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In 1906, the estimated average pumpage there was about 1,000,000 gallons a day, and by 1935 it had increased to 15,400,000 gallons a day. The water-bearing beds, consisting of sand and gravel interbedded wire clay, tie in the deep structural trough known as the Hueco bolson, between the Organ and Franklin Mountains on the west, the Hueco, Finlay, and Malone Mountains on the east, the Tularosa Basin on the north, and the mountain ranges of Mexico on the south. From the gorge above El Paso to that beginning near Fort Quitman, about 90 miles southeast .of El Paso, the Rio Grande has eroded a flat-bottomed, steepwalled valley, 6 to 8 miles wide and 225 to 350 feet deep. No other large drainage channels have been developed on the bolson. The valley is known as the El Paso Valley, and the uneroded upland part of the bolson is called the Mesa. In the lowest parts of the El Paso Valley, the water-table is nearly at the surface. The quality of the underground water in the valley varies greatly both vertically and laterally. To a depth of about 400 to 500 feet it is in general too highly mineralized for municipal use, but between about. 500 and 900 feet good water may be obtained from several beds. In the beds between 500 and 900 feet the water level in wells is in places as. much as 20 feet lower than that in the shallow beds. Beneath the Mesa the water level .varies from about 200 feet beneath the surface, where the ground elevation is least, to about 400 feet. where it is highest. The water beneath the Mesa in general is of satisfactory quality and contains less than 500 parts per million of dissolved solids. Two cones of depression in the water table have been formed by the pumping near El Paso--one m the vicinity of the Mesa well field, the other around the Montana well field in the valley. The water released from storage by the formation of the cone centering in the Mesa field was calculated at 22,000 acre-feet, but the total pumpage was estimated to have been 90,000 acre-feet. Thus, about one-fourth of the total pumpage was taken from storage; the remaining three-fourths and apparently was taken from recharge. About 210,000 acre-feet of water has been pumped from the cone of depression in the El Paso Valley in and near El Paso. The volume of this cone could not be determined because there are artesian conditions in this area. Computations were made of the amount of water that would be recovered from storage if, for a distance of 10 miles north of the Mesa well field, the water level in a series of wells were drawn down the same amount as the present drawdown in the wells in that field. The water that would be recovered from storage in the formation 0f this depression in the ground water surface was calculated at about 130,000 acre-feet, the equivalent of about 70 years' supply at the 1935 rate of pumping.It is, of course, available in addition to the annual recharge. The sudden increase in 1924 in the saltwater content of the water from El Paso well 3 (well 52), in the Montana well field, was shown to be the result of a leak in the casing at a depth of about 127 feet, and the well was successfully repaired during the investigation. However, the chloride content of all of the wells in the field has been increasing gradually. This may indicate that salty water is being pulled in from considerable distances or that the barriers between the fresh-water-bearing beds and the saltwater-bearing beds above-them are not capable of preventing vertical movement of the ground water. The fact that in the valley the static water level in the shallow beds yielding poor water is higher than that in the deeper beds is disquieting, and if the level in the lower beds continues to decline, seepage from the river will eventually force the shallow highly mineralized water
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Paso\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683c12","contributors":{"authors":[{"text":"King, Philip Burke","contributorId":15607,"corporation":false,"usgs":true,"family":"King","given":"Philip","email":"","middleInitial":"Burke","affiliations":[],"preferred":false,"id":279267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Robert E.","contributorId":91187,"corporation":false,"usgs":true,"family":"King","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":279268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knight, James Brooks","contributorId":97199,"corporation":false,"usgs":true,"family":"Knight","given":"James Brooks","affiliations":[],"preferred":false,"id":279269,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70210118,"text":"70210118 - 1945 - Structural and economic characteristics of New England mica deposits","interactions":[],"lastModifiedDate":"2021-03-22T15:24:02.172502","indexId":"70210118","displayToPublicDate":"1945-12-31T12:35:45","publicationYear":"1945","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":"Structural and economic characteristics of New England mica deposits","docAbstract":"In connection with the intensive wartime exploitation of domestic mica deposits, the Geological Survey has been engaged in a comprehensive investigation of New England mica pegmatites. More than 200 pegmatites have been mapped and studied in detail and some hundreds of others have been given brief examination. The opportunity for pegmatite study has been unprecedented, and much new information on the characteristics of pegmatites has been obtained. Geologic analysis of pegmatites has helped to clarify the relationships between mica distribution and structural features and has led to a classification of mica deposits into basic types, of which five are especially important: wall-zone, intermediate-zone, pod, fracture-controlled, and disseminated. In some pegmatites, designated complex deposits, combinations of two or more of the basic types have been found. The different types are described and illustrated and their relative economic importance is shown by production figures. Analyses show clearly that certain types of deposits are far more productive than others and are far more likely to sustain profitable mining operations. Applications of current studies to mica mining, prospecting, and exploration are discussed.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.40.6.369","usgsCitation":"Cameron, E.N., Larrabee, D., McNair, A., Page, J., Shainin, V.E., and Stewart, G.W., 1945, Structural and economic characteristics of New England mica deposits: Economic Geology, v. 40, no. 6, p. 369-393, https://doi.org/10.2113/gsecongeo.40.6.369.","productDescription":"25 p.","startPage":"369","endPage":"393","costCenters":[],"links":[{"id":374835,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Maine, New Hampshire","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.8228759765625,\n 41.347948493443546\n ],\n [\n -72.2186279296875,\n 41.347948493443546\n ],\n [\n -72.2186279296875,\n 41.72213058512578\n ],\n [\n -72.8228759765625,\n 41.72213058512578\n ],\n [\n -72.8228759765625,\n 41.347948493443546\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.36145019531249,\n 42.775243380699706\n ],\n [\n -71.927490234375,\n 42.775243380699706\n ],\n [\n -71.927490234375,\n 43.40504748787035\n ],\n [\n -72.36145019531249,\n 43.40504748787035\n ],\n [\n -72.36145019531249,\n 42.775243380699706\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.158203125,\n 43.64005063334696\n ],\n [\n -71.44958496093749,\n 43.64005063334696\n ],\n [\n -71.44958496093749,\n 44.26093725039923\n ],\n [\n -72.158203125,\n 44.26093725039923\n ],\n [\n -72.158203125,\n 43.64005063334696\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.94970703125,\n 44.07574700247845\n ],\n [\n -70.059814453125,\n 44.07574700247845\n ],\n [\n -70.059814453125,\n 44.67646564865964\n ],\n [\n -70.94970703125,\n 44.67646564865964\n ],\n [\n -70.94970703125,\n 44.07574700247845\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.1422119140625,\n 43.70362249839005\n ],\n [\n -69.5489501953125,\n 43.70362249839005\n ],\n [\n -69.5489501953125,\n 44.067853669357596\n ],\n [\n -70.1422119140625,\n 44.067853669357596\n ],\n [\n -70.1422119140625,\n 43.70362249839005\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"40","issue":"6","noUsgsAuthors":false,"publicationDate":"1945-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Cameron, Eugene N.","contributorId":59498,"corporation":false,"usgs":true,"family":"Cameron","given":"Eugene","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":789189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larrabee, David M.","contributorId":56626,"corporation":false,"usgs":true,"family":"Larrabee","given":"David M.","affiliations":[],"preferred":false,"id":789190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McNair, A.H.","contributorId":49441,"corporation":false,"usgs":true,"family":"McNair","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":789191,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Page, James J.","contributorId":23224,"corporation":false,"usgs":true,"family":"Page","given":"James J.","affiliations":[],"preferred":false,"id":789192,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shainin, Vincent E.","contributorId":59883,"corporation":false,"usgs":true,"family":"Shainin","given":"Vincent","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":789193,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stewart, G. W.","contributorId":99621,"corporation":false,"usgs":true,"family":"Stewart","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":789194,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70206842,"text":"70206842 - 1945 - Solution effects on elevated limestone terraces","interactions":[],"lastModifiedDate":"2019-11-25T07:48:42","indexId":"70206842","displayToPublicDate":"1945-12-31T07:43:53","publicationYear":"1945","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":"Solution effects on elevated limestone terraces","docAbstract":"Limestone terraces on a number of islands in the southwest Pacific show a well-developed wall or rampart along their seaward edges that apparently is formed by solution. Such rimmed terraces resemble, on a much enlarged scale, the solution facets developed on flat-lying joint blocks of limestone, recently described by Smith and Albritton (1941). In an attempt to check the interpretation of field observations, a rimmed facet was produced experimentally in the laboratory. The artificial structure appears to be very similar to the natural facets on joint blocks and in many ways closely resembles the much larger rimmed terraces of the Pacific islands. It is believed that rimmed terraces with a profile similar to that of the island of Eua, Tonga, indicate island uplift accompanied by tilting. © 1945, The Geological Society of America, Inc.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1945)56[809:SEOELT]2.0.CO;2","issn":" 00167606","usgsCitation":"Hoffmeister, J.E., and Ladd, H.S., 1945, Solution effects on elevated limestone terraces: Geological Society of America Bulletin, v. 56, no. 8, p. 809-818, https://doi.org/10.1130/0016-7606(1945)56[809:SEOELT]2.0.CO;2.","productDescription":"10 p. ","startPage":"809","endPage":"818","costCenters":[],"links":[{"id":369525,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hoffmeister, J. E.","contributorId":220861,"corporation":false,"usgs":false,"family":"Hoffmeister","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":776015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ladd, H. S.","contributorId":95537,"corporation":false,"usgs":true,"family":"Ladd","given":"H.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":776016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37891,"text":"37891 - 1945 - Dealers in upland game birds","interactions":[],"lastModifiedDate":"2014-07-22T10:38:33","indexId":"37891","displayToPublicDate":"1945-11-01T10:37:38","publicationYear":"1945","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":"281","title":"Dealers in upland game birds","docAbstract":"No abstract available.","language":"English","publisher":"U.s. Department of the Interior","publisherLocation":"Chicago, IL","collaboration":"Compiled in the Division of Wildlife Research.","usgsCitation":"U.S. Fish and Wildlife Service, 1945, Dealers in upland game birds: Wildlife Leaflet 281, 35 p.","productDescription":"35 p.","numberOfPages":"35","costCenters":[],"links":[{"id":290680,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffda09e4b0824b2d178869","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37890,"text":"37890 - 1945 - Dealers in amphibians and reptiles","interactions":[],"lastModifiedDate":"2014-07-22T10:35:51","indexId":"37890","displayToPublicDate":"1945-11-01T10:34:56","publicationYear":"1945","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":"280","title":"Dealers in amphibians and reptiles","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Chicago, IL","collaboration":"Prepared in the Division of Wildlife Research.","usgsCitation":"U.S. Fish and Wildlife Service, 1945, Dealers in amphibians and reptiles: Wildlife Leaflet 280, 3 p.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":290679,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffda09e4b0824b2d17886b","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70215110,"text":"70215110 - 1945 - Stratigraphy and structure of west-central Vermont","interactions":[],"lastModifiedDate":"2020-10-07T17:14:52.33429","indexId":"70215110","displayToPublicDate":"1945-10-07T12:00:39","publicationYear":"1945","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and structure of west-central Vermont","docAbstract":"The lithologic units recognizable in the fossiliferous succession along southern Lake Champlain are structurally continuous with and traceable eastward into the “marble belt” of west-central Vermont immediately west of the Green Mountain Front. They are also traceable northward through west-central Vermont into a succession in northwestern Vermont bounded on the east and west by major thrusts, where they pass laterally northeastward into fossiliferous shales, the faunal zones of which are correlated with those along southern Lake Champlain and in the Hudson and Mohawk valleys. The Cambrian strata are traced into west-central from northwestern Vermont whereas the Ordovician correlation is with rocks in the Mohawk-Hudson-Champlain region. Certain of the Upper Cambrian strata can be correlated with established formations of this age in both of the outlying areas.
The structural pattern reflects movements dependent upon the original distribution of sedimentary facies. Interbedded Carnbro-Ordovician limestones and dolomites grade westward into foreland sandstones and eastward into geosynclinal shales. Cambrian and early Ordovician sandstone tongues extend far to the east. Later Ordovician strata of the shale facies overlie the calcareous and sandy succession and are locally unconformable on it. In the Taconic Range allochthonous Cambrian strata of shale facies are superposed upon the autochthonous Ordovician beds. The rocks of the klippe were derived from a zone at least 50 miles east of the present westernmost exposures, arriving there by movements confined largely to the shale facies. Flexural folding and thrusting, effects of alternating competency and incompetency of the foreland sequence, affected the latter succession and possibly the Taconic Allochthone. Breaking of competent strata in the flexures initiated the thrusts; thrusting continued by the stripping of competent from incompetent beds. This was accompanied by counterclockwise rotation of the thrust slices around pivotal zones bordering on a foreland massif to the southwest. Thus rock cropping out in the north-south thrust slices originally extended northeast-southwest. The thrusts are concentric to the Adirondack crystallines and are cut by the Adirondack normal faults; probably they were warped during normal faulting and uplift of the Adirondacks.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1945)56[515:SASOWV]2.0.CO;2","usgsCitation":"Cady, W., 1945, Stratigraphy and structure of west-central Vermont: GSA Bulletin, v. 56, no. 5, p. 515-588, https://doi.org/10.1130/0016-7606(1945)56[515:SASOWV]2.0.CO;2.","productDescription":"74 p.","startPage":"515","endPage":"588","costCenters":[],"links":[{"id":379183,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Vermont","otherGeospatial":"West central vermont","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.3062744140625,\n 43.830564195198264\n ],\n [\n -72.83935546875,\n 43.82660134505382\n ],\n [\n -72.861328125,\n 44.276671273775186\n ],\n [\n -73.3062744140625,\n 44.296332880058706\n ],\n [\n -73.4051513671875,\n 44.134913443750726\n ],\n [\n -73.4161376953125,\n 43.92559366355069\n ],\n [\n -73.4161376953125,\n 43.83452678223682\n ],\n [\n -73.3062744140625,\n 43.830564195198264\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"56","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cady, Wallace M.","contributorId":146958,"corporation":false,"usgs":true,"family":"Cady","given":"Wallace M.","affiliations":[],"preferred":false,"id":800910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}