{"pageNumber":"6029","pageRowStart":"150700","pageSize":"25","recordCount":184582,"records":[{"id":70232221,"text":"70232221 - 1976 - Cenozoic deposits of southeastern New Mexico and an outline of the history of evaporite dissolution","interactions":[],"lastModifiedDate":"2022-06-15T15:34:50.74069","indexId":"70232221","displayToPublicDate":"1976-03-01T10:25:51","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Cenozoic deposits of southeastern New Mexico and an outline of the history of evaporite dissolution","docAbstract":"

Sedimentary records of Cenozoic history in southeastern New Mexico begin with the Ogallala Formation of Miocene and Pliocene age. Later records include the Gatuna Formation of early or middle Pleistocene age, Mescalero caliche, an informal term, of middle Pleistocene age, and fluvial deposits of late Pleistocene age but there are many gaps in the record. The modern landscape is the result of erosion and deposition in climates that have ranged from semihumid to semiarid as well as dissolution of soluble rocks in Permian formations in the subsurface. This dissolution may have begun as early as Jurassic time and has continued intermittently to the present.

","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Bachman, G.O., 1976, Cenozoic deposits of southeastern New Mexico and an outline of the history of evaporite dissolution: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 135-149.","productDescription":"15 p.","startPage":"135","endPage":"149","costCenters":[],"links":[{"id":402207,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402205,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"New 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history of the region","docAbstract":"

The oldest rocks in Costa Rica, the Nicoya Complex, crop out in an arcuate belt along the Pacific coast and outside the mapped area. The complex is an ophiolite assemblage and indicates that a Late Cretaceous arc-trench system, probably a southerly extension of the Middle America Trench, lay along and west of the present Pacific coast. Polarity of the system is indicated by the presence of a volcanic olivine basalt arc east of the ophiolite belt and by a younger magmatic arc farther east. Relative lack of metamorphism of the ophiolite assemblage suggests that the rocks were obducted rather than subducted. Fossil evidence indicates that the complex was emplaced no later than the late Campanian. By the late Eocene both the ophiolite assemblage and the olivine basalt arc had been established as major sediment sources for basins that lay to the east, and they continued as such through the Oligocene and possibly into the middle Miocene. Widespread deposition of trachyandesite lava and volcaniclastic sediments, local marine planation, uplift, and renewed volcanism mark what is presumed to be the end of the Miocene. Extreme south-to-north coarsening of the unconformably superposed Doan Formation and the presence of corals in the shaly facies of the Doan in the southern part of the mapped areas suggest that marine sedimentation there was undisturbed by orogeny and that intrusion of the Talamancan magmatic rocks must have followed deposition of the Doan. Volcaniclastic block breccia, characteristic of northern exposures of the Doan, indicates that volcanism in the proto- Cordillera Central had begun by at least Doan time. Volcanism has been a dominant process in central Costa Rica since that time.

","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Krushensky, R.D., Malavassi, E.V., and Castillo, R.M., 1976, Geology of central Costa Rica and its implications in the geologic history of the region: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 127-134.","productDescription":"8 p.","startPage":"127","endPage":"134","costCenters":[],"links":[{"id":402203,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402202,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"Costa Rica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.638916015625,\n 9.112944562617598\n ],\n [\n -82.96875,\n 9.893098633379584\n ],\n [\n -83.51806640624999,\n 10.563422129963456\n ],\n [\n -84.88037109375,\n 10.055402736564236\n ],\n [\n -84.66064453125,\n 9.611582210984674\n ],\n [\n -83.638916015625,\n 9.112944562617598\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Krushensky, Richard D.","contributorId":106994,"corporation":false,"usgs":true,"family":"Krushensky","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":844705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malavassi, Enrique V.","contributorId":18853,"corporation":false,"usgs":true,"family":"Malavassi","given":"Enrique","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":844706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Castillo, Rolando M.","contributorId":27143,"corporation":false,"usgs":true,"family":"Castillo","given":"Rolando","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":844707,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70232253,"text":"70232253 - 1976 - Determination, storage, and preservation of low molecular weight hydrocarbon gases in aqueous solution","interactions":[],"lastModifiedDate":"2022-06-17T15:13:32.773557","indexId":"70232253","displayToPublicDate":"1976-03-01T10:00:02","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Determination, storage, and preservation of low molecular weight hydrocarbon gases in aqueous solution","docAbstract":"

A gas chromatograph with a flame ionization detector was used in conjunction with a stripping chamber and cold trap apparatus to measure microgram-per-litre quantities of low molecular weight hydrocarbon gases in water samples. Glass bottles with ground-glass stoppers were used to store the samples. Formalin was added to stop bacterial activity and preserve samples with no measurable losses for as much as 7 days.

","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Schultz, D.J., Pankow, J.F., Tai, D.Y., Stephens, D.W., and Rathbun, R.E., 1976, Determination, storage, and preservation of low molecular weight hydrocarbon gases in aqueous solution: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 247-251.","productDescription":"5 p.","startPage":"247","endPage":"251","costCenters":[],"links":[{"id":402334,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402333,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schultz, D. J.","contributorId":292492,"corporation":false,"usgs":false,"family":"Schultz","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":844811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pankow, J. F.","contributorId":20917,"corporation":false,"usgs":true,"family":"Pankow","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":844812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":844813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":844814,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":844815,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70232250,"text":"70232250 - 1976 - Solute transport and modeling of water quality in a small stream","interactions":[],"lastModifiedDate":"2022-06-17T14:50:02.510847","indexId":"70232250","displayToPublicDate":"1976-03-01T09:40:26","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Solute transport and modeling of water quality in a small stream","docAbstract":"

An injection of chloride, sodium, and stable strontium was made at a constant rate for 3 hours into Uvas Creek, Santa Clara County, Calif., to determine the mass transport processes in a small stream. Five observation points were selected within a 610-metre reach of the stream below the injection site. Water samples were collected at the observation points during and immediately after the injection. A mathematical model of the stream was obtained by solving analytically and optimally the one-dimensional mass transport equation of the solutes in the stream. Comparison of field results with a simplified mathematical model indicates the dominance of convection in the behavior of sodium and chloride. The concentration of chloride and sodium can be closely simulated by the model. However, strontium cannot be well represented by the simplified model, which contains a first-order decay-type sink.

","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Zand, S.M., Kennedy, V.C., Zellweger, G.W., and Avanzino, R., 1976, Solute transport and modeling of water quality in a small stream: Journal of Research of the U.S. Geological Survey, p. 233-240.","productDescription":"8 p.","startPage":"233","endPage":"240","costCenters":[],"links":[{"id":402330,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402329,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Santa Clara County","otherGeospatial":"Uvas Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.84627532958984,\n 37.07147779838202\n ],\n [\n -121.74156188964845,\n 37.07147779838202\n ],\n [\n -121.74156188964845,\n 37.10516392042412\n ],\n [\n -121.84627532958984,\n 37.10516392042412\n ],\n [\n -121.84627532958984,\n 37.07147779838202\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zand, S. M.","contributorId":292491,"corporation":false,"usgs":false,"family":"Zand","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":844805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":844806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zellweger, G. W.","contributorId":55445,"corporation":false,"usgs":true,"family":"Zellweger","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":844807,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Avanzino, R.J.","contributorId":37336,"corporation":false,"usgs":true,"family":"Avanzino","given":"R.J.","affiliations":[],"preferred":false,"id":844808,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1007781,"text":"1007781 - 1976 - The abundance and diversity of the herpetofaunas of tropical forest litters","interactions":[],"lastModifiedDate":"2023-08-29T15:58:35.649798","indexId":"1007781","displayToPublicDate":"1976-03-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1045,"text":"Biotropica","active":true,"publicationSubtype":{"id":10}},"title":"The abundance and diversity of the herpetofaunas of tropical forest litters","docAbstract":"

Quantitative and qualitative samples of amphibian and lizard faunas were taken from forest litter in Costa Rica and compared with similar samples collected in Borneo, the Philippines, and Panama. Animal abundance is about ten times greater in Costa Rican lowland wet forest than in Borneo. Radically different routes and rates of energy flow are postulated to account for the difference. In a series of upland (1010-1425 m) samples in the Philippines, the number of litter lizards and frogs increases with elevation. A single upland (1200 m) Costa Rican sample contains about three times as many animals per 100 m2 as two lowland sites. This increase with altitude correlates well with hypotheses that overall tropical forest productivity is greatest at intermediate elevations. Herpetofaunal densities are greater in wet areas compared to dry sites and flat terrain compared to slopes. These observations are linked to the greater variation and lesser total litter fall in dry sites and/or slopes. The number of species of amphibians and lizards regularly inhabiting the litter is similar in all wet lowland forests studied. Increasing elevation and decreasing rainfall correlate with faunas having fewer species. The former is seen as the result of the differential ability of lowland species to invade uplands, and the latter as a decrease in the kind and duration of frog-spawning sites. Reduced equitability with increasing elevation is principally due to the much greater proportional increase of the commonest species. In the evolution of American and Bornean-Philippine wet lowland faunas, frogs with direct development (Eleutherodactylus) have radiated in the former in the same fashion that skinks have in the latter.

","language":"English","publisher":"Wiley","doi":"10.2307/2387818","usgsCitation":"Scott, N.J., 1976, The abundance and diversity of the herpetofaunas of tropical forest litters: Biotropica, v. 8, p. 41-58, https://doi.org/10.2307/2387818.","productDescription":"18 p.","startPage":"41","endPage":"58","numberOfPages":"18","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129860,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66acbe","contributors":{"authors":[{"text":"Scott, Norman J. Jr.","contributorId":112614,"corporation":false,"usgs":true,"family":"Scott","given":"Norman","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":316020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1007751,"text":"1007751 - 1976 - Differential seed predation on two species of Arctostaphylos (Ericaceae)","interactions":[],"lastModifiedDate":"2025-05-23T17:03:49.681884","indexId":"1007751","displayToPublicDate":"1976-03-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2932,"text":"Oecologia","active":true,"publicationSubtype":{"id":10}},"title":"Differential seed predation on two species of Arctostaphylos (Ericaceae)","docAbstract":"

The fire-prone California chaparral contains two sympatric species of shrubs: Arctostaphylos glauca and A. glandulosa. A previous study showed that in a stand where both species had similar amounts of coverage, A. glauca had fewer seeds in the soil. We attempt to answer the questions: 1) Could ground-foraging seed predators produce the lower population of A. glauca seeds in the soil? 2) Do predators select fruits randomly with respect to fruit size? 3) Do the fruits of the two species differ in the proportions of fruit components (i.e. seeds, endocarp, mesocarp, and exocarp) in ways that could be important to seed predators? Predation was measured on artificial caches of fruits, for 17 weeks. Selection by predators was examined by comparing weights of fruits recovered from soil samples with newlymatured fruits on the shrubs. Fruits components were characterized by dividing fruits into 3 fractions and weighing. More fruits of A. glauca were removed from the caches. Fruits of both species recovered from the soil were lighter than those on the shrubs. The weights of seeds, stony and fleshy fruit layers were all larger in A. glauca. Within fruits of A. glandulosa, the weights of the three components, various combinations, and ratios were all significantly correlated, while in A. glauca no other component, combination of components, or ratio examined was significantly correlated with the weights of the seeds.

","language":"English","publisher":"Springer Nature","doi":"10.1007/BF00545488","usgsCitation":"Keeley, J., and Hays, R., 1976, Differential seed predation on two species of Arctostaphylos (Ericaceae): Oecologia, v. 24, p. 71-81, https://doi.org/10.1007/BF00545488.","productDescription":"11 p.","startPage":"71","endPage":"81","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130184,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"San Diego County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.32686845808135,\n 32.9169897810403\n ],\n [\n -117.32686845808135,\n 32.55935355113901\n ],\n [\n -116.88408260322085,\n 32.55935355113901\n ],\n [\n -116.88408260322085,\n 32.9169897810403\n ],\n [\n -117.32686845808135,\n 32.9169897810403\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"24","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d6cf","contributors":{"authors":[{"text":"Keeley, Jon E. 0000-0002-4564-6521","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":69082,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon E.","affiliations":[],"preferred":false,"id":315966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hays, R.L.","contributorId":40162,"corporation":false,"usgs":true,"family":"Hays","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":315965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5223543,"text":"5223543 - 1976 - Establishment of the black-tailed jackrabbit on the Virginia eastern shore","interactions":[],"lastModifiedDate":"2025-03-10T16:38:18.767277","indexId":"5223543","displayToPublicDate":"1976-02-27T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Establishment of the black-tailed jackrabbit on the Virginia eastern shore","docAbstract":"

No abstract available. 

","language":"English","publisher":"Oxford Academic","doi":"10.2307/1379525","usgsCitation":"Clapp, R.B., Weske, J., and Clapp, T., 1976, Establishment of the black-tailed jackrabbit on the Virginia eastern shore: Journal of Mammalogy, v. 57, no. 1, p. 180-181, https://doi.org/10.2307/1379525.","productDescription":"2 p.","startPage":"180","endPage":"181","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.53318689722039,\n 37.98487341318935\n ],\n [\n -76.53318689722039,\n 36.62076603430651\n ],\n [\n -75.79097825485586,\n 36.62076603430651\n ],\n [\n -75.79097825485586,\n 37.98487341318935\n ],\n [\n -76.53318689722039,\n 37.98487341318935\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd5a","contributors":{"authors":[{"text":"Clapp, R. B.","contributorId":9371,"corporation":false,"usgs":true,"family":"Clapp","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":338952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weske, J.S.","contributorId":102423,"corporation":false,"usgs":true,"family":"Weske","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":338954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clapp, T.C.","contributorId":45812,"corporation":false,"usgs":true,"family":"Clapp","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":338953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70200400,"text":"70200400 - 1976 - Geochemistry of thermal waters in Long Valley, Mono County, California","interactions":[],"lastModifiedDate":"2018-10-16T14:58:14","indexId":"70200400","displayToPublicDate":"1976-02-10T14:58:01","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of thermal waters in Long Valley, Mono County, California","docAbstract":"

Thermal springs and wells in Long Valley, California, issue sodium bicarbonate‐chloride waters containing 1000–1420 mg/l of dissolved solids. Thermal waters of sodium bicarbonate‐chloride composition are usually associated with hot‐water reservoirs. Chloride concentrations and stable isotope data indicate that the thermal waters have had varied histories. All of the thermal springs issue a mixture of fluid from the thermal reservoir and less saline, cooler water from one or more shallow aquifers. The composition of springs in Hot Creek Gorge may have been further altered by minor subsurface boiling. Thermal springs between Hot Creek and Lake Crowley issue mixtures of fresh and thermal waters which have lost heat by conductive cooling and changed composition by reaction with rock in the shallow aquifer. The silica content of water from Magma Richie 5 and mixing calculations based on the concentrations of silica in thermal waters collected from springs in Hot Creek Gorge and along Little Hot Creek indicate a temperature of at least 200°C in the thermal reservoir. The sodium‐potassium‐calcium geothermometer yields a reservoir temperature estimate near 200°C for most of the thermal springs. If geothermal energy is developed in Long Valley, the high concentrations of arsenic (up to 2.2 mg/l), boron (up to 15 mg/l), and total dissolved solids in the thermal fluids will make it necessary to isolate the effluent of production wells from the freshwater system.

","language":"English","publisher":"AGU","doi":"10.1029/JB081i005p00792","usgsCitation":"Mariner, R.H., and Willey, L.M., 1976, Geochemistry of thermal waters in Long Valley, Mono County, California: Journal of Geophysical Research, v. 81, no. 5, p. 792-800, https://doi.org/10.1029/JB081i005p00792.","productDescription":"9 p.","startPage":"792","endPage":"800","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":358407,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Mono County","otherGeospatial":"Long Valley","volume":"81","issue":"5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Mariner, Robert H. rmariner@usgs.gov","contributorId":3290,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"rmariner@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":748725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willey, Lawrence M.","contributorId":209752,"corporation":false,"usgs":false,"family":"Willey","given":"Lawrence","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":748726,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70119558,"text":"70119558 - 1976 - Roosting ecology of the pallid bat, Antrozous pallidus","interactions":[],"lastModifiedDate":"2014-08-07T12:55:12","indexId":"70119558","displayToPublicDate":"1976-02-01T12:48:31","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Roosting ecology of the pallid bat, Antrozous pallidus","docAbstract":"Daytime roosting behavior of pallid bats (Antrozous pallidus) was studied in central Arizona. Bats were present in the area from March or April until November and roosted in cliffs in colonies generally including 20 or more individuals. Pallid bats were highly selective in their choice of roost sites and minimized diurnal energy output by adaptive hypothermia and behavioral thermo-regulation. In spring and autumn the bats roosted in vertical crevices responsive to changes in ambient temperatures. Here temperatures remained low and the bats were torpid for much of the day, but when the crevices became heated in the late afternoon the bats were passively warmed prior to emergence. Deep, horizontal crevices were preferred in summer; cliffs function as massive heat sinks, and in summer crevice temperatures remained moderate and relatively stable. Throughout most of the day both the deep parts of the crevices and the body temperatures of the bats remained close to 30ºC; at this body temperature pallid bats have unexpectedly low metabolic rates (Trune, 1974). By adjusting their positions and closeness to other bats in the thermal gradient within the crevice, bats dissipate heat early in the day, maintain a low metabolic rate through most of the fat and elevate the body temperature prior to emergence in the evening. Of vital important to pallid bats in the summer are social behaviors that promote communal roosting at \"traditional\" crevices.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Mammalogy","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society of Mammalogists","publisherLocation":"Provo, UT","doi":"10.2307/1379510","usgsCitation":"Vaughan, T.A., and O'Shea, T., 1976, Roosting ecology of the pallid bat, Antrozous pallidus: Journal of Mammalogy, v. 57, no. 1, p. 19-42, https://doi.org/10.2307/1379510.","productDescription":"24 p.","startPage":"19","endPage":"42","numberOfPages":"24","costCenters":[],"links":[{"id":291841,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291840,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1379510"}],"volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e492cfe4b0fff40428a5e7","contributors":{"authors":[{"text":"Vaughan, Terry A.","contributorId":90648,"corporation":false,"usgs":true,"family":"Vaughan","given":"Terry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":497713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Shea, Thomas J. 0000-0002-0758-9730","orcid":"https://orcid.org/0000-0002-0758-9730","contributorId":78071,"corporation":false,"usgs":true,"family":"O'Shea","given":"Thomas J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":497712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010234,"text":"70010234 - 1976 - Application of multi-regional planning models to the scheduling of large-scale water resource systems development","interactions":[],"lastModifiedDate":"2025-04-10T15:32:02.76064","indexId":"70010234","displayToPublicDate":"1976-02-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Application of multi-regional planning models to the scheduling of large-scale water resource systems development","docAbstract":"

No abstract available. 

","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(76)90062-7","issn":"00221694","usgsCitation":"Moody, D., 1976, Application of multi-regional planning models to the scheduling of large-scale water resource systems development: Journal of Hydrology, v. 28, no. 2-4, p. 101-125, https://doi.org/10.1016/0022-1694(76)90062-7.","productDescription":"25 p.","startPage":"101","endPage":"125","costCenters":[],"links":[{"id":219436,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Puerto 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of Earth resources data that have been collected by agencies of the United States Government and to find out where and how these data may be obtained. Earth resources data as discussed here are those obtained by remote-sensing instruments, including aerial cameras, multispectral cameras, multispectral scanners, and radar. They are obtained by spacecraft and high-altitude aircraft. Also, various agencies have been acquiring vast quantities of conventional aerial mapping photography from low and medium altitudes for more than 50 years. There is also brief information to assist the reader in locating published references and identifying research projects relating to application of Earth resources data to a variety of purposes. In all cases, it is not the intent to say what data are needed or how the data are to be used, but to describe where an interested person can begin to locate Earth resources data.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039205","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Availability of Earth resources data: General Information Product, 46 p., https://doi.org/10.3133/70039205.","productDescription":"46 p.","numberOfPages":"48","costCenters":[],"links":[{"id":261376,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039205/report.pdf"},{"id":261377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039205/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ef08e4b0c8380cd4a0dd","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":535243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207697,"text":"70207697 - 1976 - Structure and evolution of Bering Sea shelf south of St. Lawrence Island","interactions":[],"lastModifiedDate":"2020-06-15T15:19:07.448226","indexId":"70207697","displayToPublicDate":"1976-01-06T15:44:21","publicationYear":"1976","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":"Structure and evolution of Bering Sea shelf south of St. Lawrence Island","docAbstract":"

The virtually featureless Beringian shelf south of St. Lawrence Island is underlain structurally by at least 14 basins. Encompassing a total area of more than 300,000 sq km, most of the basins are either elongate structural sags, grabens, or half (asymmetric) grabens beneath the outer shelf. The regional trend of these basins is northwest, parallel with that of the continental margin. Two of the basins, St. George and Navarin, contain 7 to 10 km of Upper Cretaceous(?) and Cenozoic sedimentary strata. A major divergence in dip of beds in the upper half of the sedimentary section may reflect an abrupt shelf-wide change in the rate of sedimentation and/or subsidence, probably during the Miocene. The outer sub-shelf basement grabens and adjacent ridges (horsts) are bounded by high-angle normal faults that exhibit growth-type structure.

St. Matthew basin, an elongate, southwest-trending feature of the inner shelf, lies along the offshore expression of the Kaltag fault of western Alaska. The Kaltag fault, like the Denali fault in southwestern Alaska, does not extend to the outer Bering Sea shelf but ends or turns parallel with the margin within the inner shelf.

The inner shelf is underlain by a broad basement high, Nunivak arch, the seaward half of which is characterized by an arcuate belt of high-frequency and high-amplitude magnetic anomalies. This zone of intense magnetic anomalies along the shelf is probably the signature of a Mesozoic magmatic arc that extends from southwestern Alaska to eastern Siberia and consists of Jurassic to Cretaceous plutonic and volcanic rocks. We speculate that this magmatic arc resulted from oblique convergence and subduction in the Mesozoic between the Kula(?) and North American plates along the eastern Beringian margin. Folding and uplift in the area of the present outer shelf occurred contemporaneously with magmatism along the inner shelf. Plate convergence apparently ceased by the end of the Mesozoic or t e beginning of the Cenozoic. Subsequently, the foldbelt underlying the outer shelf was eroded extensively and rifted extensionally to form large, deep basins. On the average, the shelf has subsided more than 1.5 km. Subsidence and sediment burial of the eroded orogen formed the modern Beringian shelf.

","language":"English","publisher":"AAPG","doi":"10.1306/83D92299-16C7-11D7-8645000102C1865D","usgsCitation":"Marlow, M.S., Scholl, D.W., Cooper, A.K., and Buffington, E.C., 1976, Structure and evolution of Bering Sea shelf south of St. Lawrence Island: AAPG Bulletin, v. 60, no. 2, p. 161-183, https://doi.org/10.1306/83D92299-16C7-11D7-8645000102C1865D.","productDescription":"23 p.","startPage":"161","endPage":"183","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371026,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bering Sea Shelf","volume":"60","issue":"2","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":779000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":779001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":779002,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buffington, E. C.","contributorId":13948,"corporation":false,"usgs":true,"family":"Buffington","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":779003,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70207696,"text":"70207696 - 1976 - Plate tectonic model for the evolution of the eastern Bering Sea Basin","interactions":[],"lastModifiedDate":"2020-06-15T15:17:00.551395","indexId":"70207696","displayToPublicDate":"1976-01-06T15:33:44","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Plate tectonic model for the evolution of the eastern Bering Sea Basin","docAbstract":"

The eastern Bering Sea Basin, composed of the Aleutian and Bowers Basins, is flanked to the north by Mesozoic foldbelts that probably represent zones of plate subduction in Mesozoic time. Present plate subduction occurs 400 to 1,000 km farther south, at the Aleutian Trench. North-south magnetic lineations that formed at an oceanic spreading ridge, probably in Mesozoic time (117 to 132 m.y. ago), have been identified in the Aleutian Basin. The orientation and age of those anomalies can be explained by reconstructing Kula-Farallon Pacific plate motions during late Mesozoic–early Tertiary time.

In Mesozoic time, subduction of the Kula plate occurred north of the Aleutian Trench near the present location of the Bering Sea continental margin. At about 70 m.y. B.P. (Late Cretaceous), the zone of subduction shifted south to the present location of the Aleutian Trench, thereby trapping a fragment of oceanic plate imprinted with north-south magnetic lineations within the eastern Bering Sea Basin. A stable basin framework has prevailed behind the Aleutian arc since early Tertiary time.

","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1976)87<1119:PTMFTE>2.0.CO;2","usgsCitation":"Cooper, A.K., Scholl, D.W., and Marlow, M.S., 1976, Plate tectonic model for the evolution of the eastern Bering Sea Basin: GSA Bulletin, v. 87, no. 8, p. 1119-1126, https://doi.org/10.1130/0016-7606(1976)87<1119:PTMFTE>2.0.CO;2.","productDescription":"8 p.","startPage":"1119","endPage":"1126","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371025,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Eastern Bering Sea basin","volume":"87","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"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":778997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":778998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":778999,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70198909,"text":"70198909 - 1976 - Geology of the Shenandoah National Park, Virginia","interactions":[],"lastModifiedDate":"2018-08-24T14:40:22","indexId":"70198909","displayToPublicDate":"1976-01-05T14:34:51","publicationYear":"1976","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Geology of the Shenandoah National Park, Virginia","largerWorkTitle":"Virginia Division of Mineral Resources Bulletin","publisher":"Commonwealth of Virginia, Dept. of Conservation and Economic Development, Division of Mineral Resources","publisherLocation":"Charlottesville, VA","usgsCitation":"Gathright, T.M., 1976, Geology of the Shenandoah National Park, Virginia, v. 86, 93 p.","productDescription":"93 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356737,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.dmme.virginia.gov/commercedocs/BUL_86.pdf","text":"Document"}],"country":"United States","state":"Virginia","otherGeospatial":"Shenandoah National Park","volume":"86","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gathright, Thomas M. II","contributorId":207266,"corporation":false,"usgs":false,"family":"Gathright","given":"Thomas","suffix":"II","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":743380,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15439,"text":"ofr7691 - 1976 - Ground-water quality at the site of a proposed deep-well injection system for treated wastewater, West Palm Beach, Florida","interactions":[],"lastModifiedDate":"2022-01-05T16:40:33.95307","indexId":"ofr7691","displayToPublicDate":"1976-01-01T22:10:00","publicationYear":"1976","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":"76-91","title":"Ground-water quality at the site of a proposed deep-well injection system for treated wastewater, West Palm Beach, Florida","docAbstract":"The U.S. Geological Survey collected scientific and technical information before, during, and after construction of a deep test well at the location of a future regional waste-water treatment plant to be built for the city of West Palm Beach, Florida. Data from the test well will be used by the city in the design of a proposed deep-well injection system for disposal of effluent from the treatment plant. Shallow wells in the vicinity of the drilling site were inventoried and sampled to provide a data base for detecting changes in ground water quality during construction and later operation of the deep wells. In addition, 16 small-diameter monitor wells, ranging in depth from 10 to 162 feet, were drilled at the test site. During the drilling of the deep test well, water samples were collected weekly from the 16 monitor wells for determination of chloride content and specific conductance. Evidence of small spills of salt water were found in monitor wells ranging in depth from 10 to 40 feet. Efforts to remove the salt water from the shallow unconfined aquifer by pumping were undertaken by the drilling contractor at the request of the city of West Palm Beach. The affected area is small and there has been a reduction of chloride concentration.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr7691","collaboration":"Prepared in cooperation with the City of West Palm Beach, Florida","usgsCitation":"Pitt, W.A., and Meyer, F.W., 1976, Ground-water quality at the site of a proposed deep-well injection system for treated wastewater, West Palm Beach, Florida: U.S. Geological Survey Open-File Report 76-91, 43 p., https://doi.org/10.3133/ofr7691.","productDescription":"43 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":1000,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0091/ofr7691.pdf","text":"Report","size":"1.50 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":148425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0091/coverthb.jpg"}],"country":"United States","state":"Florida","city":"West Palm Beach","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.13496398925781,\n 26.70513306062492\n ],\n [\n -80.09685516357422,\n 26.70513306062492\n ],\n [\n -80.09685516357422,\n 26.753581490264136\n ],\n [\n -80.13496398925781,\n 26.753581490264136\n ],\n [\n -80.13496398925781,\n 26.70513306062492\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a870","contributors":{"authors":[{"text":"Pitt, William A. J. Jr.","contributorId":19427,"corporation":false,"usgs":true,"family":"Pitt","given":"William","suffix":"Jr.","email":"","middleInitial":"A. J.","affiliations":[],"preferred":false,"id":171140,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Frederick W.","contributorId":39373,"corporation":false,"usgs":true,"family":"Meyer","given":"Frederick","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":171139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9844,"text":"ofr76651 - 1976 - Simulations of water-level drawdowns in proposed well-field areas, Dade County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T17:03:47.780638","indexId":"ofr76651","displayToPublicDate":"1976-01-01T22:10:00","publicationYear":"1976","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":"76-651","title":"Simulations of water-level drawdowns in proposed well-field areas, Dade County, Florida","docAbstract":"Electrical analog model simulations of hydraulic conditions in the Biscayne aquifer were made at proposed inland well-field sites in Dade County, Florida. Simulated drawdowns of water levels after 7 months of continuous pumping at 50, 100, and 150 million gallons per day were obtained at each site. Simultaneous pumping of each of the sites at 50 million gallons per day showed that after 7 months pumping there would be interference between proposed well fields. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr76651","collaboration":"Prepared in cooperation with the Miami-Dade Water and Sewer Authority","usgsCitation":"Klein, H., 1976, Simulations of water-level drawdowns in proposed well-field areas, Dade County, Florida: U.S. Geological Survey Open-File Report 76-651, iv, 14 p., https://doi.org/10.3133/ofr76651.","productDescription":"iv, 14 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":141890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0651/coverthb.jpg"},{"id":960,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0651/ofr76651.pdf","text":"Report","size":"600 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Florida","county":"Miami-Dade County","otherGeospatial":"Dade County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.53390502929688,\n 25.247180194609925\n ],\n [\n -80.13015747070312,\n 25.247180194609925\n ],\n [\n -80.13015747070312,\n 26.046912801683984\n ],\n [\n -80.53390502929688,\n 26.046912801683984\n ],\n [\n -80.53390502929688,\n 25.247180194609925\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1846","contributors":{"authors":[{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":160397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11039,"text":"ofr76713 - 1976 - Geologic data from test drilling in Palm Beach County, Florida since 1970","interactions":[],"lastModifiedDate":"2022-01-05T16:46:35.547986","indexId":"ofr76713","displayToPublicDate":"1976-01-01T22:10:00","publicationYear":"1976","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":"76-713","title":"Geologic data from test drilling in Palm Beach County, Florida since 1970","docAbstract":"Test hole data, in Palm Beach County, Florida, include lithologic logs from 66 test wells and geophysical logs from 54 test wells. The purpose of the study is to provide the geohydrologic information needed for water management and land use decisions, with emphasis on the urbanized eastern part of the county and the readily developable area in the central part. 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Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8e8","contributors":{"authors":[{"text":"Schneider, James J.","contributorId":22356,"corporation":false,"usgs":true,"family":"Schneider","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28673,"text":"wri7629 - 1976 - Nitrogen and phosphorus uptake in the Everglades Conservation Areas, Florida, with special reference to the effects of backpumping runoff","interactions":[],"lastModifiedDate":"2022-01-05T18:52:24.717791","indexId":"wri7629","displayToPublicDate":"1976-01-01T21:35:00","publicationYear":"1976","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":"76-29","title":"Nitrogen and phosphorus uptake in the Everglades Conservation Areas, Florida, with special reference to the effects of backpumping runoff","docAbstract":"In much of the water pumped into the northern Everglades, Florida, concentrations of inorganic nitrogen and phosphorus are relatively high. These nutrients are transported in the canals or into the peripheral marshes. Concentrations decrease sharply within 330 feet or less of the canals, whereas specific conductance remains essentially unchanged within this distance. The sharp decrease in inorganic nitrogen and phosphorus near the canal edge indicates net uptake in these shallow waters. Concentrations of nitrogen and phosphorus also decrease as water moves through the conservation areas in canals. This decrease is due partly to dilution by rainfall and runoff, and partly to net uptake in the canals and their peripheral marsh. The large canals of the northern and eastern parts of the conservation areas often have relatively low concentrations of dissolved oxygen which show little fluctuation within 24 hours. Backpumping 50 percent of the total annual canal runoff in southeast Florida would add from 990 to 6,160 tons of nitrogen and from 10 to 62 tons of phosphorus to the conservation areas. The bottom sediments of the Everglades are a sink for nitrogen and phosphorus. They can, however, be a source of these nutrients when anaerobic conditions exist at the water-sediment interface or when bottom material becomes resuspended. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7629","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"McPherson, B.F., Waller, B.G., and Mattraw, H., 1976, Nitrogen and phosphorus uptake in the Everglades Conservation Areas, Florida, with special reference to the effects of backpumping runoff: U.S. Geological Survey Water-Resources Investigations Report 76-29, 120 p., https://doi.org/10.3133/wri7629.","productDescription":"120 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2265,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0029/wri7629.pdf","text":"Report","size":"2.47 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":158277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0029/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.09832763671875,\n 26.966141794817037\n ],\n [\n -81.3372802734375,\n 26.88288045572338\n ],\n [\n -81.23291015625,\n 26.703906250401882\n ],\n [\n -81.05987548828125,\n 26.73089302213736\n ],\n [\n -80.99945068359375,\n 26.73334604773261\n ],\n [\n -80.88958740234375,\n 26.261399213411483\n ],\n [\n -80.88409423828125,\n 25.995081230575074\n ],\n [\n -80.91705322265625,\n 25.851808634972723\n ],\n [\n -81.13677978515625,\n 25.728158254981707\n ],\n [\n -80.9857177734375,\n 25.58456258101669\n ],\n [\n -80.90606689453124,\n 25.435833800555567\n ],\n [\n -80.76873779296875,\n 25.25711665985981\n ],\n [\n -80.47760009765624,\n 25.32664914186939\n ],\n [\n -80.35675048828125,\n 25.631621577258493\n ],\n [\n -80.244140625,\n 25.78258030688864\n ],\n [\n -80.145263671875,\n 26.340191416286576\n ],\n [\n -80.09307861328125,\n 26.659732285135714\n ],\n [\n -80.12603759765625,\n 26.895128623179364\n ],\n [\n -80.233154296875,\n 27.051787740992335\n ],\n [\n -80.27984619140625,\n 26.76768285044102\n ],\n [\n -80.72479248046875,\n 27.188685315271673\n ],\n [\n -80.6671142578125,\n 27.04200293656626\n ],\n [\n -80.64239501953125,\n 26.944108009688595\n ],\n [\n -80.70556640625,\n 26.82897275381776\n ],\n [\n -80.78521728515625,\n 26.775039386999605\n ],\n [\n -80.88409423828125,\n 26.78729922215609\n ],\n [\n -80.97198486328125,\n 26.944108009688595\n ],\n [\n -81.09832763671875,\n 26.966141794817037\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c02b","contributors":{"authors":[{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":200209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mattraw, H. C.","contributorId":45712,"corporation":false,"usgs":true,"family":"Mattraw","given":"H. C.","affiliations":[],"preferred":false,"id":200210,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26650,"text":"wri7693 - 1976 - Analog-model simulations for secondary canal controls and forward pumping water-management schemes in southeast Florida","interactions":[],"lastModifiedDate":"2022-01-05T18:40:15.387247","indexId":"wri7693","displayToPublicDate":"1976-01-01T21:35:00","publicationYear":"1976","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":"76-93","title":"Analog-model simulations for secondary canal controls and forward pumping water-management schemes in southeast Florida","docAbstract":"

The analog model of the Biscayne aquifer of southeast Florida was used to approximate the effects of two proposed water-management schemes. One involved adding a secondary control structure in a major canal which is controlled near the coast. In the model the controls were operated in accordance with canal water level both above and below the secondary control. Although the model could not differentiate between control openings of 1 foot or 5 feet, it showed that the secondary control is a viable method of conserving ground water.

The second scheme involved pumping ground water ('forward pumping') from the Biscayne aquifer in inland areas during the dry season to: (1) augment canal flows toward the coast to sustain ground-water levels there, and (2) generate additional ground-water storage space for recharge in the wet season. Several sites on the model were programmed for forward pumping wells and the storage change was noted as a percentage of the ground-water withdrawal. (Woodard-USGS)

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7693","collaboration":"Prepared in cooperation with Central and Southern Florida Flood Control District","usgsCitation":"Cordes, E.H., and Gardner, R.A., 1976, Analog-model simulations for secondary canal controls and forward pumping water-management schemes in southeast Florida: U.S. Geological Survey Water-Resources Investigations Report 76-93, v, 60 p., https://doi.org/10.3133/wri7693.","productDescription":"v, 60 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":158399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0093/coverthb.jpg"},{"id":2026,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0093/wri7693.pdf","text":"Report","size":"2.65 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Florida","county":"Miami-Dade County","otherGeospatial":"Dade County, Snake Creek Canal","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.44532775878906,\n 26.062334442780692\n ],\n [\n -80.44120788574219,\n 25.941374418200503\n ],\n [\n -80.18577575683594,\n 25.75784610230624\n ],\n [\n -80.18508911132812,\n 25.79123606041021\n ],\n [\n -80.17616271972656,\n 25.834505347339903\n ],\n [\n -80.167236328125,\n 25.86725585969518\n ],\n [\n -80.14595031738281,\n 25.89690887065143\n ],\n [\n -80.13153076171875,\n 25.903703303407667\n ],\n [\n -80.12947082519531,\n 25.922231585619894\n ],\n [\n -80.1177978515625,\n 25.98520595593358\n ],\n [\n -80.11093139648436,\n 26.069119321860896\n ],\n [\n -80.44532775878906,\n 26.062334442780692\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.44189453125,\n 25.940139490600565\n ],\n [\n -80.48789978027344,\n 25.891967219290756\n ],\n [\n -80.48515319824217,\n 25.774542255850353\n ],\n [\n -80.49888610839844,\n 25.761556561592343\n ],\n [\n -80.31692504882812,\n 25.765885284201275\n ],\n [\n -80.32241821289062,\n 25.852426562716428\n ],\n [\n -80.44189453125,\n 25.940139490600565\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.50094604492186,\n 25.762174960200042\n ],\n [\n -80.48721313476562,\n 25.773305584277654\n ],\n [\n -80.48789978027344,\n 25.835741380387113\n ],\n [\n -80.6781005859375,\n 25.83512336547731\n ],\n [\n -80.67741394042969,\n 25.762793355586627\n ],\n [\n -80.50094604492186,\n 25.762174960200042\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.66505432128905,\n 25.83697740052369\n ],\n [\n -80.54145812988281,\n 25.9469314321602\n ],\n [\n -80.60600280761719,\n 26.00310428015198\n ],\n [\n -80.72616577148438,\n 25.890731774122894\n ],\n [\n -80.66505432128905,\n 25.83697740052369\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.53871154785156,\n 25.935817142040126\n ],\n [\n -80.4473876953125,\n 25.935817142040126\n ],\n [\n -80.4473876953125,\n 26.028404154179178\n ],\n [\n -80.53871154785156,\n 26.028404154179178\n ],\n [\n -80.53871154785156,\n 25.935817142040126\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68391f","contributors":{"authors":[{"text":"Cordes, E. H.","contributorId":49002,"corporation":false,"usgs":true,"family":"Cordes","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, Richard Alfred","contributorId":89134,"corporation":false,"usgs":true,"family":"Gardner","given":"Richard","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":196773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30333,"text":"wri7628 - 1976 - Analysis of selected benthic communities in Florida Everglades with reference to their physical and chemical environment","interactions":[],"lastModifiedDate":"2022-01-05T17:26:08.043665","indexId":"wri7628","displayToPublicDate":"1976-01-01T21:20:00","publicationYear":"1976","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":"76-28","title":"Analysis of selected benthic communities in Florida Everglades with reference to their physical and chemical environment","docAbstract":"

Species diversity and numbers of benthic macroinvertebrates were determined at 12 sites, both canals and marshes, in the Everglades of south Florida. The values calculated are used to indicate long-term trends in water quality and variations between study areas.

Species diversity at all sites was generally in a range indicative of degraded water quality. The number of organisms per square metre of bottom surface was highly variable ranging from 43 to 8,200 organisms.

Chemical analysis of water and bottom material indicated no gross contamination from sewage or agricultural runoff in any of the canals where benthic organisms were collected. Other physical factors such as depth, velocity of flow, substrate type, and water-level fluctuation were responsible for the low species diversities and variable numbers of organisms, rather than contamination from urban or agricultural areas.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7628","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers Jacksonville District","usgsCitation":"Waller, B.G., 1976, Analysis of selected benthic communities in Florida Everglades with reference to their physical and chemical environment: U.S. Geological Survey Water-Resources Investigations Report 76-28, 33 p., https://doi.org/10.3133/wri7628.","productDescription":"33 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2468,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0028/wri7628.pdf","text":"Report","size":"840 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":159291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0028/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.2054443359375,\n 25.070672916651077\n ],\n [\n -79.9639892578125,\n 25.070672916651077\n ],\n [\n -79.9639892578125,\n 26.956349533411863\n ],\n [\n -81.2054443359375,\n 26.956349533411863\n ],\n [\n -81.2054443359375,\n 25.070672916651077\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680f20","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32540,"text":"32540 - 1976 - National Atlas, Middle Atlantic states","interactions":[],"lastModifiedDate":"2017-03-29T11:26:35","indexId":"32540","displayToPublicDate":"1976-01-01T16:42:41","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"National Atlas, Middle Atlantic states","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/32540","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, National Atlas, Middle Atlantic states (Rev. 1972.), 1 map, https://doi.org/10.3133/32540.","productDescription":"1 map","costCenters":[],"links":[{"id":291551,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.55,31.97 ], [ -84.55,42.95 ], [ -69.59,42.95 ], [ -69.59,31.97 ], [ -84.55,31.97 ] ] ] } } ] }","edition":"Rev. 1972.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9c6e4b076157863773a","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":529407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32541,"text":"32541 - 1976 - National Atlas, Southern Mississippi Valley states","interactions":[],"lastModifiedDate":"2017-03-29T11:27:06","indexId":"32541","displayToPublicDate":"1976-01-01T16:26:31","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"National Atlas, Southern Mississippi Valley states","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/32541","isbn":"0607542403","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, National Atlas, Southern Mississippi Valley states (Rev. 1972.), 1 map, https://doi.org/10.3133/32541.","productDescription":"1 map","costCenters":[],"links":[{"id":291549,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Mississippi","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.65,30.17 ], [ -91.65,35.0 ], [ -88.1,35.0 ], [ -88.1,30.17 ], [ -91.65,30.17 ] ] ] } } ] }","edition":"Rev. 1972.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9c7e4b076157863773e","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":529408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168649,"text":"70168649 - 1976 - Water resources data for Iowa, water year 1975","interactions":[],"lastModifiedDate":"2016-02-22T15:07:13","indexId":"70168649","displayToPublicDate":"1976-01-01T16:15:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Iowa, water year 1975","docAbstract":"

No abstract available.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56cc402de4b059daa47e4833","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128037,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":621152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70199342,"text":"70199342 - 1976 - Lakes of Oregon, Volume 4: Clackamas County","interactions":[],"lastModifiedDate":"2018-09-21T14:39:26","indexId":"70199342","displayToPublicDate":"1976-01-01T15:39:11","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Lakes of Oregon, Volume 4: Clackamas County","docAbstract":"

An inventory of lakes and reservoirs of Oregon is essential for a complete evaluation of the total surface-water supply of the State and to provide a basis for answering questions about Oregon's lakes. Much of the information on lakes and reservoirs previously collected by Federal and State agencies has never been published. Those data were compiled and used as a basis for collecting additional information. This report provides information for use by city, county, and State planning groups as well as for sportsmen, tourists, and others interested in preserving the recreational value of Oregon's lakes.

Because of the large number of lakes and reservoirs in Oregon, a single report covering the State would be bulky. Therefore, the lake information is being issued in several volumes on a county or multicounty basis. Volume 1, released in 1973, covered Clatsop, Columbia, and Tillamook Counties; volume 2 (1974 included Benton, Lincoln, and Polk Counties; and volume 3 (1975) included Hood River, Multnomah, Washington, and Yamhill Counties. Clackamas County was selected for volume 4. (See figure 1.)

In addition to office compilation of existing data, each lake was visited. Most visits were made in summer or early fall when lakes were most accessible and when water temperature and biological activity were near maximum.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70199342","collaboration":"Prepared in cooperation with the Oregon State Water Resources Department","usgsCitation":"Shulters, M., 1976, Lakes of Oregon, Volume 4: Clackamas County: Open-File Report, iii, 76 p., https://doi.org/10.3133/70199342.","productDescription":"iii, 76 p.","costCenters":[],"links":[{"id":357633,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70199342/report-thumb.jpg"},{"id":357634,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70199342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Clackamas County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.75,\n 44.75\n ],\n [\n -121.75,\n 44.75\n ],\n [\n -121.75,\n 45.471688258104614\n ],\n [\n -122.75,\n 45.471688258104614\n ],\n [\n -122.75,\n 44.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shulters, M.V.","contributorId":54583,"corporation":false,"usgs":true,"family":"Shulters","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":746023,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70121413,"text":"70121413 - 1976 - Coral reef recovery in Florida and the Persian Gulf","interactions":[],"lastModifiedDate":"2023-10-25T15:22:32.22494","indexId":"70121413","displayToPublicDate":"1976-01-01T15:37:40","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Coral reef recovery in Florida and the Persian Gulf","docAbstract":"

Long-term observations and study of coral reef destruction by hurricanes in the Florida Keys show, surprisingly, that although corals are devastated on a grand scale during storms, recovery is rapid. Recovery occurs because of the widespread scattering of live fragments, many of which become growth sites of new colonies. Reef recovery from death by chilling in the Persian Gulf was well under way when last observed, but it is not yet known if the recovery rate was as rapid as recovery from the storm destruction in Florida. Recovery from death by chilling requires settlement of transported coral larvae and a substrate suitable for larval attachment. Such resettlement is subject to the effects of currents, predators, pollution, and competition for substrate.

A growth rate of 10 cm per year combined with geometrical progression of branch formation accounts for rapid Acropora cervicornis recovery. Although calculated coral proliferation seems unusually high, it has been confirmed by serial underwater photographs spanning ten years. More precise measurements of growth and branching are needed, along with growth data for other common reef-building corals. Such data would be useful for predicting standing crop of a restocked or transplanted reef.

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