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Glacial drift and Cretaceous sedimentary rocks are the major aquifers in the Yellow Medicine River watershed unit.

\n

The Yellow Medicine and Minnesota Rivers are the major sources of surface water. For physiographic regions – Upland Plain, Slope, Lowland Plain, and Minnesota River Flood Plain – influence surface drainage, and the flow of ground water through the aquifers. The watershed comprises 1070 square miles, including the drainage basin of the Yellow Medicine River (665 square miles) and 405 square miles drained by small streams tributary to the Minnesota River.

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The Otter Tail River watershed includes three general physiographic areas- a moraine and ice-contact area, an outwash plain, and the plain of Glacial Lake Agassiz.

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The moraine and ice-contact area is a fairly rugged complex of hills characterized by local relief of several hundred feet in some areas, particularly in the extreme north and southeastern parts of the watershed. The outwash plain is fairly flat to rolling and the Glacial Lake Agassiz plain is extremely flat.

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The watershed has an area of about 1,920 square miles and includes parts of Becker, Otter Tail, Wilkin, and Clearwater Counties. The population of the area is about 55,500; 32,600 urban and 22,900 rural. The economy is largely agricultural. Grain farming is dominant, but dairying is important.

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The extremely large number of lakes in the area provides a basis for a large recreation-based economy.

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1282","usgsCitation":"Olive, W.W., and Finch, W.I., 1969, Stratigraphic and mineralogic relations and ceramic properties of clay deposits of Eocene age in the Jackson Purchase region, Kentucky, and in adjacent parts of Tennessee: U.S. Geological Survey Bulletin 1282, iv, 35 p., https://doi.org/10.3133/b1282.","productDescription":"iv, 35 p.","costCenters":[],"links":[{"id":411153,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21380.htm","linkFileType":{"id":5,"text":"html"}},{"id":63268,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1282/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165328,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1282/report-thumb.jpg"}],"country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Jackson Purchase region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -89.532,\n 37.216\n ],\n [\n -89.532,\n 36.5\n ],\n [\n -88.042,\n 36.5\n ],\n [\n -88.042,\n 37.216\n ],\n [\n -89.532,\n 37.216\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10ad","contributors":{"authors":[{"text":"Olive, Wilds W.","contributorId":51302,"corporation":false,"usgs":true,"family":"Olive","given":"Wilds","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":214560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finch, Warren Irvin","contributorId":55794,"corporation":false,"usgs":true,"family":"Finch","given":"Warren","email":"","middleInitial":"Irvin","affiliations":[],"preferred":false,"id":214561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1690,"text":"wsp1898A - 1969 - Stage-discharge characteristics of a Weir in a sand-channel stream","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1898A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1898","chapter":"A","title":"Stage-discharge characteristics of a Weir in a sand-channel stream","docAbstract":"A unique relation between water-surface elevation and water discharge usually does not exist for sand-channel streams. The relation is affected by changes in bed roughness and changes in bed elevation because of scour and fill. An artificial control on a sand-channel stream must control both the resistance to flow and the bed elevation in order to stabilize the relation between water-surface elevation and water discharge. \r\n\r\nThe weir (control structure) in the Rio Grande conveyance channel near Bernardo, N. Mex., was designed on the basis of a model study and field data (Harris and Richardson, 1964). About 72 percent of the measurements used to define the base relation between water-surface elevation and water discharge falls within plus or minus 5 percent of the mean relation for the prototype. The stage-discharge relation is not affected by backwater for values of submergence less than 90 percent. There is no consistent relation between the ratio of measured discharge to rated discharge and submergence for values of submergence greater than 90 percent. \r\n\r\nThe control does not restrict the channel capacity to less than the stated design capacity of 2,000 cubic feet per second. When the control is drowned out, or ineffective, the relation of water-surface elevation to water discharge is virtually the same as that prior to construction of the control for discharges greater than 1,500 cubic feet per second. When the control is not drowned out--that is, free-fall conditions exist--the water-surface elevation for a discharge of 2,000 cubic feet per second is greater than the minimum elevation, but is less than the maximum elevation that occurred at that discharge prior to construction. \r\n\r\nThe model study was only partially successful in predicting the operating characteristics of the prototype. Some of the differences between prototype operation and model predictions may exist because the prototype was not built exactly as recommended on the basis of the model study. In general, the prototype has operated somewhat better than the model predicted.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1898A","usgsCitation":"Gonzalez, D.D., Scott, C., and Culbertson, J.K., 1969, Stage-discharge characteristics of a Weir in a sand-channel stream: U.S. Geological Survey Water Supply Paper 1898, iii, 29 p., https://doi.org/10.3133/wsp1898A.","productDescription":"iii, 29 p.","costCenters":[],"links":[{"id":137040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1898a/report-thumb.jpg"},{"id":26775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1898a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a1b7","contributors":{"authors":[{"text":"Gonzalez, Don D.","contributorId":49774,"corporation":false,"usgs":true,"family":"Gonzalez","given":"Don","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":143978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":143979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Culbertson, James K.","contributorId":31371,"corporation":false,"usgs":true,"family":"Culbertson","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":143977,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2072,"text":"wsp1879B - 1969 - Water resources of Randolph and Lawrence Counties, Arkansas","interactions":[{"subject":{"id":52603,"text":"ofr67143 - 1967 - Well records and depth-to-water measurements in the vicinity of Randolph and Lawrence Counties, Arkansas","indexId":"ofr67143","publicationYear":"1967","noYear":false,"title":"Well records and depth-to-water measurements in the vicinity of Randolph and Lawrence Counties, Arkansas"},"predicate":"SUPERSEDED_BY","object":{"id":2072,"text":"wsp1879B - 1969 - Water resources of Randolph and Lawrence Counties, Arkansas","indexId":"wsp1879B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Water resources of Randolph and Lawrence Counties, Arkansas"},"id":1},{"subject":{"id":55853,"text":"ofr68164 - 1968 - Water resources of Randolph and Lawrence Counties, Arkansas","indexId":"ofr68164","publicationYear":"1968","noYear":false,"title":"Water resources of Randolph and Lawrence Counties, Arkansas"},"predicate":"SUPERSEDED_BY","object":{"id":2072,"text":"wsp1879B - 1969 - Water resources of Randolph and Lawrence Counties, Arkansas","indexId":"wsp1879B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Water resources of Randolph and Lawrence Counties, Arkansas"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1879B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1879","chapter":"B","title":"Water resources of Randolph and Lawrence Counties, Arkansas","docAbstract":"Water is used at an average rate of almost 27 million gallons per day in Randolph and Lawrence Counties, and quantities sufficient for any foreseeable use are available. Supplies for the large uses--municipal, industrial, and irrigation--can best be obtained from wells in .he Coastal Plain part of the counties and from streams in the Interior Highlands part. \r\n\r\nThe counties have abundant supplies of hard but otherwise good-quality surface water, particularly in the Interior Highlands and along the western boundary of the Coastal Plain. Minimum recorded flows of four streams (Black, Current, Eleven Point, and Spring Rivers) exceeded 200 cubic feet per second, or 129 million gallons per day. Five other streams have flows in excess of 13 cubic feet per second 95 percent of the time. Water supplies can be obtained without storage from the larger streams in the area. Many of the smaller streams in the Interior Highlands also have large water-supply potential because of the excellent impoundment possibilities. \r\n\r\nMost of the water used in the .two counties is obtained from ground-water reservoirs in the Coastal Plain. Wells that tap alluvial deposits of Quaternary age commonly yield 1,000 gallons per minute. However, the water often is unsuitable for many uses unless treated to remove hardness, iron, and manganese. Water possibly may be obtained in the southeastern part of the area from the Wilcox Group of Tertiary age and the Nacatoch Sand of Cretaceous age, but these formations have not been explored in the report area. \r\n\r\nWells in the Interior Highlands generally are less than 200 feet deep and yield 10 gallons per minute, or less. It may be possible to obtain greater amounts of ground water from two unexplored formations, the Roubidox and the Gunter Sandstone Member of the Van Buren Formation, in the Interior Highlands. Ground water in the Interior Highlands is very hard and is more susceptible to local bacterial contamination than is ground water in the Coastal Plain. However, with proper sanitary safeguards against contamination and with treatment for reduction of hardness, ground water in the Interior Highlands is suitable for most uses.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1879B","usgsCitation":"Lamonds, A.G., Hines, M.S., and Plebuch, R.O., 1969, Water resources of Randolph and Lawrence Counties, Arkansas: U.S. Geological Survey Water Supply Paper 1879, iv, 45 p., https://doi.org/10.3133/wsp1879B.","productDescription":"iv, 45 p.","costCenters":[],"links":[{"id":138567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1879b/report-thumb.jpg"},{"id":27625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1879b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0292","contributors":{"authors":[{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, Marion S.","contributorId":29388,"corporation":false,"usgs":true,"family":"Hines","given":"Marion","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":144640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plebuch, Raymond O.","contributorId":15177,"corporation":false,"usgs":true,"family":"Plebuch","given":"Raymond","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144639,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":16614,"text":"ofr69323 - 1969 - Paleogene floras from the Gulf of Alaska","interactions":[{"subject":{"id":16614,"text":"ofr69323 - 1969 - Paleogene floras from the Gulf of Alaska","indexId":"ofr69323","publicationYear":"1969","noYear":false,"title":"Paleogene floras from the Gulf of Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":6514,"text":"pp997 - 1977 - Paleogene floras from the Gulf of Alaska region","indexId":"pp997","publicationYear":"1977","noYear":false,"title":"Paleogene floras from the Gulf of Alaska region"},"id":1}],"supersededBy":{"id":6514,"text":"pp997 - 1977 - Paleogene floras from the Gulf of Alaska region","indexId":"pp997","publicationYear":"1977","noYear":false,"title":"Paleogene floras from the Gulf of Alaska region"},"lastModifiedDate":"2023-12-27T23:03:10.110922","indexId":"ofr69323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-323","title":"Paleogene floras from the Gulf of Alaska","docAbstract":"

Numerous collections of fossil plants from the Gulf of Alaska region were obtained from rocks that are well dated by marine mollusks. The mollusks indicate that the oldest possible age for the lowest plant assemblage is middle Eocene (Domengine) and that the youngest possible age for the highest Paleogene plant assemblage is middle Oligocene (Lincoln).

Paleobotanical correlations indicate that the lowest plant assemblage is of early late Eocene (early Ravenian) age and the highest plant assemblage is of early Oligocene (Kummerian) age. A new provincial stage--the Angoonian--is proposed, based on assemblages from rocks in southeastern Alaska. The Angoonian is thought to be of late Oligocene (early Blakeley) age. Only one stratigraphically isolated assemblage from the Gulf of Alaska region has been recognized as of Angoonian age. The biostratigraphy of the Gulf of Alaska region and of other regions in Alaska indicates that the Seldovian, Homerian, and Clamgulchian Stages are probably entirely of Neogene age.

The early Ravenian assemblages represent Paratropical Rain forest (that is, similar to vegetation of a narrow region bordering the Tropical Rain forest) based on the physiognomic analysis of foliage; the most diverse families represented are Menispermaceae and Icacinaceae. These are accompanied by palms, Anonaceae, tjristicaceae, Dipterocarpaceae, Barringtoniaceae, and Myrtaceae. A minor element is represented by broad-leaved deciduous plants. The middle Ravenian was somewhat cooler, as indicated by foliar physiognomy, the fewer Tropical Rain forest elements, and the diversity of Lauraceae. The late Ravenian assemblage represents a broad-leaved deciduous forest indicating a temperate climate. The Kummerian assemblages were again dominated by Lauraceae, and the physiognomic characters of the foliage indicate that Subtropical forest was again represented.

The existence of a broad-leaved evergreen forest in Alaska such as that of the early Ravenian indicates that extended periods of darkness could probably not have existed at that time. The Alaskan Paleogene floras, as well as those from other regions, indicate that the earth's axis of rotation may not have had as great an inclination in the past. Strong climatic fluctuations evidenced by foliar physiognomy of Tertiary floras is thought to have been the result of changes in the inclination of the earth's axis.

The history of the development of the Arcto-Tertiary concept is reviewed, and the fundamental lack of evidence for this concept is shown. An alternative, more complex, concept is proposed for the development of the Mixed Mesophytic forest. Paleobotanical evidence indicates that tolerances of many genera have changed during the Tertiary. Many Mixed Mesophytic genera--particularly those that are today temperate outliers of basically tropical groups--may have had a wide distribution in the Paleogene Paratropical Rain and Subtropical forests and have entered the warm temperate forests only during the later Paleogene or Neogene. Some Mixed Mesophytic groups appear to be of later Neogene origin and have been significant members of the warm temperate forests since that time. Some Mixed Mesophytic genera apparently were members of the Paratropical Rain forest only in the earliest Paleogene and became adapted to warm temperate climates by the late Eocene or perhaps even earlier. The Mixed Mesophytic forest may have developed independently in Eurasia, western North America, and eastern North America.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69323","usgsCitation":"Wolfe, J.A., 1969, Paleogene floras from the Gulf of Alaska: U.S. Geological Survey Open-File Report 69-323, ii, 111 p., https://doi.org/10.3133/ofr69323.","productDescription":"ii, 111 p.","costCenters":[],"links":[{"id":423920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0323/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0323/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -136.15250770661777,\n 56.82863558130717\n ],\n [\n -136.15250770661777,\n 60.5418529177804\n ],\n [\n -157.32762172640042,\n 60.5418529177804\n ],\n [\n -157.32762172640042,\n 56.82863558130717\n ],\n [\n -136.15250770661777,\n 56.82863558130717\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ce0","contributors":{"authors":[{"text":"Wolfe, Jack A.","contributorId":102474,"corporation":false,"usgs":true,"family":"Wolfe","given":"Jack","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":173153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2904,"text":"wsp1873A - 1969 - Factors initiating phytoplankton blooms and resulting effects on dissolved oxygen in Duwamish River estuary, Seattle, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp1873A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1873","chapter":"A","title":"Factors initiating phytoplankton blooms and resulting effects on dissolved oxygen in Duwamish River estuary, Seattle, Washington","docAbstract":"Phytoplankton productivity, standing stock, and related environmental factors were studied during 1964-66 in the Duwamish River estuary, at Seattle, Wash., to ascertain the factors that affect phytoplankton growth in the estuary; a knowledge of these factors in turn permits the detection and evaluation of the influence that effluent nutrients have on phytoplankton production. The factors that control the concentration of dissolved oxygen were also evaluated because of the importance of dissolved oxygen to the salmonid populations that migrate through the estuary. \r\n\r\nPhytoplankton blooms, primarily of diatoms, occurred in the lower estuary during August 1965 and 1966. No bloom occurred during 1964, but the presence of oxygen-supersaturated surface water in August 1963 indicates that a bloom did occur then. \r\n\r\nNutrients probably were not the primary factor controlling the timing of phytoplankton blooms. Ammonia ,and phosphate concentrations increased significantly downstream from the Municipality of Metropolitan Seattle's Renton Treatment Plant outfall after the plant began operation in June 1965, and concentrations of nitrogen and phosphorus were relatively high before operation of the Renton Treatment Plant and during nonbloom periods. The consistent coincidence of blooms with minimum fresh-water discharge and tidal exchange during August throughout the study period indicates that bloom timing probably was controlled mostly by hydrographic factors that determine retention time and stability of the surface-water layer. This control was demonstrated in part by a highly significant correlation of gross productivity with retention time (as indicated by fresh-water discharge) and vertical stability (as indicated by the difference between mean surface and mean bottom temperatures). The failure of a bloom to develop in 1964 is related to a minimum fresh-water discharge that was much greater than normal during that summer. Hydrographic factors are apparently important because, as shown by studies of other estuarine environments by other workers, phytoplankton production increases when the zone of vertical turbulent mixing is not markedly deeper than the compensation depth. \r\n\r\nPhytoplankton cells produced in the surface waters sink, thereby contributing oxidizable organic matter to the bottom saline-water wedge. The maximum BOD (biochemical oxygen demand) in this bottom wedge occurs in the same section of the estuary and ,at the same time as the maximum phytoplankton biomass (as indicated by chlorophyll a) and minimum DO (dissolved oxygen). Other sources of BOD occur in the estuary, and conditions of minimum discharge and tidal exchange assist in reducing DO. Nonetheless, the highly significant correlation of chlorophyll a with BOD throughout the summer indicates that respiration and decomposition of phytoplankton cells is dearly an important contributor of BOD. \r\n\r\nIncreases in the biomass and resultant B0D of blooms because of increased effluent nutrients presumably would further decrease the concentration of DO. This possible effect of effluent nutrients was evaluated by laboratory .bioassays and by a comparison of mean annual biomasses in the estuary. A green algal population in vitro did increase in response to added effluent nutrients; however, the available field data suggest that a 46-percent increase in effluent discharge between 1965 and 1966 did not increase the estuary's phytoplankton biomass significantly.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1873A","usgsCitation":"Welch, E.B., 1969, Factors initiating phytoplankton blooms and resulting effects on dissolved oxygen in Duwamish River estuary, Seattle, Washington: U.S. Geological Survey Water Supply Paper 1873, v, 62 p. :ill. map ;24 cm., https://doi.org/10.3133/wsp1873A.","productDescription":"v, 62 p. :ill. map ;24 cm.","costCenters":[],"links":[{"id":138393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873a/report-thumb.jpg"},{"id":29584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64964b","contributors":{"authors":[{"text":"Welch, Eugene Brummer","contributorId":48947,"corporation":false,"usgs":true,"family":"Welch","given":"Eugene","email":"","middleInitial":"Brummer","affiliations":[],"preferred":false,"id":145985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63453,"text":"gq821 - 1969 - Geologic map of the Buffalo Mountain quadrangle, Pershing and Churchill Counties, Nevada","interactions":[],"lastModifiedDate":"2018-06-19T17:06:05","indexId":"gq821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"821","title":"Geologic map of the Buffalo Mountain quadrangle, Pershing and Churchill Counties, Nevada","language":"ENGLISH","doi":"10.3133/gq821","usgsCitation":"Wallace, R.E., Silberling, N., Irwin, W., and Tatlock, D., 1969, Geologic map of the Buffalo Mountain quadrangle, Pershing and Churchill Counties, Nevada: U.S. Geological Survey Geologic Quadrangle 821, Map: 76.8 x 67.8 cm, https://doi.org/10.3133/gq821.","productDescription":"Map: 76.8 x 67.8 cm","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":249544,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0821/report.pdf","size":"30","linkFileType":{"id":1,"text":"pdf"}},{"id":103537,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2123.htm","linkFileType":{"id":5,"text":"html"},"description":"2123"},{"id":253109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0821/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.25,40 ], [ -118.25,40.25 ], [ -118,40.25 ], [ -118,40 ], [ -118.25,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d71c","contributors":{"authors":[{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":268878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silberling, N. J.","contributorId":34919,"corporation":false,"usgs":true,"family":"Silberling","given":"N. J.","affiliations":[],"preferred":false,"id":738410,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738411,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tatlock, D.B.","contributorId":22748,"corporation":false,"usgs":true,"family":"Tatlock","given":"D.B.","affiliations":[],"preferred":false,"id":738412,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":63151,"text":"gq835 - 1969 - Geologic map of the Mellen Hill quadrangle, Rio Blanco and Moffat Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq835","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"835","title":"Geologic map of the Mellen Hill quadrangle, Rio Blanco and Moffat Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq835","usgsCitation":"Cullins, H.L., 1969, Geologic map of the Mellen Hill quadrangle, Rio Blanco and Moffat Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 835, 1 map :col. ;58 x 44 cm., on sheet 84 x 101 cm., folded to 28 x 21 cm., in envelope 30 x 24 cm., https://doi.org/10.3133/gq835.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 84 x 101 cm., folded to 28 x 21 cm., in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103551,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2137.htm","linkFileType":{"id":5,"text":"html"},"description":"2137"},{"id":180392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89041,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gq/0835/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109,40.1175 ], [ -109,40.25 ], [ -108.86749999999999,40.25 ], [ -108.86749999999999,40.1175 ], [ -109,40.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a3f","contributors":{"authors":[{"text":"Cullins, Henry L.","contributorId":23149,"corporation":false,"usgs":true,"family":"Cullins","given":"Henry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":268411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67381,"text":"i578 - 1969 - Geologic map of the Wheeler Peak and Garrison quadrangles, Nevada and Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i578","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"578","subseriesTitle":"NONE","title":"Geologic map of the Wheeler Peak and Garrison quadrangles, Nevada and Utah","language":"ENGLISH","doi":"10.3133/i578","usgsCitation":"Whitebread, D., 1969, Geologic map of the Wheeler Peak and Garrison quadrangles, Nevada and Utah: U.S. Geological Survey IMAP 578, 1 map :col. ;58 x 90 cm. on sheet 91 x 124 cm., https://doi.org/10.3133/i578.","productDescription":"1 map :col. ;58 x 90 cm. on sheet 91 x 124 cm.","costCenters":[],"links":[{"id":106847,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9363.htm","linkFileType":{"id":5,"text":"html"},"description":"9363"},{"id":188112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.5,38.75 ], [ -114.5,39 ], [ -114,39 ], [ -114,38.75 ], [ -114.5,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a07b","contributors":{"authors":[{"text":"Whitebread, D. H.","contributorId":96251,"corporation":false,"usgs":true,"family":"Whitebread","given":"D. H.","affiliations":[],"preferred":false,"id":276095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63838,"text":"gp691 - 1969 - Aeromagnetic map of the Plains, Perma, Superior, and Tarkio quadrangles, Sanders, Mineral, and Missoula Counties, Montana","interactions":[],"lastModifiedDate":"2025-06-23T17:19:25.223424","indexId":"gp691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"691","title":"Aeromagnetic map of the Plains, Perma, Superior, and Tarkio quadrangles, Sanders, Mineral, and Missoula Counties, Montana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp691","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Plains, Perma, Superior, and Tarkio quadrangles, Sanders, Mineral, and Missoula Counties, Montana: U.S. Geological Survey Geophysical Investigations Map 691, 1 Plate: 30.69 x 39.96 inches, https://doi.org/10.3133/gp691.","productDescription":"1 Plate: 30.69 x 39.96 inches","costCenters":[],"links":[{"id":250091,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0691/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253611,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0691/report-thumb.jpg"},{"id":250090,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0691/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491119,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6057.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"Montana","county":"Mineral County, Missoula County, Sanders County","otherGeospatial":"Plains, Perma, Superior, and Tarkio quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115,\n 47.5\n ],\n [\n -115,\n 47\n ],\n [\n -114.5,\n 47\n ],\n [\n -114.5,\n 47.5\n ],\n [\n -115,\n 47.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691ada","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":533307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63885,"text":"gp660 - 1969 - Aeromagnetic map of the Mt. Toby quadrangle and part of the Greenfield quadrangle, Franklin and Hampshire Counties, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-20T17:50:43.109735","indexId":"gp660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"660","title":"Aeromagnetic map of the Mt. Toby quadrangle and part of the Greenfield quadrangle, Franklin and Hampshire Counties, Massachusetts","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp660","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Mt. Toby quadrangle and part of the Greenfield quadrangle, Franklin and Hampshire Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 660, 1 Plate: 21.32 x 33.91 inches, https://doi.org/10.3133/gp660.","productDescription":"1 Plate: 21.32 x 33.91 inches","costCenters":[],"links":[{"id":250177,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0660/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250176,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0660/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491048,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6027.htm","linkFileType":{"id":5,"text":"html"}},{"id":253654,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0660/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Franklin County, Hampshire County","otherGeospatial":"Mt. Toby quadrangle and part of the Greenfield quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.5,\n 42.375\n ],\n [\n -72.5,\n 42.5\n ],\n [\n -72.625,\n 42.5\n ],\n [\n -72.625,\n 42.375\n ],\n [\n -72.5,\n 42.375\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cd9","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":533354,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63884,"text":"gp662 - 1969 - Aeromagnetic map of the Mt. Holyoke quadrangle, Hampshire and Hampden Counties, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-20T18:47:29.059536","indexId":"gp662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"662","title":"Aeromagnetic map of the Mt. Holyoke quadrangle, Hampshire and Hampden Counties, Massachusetts","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp662","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Mt. Holyoke quadrangle, Hampshire and Hampden Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 662, 1 Plate: 22.49 x 33.78 inches, https://doi.org/10.3133/gp662.","productDescription":"1 Plate: 22.49 x 33.78 inches","costCenters":[],"links":[{"id":253653,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0662/report-thumb.jpg"},{"id":250175,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0662/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250174,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491053,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6029.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Hampden County, Hampshire County","otherGeospatial":"Mt. Holyoke quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.5,\n 42.25\n ],\n [\n -72.5,\n 42.375\n ],\n [\n -72.625,\n 42.375\n ],\n [\n -72.625,\n 42.25\n ],\n [\n -72.5,\n 42.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d22","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":533353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42213,"text":"ofr69155 - 1969 - A preliminary geologic map of the Rochford district, Black Hills, South Dakota","interactions":[{"subject":{"id":42213,"text":"ofr69155 - 1969 - A preliminary geologic map of the Rochford district, Black Hills, South Dakota","indexId":"ofr69155","publicationYear":"1969","noYear":false,"title":"A preliminary geologic map of the Rochford district, Black Hills, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":33741,"text":"b1332A - 1972 - A preliminary report on the geology and gold deposits of the Rochford District, Black Hills, South Dakota","indexId":"b1332A","publicationYear":"1972","noYear":false,"chapter":"A","title":"A preliminary report on the geology and gold deposits of the Rochford District, Black Hills, South Dakota"},"id":1}],"supersededBy":{"id":33741,"text":"b1332A - 1972 - A preliminary report on the geology and gold deposits of the Rochford District, Black Hills, South Dakota","indexId":"b1332A","publicationYear":"1972","noYear":false,"title":"A preliminary report on the geology and gold deposits of the Rochford District, Black Hills, South Dakota"},"lastModifiedDate":"2022-05-11T19:33:07.245305","indexId":"ofr69155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-155","title":"A preliminary geologic map of the Rochford district, Black Hills, South Dakota","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69155","usgsCitation":"McGehee, R.V., and Bayley, R.W., 1969, A preliminary geologic map of the Rochford district, Black Hills, South Dakota: U.S. Geological Survey Open-File Report 69-155, 2 Plates: 24.29 x 31.25 inches and 23.96 x 29.90 inches, https://doi.org/10.3133/ofr69155.","productDescription":"2 Plates: 24.29 x 31.25 inches and 23.96 x 29.90 inches","costCenters":[],"links":[{"id":400548,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0155/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400547,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0155/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0155/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"South Dakota","otherGeospatial":"Rochford district, Black Hills","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.72261047363281,\n 44.12246875782058\n ],\n [\n -103.71437072753906,\n 44.12246875782058\n ],\n [\n -103.71437072753906,\n 44.127890527477824\n ],\n [\n -103.72261047363281,\n 44.127890527477824\n ],\n [\n -103.72261047363281,\n 44.12246875782058\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aadb5","contributors":{"authors":[{"text":"McGehee, R. V.","contributorId":73260,"corporation":false,"usgs":true,"family":"McGehee","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":226098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayley, R. W.","contributorId":74438,"corporation":false,"usgs":true,"family":"Bayley","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":226099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63928,"text":"gp687 - 1969 - Aeromagnetic map of the Hubbart Reservoir-Hot Springs area, Sanders, Flathead, and Lake Counties, Montana","interactions":[],"lastModifiedDate":"2025-06-23T17:01:37.140882","indexId":"gp687","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"687","title":"Aeromagnetic map of the Hubbart Reservoir-Hot Springs area, Sanders, Flathead, and Lake Counties, Montana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp687","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Hubbart Reservoir-Hot Springs area, Sanders, Flathead, and Lake Counties, Montana: U.S. Geological Survey Geophysical Investigations Map 687, 1 Plate: 30.06 x 39.17 inches, https://doi.org/10.3133/gp687.","productDescription":"1 Plate: 30.06 x 39.17 inches","costCenters":[],"links":[{"id":491114,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6053.htm","linkFileType":{"id":5,"text":"html"}},{"id":250262,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0687/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250261,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0687/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253779,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0687/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Montana","county":"Flathead County, Lake County, Sanders County","otherGeospatial":"Hubbart Reservoir-Hot Springs area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115,\n 48\n ],\n [\n -115,\n 47.5\n ],\n [\n -114.5,\n 47.5\n ],\n [\n -114.5,\n 48\n ],\n [\n -115,\n 48\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db6921a1","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":533397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64879,"text":"i599 - 1969 - (RLC-14) Geologic map of the Alphonsus region of the moon","interactions":[],"lastModifiedDate":"2023-03-29T15:43:54.960798","indexId":"i599","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"599","subseriesTitle":"MOON","title":"(RLC-14) Geologic map of the Alphonsus region of the moon","docAbstract":"

This 1:250,000- scale geologic map is one of a series prepared largely from photographs transmitted by Ranger IX (reproduced in a report by Jet Propulsion Lab., 1966). It depicts the geology of the crater Alphonsus (in which Ranger IX impacted) and environs. The primary objective of the mapping was to apply extant lunar mapping techniques used on relatively small scale telescopic photographs to the larger scale Ranger photographs, in preparation for extensive analysis of Lunar Orbiter photography in support of the Apollo program. An additional objective was to shed more light on the formation of Alphonsus and its associated features. The map outlines rock units that are inferred from surface features and characteristics, such as topography and albedo. Each rock unit is assigned an age and arranged in the explanation so that the youngest unit are at the top and the oldest at the bottom. The age classification is based on the early work of Shoemaker and Hackman (1962), and subsequent revisions reported by McCauley (1967) and Wilhelms (1966). Geology of the region has been mapped at a scale of 1:1,000,000 on the basis of Earth-based photographs and observations (Howard and Masursky, 1968). A more detailed, 1;50,000-scale map of part of the Alphonsus floor was prepared by McCauley (1969), who used Ranger IX photographs as his source of geologic information. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i599","collaboration":"prepared in cooperation with Jet Propulsion Laboratory, California Institute of Technology National Aeronautics and Space Administration, and the USAF Aeronautical Chart and Information Center","usgsCitation":"Carr, M.H., 1969, (RLC-14) Geologic map of the Alphonsus region of the moon: U.S. Geological Survey IMAP 599, Report; 1 map, https://doi.org/10.3133/i599.","productDescription":"Report; 1 map","costCenters":[],"links":[{"id":486697,"rank":5,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P1RZNFUX","text":"USGS data release","linkHelpText":"Interactive Map: IMAP 599 - (RLC-14) Geologic map of the Alphonsus region of the moon"},{"id":439075,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9WZPPZ8","text":"USGS data release","linkHelpText":"Geologic Map of the Alphonsus Region of the Moon"},{"id":189055,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0599/report-thumb.jpg"},{"id":114855,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0599/plate-1.pdf","size":"8446","linkFileType":{"id":1,"text":"pdf"}},{"id":114854,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0599/report.pdf","size":"47","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","otherGeospatial":"Alphonsus Crater, Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4906e4b0b290850eed1d","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":272304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63922,"text":"gp669 - 1969 - Aeromagnetic map of the Harrisburg-Scranton area, northeastern Pennsylvania","interactions":[],"lastModifiedDate":"2025-06-20T19:21:11.999807","indexId":"gp669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"669","title":"Aeromagnetic map of the Harrisburg-Scranton area, northeastern Pennsylvania","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp669","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Harrisburg-Scranton area, northeastern Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 669, 1 Plate: 24.47 x 35.76 inches, https://doi.org/10.3133/gp669.","productDescription":"1 Plate: 24.47 x 35.76 inches","costCenters":[],"links":[{"id":250252,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0669/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250251,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0669/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491059,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6036.htm","linkFileType":{"id":5,"text":"html"}},{"id":253774,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0669/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Pennsylvania","otherGeospatial":"Harrisburg-Scranton area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77,\n 41.875\n ],\n [\n -77,\n 40\n ],\n [\n -75.375,\n 40\n ],\n [\n -75.375,\n 41.875\n ],\n [\n -77,\n 41.875\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db69231b","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":533391,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63873,"text":"gp642 - 1969 - Aeromagnetic map of the Norfolk quadrangle and parts of the West Torrington and South Sandisfield quadrangles, Litchfield County, Connecticut","interactions":[],"lastModifiedDate":"2025-06-18T19:30:41.48641","indexId":"gp642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"642","title":"Aeromagnetic map of the Norfolk quadrangle and parts of the West Torrington and South Sandisfield quadrangles, Litchfield County, Connecticut","docAbstract":"

No abstract available.

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No abstract available.

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