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","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1906, Part II, Coal, lignite, and peat (Bulletin 316)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b316F","usgsCitation":"Shaler, M., and Campbell, M.R., 1907, A reconnaissance survey of the western part of the Durango-Gallup coal field of Colorado and New Mexico. The Una del Gato coal field, Sandoval County, N. Mex. Coal in the vicinity of Fort Stanton Reservation, Lincoln County, N. Mex. Coal of Stone Canyon, Monterey County, Cal.: U.S. Geological Survey Bulletin 316, 63 p., https://doi.org/10.3133/b316F.","productDescription":"63 p.","startPage":"376","endPage":"438","costCenters":[],"links":[{"id":483849,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28099.htm","linkFileType":{"id":5,"text":"html"}},{"id":175728,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0316f/report-thumb.jpg"},{"id":114427,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0316f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973d5","contributors":{"authors":[{"text":"Shaler, M.K.","contributorId":63090,"corporation":false,"usgs":true,"family":"Shaler","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":239319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, M. 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1907 - Flowing wells and municipal water supplies in the middle and northern portions of the southern peninsula of Michigan","interactions":[],"lastModifiedDate":"2017-01-11T14:20:29","indexId":"wsp183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1907","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":"183","title":"Flowing wells and municipal water supplies in the middle and northern portions of the southern peninsula of Michigan","docAbstract":"A large amount of data on water supplies was collected by the writer in the course of glacial investigations made under the direction of Prof. T. C. Chamberlin in the last five years in the Southern Peninsula of Michigan. These investigations resulted in a partial acquaintance with conditions in about 200 separate flowing-well districts and brought out matters of such exceptional importance that arrangements were made to extend them by examining each of the flowing-well districts in the State sufficiently to determine its essential characteristics, present state of development, and probable capacity for future development. It was arranged also that the quality of various classes of water, both surface and underground, as well as water supplies of, cities and villages, should be given attention. As the mineral waters of the State had already been discussed in some detail by the State geologist, Dr. A. C. Lane, in Water-Supply Paper No. 31 of the United States Geological Survey, it was deemed unnecessary to prepare another report on that subject, but arrangements were made with Doctor Lane for embodying in this report the large amount of material which had accumulated at his office relative to other classes of water supply, and also for furnishing reports on certain counties in which special investigations had been carried on by the State survey. The results of all these studies, so far as they apply to the middle- and northern counties (see fig. 1, on next page), are embodied in the present report; the remainder appears in a companion report on the southern counties of the Southern Peninsula of Michigan.
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The contentions of both parties to the suit' are supported by the most eminently qualified men in the United States. The evidence presented and the discussions recorded are therefore of unique importance. The final record of testimony occupies 8,000 printed pages, much of which is irrelevant. This digest of testimony is the result of an attempt to recover the valuable material and present it in concise form. A consistent endeavor has been made by the reviewer to eliminate all personal opinions with reference to the issue and to make an impartial presentation of so much of the testimony as in his opinion appears to be relevant and of scientific importance. It will be well to remember in this connection that any digest of so large a volume of testimony must be the result of a final exercise of personal opinion by the reviewer as to those parts which may best be excluded. 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