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,{"id":55276,"text":"ofr4398 - 1943 - Vanadium in Idaho and Wyoming","interactions":[],"lastModifiedDate":"2013-08-29T10:54:10","indexId":"ofr4398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"43-98","title":"Vanadium in Idaho and Wyoming","language":"ENGLISH","doi":"10.3133/ofr4398","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1943, Vanadium in Idaho and Wyoming: U.S. Geological Survey Open-File Report 43-98, 3 p., https://doi.org/10.3133/ofr4398.","productDescription":"3 p.","costCenters":[],"links":[{"id":181931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602c82","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":755,"text":"wsp937 - 1943 - Water levels and artesian pressure in observation wells in the United States, 1941, Part 2, Southeastern States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"937","title":"Water levels and artesian pressure in observation wells in the United States, 1941, Part 2, Southeastern States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp937","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1943, Water levels and artesian pressure in observation wells in the United States, 1941, Part 2, Southeastern States: U.S. Geological Survey Water Supply Paper 937, iv, 119 p. ;23 cm., https://doi.org/10.3133/wsp937.","productDescription":"iv, 119 p. ;23 cm.","costCenters":[],"links":[{"id":136410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0937/report-thumb.jpg"},{"id":25322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0937/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa0f0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":754,"text":"wsp936 - 1943 - Water levels and artesian pressure in observation wells in the United States, 1941, Part 1, Northeastern States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp936","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"936","title":"Water levels and artesian pressure in observation wells in the United States, 1941, Part 1, Northeastern States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp936","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1943, Water levels and artesian pressure in observation wells in the United States, 1941, Part 1, Northeastern States: U.S. Geological Survey Water Supply Paper 936, iv, 251 p. ;23 cm., https://doi.org/10.3133/wsp936.","productDescription":"iv, 251 p. ;23 cm.","costCenters":[],"links":[{"id":136409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0936/report-thumb.jpg"},{"id":25321,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0936/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa0ed","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":757,"text":"wsp939 - 1943 - Water levels and artesian pressure in observation wells in the United States, 1941, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp939","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"939","title":"Water levels and artesian pressure in observation wells in the United States, 1941, Part 4, South-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp939","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1943, Water levels and artesian pressure in observation wells in the United States, 1941, Part 4, South-Central States: U.S. Geological Survey Water Supply Paper 939, iii, 178 p. ;23 cm., https://doi.org/10.3133/wsp939.","productDescription":"iii, 178 p. ;23 cm.","costCenters":[],"links":[{"id":136412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0939/report-thumb.jpg"},{"id":25324,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0939/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494a4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":759,"text":"wsp941 - 1943 - Water levels and artesian pressure in observation wells in the United States, 1941, Part 6, Southwestern States and Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"941","title":"Water levels and artesian pressure in observation wells in the United States, 1941, Part 6, Southwestern States and Hawaii","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp941","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1943, Water levels and artesian pressure in observation wells in the United States, 1941, Part 6, Southwestern States and Hawaii: U.S. Geological Survey Water Supply Paper 941, iv, 282 p. ;23 cm., https://doi.org/10.3133/wsp941.","productDescription":"iv, 282 p. ;23 cm.","costCenters":[],"links":[{"id":136414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0941/report-thumb.jpg"},{"id":25326,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0941/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa169","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53632,"text":"ofr4617 - 1943 - Tungsten deposits in the southern Santa Rosa mountains, Paradise district, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr4617","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"46-17","title":"Tungsten deposits in the southern Santa Rosa mountains, Paradise district, Humboldt County, Nevada","language":"ENGLISH","doi":"10.3133/ofr4617","usgsCitation":"Chesterman, C., Joralemon, P., and Klepper, M.R., 1943, Tungsten deposits in the southern Santa Rosa mountains, Paradise district, Humboldt County, Nevada: U.S. Geological Survey Open-File Report 46-17, 4 p.; 3 maps, https://doi.org/10.3133/ofr4617.","productDescription":"4 p.; 3 maps","costCenters":[],"links":[{"id":177065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1946/0017/report-thumb.jpg"},{"id":87495,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0017/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87496,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1946/0017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624052","contributors":{"authors":[{"text":"Chesterman, C.W.","contributorId":13626,"corporation":false,"usgs":true,"family":"Chesterman","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":247960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joralemon, P.","contributorId":99213,"corporation":false,"usgs":true,"family":"Joralemon","given":"P.","affiliations":[],"preferred":false,"id":247962,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klepper, M. R.","contributorId":64278,"corporation":false,"usgs":true,"family":"Klepper","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":247961,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11651,"text":"ofr79352 - 1943 - Preliminary report on Orange and Gove copper mines, Strafford, Vermont","interactions":[],"lastModifiedDate":"2023-08-25T21:29:16.17488","indexId":"ofr79352","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-352","title":"Preliminary report on Orange and Gove copper mines, Strafford, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79352","usgsCitation":"White, W., Eric, J.H., and Amsden, T.W., 1943, Preliminary report on Orange and Gove copper mines, Strafford, Vermont: U.S. Geological Survey Open-File Report 79-352, 4 p., https://doi.org/10.3133/ofr79352.","productDescription":"4 p.","costCenters":[],"links":[{"id":39509,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0352/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143828,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0352/report-thumb.jpg"}],"country":"United States","state":"Vermont","city":"Strafford","otherGeospatial":"Orange and Gove copper mines","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.3553,\n              43.8886\n            ],\n            [\n              -72.3553,\n              43.8861\n            ],\n            [\n              -72.3514,\n              43.8861\n            ],\n            [\n              -72.3514,\n              43.8886\n            ],\n            [\n              -72.3553,\n              43.8886\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cb98","contributors":{"authors":[{"text":"White, Walter S.","contributorId":34492,"corporation":false,"usgs":true,"family":"White","given":"Walter S.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":163508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eric, John H.","contributorId":89530,"corporation":false,"usgs":true,"family":"Eric","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":163509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Amsden, Thomas William","contributorId":25153,"corporation":false,"usgs":true,"family":"Amsden","given":"Thomas","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":163507,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70206703,"text":"70206703 - 1943 -  Geology of the Cimarron Range, New Mexico","interactions":[],"lastModifiedDate":"2019-11-18T12:49:56","indexId":"70206703","displayToPublicDate":"1943-12-31T12:41:16","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":" Geology of the Cimarron Range, New Mexico","docAbstract":"<p><span>In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks. Faulting along the eastern and western margins of the anticline separates the mountains from the Great Plains and the Moreno Valley. North of Cimarron Canyon the anticline plunges beneath the Tertiary sediments of the Raton Coal Basin. To the south the structure is obscured by the basaltic flows of the Ocaté Mesa. Upturned Paleozoic to Tertiary sedimentary rocks crop out along the eastern and northern margin of the anticlinal uplift. Regional relations are obscured by extensive Tertiary intrusions in the northern portion of the area and by the lava flows to the south. In the valley of Rayado Creek a volcanic plug which fed some of the lava flows has been exposed by erosion. In this region there is evidence for a Mid-Tertiary surface of low relief in the central portion of the mountains, a later lava-capped surface believed to be the equivalent of the Broad Valley Stage, the surface of the Park Plateau, and the Ocate Mesa. Three well-developed gravel-capped Pleistocene pediment surfaces extend steplike from the mountain front into the Great Plains. Both structurally and topographically the Cimarron Range is similar to the Colorado Front Range. An attempt is made to reconstruct the geologic history of the Cimarron Range and to fit it into the broader story of the development of the Southern Rocky Mountains in New Mexico. © 1943 Geological Society of America.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.1130/GSAB-54-891","issn":"00167606","usgsCitation":"Smith , J., and Ray, L., 1943,  Geology of the Cimarron Range, New Mexico: Geological Society of America Bulletin, v. 54, no. 7, p. 891-924, https://doi.org/10.1130/GSAB-54-891.","productDescription":"34 p. 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,{"id":70206099,"text":"70206099 - 1943 - Quartz veins in the Ouachita mountains of Arkansas and Oklahoma (Their relations to structure, metamorphism, and metalliferous deposits)?","interactions":[],"lastModifiedDate":"2019-10-22T09:54:59","indexId":"70206099","displayToPublicDate":"1943-10-22T09:48:18","publicationYear":"1943","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":"Quartz veins in the Ouachita mountains of Arkansas and Oklahoma (Their relations to structure, metamorphism, and metalliferous deposits)?","docAbstract":"<p>An important chapter of the total geologic history of the Ouachita Mountains is revealed by the quartz veins and crystals. These and the associated minerals are hydrothermal deposits of probable magmatic origin, formed during the closing stage of the mid-Permsylvanian orogeny. The metalliferous deposits of the Ouachita Mountains appear to have been formed at the time of the quartz vein deposition. This /act should be considered in dating the lead and zinc mineralization in other areas of the Mississippi Valley region. © 1943 Society of Economic Geologists, Inc.</p>","language":"English ","publisher":"Elsevier","doi":"10.2113/gsecongeo.38.2.91","issn":"03610128","usgsCitation":"Miser, H.D., 1943, Quartz veins in the Ouachita mountains of Arkansas and Oklahoma (Their relations to structure, metamorphism, and metalliferous deposits)?: Economic Geology, v. 38, no. 2, p. 91-118, https://doi.org/10.2113/gsecongeo.38.2.91.","productDescription":"28 p. ","startPage":"91","endPage":"118","costCenters":[],"links":[{"id":368484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Arkansas, Oklahoma ","otherGeospatial":"Ouachita mountains ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.976318359375,\n              34.00713506435885\n            ],\n            [\n              -92.142333984375,\n              34.00713506435885\n            ],\n            [\n              -92.142333984375,\n              35.862343734896484\n            ],\n            [\n              -96.976318359375,\n              35.862343734896484\n            ],\n            [\n              -96.976318359375,\n              34.00713506435885\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"38","issue":"2","noUsgsAuthors":false,"publicationDate":"1943-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Miser, Hugh Dinsmore","contributorId":95130,"corporation":false,"usgs":true,"family":"Miser","given":"Hugh","email":"","middleInitial":"Dinsmore","affiliations":[],"preferred":false,"id":773574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213056,"text":"70213056 - 1943 - A frequency‐method of evaluating ground‐water levels","interactions":[],"lastModifiedDate":"2020-09-08T17:48:35.321791","indexId":"70213056","displayToPublicDate":"1943-09-09T12:40:07","publicationYear":"1943","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 frequency‐method of evaluating ground‐water levels","docAbstract":"<p><span>Water‐levels in wells, which are utilized by the hydrologist as a measure of ground‐water storage, customarily are measured in terms of distance below a convenient measuring point and expressed with reference to a fixed datum. Datum‐planes or surfaces of several types have been used—each serving some particular purpose advantageously. These include: “Planes” of regional extent, such as mean sea‐level; irregular surfaces defining a particular hydrologic condition, such as low‐water level (if known) or the water‐level on some particular date; and local reference‐planes at each observation‐well, such as a horizontal plane through the measuring point or at the average height of the land‐surface. Recently the Geological Survey has considered the standard use of a land‐surface datum, precisely defined for each observation‐well. This procedure has the practical advantage that the water‐levels can be recorded in final form as soon as the initial measurement is made, without leveling to establish a regional datum or waiting to accumulate sufficient data for defining a particular hydrologic condition.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i002p00573","usgsCitation":"Huff, L.C., 1943, A frequency‐method of evaluating ground‐water levels: Eos, Transactions, American Geophysical Union, v. 24, no. 2, p. 573-580, https://doi.org/10.1029/TR024i002p00573.","productDescription":"8 p.","startPage":"573","endPage":"580","costCenters":[],"links":[{"id":378213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Huff, Lyman C.","contributorId":47440,"corporation":false,"usgs":true,"family":"Huff","given":"Lyman","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":798087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213061,"text":"70213061 - 1943 - Correlation of ground‐water levels and precipitation on Long Island, New York","interactions":[],"lastModifiedDate":"2020-09-09T13:49:09.514078","indexId":"70213061","displayToPublicDate":"1943-09-08T13:57:03","publicationYear":"1943","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":"Correlation of ground‐water levels and precipitation on Long Island, New York","docAbstract":"<p><span>Long Island simulates in a general way an aquifer in the form of an infinite strip confined between parallel boundaries at constant head (sea‐level), over which recharge precipitation is assumedly uniform. The non‐steady flow of water in this idealized system is analyzed assuming provisionally that the effective thickness of saturated beds below sea‐level is great compared to the maximum height of the water‐table above sea‐level. The rate of accretion to the water‐table is assumed to vary discontinuously, supposedly being constant for each of the successive periods (yearly or monthly) and proportional to the average rate of precipitation during that period. The decay of the water‐table profile, beginning with any one of the succession of super‐posed non‐steady states, is shown to follow in general a relation composed of terms varying with time as exp(−t/t</span><sub>o</sub><span>) in which t</span><sub>o</sub><span>&nbsp;is a function of the effective porosity, the thickness and the transmission‐constant of the aquifer. This exponential curve may be approximated by a parabola which is used to determine values of “effective average rate of precipitation” from published records in annual or monthly precipitation. By the “effective average rate of precipitation” at any time is meant that rate of precipitation which, had it been maintained uninterruptedly throughout the past, would have produced the same water‐table profile as actually existed at that particular time. It is demonstrated that fee effective average rate of precipitation may be determined also simply by cumulating departures from progressive averages of precipitation, multiplying the values thus determined by a known rational coefficient, and adding the appropriate initial value of effective average precipitation.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i002p00564","usgsCitation":"Jacob, C.E., 1943, Correlation of ground‐water levels and precipitation on Long Island, New York: Eos, Transactions, American Geophysical Union, v. 24, no. 2, p. 564-573, https://doi.org/10.1029/TR024i002p00564.","productDescription":"10 p.","startPage":"564","endPage":"573","costCenters":[],"links":[{"id":378217,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.036865234375,\n              40.58058466412761\n            ],\n            [\n              -71.8341064453125,\n              40.58058466412761\n            ],\n            [\n              -71.8341064453125,\n              41.18278832811288\n            ],\n            [\n              -74.036865234375,\n              41.18278832811288\n            ],\n            [\n              -74.036865234375,\n              40.58058466412761\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","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":798092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213059,"text":"70213059 - 1943 - The Finley Site: Antiquity of the Finley Site","interactions":[],"lastModifiedDate":"2020-09-08T18:33:30.322507","indexId":"70213059","displayToPublicDate":"1943-09-08T13:12:23","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":700,"text":"American Antiquity","active":true,"publicationSubtype":{"id":10}},"title":"The Finley Site: Antiquity of the Finley Site","docAbstract":"<p>This report is based on two months reconnaissance in the summer of 1941 in the Eden Valley, Wyoming. The work is as yet far from complete and the conclusions presented here must be regarded as tentative. It is hoped that in the future more extensive geological work may be undertaken.</p><p>The Finley site provides a promising opportunity for a determination of the age of the Yuma culture. The points and bones described by Dr. Howard occur in a culture layer which has been found in a large dune area, here called the Killpecker dunes. The deposition of the culture layer is one of a series of events in the dune area which can be correlated with the cutting and filling of gravel terraces in the Eden Valley to the west, and these in turn may be related to the glacial chronology in the Wind River Mountains which lie to the north.</p>","language":"English","publisher":"Society for American Archaeology","doi":"10.2307/275903","usgsCitation":"Hack, J., 1943, The Finley Site: Antiquity of the Finley Site: American Antiquity, v. 8, no. 3, p. 235-241, https://doi.org/10.2307/275903.","productDescription":"7 p.","startPage":"235","endPage":"241","costCenters":[],"links":[{"id":378215,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Eden Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.06103515625,\n              41.49623534616764\n            ],\n            [\n              -108.67675781249999,\n              41.49623534616764\n            ],\n            [\n              -108.67675781249999,\n              42.28950073090457\n            ],\n            [\n              -110.06103515625,\n              42.28950073090457\n            ],\n            [\n              -110.06103515625,\n              41.49623534616764\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Hack, John T.","contributorId":45168,"corporation":false,"usgs":true,"family":"Hack","given":"John T.","affiliations":[],"preferred":false,"id":798090,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213033,"text":"70213033 - 1943 - The mosses of Luray Cavern, Virginia","interactions":[],"lastModifiedDate":"2020-09-08T15:14:28.880812","indexId":"70213033","displayToPublicDate":"1943-09-04T14:05:06","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"The mosses of Luray Cavern, Virginia","docAbstract":"<p>No abstract available.</p>","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.98.2538.173","usgsCitation":"Lang, W., 1943, The mosses of Luray Cavern, Virginia: Science, v. 98, no. 2538, p. 173-174, https://doi.org/10.1126/science.98.2538.173.","productDescription":"2 p","startPage":"173","endPage":"174","costCenters":[],"links":[{"id":378174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","city":"Luray","otherGeospatial":"Luray Caverns","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.49800109863281,\n              38.65991177565927\n            ],\n            [\n              -78.47551345825195,\n              38.65991177565927\n            ],\n            [\n              -78.47551345825195,\n              38.67197479347275\n            ],\n            [\n              -78.49800109863281,\n              38.67197479347275\n            ],\n            [\n              -78.49800109863281,\n              38.65991177565927\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"98","issue":"2538","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lang, Walter B.","contributorId":27507,"corporation":false,"usgs":true,"family":"Lang","given":"Walter B.","affiliations":[],"preferred":false,"id":798018,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213032,"text":"70213032 - 1943 - A method for determining transmissibility‐ and storage‐coefficients by tests of multiple well‐systems","interactions":[],"lastModifiedDate":"2020-09-04T19:02:30.486128","indexId":"70213032","displayToPublicDate":"1943-09-04T13:56:02","publicationYear":"1943","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 method for determining transmissibility‐ and storage‐coefficients by tests of multiple well‐systems","docAbstract":"<p><span>Ground‐water has long been recognized as one of our important natural resources, but only in about the last 20 years has concentrated effort been made to place ground‐water hydrology on a quantitative basis. The quantitative approach to ground‐water work has been brought about largely through the leadership of O. E. MEINZER, Chief of the Ground‐Water Division of the Geological Survey, United States Department of the Interior, who has originated and applied many quantitative methods himself, and who has consistently fostered and encouraged this method of attack by his coworkers. That this effort has been ably directed and especially fruitful Is shown by the vast number of important ground‐water problems relating to the water‐supplies for war activities that have been worked out by means of quantitative methods in the last few years.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i002p00547","usgsCitation":"Wenzel, L., and Greenlee, A., 1943, A method for determining transmissibility‐ and storage‐coefficients by tests of multiple well‐systems: Eos, Transactions, American Geophysical Union, v. 24, no. 2, p. 547-564, https://doi.org/10.1029/TR024i002p00547.","productDescription":"18 p.","startPage":"547","endPage":"564","costCenters":[],"links":[{"id":378173,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, Leland K.","contributorId":46077,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland K.","affiliations":[],"preferred":false,"id":798016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greenlee, A.L.","contributorId":239885,"corporation":false,"usgs":false,"family":"Greenlee","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":798017,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70213030,"text":"70213030 - 1943 - Helvite, a product of magmatic emanations at Iron Mountain, Sierra Socorro Counties, New Mexico","interactions":[],"lastModifiedDate":"2020-09-04T18:51:08.627991","indexId":"70213030","displayToPublicDate":"1943-09-04T13:19:42","publicationYear":"1943","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":"Helvite, a product of magmatic emanations at Iron Mountain, Sierra Socorro Counties, New Mexico","docAbstract":"<p><span>The recent discovery of the widespread occurrence of helvite, a beryllium‐bearing mineral, at Iron Mountain, New Mexico, has aroused interest in the commercial possibilities of a mineral which heretofore has been considered to have only scientific significance. Helvite contains about 13 per cent beryllium oxide as compared with five to ten per cent beryllium oxide in the mineral, beryl, which at present is the principal source of commercial beryllium. Helvite is consistently distributed, though sparingly in some places, through great masses of contact‐metamorphic rock at Iron Mountain and, therefore, provides great hope for the future when the metallurgical problems have been solved and large‐tonnage, low‐grade ore can be utilized.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i001p00252","usgsCitation":"Glass, J.J., 1943, Helvite, a product of magmatic emanations at Iron Mountain, Sierra Socorro Counties, New Mexico: Eos, Transactions, American Geophysical Union, v. 24, no. 1, p. 252-257, https://doi.org/10.1029/TR024i001p00252.","productDescription":"5 p.","startPage":"252","endPage":"257","costCenters":[],"links":[{"id":378171,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Iron Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.5064697265625,\n              31.863562548378965\n            ],\n            [\n              -106.962890625,\n              31.863562548378965\n            ],\n            [\n              -106.962890625,\n              34.52918706954935\n            ],\n            [\n              -108.5064697265625,\n              34.52918706954935\n            ],\n            [\n              -108.5064697265625,\n              31.863562548378965\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Glass, Jewell J.","contributorId":106948,"corporation":false,"usgs":true,"family":"Glass","given":"Jewell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":798014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213028,"text":"70213028 - 1943 - Report of Committee on Runoff, 1942–43","interactions":[],"lastModifiedDate":"2020-09-04T18:02:40.604887","indexId":"70213028","displayToPublicDate":"1943-09-04T12:45:06","publicationYear":"1943","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 Runoff, 1942–43","docAbstract":"<p>The Committee on Runoff was not formally constituted until February 6, 1943, when the members of the Section, as listed above, were asked to serve. At the suggestion of President CHURCH the Committee has been so selected that there is Nation‐wide geographic distribution from West to East with the majority of the Committee composed of younger men.</p><p>If the 33 papers prepared for discussion at the regular sessions of the Section of Hydrology at the annual meeting of 1943 can be used as a measure, war instead of curtailing the activities of the Section has acted as an impetus. Also in the field of hydrology as a whole, war activities have apparently not resulted in a decrease of activities. There has been, however, a gradual decrease of activities in the field of research and an increase of activities in the field of applied hydrology. The enormous expansion of our industrial machine and the great concentration of armies and industrial workers into restricted areas; the demands for water, for power, for food and for municipal use; and operations underlying many of our war efforts, secret and otherwise—all these have created problems requiring the full‐time effort of hydrologists, both in private and governmental service. It is with some degree of satisfaction that each one of us can feel that either as a result of our past research or in our present positions we have been or are doing our bit to win the war.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i002p00422","usgsCitation":"Hoyt, W.G., Barnes, B., Cooke, H., Cullings, E., Hathaway, G., Jetter, K.R., Leupold, N., Light, P., McDonald, C.C., Mavis, F., Sherman, L., Smith, W.E., Snyder, F., and Wilm, H., 1943, Report of Committee on Runoff, 1942–43: Eos, Transactions, American Geophysical Union, v. 24, no. 2, p. 422-423, https://doi.org/10.1029/TR024i002p00422.","productDescription":"2 p.","startPage":"422","endPage":"423","costCenters":[],"links":[{"id":378169,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hoyt, W. 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,{"id":70213027,"text":"70213027 - 1943 - Appendix B—The work of the Geological Survey and cooperating state agencies on ground water for war purposes","interactions":[],"lastModifiedDate":"2020-09-04T17:43:26.120553","indexId":"70213027","displayToPublicDate":"1943-09-04T12:30:19","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"title":"Appendix B—The work of the Geological Survey and cooperating state agencies on ground water for war purposes","docAbstract":"<p><span>The very large service which the geologists and engineers trained in ground‐water hydrology are rendering in this country in the prosecution of the war is due largely to the effective organization for this purpose. The Federal agency in which this service centers is the Water Resources Branch of the United States Geological Survey. The Ground Water Division of this branch has a technical personnel of nearly 100 geologists, engineers, and physicists, and its work is supported by the chemists of the Quality of Water Division and the engineers of the other Divisions of the Branch. It functions through a central office in Washington and 25 widely distributed field‐offices. Moreover, this service is effectively supported by the State Geological surveys, State Engineer offices, and other State agencies concerned with water‐resources, not only in the 34 States in which there is formal cooperation with the Federal Geological Survey in ground‐water investigations but also in those States in which there are no formal cooperative agreements. The magnitude of the civilian service rendered is indicated by the fact that to date about 1,600 reports on water‐supplies from wells have been made to the War and Navy Departments and other war agencies by the Geological Survey and cooperating State organizations.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i002p00418-2","usgsCitation":"Meinzer, O.E., 1943, Appendix B—The work of the Geological Survey and cooperating state agencies on ground water for war purposes, v. 24, no. 2, p. 418-420, https://doi.org/10.1029/TR024i002p00418-2.","productDescription":"3 p.","startPage":"418","endPage":"420","costCenters":[],"links":[{"id":378168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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