{"pageNumber":"5940","pageRowStart":"148475","pageSize":"25","recordCount":165658,"records":[{"id":16315,"text":"ofr65163 - 1965 - Palynological investigations in the Upper Cretaceous and Tertiary of the Mississippi Embayment Region - I","interactions":[],"lastModifiedDate":"2017-05-19T18:30:49","indexId":"ofr65163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-163","title":"Palynological investigations in the Upper Cretaceous and Tertiary of the Mississippi Embayment Region - I","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65163","usgsCitation":"Tschudy, R.H., 1965, Palynological investigations in the Upper Cretaceous and Tertiary of the Mississippi Embayment Region - I: U.S. Geological Survey Open-File Report 65-163, 63 p. ;29 cm., https://doi.org/10.3133/ofr65163.","productDescription":"63 p. ;29 cm.","costCenters":[],"links":[{"id":149671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68968e","contributors":{"authors":[{"text":"Tschudy, Robert H.","contributorId":67879,"corporation":false,"usgs":true,"family":"Tschudy","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":172614,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16316,"text":"ofr65164 - 1965 - Palynological investigations in the Upper Cretaceous and Tertiary of the Mississippi Embayment Region - II","interactions":[],"lastModifiedDate":"2022-09-30T23:08:33.238092","indexId":"ofr65164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-164","title":"Palynological investigations in the Upper Cretaceous and Tertiary of the Mississippi Embayment Region - II","docAbstract":"

As a part of the cooperative mapping project between the Kentucky Geological Survey and the U. S. Geological Survey, a study of Cretaceous and Tertiary spores and pollen assemblages has been undertaken to aid in distinguishing formations and to facilitate surface and subsurface correlations of strata.

Reports completed from January 1, 1965 to the end of June 1965 are included in this report; others will be placed in open-file as they are completed and released for general use.

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fluorite and beryllium deposits, Lost River area, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr65143","usgsCitation":"Sainsbury, C., 1965, Planetable maps and drill logs of fluorite and beryllium deposits, Lost River area, Alaska: U.S. Geological Survey Open-File Report 65-143, 38 p. ill. 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Additional supplies of water are available near the municipalities on the central Mesabi Iron Range. Ground water presents the greatest potential yield, and most of the productive aquifers are in the Biwabik Iron-Formation and the stratified glacial drift. /k single body of ice-contact stratified drift underlies parts of all but one of the five municipality areas mapped. Surface-water supplies are generally inadequate. The Two River system in the eastern part of the area of this report offers some possibilities. Flow data from one discharge station and one miscellaneous gaging site are presented.

\n

Analyses of water from many sources are presented as are data from many wells and test holes. Ground water commonly has a concentration of high iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored.

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This report describes the most outstanding floods in the United States during 1960. No major floods occurred during the year, although two floods caused severe damage the first in March and April in eastern Nebraska and adjacent areas, and the second in September in Puerto Rico.

Unseasonal rains in mid-March caused extensive flooding in north-central Florida. Several thousand persons were evacuated from their homes, and damage to homes, roads, and crops was extensive.

The most widespread flooding ever known in Nebraska occurred late in March and early in April as a result of rapid melting of a heavy snow cover. Most of the flood damage, estimated at about $3 million, was to roads and bridges. The flood area extended into South Dakota, Iowa, Kansas, Missouri, and Wisconsin.

Snowmelt in April supplemented by rains and later heavy rains in early May caused severe flooding in northern Wisconsin and in Michigan Upper Peninsula.

The most destructive flood of the year was in eastern Puerto Rico as the result of hurricane Donna. More than one hundred persons died, and considerably more than one hundred persons were injured; property damage was f.bout $7 million. Hurricane Donna also caused severe flooding as it passed over Florida and along the Atlantic coastline.

In addition to these floods mentioned, 31 others of lesser magnitude were significant enough to report in this annual summary.

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Additional supplies of water are available near the municipalities on the western Mesabi Iron Range. Potential yields from both ground-water and surface-water sources are good. The most productive aquifers for ground-water supplies are the Biwabik Iron-Formation and the stratified glacial drift. Areas of stratified drift believed to have good water potential have been outlined. The most abundant surface-water supplies in the area of this report are from the Mississippi River and its tributaries.

\n

The ground water is generally hard and has a high concentration of iron and manganese. The surface water is generally high in iron and is colored. Analyses of water from many sources are included.

\n

Data from many wells and test holes are given as are flow data for two discharge stations.

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Off.,","doi":"10.3133/wsp1948","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1963, Parts 3 and 4, Ohio River basin and St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1948, x, 390 p. ;23 cm., https://doi.org/10.3133/wsp1948.","productDescription":"x, 390 p. ;23 cm.","costCenters":[],"links":[{"id":136095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1948/report-thumb.jpg"},{"id":24801,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1948/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651bee","contributors":{"authors":[{"text":"Love, S. 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Additional supplies of water are available near the municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range. On the eastern Mesabi Range the potential for additional development of both ground-water and surface-water supplies are good, and on the Vermilion Range the best potential for development is from surface-water resources.

\n

The most productive aquifers in the area of this report are the Biwabik Iron-Formation and the stratified glacial drift; Bast of Colby Lake the Biwabik Iron-Formation is not an important aquifer, and it is entirely absent on the Vermilion Range. Also, on the Vermilion Range the glacial drift is generally too thin to yield the quantities of water found on the Mesabi Range.

\n

Surface-water supplies in the area of this report are good. An extensive network of river systems and many lakes form a large untapped potential supply. Records of flow from eight gaging stations are presented as are data from many wells and test holes.

\n

Ground water commonly has a high concentration of iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored. Analyses of water from many sources are included.

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