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Great Salt Lake- An Overview of a Brine Resource 大盐湖-一种盐水资源概述
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-1_69
J. A. Whelan
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引用次数: 0
Mt. Olympus Cove Environmental Geology Study: An Alluvial Fan Case History 奥林匹斯山湾环境地质研究:一个冲积扇案例历史
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-1-1_21
B. Kaliser
{"title":"Mt. Olympus Cove Environmental Geology Study: An Alluvial Fan Case History","authors":"B. Kaliser","doi":"10.34191/ug-1-1_21","DOIUrl":"https://doi.org/10.34191/ug-1-1_21","url":null,"abstract":"This environmental geology study of the Mt. Olympus Cove area is largely the result of concerns of Salt Lake County as expressed by the chairman of the County Commission and reiterated by the County Planning Commission, County Intergovernmental Relations Office, and the County Offices of Planning and Zoning, Surveyor, BUilding Inspection, and Flood Control. These concerns were shared by an ad hoc body constituted by the County Office of Intergovernmental Relations and consisting of technical representatives from the various county offices, Utah Geological and Mineral Survey, Utah Division of Forestry, Utah State Water Laboratory, U. S. Forest Service, U. S. Soil Conservation Service, and the U. S. Army Corps of Engineers. Meetings of the ad hoc committee led to the awarding of two contracts: the Utah Geological and Mineral Survey was to study all aspects of the terrain that might have some bearing upon the future course of development of the study area, and the Utah State Water Laboratory was to evaluate the surface water hydrology of the study area. The two contractors were charged with acquiring all available data before development of original information relevant to their responsibilities. It was intended that the report of each contractor should complement the report of the other for the purpose of establishing an overall development plan for the Mt. Olympus Cove area.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"11 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128085131","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Primary and Secondary Sedimentary Structures in Oil Shale and Other Fine-grained rocks, Green River Formation (Eocene), Utah and Colorado 美国犹他州和科罗拉多州始新世绿河组油页岩和其他细粒岩的原生和次生沉积构造
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-1_49
R. Cole, M. Picard
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引用次数: 7
Earthquake Activity in Utah May through December, 1973 1973年5月至12月犹他州的地震活动
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-1-1_91
{"title":"Earthquake Activity in Utah May through December, 1973","authors":"","doi":"10.34191/ug-1-1_91","DOIUrl":"https://doi.org/10.34191/ug-1-1_91","url":null,"abstract":"","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"14 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123620694","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Detailed Magnetic Surveys in the Star Range, Beaver County, Utah 犹他州比弗县恒星范围的详细磁测量
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-1-1_51
J. Schmoker
{"title":"Detailed Magnetic Surveys in the Star Range, Beaver County, Utah","authors":"J. Schmoker","doi":"10.34191/ug-1-1_51","DOIUrl":"https://doi.org/10.34191/ug-1-1_51","url":null,"abstract":"Vertical-field ground magnetic data were obtained in four areas of the Star Range, and interpreted in terms of causative geologic structures. Eight magnetic profiles were taken over the Milford Flat intrusive body, and provided the basis for interpreting the intrusive structure under the alluvium. Gridded magnetic data were obtained in the vicinity of the Wild Bill mine. No extensive zones of contact mineralization are apparent in this data; an anomaly in the south-central portion of the grid is attributed to an upward protrusion of the local intrusive body. Along the southeastern contact of the Shauntie intrusive body, magnetic data show four areas of appreciable magnetite mineralization ranging from eight to twenty-five feet thick. Data collected south of the exposed Shauntie intrusive show an anomaly of uncertain origin that probably reflects the buried southeastern contact zone.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"512 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123570337","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
A Comparison of Models for Flow Through the Causeway, Great Salt Lake, Utah 犹他州大盐湖堤道水流模型的比较
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-2_125
J. A. Whelan, C. Petersen
{"title":"A Comparison of Models for Flow Through the Causeway, Great Salt Lake, Utah","authors":"J. A. Whelan, C. Petersen","doi":"10.34191/ug-2-2_125","DOIUrl":"https://doi.org/10.34191/ug-2-2_125","url":null,"abstract":"Both scientific and economic importance is attached to knowledge of the mechanism and quantity of brine flow through a rock-fill causeway in Great Salt Lake, Utah. Several mathematical models have been devised to describe the flow and also the characteristics of south arm brines. Among these models, the most useful is the Waddell-BoIke digital computer model, which is based on the total hydrology of the lake.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"43 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125719123","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Relict Patterned Ground, Bear River Range, North-Central Utah 残存的图案地面，熊河山脉，中北部犹他州
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-3-2_111
J. Degraff
{"title":"Relict Patterned Ground, Bear River Range, North-Central Utah","authors":"J. Degraff","doi":"10.34191/ug-3-2_111","DOIUrl":"https://doi.org/10.34191/ug-3-2_111","url":null,"abstract":"In the Bear River Range, northcentral Utah, thirty-nine widely distributed localities of three acres or larger show a morphology resembling periglacial patterned ground. In the total of 2,359 acres (954 ha) under study, aerial photographs reveal an arrangement of mounds by an alternately dark and light pattern. The mounds are evenly distributed on slopes of less than 10 percent and aligned in beaded stripes on slopes of more than 10 percent. The mounds range from 13 to 66 feet (4 to 20 m) across; the average mound diameter is about 40 feet (12 m). Only regolith is affected by the patterned morphology. The regolith in and between the mounds is derived from the same source, but the parent material varies among different localities. The location of patterned areas appears to be controlled by temperature and soil. Temperature is the primary factor. Slope aspect, potential insolation, average elevation, and amount of terrain affected correlate for different localities. These factors interact to produce approximately the same average annual, summer, and winter temperatures in patterned ground areas. The patterned ground is located where the controlling temperature coincides with the appropriate soil. Twenty-two areas of patterned ground are within the boundaries of a recent soil survey. An analysis of the soils suggests that patterned ground genesis is facilitated by soils with significant silt and clay components. Some soils affected by patterned morphology have large amounts of stones and cobbles. The evidence of erosion subsequent to formation indicates that patterned areas did not originate under present climatic conditions. During Pleistocene glacial periods, the calculated average annual temperature at these localities was 32°F. Differential frost heaving during the cooler periods of the Pleistocene is suggested as the process responsible for the creation of patterned morphology in the Bear River Range.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"30 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133086489","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Cretaceous Foraminifera from the Mule Ear Diatreme, San Juan County, Utah 犹他州圣胡安县白垩纪Mule Ear Diatreme的有孔虫
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-1-1_93
A. Mcgugan
{"title":"Cretaceous Foraminifera from the Mule Ear Diatreme, San Juan County, Utah","authors":"A. Mcgugan","doi":"10.34191/ug-1-1_93","DOIUrl":"https://doi.org/10.34191/ug-1-1_93","url":null,"abstract":"On a recent Four Corners Geological Society field trip down the San Juan River, Utah, samples containing Gryphaea newberryi were collected from Cretaceous strata in the Mule Ear Diatreme (StuartAlexander, et al., 1972; Ellingson, 1973). The diatreme is located in the south-central part of T. 41 S., R. 20 E., San Juan County, Utah.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"55 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129321043","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
A Second New Theropod Dinosaur from the Late Jurassic of East Central Utah 犹他州中东部晚侏罗世发现的第二种新兽脚亚目恐龙
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-3-1_51
J. Madsen
{"title":"A Second New Theropod Dinosaur from the Late Jurassic of East Central Utah","authors":"J. Madsen","doi":"10.34191/ug-3-1_51","DOIUrl":"https://doi.org/10.34191/ug-3-1_51","url":null,"abstract":"Marshosaurus bicentesimus (Reptilia: Saurischia), a new theropod dinosaur from the Late Jurassic Morrison Formation of east central Utah, is distinct from other Morrison theropods, Allosaurus, Ceratosaurus, and Stokesosaurus, of the Cleveland-Lloyd Dinosaur Collection in the unusual character of the type specimen, a left ilium, and in the referred materials, which include the toothbearing elements of the skull and jaw and the complete pelvic girdle. A relatively complete, articulated skeleton of Marshosaurus is unknown at this time.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127446513","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 33
The Boundary Between Uintah and Grand Counties, Utah 犹他州犹他和大县之间的边界
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-4-1_49
H. Ritzma
{"title":"The Boundary Between Uintah and Grand Counties, Utah","authors":"H. Ritzma","doi":"10.34191/ug-4-1_49","DOIUrl":"https://doi.org/10.34191/ug-4-1_49","url":null,"abstract":"The boundary between Uintah and Grand Counties in the area immediately west of the Utah-Colorado boundary is shown in many ways on published maps. U. S. Geological Survey topographic map, Jim Canyon Utah-Colorado quadrangle, 1970, shows the boundary as defined in the Utah Code.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"14 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126820337","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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