No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3808320","usgsCitation":"Haramis, G., and Nice, A.D., 1980, An improved web-tagging technique for waterfowl: Journal of Wildlife Management, v. 44, no. 4, p. 898-899, https://doi.org/10.2307/3808320.","productDescription":"2 p.","startPage":"898","endPage":"899","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198992,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Montezuma National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.82041643301584,\n 43.03969461549909\n ],\n [\n -76.82041643301584,\n 42.94072495607546\n ],\n [\n -76.72774197584917,\n 42.94072495607546\n ],\n [\n -76.72774197584917,\n 43.03969461549909\n ],\n [\n -76.82041643301584,\n 43.03969461549909\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684755","contributors":{"authors":[{"text":"Haramis, G.Michael","contributorId":112286,"corporation":false,"usgs":true,"family":"Haramis","given":"G.Michael","email":"","affiliations":[],"preferred":false,"id":334237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nice, Allen D.","contributorId":93159,"corporation":false,"usgs":true,"family":"Nice","given":"Allen","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":334236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001204,"text":"1001204 - 1980 - Net-firing gun for capturing breeding waterfowl","interactions":[],"lastModifiedDate":"2024-10-28T15:16:25.723186","indexId":"1001204","displayToPublicDate":"1980-10-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Net-firing gun for capturing breeding waterfowl","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3808318","usgsCitation":"Mechlin, L.M., and Shaiffer, C.W., 1980, Net-firing gun for capturing breeding waterfowl: Journal of Wildlife Management, v. 44, no. 4, p. 895-896, https://doi.org/10.2307/3808318.","productDescription":"2 p.","startPage":"895","endPage":"896","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129102,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697ad7","contributors":{"authors":[{"text":"Mechlin, Larry M.","contributorId":107842,"corporation":false,"usgs":true,"family":"Mechlin","given":"Larry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":310699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaiffer, Charles W.","contributorId":16148,"corporation":false,"usgs":true,"family":"Shaiffer","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":310698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70237066,"text":"70237066 - 1980 - Basin development along the Late Mesozoic and Cainozoic California Margin: A plate tectonic margin of subduction, oblique subduction and transform tectonics","interactions":[],"lastModifiedDate":"2022-09-29T11:58:47.234811","indexId":"70237066","displayToPublicDate":"1980-09-29T06:55:12","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"4","title":"Basin development along the Late Mesozoic and Cainozoic California Margin: A plate tectonic margin of subduction, oblique subduction and transform tectonics","docAbstract":"Along the Californian margin of the North American plate, the configuration and structural stability of late Mesozoic and Cainozoic basins are related to plate kinematics. Three tectonic regimes are recorded; orthogonal high-angle subduction, oblique low-angle subduction, and transform slip. During the first, regionally extensive forearc basins developed; during the second and third, borderland settings formed as a consequence of wrench faulting. In the forearc basins, sedimentological facies constitute regional belts that persist for hundreds of kilometres, with stratigraphic sequences that are 1–15 km thick. Shorelines are relatively straight, shelf facies are broad and well developed, and basin fill is composed of shallow marine, shelf and coalescing submarine-fan facies. Sediment transport in the deeper water facies commonly is parallel to the basin axis. Borderland basins reflect tectonic instability. A principal effect of wrench tectonics is the vertical reciprocation of crustal blocks. Shorelines are generally irregular, and narrow shelves pass abruptly into deep basins. Lithofacies change dramatically along strike, and stratigraphic thicknesses are variable from basin to basin, from tens of metres up to 6 km. Basin-margin facies are marked by unconformities, slump aprons, lithological pinch-outs and submarine canyon channels. Penecontemporaneous slip along the basin-margin faults complicates these lithofacies patterns. Borderland type palaeogeography is most extensively developed in the transform tectonic regime, and therefore the more seaward offshore basins are relatively depleted of terrigenous debris owing to transport barriers.
Washteaw County is underlain by glacial deposits that range in thickness from about 50 feet to about 450 feet. Underlying the glacial deposits are sedimentary rocks of Mississippian and Devonian age. The youngest of these rocks are the sandstones of the Marshall Formation in the western part of the county; the oldest are the limestones of the Detroit River Group in the southeast corner.
Sand and gravel deposits in some places in the county may yield more than 500 gallons per minute of water. Approximately 50 percent of the wells tapping the Marshall Formation, the most reliable bedrock aquifer, can yield as much as 60 gallons per minute.
Washtenaw County has sand and gravel deposits that are more than 50 feet thick. The deposits are mined in several areas and are of economic importance. In addition, there may be potential for peat production in the western part of the county and for clay production in the eastern part.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/70185555","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Fleck, W.B., 1980, Geology and hydrology for environmental planning in Washtenaw County, Michigan: Open-File Report, iv, 23 p., https://doi.org/10.3133/70185555.","productDescription":"iv, 23 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":503231,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70185555/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":338212,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70185555/report-thumb.jpg"}],"country":"United States","state":"Michigan","county":"Washtenaw County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.553,42.4351],[-83.5492,42.3486],[-83.5417,42.1744],[-83.5399,42.0853],[-83.6563,42.0833],[-83.7763,42.0823],[-83.8927,42.0797],[-84.0164,42.0789],[-84.0165,42.0749],[-84.1353,42.073],[-84.136,42.1611],[-84.1319,42.2483],[-84.132,42.3356],[-84.1333,42.4238],[-84.0196,42.423],[-83.9065,42.4249],[-83.7864,42.4288],[-83.6669,42.4312],[-83.553,42.4351]]]},\"properties\":{\"name\":\"Washtenaw\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d4df18e4b05ec79911d205","contributors":{"authors":[{"text":"Fleck, William B.","contributorId":17587,"corporation":false,"usgs":true,"family":"Fleck","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":685944,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012213,"text":"70012213 - 1980 - Sediment waves on the Monterey fan levee: a preliminary physical interpretation.","interactions":[],"lastModifiedDate":"2024-09-27T14:57:36.972885","indexId":"70012213","displayToPublicDate":"1980-08-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment waves on the Monterey fan levee: a preliminary physical interpretation.","docAbstract":"Sediment waves on the deep ocean floor occur mostly on the lower continental rise on slopes of 1° or less. Previous studies show that their amplitude and wavelength vary greatly, but little is known about their shape in plan. A detailed survey of a 30-km2 area of abyssal-depth sediment waves associated with the levee of the Monterey fan valley shows a pattern of sinuous crests and troughs with parallel, well-bedded internal structure. Material in the upper 1 m of sediment consists predominantly of bioturbated, muddy coccolith ooze. A single thin, silty horizon can be correlated between adjoining waves.
On the basis of measured wave dimensions and an estimate of flow velocity we use a simple two-layer model for water movement to infer approximate flow parameters. The sediment waves are considered to be formed most likely by low-velocity (10 cm/s), low-concentration turbidity flows approximately 100–800 m thick. This interpretation emphasizes the role of low-speed, low-concentration turbidity currents in the downslope movement of fine-grained material. This type of transport—deposition regime explains the formation of sediment waves very well except for certain waves occurring on depositional ridges in the deep ocean.
","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(80)90009-2","usgsCitation":"Normark, W.R., Hess, G.R., Stow, D., and Bowen, A., 1980, Sediment waves on the Monterey fan levee: a preliminary physical interpretation.: Marine Geology, v. 37, no. 1-2, p. 1-18, https://doi.org/10.1016/0025-3227(80)90009-2.","productDescription":"18 p.","startPage":"1","endPage":"18","costCenters":[],"links":[{"id":222399,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b89f0e4b08c986b316f53","contributors":{"authors":[{"text":"Normark, William R.","contributorId":69570,"corporation":false,"usgs":true,"family":"Normark","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Gordon R.","contributorId":102119,"corporation":false,"usgs":true,"family":"Hess","given":"Gordon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stow, D.A.V.","contributorId":35441,"corporation":false,"usgs":true,"family":"Stow","given":"D.A.V.","email":"","affiliations":[],"preferred":false,"id":363000,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bowen, A.J.","contributorId":87292,"corporation":false,"usgs":true,"family":"Bowen","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":363002,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1001696,"text":"1001696 - 1980 - Small-format cameras and fine-grain film used for waterfowl population studies","interactions":[],"lastModifiedDate":"2024-10-28T15:43:37.530207","indexId":"1001696","displayToPublicDate":"1980-07-02T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Small-format cameras and fine-grain film used for waterfowl population studies","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3808021","usgsCitation":"Ferguson, E.L., and Gilmer, D.S., 1980, Small-format cameras and fine-grain film used for waterfowl population studies: Journal of Wildlife Management, v. 44, no. 3, p. 691-694, https://doi.org/10.2307/3808021.","productDescription":"4 p.","startPage":"691","endPage":"694","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129259,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"Sand Lake National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -98.29836946820163,\n 45.82389634024136\n ],\n [\n -98.29836946820163,\n 45.682056147284726\n ],\n [\n -98.20220119441676,\n 45.682056147284726\n ],\n [\n -98.20220119441676,\n 45.82389634024136\n ],\n [\n -98.29836946820163,\n 45.82389634024136\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"44","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd4b","contributors":{"authors":[{"text":"Ferguson, Edgar L.","contributorId":77210,"corporation":false,"usgs":true,"family":"Ferguson","given":"Edgar","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":311536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilmer, David S.","contributorId":59508,"corporation":false,"usgs":true,"family":"Gilmer","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":311535,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221633,"text":"5221633 - 1980 - Transfer of crude oil from contaminated water to bird eggs","interactions":[],"lastModifiedDate":"2020-02-26T11:23:12","indexId":"5221633","displayToPublicDate":"1980-06-16T12:19:23","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1561,"text":"Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"Transfer of crude oil from contaminated water to bird eggs","docAbstract":"Paris of breeding mallard ducks were exposed to oiled water for 2 days during the first week of incubation. Hatching success of ducks exposed to 100 ml of Prudhoe Bay crude oil per square meter of water surface was significantly less than that of controls. Hatching success of ducks exposed to 5 ml of crude oil per square meter of water surface was less than that of controls but the difference was not significant. The presence of oil on the eggs of ducks exposed to oiled water was confirmed by chemical analysis. Thermocouple probes were used to monitor the egg and nest temperatures of some of the ducks in each of the three groups. Incubation temperatures of oiled females were not significantly different from those of the controls. The incubation behavior of females exposed to oiled water and the first-week survival of their ducklings was not affected by the oil.","language":"English","publisher":"ScienceDirect","doi":"10.1016/0013-9351(80)90143-7","usgsCitation":"Albers, P., 1980, Transfer of crude oil from contaminated water to bird eggs: Environmental Research, v. 22, no. 2, p. 307-314, https://doi.org/10.1016/0013-9351(80)90143-7.","productDescription":"8 p.","startPage":"307","endPage":"314","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18276,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6WDS-4F1YBYG-4W&_user=696292&_handle=V-WA-A-W-WC-MsSAYVW-UUW-U-AACAUEZWUU-AAVYZDDUUU-YEWVBAUZY-WC-U&_fmt=summary&_coverDate=08%2F31%2F1980&_rdoc=5&_orig=browse&_srch=%23toc%236774%231980%23999779997%23544458!&_cdi=6774&view=c&_acct=C000038819&_version=1&_urlVersion=0&_userid=696292&md5=b116a475681e116ec29ed67111623646","linkFileType":{"id":5,"text":"html"}}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626d9e","contributors":{"authors":[{"text":"Albers, P.H.","contributorId":26646,"corporation":false,"usgs":true,"family":"Albers","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":334322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70200638,"text":"70200638 - 1980 - Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California","interactions":[],"lastModifiedDate":"2018-10-25T13:28:00","indexId":"70200638","displayToPublicDate":"1980-05-10T13:27:17","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California","docAbstract":"The Coso Range lies at the west edge of the Great Basin, adjacent to the southern part of the Sierra Nevada. A basement complex of pre‐Cenozoic plutonic and metamorphic rocks is partly buried by ∼35 km3 of late Cenozoic volcanic rocks that were erupted during two periods, as defined by K‐Ar dating: (1) 4.0–2.5 m.y., ∼31 km3 of basalt, rhyodacite, dacite, andesite, and rhyolite, in descending order of abundance, and (2) ≤1.1 m.y., nearly equal amounts of basalt and rhyolite, most of the rhyolite being ≤0.3 m.y. old. Vents for the volcanic rocks of the younger period are localized on and near a horst of basement rocks within a concavity defined by the distribution of vents of the older period. The alignment of many vents and the presence of a considerable number of roughly north‐trending normal faults of late Cenozoic age reflect basin and range tectonics dominated by roughly east‐west lithospheric extension. Fumaroles, intermittently active thermal springs, and associated altered rocks occur within and immediately east of the central part of the field of Quaternary rhyolite, in an area characterized by various geophysical anomalies that are evidently related to an active hot‐water geothermal system. This system apparently is heated by a reservoir of silicic magma at ≥8‐km depth, itself produced and sustained through partial melting of crustal rocks by thermal energy contained in mantle‐derived basaltic magma that intrudes the crust in response to lithospheric extension.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB05p02381","usgsCitation":"Duffield, W.A., Bacon, C.R., and Dalrymple, G.B., 1980, Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California: Journal of Geophysical Research B: Solid Earth, v. 85, no. B5, p. 2381-2404, https://doi.org/10.1029/JB085iB05p02381.","productDescription":"24 p.","startPage":"2381","endPage":"2404","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":358822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Inyo","otherGeospatial":"Coso Range","volume":"85","issue":"B5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Duffield, Wendell A.","contributorId":14363,"corporation":false,"usgs":true,"family":"Duffield","given":"Wendell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacon, Charles R. 0000-0002-2165-5618 cbacon@usgs.gov","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":2909,"corporation":false,"usgs":true,"family":"Bacon","given":"Charles","email":"cbacon@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":749799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. Brent","contributorId":54564,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":749800,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012433,"text":"70012433 - 1980 - Sediment transport in Norton Sound, Alaska","interactions":[],"lastModifiedDate":"2024-10-11T15:35:55.48006","indexId":"70012433","displayToPublicDate":"1980-05-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment transport in Norton Sound, Alaska","docAbstract":"The Yukon River, the largest single source of Bering Sea sediment, delivers > 95% of its sediment load at the southwest comer of Norton Sound during the ice-free months of late May through October. During this period, surface winds in the northern Bering Sea area are generally light from the south and southwest, and surface waves are not significant. Although wind stress may cause some transport of low-density turbid surface water into the head of Norton Sound, the most significant transport of Yukon River suspended matter occurs within advective currents flowing north across the outer part of the sound. The thickest accumulations of modern Yukon silt and very fine sand occur beneath this persistent current.
We monitored temporal variations in bottom currents, pressure, and suspended-matter concentrations within this major transport pathway for 80 days in the summer of 1977 using a Geological Processes Bottom Environmental (GEOPROBE) tripod system. The record reveals two distinctive periods of bottom flow and sediment transport: an initial 59 days (July 8–September 5) of fair-weather conditions, characterized by tidally dominated currents and relatively low, stable suspended-matter concentrations; and a 21-day period (September 5–September 26) during which several storms traversed the northern Bering Sea, mean suspended-matter concentrations near the bottom increased by a factor of five, and the earlier tidal dominance was overshadowed by wind-driven and oscillatory wave-generated currents.
Friction velocities (u*) at the GEOPROBE site were generally subcritical during the initial fair-weather period. In contrast, the 21-day stormy period was characterized by uFriction velocities (u*) at the GEOPROBE site were generally subcritical during the initial fair-weather period. In contrast, the 21-day stormy period was characterized by u*values that exceeded the critical level of 1.3 cm/s more than 60% of the time. The GEOPROBE data suggest that the very fine sand constituting about 50% of the sediment on the outer part of the Yukon prodelta is transported during a few late-summer and fall storms each year. A conservative estimate shows that suspended-matter transport during the storms in September 1977 was equal to four months of fair-weather transport. values that exceeded the critical level of 1.3 cm/s more than 60% of the time. The GEOPROBE data suggest that the very fine sand constituting about 50% of the sediment on the outer part of the Yukon prodelta is transported during a few late-summer and fall storms each year. A conservative estimate shows that suspended-matter transport during the storms in September 1977 was equal to four months of fair-weather transport.
","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(80)90043-2","usgsCitation":"Drake, D., Cacchione, D., Muench, R., and Nelson, C., 1980, Sediment transport in Norton Sound, Alaska: Marine Geology, v. 36, no. 1-2, p. 97-126, https://doi.org/10.1016/0025-3227(80)90043-2.","productDescription":"30 p.","startPage":"97","endPage":"126","costCenters":[],"links":[{"id":222201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Norton Sound","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -166.93816207810704,\n 65.1847517876121\n ],\n [\n -166.93816207810704,\n 62.997485781439735\n ],\n [\n -160.32671205235334,\n 62.997485781439735\n ],\n [\n -160.32671205235334,\n 65.1847517876121\n ],\n [\n -166.93816207810704,\n 65.1847517876121\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"36","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b89d9e4b08c986b316ee5","contributors":{"authors":[{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":363567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":363568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muench, R.D.","contributorId":83270,"corporation":false,"usgs":true,"family":"Muench","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":363569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":363570,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70209240,"text":"70209240 - 1980 - Variability of currents and sediment transport on continental shelves: Optical and current meter studies of the bottom boundary layer","interactions":[],"lastModifiedDate":"2020-03-25T11:37:09","indexId":"70209240","displayToPublicDate":"1980-03-25T11:32:06","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5446,"text":"Proceedings of SPIE","active":true,"publicationSubtype":{"id":10}},"title":"Variability of currents and sediment transport on continental shelves: Optical and current meter studies of the bottom boundary layer","docAbstract":"The Continental Margin Sediment Dynamics program of the U.S. Geological Survey has been using a variety of optical instruments to monitor water turbidity as part of our studies of sediment transport. Although we suspect that optical devices will eventually be supplanted by more direct measures of suspended sediments, results of several field experiments indicate that for now transmissometers and nephelometers offer the best solution to the problem of long term environmental monitoring in the ocean. The Continental Margin Sediment Dynamics (CMSD) program of the U.S. Geological Survey is structured to investigate those oceanographic and geological processes which influence and control the active transport of sediments and other materials over continental margins. The focus of this program is on active sedimentary processes, the mechanisms which create them, and the effects they produce (see Figure 1 for a diagrammatic depiction). Basically, we design our experiments to investigate (1) transport mechanisms of oceanic sediments and other materials as suspended load and bed load, and (2) relationships of erosion and deposition to the dynamical characteristics of oceanic bottom boundary layers. The purpose of this report is to describe briefly those aspects of equipment and experiments that relate to our study of suspended particulate matter and water turbidity. Much of our understanding of the spatial distribution and temporal variability of suspended sediments depends upon measurements from optical instruments. In this report we describe those instruments and give examples of their use and some results of two field experiments.
","language":"English","publisher":"SPIE","doi":"10.1117/12.958270","usgsCitation":"Karl, H.A., Drake, D., and Cacchione, D., 1980, Variability of currents and sediment transport on continental shelves: Optical and current meter studies of the bottom boundary layer: Proceedings of SPIE, v. 208, p. 143-150, https://doi.org/10.1117/12.958270.","productDescription":"8 p.","startPage":"143","endPage":"150","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":373509,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"208","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Karl, H. A.","contributorId":115791,"corporation":false,"usgs":true,"family":"Karl","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":785517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":785518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":785519,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70209238,"text":"70209238 - 1980 - Liquefaction potential of the Yukon Prodelta, Bering Sea","interactions":[],"lastModifiedDate":"2020-03-25T11:28:50","indexId":"70209238","displayToPublicDate":"1980-03-25T11:09:32","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Liquefaction potential of the Yukon Prodelta, Bering Sea","docAbstract":"The Yukon prodelta is exposed to large storm waves propagating northward from the southern Bering Sea. Shallow water depths of the prodelta enhance the transfer of energy from the surface waves to the bottom. As the bottom deposits are cyclically loaded by large storm waves, potential decrease in their resistance to shear could ultimately cause liquefaction. A preliminary assessment of the engineering properties of Yukon sandy silt suggests that the prodelta deposits may be susceptible to wave induced liquefaction during severe storm events. In addition, erosion and are suspension of sediment in the prodelta may be intensified because of the liquefaction process.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"12th annual offshore technology conference; Proceedings","conferenceTitle":"Offshore Technology Conference","conferenceDate":"May, 5-8, 1980","conferenceLocation":"Houston, Texas","language":"English","publisher":"OnePetro","doi":"10.4043/3773-MS","usgsCitation":"Clukey, E., Cacchione, D., and Nelson, C., 1980, Liquefaction potential of the Yukon Prodelta, Bering Sea, in 12th annual offshore technology conference; Proceedings, v. 12, Houston, Texas, May, 5-8, 1980, p. 315-325, https://doi.org/10.4043/3773-MS.","productDescription":"11 p.","startPage":"315","endPage":"325","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":373508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","noUsgsAuthors":false,"publicationDate":"2013-04-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Clukey, E.C.","contributorId":52720,"corporation":false,"usgs":true,"family":"Clukey","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":785507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":785508,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":785509,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012312,"text":"70012312 - 1980 - Current-controlled, abyssal microtopography and sedimentation in Mozambique Basin, southwest Indian Ocean","interactions":[],"lastModifiedDate":"2024-10-09T17:23:27.334052","indexId":"70012312","displayToPublicDate":"1980-02-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Current-controlled, abyssal microtopography and sedimentation in Mozambique Basin, southwest Indian Ocean","docAbstract":"The Antarctic Bottom Water (AABW) activity and the variations in the abundance and grain size of the terrigenous sediments, derived from Africa and Madagascar land masses, are reflected in different types of microtopography in the Mozambique Basin. In southerly areas, where the sediment supply is much less, the bottom-current activity has resulted in the presence of manganese nodules, a thin veneer of sediments, and the absence of sediment waves. Farther north, along the marginal areas of the basin where the fine-grained sediments from the Africa—Madagascar source have been supplied in abundance, wavy bedforms have been generated by AABW. Wavy bedforms do not exist even in the northerly areas if coarse-grained, turbidite sediments are present on the sea floor. The continuation of acoustic reflectors from the zone of turbidites in the central areas of the basin into the zone of sediment waves along the margins, and the lithology and structures in sediment cores from these zones suggest that the turbidity-current-fed, fine-grained sediments were deposited as wavy bedforms by AABW flow. Thus, sediment waves formed readily during Pleistocene times. The enrichment of quartz and displaced Antarctic diatoms, and the relatively low kaolinite/chlorite ratios in the sediments, the north-pointing current lineations on the sea floor, the lack of any perceptible sedimentary fill in the troughs of waves, and the dense nepheloid layer in the westerly areas of the Mozambique Basin, attest to the current-controlled sedimentation and generation of wavy bedforms during Holocene time also. The formation of sediment waves in the Mozambique Basin can be modeled after a fluvial antidune mechanism. This model envisages that internal waves, focused on a benthic boundary layer cap, have been locked in phase with sediment waves in the presence of an 8–10 cm/sec current in the Mozambique Basin. A density contrast of 2·10−6 g/cm3 appears to exist at the tops of benthic boundary layers in the Mozambique Basin and is quite sufficient for supporting the internal waves. The densiometric Froude number calculated for a 60–280 m thick boundary layer in the basin is close to unity or greater, and is compatible with the antidune model.
","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(80)90071-7","usgsCitation":"Kolla, V., Eittreim, S., Sullivan, L., Kostecki, J., and Burckle, L., 1980, Current-controlled, abyssal microtopography and sedimentation in Mozambique Basin, southwest Indian Ocean: Marine Geology, v. 34, no. 3-4, p. 171-206, https://doi.org/10.1016/0025-3227(80)90071-7.","productDescription":"36 p.","startPage":"171","endPage":"206","costCenters":[],"links":[{"id":221938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd1ae4b0c8380cd4e625","contributors":{"authors":[{"text":"Kolla, V.","contributorId":70540,"corporation":false,"usgs":true,"family":"Kolla","given":"V.","email":"","affiliations":[],"preferred":false,"id":363245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eittreim, S.","contributorId":74878,"corporation":false,"usgs":true,"family":"Eittreim","given":"S.","affiliations":[],"preferred":false,"id":363246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sullivan, L.","contributorId":85327,"corporation":false,"usgs":true,"family":"Sullivan","given":"L.","email":"","affiliations":[],"preferred":false,"id":363247,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kostecki, J.A.","contributorId":23691,"corporation":false,"usgs":true,"family":"Kostecki","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":363244,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burckle, L.H.","contributorId":16977,"corporation":false,"usgs":true,"family":"Burckle","given":"L.H.","affiliations":[],"preferred":false,"id":363243,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70175093,"text":"70175093 - 1980 - High frequency radar measurements of tidal currents flowing through San Pablo Strait, San Francisco Bay","interactions":[],"lastModifiedDate":"2016-07-28T15:18:24","indexId":"70175093","displayToPublicDate":"1980-02-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"High frequency radar measurements of tidal currents flowing through San Pablo Strait, San Francisco Bay","docAbstract":"High frequency (HF) radar measurements of the surface current averaged over the upper 0.5 m in San Pablo Strait were compared with current meter measurements of the subsurface current made at 9.4 m below mean lower low water (MLLW) over two 12.4-h tidal cycles. After averaging the radar and current meter data over two tidal cycles, a southerly (ebbing direction) surface current of 32 cm·s−1 was deduced from the radar measurements and a northerly (flooding direction) subsurface current of 7 cm·s−1 from the current meter measurements. This nontidal flow is maintained by freshwater discharge from the Sacramento–San Joaquin Rivers into Suisun and San Pablo Bays. The radar measurement technique provides quantitative estimates of the surface currents that previously were determined only from surface drifter studies.
","language":"English","publisher":"ASLO","doi":"10.4319/lo.1980.25.5.0929","usgsCitation":"Maresca, J.W., Padden, R.R., Cheng, R.T., and Seibel, E., 1980, High frequency radar measurements of tidal currents flowing through San Pablo Strait, San Francisco Bay: Limnology and Oceanography, v. 25, no. 5, p. 929-935, https://doi.org/10.4319/lo.1980.25.5.0929.","productDescription":"7 p.","startPage":"929","endPage":"935","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"579b2cb0e4b0589fa1c980b3","contributors":{"authors":[{"text":"Maresca, Joseph W. Jr.","contributorId":173246,"corporation":false,"usgs":false,"family":"Maresca","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":643886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Padden, Robin R.","contributorId":173247,"corporation":false,"usgs":false,"family":"Padden","given":"Robin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":643887,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cheng, Ralph T.","contributorId":69134,"corporation":false,"usgs":true,"family":"Cheng","given":"Ralph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":643888,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Seibel, Erwin","contributorId":173248,"corporation":false,"usgs":false,"family":"Seibel","given":"Erwin","email":"","affiliations":[],"preferred":false,"id":643889,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":63,"text":"63 - 1980 - Geological and geophysical studies of the Navajo Nation: seminar","interactions":[],"lastModifiedDate":"2014-08-04T11:28:00","indexId":"63","displayToPublicDate":"1980-01-18T11:26:26","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geological and geophysical studies of the Navajo Nation: seminar","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/63","collaboration":"Conducted by the U.S. Geological Survey in cooperation with the Bureau of Indian Affairs.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Geological and geophysical studies of the Navajo Nation: seminar, 20 p., https://doi.org/10.3133/63.","productDescription":"20 p.","numberOfPages":"20","costCenters":[],"links":[{"id":291593,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e54e4b0beb42bdca40b","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":527163,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207700,"text":"70207700 - 1980 - Mesozoic and Cenozoic structural trends under southern Bering Sea shelf","interactions":[],"lastModifiedDate":"2020-06-15T15:02:51.444631","indexId":"70207700","displayToPublicDate":"1980-01-06T16:14:26","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":605,"text":"AAPG Bulletin","printIssn":"0149-1423","active":true,"publicationSubtype":{"id":10}},"title":"Mesozoic and Cenozoic structural trends under southern Bering Sea shelf","docAbstract":"Mesozoic rocks exposed near the tip of the Alaska Peninsula form an antiformal structure that flanks the southern side of Bristol Bay basin and that can be traced with geophysical data about 700 km offshore to the vicinity of the Pribilof Islands. Upper Jurassic sandstone and Upper Cretaceous mudstone dredged from the top and flanks of this structure near the islands confirm that Mesozoic rocks extend from the Alaska Peninsula to the Bering sea margin.
The southern part of the Bering Sea Shelf is underlain by several large structural basins: St. George, Amak, and Bristol Bay basins. These filled basins encompass an offshore area of about 31,000 sq km; St. George basin contains more than 10 km of strata. Reflection profiles show that the surface of the offshore antiformal structures is an angular unconformity overlain by Cenozoic beds. This unconformity can be traced toward the axes of the adjacent subshelf basins where, as a disconformity, it parallels underlying and overlying strata. Dredge data suggest that the unconformity and disconformity may be as old as middle to Late Cretaceous. The downdip trace of the unconformity in Bristol Bay basin is underlain by reflectors paralleling the contact, a relation suggesting that the basin and perhaps other shelf basins may be underlain by ancient Mesozoic depocenters. The bulk of the thick sections in these basins is, however, thought to be mainly Cenozoic in age. Strata in the basins are cut by high-angle growth faults. The faults commonly offset the seafloor, which implies that basin subsidence and filling continue to the present. Shallow-water diatomaceous mudstone of Eocene and Oligocene age dredged from the continental slope near the Pribilof Islands indicates that collapse of the margin and outer shelf basins began by at least early Tertiary time.
In Mesozoic time, the Bering margin between Siberia and the Alaska Peninsula (Beringian margin) may have been a zone of either oblique underthrusting or transform motion between the North American and Pacific lithosphere (Kula plate?). This motion may have rifted the edge of the North American plate, resulting in the formation of a series of elongate basins and ridges paralleling the plate edge. These hypothetical basins may have controlled the location and initial subsidence of Bristol Bay, Amak, and St. George basins. Formation of the Aleutian Island arc in late Mesozoic or earliest Tertiary time presumably terminated plate interaction along the Beringian margin. Sediment loading and subsequent subsidence of the remnant plate within the abyssal Bering Sea may have caused continuing collapse of the Beringian margin in latest Cretaceous and earliest Tertiary time.
","language":"English","publisher":"AAPG","doi":"10.1306/2F919751-16CE-11D7-8645000102C1865D","usgsCitation":"Marlow, M.S., and Cooper, A.K., 1980, Mesozoic and Cenozoic structural trends under southern Bering Sea shelf: AAPG Bulletin, v. 64, no. 12, p. 2139-2155, https://doi.org/10.1306/2F919751-16CE-11D7-8645000102C1865D.","productDescription":"17 p.","startPage":"2139","endPage":"2155","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371029,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bering Sea Shelf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -153.6328125,\n 56.26776108757582\n ],\n [\n -157.32421875,\n 61.05828537037916\n ],\n [\n -169.45312499999997,\n 58.58543569119917\n ],\n [\n -163.828125,\n 52.429222277955134\n ],\n [\n -153.6328125,\n 56.26776108757582\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"64","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":779012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":779013,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23595,"text":"ofr801207 - 1980 - Water-resources investigations, Collier County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T15:17:00.087609","indexId":"ofr801207","displayToPublicDate":"1980-01-01T22:05:00","publicationYear":"1980","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":"80-1207","title":"Water-resources investigations, Collier County, Florida","docAbstract":"Early water-resources investigations in Collier County, Fla., were related to saltwater intrusion in Naples. With the advent of canal drainage and land reclamation farther inland, investigations were directed at effects of canals on water resources and the environment. High on the list of investigative needs are: (1) areal and vertical delineation of the shallow aquifer, the prime source of freshwater; (2) delineation of areas of poor quality ground water and the sources of the poor quality; (3) establishment of network of hydrologic data stations; and (4) determination of the relation between canals and the shallow aquifer. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801207","issn":"0094-9140","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Klein, H., 1980, Water-resources investigations, Collier County, Florida: U.S. Geological Survey Open-File Report 80-1207, v, 29 p., https://doi.org/10.3133/ofr801207.","productDescription":"v, 29 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":1644,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1207/ofr801207.pdf","text":"Report","size":"851 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":154846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1207/coverthb2.jpg"}],"country":"United States","state":"Florida","county":"Collier 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Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Approximately 8.0 percent of the water used in Lee County comes from underground sources. It is estimated that the use of ground water in the county currently approaches 2.8 billion gallons per year. For comparison, this amount would provide each resident with 172 gallons of water a day during a year. Actually, few if any households use this much water, and this greater per capita use reflects the county's commercial, agribusiness, and municipal needs.
\nThe users of ground water in the county draw their supplies from several different geologic sources. Several factors must be considered in determining the availability of ground water and the adequacy of a supply source:
\ndistribution - having water where it is needed,
\naccessibility - affects the cost for drilling wells and pumping water,
\nyield - relates to the magnitude of the supply that can be SUStained,
\nquality - determines for what purposes the water can be used.
\nIn terms of these factors, there are few locations in Lee County where the availability of ground water is not limited to some degree. The most common limitation is poor water quality, that is, highly mineralized ground water. Secondary limitations are generally related to poor distribution, small yields from some sources, and poor accessibility due to the great depths to adequate sources.
","language":"English","publisher":"Iowa Geological Survey","usgsCitation":"Gordon, D.L., 1980, Ground water resources of Lee County, 28 p.","productDescription":"28 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":324313,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","county":"Lee","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.10412597656249,\n 40.697299008636755\n ],\n [\n -91.16729736328125,\n 40.72852712420599\n ],\n [\n -91.2139892578125,\n 40.74725696280421\n ],\n [\n -91.2689208984375,\n 40.76806170936614\n ],\n [\n -91.34307861328125,\n 40.78262115769851\n ],\n [\n -91.39801025390625,\n 40.811730481593585\n ],\n [\n -91.7303466796875,\n 40.81380923056958\n ],\n [\n -91.7303466796875,\n 40.61603737424185\n ],\n [\n -91.702880859375,\n 40.58267063809529\n ],\n [\n -91.70013427734375,\n 40.55763465737646\n ],\n [\n -91.61773681640625,\n 40.54093880017256\n ],\n [\n -91.63421630859374,\n 40.50544628405211\n ],\n [\n -91.61224365234375,\n 40.49709237269567\n ],\n [\n -91.58477783203125,\n 40.463666324587685\n ],\n [\n -91.53533935546875,\n 40.457397087754444\n ],\n [\n -91.52984619140625,\n 40.40303919701655\n ],\n [\n -91.4996337890625,\n 40.39885600103786\n ],\n [\n -91.48590087890624,\n 40.384212768155045\n ],\n [\n -91.4501953125,\n 40.37375136672048\n ],\n [\n -91.41998291015625,\n 40.37375136672048\n ],\n [\n -91.37054443359375,\n 40.39258071969131\n ],\n [\n -91.37054443359375,\n 40.40931350359072\n ],\n [\n -91.38153076171875,\n 40.43858586704328\n ],\n [\n -91.35955810546875,\n 40.48455955508278\n ],\n [\n -91.36505126953125,\n 40.51797520038849\n ],\n [\n -91.40350341796875,\n 40.54093880017256\n ],\n [\n -91.3787841796875,\n 40.57432635193039\n ],\n [\n -91.34582519531249,\n 40.59935608796518\n ],\n [\n -91.29364013671875,\n 40.61812224225511\n ],\n [\n -91.24969482421875,\n 40.63479884404164\n ],\n [\n -91.1920166015625,\n 40.63479884404164\n ],\n [\n -91.14532470703125,\n 40.65563874006115\n ],\n [\n -91.12335205078125,\n 40.6723059714534\n ],\n [\n -91.10412597656249,\n 40.697299008636755\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576d0830e4b07657d1a37560","contributors":{"authors":[{"text":"Gordon, Donivan L.","contributorId":167291,"corporation":false,"usgs":false,"family":"Gordon","given":"Donivan","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":621766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25321,"text":"25321 - 1980 - Gulf of Mexico Outer Continental Shelf orders governing oil and gas lease operations","interactions":[],"lastModifiedDate":"2014-07-09T14:33:16","indexId":"25321","displayToPublicDate":"1980-01-01T14:29:39","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Gulf of Mexico Outer Continental Shelf orders governing oil and gas lease operations","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/25321","issn":"0364-7064","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Gulf of Mexico Outer Continental Shelf orders governing oil and gas lease operations, 1 p., https://doi.org/10.3133/25321.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":289688,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States;Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.86,18.18 ], [ -97.86,30.4 ], [ -81.04,30.4 ], [ -81.04,18.18 ], [ -97.86,18.18 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be6478e4b0527d5d4097bc","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":529210,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36664,"text":"36664 - 1980 - Water resources planning under the Fish and Wildlife Coordination Act","interactions":[],"lastModifiedDate":"2014-07-18T14:33:44","indexId":"36664","displayToPublicDate":"1980-01-01T14:23:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"80/44","title":"Water resources planning under the Fish and Wildlife Coordination Act","docAbstract":"This paper briefly discusses the more significant provisions of the Fish and Wildlife Coordination Act (1958). It covers pertinent aspects of legislative history, the development and current status (April 1980) of certain policies relevant to administering the Act, and other matters. It is directed primarily to practicing fish and wildlife agency field biologists, planners, and decisionmakers engaged in water resources development activities under the Act. It is not intended to be exhaustive in its treatment.
\nThe Fish and Wildlife Coordination Act provides a basic procedural framework for the orderly consideration of fish and wildlife conservation measures to be incorporated into Federal and Federally permitted or licensed water development projects. The principal provisions of the Act include:
\n1. a statement of Congressional purpose that fish and wildlife conservation shall receive equal consideration with other project features;
\n2. mandatory consultation with wildlife agencies with a view to achieving such conservation;
\n3. full consideration by action of the recommendations stemming from consultation;
\n4. authority for action agencies to implement such recommendations as they find acceptable.
\nThe FWCA in effect amends, conditions, or supplements other Federal laws and is thus closely linked in its application and interpretation. It is similarly linked to Federal planning standards and procedures. Because of this, interpretations tend to be flexible and evolve, adapting to changing situations.
\nThe following reference matrix outlines selected sections of the Fish and Wildlife Coordination Act which are of particular relevance to planners.
","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Performed for the Eastern Energy and Land Use Team, Office of Biological Services, Fish and Wildlife Service, U.S. Department of the Interior","usgsCitation":"Stutzman, K.F., 1980, Water resources planning under the Fish and Wildlife Coordination Act: FWS/OBS 80/44, xii, 44 p.","productDescription":"xii, 44 p.","costCenters":[],"links":[{"id":290477,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7cd9e4b0b2908510f054","contributors":{"authors":[{"text":"Stutzman, Karl F.","contributorId":28900,"corporation":false,"usgs":true,"family":"Stutzman","given":"Karl","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":216759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70120118,"text":"70120118 - 1980 - The quantification and reservation of instream flows","interactions":[],"lastModifiedDate":"2014-08-12T12:57:20","indexId":"70120118","displayToPublicDate":"1980-01-01T12:56:05","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3195,"text":"Progress in water technology","active":true,"publicationSubtype":{"id":10}},"title":"The quantification and reservation of instream flows","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Progress in water technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"International Association on Water Pollution Research","publisherLocation":"Oxford","usgsCitation":"Milhouse, R.T., and Grenney, W., 1980, The quantification and reservation of instream flows: Progress in water technology, v. 43, p. 129-130.","productDescription":"2 p.","startPage":"129","endPage":"130","numberOfPages":"2","costCenters":[],"links":[{"id":292024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a90e4b0461e44764adb","contributors":{"authors":[{"text":"Milhouse, Robert T.","contributorId":68233,"corporation":false,"usgs":true,"family":"Milhouse","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":497928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grenney, W.J.","contributorId":107624,"corporation":false,"usgs":true,"family":"Grenney","given":"W.J.","affiliations":[],"preferred":false,"id":497929,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70099969,"text":"70099969 - 1980 - Hydrogeologic data for south central Connecticut","interactions":[],"lastModifiedDate":"2014-04-10T06:56:47","indexId":"70099969","displayToPublicDate":"1980-01-01T09:35:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"32","title":"Hydrogeologic data for south central Connecticut","docAbstract":"No abstract available.","language":"English","publisher":"Connecticut Department of Environmental Protection","usgsCitation":"Haeni, F.P., and Anderson, H., 1980, Hydrogeologic data for south central Connecticut: Connecticut Water Resources Bulletin 32, Report: ii, 43 p.; 1 Plate: 31.87 x 54.54 inches.","productDescription":"Report: ii, 43 p.; 1 Plate: 31.87 x 54.54 inches","costCenters":[],"links":[{"id":286030,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70099969/report-thumb.jpg"},{"id":286029,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70099969/plate-1.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.125,41.125 ], [ -73.125,41.75 ], [ -72.625,41.75 ], [ -72.625,41.125 ], [ -73.125,41.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559475e4b0120853e8c004","contributors":{"authors":[{"text":"Haeni, F. Peter","contributorId":41479,"corporation":false,"usgs":true,"family":"Haeni","given":"F.","email":"","middleInitial":"Peter","affiliations":[],"preferred":false,"id":492073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":492074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70120203,"text":"70120203 - 1980 - Technical considerations in water quality management","interactions":[],"lastModifiedDate":"2014-08-13T09:10:45","indexId":"70120203","displayToPublicDate":"1980-01-01T09:09:05","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Technical considerations in water quality management","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Water quality administration, a focus on Section 208","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Ann Arbor Science","publisherLocation":"Ann Arbor, MI","usgsCitation":"Milhous, R.T., 1980, Technical considerations in water quality management, chap. of Water quality administration, a focus on Section 208, p. 29-40.","productDescription":"12 p.","startPage":"29","endPage":"40","numberOfPages":"12","costCenters":[],"links":[{"id":292053,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bd3e4b02bf5a76740b8","contributors":{"editors":[{"text":"Lamb, Berton L.","contributorId":6775,"corporation":false,"usgs":true,"family":"Lamb","given":"Berton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":509944,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Milhous, Robert T.","contributorId":28646,"corporation":false,"usgs":true,"family":"Milhous","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":497970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176100,"text":"70176100 - 1980 - Water-level, recharge, discharge, specific-capacity, well-yield, and aquifer-test data for the Edwards aquifer in the San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-25T16:25:32","indexId":"70176100","displayToPublicDate":"1980-01-01T01:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5176,"text":"Texas Department of Water Resources Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"LP-133","title":"Water-level, recharge, discharge, specific-capacity, well-yield, and aquifer-test data for the Edwards aquifer in the San Antonio area, Texas","docAbstract":"This report presents data and informat ion, and indicates other sources of data, on water level s, recharge, discharge, spec ifi c capacity, well yields, and aquifer tests for the Edwards aquifer in the Sa n Antonio area, Texas.
","language":"English","publisher":"Texas Department of Water Resources","usgsCitation":"Maclay, R., Small, T.A., and Rettman, P., 1980, Water-level, recharge, discharge, specific-capacity, well-yield, and aquifer-test data for the Edwards aquifer in the San Antonio area, Texas: Texas Department of Water Resources Report LP-133, 83 p.","productDescription":"83 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327864,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.twdb.texas.gov/publications/reports/limited_printing/doc/LP-133/LP-133.pdf"},{"id":327865,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c016d1e4b0f2f0ceb8737c","contributors":{"authors":[{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":647101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Small, T. A.","contributorId":105731,"corporation":false,"usgs":true,"family":"Small","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":647102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":647103,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70176029,"text":"70176029 - 1980 - Records of ground-water recharge and discharge, 1934-78; water levels, 1975-78; and chemical quality of water, 1977-78, for the Edwards aquifer in the San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-23T16:29:07","indexId":"70176029","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"38","title":"Records of ground-water recharge and discharge, 1934-78; water levels, 1975-78; and chemical quality of water, 1977-78, for the Edwards aquifer in the San Antonio area, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Reeves, R., Maclay, R., and Davis, M., 1980, Records of ground-water recharge and discharge, 1934-78; water levels, 1975-78; and chemical quality of water, 1977-78, for the Edwards aquifer in the San Antonio area, Texas: Edwards Underground Water District Bulletin 38, 53 p.","productDescription":"53 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327757,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73eee4b03fd6b7df2d7f","contributors":{"authors":[{"text":"Reeves, R.D.","contributorId":95043,"corporation":false,"usgs":true,"family":"Reeves","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":646818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":646819,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, M.F.","contributorId":79400,"corporation":false,"usgs":true,"family":"Davis","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":646820,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70171194,"text":"70171194 - 1980 - Food of alewives, yellow perch, spottail shiners, trout-perch, and slimy and fourhorn sculpins in southeastern Lake Michigan","interactions":[],"lastModifiedDate":"2016-05-25T13:21:32","indexId":"70171194","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesNumber":"98","subseriesTitle":"Technical papers of the U.S. Fish and Wildlife Service","title":"Food of alewives, yellow perch, spottail shiners, trout-perch, and slimy and fourhorn sculpins in southeastern Lake Michigan","docAbstract":"Stomachs of 1, 064 alewives (Alosa pseudoharengus), 1, 103 yellow perch (Perca flavescens), 246 spottail shiners (Notropis hudsonius), 288 trout-perch (Percopsis omiscomaycus), 454 slimy sculpins (Cottus cognatus), and 562 fourhorn sculpins (Myoxocephalus quadricornis) from Lake Michigan were examined for food contents. Fish were sampled primarily from March to November and nearly all were caught at the bottom in the southeastern part of the lake near Saugatuck, Michigan. Depths of capture (m) were: alewives, 5 to 110; yellow perch, 5 to 26; spottail shiners, 5 to 31; trout-perch, 9 to 46; slimy sculpins, 31 to 91; and fourhorn sculpins, 73 to 110. Alewives, particularly those less than 140 mm long, fed chiefly on zooplankton; Pontoporeia usually constituted most of the rest of the food, although Mysis and immature midges were occasionally eaten in considerable quantity. Yellow perch ate primarily Pontoporeia, fish eggs, Mysis, and crayfish; Pontoporeiawas consumed most heavily by perch less than 250 mm long and those in relatively deep water, fish (mainly slimy sculpins) by those 200 mm long or longer, Mysis by those in deep water, and crayfish by those on rocky bottom. Spottail shiners fed most commonly on immature midges, Pontoporeia, zooplankton, fingernail clams, and (in July only) fish eggs; immature midges were eaten mainly by shiners in shallow water; and Pontoporeia by those in deeper areas. The diet of trout-perch was strongly dominated by Pontoporeia and immature midges. Slimy sculpins ate Pontoporeia almost exclusively. Fourhorn sculpins fed almost entirely on Mysis and Pontoporeia Pontoporeia was particularly important in the diet of the larger fish.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Wells, L., 1980, Food of alewives, yellow perch, spottail shiners, trout-perch, and slimy and fourhorn sculpins in southeastern Lake Michigan, 12 p.","productDescription":"12 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccb9e4b07e28b662dcb7","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":630242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}