The drainage‐basin of the Pecos River in New Mexico is a broad asymmetric trough extending from the Sangre de Cristo Mountains southward into Texas (see Fig. 1). It is bounded on the east by the westward facing escarpment of the High Plains and on the west by the crests of the Guadalupe, Sacramento and Sierra Blanca mountains, and a poorly defined divide extending northward through Gallinas Mountain and Pedernal Mountain to Glorieta Mesa. Most of the basin is formed by extensive upland erosion‐surfaces that slope gently toward the river. The valley proper, through much of its length, is relatively narrow and is bounded by steep marginal bluffs, but in some sections, notably between Acme and Lakewood (the Roswell artesian basin) and between Carlsbad and Black River, it is considerably expanded and the lowlands adjoining the river extend from 3 to 16 miles back from the river.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00027","usgsCitation":"Morgan, A., 1942, Solution‐phenomena in the Pecos basin in New Mexico: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 27-25, https://doi.org/10.1029/TR023i001p00027.","productDescription":"9 p.","startPage":"27","endPage":"25","costCenters":[],"links":[{"id":378278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Pecos River Drainage Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.1396484375,\n 35.94243575255426\n ],\n [\n -106.45751953125,\n 36.03133177633187\n ],\n [\n -107.99560546875,\n 35.67514743608467\n ],\n [\n -107.4462890625,\n 33.211116472416855\n ],\n [\n -107.20458984375,\n 32.008075959291055\n ],\n [\n -103.24951171875,\n 32.045332838858506\n ],\n [\n -103.1396484375,\n 35.94243575255426\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","edition":"18","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, Arthur M.","contributorId":59051,"corporation":false,"usgs":true,"family":"Morgan","given":"Arthur M.","affiliations":[],"preferred":false,"id":798436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213111,"text":"70213111 - 1942 - Quality of stored water available for use in the lower basin of the Pecos River, Texas","interactions":[],"lastModifiedDate":"2020-09-09T17:34:29.239201","indexId":"70213111","displayToPublicDate":"1942-09-09T12:24:41","publicationYear":"1942","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":"Quality of stored water available for use in the lower basin of the Pecos River, Texas","docAbstract":"Storage of water in reservoir s may be for (1) irrigation, (2) power‐generation sometimes in connection with releases for irrigation, (3) flood‐control, (4) recreation, or combinations of these four uses. The control of releases of the stored water may involve conflicts of interests as to the best use of the available supply.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00593","usgsCitation":"Howard, C.S., 1942, Quality of stored water available for use in the lower basin of the Pecos River, Texas: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 593-598, https://doi.org/10.1029/TR023i002p00593.","productDescription":"6 p.","startPage":"593","endPage":"598","costCenters":[],"links":[{"id":378277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas, New Mexico","otherGeospatial":"Pecos River Drainage Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.83203125,\n 36.13787471840729\n ],\n [\n -106.69921875,\n 36.13787471840729\n ],\n [\n -106.5234375,\n 34.813803317113155\n ],\n [\n -106.171875,\n 33.100745405144245\n ],\n [\n -105.4248046875,\n 31.5504526754715\n ],\n [\n -103.4912109375,\n 30.486550842588485\n ],\n [\n -101.6455078125,\n 30.637912028341123\n ],\n [\n -100.94238281249999,\n 33.50475906922609\n ],\n [\n -101.29394531249999,\n 36.06686213257888\n ],\n [\n -102.83203125,\n 36.13787471840729\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","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":798275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213109,"text":"70213109 - 1942 - Hydraulic criteria for sand‐waves ","interactions":[],"lastModifiedDate":"2020-09-09T17:24:00.712348","indexId":"70213109","displayToPublicDate":"1942-09-09T12:10:10","publicationYear":"1942","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":"Hydraulic criteria for sand‐waves ","docAbstract":"Sand‐waves on rivers are rhythmic successions of waves which occur at flood‐stages of streams heavily loaded with sediments. They take their name from the fact that sand and associated silts and gravels form a large part of the load transported by a river at such times. They seem to be peculiar to the Southwest and many vivid descriptions of them can be found in the literature of that region. R. C. PIERCE [see 1 of “References” at end of paper[, who observed many sand‐waves on the San Juan River in Utah, has described them as resembling in appearance “the waves thrown up by a stern‐wheel river steamboat.” He further describes their appearances as follows: “The sand‐waves are not continuous, but follow a rhythmic movement. At one moment the stream is running smoothly for a distance of perhaps several hundred yards. Then suddenly a number of waves, usually from six to ten, appear. They reach their full size in a few seconds, flow for perhaps two or three minutes, then suddenly disappear. Often, for perhaps half a minute before disappearing, the crests of the waves go through a combing movement, accompanied by a roaring sound. On first appearance it seems that the wave‐forms occupy fixed positions, but by watching them closely it is seen that they move slowly upstream. In the narrow parts of the stream the waves may reach nearly the width of the river, but in the wider parts they occupy smaller proportional widths. Usually they are at right‐angles to the axis of the stream, but at some places, particularly in the wider parts of the river, they may suddenly assume a diagonal position, moving rather rapidly across the stream in the direction toward which the upstream side of the wave has turned.” Many such descriptions may be found which in the main bear out PIERCE'S account, varying, however, as to size of wave, rate, and sometimes as to direction of movement.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00615","usgsCitation":"Langbein, W., 1942, Hydraulic criteria for sand‐waves : Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 615-619, https://doi.org/10.1029/TR023i002p00615.","productDescription":"4 p.","startPage":"615","endPage":"619","costCenters":[],"links":[{"id":378276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","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":798274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213108,"text":"70213108 - 1942 - Report of Committee on Underground Waters, 1941–42","interactions":[],"lastModifiedDate":"2020-09-09T17:02:34.270957","indexId":"70213108","displayToPublicDate":"1942-09-09T11:51:57","publicationYear":"1942","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 Committee on Underground Waters, 1941–42","docAbstract":"So many ground‐water hydrologists are engaged on problems relating directly to the war that the usual annual inquiry for information as to projects that deserve review in the annual report of the Committee on Underground Waters brought relatively little response. It is in part for this reason, but also in part because the Chairman of the Committee is busy on war problems, that this report is shorter than usual.
The Boise River Project in southwestern Idaho comprises an area of about 333,000 acres of highly developed agricultural land. Precipitation in the irrigated valley averages about ten inches a year which is too low to support any but desert vegetation. Water for irrigation during the growing season is obtained from Arrowrock Reservoir located on the Boise River four miles above Moore Creek, and from Deer Flat Reservoir near Nampa. The deposition of sediment in the river‐channel, in irrigation‐canals, and in farm‐laterals has interfered with the normal operation of the irrigation‐system and has occasionally required the expenditure of considerable time and money for removal of the deposited material.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00652","usgsCitation":"Love, S.K., and Benedict, P.C., 1942, Sediment loads in the Moore Creek drainage‐basin, Idaho 1939–40: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 652-657, https://doi.org/10.1029/TR023i002p00652.","productDescription":"6 p.","startPage":"652","endPage":"657","costCenters":[],"links":[{"id":378272,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Moore Creek Drainage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.3232421875,\n 43.49676775343911\n ],\n [\n -115.27954101562499,\n 43.49676775343911\n ],\n [\n -115.27954101562499,\n 44.46123053905879\n ],\n [\n -116.3232421875,\n 44.46123053905879\n ],\n [\n -116.3232421875,\n 43.49676775343911\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":798266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, Paul Charles","contributorId":32135,"corporation":false,"usgs":true,"family":"Benedict","given":"Paul","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":798267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70213071,"text":"70213071 - 1942 - Runoff in the Santa Ynez River Basin, California, following the excessive rainfall of 1940–41","interactions":[],"lastModifiedDate":"2020-09-08T20:29:41.286539","indexId":"70213071","displayToPublicDate":"1942-09-08T15:24:21","publicationYear":"1942","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":"Runoff in the Santa Ynez River Basin, California, following the excessive rainfall of 1940–41","docAbstract":"This paper reports briefly on the runoff‐characteristics of the Santa Ynez River in Santa Barbara County, California, following the excessive rainfall in the winter of 1940–41; also, it contrasts these conditions of 1940–41 with earlier years of less rainfall. The data for this report were compiled in connection with an investigation of the water‐resources of Santa Barbara County which is being conducted by the United States Geological Survey in cooperation with the County of Santa Barbara.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00124","usgsCitation":"LaRocque, G., 1942, Runoff in the Santa Ynez River Basin, California, following the excessive rainfall of 1940–41: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 124-129, https://doi.org/10.1029/TR023i001p00124.","productDescription":"6 p.","startPage":"124","endPage":"129","costCenters":[],"links":[{"id":378227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Santa Ynez River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.673828125,\n 34.35704160076073\n ],\n [\n -119.5751953125,\n 34.35704160076073\n ],\n [\n -119.5751953125,\n 34.88593094075317\n ],\n [\n -120.673828125,\n 34.88593094075317\n ],\n [\n -120.673828125,\n 34.35704160076073\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"LaRocque, G.A. Jr.","contributorId":22837,"corporation":false,"usgs":true,"family":"LaRocque","given":"G.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":798101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213070,"text":"70213070 - 1942 - Ground‐water studies in the Southwest ","interactions":[],"lastModifiedDate":"2020-09-08T20:23:59.148789","indexId":"70213070","displayToPublicDate":"1942-09-08T15:19:02","publicationYear":"1942","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 studies in the Southwest ","docAbstract":"Geologists are concerned with the rock‐systems that form the crust of the Earth. The groundwater geologists are concerned with the rock‐systems specifically because the open spaces which the rocks contain serve as reservoirs and conduits for water—water which performs a large part of the geologic work that is in progress today and has been in progress during past ages; water which affects profoundly the whole hydrologic cycle and is still the principal source of water‐supply for mankind, as it has been for primitive man and the other land animals before the time of artificial waterworks.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00006","usgsCitation":"Meinzer, O.E., 1942, Ground‐water studies in the Southwest : Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 6-9, https://doi.org/10.1029/TR023i001p00006.","productDescription":"4 p.","startPage":"6","endPage":"9","costCenters":[],"links":[{"id":378226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","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":798100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213069,"text":"70213069 - 1942 - Report of committee on the chemistry of natural waters, 1941–42","interactions":[],"lastModifiedDate":"2020-09-09T13:53:38.452258","indexId":"70213069","displayToPublicDate":"1942-09-08T15:14:10","publicationYear":"1942","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 committee on the chemistry of natural waters, 1941–42","docAbstract":"The membership of the Committee during the past year was as follows: I. A. Dennison, National Bureau of Standards; C S. Howard (Chairman), Geological Survey; C. S. Scofield, Department of Agriculture; D. G. Thompson, Geological Survey; and T. G. Thompson, University of Washington, Seattle, Washington.
SCOFIELD has continued his studies in connection with the salt balance in irrigated areas and has made progress‐reports to interested parties concerning the salt balance on the El Paso Project, Wapato Project, and the Yuma Project. These studies are of great interest to those responsible for the operation of the projects and should be of considerable value to other projects in indicating the volumes of water that may be necessary under certain conditions to insure proper drainage of the project.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00466","usgsCitation":"Howard, C.S., 1942, Report of committee on the chemistry of natural waters, 1941–42: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 466-467, https://doi.org/10.1029/TR023i002p00466.","productDescription":"2 p.","startPage":"466","endPage":"467","costCenters":[],"links":[{"id":378225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","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":798099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213067,"text":"70213067 - 1942 - Origin of the Ayer granodiorite in the Lowell area, Massachusetts","interactions":[],"lastModifiedDate":"2020-09-09T13:55:31.765838","indexId":"70213067","displayToPublicDate":"1942-09-08T15:10:47","publicationYear":"1942","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":"Origin of the Ayer granodiorite in the Lowell area, Massachusetts","docAbstract":"The elongate stock of Ayer granodiorite exposed north and west of Lowell, Massachusetts, is reasonably typical of the many bodies of granitic rocks in the central and north‐central parts of the State. It lies within a terrane composed predominantly of steeply tilted, thinly inter bedded quartzite and biotite schist, and many of its structural relations superficially suggest for it a metasomatic origin, involving the quiet replacement of preexisting bedded and foliated rocks by invading fluids of magmatic derivation. The elongation of the stock and a distinct foliation characteristic of the granodiorite itself are both essentially conformable with country‐rock structure, and the contacts, wherever seen, also appear to be concordant. This general parallelism is further emphasized by a consistent orientation of numerous tabular inclusions, the edges of most of which have been obscured by reaction with the igneous material. Moreover, apparent transitions from country‐rock into granodiorite in a direction parallel to their structural trends occur at several places. Dikes and lenses of pegmatite are abundant within and adjacent to the granodiorite body.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00341-2","usgsCitation":"Jahns, R., 1942, Origin of the Ayer granodiorite in the Lowell area, Massachusetts: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 341-342, https://doi.org/10.1029/TR023i002p00341-2.","productDescription":"2 p.","startPage":"341","endPage":"342","costCenters":[],"links":[{"id":378224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Lowell","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.378173828125,\n 42.593532625649935\n ],\n [\n -71.26007080078125,\n 42.593532625649935\n ],\n [\n -71.26007080078125,\n 42.65012181368022\n ],\n [\n -71.378173828125,\n 42.65012181368022\n ],\n [\n -71.378173828125,\n 42.593532625649935\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jahns, Richard H.","contributorId":107757,"corporation":false,"usgs":true,"family":"Jahns","given":"Richard H.","affiliations":[],"preferred":false,"id":798098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213066,"text":"70213066 - 1942 - Results of pumping tests of the Carrizo sand in the Lufkin area, Texas","interactions":[],"lastModifiedDate":"2020-09-08T20:08:28.039461","indexId":"70213066","displayToPublicDate":"1942-09-08T15:02:23","publicationYear":"1942","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":"Results of pumping tests of the Carrizo sand in the Lufkin area, Texas","docAbstract":"The Lufkin Area, as the term is used in this paper, is comprised of Angelina and Nacogdoches counties, Texas, and parts of adjoining counties. Its surface is gently rolling, with a maximum relief of about 150 feet and a maximum altitude of less than 400 feet. The average annual rainfall is about 45 inches. Practically all of the water‐supplies in the area come from ground‐water and it has been found that the Carrizo sand contains water of better quality and is more productive than any other water‐bearing formation in the area [see 1 of “References” at end of paper]. Figure 1 is a map of the area, showing the positions of the cities of Lufkin and Nacogdoches, the wells of the Southland Paper Mill, and other wells mentioned in this paper.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00040","usgsCitation":"Guyton, W., 1942, Results of pumping tests of the Carrizo sand in the Lufkin area, Texas: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 40-48, https://doi.org/10.1029/TR023i001p00040.","productDescription":"9 p.","startPage":"40","endPage":"48","costCenters":[],"links":[{"id":378223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Lufkin Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.086669921875,\n 31.287939892641734\n ],\n [\n -94.48791503906249,\n 31.287939892641734\n ],\n [\n -94.48791503906249,\n 31.695455797778713\n ],\n [\n -95.086669921875,\n 31.695455797778713\n ],\n [\n -95.086669921875,\n 31.287939892641734\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Guyton, W.F.","contributorId":11688,"corporation":false,"usgs":true,"family":"Guyton","given":"W.F.","affiliations":[],"preferred":false,"id":798097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213064,"text":"70213064 - 1942 - Manganese-bearing veins in southwestern Virginia","interactions":[],"lastModifiedDate":"2020-09-08T19:28:14.089444","indexId":"70213064","displayToPublicDate":"1942-09-08T14:24:19","publicationYear":"1942","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":"Manganese-bearing veins in southwestern Virginia","docAbstract":"Veins carrying manganese silicates largely in the form of the manganese garnet, spessartite, occur in the crystalline schists and gneisses of Carroll and Grayson Counties, Virginia, in the southern parts of the Galax and Independence quadrangles just north of the North Carolina State line. This brief paper includes a discussion of these manganese-bearing veins which are described in a report on the Geology and Mineral resources of the Great Gossan Lead district prepared by G. W. Stose and the writer for publication by the Virginia Geological Survey
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.37.5.408","usgsCitation":"Jonas, A., 1942, Manganese-bearing veins in southwestern Virginia: Economic Geology, v. 37, no. 5, p. 408-423, https://doi.org/10.2113/gsecongeo.37.5.408.","productDescription":"16 p.","startPage":"408","endPage":"423","costCenters":[],"links":[{"id":378220,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"Blue Ridge Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.57623291015625,\n 36.55598153635691\n ],\n [\n -80.81817626953125,\n 36.55598153635691\n ],\n [\n -80.81817626953125,\n 36.767492156196745\n ],\n [\n -81.57623291015625,\n 36.767492156196745\n ],\n [\n -81.57623291015625,\n 36.55598153635691\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"1942-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Jonas, Anna I.","contributorId":73466,"corporation":false,"usgs":true,"family":"Jonas","given":"Anna I.","affiliations":[],"preferred":false,"id":798095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213063,"text":"70213063 - 1942 - Differential density of ground water in ore deposition","interactions":[],"lastModifiedDate":"2020-09-08T19:22:52.636571","indexId":"70213063","displayToPublicDate":"1942-09-08T14:14:09","publicationYear":"1942","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":"Differential density of ground water in ore deposition","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.37.5.424","usgsCitation":"McKnight, E., 1942, Differential density of ground water in ore deposition: Economic Geology, v. 37, no. 5, p. 424-426, https://doi.org/10.2113/gsecongeo.37.5.424.","productDescription":"3 p.","startPage":"424","endPage":"426","costCenters":[],"links":[{"id":378219,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"1942-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"McKnight, Edwin T.","contributorId":85039,"corporation":false,"usgs":true,"family":"McKnight","given":"Edwin T.","affiliations":[],"preferred":false,"id":798094,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213062,"text":"70213062 - 1942 - Differential density of ground water in ore deposition","interactions":[],"lastModifiedDate":"2020-09-08T19:05:53.227005","indexId":"70213062","displayToPublicDate":"1942-09-08T14:03:17","publicationYear":"1942","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":"Differential density of ground water in ore deposition","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.37.6.524","usgsCitation":"Cedarstrom, D., 1942, Differential density of ground water in ore deposition: Economic Geology, v. 37, p. 524-524, https://doi.org/10.2113/gsecongeo.37.6.524.","productDescription":"1 p.","startPage":"524","endPage":"524","costCenters":[],"links":[{"id":378218,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cedarstrom, D.J.","contributorId":102127,"corporation":false,"usgs":true,"family":"Cedarstrom","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":798093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207285,"text":"70207285 - 1942 - Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma","interactions":[],"lastModifiedDate":"2019-12-16T06:30:25","indexId":"70207285","displayToPublicDate":"1942-08-31T06:24:19","publicationYear":"1942","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‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma","docAbstract":"During the closing years of the 19th century, Haworth [see 1 and 2 of “References” at end of paper] and Johnson [3] noted the abundant depressions resembling sink‐holes in the Southern High Plains, especially in Meade and Clark counties, Kansas, and Beaver County, Oklahoma. Johnson was of the opinion that all the depressions and basins in this region were due to solution, whereas Haworth [1] believed the Meade artesian basin to be structural, although he held to a solutional origin for the Ashland and Englewood basins, which are a few miles to the east. ©1942. American Geophysical Union. All Rights Reserved.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00035","issn":"00028606","usgsCitation":"Frye, K., and Schoff, S., 1942, Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 35-39, https://doi.org/10.1029/TR023i001p00035.","productDescription":"5 p. ","startPage":"35","endPage":"39","costCenters":[],"links":[{"id":370292,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Kansas, Oklahoma ","county":"Meade, Clark, Beaver","otherGeospatial":"Meade basin ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-99.5557,37.4689],[-99.5551,37.3832],[-99.5435,37.3828],[-99.5399,36.9998],[-100.0009,36.9985],[-100.0024,36.9985],[-100.004,36.8538],[-100.0044,36.76],[-100.0045,36.5917],[-100.0044,36.5849],[-100.0038,36.4998],[-100.1458,36.4998],[-100.3204,36.4999],[-100.5459,36.4994],[-100.7022,36.5],[-100.8939,36.4998],[-100.9524,36.4998],[-100.9534,36.8476],[-100.9448,36.8478],[-100.9441,36.9988],[-100.6337,36.9986],[-100.635,37.3881],[-100.6518,37.3878],[-100.652,37.4757],[-100.217,37.4758],[-100.1068,37.4751],[-99.5557,37.4689]]]},\"properties\":{\"name\":\"Clark\",\"state\":\"KS\"}}]}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Frye, K.C.","contributorId":221248,"corporation":false,"usgs":false,"family":"Frye","given":"K.C.","email":"","affiliations":[],"preferred":false,"id":777540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoff, S.L.","contributorId":107365,"corporation":false,"usgs":true,"family":"Schoff","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":777541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220348,"text":"5220348 - 1942 - Protein requirements of bobwhite chicks for survival, growth and efficiency of feed utilization","interactions":[],"lastModifiedDate":"2025-01-08T16:02:13.818155","indexId":"5220348","displayToPublicDate":"1942-07-01T00:00:00","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Protein requirements of bobwhite chicks for survival, growth and efficiency of feed utilization","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3795900","usgsCitation":"Nestler, R.B., Bailey, W.W., and McClure, H.E., 1942, Protein requirements of bobwhite chicks for survival, growth and efficiency of feed utilization: Journal of Wildlife Management, v. 6, no. 3, p. 185-193, https://doi.org/10.2307/3795900.","productDescription":"9 p.","startPage":"185","endPage":"193","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193379,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Research Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.81358975766166,\n 39.0799855368318\n ],\n [\n -76.81358975766166,\n 39.02588241965043\n ],\n [\n -76.75620928818147,\n 39.02588241965043\n ],\n [\n -76.75620928818147,\n 39.0799855368318\n ],\n [\n -76.81358975766166,\n 39.0799855368318\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672a21","contributors":{"authors":[{"text":"Nestler, R. 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1942 - Market classification and grading of muskrat pelts taken from Blackwater Refuge in 1941","interactions":[],"lastModifiedDate":"2014-07-21T11:29:18","indexId":"38033","displayToPublicDate":"1942-03-01T11:28:12","publicationYear":"1942","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":"209","title":"Market classification and grading of muskrat pelts taken from Blackwater Refuge in 1941","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Kellogg, C.E., 1942, Market classification and grading of muskrat pelts taken from Blackwater Refuge in 1941: Wildlife Leaflet 209, 5 p.","productDescription":"5 p.","numberOfPages":"5","costCenters":[],"links":[{"id":290558,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd664ce4b0b29085100a83","contributors":{"authors":[{"text":"Kellogg, Charles E.","contributorId":94220,"corporation":false,"usgs":true,"family":"Kellogg","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":218762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37971,"text":"37971 - 1942 - Abstract of fur laws, 1942-43","interactions":[],"lastModifiedDate":"2014-07-18T16:22:40","indexId":"37971","displayToPublicDate":"1942-01-01T16:21:31","publicationYear":"1942","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":"226","title":"Abstract of fur laws, 1942-43","docAbstract":"No abstract available.","language":"English","publisher":"United States Dept. of the Interior","publisherLocation":"Chicago, IL","collaboration":"Compiled in the Section of Fur Resources, Division of Wildlife Research.","usgsCitation":"U.S. Division Of Wildlife Research, 1942, Abstract of fur laws, 1942-43 (Revises Wildlife Leaflet BS-118 (1938).): Wildlife Leaflet 226, 43 p.","productDescription":"43 p.","numberOfPages":"43","temporalStart":"1942-01-01","temporalEnd":"1943-12-31","costCenters":[],"links":[{"id":290499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet BS-118 (1938).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4ae8e4b0b290850f00e8","contributors":{"authors":[{"text":"U.S. Division Of Wildlife Research","contributorId":128226,"corporation":true,"usgs":false,"organization":"U.S. Division Of Wildlife Research","id":529787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37970,"text":"37970 - 1942 - The status of migratory game birds: 1941-42","interactions":[],"lastModifiedDate":"2014-07-18T16:17:45","indexId":"37970","displayToPublicDate":"1942-01-01T16:17:07","publicationYear":"1942","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":"225","title":"The status of migratory game birds: 1941-42","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Department","usgsCitation":"U.S. Division Of Wildlife Research, 1942, The status of migratory game birds: 1941-42: Wildlife Leaflet 225, 9 p.","productDescription":"9 p.","numberOfPages":"9","costCenters":[],"links":[{"id":290497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd78a1e4b0b2908510c489","contributors":{"authors":[{"text":"U.S. Division Of Wildlife Research","contributorId":128226,"corporation":true,"usgs":false,"organization":"U.S. Division Of Wildlife Research","id":529786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37968,"text":"37968 - 1942 - Natural plantings for attracting waterfowl to marsh and other water areas","interactions":[],"lastModifiedDate":"2014-07-18T15:49:39","indexId":"37968","displayToPublicDate":"1942-01-01T15:49:02","publicationYear":"1942","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":"223","title":"Natural plantings for attracting waterfowl to marsh and other water areas","docAbstract":"No abstract available.","language":"English","publisher":"United States Dept. of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Prepared in the Division of Wildlife Research.","usgsCitation":"U.S. Division Of Wildlife Research, 1942, Natural plantings for attracting waterfowl to marsh and other water areas (Revises and updates Wildlife Leaflet BS-125 (1939).): Wildlife Leaflet 223, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises and updates Wildlife Leaflet BS-125 (1939).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd68b6e4b0b2908510239b","contributors":{"authors":[{"text":"U.S. Division Of Wildlife Research","contributorId":128226,"corporation":true,"usgs":false,"organization":"U.S. Division Of Wildlife Research","id":529785,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37967,"text":"37967 - 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1942 - Treatment of oil-soaked birds","interactions":[],"lastModifiedDate":"2014-07-18T13:49:48","indexId":"37966","displayToPublicDate":"1942-01-01T13:49:24","publicationYear":"1942","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":"221","title":"Treatment of oil-soaked birds","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Lincoln, F.C., 1942, Treatment of oil-soaked birds: Wildlife Leaflet 221, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290474,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7992e4b0b2908510cebc","contributors":{"authors":[{"text":"Lincoln, Frederick Charles","contributorId":91025,"corporation":false,"usgs":true,"family":"Lincoln","given":"Frederick","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":218704,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35877,"text":"b917 - 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Under existing conditions of a diversity of regulations that vary between states and between the two countries, and with the present methods of fishing, the Great Lakes fisheries are doomed. This chapter deals with the common whitefish, a valuable species which many believe to be the next that will go unless positive action is forthcoming soon.
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