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,{"id":47090,"text":"ofr5625 - 1956 - Five preliminary maps of Kit Carson County, Colorado, showing the depth to the water table in the principal aquifer, altitude of the surface of the Pierre Shale, and depth to the Pierre shale","interactions":[],"lastModifiedDate":"2012-02-02T00:05:00","indexId":"ofr5625","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-25","title":"Five preliminary maps of Kit Carson County, Colorado, showing the depth to the water table in the principal aquifer, altitude of the surface of the Pierre Shale, and depth to the Pierre shale","language":"ENGLISH","doi":"10.3133/ofr5625","usgsCitation":"Chase, G.H., 1956, Five preliminary maps of Kit Carson County, Colorado, showing the depth to the water table in the principal aquifer, altitude of the surface of the Pierre Shale, and depth to the Pierre shale: U.S. Geological Survey Open-File Report 56-25, 5 maps., https://doi.org/10.3133/ofr5625.","productDescription":"5 maps.","costCenters":[],"links":[{"id":135585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0025/report-thumb.jpg"},{"id":84123,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0025/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84124,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0025/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84125,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0025/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84126,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0025/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84127,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0025/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84128,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef34f","contributors":{"authors":[{"text":"Chase, George Holden","contributorId":55789,"corporation":false,"usgs":true,"family":"Chase","given":"George","email":"","middleInitial":"Holden","affiliations":[],"preferred":false,"id":234612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46516,"text":"ofr56123 - 1956 - Map showing chemical quality of ground water, Otero County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:39","indexId":"ofr56123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-123","title":"Map showing chemical quality of ground water, Otero County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr56123","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1956, Map showing chemical quality of ground water, Otero County, New Mexico: U.S. Geological Survey Open-File Report 56-123, 1 map., https://doi.org/10.3133/ofr56123.","productDescription":"1 map.","costCenters":[],"links":[{"id":172505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659bd6","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":531694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68673,"text":"ha6 - 1956 - Reconnaissance of the geology and ground-water resources of southern Sioux County, Nebraska with a section on chemical quality of ground water","interactions":[],"lastModifiedDate":"2012-02-02T00:13:43","indexId":"ha6","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"6","title":"Reconnaissance of the geology and ground-water resources of southern Sioux County, Nebraska with a section on chemical quality of ground water","language":"ENGLISH","doi":"10.3133/ha6","usgsCitation":"Bradley, E., and Rainwater, F.H., 1956, Reconnaissance of the geology and ground-water resources of southern Sioux County, Nebraska with a section on chemical quality of ground water: U.S. Geological Survey Hydrologic Atlas 6, 2 maps on 2 sheets ;32 x 38 cm. each., https://doi.org/10.3133/ha6.","productDescription":"2 maps on 2 sheets ;32 x 38 cm. each.","costCenters":[],"links":[{"id":251466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/006/report.pdf","size":"2116","linkFileType":{"id":1,"text":"pdf"}},{"id":252445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/006/report-thumb.jpg"}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636d40","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":278699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rainwater, Francis Hays","contributorId":43045,"corporation":false,"usgs":true,"family":"Rainwater","given":"Francis","email":"","middleInitial":"Hays","affiliations":[],"preferred":false,"id":278698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69587,"text":"i175 - 1956 - Paleotectonic maps, Jurassic system","interactions":[],"lastModifiedDate":"2020-07-31T18:15:59.008758","indexId":"i175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"175","title":"Paleotectonic maps, Jurassic system","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i175","usgsCitation":"McKee, E.D., Oriel, S.S., Swanson, V., MacLachlan, M.E., MacLachlan, J., Ketner, K.B., Goldsmith, J.W., Bell, R.Y., Jameson, D.J., and Imlay, R.W., 1956, Paleotectonic maps, Jurassic system: U.S. Geological Survey IMAP 175, 1 Atlas: 6 p., 9 Plates, https://doi.org/10.3133/i175.","productDescription":"1 Atlas: 6 p., 9 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,{"id":68202,"text":"ha8 - 1956 - Availability of ground water for domestic use in Jefferson County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha8","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"8","title":"Availability of ground water for domestic use in Jefferson County, Kentucky","language":"ENGLISH","doi":"10.3133/ha8","usgsCitation":"MacCary, L., 1956, Availability of ground water for domestic use in Jefferson County, Kentucky: U.S. Geological Survey Hydrologic Atlas 8, 1 map ;43 x 49 cm., https://doi.org/10.3133/ha8.","productDescription":"1 map ;43 x 49 cm.","costCenters":[],"links":[{"id":252272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/008/report-thumb.jpg"},{"id":251448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/008/report.pdf","size":"2188","linkFileType":{"id":1,"text":"pdf"}}],"scale":"9750","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.91666666666667,38 ], [ -85.91666666666667,38.36666666666667 ], [ -82.41666666666667,38.36666666666667 ], [ -82.41666666666667,38 ], [ -85.91666666666667,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6671cf","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":277833,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37536,"text":"ssrw30 - 1956 - Waterfowl populations and breeding conditions - summer 1955","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"ssrw30","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"30","title":"Waterfowl populations and breeding conditions - summer 1955","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1956, Waterfowl populations and breeding conditions - summer 1955 (Updates and revises Special Scientific Report-Wildlife 25 (1952)): Special Scientific Report  - Wildlife 30, 267 p.","productDescription":"267 p.","numberOfPages":"267","costCenters":[],"links":[{"id":162454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101740,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486694?urlappend=%3Bseq=9"}],"edition":"Updates and revises Special Scientific Report-Wildlife 25 (1952)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bc4","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37539,"text":"ssrw33 - 1956 - 1956 status report of waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"ssrw33","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"33","title":"1956 status report of waterfowl","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Crissey, W.F., 1956, 1956 status report of waterfowl (Updates and revises Special Scientific Report-Wildlife 29 (1954)): Special Scientific Report  - Wildlife 33, 110 p.","productDescription":"110 p.","numberOfPages":"110","costCenters":[],"links":[{"id":165477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101743,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486694?urlappend=%3Bseq=453"}],"edition":"Updates and revises Special Scientific Report-Wildlife 29 (1954)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd490fe4b0b290850eed8b","contributors":{"authors":[{"text":"Crissey, W. F. (compiler)","contributorId":74046,"corporation":false,"usgs":true,"family":"Crissey","given":"W.","suffix":"(compiler)","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":218228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39149,"text":"pp288 - 1956 - Surficial geology and geomorphology of Potter County, Pennsylvania","interactions":[],"lastModifiedDate":"2022-03-31T20:22:47.985301","indexId":"pp288","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"288","title":"Surficial geology and geomorphology of Potter County, Pennsylvania","docAbstract":"<p>Potter County is located in the Appalachian Plateaus of north-central Pennsylvania and contains the headwaters of the Genesee River, the Allegheny River, and the Susquehanna River. Drift of Wisconsin age covers the northeastern part of the county. This study includes a detailed survev of the surficial deposits of the Genesee quadrangle in north-central Potter County and a reconnaissance of the remainder of the county; a soil survey and a botanical survey were carried on concurrently. The region is a deeply dissected plateau having extensive areas of steeply sloping land separated by narrow ridges and valleys; there is very little level land. Near the junction of the three watersheds the uplands rise to altitudes of more than 2,500 feet. The maximum relief in the Susquehanna drainage is more than 1,500 feet; in the Genesee and Allegheny drainage it. is about 800 feet. Valley walls are steep (15° to 30°), and the uplands have gentle slopes (0.5° to 10°). The drainage pattern is trellised. The climate is continental. Temperatures range from about -30° F. to more than 100° F. The average annual precipitation ranges approximately from 34 to 42 inches. Floods may occur at any season of the year. The large volumes of water from rain or melting snow carried by small streams come from springs. There is little precise data on frost in the ground, but it is probable that the ground seldom freezes in forested areas. The soils of Potter County have relatively immature profiles with poorly developed horizons that commonly have many characteristics inherited from their parent materials. At the great soil group level, the zonal soils are divided into Podzol soils and Brown Podzolic soils. Many soils have a high silt content in the upper part of the profile, apparently derived (at least partly) from a mantle of eolian silt. Mos~ of Potter County is covered by second-growth forests consisting of 40- to 60-year-old hardwood stands. The present forests growing on slopes and summits are composed approximately of 25 species of trees. The northern hardwood region includes most of the county, with an oak-forest region near the borders, principally along its southern margin. Potter County is underlain by sandstone, siltstone, shale, conglomerate, and minor amounts of coal and calcareous rock that range in age from Late Devonian to Pennsylvanian. These rocks form broad open folds that strike northeast. South of the border of the Wisconsin drift, and possibly at two localities inside the drift border, are scattered remnants of ancient soils (here called paleosol), that were formed in preWisconsin time-probably during the Sangamon interglacial stage. This paleosol ranges in texture from clay loam to silt loam, ranges in color from yellowish red to red, includes a few percent to more than 25 percent of rock fragments, and apparently contains a small percentage of gibbsite and varying amounts of kaolinite. Known thicknesses range from 1 to 33 feet. Paleosol was developed on diverse kinds of parent material, such as till, stratified drift, colluvium, and residuum, at altitudes ranging from a few hundred to 2,400 feet. The climatic conditions under which the paleosol formed are uncertain; however, these ancient soils may record an episode of subtropical climatic conditions during which lateritic soils were formed. Perhaps these soils are analogous to the Red-Yellow Podzolic soils of southeastern United States. Except for one possible remnant, no pre-Wisconsin drift has been recognized in Potter County. The Wisconsin glacial deposits of Potter County belong to either the Iowan or Tazewell substages and are dominantly till with minor amounts of glaciofluvial deposits. Erratics of igneous or metamorphic rock comprise less than 0.1 percent of the total number of rock fragments. The till is slightly weathered to depths ranging from 3 to about 12 feet. The drift border is indefinite and has been drawn at the southern limit of erratics or well-rounded or striated pebbles and is only locally marked by a terminal moraine or by a distinct change in the surficial deposits. The drift border is relatively straight and crosses the Genesee quadrangle in a northwesterly direction with little regard for the major topographic features, thus suggesting that the Wisconsin ice sheet had a relatively straight and steep front. Over most of the unglaciated part of Potter County, the bedrock is concealed beneath rubble that probably was formed during the Iowan or Tazewell substage, almost contemporaneously with the adjacent drift. In general, the rubble is thickest and most extensive within about 10 miles of the drift border, becoming thinner and less continuous farther away. The apparent parallelism between a belt of thick periglacial deposits and the drift border suggests that the deposits result from climatic factors in operation while the Wisconsin ice sheet was nearby. Ancient soil structures or patterned ground occur at, or near, the surface of both the periglacial deposits and the adjacent drift. These ancient soil structures are so similar to modern forms in arctic or alpine environments that they are considered to be the result of vigorous frost action. Many of the structures are believed to be a result of down-slope movement of debris by solifluction, facilitated by a frozen subsoil as much as 10 feet deep. Perennially frozen ground may have been present, but this is not a prerequisite. The periglacial deposits underlie long smooth slopes that extend from ridge crest to valley bottom. Flood plains are absent near the headwaters of many streams, the valley walls forming a V-shaped profile. While frost action was in progress, forests probably were restricted to flood plains, lower slopes, and scattered upland areas. Large parts of the upland were bare or partly covered by tundra vegetation; elsewhere, there were scattered trees but no dense forest. 1 2 SURFICIAL GEOLOGY AND GEOMORPHOLOGY OF POTTER COUNTY, PENNSYLVANIA Recent alluvium and alluvial fans include sand and sandy loams, 1 to 3 feet thick, that overlie gravel. The alluvium contains organic matter and lenses of finer materials. Thickness ranges from a few to more than 100 feet. Along the principal streams the alluvium probably overlies Pleistocene deposits. Most of the alluvial fans are composed of unstratified rubbly, pebbly, cobbly. or bouldery sandy loams to silty clay loams with local lenses of stratified sand and gravel. The alluvial fans mapped in the Genesee quadrangle probably include both Wisconsin stage and Recent deposits. The summits of the A.ppalachian Plateaus in north-central Pennsylvania have long been recognized as the remnants or traces of one or more peneplains. To test this hypothesis, a restored contour map was prepared to show the configuration of a supposed peneplain on the assumption that the plateau tops are remnants of such an old erosion surface. The restored contours delineate a surface that corresponds roughly to rock structure. In general, the uplands slope parallel to the dip of the bedrock. The major streams, such as the West Branch Susquehanna River, cross the ridges and valleys of the restored surface in such a way that it is difficult to suppose that the restored surface was ever graded to these streams. On the contrary, it is probable that the restored surface never existed and that the plateau tops are structurally controlled surfaces held up by sandstone and conglomerate beds in the Pottsville and Pocono formations. The plateau tops may have been lowered by erosion as much as 200 feet during the Pleistocene-in other words, after the major streams were incised. If this portion of the Appalachian Plateaus was ever reduced to a peneplain, such a hypothetical surface must have lain many hundreds of feet above the uplands of the present day. The only alternative that might involve peneplanation is the improbable hypothesis that the plateau tops are remnants of a slightly deformed peneplain and that the peneplain was folded along the axes of the Appalachian orogeny. This remote possibility is not supported by any known evidence. The geomorphic analysis yields no new data on the origin of the cross-axial drainage. Regardless of whether the plateaus are peneplain remnants or are structurally controlled surfaces, the beginning of the major southeastward-flowing streams long antedates the existing landscape. The geomorphic history of Potter County begins with an assumed long interval of erosion during the Mesozoic and early Cenozoic eras, for which no record remains in this area. The southeast master drainage was established by the latter part of the Tertiary period (perhaps at a much earlier date), probably as the result of the northwestward migration of the Atlanticinterior divide. In late Pliocene(?) time, areas adjacent to parts of the West Branch Susquehanna River-and probably elsewhere-had a moderate relief ranging from 300 to 700 feet. Some segments of the West Branch meandered across a broad valley that lay about 900 feet above the present streams. The landscape probably was covered by deep residual soils, perhaps by saprolite. The early Pleistocene history of Potter County is essentially unknown. No deposits of the Kansan stage are known except for a possible trace of pre-Illinoian drift on the uplands in central Potter County (Ayers Hill quadrangle). Some deposits in central and eastern Pennsylvania may be of Kansan age. It is probable that the assumed Aftonian regolith was removed by mass movements and other processes during the Kansan stage, thus resulting in a lowering of the plateau tops by as much as 10 feet. By the close of the Yarmouth(?) interglacial stage the major streams were incised to essentially their present depths. The climates of the Yarmouth interglacial stage probably produced deep residual soils over the landscape, parts of which may still be preserved in the paleosol remnants of the present day. No Illinoian drift is known in Potter County, but drift assigned to this stage occurs in areas to the northwest and to the southeast. Some valleys, such as Kettle Creek valley, were filled with sand and gravel alluvium to depths of as much as 150 feet above their present flood plains. It is assumed that the Yarmouth residual soils were removed by mass movements and other processes induced by a periglacial climate, thus lowering the plateau tops by as much as 10 feet. During the Sangamon interglacial stage, deep (10-to-20 foot) residual soils or paleosol were developed in Potter County and probably throughout much of Pennsylvania, perhaps as a result of lateritic weathering in a subtropical climate. It is possible that the paleosol was largely removed by mass movements and by running water during late Sangamon time. During either the Iowan or Tazewell substages of the Wisconsin (perhaps the Iowan), the ice sheet advanced into the northeastern part of Potter County. The drift is similar to the Olean drift (local usage). The paleosol was almost completely removed by mass movements and other processes induced· by a periglacial climate, prior to drift deposition. This removal probably resulted in a lowering of the plateau tops by as much as 10 feet since Sangamon time. Nearly contemporaneously with drift deposition, the periglacial deposits were formed by frost heaving, solifluction, and fluvial transport in areas outside the drift border. Soil structures or patterned ground were developed on both the drift and the periglacial deposits. It is probable that the forests in the periglacial area were greatly restricted and that large areas on the uplands were essentially treeless. Little is known about the history of Potter County in postOlean time. Presumably, forests completely covered the county by the onset of the next substage, during which the Binghamton drift of MacClintock and Apfel was deposited. This drift also is found in southern New York State. The formation of the alluvium and alluvial fans probably began in the Tazewell substage and continued during the Recent epoch. Since these deposits were formed there has been very little dissection. There is little, if any, difference between soils developed on periglacial deposits and soils developed on drift. The roots of fallen trees have disturbed the soil horizons, and it is unlikely that the existing soil profiles are more than 500 years old. The forested landscape of Potter County has a distinctive microrelief ranging from a few inches to a few feet of mounds and pits produced by the roots of fallen trees. Most mounds and pits range from 10 to 20 feet in length and from 6 to 15 feet in width. On level land, many mounds are oriented with their long axes trending northward, and in some areas the orientation is random. On slopes, the mounds are oriented with their long axes at right angles to the maximum slope as a result of trees falling downslope. The toppling of trees increases the permeability of surficial deposits and mixes and destroys the soil horizons. The microrelief is a factor in forest development. The toppling of trees on slopes is a significant agent of slope erosion. The process loosens, breaks up, or overturns the upper 2 to 3 feet of the forest soil, and it tends to make the surficial layer more stony and to produce features resembling soil structures. </p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp288","usgsCitation":"Denny, C.S., 1956, Surficial geology and geomorphology of Potter County, Pennsylvania: U.S. Geological Survey Professional Paper 288, Report: v, 72 p.; 8 Plates: 28.00 × 21.01 inches or smaller, https://doi.org/10.3133/pp288.","productDescription":"Report: v, 72 p.; 8 Plates: 28.00 × 21.01 inches or smaller","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":397957,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4262.htm"},{"id":66655,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66654,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66653,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66652,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66651,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66650,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66649,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0288/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66656,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0288/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0288/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Potter County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-77.7513,41.999],[-77.7031,41.9991],[-77.6884,41.9992],[-77.6096,41.9998],[-77.6077,41.9211],[-77.6076,41.9174],[-77.6076,41.9015],[-77.6063,41.8402],[-77.6057,41.8334],[-77.6056,41.8121],[-77.6056,41.8093],[-77.605,41.8007],[-77.605,41.7944],[-77.6043,41.7558],[-77.6043,41.7499],[-77.6043,41.7472],[-77.603,41.7186],[-77.603,41.6999],[-77.6017,41.6518],[-77.6017,41.6437],[-77.601,41.6128],[-77.601,41.5987],[-77.5997,41.5497],[-77.5991,41.5424],[-77.5991,41.5256],[-77.5991,41.5211],[-77.5984,41.5002],[-77.5978,41.4784],[-77.6155,41.4784],[-77.664,41.4784],[-77.6977,41.4779],[-77.6989,41.4779],[-77.7093,41.4778],[-77.7498,41.4778],[-77.7645,41.4777],[-77.7774,41.4772],[-77.8006,41.4772],[-77.8123,41.4772],[-77.8282,41.4767],[-77.8454,41.4766],[-77.8742,41.4761],[-77.903,41.476],[-77.922,41.4755],[-77.9514,41.4754],[-77.9796,41.4757],[-77.9876,41.4757],[-78.0513,41.4768],[-78.0643,41.4881],[-78.0773,41.5003],[-78.094,41.5157],[-78.0958,41.5175],[-78.0977,41.5193],[-78.1107,41.5315],[-78.1119,41.5328],[-78.1243,41.5437],[-78.1379,41.5568],[-78.1769,41.5933],[-78.1831,41.5992],[-78.1862,41.6019],[-78.1992,41.6136],[-78.2035,41.6177],[-78.2054,41.619],[-78.2048,41.625],[-78.2062,41.6967],[-78.2065,41.7875],[-78.2065,41.7925],[-78.2066,41.8029],[-78.2068,41.8197],[-78.2071,41.8479],[-78.2073,41.866],[-78.2067,41.8697],[-78.2068,41.881],[-78.2075,41.8865],[-78.2078,41.9196],[-78.2078,41.9786],[-78.2085,41.9859],[-78.2086,42],[-77.9943,41.999],[-77.9662,41.9988],[-77.8686,41.9989],[-77.7513,41.999]]]},\"properties\":{\"name\":\"Potter\",\"state\":\"PA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b69","contributors":{"authors":[{"text":"Denny, C. 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,{"id":39091,"text":"pp300 - 1956 - Contributions to the geology of uranium and thorium by the United States Geological Survey and Atomic Energy Commission for the United Nations International Conference on Peaceful Uses of Atomic Energy, Geneva, Switzerland, 1955","interactions":[],"lastModifiedDate":"2023-09-27T21:04:36.635797","indexId":"pp300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"300","title":"Contributions to the geology of uranium and thorium by the United States Geological Survey and Atomic Energy Commission for the United Nations International Conference on Peaceful Uses of Atomic Energy, Geneva, Switzerland, 1955","docAbstract":"Within the boundaries of the United States abnormal amounts of uranium have been found in rocks of nearly all geologic ages and lithologic types. Distribution of ore is more restricted. On the Colorado Plateau, the Morrison formation of Jurassic age yields 61.4 percent of the ore produced in the United States, and the Chinle conglomerate and Shinarump formation of Triassic age contribute 26.0 and 5.8 percent, respectively. Clastic, carbonaceous, and carbonate sedimentary rocks of Tertiary, Mesozoic, and Paleozoic ages and veins of Tertiary age are the source of the remaining 6.8 percent.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp300","usgsCitation":"Page, L., Stocking, H.E., and Smith, H., 1956, Contributions to the geology of uranium and thorium by the United States Geological Survey and Atomic Energy Commission for the United Nations International Conference on Peaceful Uses of Atomic Energy, Geneva, Switzerland, 1955: U.S. Geological Survey Professional Paper 300, vii, 739 p., https://doi.org/10.3133/pp300.","productDescription":"vii, 739 p.","numberOfPages":"768","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":421293,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93373.htm","linkFileType":{"id":5,"text":"html"}},{"id":271180,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0300/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164451,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0300/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af0e4b07f02db691734","contributors":{"authors":[{"text":"Page, Lincoln R.","contributorId":63367,"corporation":false,"usgs":true,"family":"Page","given":"Lincoln R.","affiliations":[],"preferred":false,"id":220940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stocking, Hobart E.","contributorId":66548,"corporation":false,"usgs":true,"family":"Stocking","given":"Hobart","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Harriet B.","contributorId":59097,"corporation":false,"usgs":true,"family":"Smith","given":"Harriet B.","affiliations":[],"preferred":false,"id":220939,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51939,"text":"ofr56120 - 1956 - Estimated use of water in Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr56120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-120","title":"Estimated use of water in Tennessee","language":"ENGLISH","doi":"10.3133/ofr56120","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1956, Estimated use of water in Tennessee: U.S. Geological Survey Open-File Report 56-120, 1 p., https://doi.org/10.3133/ofr56120.","productDescription":"1 p.","costCenters":[],"links":[{"id":177529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd045","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":532140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51941,"text":"ofr56124 - 1956 - North Mississippi floods of March 1955","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr56124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-124","title":"North Mississippi floods of March 1955","language":"ENGLISH","doi":"10.3133/ofr56124","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1956, North Mississippi floods of March 1955: U.S. Geological Survey Open-File Report 56-124, 42 p., https://doi.org/10.3133/ofr56124.","productDescription":"42 p.","costCenters":[],"links":[{"id":179476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696ce0","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":532142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51918,"text":"ofr5676 - 1956 - Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954","interactions":[{"subject":{"id":51918,"text":"ofr5676 - 1956 - Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954","indexId":"ofr5676","publicationYear":"1956","noYear":false,"title":"Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954"},"predicate":"SUPERSEDED_BY","object":{"id":2143,"text":"wsp1460A - 1954 - Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico","indexId":"wsp1460A","publicationYear":"1954","noYear":false,"chapter":"A","title":"Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico"},"id":1}],"supersededBy":{"id":2143,"text":"wsp1460A - 1954 - Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico","indexId":"wsp1460A","publicationYear":"1954","noYear":false,"title":"Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico"},"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr5676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-76","title":"Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954","language":"ENGLISH","doi":"10.3133/ofr5676","usgsCitation":"Lohr, E.W., 1956, Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954: U.S. Geological Survey Open-File Report 56-76, 39 p., https://doi.org/10.3133/ofr5676.","productDescription":"39 p.","costCenters":[],"links":[{"id":177523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e474d","contributors":{"authors":[{"text":"Lohr, E. W.","contributorId":48155,"corporation":false,"usgs":true,"family":"Lohr","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":244474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51917,"text":"ofr5675 - 1956 - Surface-water resources of Polecat Creek basin, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr5675","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-75","title":"Surface-water resources of Polecat Creek basin, Oklahoma","docAbstract":"A compilation of basic data on surface waters in Polecat Creek basin is presented on a monthly basis for Heyburn Reservoir and for Polecat Creek at Heyburn, Okla. Chemical analyses are shown for five sites in the basin.\r\nCorrelation of runoff records with those for nearby basins indicates that the average annual runoff of the basin above gaging station at Heyburn is 325 acre-feet per square mile.\r\n\r\nEstimated duration curves of daily flow indicate that under natural conditions there would be no flow in Polecat Creek at Heyburn (drainage area, 129 square miles) about 16 percent of the time on an average, and that the flow would be less than 3 cubic feet per second half of the time. As there is no significant base flow in the basin, comparable low flows during dry-weather periods may be expected in other parts of the basin.\r\n\r\nDuring drought periods Heyburn Reservoir does not sustain a dependable low-water flow in Polecat Creek. Except for possible re-use of the small sewage effluent from city of Sapulpa, dependable supplies for additional water needs on the main stem will require development of supplemental storage.\r\n\r\nThere has been no regular program for collection of chemical quality data in the basin, but miscellaneous analyses indicate a water of suitable quality for municipal and agricultural uses in Heyburn Reservoir and Polecat Creek near Heyburn. One recent chemical analysis indicates the possibility of a salt pollution problem in the Creek near Sapulpa.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr5675","usgsCitation":"Laine, L., 1956, Surface-water resources of Polecat Creek basin, Oklahoma: U.S. Geological Survey Open-File Report 56-75, 20 p., https://doi.org/10.3133/ofr5675.","productDescription":"20 p.","costCenters":[],"links":[{"id":177522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623d0e","contributors":{"authors":[{"text":"Laine, L.L.","contributorId":100464,"corporation":false,"usgs":true,"family":"Laine","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":244473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51916,"text":"ofr5670 - 1956 - Water levels in observation wells in Nebraska during 1955","interactions":[],"lastModifiedDate":"2018-11-08T15:42:49","indexId":"ofr5670","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-70","title":"Water levels in observation wells in Nebraska during 1955","docAbstract":"<p>The objective of the dbservation-well program in Nebraska is to provide an evaluation of the status of the ground-water supplies. Many uses for water-.level data are known but not all potential uses can be forseen. Among the important uses are the following:</p><ol><li>To indicate the status of ground water in storage or in transit and the availability of supplies.<br></li><li>To show the trend of ground-water supplies and the outlook for the future.<br></li><li>To estimate or forcast the base flow of streams.<br></li><li>To indicate areas in which the water level is approaching too close to the land surface (water-logging) or is receding toward economic limits of lift or tow rd impairment by water of poor quality.<br></li><li>To provide long-term vidence for evaluating the effectiveness of land-management and water...0 nservation programs in relation to water conservation actually of ected, and for use in basin or \"watershed\" studies.<br></li><li>To provide longterm ontinuous records to serve as a framework to which short-term records collected during intensive investigation may be related.<br></li></ol><p>The water level in an observation well functions as a gage to indicate the position of the water table o The water table is defined as the upper surface of the zone of saturation except where that surface is formed by overlying impermeable materials. The water table is also the boundary between the zone of saturation and the zone of aeration. It is not a level surface but is a sloping surface that has many irregularities, and it often conforms in a general way to the land surface. The irregularities are caused by several factors. In places where the recharge to the ground-water reservoir is exceptionally large, the water-table may rise to form a mound from which the water slowly spreads. Depressions or troughs in the water table indicate places where the ground water is discharging, as along streams that are below the normal level of the water table, or indicate places where water is being withdrawn by wells or vegetation.</p><p>The several factors that influence the water table vary in fact and amount from time to time because of changes in weather and the water requirements of vegetation and man; thus, the water table is nearly always rising or falling.</p><p>The fluctuations of the water table are shown by the changes in water levels in wells. Thus, the rate and amount of the fluctuation of the water table can be ascertained by observing the water levels in wells, and the magnitude of the several factors effecting the position of the water table can be interpreted by analyzing the water—level data.</p><p>Water-level measurements are given, in this report, in feet below the land surface at the well site. Water levels that are above land surface are preceded by a plus (+) sign, whereas those below land surface have no sign but are understood to be minus (-). The words \"land-surface datum\" are abbreviated \"lsd\" in tables of this report.</p><p>The altitude above mean sea level (msl) of the land surface at many of the well sites has been determined and is included in the tables of this report.</p><p>Lower case letters which appear in the table of water level measurements indicate the following: 6', nearby well pumped recently; f, dry; g, measured by outside agency; and j, frozen.</p><p>Twenty-.six observation wells in Nebraska are equipped with recording gages. Each recording gage produces a continuous graph of water-level fluctuations in the well. Only the lowest water level on the last day of record in each month, as recorded by the gage, is given in this report; the complete record is on file in the office of the U. S. Geological Survey in Lincoln, Nebr.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5670","usgsCitation":"Keech, C., 1956, Water levels in observation wells in Nebraska during 1955: U.S. Geological Survey Open-File Report 56-70, xiv, 106 p., https://doi.org/10.3133/ofr5670.","productDescription":"xiv, 106 p.","numberOfPages":"121","costCenters":[],"links":[{"id":359340,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0070/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0070/report-thumb.jpg"}],"country":"United 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