:05.946659","indexId":"70221655","displayToPublicDate":"1935-08-01T09:58:17","publicationYear":"1935","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The Piezometric surface of artesian water in the Florida peninsula","docAbstract":"

The ground‐water of the Florida Peninsula constitutes one of its most valuable natural resources and is of importance as a source of water‐supplies throughout the area. The problems relating to the development of ground‐water supplies are both quantitative and qualitative. They include such problems as the decline in yield of wells in areas of large withdrawals of water and salt‐water contamination of ground‐water supplies. In order to facilitate a better understanding and interpretation of hydrologic conditions relating to these local ground‐water problems, a general survey of the artesian water in the Florida Peninsula was made by the United States Geological Survey in 1934.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR016i002p00524","usgsCitation":"Stringfield, V.T., 1935, The Piezometric surface of artesian water in the Florida peninsula: Eos, Transactions, American Geophysical Union, v. 16, no. 2, p. 524-529, https://doi.org/10.1029/TR016i002p00524.","productDescription":"6 p.","startPage":"524","endPage":"529","costCenters":[],"links":[{"id":386778,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.8466796875,\n 24.607069137709683\n ],\n [\n -78.837890625,\n 24.607069137709683\n ],\n [\n -78.837890625,\n 31.052933985705163\n ],\n [\n -87.8466796875,\n 31.052933985705163\n ],\n [\n -87.8466796875,\n 24.607069137709683\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":818358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221680,"text":"70221680 - 1934 - Report of the committee on underground‐water, 1933–34","interactions":[],"lastModifiedDate":"2021-06-28T16:41:37.218356","indexId":"70221680","displayToPublicDate":"1934-06-01T11:39:10","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the committee on underground‐water, 1933–34","docAbstract":"

The by‐laws adopted at the meeting of the Section of Hydrology in 1933 provided that the membership of research committees should be reconstituted every three years. There have, accordingly, been some changes in the membership of the Committee on Underground‐Water. Certain members have retired because of pressure of other duties or because they are no longer actively engaged in ground‐water work. Dr. O. E. Meinzer, who retired as Chairman of the Section of Hydrology, has agreed to serve on the Committee, and probably two or three other men will be appointed to make contact with special phases of the field covered by the Committee. It is with regret that the Chairman reports the loss to the Committee by the death of A. F. Melcher, who had contributed much to the science of ground‐water hydrology by his studies on permeability and absorption of sedimentary formations for water, oil, and gas. ©1934

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00312","usgsCitation":"Thompson, D.G., 1934, Report of the committee on underground‐water, 1933–34: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 312-316, https://doi.org/10.1029/TR015i002p00312.","productDescription":"5 p.","startPage":"312","endPage":"316","costCenters":[],"links":[{"id":386806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221673,"text":"70221673 - 1934 - Appendix A—permeability","interactions":[],"lastModifiedDate":"2021-06-28T15:56:06.937317","indexId":"70221673","displayToPublicDate":"1934-06-01T10:52:41","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix A—permeability","docAbstract":"

In the paper entitled “The measurement of the permeability of porous media for homogeneous fluids” by R. D. Wyckoff and others [42] a unit of permeability is proposed which is based on centimeters, seconds, and atmospheres of pressure (76 centimeters of mercury).

In 1923, when the Hydrologic Laboratory of the United States Geological Survey was organized, much study was given to the question of a coefficient of permeability, and a coefficient was adopted which is based on feet and gallons a day (U.S. Geol. Survey Water-Supply Paper 596, p. 148). This coefficient has been extensively used and has proved very satisfactory in ground-water work. It has the merit of being readily applicable to field-conditions. It is, moreover, of convenient size, the coefficients of most water-bearing materials being integers of two or three figures, that is, between 10 and 1000. It was adopted in place of Slichter's “transmission-constant” (U.S. Geol. Survey Water-Supply Paper 67, p. 27, 1902), after much careful consideration, largely because the “transmission-constant” of most water-bearing materials is inconvenient in being only a small decimal.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00316","usgsCitation":"Meinzer, O.E., 1934, Appendix A—permeability: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 316-317, https://doi.org/10.1029/TR015i002p00316.","productDescription":"2 p.","startPage":"316","endPage":"317","costCenters":[],"links":[{"id":386798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221668,"text":"70221668 - 1934 - Appendix C—A selected list of papers relating to ground‐water hydrology","interactions":[],"lastModifiedDate":"2021-06-29T14:00:10.563864","indexId":"70221668","displayToPublicDate":"1934-06-01T09:04:11","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix C—A selected list of papers relating to ground‐water hydrology","docAbstract":"

In the following list brief statements have been added to certain references to call attention to special phases of ground‐water problems which are not apparent from the titles. Abstracts of most of these papers have been or will be published in the Annotated Bibliography of Economic Geology. 

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00318","usgsCitation":"Sayre, A., 1934, Appendix C—A selected list of papers relating to ground‐water hydrology: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 318-320, https://doi.org/10.1029/TR015i002p00318.","productDescription":"3 p.","startPage":"318","endPage":"320","costCenters":[],"links":[{"id":386848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":818496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221667,"text":"70221667 - 1934 - Appendix B—Lake and ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-28T14:02:22.088463","indexId":"70221667","displayToPublicDate":"1934-06-01T08:58:02","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix B—Lake and ground‐water levels","docAbstract":"

An outstanding achievement of the Section of Hydrology has been the work of the Committee on Glaciers in assembling the existing records of the advance and retreat of the glaciers in the Western States and in Alaska, encouraging various agencies in making periodic observations, systematizing and standardizing the work, and providing for the compilation and preservation of the data obtained from year to year.

The fluctuation of lake levels is a closely related subject that is equally fundamental in the study of hydrology. In 1922 I published a map giving the distribution of 68 Pleistocene lakes in the Basin and Range province and showed that the desiccation of these lakes could have been caused by change in temperature as well as change in precipitation (Geol. Soc. Amer. Bull., v. 33. pp. 541–552. 1922). Abundant and convincing evidences of changes in climate in the Pleistocene epoch or at its end are afforded both by the ancient drift-sheets and by the ancient lake features, but the question as to the relative importance of changes in temperature and changes in precipitation is still very obscure.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00317","usgsCitation":"Meinzer, O.E., 1934, Appendix B—Lake and ground‐water levels: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 317-318, https://doi.org/10.1029/TR015i002p00317.","productDescription":"2 p.","startPage":"317","endPage":"318","costCenters":[],"links":[{"id":386792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"western United States and Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -166.46484375,\n 57.51582286553883\n ],\n [\n -135.87890625,\n 57.51582286553883\n ],\n [\n -135.87890625,\n 70.72897946208789\n ],\n [\n -166.46484375,\n 70.72897946208789\n ],\n [\n -166.46484375,\n 57.51582286553883\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -125.5078125,\n 32.84267363195431\n ],\n [\n -109.3359375,\n 32.84267363195431\n ],\n [\n -109.3359375,\n 48.80686346108517\n ],\n [\n -125.5078125,\n 48.80686346108517\n ],\n [\n -125.5078125,\n 32.84267363195431\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221749,"text":"70221749 - 1933 - Specific yield determined from a Thiem's Pumping‐Test","interactions":[],"lastModifiedDate":"2021-06-30T18:55:53.005509","indexId":"70221749","displayToPublicDate":"1933-06-01T13:52:40","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Specific yield determined from a Thiem's Pumping‐Test","docAbstract":"

The specific yield of a water-bearing formation is defined as the ratio of (1) the volume of water, which after being saturated, it will yield by gravity to (2) its own volume (O. E. Meinzer, Outline of ground-water hydrology, U.S. Geol. Sur. Water-Supply Paper 494, p. 28, 1923). It is a measure of the quantity of water that a formation will yield when it is drained by lowering of the water-table. The determination of the specific yield is essential in many quantitative ground-water investigations.

In 1931 a pumping-test was made in the Platte River Valley, in Nebraska, to determine by Thiem's method the permeability of the water-bearing sand and gravel that underlie the Valley. This test, which constitutes a part of a cooperative investigation by the Conservation and Survey Department of the University of Nebraska and the United States Geological Survey, was briefly described in the 1932 Transactions of the American Geophysical Union (p. 393). The well was pumped continuously for 48 hours, and measurements of the discharge were made every 30 minutes. During the period of pumping and after pumping stopped about 5,000 measurements were made of the depths to the water-surfaces in 80 observation-wells, which were located on lines radiating from the pumped well to distances up to 1,200 feet. Instrumental levels were run to the measuring points on each of the wells so that the altitudes of the water-surfaces could be determined for any time. From the data obtained in this test the average coefficient of permeability was computed to be about 700. In the present paper a method is presented for determining the specific yield of the water-bearing material from the data collected in this test, and the results of the computations are given. This method for determining specific yield was suggested by Meinzer (O. E. Meinzer, Outline of methods for estimating ground-water supplies, U.S. Geol. Sur. water-Supply Paper 638-c, p. 136, 1932).

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00475","usgsCitation":"Wenzel, L., 1933, Specific yield determined from a Thiem's Pumping‐Test: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 475-477, https://doi.org/10.1029/TR014i001p00475.","productDescription":"3 p.","startPage":"475","endPage":"477","costCenters":[],"links":[{"id":386909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":818608,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221745,"text":"70221745 - 1933 - Geophysical interpretation of ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-30T16:31:51.062153","indexId":"70221745","displayToPublicDate":"1933-06-01T11:28:11","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical interpretation of ground‐water levels","docAbstract":"

The theory of rock‐pressure as a cause of artesian‐head dates back at least to early Grecian times. Thus the philosopher Thales, about 600 B.C., taught that the springs derive their water from the ocean through subterranean channels and that the water is lifted to the springs by rook‐pressure. The theory of rock‐pressure has had a number of recent advocates, chief among whom was the British geologist, J. W. Gregory, but apparently no effective attempt was made by any of them to apply critical data to the problem. In general, geologists and hydrologists have rejected rock‐pressure as a vague heresy and have assumed that the artesian formations function as perfectly rigid and inert containers, not recognizing the fact that the data in regard to the performance of wells appear to conflict with such an interpretation. 

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00036","usgsCitation":"Meinzer, O.E., 1933, Geophysical interpretation of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 36-37, https://doi.org/10.1029/TR014i001p00036.","productDescription":"2 p.","startPage":"36","endPage":"37","costCenters":[],"links":[{"id":386904,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221744,"text":"70221744 - 1933 - Some relations between ground‐water hydrology and oceanography","interactions":[],"lastModifiedDate":"2021-06-30T16:23:44.914113","indexId":"70221744","displayToPublicDate":"1933-06-01T11:19:31","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Some relations between ground‐water hydrology and oceanography","docAbstract":"

In many areas along the sea-coasts of the world the water-supply for human use is derived largely, and in some areas wholly, from underground sources. Because of the proximity to the ocean in these areas, in some respects the geologic and hydrologic conditions that govern the occurrence and movement of ground-water are quite different from those in inland areas, and to properly interpret them the ground-water hydrologist must avail himself of facts developed by the oceanographer.

These conditions are encountered in a marginal zone that in different localities may extend only a few feet or many miles inland from the coast, and presumably for greater or less distances out beneath the ocean. These special conditions have been recognized and extensively studied for many years, for example, in the lowland-area of Holland that lies between the Zuider Zee and the North Sea, and on Long Island, New York. Within recent years more or less attention has been given to these conditions in many of the coastal states of the United States, and in the Hawaiian Islands and Cuba. It is the purpose of this statement to indicate some of the problems of groundwater hydrology that are related to oceanography.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00030","usgsCitation":"Thompson, D., 1933, Some relations between ground‐water hydrology and oceanography: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 30-33, https://doi.org/10.1029/TR014i001p00030.","productDescription":"4 p.","startPage":"30","endPage":"33","costCenters":[],"links":[{"id":386903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David G.","contributorId":8443,"corporation":false,"usgs":true,"family":"Thompson","given":"David G.","affiliations":[],"preferred":false,"id":818603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221743,"text":"70221743 - 1933 - Deep‐well salinity‐exploration","interactions":[],"lastModifiedDate":"2021-06-30T16:05:47.249003","indexId":"70221743","displayToPublicDate":"1933-06-01T11:00:20","publicationYear":"1933","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Deep‐well salinity‐exploration","docAbstract":"

One of the outstanding accomplishments of recent years in connection with the study of the geologic source of groundwater and the quality of water yielded by different formations has been the development of methods and equipment for the exploration of wells. The description and use of the deep‐well current‐meter on well‐exploration work in Hawaii and New Mexico has already appeared in published literature (John McCombs and A. G. Fiedler, Methods of exploring and repairing leaky artesian wells, U.S. Geol. Sur. Water‐Supply Paper 596, pp. 1–32, 1928) on hydrology but recent developments in the application of electrical conductivity‐measurements for determining the salinity of water in wells have not heretofore been presented. In addition to being of considerable scientific importance in connection with problems of ground‐water hydrology, the practical value of locating the place at which salt water is entering a well and contaminating a potable water‐supply is great. Such information may be the means of preventing the loss of large investments in industries, irrigation‐projects, and cities that are dependent upon well‐water supplies that may at some time become contaminated by salty or other highly mineralized water. 

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00478","usgsCitation":"Fiedler, A., 1933, Deep‐well salinity‐exploration: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 478-480, https://doi.org/10.1029/TR014i001p00478.","productDescription":"3 p.","startPage":"478","endPage":"480","costCenters":[],"links":[{"id":386902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada, Hawaii","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.984375,\n 31.42866311735861\n ],\n [\n -103.22753906249999,\n 31.42866311735861\n ],\n [\n -103.22753906249999,\n 37.09023980307208\n ],\n [\n -108.984375,\n 37.09023980307208\n ],\n [\n -108.984375,\n 31.42866311735861\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -161.54296875,\n 18.396230138028827\n ],\n [\n -151.875,\n 18.396230138028827\n ],\n [\n -151.875,\n 23.483400654325642\n ],\n [\n -161.54296875,\n 23.483400654325642\n ],\n [\n -161.54296875,\n 18.396230138028827\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fiedler, A.G.","contributorId":11272,"corporation":false,"usgs":true,"family":"Fiedler","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":818602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","interactions":[{"subject":{"id":25079,"text":"wsp638A - 1932 - A preliminary report on the artesian water supply of Memphis, Tennessee","indexId":"wsp638A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A preliminary report on the artesian water supply of Memphis, Tennessee"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":1},{"subject":{"id":25080,"text":"wsp638B - 1932 - Water-power resources of the Rogue River drainage basin, Oregon","indexId":"wsp638B","publicationYear":"1932","noYear":false,"chapter":"B","title":"Water-power resources of the Rogue River drainage basin, Oregon"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":2},{"subject":{"id":25081,"text":"wsp638C - 1932 - Outline of methods for estimating ground-water supplies","indexId":"wsp638C","publicationYear":"1932","noYear":false,"chapter":"C","title":"Outline of methods for estimating ground-water supplies"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":3},{"subject":{"id":25082,"text":"wsp638D - 1932 - Quality of water of the Colorado River in 1928-1930","indexId":"wsp638D","publicationYear":"1932","noYear":false,"chapter":"D","title":"Quality of water of the Colorado River in 1928-1930"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":4}],"lastModifiedDate":"2024-02-05T21:21:47.532833","indexId":"wsp638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1932","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":"638","title":"Contributions to the hydrology of the United States 1931","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp638","usgsCitation":"Grover, N., 1932, Contributions to the hydrology of the United States 1931: U.S. Geological Survey Water Supply Paper 638, v, 162 p., https://doi.org/10.3133/wsp638.","productDescription":"v, 162 p.","costCenters":[],"links":[{"id":30204,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0638/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139042,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0638/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691299","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":146441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","interactions":[{"subject":{"id":25083,"text":"wsp659A - 1932 - A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","indexId":"wsp659A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah"},"predicate":"IS_PART_OF","object":{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","indexId":"wsp659","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States, 1932"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1932","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":"659","title":"Contributions to the hydrology of the United States, 1932","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey,","doi":"10.3133/wsp659","usgsCitation":"Grover, N., 1932, Contributions to the hydrology of the United States, 1932: U.S. Geological Survey Water Supply Paper 659, v, 209 p. :ill., maps (2 maps in pocket) ;23 cm., https://doi.org/10.3133/wsp659.","productDescription":"v, 209 p. :ill., maps (2 maps in pocket) ;23 cm.","costCenters":[],"links":[{"id":137070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0659/report-thumb.jpg"},{"id":26547,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0659/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26548,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0659/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0659/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68be27","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":143744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25083,"text":"wsp659A - 1932 - A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","interactions":[{"subject":{"id":25083,"text":"wsp659A - 1932 - A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","indexId":"wsp659A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah"},"predicate":"IS_PART_OF","object":{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","indexId":"wsp659","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States, 1932"},"id":1}],"isPartOf":{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","indexId":"wsp659","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States, 1932"},"lastModifiedDate":"2023-09-21T21:11:59.936443","indexId":"wsp659A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1932","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":"659","chapter":"A","title":"A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","docAbstract":"

Fluctuations of water levels in wells, if critically studied, may give much information as to the occurrence, movement, and quantity of available ground water. In some localities the ground-water level has been observed to decline during the day and to rise at night, the decline beginning at about the same hour every morning and the rise at about the same hour every night. This daily decline is due to the withdrawal of ground water from the zone of saturation by plants, and the rise at night is due to upward movement of water under slight artesian pressure from permeable beds of sand and gravel at some depth beneath the water table.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1932 (Water Supply Paper 659)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp659A","usgsCitation":"White, W.N., 1932, A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah: U.S. Geological Survey Water Supply Paper 659, Report: 105 p.; 1 Plate: 14.65 x 21.52 inches, https://doi.org/10.3133/wsp659A.","productDescription":"Report: 105 p.; 1 Plate: 14.65 x 21.52 inches","numberOfPages":"115","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":421031,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24621.htm","linkFileType":{"id":5,"text":"html"}},{"id":54081,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0659a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264574,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0659a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156866,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0659a/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Escalante Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.69688804144857,\n 37.53657815987634\n ],\n [\n -113.16519847993968,\n 37.662594400449564\n ],\n [\n -112.86981539021227,\n 37.91040066781825\n ],\n [\n -112.86981744366477,\n 38.42843951649698\n ],\n [\n -112.87890615411786,\n 38.62042242875168\n ],\n [\n -113.51057153061132,\n 38.517384159387944\n ],\n [\n -113.92410785622891,\n 37.81712147838752\n ],\n [\n -113.69688804144857,\n 37.53657815987634\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae054","contributors":{"authors":[{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":193180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220411,"text":"70220411 - 1932 - Investigations of underground water problems in Arizona, California, New Mexico, and Oregon","interactions":[],"lastModifiedDate":"2021-05-12T12:34:20.907919","indexId":"70220411","displayToPublicDate":"1932-05-12T07:26:58","publicationYear":"1932","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Investigations of underground water problems in Arizona, California, New Mexico, and Oregon","docAbstract":"

This report is a summary of investigations in progress in 1932 in the southwestern portion of the United States. It covers only those investigations that deal with water in the zone of saturation, and excludes those that deal primarily with water in the zone of aeration. Arizona H. C. Schwalen, Irrigation Engineer, Agricultural Experiment‐Station, Tucson, Arizona, has proposed to undertake a study of the effect of pumping from wells, and of the capacity of water‐bearing strata, but no report of progress is available. Several other hydrologic investigations are now being made by the Agricultural Experiment‐ Station, but relate primarily to infiltration and transpiration.

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It is doubtless known to many members of the Section of Hydrology that prior to the World War there existed an International Glacier Commission (la Commission Internationale des Glaciers) whose self‐appointed task it was to gather and publish the results of all available measurements showing the annual variations in length—advance or recession—of glaciers in different parts of the world. On this Commission the United States was represented by two men who made frequent contributions to the International record.

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It is doubtless known to many members of the Section of Hydrology that prior to the World War there existed an International Glacier Commission (la Commission Internationale des Glaciers) whose self‐appointed task it was to gather and publish the results of all available measurements showing the annual variations in length—advance or recession—of glaciers in different parts of the world. On this Commission the United States was represented by two men who made frequent contributions to the International record.

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This report gives the results obtained in the continuation of a study of the Colorado River begun in 1925.1 Most of the analyses here given represent composites of daily samples collected by the observers at the gaging stations on the Colorado River at Grand Canyon, Topock, and Yuma, Ariz. The other samples analyzed were taken at Lees Ferry and on tributaries of the Colorado. These stations are operated under the direction of W. E. Dickinson, district engineer of the Geological Survey at Tucson, Ariz., who personally collected some of the samples at other points and arranged for the collection of others. The average discharges in Table 2 were calculated from data furnished by W. E. Dickinson. Complete discharge data for this period will be published in the regular series of water-supply papers.

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Determinations of the quantity of solid material carried by the Colorado River are necessary for the proper consideration of plans for the development of the resources of the river. Much of the material carried by the river will be deposited in the proposed reservoirs and eventually will occupy a large part of the capacity of the reservoirs, so that their effectiveness for flood control or river regulation will be greatly decreased. A capacity of 6,000,000 acre-feet is reserved for silt storage in plans for a reservoir in Boulder Canyon that is to have a maximum capacity of about 25,000,000 to 30,000,000 acre-feet. It has been estimated that such a silt-storage capacity will not be entirely used for nearly 100 years.1 However, the discharge of sediment including the sediment from the Gila was reported to be more than 1,000,000 acre-feet for the four years 1909-19122 and a similar quantity for the four years 1912-1916.3

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