The Eudoxus quadrangle is in the northeastern part of the Moon’s nearside hemisphere. It is bordered on the west by Montes Caucasus, which form part of the main rim of the multi-ring Imbrium basin (Hartmann and Kuiper, 1962), and on the south side by Mare Serenitatis, which occupies another large multi-ringed basin. South and east of the prominent crater Eudoxus elevations decrease and the rugged highland terrain becomes more subdued and covered by mare materials in the Serenitatis basin, Lacus Somniorum, and Lacus Mortis.
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J.","contributorId":95037,"corporation":false,"usgs":true,"family":"Frank","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":152337,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67011,"text":"i685 - 1972 - Geologic map of the Teller Quadrangle, western Seward Peninsula, Alaska","interactions":[{"subject":{"id":15760,"text":"ofr70283 - 1970 - Geologic map of the Teller quadrangle, Alaska","indexId":"ofr70283","publicationYear":"1970","noYear":false,"title":"Geologic map of the Teller quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":67011,"text":"i685 - 1972 - Geologic map of the Teller Quadrangle, western Seward Peninsula, Alaska","indexId":"i685","publicationYear":"1972","noYear":false,"title":"Geologic map of the Teller Quadrangle, western Seward Peninsula, Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i685","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":"685","subseriesTitle":"NONE","title":"Geologic map of the Teller Quadrangle, western Seward Peninsula, Alaska","language":"ENGLISH","doi":"10.3133/i685","usgsCitation":"Sainsbury, C., 1972, Geologic map of the Teller Quadrangle, western Seward Peninsula, Alaska: U.S. Geological Survey IMAP 685, 1 map :col. ;45 x 76 cm. folded in envelope 30 x 24 cm. +1 text., https://doi.org/10.3133/i685.","productDescription":"1 map :col. ;45 x 76 cm. folded in envelope 30 x 24 cm. +1 text.","costCenters":[],"links":[{"id":108198,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12255.htm","linkFileType":{"id":5,"text":"html"},"description":"12255"},{"id":256399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0685/report.pdf","size":"499","linkFileType":{"id":1,"text":"pdf"}},{"id":256400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0685/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -169,65 ], [ -169,66 ], [ -165,66 ], [ -165,65 ], [ -169,65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a586","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":275448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64944,"text":"i672 - 1972 - Geologic map of the Yost Quadrangle, Box Elder County, Utah, and Cassia County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:11:07","indexId":"i672","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":"672","subseriesTitle":"NONE","title":"Geologic map of the Yost Quadrangle, Box Elder County, Utah, and Cassia County, Idaho","language":"ENGLISH","doi":"10.3133/i672","usgsCitation":"Compton, R., 1972, Geologic map of the Yost Quadrangle, Box Elder County, Utah, and Cassia County, Idaho: U.S. Geological Survey IMAP 672, 1 map :col. ;88 x 66 cm. folded in envelope 30 x 24 cm. +1 text., https://doi.org/10.3133/i672.","productDescription":"1 map :col. ;88 x 66 cm. folded in envelope 30 x 24 cm. +1 text.","costCenters":[],"links":[{"id":106908,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9449.htm","linkFileType":{"id":5,"text":"html"},"description":"9449"},{"id":254819,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0672/report.pdf","size":"726","linkFileType":{"id":1,"text":"pdf"}},{"id":254820,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0672/report-thumb.jpg"}],"scale":"680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.75,41.75 ], [ -113.75,42 ], [ -113.5,42 ], [ -113.5,41.75 ], [ -113.75,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689725","contributors":{"authors":[{"text":"Compton, R.R.","contributorId":20420,"corporation":false,"usgs":true,"family":"Compton","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":272403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2844,"text":"wsp2000 - 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The southern part of the county is overlapped by the suburbs of the city of Detroit.
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.
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.
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.
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.
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