The habitat use information and Habitat Suitability Index (HSI) models presented in this document are intended for use in impact assessment and habitat management activities. Literature concerning the habitat requirements and preferences of northern pike is reviewed and then synthesized into HSI models, which are scaled to produce an index between 0 (unsuitable habitat) and 1 (optimal habitat). Assumptions used to transform habitat use information into these quantitative models are noted, and guidelines for model application are described. Other models found in the literature which may also be used to calculate an HSI are cited.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Inskip, P.D., 1982, Habitat Suitability Index Models: Northern pike: FWS/OBS 82/10.17, v, 40 p.","productDescription":"v, 40 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497c9","contributors":{"authors":[{"text":"Inskip, Peter D.","contributorId":75980,"corporation":false,"usgs":true,"family":"Inskip","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":216670,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7462,"text":"ofr82782 - 1982 - Progress report on lithium-related geologic investigations in Bolivia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr82782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-782","title":"Progress report on lithium-related geologic investigations in Bolivia","docAbstract":"The September 1, 1981, Samoa Islands Region earthquake occurred at the extreme northern end of the Tonga arc in a region where the Pacific plate may be disjointed along a hinge fault. In the last 50 years, magnitude 7 or greater earthquakes have occurred in this region on the average of once every six years, but four 7+ events have now occurred within the last six years. The mainshock was preceded about two hours earlier by a foreshock that was used as a calibration event for the Joint Epicenter Determination relocation of the mainshock and nearby seismicity occurring within a period seven months prior to and one week after the mainshock. The foreshock, better-located events of the prior seismicity, and most aftershocks are concentrated in a group near the mainshock epicenter, but several more distant aftershocks suggest that the aftershock zone may have been as large as 125 km in length and trended about S35?E. Identification of depth phases from a full suite of broadband records gives source depths of 25-3km for the mainshock and 29.5?3 km for the foreshock using a JB earth model. \r\n\r\nSource parameters were determined for the mainshock utilizing WWSSN analog and GDSN digital data. The preferred fault plane solution based on P-wave first motion data is a south by southwesterly steeply dipping normal fault, remarkably similar to the mechanism reported by Johnson and Molnar (1972) for the nearby earthquake of April 20, 196B. A waveform inversion technique described by Sipkin (1982), when applied to long-period P waveforms, gives an 'average' point source solution for a purely deviatoric moment rate tensor at a preferred source depth of 22 km. Very similar results were obtained from long-period GDSN body-wave and mantle-wave data using a centroid-moment tensor inversion technique described in Dziewonski, and others (1981). Both techniques provide solutions very close to a double couple source with a south by southwesterly shallow-dipping normal fault mechanism. \r\n\r\nTo obtain the scalar mantle wave moment, GDSN vertical and transverse records 20,000 see in length were processed as described by Buland and Taggart (1981). Averaging all the data from Rayleigh and Love waves yields an estimate of 3.8 x 10^27 dyne-cm (as compared to about 1.9 x 10^27 from body-wave moment tensor inversions) or a moment magnitude (Mr) of 7.6. \r\n\r\nFor the portion of the waveform analysed (50-5B sec), the body-wave inversion performed by Sipkin gives a source time function of duration approximately 28 sec with two peaks in activity. Simultaneous analysis of short-period records, and broadband ground displacements and velocities, a method described by Harvey and Choy (1982) and Choy and Boatwright (1981) revealed a complex rupture consisting of two subevents, of about the same moment, separated in time by about 25 sec, and with durations of about 25 sec each. The two peaks in activity resolved by the body-wave moment tensor inversion correspond to the first of these subevents.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82782","usgsCitation":"Davis, J., Howard, K.A., Rettig, S., Smith, R.L., Ericksen, G.E., Risacher, F., Alarcon, H., and Morales, R., 1982, Progress report on lithium-related geologic investigations in Bolivia: U.S. Geological Survey Open-File Report 82-782, 18 p., maps ;28 cm., https://doi.org/10.3133/ofr82782.","productDescription":"18 p., maps ;28 cm.","costCenters":[],"links":[{"id":140516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0782/report-thumb.jpg"},{"id":34882,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0782/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688582","contributors":{"authors":[{"text":"Davis, J.R.","contributorId":83907,"corporation":false,"usgs":true,"family":"Davis","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":155724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, K. A.","contributorId":48938,"corporation":false,"usgs":false,"family":"Howard","given":"K.","middleInitial":"A.","affiliations":[],"preferred":false,"id":155722,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rettig, S.L.","contributorId":42592,"corporation":false,"usgs":true,"family":"Rettig","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":155720,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, R. L.","contributorId":93904,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":155725,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ericksen, G. E.","contributorId":44538,"corporation":false,"usgs":true,"family":"Ericksen","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155721,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Risacher, Francois","contributorId":74748,"corporation":false,"usgs":true,"family":"Risacher","given":"Francois","email":"","affiliations":[],"preferred":false,"id":155723,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Alarcon, Hugo","contributorId":96678,"corporation":false,"usgs":true,"family":"Alarcon","given":"Hugo","email":"","affiliations":[],"preferred":false,"id":155726,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morales, Ricardo","contributorId":10796,"corporation":false,"usgs":true,"family":"Morales","given":"Ricardo","email":"","affiliations":[],"preferred":false,"id":155719,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":7805,"text":"ofr82985 - 1982 - Set-up manual for orienting stereo models of aerial photographs on the Kern PG2 photogrammetric plotter","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82985","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-985","title":"Set-up manual for orienting stereo models of aerial photographs on the Kern PG2 photogrammetric plotter","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82985","usgsCitation":"Banks, N., 1982, Set-up manual for orienting stereo models of aerial photographs on the Kern PG2 photogrammetric plotter: U.S. Geological Survey Open-File Report 82-985, 29 p., ill. ;28 cm., https://doi.org/10.3133/ofr82985.","productDescription":"29 p., ill. ;28 cm.","costCenters":[],"links":[{"id":140377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0985/report-thumb.jpg"},{"id":35304,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0985/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5219","contributors":{"authors":[{"text":"Banks, N.G.","contributorId":60635,"corporation":false,"usgs":true,"family":"Banks","given":"N.G.","email":"","affiliations":[],"preferred":false,"id":156639,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7576,"text":"ofr82535 - 1982 - Thermal regime of permafrost at Prudhoe Bay, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr82535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-535","title":"Thermal regime of permafrost at Prudhoe Bay, Alaska","docAbstract":"Temperature measurements through permafrost in the oil field at Prudhoe Bay, Alaska, combined with laboratory measurements of the thermal conductivity of drill cuttings permit an evaluation of in situ thermal properties and an understanding of the general factors that control the geothermal regime. A sharp contrast in temperature gradient at ~600 m represents a contrast in thermal conductivity caused by the downward change from interstitial ice to interstitial water at the base of permafrost under near steady-state conditions. Interpretation of the gradient contrast in terms of a simple model for the conductivity of an aggregate yields the mean ice content and thermal conductivities for the frozen and thawed sections (8.1 and 4.7 mcal/cm sec ?C, respectively). These results yield a heat flow of ~1.3 HFU which is similar to other values on the Alaskan Arctic Coast; the anomalously deep permafrost is a result of the anomalously high conductivity of the siliceous ice-rich sediments. Curvature in the upper 160 m of the temperature profiles represents a warming of ~1.8?C of the mean surface temperature, and a net accumulation of 5-6 kcal/cm 2 by the solid earth surface during the last 100 years or so. Rising sea level and thawing sea cliffs probably caused the shoreline to advance tens of kilometers in the last 20,000 years, inundating a portion of the continental shelf that is presently the target of intensive oil exploration. A simple conduction model suggests that this recently inundated region is underlain by near-melting ice-rich permafrost to depths of 300-500 m; its presence is important to seismic interpretations in oil exploration and to engineering considerations in oil production. With confirmation of the permafrost configuration by offshore drilling, heat-conduction models can yield reliable new information on the chronology of arctic shorelines.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82535","usgsCitation":"Lachenbruch, A., Sass, J., Marshall, B., and Moses, T.H., 1982, Thermal regime of permafrost at Prudhoe Bay, Alaska: U.S. Geological Survey Open-File Report 82-535, 77 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82535.","productDescription":"77 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":140718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0535/report-thumb.jpg"},{"id":35038,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0535/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa30a","contributors":{"authors":[{"text":"Lachenbruch, A.H.","contributorId":76737,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"A.H.","affiliations":[],"preferred":false,"id":156198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":156196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marshall, B.V.","contributorId":72375,"corporation":false,"usgs":true,"family":"Marshall","given":"B.V.","affiliations":[],"preferred":false,"id":156197,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moses, T. H. Jr.","contributorId":70385,"corporation":false,"usgs":true,"family":"Moses","given":"T.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":156195,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":36621,"text":"fwsobs82_10_15 - 1982 - Habitat Suitability Index Models: Green sunfish","interactions":[],"lastModifiedDate":"2022-02-15T14:27:54.093253","indexId":"fwsobs82_10_15","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.15","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Green sunfish","docAbstract":"This is one of a series of publications that provide information on the habitat requirements of selected fish and wildlife species. Literature describing the relationship between habitat variables related to life requisites and habitat suitability for the Green sunfish (Lepomis cyanellus) are synthesized. These data are subsequently used to develop Habitat Suitability (HIS) models. The HSI models are designed to provide information that can be used in impact assessment and habitat management.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Stuber, R.J., Gebhart, G., and Maughan, O.E., 1982, Habitat Suitability Index Models: Green sunfish: FWS/OBS 82/10.15, vi, 28 p.","productDescription":"vi, 28 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649865","contributors":{"authors":[{"text":"Stuber, Robert J.","contributorId":10849,"corporation":false,"usgs":true,"family":"Stuber","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":216664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":216666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":216665,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":36618,"text":"fwsobs82_10_12 - 1982 - Habitat Suitability Index Models: Common carp","interactions":[],"lastModifiedDate":"2022-02-15T14:29:21.252093","indexId":"fwsobs82_10_12","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.12","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Common carp","docAbstract":"The common carp (Cyprinus carpio) is a native of Asia. It is now found on every continent except Antarctica (Jester 1974) and in all 48 contiguous States (Sigler 1958). The northern limit to carp distribution appears to be the 18° C isotherm (Keleher 1956). The common carp hybridizes in nature with the goldfish (Carassius auratus) (Bardach et al. 1972; Smith 1979).
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Edwards, E.A., and Twomey, K., 1982, Habitat Suitability Index Models: Common carp: FWS/OBS 82/10.12, v, 28 p.","productDescription":"v, 28 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649d6e","contributors":{"authors":[{"text":"Edwards, Elizabeth A.","contributorId":39421,"corporation":false,"usgs":true,"family":"Edwards","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twomey, Katie","contributorId":66749,"corporation":false,"usgs":true,"family":"Twomey","given":"Katie","email":"","affiliations":[],"preferred":false,"id":216660,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26367,"text":"wri8237 - 1982 - Water resources and data-network assessment of the Manasota Basin, Manatee and Sarasota Counties, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri8237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-37","title":"Water resources and data-network assessment of the Manasota Basin, Manatee and Sarasota Counties, Florida","docAbstract":"The average annual rainfall in the Manasota Basin is 53.7 inches , and annual evapotranspiration is about 39 inches. Annual runoff from gaged parts of the Basin ranges from about 13 to 17 inches per year. Streamflow in the upland areas diminishes rapidly following the end of the rainy season and approaches zero during extended dry periods. Generally, surface water is of good quality except in tidally affected, coastal areas. Its quality varies seasonally, generally becoming more mineralized during the dry season. The principal hydrogeologic units are the surficial aquifer, the upper confining beds and minor artesian aquifers, the Floridan acquifer, and the lower confining bed. The quality of ground water is generally good except in the western and southern parts where saltwater intrusion or incomplete flushing of residual seawater has occurred. Land-use changes and stream impoundments and diversions require reassessment of the type and use of data collected by the surface-water network. Such changes may require modification of existing sites and establishment of new ones. Development and completion of the monitoring plan could provide most of the data necessary to define the groundwater system. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8237","usgsCitation":"Brown, D., 1982, Water resources and data-network assessment of the Manasota Basin, Manatee and Sarasota Counties, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-37, vi, 80 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8237.","productDescription":"vi, 80 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0037/report-thumb.jpg"},{"id":55161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8244","contributors":{"authors":[{"text":"Brown, David P.","contributorId":85590,"corporation":false,"usgs":true,"family":"Brown","given":"David P.","affiliations":[],"preferred":false,"id":196266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36617,"text":"fwsobs82_10_11 - 1982 - Habitat Suitability Index Models: Marten","interactions":[],"lastModifiedDate":"2022-02-15T14:29:46.968745","indexId":"fwsobs82_10_11","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.11","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Marten","docAbstract":"Habitat preferences and species characteristics of the pine marten (Martes americana) are described in this publication. It is one of a series of Habitat Suitability Index (HSI) models and was developed through an analysis of available scientific data on the species-habitat requirements of the pine marten. Habitat use information is presented in a review of the literature, followed by the development of a HSI model. The model is presented in three formats: graphic, word and mathematical. Suitability index graphs quantify the species-habitat relationship. These data are then synthesized into a model which is designed to provide information for use in impact assessment and habitat management activities.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Allen, A.W., 1982, Habitat Suitability Index Models: Marten (Revised 1984): FWS/OBS 82/10.11, vi, 9 p.","productDescription":"vi, 9 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":193123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"scale":"100000","edition":"Revised 1984","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497fa","contributors":{"authors":[{"text":"Allen, Arthur W.","contributorId":40648,"corporation":false,"usgs":true,"family":"Allen","given":"Arthur","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":216658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36616,"text":"fwsobs82_10_10 - 1982 - Habitat Suitability Index Models: Ferruginous hawk","interactions":[],"lastModifiedDate":"2022-02-15T14:30:11.663014","indexId":"fwsobs82_10_10","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.10","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Ferruginous hawk","docAbstract":"The ferruginous hawk inhabits grasslands, shrublands, and steppe-deserts of the Western United States. It is a common nester in Colorado, Idaho, Montana, Utah, and Wyoming (Call 1978). Populations in the more Northern States tend to be migratory, spending the winter in New Mexico, Colorado, Kansas, Texas, and Oklahoma (Call 1979).
Ferruginous hawks thrive in areas that favor the production of rabbits (Lagomorpha), prairie dogs (Cynomys spp.), or ground squirrels (Citellus spp. and Spermophilus spp.) (Call 1979), provided that suitable nesting sites are available. Foraging habitat consists of nonforested, nonmountainous areas, such as desert shrub and grassland communities. Nesting habitat consists of communities with isolated trees, woodland edges, buttes, cliffs, and/or grassland with some relief.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Jasikoff, T.M., 1982, Habitat Suitability Index Models: Ferruginous hawk: FWS/OBS 82/10.10, vi, 18 p.","productDescription":"vi, 18 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649936","contributors":{"authors":[{"text":"Jasikoff, Thomas M.","contributorId":40254,"corporation":false,"usgs":true,"family":"Jasikoff","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":216657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36615,"text":"fwsobs82_10_9 - 1982 - Habitat Suitability Index Models: Slough darter","interactions":[],"lastModifiedDate":"2022-02-15T14:30:38.749498","indexId":"fwsobs82_10_9","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.9","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Slough darter","docAbstract":"The native range of the slough darter (Etheostoma gracile) extends from western Alabama (Smith-Vaniz 1968) to central Texas and northward in the lowland areas of the former Mississippi Embayment and the Interior Low Plateau to central Illinois (Collette 1962) and southwestern Indiana (Gerking 1945). Its distribution also includes southeast Kansas (Metcalf 1959; Cross 1967) and northeast Oklahoma (Blair 1959). Natural hybridization with the blackside darter (Percina maculata) has been recorded (Page 1976).
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Edwards, E.A., Bacteller, M., and Maughan, O.E., 1982, Habitat Suitability Index Models: Slough darter: FWS/OBS 82/10.9, vi, 13 p.","productDescription":"vi, 13 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649758","contributors":{"authors":[{"text":"Edwards, Elizabeth A.","contributorId":39421,"corporation":false,"usgs":true,"family":"Edwards","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacteller, Mary","contributorId":74427,"corporation":false,"usgs":true,"family":"Bacteller","given":"Mary","email":"","affiliations":[],"preferred":false,"id":216656,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":216655,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":36614,"text":"fwsobs82_10_7 - 1982 - Habitat Suitability Index models: White crappie","interactions":[],"lastModifiedDate":"2022-02-15T14:31:04.515306","indexId":"fwsobs82_10_7","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.7","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index models: White crappie","docAbstract":"The white crappie (Pomoxis annularis) is native to freshwater lakes and streams from the southern Great Lakes, west to Nebraska, south to Texas and Alabama, east to North Carolina, then west of the Appalachian Mountains to New York. It has been widely introduced outside this range throughout North America (Hubbs and Lagler 1958; Goodson 1966; Scott and Crossman 1973).
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Edwards, E.A., Krieger, D.A., Gebhart, G., and Maughan, O.E., 1982, Habitat Suitability Index models: White crappie: FWS/OBS 82/10.7, vi, 22 p.","productDescription":"vi, 22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":164740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649710","contributors":{"authors":[{"text":"Edwards, Elizabeth A.","contributorId":39421,"corporation":false,"usgs":true,"family":"Edwards","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krieger, Douglas A.","contributorId":107758,"corporation":false,"usgs":true,"family":"Krieger","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":216652,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":216651,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":36612,"text":"fwsobs82_10_5 - 1982 - Habitat suitability index models: Cutthroat trout","interactions":[],"lastModifiedDate":"2022-02-15T14:32:15.628431","indexId":"fwsobs82_10_5","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.5","subseriesTitle":"Habitat Suitability Index","title":"Habitat suitability index models: Cutthroat trout","docAbstract":"Cutthroat trout, Salmo clarki, are a polytypic species consisting of several geographically distinct forms with a broad distribution and a great amount of genetic diversity (Hickman 1978; Behnke 1979). Behnke (1979) recognized 13 extant subspecies: Coastal cutthroat (S. c. clarki) in coastal streams from Prince William Sound, Alaska to the Eel Rlver in California; mountain cutthroat (~. ~. alpestris) in upper Columbia and F~Dser River drainages of British Columbia; west slope cutthroat (S. c. lewisi) in the upper Columbia, Salmon, Clearwater, South Saskatchewan and upper Missouri drainages of Montana and Idaho; an undescribed subspecies in the Alvord basin, Oregon; Lahonton cutthroat (S. c ..henshawi), Pauite cutthroat (S. c. seleniris), and an undescribed- subspecies in the Humboldt River drafnage of the Lahontan basin of Nevada and California; Yellowstone cutthroat (S. c. bouvieri) in the Yellowstone drainage of Wyoming and Montana and the Snake River drainage of Wyoming, Idaho, and Nevada; an undescribed subspecies (fine spotted) in the upper Snake River, Wyoming; Bonneville cutthroat (S. c. utah) in the Bonneville basin in Utah, Nevada, Idaho, and Wyoming; Colorado River cutthroat (~. ~. pleuriticus) in the Colorado River drainage in Wyoming, Utah, New Mexico, and Colorado; greenback cutthroat (S. c. stomias) in the South Platte and Arkansas River systems; and Rio Grande cutthroat (~. ~. virginalis) in the Rio Grande River drainage of Colorado and New Mexico. Many of these 13 subspecies are included on Federal or State endangered or threatened species lists.
Temperature and chemical preferences, migration, and other ecological and life history attributes vary among cutthroat subspecies (Behnke 1979). Differences in growth rate (Carlander 1969; Scott and Crossman 1973; Behnke 1979) and food preferences have also been reported (Trojnar and Behnke 1974) between some subspecies.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hickman, T.J., and Raleigh, R.F., 1982, Habitat suitability index models: Cutthroat trout: FWS/OBS 82/10.5, vi, 38 p.","productDescription":"vi, 38 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6499ff","contributors":{"authors":[{"text":"Hickman, Terry J.","contributorId":49840,"corporation":false,"usgs":true,"family":"Hickman","given":"Terry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":216644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raleigh, Robert F.","contributorId":49841,"corporation":false,"usgs":true,"family":"Raleigh","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":216645,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38576,"text":"pp1258A - 1982 - Continuity equation model of the predicted drastic retreat of Columbia Glacier, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1258A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1258","chapter":"A","title":"Continuity equation model of the predicted drastic retreat of Columbia Glacier, Alaska","language":"ENGLISH","doi":"10.3133/pp1258A","usgsCitation":"Rasmussen, L.A., and Meier, M.F., 1982, Continuity equation model of the predicted drastic retreat of Columbia Glacier, Alaska: U.S. Geological Survey Professional Paper 1258, p. A1-A23, https://doi.org/10.3133/pp1258A.","productDescription":"p. A1-A23","costCenters":[],"links":[{"id":122588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1258a/report-thumb.jpg"},{"id":65352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1258a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699013","contributors":{"authors":[{"text":"Rasmussen, Lowell A.","contributorId":36930,"corporation":false,"usgs":true,"family":"Rasmussen","given":"Lowell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":220093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meier, M. F.","contributorId":98713,"corporation":false,"usgs":true,"family":"Meier","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":220094,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36610,"text":"fwsobs82_10_2 - 1982 - Habitat suitability index models: Channel catfish","interactions":[],"lastModifiedDate":"2022-02-15T14:33:00.35072","indexId":"fwsobs82_10_2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/10.2","subseriesTitle":"Habitat Suitability Index","title":"Habitat suitability index models: Channel catfish","docAbstract":"The native range of channel catfish (Ictalurus Runctatus) extends from the southern portions of the Canadian prairie provinces south to the Gulf states, west to the Rocky Mountains, and east to the Appalachian Mountains (Trautman 1957; Miller 1966; Scott and Crossman 1973). They have been widely introduced outside this range and occur in essentially all of the Pacific and Atlantic drainages in the 48 contiguous states (Moore 1968; Scott and Crossman 1973). The greatest abundance of channel catfish generally occurs in the open (unleveed) floodplains of the Mississippi and Missouri River drainages (Walden 1964).
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McMahon, T., and Terrell, J.W., 1982, Habitat suitability index models: Channel catfish: FWS/OBS 82/10.2, vi, 29 p.","productDescription":"vi, 29 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649c45","contributors":{"authors":[{"text":"McMahon, Thomas E.","contributorId":93548,"corporation":false,"usgs":true,"family":"McMahon","given":"Thomas E.","affiliations":[],"preferred":false,"id":216640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terrell, James W. 0000-0001-5394-5663","orcid":"https://orcid.org/0000-0001-5394-5663","contributorId":92726,"corporation":false,"usgs":true,"family":"Terrell","given":"James","email":"","middleInitial":"W.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":216639,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36476,"text":"fwsobs82_59 - 1982 - Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options","interactions":[],"lastModifiedDate":"2018-01-30T12:45:31","indexId":"fwsobs82_59","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/59","title":"Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options","docAbstract":"This volume contains 16 papers and panel discussions from a conference held in Baton Rouge, La., 5-6 October 1981. The presentations consider the causes and consequences of coastal erosion and wetland modification in Louisiana and the mitigative options available to slow or reverse the rapid rate of coastal land loss. Detailed habitat mapping studies have allowed accurate estimates of coastal habitat change and land loss through 1978. Projections from these rates of change indicate an annual rate of land loss in coastal Louisiana in the early 1980's of approximately 130 km2/yr (50 m2/yr).
The projected effects of wetland modification on the bountiful living resources of coastal Louisiana (fisheries, fur and hide bearers and waterfowl) are major because of the close dependence of these resources on estuarine wetlands. These changes and others related to flood protection, transportation and ownership of mineral resources are projected to have extensive social and economic consequences.
Options proposed to slow coastal land loss include major and minor diversion of the Mississippi River, barrier island and shoreline restoration protection, hydrological management of wetlands and more restrictive permitting of dredging activities.
","language":"English","publisher":"U.S. Fish and Wildlife Service, Biological Services Program","publisherLocation":"Washington, D.C.","usgsCitation":"1982, Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options: FWS/OBS 82/59, viii, 256 p.","productDescription":"viii, 256 p.","numberOfPages":"265","costCenters":[],"links":[{"id":289595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289594,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fwsobs/1982/0059/report.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0434,28.9254 ], [ -94.0434,33.0195 ], [ -88.8162,33.0195 ], [ -88.8162,28.9254 ], [ -94.0434,28.9254 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660489","contributors":{"editors":[{"text":"Boesch, Donald F.","contributorId":23599,"corporation":false,"usgs":true,"family":"Boesch","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":504035,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":36490,"text":"fwsobs82_13_1 - 1982 - Procedure for developing biological input for the design, location, or modification of water intake structures","interactions":[],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"fwsobs82_13_1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82/13.1","title":"Procedure for developing biological input for the design, location, or modification of water intake structures","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Neitzel, D., and McKenzie, D., 1982, Procedure for developing biological input for the design, location, or modification of water intake structures: FWS/OBS 82/13.1, vi, 38, [45] p. : ill. ; 28 cm.","productDescription":"vi, 38, [45] p. : ill. ; 28 cm.","costCenters":[],"links":[{"id":163985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6609dc","contributors":{"authors":[{"text":"Neitzel, D.A.","contributorId":100905,"corporation":false,"usgs":true,"family":"Neitzel","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":216409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKenzie, D.H.","contributorId":89195,"corporation":false,"usgs":true,"family":"McKenzie","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":216408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70114182,"text":"70114182 - 1982 - Earthquake history of the United States","interactions":[],"lastModifiedDate":"2014-07-15T10:39:29","indexId":"70114182","displayToPublicDate":"1985-01-01T08:28:54","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":63,"text":"Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"41-1","title":"Earthquake history of the United States","docAbstract":"This publication is a history of the prominent earthquakes in the United States from historical times through 1970. It supersedes all previous editions with the same or similar titles (see page ii) and, in addition to updating earthquake listings through 1970, contains several additions and corrections to previous issues. It also brings together under a common cover earthquake data previously listed in two separate reports: Earthquake History of the United States, Part I, Stronger Earthquakes of the United States (Exclusive of California and Western Nevada) and Earthquake History of the United States, Part II, Stronger Earthquakes of California and Western Nevada. Another addition to this publication is the inclusion of a section describing earthquakes in the Puerto Rico region.
\nFor the purpose of listing and describing earthquakes, the United States has been divided into nine regions: (1) Northeastern Region, which includes New England and New York activity and observations of the principal earthquakes of eastern Canada; (2) Eastern Region, including the central Appalachian seismic region activity and the area near Charleston, S.C.; (3) Central Region, which consists of the area between the region just described and the Rocky Mountains; (4) Western Mountain Region, which includes all remaining states except those on the Pacific coast; (5) Washington and Oregon; (6) Alaska; (7) Hawaii; (8) Puerto Rico; and (9) California and Western Nevada. This arrangement has been made chiefly with reference to the natural seismic divisions. It also is a convenient arrangement because there are only three states where there is an important division of earthquake activity: In Tennessee, there are quite distinct areas at opposite ends of the state that fall into different regions. Only central and eastern Nevada are included in the Western Mountain Region, as the activity of the western part is closely associated with that of California. Some earthquake activity has occurred in the part of Texas located in the Western Mountain Region.
\nThe map facing page 1 shows locations of all earthquakes in the regions that follow. A small map showing the area covered by each region immediately precedes the résumé of each chapter (except for the Alaska, Puerto Rico, and Hawaii regions). The seismic risk map below was developed in January 1969 for the conterminous United States by Dr. S. T. Algermissen of NOAA's Environmental Research Laboratories. Subject to revision as continuing research warrants, it is an updated edition of a map divides the United States into four zones: Zone 0, areas with no reasonable expectancy of earthquake damage; Zone 1, expected minor damage; Zone 2, expected moderate damage; and Zone 3, major destructive earthquakes may occur.
","language":"English","publisher":"U.S. Department of Commerce, National Oceanic and Atmospheric Administration; U.S. Department of the Interior, Geological Survey","publisherLocation":"Boulder, CO","usgsCitation":"Coffman, J.L., Von Hake, C.A., and Stover, C.W., 1982, Earthquake history of the United States (Revised edition (through 1970), reprinted 1982 with supplement (1971-80)): Publication 41-1, xii, 208 p., v, 50 p.","productDescription":"xii, 208 p., v, 50 p.","numberOfPages":"277","costCenters":[],"links":[{"id":290115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290114,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114182/report.pdf"}],"country":"Canada;United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -63.9832,71.833333 ], [ -63.9832,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","edition":"Revised edition (through 1970), reprinted 1982 with supplement (1971-80)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9de9e4b065055fab1662","contributors":{"editors":[{"text":"Coffman, Jerry L.","contributorId":49706,"corporation":false,"usgs":true,"family":"Coffman","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":509910,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"von Hake, Carl A.","contributorId":112151,"corporation":false,"usgs":true,"family":"von Hake","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":509911,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":509909,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Coffman, Jerry L.","contributorId":49706,"corporation":false,"usgs":true,"family":"Coffman","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":495255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Von Hake, Carl A.","contributorId":42634,"corporation":false,"usgs":true,"family":"Von Hake","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":495254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495253,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70164423,"text":"70164423 - 1982 - On Lagrangian residual currents with applications in south San Francisco Bay, California","interactions":[],"lastModifiedDate":"2018-02-05T12:40:53","indexId":"70164423","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"On Lagrangian residual currents with applications in south San Francisco Bay, California","docAbstract":"The Lagrangian residual circulation has often been introduced as the sum of the Eulerian residual circulation and the Stokes' drift. Unfortunately, this definition of the Lagrangian residual circulation is conceptually incorrect because both the Eulerian residual circulation and the Stokes' drift are Eulerian variables. In this paper a classification of various residual variables are reviewed and properly defined. The Lagrangian residual circulation is then studied by means of a two-stage formulation of a computer model. The tidal circulation is first computed in a conventional Eulerian way, and then the Lagrangian residual circulation is determined by a method patterned after the method of markers and cells. To demonstrate properties of the Lagrangian residual circulation, application of this approach in South San Francisco Bay, California, is considered. With the aid of the model results, properties of the Eulerian and Lagrangian residual circulation are examined. It can be concluded that estimation of the Lagrangian residual circulation from Eulerian data may lead to unacceptable error, particularly in a tidal estuary where the tidal excursion is of the same order of magnitude as the length scale of the basin. A direction calculation of the Lagrangian residual circulation must be made and has been shown to be feasible.
By 1980 there were 1,608 reservoirs (over 202 ha each) with a surface area of 4 million ha in the United States. Construction of new reservoirs has decreased in recent years because of the lack of suitable sites and the opposition of environmental interests. Reservoirs have characteristics of both lacustrine and riverine ecosystems. Reservoirs have been segmented into riverine, transitional and lacustrine zones for simulation modelling.Fish and plankton production increases rapidly after initial impoundment and then decreases and stabilizes at lower levels. Decreases in the number of fish species and in fish biomass following impoundment are caused by reduced quantity and quality of spawning and nursery habitat and decreased detrital input. Plankton populations can be followed downstream in a series of reservoirs and increases in abundance were associated with the inundation of vegetation or the introduction of nutrients.In addition to water level management, the most effective fish management programs have included introducing new fishes, developing vegetation or building structures on the reservoir bottom. Considerable progress has been made in predicting the effects of environmental parameters on fish production.
","language":"English","publisher":"Informa","doi":"10.4296/cwrj0701002","usgsCitation":"Benson, N.G., 1982, Some observations on the ecology and fish management of reservoirs in the United States: Canadian Water Resources Journal, v. 7, no. 1, p. 2-25, https://doi.org/10.4296/cwrj0701002.","productDescription":"24 p.","startPage":"2","endPage":"25","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":480246,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4296/cwrj0701002","text":"Publisher Index Page"},{"id":371115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota","otherGeospatial":"Missouri River reservoirs","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.072509765625,\n 47.71715357016648\n ],\n [\n -108.314208984375,\n 47.5394554474239\n ],\n [\n -108.050537109375,\n 47.234489635299184\n ],\n [\n -106.14990234375,\n 47.53203824675999\n ],\n [\n -104.490966796875,\n 47.98256841921405\n ],\n [\n -102.952880859375,\n 47.923704717745686\n ],\n [\n -102.568359375,\n 47.42808726171425\n ],\n [\n -101.513671875,\n 47.27922900257082\n ],\n [\n -100.821533203125,\n 46.05036097561633\n ],\n [\n -100.887451171875,\n 45.18978009667531\n ],\n [\n -101.304931640625,\n 44.70770622183535\n ],\n [\n -100.61279296875,\n 44.26093725039923\n ],\n [\n -98.997802734375,\n 43.0287452513488\n ],\n [\n -98.646240234375,\n 42.91620643817353\n ],\n [\n -98.316650390625,\n 43.1090040242731\n ],\n [\n -99.47021484375,\n 44.26093725039923\n ],\n [\n -100.4150390625,\n 44.66083904265621\n ],\n [\n -100.14038085937499,\n 45.034714778688624\n ],\n [\n -100.184326171875,\n 45.598665689820635\n ],\n [\n -100.38208007812499,\n 46.15700496290803\n ],\n [\n -100.294189453125,\n 46.64189395892872\n ],\n [\n -100.94238281249999,\n 47.64318610543658\n ],\n [\n -102.008056640625,\n 47.71715357016648\n ],\n [\n -102.161865234375,\n 48.03401915864286\n ],\n [\n -103.095703125,\n 48.29050321714062\n ],\n [\n -104.99633789062499,\n 48.20271028869972\n ],\n [\n -106.12792968749999,\n 48.12943437745315\n ],\n [\n -106.6552734375,\n 48.04870994288686\n ],\n [\n -106.951904296875,\n 47.87214396888731\n ],\n [\n -107.46826171874999,\n 47.79839667295524\n ],\n [\n -108.072509765625,\n 47.71715357016648\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Benson, N. G.","contributorId":9593,"corporation":false,"usgs":true,"family":"Benson","given":"N.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":779202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70188838,"text":"70188838 - 1982 - The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain","interactions":[],"lastModifiedDate":"2017-06-26T11:13:55","indexId":"70188838","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","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":"The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain","docAbstract":"Seismic refraction profiles recorded along the eastern Snake River Plain (ESRP) in southeastern Idaho during the 1978 Yellowstone-Snake River Plain cooperative seismic profiling experiment are interpreted to infer the crustal velocity and attenuation (Q-1) structure of the ESRP. Travel-time and synthetic seismogram modeling of a 250 km reversed refraction profile as well as a 100 km detailed profile indicate that the crust of the ESRP is highly anomalous. Approximately 3 to 6 km of volcanic rocks (with some interbedded sediments) overlie an upper-crustal layer (compressional velocity ≅6.1 km/s) which thins southwestward along the ESRP from a thickness of 10 km near Island Park Caldera to 2 to 3 km beneath the central and southwestern portions of the ESRP. An intermediate-velocity (≅6.5 km/s) layer extends from ≅10 to ≅20 km depth. A thick (≅22 km) lower crust of compressional velocity 6.8 km/s, a total crustal thickness of ≅42 km, and a Pnvelocity of ≅7.9 km/s is observed in the ESRP, similar to the western Snake River Plain and the Rocky Mountains Provinces. High attenuation is evident on the amplitude corrected seismic data due to low-Q values in the volcanic rocks (Qp = 20 to 200) and throughout the crust (Qp = 160 to 300). Based on these characteristics of the crustal structure and volcanic-age progression data, it is suggested that the ESRP has resulted from an intensive period of intrusion of mantle-derived basaltic magma into the upper crust generating explosive silicic volcanism and associated regional uplift and caldera collapse. This activity began about 15 m.y. ago in southwestern Idaho and has migrated northeast to its present position at Yellowstone. Subsequent cooling of the intruded upper crust results in the 6.5 km/s velocity intermediate layer. Crustal subsidence and periodic basaltic volcanism as represented by the ESRP complete the sequence of crustal evolution.
","language":"English","publisher":"Wiley","doi":"10.1029/JB087iB04p02597","usgsCitation":"Braile, L., Smith, R.B., Ansorge, J., Baker, M., Sparlin, M., Prodehl, C., Schilly, M., Healy, J.H., , M., and Olsen, K., 1982, The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain: Journal of Geophysical Research B: Solid Earth, v. 87, no. B4, p. 2597-2609, https://doi.org/10.1029/JB087iB04p02597.","productDescription":"13 p.","startPage":"2597","endPage":"2609","costCenters":[],"links":[{"id":342866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B4","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"59521d2ae4b062508e3c36f1","contributors":{"authors":[{"text":"Braile, L.W.","contributorId":85332,"corporation":false,"usgs":true,"family":"Braile","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":700633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. B.","contributorId":64589,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":700634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ansorge, J.","contributorId":38318,"corporation":false,"usgs":true,"family":"Ansorge","given":"J.","email":"","affiliations":[],"preferred":false,"id":700635,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, M.R.","contributorId":193474,"corporation":false,"usgs":false,"family":"Baker","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":700636,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sparlin, M.A.","contributorId":193497,"corporation":false,"usgs":false,"family":"Sparlin","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":700637,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Prodehl, C.","contributorId":100376,"corporation":false,"usgs":true,"family":"Prodehl","given":"C.","affiliations":[],"preferred":false,"id":700638,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schilly, M.M.","contributorId":193496,"corporation":false,"usgs":false,"family":"Schilly","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":700639,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":700640,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":" Mueller","contributorId":19328,"corporation":false,"usgs":true,"given":"Mueller","email":"","affiliations":[],"preferred":false,"id":700641,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Olsen, K.H.","contributorId":95201,"corporation":false,"usgs":true,"family":"Olsen","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":700642,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70188756,"text":"70188756 - 1982 - Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California","interactions":[],"lastModifiedDate":"2020-10-21T15:44:58.054907","indexId":"70188756","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California","docAbstract":"If the San Andreas fault with about 300 km of right slip, the Carlock fault with about 60 km of left slip, and the Big Pine fault with about 15 km of left slip are considered to have been contemporaneously active, a space problem at their high-angle junctions becomes apparent. Large crustal masses converge in the area of the junctions as a result of the simultaneous large displacements on the faults. We present here a model in which an early straight north-northwest–trending San Andreas deforms to its present bent configuration in response to a westward displacement of crust north of the Garlock fault. During this deformation, the crust north of the Garlock in the vicinity of the junction undergoes north-south shortening, while the fault junction migrates along the trace of the San Andreas fault to the southeast relative to its original position. As a result of this migration, the Mojave area is displaced to the east relative to the original junction position. We suggest a similar history in mirror image for the Big Pine fault and the areas of crust adjacent to it.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<358:KEOTJO>2.0.CO;2","usgsCitation":"Bohannon, R.G., and Howell, D.G., 1982, Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California: Geology, v. 10, no. 7, p. 358-363, https://doi.org/10.1130/0091-7613(1982)10<358:KEOTJO>2.0.CO;2.","productDescription":"6 p.","startPage":"358","endPage":"363","costCenters":[],"links":[{"id":342792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Big Pine fault, Garlock fault, San Andreas 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