{"pageNumber":"7226","pageRowStart":"180625","pageSize":"25","recordCount":185258,"records":[{"id":70213863,"text":"70213863 - 1940 - Salinity of the lower Savannah River in relation to stream‐flow and tidal action","interactions":[],"lastModifiedDate":"2020-09-18T20:53:55.899578","indexId":"70213863","displayToPublicDate":"1940-09-18T14:35:06","publicationYear":"1940","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":"Salinity of the lower Savannah River in relation to stream‐flow and tidal action","docAbstract":"

In order to obtain information needed in planning for industrial development along the Savannah River and in the city of Savannah, Georgia, a study of the salinity of the Savannah River was undertaken by the Geological Survey, United States Department of the Interior, in cooperation with the Georgia Division of Mines, Mining, and Geology. The Works Progress Administration of Georgia and the city of Savannah also cooperated in the study.

The Savannah River lies on the boundary between the States of Georgia and South Carolina. The River proper from the mouth to the junction of the Tugaloo and Senaca rivers is 314 miles in length. The area of its watershed is about 10,579 square miles, of which 9,850 square miles are above the stream‐flow gaging‐station near Clyo, Georgia. The River is tidal for about 50 miles above its mouth. The average streamflow for the Savannah River near Clyo, Georgia, was 10,410 and 10,820 second‐feet, respectively, for the years ending September 30, 1938 and 1939. The city of Savannah, Georgia, located on the Savannah River 17 miles above its mouth, is an important seaport and industrial center. The lower Savannah River near the city of Savannah is shown in Figure 1.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00463","usgsCitation":"Lamar, W.L., 1940, Salinity of the lower Savannah River in relation to stream‐flow and tidal action: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 463-470, https://doi.org/10.1029/TR021i002p00463.","productDescription":"8 p.","startPage":"463","endPage":"470","costCenters":[],"links":[{"id":378578,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia, South Carolina","otherGeospatial":"Savannah River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.14227294921875,\n 31.962648655655887\n ],\n [\n -80.81954956054688,\n 31.962648655655887\n ],\n [\n -80.81954956054688,\n 32.19304652202036\n ],\n [\n -81.14227294921875,\n 32.19304652202036\n ],\n [\n -81.14227294921875,\n 31.962648655655887\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lamar, William L.","contributorId":15592,"corporation":false,"usgs":true,"family":"Lamar","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":799250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213853,"text":"70213853 - 1940 - On the flow of water in an elastic artesian aquifer","interactions":[],"lastModifiedDate":"2020-09-18T19:33:42.068559","indexId":"70213853","displayToPublicDate":"1940-09-18T14:23:23","publicationYear":"1940","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":"On the flow of water in an elastic artesian aquifer","docAbstract":"

Slichter showed in 1898 that a solution may be obtained for a given problem in the steady motion of ground‐water by solving the familiar Laplace equation and that therefore in steady‐state conditions a problem in the motion of ground‐water is mathematically analogous to a problem in the steady flow of heat or electricity [see 1 of “References” at end of paper]. More recently it has been recognized that the analogy holds also for the non‐steady‐state flow of compressible liquids, in elastic systems as well as in rigid systems.

In studying the effect of the discharge of flowing wells on the head in the Dakota sandstone, Meinzer [2, 3] concluded that the water discharged by the wells had largely been derived locally from storage. It was found that the amount of water withdrawn from storage could not be accounted for on the basis of the compressibility of water alone but that it might be accounted for on the basis of the probable compressibility of the sandstone itself. Prior to that time, estimates of water‐supplies from artesian aquifers had been based upon the assumption that artesian aquifers are perfectly incompressible and inelastic However, as Meinzer states [2, p. 289], “artesian aquifers are apparently all more or less compressible and elastic though they differ widely in the degree and relative importance of these properties. In general, the properties of compressibility and elasticity are of the most consequence in aquifers that have low permeability, slow recharge, and high head.”

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00574","usgsCitation":"Jacob, C.E., 1940, On the flow of water in an elastic artesian aquifer: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 574-586, https://doi.org/10.1029/TR021i002p00574.","productDescription":"13 p.","startPage":"574","endPage":"586","costCenters":[],"links":[{"id":378577,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":799249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213852,"text":"70213852 - 1940 - Additional evidence on the relation of temperature to structure in the Salt Creek Oil field, Natrona County, Wyoming ","interactions":[],"lastModifiedDate":"2020-09-18T20:55:35.527682","indexId":"70213852","displayToPublicDate":"1940-09-18T14:17:56","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Additional evidence on the relation of temperature to structure in the Salt Creek Oil field, Natrona County, Wyoming ","docAbstract":"

Observations of bottom hole temperatures in approximately 100 deep wells in the Salt Creek field have been made during the past few years by the Stanolind Oil and Gas Company. These recent observations confirm and extend in a remarkable manner the results obtained in the summers of 1922 and 1923  when it was found from temperature surveys in 21 wells that the temperatures over a considerable portion of the field were definitely related to the structure.

","language":"English","publisher":"Society of Economic Geophysicists","doi":"10.1190/1.1441793","usgsCitation":"Van Orstrand, C.E., 1940, Additional evidence on the relation of temperature to structure in the Salt Creek Oil field, Natrona County, Wyoming : Geophysics, v. 5, no. 1, p. 47-56, https://doi.org/10.1190/1.1441793.","productDescription":"10 p.","startPage":"47","endPage":"56","costCenters":[],"links":[{"id":378576,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Natrona County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-107.1077,43.4996],[-107.1078,43.4942],[-107.0478,43.4947],[-107.0144,43.4949],[-106.9014,43.4949],[-106.8743,43.4951],[-106.8333,43.4943],[-106.774,43.4942],[-106.5948,43.4938],[-106.5569,43.4938],[-106.5152,43.4938],[-106.502,43.4941],[-106.4824,43.4939],[-106.4629,43.4941],[-106.4433,43.4939],[-106.4042,43.4944],[-106.3884,43.4937],[-106.3284,43.4943],[-106.3089,43.4945],[-106.2887,43.4943],[-106.2477,43.4942],[-106.0671,43.4944],[-106.0671,43.4734],[-106.0683,43.387],[-106.0687,43.3706],[-106.0696,43.3415],[-106.0705,43.2851],[-106.0709,43.271],[-106.0711,43.241],[-106.0715,43.2268],[-106.0717,43.154],[-106.0721,43.1395],[-106.072,43.0972],[-106.0724,43.0826],[-106.0724,43.039],[-106.0722,43.0235],[-106.0726,43.0089],[-106.0699,42.8588],[-106.0684,42.7792],[-106.0765,42.7789],[-106.0753,42.6643],[-106.0755,42.5898],[-106.0753,42.5752],[-106.075,42.5193],[-106.0735,42.4611],[-106.0749,42.4325],[-106.1054,42.4325],[-106.1228,42.4323],[-106.1265,42.4328],[-106.1464,42.4326],[-106.239,42.4321],[-106.2471,42.4317],[-106.2651,42.4315],[-106.3235,42.4314],[-106.3434,42.4312],[-106.3546,42.4309],[-106.3658,42.431],[-106.4323,42.4305],[-106.4435,42.4306],[-106.474,42.4305],[-106.4814,42.4306],[-106.5137,42.431],[-106.5336,42.4312],[-106.592,42.4314],[-106.6007,42.4315],[-106.6088,42.4311],[-106.6187,42.4312],[-106.6864,42.4315],[-106.7076,42.4317],[-106.7169,42.4322],[-106.738,42.4324],[-106.7834,42.4324],[-106.7958,42.4325],[-106.8219,42.4328],[-106.8362,42.4324],[-106.8492,42.4321],[-106.8642,42.4322],[-106.8747,42.4323],[-106.9387,42.4333],[-106.9412,42.4333],[-106.9455,42.4334],[-106.9574,42.433],[-106.9704,42.4331],[-107.0742,42.4343],[-107.0934,42.4345],[-107.173,42.4346],[-107.1916,42.4347],[-107.2885,42.4343],[-107.3084,42.4349],[-107.3457,42.4346],[-107.3873,42.4344],[-107.4041,42.4345],[-107.4234,42.4341],[-107.4426,42.4342],[-107.5209,42.4336],[-107.5408,42.4332],[-107.5414,42.4473],[-107.5412,42.465],[-107.5412,42.4791],[-107.5411,42.4918],[-107.5415,42.5182],[-107.5421,42.52],[-107.542,42.5341],[-107.5419,42.5486],[-107.5416,42.5932],[-107.5422,42.6077],[-107.5421,42.6222],[-107.542,42.635],[-107.5418,42.6568],[-107.5416,42.6968],[-107.5415,42.7113],[-107.5429,42.7813],[-107.4992,42.7812],[-107.4989,42.8244],[-107.4994,42.8394],[-107.4993,42.8539],[-107.4998,42.8676],[-107.4995,42.9108],[-107.4999,42.9403],[-107.4998,42.9567],[-107.502,42.9995],[-107.5025,43.014],[-107.5024,43.0286],[-107.5017,43.0431],[-107.4941,43.1295],[-107.5142,43.1296],[-107.5131,43.2024],[-107.513,43.2146],[-107.5127,43.2551],[-107.5124,43.2993],[-107.5121,43.342],[-107.5114,43.3566],[-107.5124,43.3862],[-107.5108,43.428],[-107.5105,43.4722],[-107.5351,43.4718],[-107.5343,43.4991],[-107.5116,43.4995],[-107.4914,43.4994],[-107.4731,43.4998],[-107.4504,43.4997],[-107.3513,43.4988],[-107.2314,43.5],[-107.203,43.4998],[-107.1847,43.4997],[-107.1456,43.4994],[-107.1077,43.4996]]]},\"properties\":{\"name\":\"Natrona\",\"state\":\"WY\"}}]}","volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Van Orstrand, C. E.","contributorId":37231,"corporation":false,"usgs":true,"family":"Van Orstrand","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":799248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213842,"text":"70213842 - 1940 - A brief review of ground‐water conditions in Michigan","interactions":[],"lastModifiedDate":"2020-09-18T20:57:02.601391","indexId":"70213842","displayToPublicDate":"1940-09-18T13:59:19","publicationYear":"1940","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":"A brief review of ground‐water conditions in Michigan","docAbstract":"

The State of Michigan makes up about one‐half of the area of the great Michigan Synclinal Basin, the remainder of which embraces Lakes Michigan and Huron and small parts of Wisconsin, Illinois, Indiana, Ohio, and Ontario [see 1 (p. 7) of “References” at end of paper]. The Basin has characteristics of both a geosyncline and a major structural basin. The geosynclinal origin is indicated by the facts that the Basin has been progressively downwarped, the beds thicken markedly into the central area, the outline of the course of the outcropping rocks is roughly oval, and the minor structures within the Basin are mostly parallel to the longer diameter of the downwarp. Evidence of several periods of isolation and evaporation and the absence of thick series of coarse clastic sediments in the post‐Cambrian rock‐column are features that are more characteristic of structural basins.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i004p01122","usgsCitation":"McGuinness, C., 1940, A brief review of ground‐water conditions in Michigan: Eos, Transactions, American Geophysical Union, v. 21, no. 4, p. 1122-1126, https://doi.org/10.1029/TR021i004p01122.","productDescription":"5 p.","startPage":"1122","endPage":"1126","costCenters":[],"links":[{"id":378575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"McGuinness, Charles L.","contributorId":32902,"corporation":false,"usgs":true,"family":"McGuinness","given":"Charles L.","affiliations":[],"preferred":false,"id":799247,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213832,"text":"70213832 - 1940 - The contamination of ground‐water by salt water near Parlin, New Jersey","interactions":[],"lastModifiedDate":"2020-09-18T20:58:18.757831","indexId":"70213832","displayToPublicDate":"1940-09-18T13:49:11","publicationYear":"1940","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 contamination of ground‐water by salt water near Parlin, New Jersey","docAbstract":"

The classic studies of Badon Ghyben [see 1 of “References” at end of paper] and Alexander Herzoerg [2].that defined the basic principles governing the relation between salt water and fresh water in water‐bearing sands are now fairly well known. They showed that fresh water floats on the heavier salt Water and that, under static conditions, the ratio between the head of the fresh water above mean sea‐level and the depth of the contact between fresh and salt water below mean sea‐level, is determined by the relative specific gravities of the two waters. Other studies have shown that under ordinary conditions there is little mixing between the fresh and salt waters, so that the zone of contact is narrow. Instances have been observed in which the chloride‐content of the water has ranged from a few parts to several thousand parts per million within a few feet. It would seem, therefore, that the basic conditions under which fresh and salt water occur together in water‐bearing sands are somewhat similar to those in the tidal estuaries of streams. The principal differences are caused by the frictional resistance of the sand which prevents rapid movements of both fluids and probably retards their mixing.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00471","usgsCitation":"Barksdale, H., 1940, The contamination of ground‐water by salt water near Parlin, New Jersey: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 471-474, https://doi.org/10.1029/TR021i002p00471.","productDescription":"4 p.","startPage":"471","endPage":"474","costCenters":[],"links":[{"id":378574,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","city":"Parlin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.41280364990234,\n 40.44093755756703\n ],\n [\n -74.33624267578125,\n 40.44093755756703\n ],\n [\n -74.33624267578125,\n 40.492653934148\n ],\n [\n -74.41280364990234,\n 40.492653934148\n ],\n [\n -74.41280364990234,\n 40.44093755756703\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Barksdale, H.C.","contributorId":65912,"corporation":false,"usgs":true,"family":"Barksdale","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":799246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213822,"text":"70213822 - 1940 - Ground‐water recharge in areas of deep water‐table in the Great Plains","interactions":[],"lastModifiedDate":"2020-09-18T21:00:35.5027","indexId":"70213822","displayToPublicDate":"1940-09-18T13:41:29","publicationYear":"1940","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":"Ground‐water recharge in areas of deep water‐table in the Great Plains","docAbstract":"

It is unanimously agreed, I think, that of the water which falls upon the Earth's surface, a part runs off toward the sea, a part is at least temporarily detained, a part of it evaporates, and a part sinks beneath the ground‐surface. But among students of that water which sinks beneath the Earth's surface, complete agreement as to the course it then takes has not always prevailed. Ground‐water hydrologists have assumed that water can and does reach the water‐table by descending through a great thickness of subsoil in the semi‐arid upland divides of the Great Plains. But many students of soil‐moisture and its use by vegetation in the Great Plains have concluded from their soil‐moisture sampling that water does not descend to the water‐table where the depth to the water‐table is great. Thus Cole and Mathews state in Technical Bulletin 637 of the United States Department of Agriculture, page 69, that “It can be safely said, however, that on the short‐grass land of the Great Plains there is no penetration of upland surface‐water to the water‐table.”

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00570","usgsCitation":"Cady, R., 1940, Ground‐water recharge in areas of deep water‐table in the Great Plains: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 570-574, https://doi.org/10.1029/TR021i002p00570.","productDescription":"5 p.","startPage":"570","endPage":"574","costCenters":[],"links":[{"id":378573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Box Butte County, Keith County","otherGeospatial":"Great Plains","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-102.7742,42.4402],[-102.7499,42.4394],[-102.7498,42.3576],[-102.7477,42.3531],[-102.7476,42.2708],[-102.7428,42.1809],[-102.7431,42.0923],[-102.7035,42.0922],[-102.6989,42.0051],[-102.8149,42.0026],[-102.936,42.0022],[-103.0521,42.0027],[-103.1689,42.0021],[-103.3605,42.0037],[-103.3995,42.004],[-103.4012,42.0903],[-103.4457,42.0905],[-103.4438,42.176],[-103.4432,42.2646],[-103.4444,42.4387],[-103.361,42.4377],[-103.2416,42.4376],[-103.0893,42.4381],[-102.8885,42.4391],[-102.7742,42.4402]]],[[[-101.2702,41.3959],[-101.2688,41.0488],[-101.2487,41.0476],[-101.248,41.005],[-101.3618,41.0035],[-102.0504,41.0037],[-102.0505,41.0477],[-102.0542,41.0481],[-102.0556,41.2214],[-102.0551,41.3939],[-101.9853,41.3955],[-101.4055,41.3954],[-101.2702,41.3959]]]]},\"properties\":{\"name\":\"Box Butte\",\"state\":\"NE\"}}]}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Cady, R.C.","contributorId":44905,"corporation":false,"usgs":true,"family":"Cady","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":799245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213812,"text":"70213812 - 1940 - Ground‐water problems in Ohio, with special reference to the industrial area of Cincinnati in Butler and Hamilton counties","interactions":[],"lastModifiedDate":"2020-09-18T21:02:13.937359","indexId":"70213812","displayToPublicDate":"1940-09-18T13:27:42","publicationYear":"1940","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":"Ground‐water problems in Ohio, with special reference to the industrial area of Cincinnati in Butler and Hamilton counties","docAbstract":"

The importance of ground‐water as a natural resource to be used for water‐supply and industrial purposes is often overlooked by the general public. A recent survey conducted by the Engineering News‐Record [see 1 of “References” at end of paper], based on data obtained from State Sanitary engineers, shows that 9,100 out of a total of 12,700 public water‐supply systems in the United States obtain water from underground sources. Of the total population served by public water‐supplies, about 28 per cent or 22,500,000 people are served by systems using ground‐water. In addition to the quantities of water pumped for public supplies, many million gallons of ground‐water are pumped daily for rural, domestic, and industrial purposes. In many of the cities that have public supplies from surface‐sources, there is nevertheless heavy pumping from private wells for industrial purposes.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i004p01126","usgsCitation":"Klaer, F., 1940, Ground‐water problems in Ohio, with special reference to the industrial area of Cincinnati in Butler and Hamilton counties: Eos, Transactions, American Geophysical Union, v. 21, no. 4, p. 1126-1131, https://doi.org/10.1029/TR021i004p01126.","productDescription":"6 p.","startPage":"1126","endPage":"1131","costCenters":[],"links":[{"id":378572,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Klaer, F.H. Jr.","contributorId":85654,"corporation":false,"usgs":true,"family":"Klaer","given":"F.H.","suffix":"Jr.","affiliations":[],"preferred":false,"id":799244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213811,"text":"70213811 - 1940 - Committee on chemistry of natural waters, 1939–40","interactions":[],"lastModifiedDate":"2020-09-18T21:03:03.118227","indexId":"70213811","displayToPublicDate":"1940-09-18T13:16:53","publicationYear":"1940","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":"Committee on chemistry of natural waters, 1939–40","docAbstract":"

The membership of this Committee is as follows: I. A. Dennison, National Bureau of Standards, Washington, D.C.; C. S. Scofield, Bureau of Plant Industry, Department of Agriculture, Washington, D.C.; D. G. Thompson, United States Geological Survey, Washington, D.C.; Prof. T. G. Thompson, University of Washington, Seattle, Washington; and C. S. Howard (Chairman), United States Geological Survey, Washington, D.C.

The Committee arranged for the presentation of the following five papers at the 1940 Spring meeting: (1) Salt‐water intrusion in the Connecticut River, by C. S. Howard, United States Geological Survey; (2) Salinity‐movement and its causes in the Delaware River Estuary, by William D. Mason and Wallace R. Pietsch, Sun Oil Company; (3) Salinity of, lower Savannah River in relation to tidal action and stream‐flow, by William L. Lamar, United States Geological Survey; (4) Corrosion of ferrous and nonferrous metals and the behavior of metallic coatings in tidal marsh, by I. A. Dennison, National Bureau of Standards; (5) The contamination of underground waters by salt water near Parlin, New Jersey, by H. C. Barksdale, United States Geological Survey.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00369","usgsCitation":"Howard, C.S., 1940, Committee on chemistry of natural waters, 1939–40: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 369-370, https://doi.org/10.1029/TR021i002p00369.","productDescription":"2 p.","startPage":"369","endPage":"370","costCenters":[],"links":[{"id":378571,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":799243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213801,"text":"70213801 - 1940 - Determination of Manning's N from vertical‐velocity curves","interactions":[],"lastModifiedDate":"2020-09-18T18:15:55.941693","indexId":"70213801","displayToPublicDate":"1940-09-18T13:12:25","publicationYear":"1940","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":"Determination of Manning's N from vertical‐velocity curves","docAbstract":"

Professor M. P. O'Brien [see 1, 2 of “References” at end of paper] has recently shown that data on the vertical distribution of velocity through the theory of turbulent flow as developed by Prandtl, Von Karman, and others may be applied to the determination of friction‐coefficients in open channels. Hydrographers in making measurements of river‐flow have often noticed that in streams having rough bottoms appreciable difference is generally found between the measured velocity at 0.2‐ and 0.8‐depth. It is satisfying to note that Professor O'Brien's calculations are in accord with these general observations.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00618","usgsCitation":"Langbein, W., 1940, Determination of Manning's N from vertical‐velocity curves: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 618-620, https://doi.org/10.1029/TR021i002p00618.","productDescription":"3 p.","startPage":"618","endPage":"620","costCenters":[],"links":[{"id":378570,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, Walter B.","contributorId":98294,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter B.","affiliations":[],"preferred":false,"id":799242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213800,"text":"70213800 - 1940 - Salt‐water intrusion in the Connecticut River","interactions":[],"lastModifiedDate":"2020-09-18T21:07:43.151931","indexId":"70213800","displayToPublicDate":"1940-09-18T13:01:31","publicationYear":"1940","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":"Salt‐water intrusion in the Connecticut River","docAbstract":"

The intrusion of salt water in the lower Connecticut River Basin was studied during October 1, 1934, to June 30, 1939. The field‐ and laboratory‐work was done as a project of the Works Progress Administration under the sponsorship of the State Water Commission of the State of Connecticut. Some technical assistance was given by the Geological Survey through cooperation with the State Water Commission.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00455","usgsCitation":"Howard, C.S., 1940, Salt‐water intrusion in the Connecticut River: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 355-357, https://doi.org/10.1029/TR021i002p00455.","productDescription":"3 p.","startPage":"355","endPage":"357","costCenters":[],"links":[{"id":378567,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","otherGeospatial":"Connecticut River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.56057739257812,\n 41.25612970800976\n ],\n [\n -72.29141235351561,\n 41.25612970800976\n ],\n [\n -72.29141235351561,\n 41.50034959128928\n ],\n [\n -72.56057739257812,\n 41.50034959128928\n ],\n [\n -72.56057739257812,\n 41.25612970800976\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":799241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213790,"text":"70213790 - 1940 - The evaluation of magnetic anomalies by means of scales","interactions":[],"lastModifiedDate":"2020-09-18T18:00:27.457349","indexId":"70213790","displayToPublicDate":"1940-09-18T12:56:47","publicationYear":"1940","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 evaluation of magnetic anomalies by means of scales","docAbstract":"

At the 1939 meeting of the Union [Fundamental research in geophysics relating to prospecting, Trans. Amer. Geophys. Union, 1939, pp. 302 and 390], the writer described a set of scales for aiding in the evaluation of the magnetic anomaly due to a selected magnetized body. During the past year, these scales have been modified in several minor details. The revised forms are shown by typical scales illustrated in Figure 1.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00319","usgsCitation":"Roman, I., 1940, The evaluation of magnetic anomalies by means of scales: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 319-321, https://doi.org/10.1029/TR021i002p00319.","productDescription":"3 p.","startPage":"319","endPage":"321","costCenters":[],"links":[{"id":378566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Roman, Irwin","contributorId":57834,"corporation":false,"usgs":true,"family":"Roman","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":799240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213789,"text":"70213789 - 1940 - Committee on glaciers, 1939–40","interactions":[],"lastModifiedDate":"2020-09-18T21:08:36.376557","indexId":"70213789","displayToPublicDate":"1940-09-18T12:20:09","publicationYear":"1940","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":"Committee on glaciers, 1939–40","docAbstract":"

The Committee on Glaciers is now composed of the following members: Harry Fielding Reid, Professor Emeritus of Geology, Johns Hopkins University, 608 Cathedral Street, Baltimore, Maryland; William H. Hobbs, Professor Emeritus of Geology, University of Michigan, Ann Arbor, Michigan; Lawrence Martin, Chief of the Division of Maps, Library of Congress, Washington, D.C.; J. E. Church, Professor of Meteorology, Agricultural Experiment Station, University of Nevada, Reno, Nevada; Wm. Osgood Field, Jr., Explorer, 18 West Twelfth Street, New York, N.Y.; Earl A. Trager, Chief of the Naturalist Division, National Park Service, Washington, D.C.; Oliver Kehrlein, Chairman, Committee on Glacier Studies, 1050 Mills Tower, 220 Bush Street, San Francisco, California; Kenneth N. Phillips, Associate Hydraulic Engineer, Water Resources Branch, United States Geological Survey, Chairman, Research Committee of the Mazamas, 606 Post‐Office Building, Portland, Oregon; William S. Cooper, Professor of Botany, University of Minnesota, Minneapolis, Minnesota; Gerald FitzGerald, Senior Topographic Engineer, Alaska Branch, United States Geological Survey, Washington, D.C.; Lawrence M. Gould, Professor of Geology, Carleton College, Northfield, Minnesota; François E. Matthes (Chairman), Senior Geologist, Section of Glacial Geology, United States Geological Survey, Washington, D.C.

The international relations of the Committee have changed somewhat during the past year as a result of the consolidation of the International Commission of Glaciers with the International Commission of Snow. That consolidation was effected by the International Association of Scientific Hydrology (to which both commissions belonged) at the triennial meeting in Washington, in September, 1939. Inasmuch as the membership of the new International Commission of Snow and Glaciers comprises the personnel of the two former commissions, our Committee on Glaciers now automatically is represented on the new International Commission by four men—Church, Hobbs, Gould, and Matthes. Moreover, Church is acting President, and it is understood that he will become President as soon as the political situation in Europe permits the holding of a formal election of officers at which all nations interested can exercise their right of voting

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00396","usgsCitation":"Matthes, F.E., 1940, Committee on glaciers, 1939–40: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 396-406, https://doi.org/10.1029/TR021i002p00396.","productDescription":"11 p.","startPage":"396","endPage":"406","costCenters":[],"links":[{"id":378565,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Matthes, Francois E.","contributorId":97963,"corporation":false,"usgs":true,"family":"Matthes","given":"Francois","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":799239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213474,"text":"70213474 - 1940 - Committee on underground waters, 1939–40","interactions":[],"lastModifiedDate":"2020-09-18T21:09:54.123533","indexId":"70213474","displayToPublicDate":"1940-09-17T15:00:10","publicationYear":"1940","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":"Committee on underground waters, 1939–40","docAbstract":"

The Committee on Underground Waters for the new triennium is composed of the following: H. F. Blaney; E. B. Burwell; W. Gardner; C. S. Howard; F. H. Lahee; G. W. Musgrave; A. M. Piper; A. C. Swinnerton; L. K. Wenzel; D. G. Thompson (Chairman).

The outstanding event of the year for ground‐water hydrologists was the meeting of the International Association of Scientific Hydrology, as a part of the International Union of Geodesy and Geophysics, at Washington, D.C., in September, 1939. One day was devoted to “questions” or topics of symposia of the Commission on Subterranean Water.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00433-2","usgsCitation":"Thompson, D.G., 1940, Committee on underground waters, 1939–40: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 433-439, https://doi.org/10.1029/TR021i002p00433-2.","productDescription":"7 p.","startPage":"433","endPage":"439","costCenters":[],"links":[{"id":378541,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David Grosh","contributorId":19141,"corporation":false,"usgs":true,"family":"Thompson","given":"David","email":"","middleInitial":"Grosh","affiliations":[],"preferred":false,"id":799123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213461,"text":"70213461 - 1940 - Committee on runoff, 1939–40","interactions":[],"lastModifiedDate":"2020-09-21T14:09:00.139912","indexId":"70213461","displayToPublicDate":"1940-09-17T14:29:09","publicationYear":"1940","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":"Committee on runoff, 1939–40","docAbstract":"

The Runoff Committee during the year has consisted of H. K. Barrows, Merrill Bernard, E. S. Callings, R. S. Goodridge, G. A. Hathaway, Joseph Jacobs, Prof. F. T. Mavis, H. S. Riesbol, Waldo E. Smith, F. F. Snyder, and H. G. Wilm. The Committee represents a rather wide geographic distribution, quite a large variety of interests, and most of the agencies interested in runoff‐problems.

Throughout the year members of the Committee have shown interest in runoff‐problems of various kinds as evidenced by numerous articles and discussions in technical publications and by their participation in the deliberations of many working or advisory committees dealing with hydrologic problems. As the Chairman views it, the functions of the members of the research committees are not only to keep abreast of, and to make advances in, the technique relating to their particular fields, but also to demonstrate the practicability of the technique in the field of applied hydrology. Members of the Committee on Runoff have kept these aims in view. As in past years, the Committee is indebted to Miss Mary Soroka of New York City, Chairman of the International Committee on Bibliography, for her compilations of references to all articles relating to runoff, and to Mr. Beij for his work in connection therewith.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00373","usgsCitation":"Hoyt, W.G., 1940, Committee on runoff, 1939–40: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 373-374, https://doi.org/10.1029/TR021i002p00373.","productDescription":"2 p.","startPage":"373","endPage":"374","costCenters":[],"links":[{"id":378538,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hoyt, W. G.","contributorId":38547,"corporation":false,"usgs":true,"family":"Hoyt","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":799120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213457,"text":"70213457 - 1940 - Magnetic studies of the Florida peninsula","interactions":[],"lastModifiedDate":"2020-09-17T19:17:00.216598","indexId":"70213457","displayToPublicDate":"1940-09-17T14:07:15","publicationYear":"1940","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":"Magnetic studies of the Florida peninsula","docAbstract":"

This investigation was undertaken primarily as a pilot‐experiment for gaining information concerning the field‐technique and accuracy which is needed for covering large areas in detail and at the same time economically. Owing to the complex nature of magnetic observations, such a pilot‐study serves, in addition, as a basis for determining the best methods of presenting the results of large areal studies in an easily comprehensible form. The State of Florida was chosen for such preliminary study for the following reasons: First, because it is geologically ideal for such an investigation since it comprises a series of unconsolidated, flat‐lying, Tertiary and Cretaceous sediments of low magnetic permeability covering a complex and much‐folded crystalline basement composed largely of rocks carrying strongly paramagnetic materials; secondly, because information concerning the structural trends of the crystalline basement would be of great interest and importance in the study of Appalachian orogeny and the relationship of the Florida Peninsula to both the Appalachian and Antillean tectonic systems.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR021i002p00297","usgsCitation":"Lee, F., and Swartz, J., 1940, Magnetic studies of the Florida peninsula: Eos, Transactions, American Geophysical Union, v. 21, no. 2, p. 297-301, https://doi.org/10.1029/TR021i002p00297.","productDescription":"5 p.","startPage":"297","endPage":"301","costCenters":[],"links":[{"id":378537,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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No abstract available.

","language":"English","publisher":"American Chemical Society","doi":"10.1021/ie50369a018","usgsCitation":"Smith, H.I., 1940, Potash: Industrial and Engineering Chemistry, v. 32, no. 9, p. 1171-1172, https://doi.org/10.1021/ie50369a018.","productDescription":"2 p.","startPage":"1171","endPage":"1172","costCenters":[],"links":[{"id":378533,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"9","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, H. I.","contributorId":236986,"corporation":false,"usgs":false,"family":"Smith","given":"H.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":799115,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213445,"text":"70213445 - 1940 - Phosphate deposits of the United States ","interactions":[],"lastModifiedDate":"2020-09-17T18:32:14.929559","indexId":"70213445","displayToPublicDate":"1940-09-17T13:21:00","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Phosphate deposits of the United States ","docAbstract":"

Different types of phosphate deposits and different sources of phosphate in the United States are briefly discussed. In Florida two types of phosphate are now mined, land pebble and hard rock. The principal characteristics of these types of rock are stated and methods of prospecting, mining and recovery briefly outlined. Testimony given before the Congressional Committee to Investigate the Adequacy and Use of Phosphate Resources of the United States, November 28, 1938, at Lakeland, Fla., showed Florida's reserves to be far greater than previously supposed. Similarly at corresponding hearings in Tennessee a few days earlier the reserves of brown phosphate, the only type now mined in that State, were shown to exceed earlier official estimates. Reserves of the Western fields have been raised a little to bring them abreast of current information but no attempt has been made, as in the other States named, to include lower grades of rock than those formerly considered in the estimates. Professor J. Stewart Williams has shown for Utah that such a procedure would tremendously increase these figures.

Reserves of the United States as a whole are now considered to exceed ten billion tons, not counting those classed as possible or certain phosphatic limestones mentioned at the hearings of the Congressional Committee. As nearly 2,000,000 acres of public land in the Western States and 66,000 acres in Florida remain to be examined for their phosphate content the stated figure will ultimately be greatly increased. At the present rate of consumption, 3,000,000 tons annually, ten billion tons would last more than 3,000 years.

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1940 - Grubs in minks","interactions":[],"lastModifiedDate":"2014-07-17T12:47:17","indexId":"38010","displayToPublicDate":"1940-09-01T12:46:08","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"167","title":"Grubs in minks","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Shillinger, J., 1940, Grubs in minks: Wildlife Leaflet 167, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6004e4b0b290850fca6e","contributors":{"authors":[{"text":"Shillinger, J.E.","contributorId":47879,"corporation":false,"usgs":true,"family":"Shillinger","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":218740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38012,"text":"38012 - 1940 - Mink breeding: elementary principles","interactions":[],"lastModifiedDate":"2014-07-17T12:50:01","indexId":"38012","displayToPublicDate":"1940-08-01T12:49:00","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"169","title":"Mink breeding: elementary principles","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"In cooperation with Swarthmore College and the Fish and Wildlife Service, Department of the Interior","usgsCitation":"Enders, R.K., 1940, Mink breeding: elementary principles: Wildlife Leaflet 169, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd67c1e4b0b29085101952","contributors":{"authors":[{"text":"Enders, Robert K.","contributorId":23852,"corporation":false,"usgs":true,"family":"Enders","given":"Robert","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":218742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38009,"text":"38009 - 1940 - Infectious myxomatosis of domestic rabbits","interactions":[],"lastModifiedDate":"2014-07-17T12:45:04","indexId":"38009","displayToPublicDate":"1940-07-01T12:44:35","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"166","title":"Infectious myxomatosis of domestic rabbits","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"McKenney, F.D., and Vail, E., 1940, Infectious myxomatosis of domestic rabbits (Reissued with slight revisions from Wildlife Leaflet BS-89 (1937).): Wildlife Leaflet 166, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290365,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued with slight revisions from Wildlife Leaflet BS-89 (1937).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd626fe4b0b290850fe2da","contributors":{"authors":[{"text":"McKenney, Frank D.","contributorId":31314,"corporation":false,"usgs":true,"family":"McKenney","given":"Frank","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":218738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vail, E.L.","contributorId":81810,"corporation":false,"usgs":true,"family":"Vail","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":218739,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70174985,"text":"70174985 - 1940 - Memorandum in regard to prospecting for a softer water supply for the Kansas State Penitentiary at Lansing, Kansas","interactions":[],"lastModifiedDate":"2016-07-26T09:34:02","indexId":"70174985","displayToPublicDate":"1940-06-25T14:30:00","publicationYear":"1940","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Memorandum in regard to prospecting for a softer water supply for the Kansas State Penitentiary at Lansing, Kansas","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70174985","usgsCitation":"Lohman, S.W., and Mitchell, A., 1940, Memorandum in regard to prospecting for a softer water supply for the Kansas State Penitentiary at Lansing, Kansas: Open-File Report, 17 p., https://doi.org/10.3133/70174985.","productDescription":"17 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":325623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Kansas","city":"Lansing","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.83192443847656,\n 39.25246120620433\n ],\n [\n -94.84291076660156,\n 39.26203141523749\n ],\n [\n -94.90333557128906,\n 39.261499771230774\n ],\n [\n -94.90333557128906,\n 39.27797886039667\n ],\n [\n -94.89646911621094,\n 39.281699408719746\n ],\n [\n -94.89990234375,\n 39.28648268048973\n ],\n [\n -94.90402221679688,\n 39.29498546816049\n ],\n [\n -94.91981506347656,\n 39.29498546816049\n ],\n [\n -94.92324829101562,\n 39.28967134685658\n ],\n [\n -94.93011474609375,\n 39.28648268048973\n ],\n [\n -94.93011474609375,\n 39.2827623862317\n ],\n [\n -94.94453430175781,\n 39.280636415076756\n ],\n [\n -94.94453430175781,\n 39.2854197594374\n ],\n [\n -94.95140075683594,\n 39.2854197594374\n ],\n [\n -94.95140075683594,\n 39.28223089949212\n ],\n [\n -94.97474670410156,\n 39.280636415076756\n ],\n [\n -94.97817993164061,\n 39.26681602984699\n ],\n [\n -94.98641967773436,\n 39.27160031783707\n ],\n [\n -94.98641967773436,\n 39.280636415076756\n ],\n [\n -95.00289916992188,\n 39.279573405302806\n ],\n [\n -95.03585815429688,\n 39.279041894366785\n ],\n [\n -95.04615783691406,\n 39.27851037939807\n ],\n [\n -95.04547119140625,\n 39.23703978837414\n ],\n [\n -94.99740600585938,\n 39.23757161784572\n ],\n [\n -94.92942810058594,\n 39.23384872688399\n ],\n [\n -94.93080139160156,\n 39.150297710716686\n ],\n [\n -94.86900329589842,\n 39.150297710716686\n ],\n [\n -94.866943359375,\n 39.20991113991019\n ],\n [\n -94.84840393066406,\n 39.20937910082159\n ],\n [\n -94.85389709472655,\n 39.23863526469436\n ],\n [\n -94.85389709472655,\n 39.248739105448365\n ],\n [\n -94.83192443847656,\n 39.25246120620433\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"579889b8e4b0589fa1c6ba7f","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":643512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, Alexander","contributorId":173164,"corporation":false,"usgs":false,"family":"Mitchell","given":"Alexander","email":"","affiliations":[],"preferred":false,"id":643513,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70174984,"text":"70174984 - 1940 - Ground-water resources of Kansas","interactions":[],"lastModifiedDate":"2016-08-19T11:28:49","indexId":"70174984","displayToPublicDate":"1940-06-25T14:30:00","publicationYear":"1940","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water resources of Kansas","docAbstract":"

Introduction: Water is a necessity of life. Accordingly, every person is deeply interested in the subject of water supply. He knows that he must have water to drink. He depends indirectly on water for all his food and clothing. He may want water in which to wash. Civilized man has learned also that water serves admirably for a large and ever enlarging list of uses that depend on its easy convertibility from a liquid to a solid or gaseous state and its adaptability as a chemical solvent, a medium for transfer of matter or energy, and a regulator of temperature. 

\n

The average consumption of water in towns and cities of the United States amounts to about 100 gallons per person per day. Because of long familiarity with never-failing supplies  of water provided by nature, or equally, because of unthinking dependence on others, many individuals are probably unaware of their interest in water, but let water become difficult or impossible to obtain, or let the quality of water be greatly changed, and there is immediate concern. Many Kansas persons—without doubt too many—give little thought to the subject of water when rainfall is normal and when ponds and streams are full, but not too full.  Kansas has a smaller natural water supply than many other regions, but we are used to these conditions, and it is strongly marked departures from what we regard as normal that cause anxiety. Periods of excessive heat and drought such as have recurred in Kansas, especially during the last half-dozen years, bring hardships to very many persons, particularly dwellers on the farm. Alarm is felt when field crops and pasture shrivel from lack of moisture and from heat, when there is insufficient water for the stock, when wells go dry, and when even some towns and cities must haul water in tank cars. Everyone is then water-conscious, as is true also under reverse conditions, when overabundance of rainfall produces disastrous floods. 

\n

It is obvious, however, that the subject of water supply should not be given attention only in times of deficiency or overabundance. All citizens of Kansas should have enduring interest in quests of water control and conservation that will make for equable supply. No individual or government agency can increase or diminish the annual rainfall, nor safeguard wholly against floods. It is possible, on the other hand, largely to avoid the distress due to severe shortage of water in recent years. This statement calls attention to the subject of water in the ground, or as commonly known, ground water. I have been asked to discuss the underground water resources of Kansas. I am asked to give answers to such questions as: In what places and under what conditions may water that is suitable for domestic and stock use be obtained from wells? Why are some water wells in Kansas never-failing large producers of excellent waters, whereas other yield only small amounts of poor water and readily go dry? What improvements are possible in methods of finding and utilizing the ground-water resources that exist in Kansas? What provisions can be made to safeguard best against effects of prolonged drought? 

\n

These questions call for a discussion of some general principles that apply to accumulation and movement of water beneath the surface of in Kansas, and especially to the various geologic conditions that are fundamental factors in controlling variation in water supply from the below ground. It will be desirable also to consider the characteristics of various districts in Kansas that may be differentiated as natural ground-water provinces, pointing out the distinguishing features of these districts. The basis for these distinctions is a difference in water-supply conditions that depends mainly on variation in underground rock structure. 

\n

Importance of ground-water resources.—The importance of Kansas' ground-water resources may be emphasized from various viewpoints and in different ways. More than three-fourths of the public water supplies of Kansas are obtained from wells. In 1939, only 60 out of 375 municipal water supplies in Kansas, which is 16 percent, utilized surface waters. If the water wells of the cities and those located on all privately owned land in the state were suddenly destroyed, making it necessary to go to streams, springs, lakes (which are almost all artificial), and ponds for water supply domestic, stock, and industrial use, there would be almost incalculable difficulty and expense. If one could not go to springs, or dig new wells, or use any surface water derived from underground flow, much of Kansas would become uninhabitable.  These suggested conditions seem absurd, but they emphasize our dependence on ground-water resources. Fromm a quantitative standpoint, ground-water supplies existent in Kansas far outweigh surface waters that are present in the state at any one time. No exact figures for such comparison can be given, but, taking 384 square miles as the total surface water area of the state and estimating an average water depth of five feet, the computed volume of surface waters is found to be 1/100th of that of the conservatively estimated ground-water storage in Kansas. The latter takes account only of potable fresh water and is based on an assumed mean thickness of ten feet of reservoir having an effective porosity of twenty percent. It is to be remembered, however, that most of the surface water is run-off, which soon leaves the state, stream valleys being replenished from rainfall and flow from ground-water reservoirs. Most of the ground-water supplies, on the other hand, have existed for many years with almost no appreciable movement--in fact, it is reasonably certain that some well water drawn from beneath the surface of Kansas in 1940 represents rainfall in this region at time before the first white man entered Kansas, even before the visit of Coronado in the 16th century. Most ground water is to be regarded as water in storage rather than water in transit.   

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