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Data obtained from more than 2,200 wells are analyzed. Seventeen chronostratigraphic units are mapped in the subsurface. They range in age from Jurassic(?) to post-Miocene. The purpose of the mapping program was to determine the external and internal geometry of mappable chronostratigraphic units and to derive and construct a permeability-distribution network for each unit based upon contrasts in the textures and compositions of its contained sediments. </p><p>The report contains a structure map and a combined isopach, lithofacies, and permeability-distribution map for each of the chronostratigraphic units delineated in the subsurface. In addition, it contains a map of the top of the basement surface. These maps, together with 36 stratigraphic cross sections, present a three-dimensional view of the regional subsurface hydrogeology. They provide focal points of reference for a discussion of regional tectonics, structure, stratigraphy, and permeability distribution. Taken together and in chronologic sequence, the maps constitute a detailed sedimentary model, the first such model to be constructed for the middle Atlantic Coastal Plain. </p><p>The chronostratigraphic units mapped record a structural history dominated by lateral and vertical movement along a system of intersecting hinge zones. Taphrogeny, related to transcurrent faulting, is the dominant type of deformation that controlled the geometry of the sedimentary model. </p><p>Twelve of the seventeen chronostratigraphic units mapped have depositional alinements and thickening trends that are independent of the present-day configuration of the underlying basement surface. These 12 units, classified as genetically unrooted units, are assigned to a first-order tectonic stage. A structural model is proposed whose alinements of positive and negative structural features are accordant with the depositional geometry of the chronostratigraphic units assigned to this tectonic stage. The dominant features of the structural model are northeast-plunging half grabens arranged en echelon and bordered by northeast-plunging fault-block anticlines. Tension-type hinge zones that strike north lie athwart the half grabens. </p><p>Five of the seventeen chronostratigraphic units mapped have depositional alinements and thickening trends that are accordant with the present-day configuration of the underlying basement surface. These five units, classified as genetically rooted units, are assigned to a second-order tectonic stage. A structural model is proposed whose alinements of positive and negative features are accordant with the depositional geometry of the chronostratigraphic units assigned to this tectonic stage. The dominant feature of this model is a graben that stands tangential to southeast-plunging asymmetrical anticlines. Tension-type hinge zones that strike northeast lie athwart the graben.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp796","usgsCitation":"Brown, P.M., Miller, J.A., and Swain, F.M., 1972, Structural and stratigraphic framework, and spatial distribution of permeability of the Atlantic Coastal Plain, North Carolina to New York: U.S. Geological Survey Professional Paper 796, Report: v, 79 p.; 59 Plates: 57.00 × 38.00 inches or smaller, https://doi.org/10.3133/pp796.","productDescription":"Report: v, 79 p.; 59 Plates: 57.00 × 38.00 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":67310,"text":"i766B - 1972 - Map showing relative ages of faults in the Sugar House quadrangle, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2025-08-05T17:12:21.891097","indexId":"i766B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"766","subseriesTitle":"NONE","chapter":"B","title":"Map showing relative ages of faults in the Sugar House quadrangle, Salt Lake County, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i766B","usgsCitation":"Van Horn, R., 1972, Map showing relative ages of faults in the Sugar House quadrangle, Salt Lake County, Utah: U.S. Geological Survey IMAP 766, 1 Plate: 34.81 x 28.05 inches, https://doi.org/10.3133/i766B.","productDescription":"1 Plate: 34.81 x 28.05 inches","costCenters":[],"links":[{"id":493580,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9521.htm","linkFileType":{"id":5,"text":"html"}},{"id":256350,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0766b/report-thumb.jpg"},{"id":256349,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0766b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256348,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0766b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Utah","county":"Salt Lake County","otherGeospatial":"Sugar House quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.75,\n              40.625\n            ],\n            [\n              -111.75,\n              40.75\n            ],\n            [\n              -111.875,\n              40.75\n            ],\n            [\n              -111.875,\n              40.625\n            ],\n            [\n              -111.75,\n              40.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3407","contributors":{"authors":[{"text":"Van Horn, Richard","contributorId":52169,"corporation":false,"usgs":true,"family":"Van Horn","given":"Richard","email":"","affiliations":[],"preferred":false,"id":275964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2844,"text":"wsp2000 - 1972 - Water for a rapidly growing urban community — Oakland County, Michigan","interactions":[],"lastModifiedDate":"2021-12-15T21:59:00.124099","indexId":"wsp2000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"2000","title":"Water for a rapidly growing urban community — Oakland County, Michigan","docAbstract":"<p>Oakland County, an area of 899 square miles, is in southeastern Michigan. The southern part of the county is overlapped by the suburbs of the city of Detroit. </p><p>In 1970, about 850,000 people were living in the county and using about 100 million gallons of water a day. More than 80 percent of the water used for large industrial and municipal supplies came from Detroit's water system. </p><p>The average annual rate of streamflow from the county is about 370 million gallons per day (575 cubic feet per second). Median annual 7-day low flows range from 0 to 0.25 cfs per square mile. Low flows can be augmented by more than 60,000 acre-feet of water captured during high streamflow by construction of small reservoirs at 21 inventoried sites. </p><p>Glacial deposits and the Marshall Sandstone are the prime sources of ground water. Most wells that penetrate the full thickness of glacial deposits in the northwestern part of the county will yield at least 50 gpm (gallons per minute), and many will yield more than 400 gpm. The Marshall Sandstone, which occurs only in the Holly area, is capable of yielding more than 1,000 gpm. </p><p>The chemical quality of both surface and ground water is relatively good throughout the county. Only in the southern part of the county is the dissolved solids above the acceptable standard of 500 milligrams per liter.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2000","collaboration":"Prepared in cooperation with Oakland County and the State of Michigan","usgsCitation":"Twenter, F.R., and Knutilla, R., 1972, Water for a rapidly growing urban community — Oakland County, Michigan: U.S. Geological Survey Water Supply Paper 2000, ix, 150 p., https://doi.org/10.3133/wsp2000.","productDescription":"ix, 150 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":138695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wsp2000.JPG"},{"id":392975,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25468.htm"},{"id":38,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wsp2000/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","county":"Oakland County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.4546,42.8798],[-83.2227,42.887],[-83.1025,42.8884],[-83.0986,42.801],[-83.0905,42.6238],[-83.0867,42.5355],[-83.0843,42.4463],[-83.3264,42.4416],[-83.4403,42.4393],[-83.553,42.4351],[-83.6669,42.4312],[-83.6733,42.5196],[-83.6863,42.7822],[-83.6902,42.871],[-83.5737,42.8744],[-83.4541,42.8766],[-83.4546,42.8798]]]},\"properties\":{\"name\":\"Oakland\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ac69","contributors":{"authors":[{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knutilla, R. L.","contributorId":65451,"corporation":false,"usgs":true,"family":"Knutilla","given":"R. L.","affiliations":[],"preferred":false,"id":145892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66718,"text":"i784N - 1972 - Low flow of streams, Hartford North Quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:11:19","indexId":"i784N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"784","subseriesTitle":"NONE","chapter":"N","title":"Low flow of streams, Hartford North Quadrangle, Connecticut","language":"ENGLISH","doi":"10.3133/i784N","usgsCitation":"Olin, D., 1972, Low flow of streams, Hartford North Quadrangle, Connecticut: U.S. Geological Survey IMAP 784, 1 map., https://doi.org/10.3133/i784N.","productDescription":"1 map.","costCenters":[],"links":[{"id":255452,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0784n/plate-1.pdf","size":"4628","linkFileType":{"id":1,"text":"pdf"}},{"id":255453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0784n/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":255454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0784n/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.75,41.75 ], [ -72.75,41.8675 ], [ -72.61749999999999,41.8675 ], [ -72.61749999999999,41.75 ], [ -72.75,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64491b","contributors":{"authors":[{"text":"Olin, D.A.","contributorId":106905,"corporation":false,"usgs":true,"family":"Olin","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":274959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66785,"text":"i784A - 1972 - Unconsolidated materials, Hartford North quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2022-04-12T20:16:24.281479","indexId":"i784A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"784","chapter":"A","title":"Unconsolidated materials, Hartford North quadrangle, Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i784A","usgsCitation":"Pessl, F., and Hildreth, C.T., 1972, Unconsolidated materials, Hartford North quadrangle, Connecticut: U.S. Geological Survey IMAP 784, Report: 1 p.; 1 Plate: 43.53 × 28.99 inches, https://doi.org/10.3133/i784A.","productDescription":"Report: 1 p.; 1 Plate: 43.53 × 28.99 inches","costCenters":[],"links":[{"id":398594,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9580.htm"},{"id":256073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0784a/report-thumb.jpg"},{"id":256072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0784a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256071,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0784a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Connecticut","otherGeospatial":"Hartford North quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.75,\n              41.75\n            ],\n            [\n              -72.625,\n              41.75\n            ],\n            [\n              -72.625,\n              41.875\n            ],\n            [\n              -72.75,\n              41.875\n            ],\n            [\n              -72.75,\n              41.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f7dd","contributors":{"authors":[{"text":"Pessl, Fred Jr.","contributorId":54211,"corporation":false,"usgs":true,"family":"Pessl","given":"Fred","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":275079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildreth, C. T.","contributorId":14456,"corporation":false,"usgs":true,"family":"Hildreth","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":275078,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6367,"text":"pp749 - 1972 - Distribution of the Middle Ordovician Copenhagen formation and its trilobites in Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"pp749","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"749","title":"Distribution of the Middle Ordovician Copenhagen formation and its trilobites in Nevada","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp749","usgsCitation":"Ross, R.J., and Shaw, F.C., 1972, Distribution of the Middle Ordovician Copenhagen formation and its trilobites in Nevada: U.S. Geological Survey Professional Paper 749, 33 p., https://doi.org/10.3133/pp749.","productDescription":"33 p.","costCenters":[],"links":[{"id":117536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0749/report-thumb.jpg"},{"id":33741,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0749/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f408","contributors":{"authors":[{"text":"Ross, Reuben James Jr.","contributorId":36911,"corporation":false,"usgs":true,"family":"Ross","given":"Reuben","suffix":"Jr.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":152584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, Frederick C.","contributorId":66247,"corporation":false,"usgs":true,"family":"Shaw","given":"Frederick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":152585,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66629,"text":"i724 - 1972 - Metamorphic map of the Appalachians","interactions":[],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i724","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"724","subseriesTitle":"NONE","title":"Metamorphic map of the Appalachians","language":"ENGLISH","doi":"10.3133/i724","usgsCitation":"Morgan, B., 1972, Metamorphic map of the Appalachians: U.S. Geological Survey IMAP 724, 1 map :col. ;94 x 67 cm., https://doi.org/10.3133/i724.","productDescription":"1 map :col. ;94 x 67 cm.","costCenters":[],"links":[{"id":255997,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0724/plate-1.pdf","size":"4462","linkFileType":{"id":1,"text":"pdf"}},{"id":255998,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0724/report.pdf","size":"1023","linkFileType":{"id":1,"text":"pdf"}},{"id":255999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0724/report-thumb.jpg"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,30 ], [ -85,51 ], [ -64,51 ], [ -64,30 ], [ -85,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6287ab","contributors":{"authors":[{"text":"Morgan, B. A.","contributorId":87128,"corporation":false,"usgs":true,"family":"Morgan","given":"B. A.","affiliations":[],"preferred":false,"id":274825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6265,"text":"pp762 - 1972 - Instrumentation studies of earth tremors related to geology and to mining at the Somerset coal mine, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"pp762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"762","title":"Instrumentation studies of earth tremors related to geology and to mining at the Somerset coal mine, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp762","usgsCitation":"Osterwald, F.W., Dunrud, C., Bennetti, J., and Maberry, J., 1972, Instrumentation studies of earth tremors related to geology and to mining at the Somerset coal mine, Colorado: U.S. Geological Survey Professional Paper 762, 27 p., https://doi.org/10.3133/pp762.","productDescription":"27 p.","costCenters":[],"links":[{"id":117069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0762/report-thumb.jpg"},{"id":33494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0762/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6c53","contributors":{"authors":[{"text":"Osterwald, Frank W.","contributorId":98301,"corporation":false,"usgs":true,"family":"Osterwald","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":152411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunrud, C.R.","contributorId":94290,"corporation":false,"usgs":true,"family":"Dunrud","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":152410,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennetti, J.B. Jr.","contributorId":13968,"corporation":false,"usgs":true,"family":"Bennetti","given":"J.B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":152408,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maberry, J. O.","contributorId":56636,"corporation":false,"usgs":true,"family":"Maberry","given":"J. O.","affiliations":[],"preferred":false,"id":152409,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":66907,"text":"i786B - 1972 - Vegetation map of the Evergreen Quadrangle, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i786B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"786","subseriesTitle":"NONE","chapter":"B","title":"Vegetation map of the Evergreen Quadrangle, Jefferson County, Colorado","language":"ENGLISH","doi":"10.3133/i786B","usgsCitation":"Reed, J.C., and Keith, J.R., 1972, Vegetation map of the Evergreen Quadrangle, Jefferson County, Colorado: U.S. Geological Survey IMAP 786, 1 map :col. ;58 x 45 cm. on sheet 74 x 100 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i786B.","productDescription":"1 map :col. ;58 x 45 cm. on sheet 74 x 100 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":256184,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0786b/plate-1.pdf","size":"8382","linkFileType":{"id":1,"text":"pdf"}},{"id":256185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0786b/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":256186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0786b/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.36749999999999,39.6175 ], [ -105.36749999999999,39.75 ], [ -105.25,39.75 ], [ -105.25,39.6175 ], [ -105.36749999999999,39.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025c4","contributors":{"authors":[{"text":"Reed, J. C. Jr.","contributorId":97063,"corporation":false,"usgs":true,"family":"Reed","given":"J.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keith, J. R.","contributorId":46513,"corporation":false,"usgs":true,"family":"Keith","given":"J.","middleInitial":"R.","affiliations":[],"preferred":false,"id":275264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48176,"text":"ofr73199 - 1972 - Geology and ground water of the Pajaro Valley area, Santa Cruz and Monterey Counties, California","interactions":[],"lastModifiedDate":"2021-12-23T19:54:13.902678","indexId":"ofr73199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"73-199","title":"Geology and ground water of the Pajaro Valley area, Santa Cruz and Monterey Counties, California","docAbstract":"The Pajaro Valley area, California, covering about 120 square miles, extends from the southern part of Santa Cruz County to several miles south of the county line into Monterey County. It borders the Pacific Ocean on the west and the Santa Cruz Mountains on the east. The city of Watsonville is the largest center of population.\r\n\r\nDeposits that range in age from Pliocene to Holocene make up the ground-water reservoir. These include, from oldest to youngest, the Purisima Formation, Aromas Red Sands of Allen (1946), terrace deposits, alluvium, and dune sand. These deposits underlie an area of about 80 square miles and have a maximum thickness of about 4,000 feet. The alluvium yields most of the water pumped from wells in the area.\r\n\r\nPre-Pliocene rocks underlie and form the boundaries of the ground-water reservoir. These rocks contain ground water in fractures and in sandstone beds. However, they are not an important source of ground water. There is close continuity between the geology of the Pajaro Valley area and that of the Soquel-Aptos area, which is contiguous on the north.\r\n\r\nGround water in the Pajaro Valley area is derived from three sources: (1) Precipitation within the Pajaro Valley area that reaches the ground-water body by direct infiltration or by seepage from streams, (2) seepage from the Pajaro River as it crosses the Pajaro Valley carrying runoff which originates upstream from the valley, and (3) precipitation in the Soquel-Aptos area that infiltrates and then moves southeastward at depth into the Pajaro Valley area.\r\n\r\nGround water in most wells in the Pajaro Valley area occurs under confined (artesian) conditions; the only exception is ground water in the upper, near-surface part of the alluvium and that in the dune sand. It moves south from the north part of the area and southwest away from the San Andreas fault toward and out under Monterey Bay. In the south part of the area, ground-water movement is almost due west. The San Andreas fault probably is the only fault that has a restrictive effect on the movement of ground water.\r\n\r\nWater levels in wells in the Pajaro Valley area in 1970 averaged about 2 feet lower than that in 1950. Ground-water pumpage averaged 46,100 acre-feet per year during the period 1963 through 1969.\r\n\r\nThere are two distinct ground-water quality zones in the Pajaro Valley area: a shallow, semiperched zone of poor-quality water and a deeper, confined zone of good quality-water. Also, sea-water intrusion has occurred in limited areas near the mouth of the Pajaro River and in the vicinity of McClusky Slough.\r\n\r\nThe channel of the Pajaro River near Aromas and the beds of streams that drain the area north and northeast of Watsonville have the greatest potential for artificial recharge by surface infiltration of water. The gravel at the base of the alluvium is the best zone for injection of water through wells.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73199","usgsCitation":"Muir, K.S., 1972, Geology and ground water of the Pajaro Valley area, Santa Cruz and Monterey Counties, California: U.S. Geological Survey Open-File Report 73-199, Report: iv, 33 p.; 3 Plates: 33.53 × 21.22 inches or smaller, https://doi.org/10.3133/ofr73199.","productDescription":"Report: iv, 33 p.; 3 Plates: 33.53 × 21.22 inches or smaller","costCenters":[],"links":[{"id":388963,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2298.htm"},{"id":84907,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0199/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0199/report-thumb.jpg"},{"id":84910,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0199/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84908,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0199/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84909,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0199/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Monterey County, Santa Cruz County","otherGeospatial":"Pajaro Valley area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.87408447265625,\n              36.81808022778526\n            ],\n            [\n              -121.6021728515625,\n              36.81808022778526\n            ],\n            [\n              -121.6021728515625,\n              37.0833\n            ],\n            [\n              -121.87408447265625,\n              37.0833\n            ],\n            [\n              -121.87408447265625,\n              36.81808022778526\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cacf","contributors":{"authors":[{"text":"Muir, K. 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,{"id":66971,"text":"i791 - 1972 - Maps showing the approximate configuration and depth to the top of the Laramie-Fox Hills aquifer, Denver Basin, Colorado","interactions":[],"lastModifiedDate":"2025-08-05T20:58:33.86822","indexId":"i791","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"791","title":"Maps showing the approximate configuration and depth to the top of the Laramie-Fox Hills aquifer, Denver Basin, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i791","usgsCitation":"Romero, J.C., and Hampton, E.R., 1972, Maps showing the approximate configuration and depth to the top of the Laramie-Fox Hills aquifer, Denver Basin, Colorado: U.S. Geological Survey IMAP 791, 1 Plate: 31.07 x 22.51 inches, https://doi.org/10.3133/i791.","productDescription":"1 Plate: 31.07 x 22.51 inches","costCenters":[],"links":[{"id":493631,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9627.htm","linkFileType":{"id":5,"text":"html"}},{"id":256221,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0791/report-thumb.jpg"},{"id":256220,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0791/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256219,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0791/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Colorado","otherGeospatial":"Denver Basin, Laramie-Fox Hills aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.348,\n              40.454\n            ],\n            [\n              -105.348,\n              38.686\n            ],\n            [\n              -103.722,\n              38.686\n            ],\n            [\n              -103.722,\n              40.454\n            ],\n            [\n              -105.348,\n              40.454\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db606139","contributors":{"authors":[{"text":"Romero, J. C.","contributorId":58635,"corporation":false,"usgs":false,"family":"Romero","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":275390,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67177,"text":"i700 - 1972 - Geologic map of the Lunar Crater Quadrangle, Nye County, Nevada","interactions":[{"subject":{"id":46925,"text":"ofr69263 - 1969 - Geologic map of the Lunar Crater quadrangle, Nye County, Nevada","indexId":"ofr69263","publicationYear":"1969","noYear":false,"title":"Geologic map of the Lunar Crater quadrangle, Nye County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":67177,"text":"i700 - 1972 - Geologic map of the Lunar Crater Quadrangle, Nye County, Nevada","indexId":"i700","publicationYear":"1972","noYear":false,"title":"Geologic map of the Lunar Crater Quadrangle, Nye County, Nevada"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i700","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"700","subseriesTitle":"NONE","title":"Geologic map of the Lunar Crater Quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/i700","usgsCitation":"Snyder, R., Ekren, E.B., and Dixon, G.L., 1972, Geologic map of the Lunar Crater Quadrangle, Nye County, Nevada: U.S. Geological Survey IMAP 700, 1 map :col. ;57 x 46 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i700.","productDescription":"1 map :col. ;57 x 46 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":108199,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12256.htm","linkFileType":{"id":5,"text":"html"},"description":"12256"},{"id":188809,"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\": [ [ [ -116.25,38.25 ], [ -116.25,38.5 ], [ -116,38.5 ], [ -116,38.25 ], [ -116.25,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d4c","contributors":{"authors":[{"text":"Snyder, R.P.","contributorId":9647,"corporation":false,"usgs":true,"family":"Snyder","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":275722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":275723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dixon, G. L.","contributorId":95468,"corporation":false,"usgs":true,"family":"Dixon","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5727,"text":"pp760 - 1972 - Paleomagnetism of some Lake Superior Keweenawan rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"pp760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"760","title":"Paleomagnetism of some Lake Superior Keweenawan rocks","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp760","usgsCitation":"Books, K.G., 1972, Paleomagnetism of some Lake Superior Keweenawan rocks: U.S. Geological Survey Professional Paper 760, 42 p., https://doi.org/10.3133/pp760.","productDescription":"42 p.","costCenters":[],"links":[{"id":121482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0760/report-thumb.jpg"},{"id":32307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ba3","contributors":{"authors":[{"text":"Books, Kenneth G.","contributorId":25910,"corporation":false,"usgs":true,"family":"Books","given":"Kenneth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":151491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6372,"text":"pp741 - 1972 - The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"pp741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"741","title":"The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp741","usgsCitation":"Rowe, J.J., Morey, G.W., and Zen, C., 1972, The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data: U.S. Geological Survey Professional Paper 741, 37 p., https://doi.org/10.3133/pp741.","productDescription":"37 p.","costCenters":[],"links":[{"id":117540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0741/report-thumb.jpg"},{"id":33746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0741/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641223","contributors":{"authors":[{"text":"Rowe, Jack James","contributorId":73583,"corporation":false,"usgs":true,"family":"Rowe","given":"Jack","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":152598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morey, George Washington","contributorId":62267,"corporation":false,"usgs":true,"family":"Morey","given":"George","email":"","middleInitial":"Washington","affiliations":[],"preferred":false,"id":152597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zen, C.S.","contributorId":26572,"corporation":false,"usgs":true,"family":"Zen","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":152596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66849,"text":"i713 - 1972 - Geologic map of the Tycho Quadrangle of the Moon","interactions":[{"subject":{"id":20484,"text":"ofr70263 - 1970 - Preliminary geologic map of the Tycho quadrangle of the Moon","indexId":"ofr70263","publicationYear":"1970","noYear":false,"title":"Preliminary geologic map of the Tycho quadrangle of the Moon"},"predicate":"SUPERSEDED_BY","object":{"id":66849,"text":"i713 - 1972 - Geologic map of the Tycho Quadrangle of the Moon","indexId":"i713","publicationYear":"1972","noYear":false,"title":"Geologic map of the Tycho Quadrangle of the Moon"},"id":1}],"lastModifiedDate":"2023-05-04T11:13:00.847891","indexId":"i713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"713","subseriesTitle":"MOON","title":"Geologic map of the Tycho Quadrangle of the Moon","docAbstract":"<p><span class=\"TextRun SCXW220402250 BCX8\" lang=\"EN-US\" xml:lang=\"EN-US\" data-contrast=\"auto\"><span class=\"NormalTextRun SCXW220402250 BCX8\">The Tycho quadrangle is centrally located in the southern half of the earthside hemisphere</span> <span class=\"NormalTextRun SCXW220402250 BCX8\">of the Moon. The area is characterized by</span><span class=\"NormalTextRun SCXW220402250 BCX8\"> a high density of craters, the</span><span class=\"NormalTextRun SCXW220402250 BCX8\"> largest of which </span><span class=\"NormalTextRun SCXW220402250 BCX8\">–</span> <span class=\"SpellingError SCXW220402250 BCX8\">Stofler</span> <span class=\"NormalTextRun SCXW220402250 BCX8\">– is about 140 km in diameter. The northern and </span><span class=\"NormalTextRun SCXW220402250 BCX8\">eastern parts if the quadrangle </span><span class=\"ContextualSpellingAndGrammarError SCXW220402250 BCX8\">are</span><span class=\"NormalTextRun SCXW220402250 BCX8\"> dominated by plains (</span><span class=\"SpellingError SCXW220402250 BCX8\">pIp</span><span class=\"NormalTextRun SCXW220402250 BCX8\">, Ip</span><span class=\"NormalTextRun SCXW220402250 BCX8\">) and hilly terra (</span><span class=\"SpellingError SCXW220402250 BCX8\">IpIt</span><span class=\"NormalTextRun SCXW220402250 BCX8\">) units of regional extent</span><span class=\"NormalTextRun SCXW220402250 BCX8\">, and the western part</span><span class=\"NormalTextRun SCXW220402250 BCX8\"> by the crater Tycho and its ejecta blanket. Structural features probably associated with the </span><span class=\"NormalTextRun SCXW220402250 BCX8\">Imbrium</span><span class=\"NormalTextRun SCXW220402250 BCX8\"> basin to the north and Orienta</span><span class=\"NormalTextRun SCXW220402250 BCX8\">le </span><span class=\"NormalTextRun SCXW220402250 BCX8\">and </span><span class=\"NormalTextRun SCXW220402250 BCX8\">Humorum</span><span class=\"NormalTextRun SCXW220402250 BCX8\"> basins to the northwest are present, although blanketing units related to these basins are not recognized.</span></span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i713","usgsCitation":"Pohn, H., 1972, Geologic map of the Tycho Quadrangle of the Moon: U.S. Geological Survey IMAP 713, 1 Plate:  66.67 × 37.33 inches, https://doi.org/10.3133/i713.","productDescription":"1 Plate:  66.67 × 37.33 inches","costCenters":[],"links":[{"id":439047,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9Q3B4SK","text":"USGS data release","linkHelpText":"Geologic map of the Tycho Quadrangle of the Moon"},{"id":188754,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101371,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0713/plate-1.pdf","size":"8830","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","otherGeospatial":"Moon, Tycho Crater","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2b9","contributors":{"authors":[{"text":"Pohn, H. A.","contributorId":6912,"corporation":false,"usgs":true,"family":"Pohn","given":"H. A.","affiliations":[],"preferred":false,"id":275179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66792,"text":"i733 - 1972 - Geologic map of the Rio Grande Quadrangle, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"733","subseriesTitle":"NONE","title":"Geologic map of the Rio Grande Quadrangle, Puerto Rico","language":"ENGLISH","doi":"10.3133/i733","usgsCitation":"Pease, M., and Briggs, R.P., 1972, Geologic map of the Rio Grande Quadrangle, Puerto Rico: U.S. Geological Survey IMAP 733, 1 map :col. ;70 x 66 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i733.","productDescription":"1 map :col. ;70 x 66 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106938,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9490.htm","linkFileType":{"id":5,"text":"html"},"description":"9490"},{"id":188203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91607,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0733/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -65.86749999999999,18.3675 ], [ -65.86749999999999,18.5 ], [ -65.75,18.5 ], [ -65.75,18.3675 ], [ -65.86749999999999,18.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6912d9","contributors":{"authors":[{"text":"Pease, M. H.","contributorId":102485,"corporation":false,"usgs":true,"family":"Pease","given":"M. H.","affiliations":[],"preferred":false,"id":275087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, R. P.","contributorId":47797,"corporation":false,"usgs":true,"family":"Briggs","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":275086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3293,"text":"cir648 - 1972 - Reports and maps of the Geological Survey released only in the open files, 1971","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir648","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"648","title":"Reports and maps of the Geological Survey released only in the open files, 1971","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir648","usgsCitation":"Weld, B., Iseri, K.T., and Brett, G.W., 1972, Reports and maps of the Geological Survey released only in the open files, 1971: U.S. Geological Survey Circular 648, 26 p. :26 cm., https://doi.org/10.3133/cir648.","productDescription":"26 p. :26 cm.","costCenters":[],"links":[{"id":117589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1972/0648/report-thumb.jpg"},{"id":30289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1972/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f385","contributors":{"authors":[{"text":"Weld, Betsy A.","contributorId":68714,"corporation":false,"usgs":true,"family":"Weld","given":"Betsy A.","affiliations":[],"preferred":false,"id":146611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iseri, Kathleen T.","contributorId":77910,"corporation":false,"usgs":true,"family":"Iseri","given":"Kathleen","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":146612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brett, George W.","contributorId":58622,"corporation":false,"usgs":true,"family":"Brett","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146610,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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,{"id":67022,"text":"i787B - 1972 - Slope map of Anchorage and vicinity, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i787B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"787","subseriesTitle":"NONE","chapter":"B","title":"Slope map of Anchorage and vicinity, Alaska","language":"ENGLISH","doi":"10.3133/i787B","usgsCitation":"Schmoll, H., and Dobrovolny, E., 1972, Slope map of Anchorage and vicinity, Alaska: U.S. Geological Survey IMAP 787, 1 map :col. ;125 x 103 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i787B.","productDescription":"1 map :col. ;125 x 103 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106969,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9614.htm","linkFileType":{"id":5,"text":"html"},"description":"9614"},{"id":187489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.08333333333334,61.06666666666667 ], [ -150.08333333333334,61.333333333333336 ], [ -149.6175,61.333333333333336 ], [ -149.6175,61.06666666666667 ], [ -150.08333333333334,61.06666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee2b4","contributors":{"authors":[{"text":"Schmoll, H. R.","contributorId":71543,"corporation":false,"usgs":true,"family":"Schmoll","given":"H. R.","affiliations":[],"preferred":false,"id":275466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dobrovolny, Ernest","contributorId":45288,"corporation":false,"usgs":true,"family":"Dobrovolny","given":"Ernest","affiliations":[],"preferred":false,"id":275465,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2615,"text":"wsp1663G - 1972 - Ground-water in the Teresina-Campo Maior area, Piaui, Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1663G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1663","chapter":"G","title":"Ground-water in the Teresina-Campo Maior area, Piaui, Brazil","docAbstract":"The Teresina-Campo Maior area lies in a presently developing farming and grazing region near the margin of drought-prone northeast Brazil where irrigated farming offers the best potential for economic development. The area comprises 9,700 square kilometers largely of catinga-covered tabular uplands which are drained by the perennial Rio Parnatba. The climate is hot and humid most of the year but with distinct wet and dry seasons. Temperature extremes range from 20?C to 39?C and the annum rainfall averages 1,200 millimeters. \r\n\r\nThe area's ground-water reservoir is contained chiefly in sandstone aquifers of six westward-dipping sedimentary rock formations, all part of the Maranhao sedimentary basin. The youngest of these formations, namely the Piaut (Pennsylvarian), Poti (Mississippian), Longa (Upper Devonian), and Cabecas (Middle Devoniar), contain the principal aquifers. Precipitation is the primary source of recharge to these aquifers and is more than sufficient to replenish current withdrawals from wells. Underlying the principal aquifers are the untapped Pimenteiras and Serra Grande Formations (both Lower Devonian) which in areas adjacent to the report area are moderately good to excellent water producers. These aquifers are recharged principally by lateral inflow from the east. Water also occurs in the alluvial deposits (Quaternary) underlying the flood plain of the Rio Parnatba but recurrent and uncontrolled flooding at present (1966) precludes their development. Of little economic importance, because they lie above the zone of saturation, are the thin erosional remnants of the Pastos Bons (Upper Triassic), Matuca, and Pedra de Fogo (both Permian) Formations. \r\n\r\nThere are in the report area about 200 drilled wells most of which are pumped with power-driven engines. The wells range from 40 to 500 meters deep but most do not exceed 150 meters, and practically all are completed open hole. Yields range from 500 liters per day for 6-inch-diameter domestic wells to 240,000 liters per hour for 10-inch high-capacity municipal wells. Although there are many more dug wells than drilled wells, dug wells account for less than 1 percent of the current (1966) draft. The current annual withdrawal from the principal aquifers is approximately 5 million cubic meters of which almost half is used for municipal supply and the rest for rural household and irrigation uses. Additional water for public supply is available from aquifers now being pumped, and larger yields probably could be obtained from rural wells designed to take full advantage of the aquifer. Analyses of 28 samples show that the chemical quality of the water is well below the \r\n\r\naccepted limits of mineral concentration for most uses. Water from the Longa Formation averages 842 milligrams per liter in total dissolved solids and is more mineralized than that in the Piaul and Port Formations which contain water averaging less than 300 milligrams per liter. The water in the Piaui and Poti aquifers is the most suitable in the area for irrigation and has SAR values of C1-S1 and C2-S1. \r\n\r\nThe quantities of water currently being used for irrigation are relatively small (600,000 cubic meters annually) but will increase substantially when intensive irrigation becomes a reality. Divisio de Hydrogeologia da Superintendancia do Desenvolvimento do Nordeste estimates that about 2,500 million cubic meters of water per year would be needed to irrigate about 250,000 hectares in the Teresina-Campo Maior area (about 25 percent of the total area). This goal, however, is not likely to be realized as the water requirement is five times the estimated natural recharge to the aquifers of the area. \r\n\r\nMost of the water-bearing formations in the report area have barely been tapped and can be developed a great deal more. In fact, the current annual withdrawal from the principal aquifers is less than 0.0025 percent of a conservative estimate of annual replenishment from rainfall. Additionally, only the","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1663G","usgsCitation":"Rodis, H.G., and Suszczynski, E.F., 1972, Ground-water in the Teresina-Campo Maior area, Piaui, Brazil: U.S. Geological Survey Water Supply Paper 1663, iv, G 1-G 34 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1663G.","productDescription":"iv, G 1-G 34 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1663g/report-thumb.jpg"},{"id":28905,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1663g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28906,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1663g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66823c","contributors":{"authors":[{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suszczynski, Edison F.","contributorId":14804,"corporation":false,"usgs":true,"family":"Suszczynski","given":"Edison","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145498,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67402,"text":"i591L - 1972 - Map showing landslides and areas of potential landsliding in the Salina quadrangle, Utah","interactions":[],"lastModifiedDate":"2025-08-04T21:22:21.882867","indexId":"i591L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"591","chapter":"L","title":"Map showing landslides and areas of potential landsliding in the Salina quadrangle, Utah","docAbstract":"<p>The term “landslide” is broadly defined as any “downward and outward movement of slope-forming materials composed of natural rock, soils, artificial fills, or combinations of these materials. The moving mass may proceed by any one of three principal types of movement: falling, sliding, or flossing, or by their combinations” (Varnes, 1958). Landslides and areas of potential landslides are fairly common in the rugged terrain of the Salina quadrangle. In much of the western half of the map area, relatively high rainfall, steep slopes, and flat layers of hard rock on top of very soft incompetent rock all favor landsliding, chiefly as slides and earth flows. In arid parts of the quadrangle, principally in the east half, alternating flat layers of hard and soft rocks are eroded to bare cliffs separated by benches, and rockfalls are the dominant type of landsliding. Landslides were more active in the wetter climate of the Pleistocene Epoch, which ended several thousand years ago (Smith and others, 1963, p. 52). Although landslide deposits are abundant in the Salina quadrangle, few landslide movements have been documented during historic time, partly because landslides are generally less active now than during Pleistocene times, partly because movement is commonly very slow and thus escapes notice, and partly because of the remoteness and sparse population of the area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i591L","usgsCitation":"Williams, P., 1972, Map showing landslides and areas of potential landsliding in the Salina quadrangle, Utah: U.S. Geological Survey IMAP 591, 1 Plate: 39.86 x 27.62 inches; Cover: 9.18 x 11.77 inches, https://doi.org/10.3133/i591L.","productDescription":"1 Plate: 39.86 x 27.62 inches; Cover: 9.18 x 11.77 inches","costCenters":[],"links":[{"id":493513,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9385.htm","linkFileType":{"id":5,"text":"html"}},{"id":256589,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0591l/report-thumb.jpg"},{"id":256588,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0591l/report.pdf","text":"Folio Cover","size":"37 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":256587,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0591l/plate-1.pdf","text":"Map I-591-L","size":"9.02 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Salina quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,38 ], [ -112,39 ], [ -110,39 ], [ -110,38 ], [ -112,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c76","contributors":{"authors":[{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":276132,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63359,"text":"gq998 - 1972 - Geologic map of the Bridal Veil Falls quadrangle, Utah","interactions":[{"subject":{"id":46972,"text":"ofr7014 - 1963 - Geologic map of the Bridal Veil Falls Quadrangle, Utah","indexId":"ofr7014","publicationYear":"1963","noYear":false,"title":"Geologic map of the Bridal Veil Falls Quadrangle, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":63359,"text":"gq998 - 1972 - Geologic map of the Bridal Veil Falls quadrangle, Utah","indexId":"gq998","publicationYear":"1972","noYear":false,"title":"Geologic map of the Bridal Veil Falls quadrangle, Utah"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:02","indexId":"gq998","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"998","title":"Geologic map of the Bridal Veil Falls quadrangle, Utah","language":"ENGLISH","doi":"10.3133/gq998","usgsCitation":"Baker, A.A., 1972, Geologic map of the Bridal Veil Falls quadrangle, Utah: U.S. Geological Survey Geologic Quadrangle 998, 1 map., https://doi.org/10.3133/gq998.","productDescription":"1 map.","costCenters":[],"links":[{"id":103709,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2295.htm","linkFileType":{"id":5,"text":"html"},"description":"2295"},{"id":249460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0998/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":252942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0998/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.61749999999999,40.25 ], [ -111.61749999999999,40.3675 ], [ -111.5,40.3675 ], [ -111.5,40.25 ], [ -111.61749999999999,40.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d8f4","contributors":{"authors":[{"text":"Baker, Arthur A.","contributorId":65446,"corporation":false,"usgs":true,"family":"Baker","given":"Arthur","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}