An integrated geophysical study - comprising gravity, seismic refraction, and aeromagnetic surveys - was made of a 4,600-km2 area in Grand Teton National Park and vicinity, Wyoming, for the purpose of obtaining a better understanding of the structural relationships in the region. The Teton range is largely comprised of Precambrian crystalline rocks and layered metasedimentary gneiss, but it also includes granitic gneiss, hornblende-plagioclase gneiss, granodiorite, and pegmatite and diabase dikes. Elsewhere, the sedimentary section is thick. The presence of each system except Silurian provides a chronological history of most structures. Uplift of the Teton-Gros Ventre area began in the Late Cretaceous; most of the uplift occurred after middle Eocene time. Additional uplift of the Teton Range and downfaulting of Jackson Hole began in the late Pliocene and continues to the present.
Bouguer anomalies range from -185 mgal over Precambrian rocks of the Teton Range to -240 mgal over low-density Tertiary and Cretaceous sedimentary rocks of Jackson Hole. The Teton fault (at the west edge of Jackson Hole), as shown by steep gravity gradients and seismic-refraction data, trends north-northeast away from the front of the Teton Range in the area of Jackson Lake. The Teton fault either is shallowly inclined in the Jenny Lake area, or it consists of a series of fault steps in the fault zone; it is approximately vertical in the Arizona Creek area.
Seismic-refraction data can be fitted well by a three-layer gravity model with velocities of 2.45 km per sec for the Tertiary and Cretaceous rocks above the Cloverly Formation, 3.9 km per sec for the lower Mesozoic rocks, and 6.1 km per sec for the Paleozoic (limestone and dolomite) and Precambrian rocks. Gravity models computed along two seismic profiles are in good agreement (σ=± 2 mgal) if density contrasts with the assumed 2.67 g per cm3 Paleozoic and Precambrian rocks are assumed to be -0.35 and -0.10 g per cm3 for the 2.45 and 3.9 km per sec velocity layers, respectively. The Teton Range has a maximum vertical uplift of about 7 km, as inferred from the maximum depth to basement of about 5 km.
Aeromagnetic data show a 400γ positive anomaly in the Gros Ventre Range, which trends out of the surveyed area at the east edge. Exposed Precambrian rocks contain concentrations of magnetite and hematite. A prominent anomaly of about 100γ is associated with the Gros Ventre Range, and 100γ anomalies are associated with the layered gneiss of the Teton Range. On this basis the unmapped Precambrian rocks of the Gross Ventre Range are interpreted as layered gneiss. The sources of the magnetic anomalies, as indicated by depth determination, are at the surface of the Precambrian rocks. A model fitted to a profile across the Gros Ventre Range gives a depth to the Precambrian surface and a susceptibility of 0.0004 emu (electromagnetic units) for the source, which is consistent with modal analyses of the layered gneisses. A residual magnetic map shows that the granitic rocks and layered gneiss probably continue beneath the floor of Jackson Hole east of the Teton fault. The location of aeromagnetic anomalies is consistent with the interpretation that the Teton fault diverges from the front of the Teton Range.
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","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Bureau Of Sport Fisheries And Wildlife, 1968, Suitability of the Susquehanna River for restoration of shad: Resource Publication 55, vi, 60 p.","productDescription":"vi, 60 p.","costCenters":[],"links":[{"id":162357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629b1a","contributors":{"authors":[{"text":"Bureau Of Sport Fisheries And Wildlife","contributorId":128243,"corporation":true,"usgs":false,"organization":"Bureau Of Sport Fisheries And Wildlife","id":529621,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15834,"text":"ofr69238 - 1968 - A testing of court-stenographic techniques for recording geologic descriptions","interactions":[],"lastModifiedDate":"2024-07-31T14:39:22.085495","indexId":"ofr69238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"69-238","title":"A testing of court-stenographic techniques for recording geologic descriptions","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69238","usgsCitation":"Schleicher, D., 1968, A testing of court-stenographic techniques for recording geologic descriptions: U.S. Geological Survey Open-File Report 69-238, 13 p. ill. ;27 cm., https://doi.org/10.3133/ofr69238.","productDescription":"13 p. ill. ;27 cm.","costCenters":[],"links":[{"id":149769,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5aed","contributors":{"authors":[{"text":"Schleicher, David","contributorId":49350,"corporation":false,"usgs":true,"family":"Schleicher","given":"David","affiliations":[],"preferred":false,"id":171815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4710,"text":"twri04A2 - 1968 - Frequency curves","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri04A2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"04-A2","title":"Frequency curves","docAbstract":"This manual describes graphical and mathematical procedures for preparing frequency curves from samples of hydrologic data. It also discusses the theory of frequency curves, compares advantages of graphical and mathematical fitting, suggests methods of describing graphically defined frequency curves analytically, and emphasizes the correct interpretations of a frequency curve.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/twri04A2","issn":"0565-596X","usgsCitation":"Riggs, H.C., 1968, Frequency curves: U.S. Geological Survey Techniques of Water-Resources Investigations 04-A2, v, 15 p. :ill. ;26 cm. Reprinted in 1978, 1989., https://doi.org/10.3133/twri04A2.","productDescription":"v, 15 p. :ill. ;26 cm. Reprinted in 1978, 1989.","costCenters":[],"links":[{"id":299,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri4a2/","linkFileType":{"id":5,"text":"html"}},{"id":139156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dda","contributors":{"authors":[{"text":"Riggs, H. C.","contributorId":17210,"corporation":false,"usgs":true,"family":"Riggs","given":"H.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":149659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37238,"text":"rp49 - 1968 - Foreign game investigation: A federal-state cooperative program","interactions":[],"lastModifiedDate":"2016-11-02T15:01:54","indexId":"rp49","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"49","title":"Foreign game investigation: A federal-state cooperative program","docAbstract":"No abstract available
","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Bump, G., 1968, Foreign game investigation: A federal-state cooperative program: Resource Publication 49, [i], 14 p.","productDescription":"[i], 14 p.","costCenters":[],"links":[{"id":161940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4d1","contributors":{"authors":[{"text":"Bump, Gardiner","contributorId":79528,"corporation":false,"usgs":true,"family":"Bump","given":"Gardiner","email":"","affiliations":[],"preferred":false,"id":217731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3328,"text":"cir561 - 1968 - An atomic-absorption method for the determination of gold in large samples of geologic materials","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"cir561","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"561","title":"An atomic-absorption method for the determination of gold in large samples of geologic materials","docAbstract":"A laboratory method for the determination of gold in large (100-gram) samples has been developed for use in the study of the gold content of placer deposits and of trace amounts of gold in other geologic materials. In this method the sample is digested with bromine and ethyl ether, the gold is extracted into methyl isobutyl ketone, and the determination is made by atomicabsorption spectrophotometry. The lower limit of detection is 0.005 part per million in the sample. The few data obtained so far by this method agree favorably with those obtained by assay and by other atomic-absorption methods. About 25 determinations can be made per man-day.","language":"ENGLISH","publisher":"[U.S. Govt. Print. Off.],","doi":"10.3133/cir561","usgsCitation":"VanSickle, G.H., and Lakin, H.W., 1968, An atomic-absorption method for the determination of gold in large samples of geologic materials: U.S. Geological Survey Circular 561, iii, 4 p. ;27 cm., https://doi.org/10.3133/cir561.","productDescription":"iii, 4 p. ;27 cm.","costCenters":[],"links":[{"id":139260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0561/report-thumb.jpg"},{"id":30337,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0561/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c78","contributors":{"authors":[{"text":"VanSickle, Gordon H.","contributorId":76280,"corporation":false,"usgs":true,"family":"VanSickle","given":"Gordon","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lakin, Hubert William","contributorId":54578,"corporation":false,"usgs":true,"family":"Lakin","given":"Hubert","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":146673,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55831,"text":"ofr6825 - 1968 - Memorandum report on test drilling at Norfolk, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"ofr6825","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-25","title":"Memorandum report on test drilling at Norfolk, Virginia","language":"ENGLISH","doi":"10.3133/ofr6825","usgsCitation":"Brown, D., 1968, Memorandum report on test drilling at Norfolk, Virginia: U.S. Geological Survey Open-File Report 68-25, 32 p., 1 fig., https://doi.org/10.3133/ofr6825.","productDescription":"32 p., 1 fig.","costCenters":[],"links":[{"id":184733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db6140d0","contributors":{"authors":[{"text":"Brown, D.L.","contributorId":73173,"corporation":false,"usgs":true,"family":"Brown","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":254343,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55863,"text":"ofr68201 - 1968 - Statistical properties of dune profiles","interactions":[{"subject":{"id":55863,"text":"ofr68201 - 1968 - Statistical properties of dune profiles","indexId":"ofr68201","publicationYear":"1968","noYear":false,"title":"Statistical properties of dune profiles"},"predicate":"SUPERSEDED_BY","object":{"id":38800,"text":"pp562F - 1971 - Statistical properties of dune profiles","indexId":"pp562F","publicationYear":"1971","noYear":false,"chapter":"F","title":"Statistical properties of dune profiles"},"id":1}],"supersededBy":{"id":38800,"text":"pp562F - 1971 - Statistical properties of dune profiles","indexId":"pp562F","publicationYear":"1971","noYear":false,"title":"Statistical properties of dune profiles"},"lastModifiedDate":"2025-06-30T16:19:29.423741","indexId":"ofr68201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-201","title":"Statistical properties of dune profiles","docAbstract":"Properties of sand waves formed by subcritical unidirectional water currents are investigated by statistical analyses of records of streambed profiles. Records of bed elevation y as a function of distance x along the channel, y = y(x), and time records at a fixed point of the channel, y = y(t), were collected in three laboratory flumes that were 8 inches, 2 ft and 8 ft wide and in a straight alluvial channel that was 55 ft wide. For all cases, the bed material was fine sand. The continuous analogue records were converted to discrete data points and were analyzed by digital computer.
The analyses show that both types of records, y(x) and y(t), can be approximately represented as stationary Gaussian processes. When the data are standardized and the length or distance are expressed as ratios of the mean duration between zero-crossings of y, the statistical properties of all the flume data are similar, with no distinguishing characteristics that can be attributed to size of flume or to whether the bed forms were ripples or dunes. The field data, however, reflect the influence of large alternate bars that were not present in the flumes.
The Gaussian assumption, together with the spectral properties of the records as expressed by a dimensionless parameter, 6, permit predicting the distributions of maximum and minimum values of y between successive zeros of y. These distributions represent the probability distributions of the depth of local scour and fill due to the formation and migration of sand waves, and the parameters that specify the distributions relate approximately to flow velocity and depth.
Observed values of the number of zero and h-level crossings, the mean duration between zero crossings, and the mean duration of upward excursions of the process y(t) above the fixed level h compared reasonably well with theoretical values for the Gaussian model. The distribution of the duration of upward excursions is the conditional probability distribution of the rest period of a particle, given that it is deposited on the downstream face of a ripple or dune at the level h. Observed distributions of these durations can be approximated by a gamma distribution with parameters that relate to h, where h is measured in units of standard deviation from the mean bed level. These distributions and other probability distributions that enter into stochastic models of sediment transport can be determined either from the theoretical model or empirically from the observed data. The results of the study ,-show that even though the bed elevation deviates somewhat from the postulated normal distribution, reasonable estimates of many properties of the bed profiles can be derived from fairly simple statistical models.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68201","usgsCitation":"Nordin, C., 1968, Statistical properties of dune profiles: U.S. Geological Survey Open-File Report 68-201, xiv, 137 p., https://doi.org/10.3133/ofr68201.","productDescription":"xiv, 137 p.","costCenters":[],"links":[{"id":491571,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0201/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184022,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0201/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1e3f","contributors":{"authors":[{"text":"Nordin, C.F. Jr.","contributorId":100852,"corporation":false,"usgs":true,"family":"Nordin","given":"C.F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":254388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68271,"text":"ha287 - 1968 - Availability of ground water in Adams County, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:26","indexId":"ha287","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"287","title":"Availability of ground water in Adams County, Nebraska","language":"ENGLISH","doi":"10.3133/ha287","usgsCitation":"Keech, C.F., and Dreeszen, V., 1968, Availability of ground water in Adams County, Nebraska: U.S. Geological Survey Hydrologic Atlas 287, 1 map., https://doi.org/10.3133/ha287.","productDescription":"1 map.","costCenters":[],"links":[{"id":188555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89677,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/287/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667d6c","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":277945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dreeszen, V. H.","contributorId":8825,"corporation":false,"usgs":true,"family":"Dreeszen","given":"V. 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