2 edition of geologic, geochemical, and sedimentologic study of Flathead Lake, Montana found in the catalog.
geologic, geochemical, and sedimentologic study of Flathead Lake, Montana
A. J. Silverman
by Montana University Joint Water Resources Research Center in [Missoula?
Written in English
|Statement||Principal investigator: Arnold Silverman.|
|Series||Montana University Joint Water Resources Center., Report no. 21, Report (Montana University Joint Water Resources Research Center) ;, no. 21.|
|LC Classifications||QE134.F55 S54|
|The Physical Object|
|Number of Pages||48|
|LC Control Number||73623002|
Hofmann, M.H. et al., Late Pleistocene and Holocene depositional history of sediments in Flathead Lake, Montana; evidence from high-resolution seismic reflection interpretation. Sedimentary Geology , Horodyski, R.J., Sedimentary geology and stromatolites of the Mesoproterozoic belt Supergroup, Glacier National Park, Montana. September to June Visiting Research Scientist at the US Geological Survey, Water Re- source Division, National Research Program, Menlo Park, California ; Professor of Geol- ogy (sabbatical leave), University of Montana, Missoula, MT
Coker, W. B., and I. Nichol, , The relation of lake sediment geochemistry to mineralization in the northwest Ontario region of the Canadian Shield, Econ. Geol – CrossRef Google Scholar. Pubs Warehouse Home > Browse > Report > USGS Numbered Series > IMAP. Browse the USGS Publication Warehouse Flathead, Lake, Lewis and Clark, Missoula, and Powell counties, Montana, , IMAP Geologic map of the Bob Marshall and Great Bear Wildernesses and adjacent study areas, Montana, , IMAP
treatment of the geochemical data. The bedrock was mapped and the samples were collected in and as part of a continuing U.S. Geological Survey project to map basement rocks in the western Chugach Mountains. Most of the early work on the bedrock geology of the Anchorage B-7 quadrangle and the surrounding areas was by S. R. Capps ( Cited by: 3. Geosciences; People; Research Faculty; People. Professors; Research Faculty M.H., Sperling, E.A., , Redox Geochemical Study of the Devonian-Carboniferous Sappington Formation, Southwest Montana: Paleoenvironmental Conditions in the Sappington Formation and Comparison to the Bakken Formation. Abstracts with Programs 51/5, GSA Annual.
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A geologic, geochemical, and sedimentologic study of Flathead Lake, Montana;: Completion report (Montana University Joint Water Resources Center) [Silverman, A. J] on *FREE* shipping on qualifying offers. A geologic, geochemical, and sedimentologic study of Flathead Lake, Montana;: Completion report (Montana And sedimentologic study of Flathead Lake Joint Water Resources Center).
A geologic, geochemical, and sedimentologic study of Flathead Lake, Montana by A. Silverman,Montana University Joint Water Resources Research Center edition, in English. Buy A geologic, geochemical, and sedimentologic study of Flathead Lake, Montana;: Completion report (Montana University Joint Water Resources Center) by A.
J Silverman (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : A. J Silverman. The Flathead lobe of the Cordilleran ice sheet advanced and retreated across the Flathead Valley, a km-long by and sedimentologic study of Flathead Lake basin.
The glacier terminated at the southern end of the Flathead Valley during its last glacial maximum. I used geologic mapping, sedimentologic study, and mapping from descriptive water-well logs to define the stratigraphy of glacial and post-glacial deposits Cited by: Full text of "Geologic, geomorphic and chemical characteristics of wetlands selected for use in biocriteria development by the Montana Department of Environmental Quality" See other formats sMONTANA STATE LIBRARY Nuggc Jl IIIIIIIMIIII Appendix C 3 9 Geologic, Geomorphic and Chemical Characteristics of Wetlands Selected for Use in Biocriteria Development.
The Flathead lobe of the Cordilleran ice sheet advanced and retreated across the Flathead Valley, a km-long by 15–km-wide basin. The glacier terminated at the southern end of the Flathead.
Mercury in Fishes and Their Diet Items from Flathead Lake, Montana. ence of geological formations high in mercur y. other study of Flathead Lake, age-1 and age-2 lake. Montana book The Flathead lobe of the Cordilleran ice sheet advanced and retreated across the Flathead Valley, a km-long by 15–km-wide basin.
The glacier ter. The craggy, rugged topography in the mountains of the Flathead region is a result of the abrasive scouring action of glacial ice, which created the classic deep, straight, U-shaped valleys and knife-like ridges (arêtes), three-sided peaks (horns), and hanging valleys typical of alpine glaciated regions.
Environmental Impact Study for the Flathead River produced (related to the threat of upstream coal mining). Flathead Basin Commission established. Phosphates in detergents banned in Lake and Flathead counties.
Mysis shrimp established in Flathead Lake after being introduced earlier upstream in Whitefish and Swan lakes. University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School Acquisition and evaluation of sedimentologic paleomagnetic and geochemical time -series data from Flathead Lake Montana: Implications for late Pleistocene and Holocene paleoclimate Michael SperazzaAuthor: Michael Sperazza.
Flathead Valley Flathead Valley (Fig. 2) is an elongate intermontane Valley in northwestern Montana. The study area extends from the Mission, Swan and White Fish Mountains on the east and north to the Salish Mountains on the west and to Flathead lake on the by: 1. Located west of the continental divide at the former LGM terminal position of the Flathead Lobe of the Cordilleran Ice Sheet, Flathead Lake (Montana) contains a well preserved record of syn- and post-glacial Quaternary sedimentation.
We have studied this record through a combination of geologic mapping around the lake margins, kHz and lower frequency seismic reflection profiling of lake.
Sedimentary Geology book. Read 2 reviews from the world's largest community for readers. The two primary areas of study - sedimentary rocks and stratigra /5. MS Book and Mineral Company Montana Geology and Mining History Catalog I - Federal Publications / NORTH ABSAROKA STUDY AREA, MONTANA: GEOLOGICAL & GEOCHEMICAL INVESTIGATIONS, GEOPHYSICAL INTERPRETATIONS, ECONOMIC APPRAISAL.
SANDERS, FLATHEAD, & LAKE CO., MONTANA, $ 10 GP / AEROMAGNETIC MAP OF THE PLAINS. Sedimentary Geology is a journal that rapidly publishes high quality, original research and review papers that cover all aspects of sediments and sedimentary rocks at all spatial and temporal scales.
Submitted papers must make a significant contribution to the field of study and must place the research in a broad context, so that it is of interest to the diverse, international readership of.
Geologic units in Flathead county, Montana Additional scientific data in this geographic area Piegan Group: Helena and Wallace Formations (Middle Proterozoic) at surface, covers 24 % of this area. Audio Books & Poetry Community Audio Computers, Technology and Science Music, Arts & Culture News & Public Affairs Non-English Audio Spirituality & Religion Librivox Free Audiobook Flying Up Podcast Podcast Finding Home Podcast Daddy-Long-Legs by Jean Webster ARTE - Mini Tracks Bompopradio 12 fantastiske fortællinger GROOVE MUSIC DJ & PRODUCER.
Langton () called deposits of glaciolacustrine silt and clay deposited in lake-bottom positions throughout the glacial Lake Missoula basin the “Lake Missoula beds.” The original studies of the stratigraphy and geomorphic features formed by rapid lake drainage focused in the northern subbasins, in the areas east and west of Plains, Montana (Pardee,).
Browse the USGS Publication Warehouse Lake and Flathead counties, Montana,Open-File Report Preliminary map showing structural fabric of central Kentucky and part of Ohio,Open-File Report A geological and geochemical reconnaissance of the Tathlith one-degree quadrangle, sheet 19/43, Kingdom of Saudi Arabia.
the Flathead Lake basin and the Mission Valley, Montana, USA. Michael Sperazza,UM Ph.D., Acquisition and evaluation of sedimentologic, paleomagnetic, and geochemical time-series data from Flathead Lake, Montana: Implications for Late Pleistocene and Holocene paleoclimate.CiteScore: ℹ CiteScore: CiteScore measures the average citations received per document published in this title.
CiteScore values are based on citation counts in a given year (e.g. ) to documents published in three previous calendar years (e.g. – 14), divided by the number of documents in these three previous years (e.g. – 14). A geochemical database of 21 lake-sediment samples, analysed for 53 elements by ICP-MS after aqua-regia digestion, has been created.
Statistical tests and plots of the combined data (in some cases, after the application of levelling functions) show that the disharmony that existed previously – between analyses that employed digestions of differing strengths – can be largely : Stephen Amor, Martin McCurdy, Robert Garrett.