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Off.,","doi":"10.3133/b554","usgsCitation":"Marshall, R.B., 1914, Results of spirit leveling in Kentucky, 1898 to 1913, inclusive: U.S. Geological Survey Bulletin 554, 184 p. :pl. ;24 cm., https://doi.org/10.3133/b554.","productDescription":"184 p. :pl. ;24 cm.","costCenters":[],"links":[{"id":93090,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0554/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0554/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ecc1","contributors":{"authors":[{"text":"Marshall, Robert Bradford","contributorId":106469,"corporation":false,"usgs":true,"family":"Marshall","given":"Robert","email":"","middleInitial":"Bradford","affiliations":[],"preferred":false,"id":214108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35849,"text":"b599 - 1914 - Our mineral reserves--how to make America industrially independent","interactions":[],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b599","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"599","title":"Our mineral reserves--how to make America industrially independent","language":"ENGLISH","publisher":"Govt. 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Off.,","doi":"10.3133/b599","usgsCitation":"Smith, G.O., 1914, Our mineral reserves--how to make America industrially independent: U.S. Geological Survey Bulletin 599, 48 p. ;24 cm., https://doi.org/10.3133/b599.","productDescription":"48 p. ;24 cm.","costCenters":[],"links":[{"id":93599,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0599/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0599/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a46c","contributors":{"authors":[{"text":"Smith, George Otis","contributorId":19538,"corporation":false,"usgs":true,"family":"Smith","given":"George","email":"","middleInitial":"Otis","affiliations":[],"preferred":false,"id":215328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35083,"text":"b557 - 1914 - Results of spirit leveling in the state of Washington, 1896 to 1913, inclusive","interactions":[],"lastModifiedDate":"2012-02-02T00:09:38","indexId":"b557","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"557","title":"Results of spirit leveling in the state of Washington, 1896 to 1913, inclusive","language":"ENGLISH","publisher":"Govt. 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Off.,","doi":"10.3133/b557","usgsCitation":"Marshall, R.B., 1914, Results of spirit leveling in the state of Washington, 1896 to 1913, inclusive: U.S. Geological Survey Bulletin 557, 178 p. :pl. ;24 cm., https://doi.org/10.3133/b557.","productDescription":"178 p. :pl. ;24 cm.","costCenters":[],"links":[{"id":93073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0557/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0557/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60562a","contributors":{"authors":[{"text":"Marshall, Robert Bradford","contributorId":106469,"corporation":false,"usgs":true,"family":"Marshall","given":"Robert","email":"","middleInitial":"Bradford","affiliations":[],"preferred":false,"id":214091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35111,"text":"b559 - 1914 - Results of spirit leveling in Michigan, 1911 and 1913","interactions":[],"lastModifiedDate":"2012-02-02T00:09:47","indexId":"b559","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"559","title":"Results of spirit leveling in Michigan, 1911 and 1913","language":"ENGLISH","publisher":"Govt. 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Off.,","doi":"10.3133/b559","usgsCitation":"Marshall, R.B., 1914, Results of spirit leveling in Michigan, 1911 and 1913: U.S. Geological Survey Bulletin 559, 79 p. :pl. ;24 cm., https://doi.org/10.3133/b559.","productDescription":"79 p. :pl. ;24 cm.","costCenters":[],"links":[{"id":93100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0559/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165717,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0559/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db6740db","contributors":{"authors":[{"text":"Marshall, Robert Bradford","contributorId":106469,"corporation":false,"usgs":true,"family":"Marshall","given":"Robert","email":"","middleInitial":"Bradford","affiliations":[],"preferred":false,"id":214119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35151,"text":"b551 - 1914 - Results of triangulation and primary traverse, 1911 and 1912","interactions":[],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b551","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"551","title":"Results of triangulation and primary traverse, 1911 and 1912","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b551","usgsCitation":"Marshall, R.B., 1914, Results of triangulation and primary traverse, 1911 and 1912: U.S. Geological Survey Bulletin 551, 396 p. :1 ill., 1 folded col. map ;24 cm., https://doi.org/10.3133/b551.","productDescription":"396 p. :1 ill., 1 folded col. map ;24 cm.","costCenters":[],"links":[{"id":93155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0551/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0551/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b29","contributors":{"authors":[{"text":"Marshall, Robert Bradford","contributorId":106469,"corporation":false,"usgs":true,"family":"Marshall","given":"Robert","email":"","middleInitial":"Bradford","affiliations":[],"preferred":false,"id":214164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36278,"text":"b574 - 1914 - Mining districts of the Dillon quadrangle, Montana, and adjacent areas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:38","indexId":"b574","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"574","title":"Mining districts of the Dillon quadrangle, Montana, and adjacent areas","language":"ENGLISH","publisher":"Govt. 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Off.,","doi":"10.3133/b574","usgsCitation":"Winchell, A.N., 1914, Mining districts of the Dillon quadrangle, Montana, and adjacent areas: U.S. Geological Survey Bulletin 574, 191 p. :ill., maps, plates ;24 cm., https://doi.org/10.3133/b574.","productDescription":"191 p. :ill., maps, plates ;24 cm.","costCenters":[],"links":[{"id":93814,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0574/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0574/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d44","contributors":{"authors":[{"text":"Winchell, Alexander Newton","contributorId":9329,"corporation":false,"usgs":true,"family":"Winchell","given":"Alexander","email":"","middleInitial":"Newton","affiliations":[],"preferred":false,"id":216057,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35601,"text":"b577 - 1914 - Geology of the phosphate deposits northeast of Georgetown, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b577","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"577","title":"Geology of the phosphate deposits northeast of Georgetown, Idaho","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/b577","usgsCitation":"Richards, R.W., and Mansfield, G.R., 1914, Geology of the phosphate deposits northeast of Georgetown, Idaho: U.S. Geological Survey Bulletin 577, 76 p. :ill., plates (part fold.) fold. maps, diagr. ;24 cm., https://doi.org/10.3133/b577.","productDescription":"76 p. :ill., plates (part fold.) fold. maps, diagr. ;24 cm.","costCenters":[],"links":[{"id":93418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0577/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0577/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7c3","contributors":{"authors":[{"text":"Richards, Ralph Webster","contributorId":95943,"corporation":false,"usgs":true,"family":"Richards","given":"Ralph","email":"","middleInitial":"Webster","affiliations":[],"preferred":false,"id":214920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mansfield, George Rogers","contributorId":75506,"corporation":false,"usgs":true,"family":"Mansfield","given":"George","email":"","middleInitial":"Rogers","affiliations":[],"preferred":false,"id":214919,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39449,"text":"pp86 - 1914 - The Transportation of Debris by Running Water","interactions":[],"lastModifiedDate":"2018-12-03T09:12:07","indexId":"pp86","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","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":"86","title":"The Transportation of Debris by Running Water","docAbstract":"Scope.-The finer debris transported by a stream is borne in suspension. The coarser is swept along the channel bed. The suspended load is readily sampled and estimated, and much is known as to its quantity. The bed load is inaccessible and we are without definite information as to its amount. The primary purpose of the investigation was to learn the laws which control the movement of bed load, and especially to determine how the quantity of load is related to the stream's slope and discharge and to the degree of comminution of the debris.\r\n\r\nMethod.-To this end a laboratory was equipped at Berkeley, Cal., and experiments were performed in which each of the three conditions mentioned was separately varied and the resulting variations of load were observed and measured. Sand and gravel were sorted by sieves into grades of uniform size. Determinate discharges were used. In each experiment a specific load was fed to a stream of specific width and discharge, and measurement was made of the slope to which the stream automatically adjusted its bed so as to enable the current to transport the load.\r\n\r\nThe slope factor.-For each combination of discharge, width, and grade of debris there is a slope, called competent slope, which limits transportation. With lower slopes there is no load, or the stream has no capacity for load. With higher slopes capacity exists; and increase of slope gives increase of capacity. The value of capacity is approximately proportional to a power of the excess of slope above competent slope. If S equal the stream's slope and sigma equal competent slope, then the stream's capacity varies as (S - sigma)n. This is not a deductive, but an empiric law. The exponent n has not a fixed value, but an indefinite series of values depending on conditions. Its range of values in the experience of the laboratory is from 0.93 to 2.37, the values being greater as the discharges are smaller or the debris is coarser.\r\n\r\nThe discharge factor.-For each combination of width, slope, and grade of debris there is a competent discharge, k. Calling the stream's discharge Q, the stream's capacity varies as (Q - k)o. The observed range of values for o is from 0.81 to 1.24, the values being greater as the slopes are smaller or the debris is coarser. Under like conditions o is less than n; or, in other words, capacity is less sensitive to change3 of discharge than to changes of slope.\r\n\r\nThe fineness factor.-For each combination of width, slope, and discharge there is a limiting fineness of debris below which no transportation takes place. Calling fineness (or degree of comminution) F and competent fineness o, the stream's capacity varies with (F - o)p. The observed range of values for p is from 0.50 to 0.62, the values being greater as slopes and discharges are smaller. Capacity is less sensitive to changes in fineness of debris than to changes in discharge or slope.\r\n\r\nThe form factor.-Most of the experiments were with straight channels. A few with crooked channels yielded nearly the same estimates of capacity. The ratio of depth to width is a more important factor. For any combination of slope, discharge, and fineness it is possible to reduce capacity to zero by making the stream very wide and shallow or very narrow and deep. Between these extremes is a particular ratio of depth to width, p, corresponding to a maximum capacity. The values of p range, under laboratory conditions, from 0.5 to 0.04, being greater as slope, discharge, and fineness are less.\r\n\r\nVelocity.-The velocity which determines capacity for bed load is that near the stream's bed, but attempts to measure bed velocity were not successful. Mean velocity was measured instead. To make a definite comparison between capacity and mean velocity it is necessary to postulate constancy in some accessory condition. If slope be the constant, in which case velocity changes with discharge, capacity varies on the average with the 3.2 power of velocity. If discharge be the constant, in w","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp86","collaboration":"Bases on experiments made with the assistance of Edward Charles Murphy","usgsCitation":"Gilbert, G.K., and Murphy, E.C., 1914, The Transportation of Debris by Running Water: U.S. Geological Survey Professional Paper 86, Report: 263 p.; 3 Plates, https://doi.org/10.3133/pp86.","productDescription":"Report: 263 p.; 3 Plates","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0086/report-thumb.jpg"},{"id":22044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0086/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6735cc","contributors":{"authors":[{"text":"Gilbert, Grove Karl","contributorId":84798,"corporation":false,"usgs":true,"family":"Gilbert","given":"Grove","email":"","middleInitial":"Karl","affiliations":[],"preferred":false,"id":221468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murphy, Edward Charles","contributorId":90286,"corporation":false,"usgs":true,"family":"Murphy","given":"Edward","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":221469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1360,"text":"wsp329 - 1914 - Surface water supply of the United States, 1912, Part IX, Colorado River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","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":"329","title":"Surface water supply of the United States, 1912, Part IX, Colorado River basin","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp329","usgsCitation":"Follansbee, R., Porter, E., and Padgett, H., 1914, Surface water supply of the United States, 1912, Part IX, Colorado River basin: U.S. Geological Survey Water Supply Paper 329, 238 p. :ill. ;24 cm., https://doi.org/10.3133/wsp329.","productDescription":"238 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0329/report-thumb.jpg"},{"id":26442,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69800d","contributors":{"authors":[{"text":"Follansbee, Robert","contributorId":51713,"corporation":false,"usgs":true,"family":"Follansbee","given":"Robert","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, E.A.","contributorId":69529,"corporation":false,"usgs":true,"family":"Porter","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":143633,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Padgett, H.D.","contributorId":79085,"corporation":false,"usgs":true,"family":"Padgett","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":143634,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":45223,"text":"b540T - 1914 - Celestite deposits in California and Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"b540T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"540","chapter":"T","title":"Celestite deposits in California and Arizona","language":"ENGLISH","doi":"10.3133/b540T","usgsCitation":"Phalen, W.C., 1914, Celestite deposits in California and Arizona: U.S. Geological Survey Bulletin 540, 521-533 p., https://doi.org/10.3133/b540T.","productDescription":"521-533 p.","costCenters":[],"links":[{"id":247731,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0540t/report.pdf","size":"1008","linkFileType":{"id":1,"text":"pdf"}},{"id":252081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0540t/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6848d4","contributors":{"authors":[{"text":"Phalen, W. 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The Hawaiian Volcano Observatory (HVO) record books are annual journals in which field observations of eruptive activity at Kīlauea and Mauna Loa volcanoes, on the Island of Hawaiʻi, were compiled by HVO staff for most years from 1912 through early 1966. In addition to descriptive observations, the record books also contain hundreds of annotated photographs and sketches, as well as temperature and transit measurements. When photographs are included, the camera settings and film types used are noted. The field notes, sketches, and photographs used to compile the record books provide an unparalleled record of eruptive activity and were the basis for published newspaper reports and periodic bulletins, such as the Hawaiian Volcano Observatory bulletins and The volcano letter.  

HVO staff also painstakingly prepared a second copy of each early record book, virtually identical to the original, complete with photographs and sketches. The original version of the record book was kept at HVO, while the duplicate went to the Hawaiian Volcano Research Association, which was created by a group of Honolulu, Hawaiʻi, businessmen to promote HVO’s work. The Hawaiian Volcano Research Association, which dissolved decades ago, held the duplicate books in Honolulu, where they were more readily accessible to the public. After 1923, HVO stopped duplicating the books—at least, no duplicate records for subsequent years have been found. During the decade of the 1940s, preparation of the record books stopped altogether. In 1952, compilation of the record books resumed and continued, with long gaps, until early 1966. Entries in these later volumes are sparse, and these books are little more than photo albums of the episodic eruptions of Kīlauea. 

The original record books were held at HVO and, later, at Hawai‘i Volcanoes National Park. In 1972, the original record books for the years 1912 through 1939 were transferred to the Bishop Museum, in Honolulu, for safekeeping. These record books are now stored in archival boxes at that institution (accession number 172.265). The duplicate set of record books held by the Hawaiian Volcano Research Association were bound into volumes at an unknown date and turned over to the U.S. Geological Survey. This set of record books, spanning 1912 through 1923, is now housed in the rare book room of the U.S. Geological Survey Library in Reston, Virginia (catalog number 220(950) H3d). The record books for 1952 through early 1966 remain in storage at HVO. After 1955, typed annotations were no longer placed in the record books, and only photographs, most with captions, were included. Although the volumes titled “Record Book” end with the 1955 volume, the photograph albums that followed are similar, and the record book designation is retained for simplicity. Note that the photographs in these albums were not all originally arranged in chronological order. 

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW"} ,{"id":70261325,"text":"70261325 - 1914 - Plan and profile of North Fork of Santiam River and tributaries above Lyons, Oregon","interactions":[],"lastModifiedDate":"2024-12-06T14:27:34.651606","indexId":"70261325","displayToPublicDate":"1914-01-01T14:26:21","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Plan and profile of North Fork of Santiam River and tributaries above Lyons, Oregon","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70261325","usgsCitation":"Marshall, R., Gerdine, T., and Harrison, R., 1914, Plan and profile of North Fork of Santiam River and tributaries above Lyons, Oregon, 5 Plates: 20.72 x 17.89 inches or smaller, https://doi.org/10.3133/70261325.","productDescription":"5 Plates: 20.72 x 17.89 inches or 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marshall, R.B.","contributorId":18741,"corporation":false,"usgs":true,"family":"Marshall","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":920390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gerdine, T.G.","contributorId":346963,"corporation":false,"usgs":false,"family":"Gerdine","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":920391,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harrison, R.L.","contributorId":346964,"corporation":false,"usgs":false,"family":"Harrison","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":920392,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70268166,"text":"70268166 - 1914 - Hawaiian Volcano Observatory bulletins - 1914","interactions":[{"subject":{"id":70268166,"text":"70268166 - 1914 - Hawaiian Volcano Observatory bulletins - 1914","indexId":"70268166","publicationYear":"1914","noYear":false,"title":"Hawaiian Volcano Observatory bulletins - 1914"},"predicate":"IS_PART_OF","object":{"id":70268164,"text":"70268164 - 1913 - Hawaiian Volcano Observatory bulletins","indexId":"70268164","publicationYear":"1913","noYear":false,"title":"Hawaiian Volcano Observatory bulletins"},"id":1}],"isPartOf":{"id":70268164,"text":"70268164 - 1913 - Hawaiian Volcano Observatory bulletins","indexId":"70268164","publicationYear":"1913","noYear":false,"title":"Hawaiian Volcano Observatory bulletins"},"lastModifiedDate":"2025-06-16T15:01:57.141707","indexId":"70268166","displayToPublicDate":"1914-01-01T10:55:31","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Hawaiian Volcano Observatory bulletins - 1914","docAbstract":"

The Hawaiian Volcano Observatory (HVO) Bulletin series was an informal publication issued between the years 1913 to 1929. Individual issues contain information on volcanic and earthquake activity, volcano research, and volcano monitoring in Hawaii, and issues often included photographs, sketches, and data plots. Information on volcanic activity at other locations is also occasionally included.

The Bulletin series was published by HVO through the Hawaiian Volcano Research Association. Weekly Bulletins (initially called Reports) were issued between June 28, 1913, and July 1, 1914. Bulletins were issued monthly after July 1, 1914, though they were still named Weekly Bulletins until January 1919. Starting with the February 1919 issue, the Bulletins were named Monthly Bulletins, and they continued to be issued monthly until the series ceased in July 1929. During a single year, 1915, Seismometric Bulletins were also issued quarterly. These four issues contain summaries of seismic observations recorded by the then-nascent Whitney Laboratory of Seismology, located underground in a vault near the summit of Kīlauea.

Two of the bulletins are misnumbered:
• April 1916 volume IV no. 4 incorrectly says April 1915 volume III no. 4
• September 1916 volume IV no. 9 incorrectly says September 1916 volume VI no. 9

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\"}}]}","volume":"2","issue":"1-32","noUsgsAuthors":false,"publicationStatus":"PW"} ,{"id":70200436,"text":"70200436 - 1914 - Glaciers of Glacier National Park","interactions":[],"lastModifiedDate":"2018-10-19T09:43:42","indexId":"70200436","displayToPublicDate":"1914-01-01T10:43:23","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Glaciers of Glacier National Park","docAbstract":"

Glacier National Park derives its name and much of its interest from the presence of many small glaciers. Very much of the grandeur of its wonderful Alpine scenery, the final sculpturing of the great mountain valleys and of the amphitheaters at their heads, and the production of the basins of its many beautiful lakes are due to the action of the more extended glaciers of the past.

There are in the park about 90 small glaciers ranging in size from Blackfeet Glacier, with its 3 square miles of ice, down to masses but a few acres in extent yet exhibiting the characteristics of true glaciers. The most easily accessible of these from the beaten trails are the Blackfeet and Sperry Glaciers and the small glaciers at Iceberg Lake and at Ahern Pass. Some of the others can be reached by tourists who are willing to undergo the exertions of mountain climbing. Among these are Grinnell, Chaney, Shepard, Vulture, and Carter Glaciers, and one or two at Brown Pass. (See map facing page 17.)

After examining these features one can easily picture to himself, as he looks down the valleys, the great rivers of ice which in ages past cascaded from the cliffs below the upper cirques, converged as tributaries from the many branch valleys, and united in great trunk glaciers. In imagination lie can see these great glaciers many hundreds of feet ill depth filling the great mountain volleys from side to side, and deploying thence upon the bordering plains. lie seems to see these mighty engines plucking away the rock ribs of the mountains, smoothing, grinding, and polishing the irregularities and sweeping away the debris to be spread on the plains below. These glaciers developed and extended three times and, after each development, the congealed masses melted away on the return of milder climatic conditions, until at length only the small cliff glaciers of the present day are left lurking in the protected recesses at the heads of the capacious valleys. 

Many of the rock-walled amphitheaters are no longer occupied by ice, but from all there issue streams fed by the melting snow or ice. These plunge over the cliffs in beautiful foaming cascades and rush on down the mountain gorges. The melting glaciers left many inclosed basins large and small, and in these the waters rest a while and mirror in their crystal depths the dark green of the surrounding forests, the rich colors of the rugged mountain walls, and the deep blue of the cloud-flecked sky. On again from lake to lake the waters flow and finally start down their long courses to the sea to merge at length with the chill waters of Hudson Bay, the balm t ides of the Gulf of Mexico, or the rolling billows of the Pacific.

Compared in size with the great glaciers of Alaska the glaciers of Glacier National Park are insignificant. They are even surpassed in size by those of the Alps, of the Canadian Rockies, and of Mount Rainier, Washington. They are, however, thought small, among the best examples of this interesting type of phenomena now existing in the United States. They have also a splendid setting in magnificent Alpine scenery, unsurpassed in grandeur anywhere. Hidden away in the recesses of the mighty mountain ranges these rare and wonderful features form a climax to many of the interesting trips open to the tourist.

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