37 research outputs found
mcbooki014: Pioneer Honor Roll (cont.)
No full textPIONEER HONOR ROLL Coombs, Mark A. Fennemore, George H. Coombs, John Henderson, John Clayton, Frank Hawkins, Williams Davis, John M. Huntsman, James W. Davey, George Howd, Simeon Jr. Dean, John Fennemore, Samuel Dean, William Fernley, Edward Dean, Heber C. Goff, Joseph Dean, Jedidiah Gale, Henry Davis, Edward Gale, Henry C. Evans, William Gale, James Elmer, Elijah Greenwood, William Sr. Edwards, Samuel J. Gray, Samuel Edwards, Robert Gibson, James Edwards, William Grimshaw, Duckworth Evans, George P. Gillies, Robert J Farrer, James Gillies, Ebenezer Farnsworth, Philo T. Sr. Gillies, Robert Farnsworth, Philo T. Jr. Gillies, Daniel S. Farnsworth, Alphonzo M. Gdodwin, Albert Farnsworth, Franklin D. Goodwin, Issac Farnsworth, William H. Greenwood, William Jr. Fowler, Hyrum Greenwood, Nathan. Fowler, Moroni Greenwood, Adam Fotheringham, William Greenwood, Titus Fotheringham, John Grimshaw, John Sr. Fotheringham, Robert J. Howd, Simeon F. Field, Joseph S. Huntington, Joseph Frazer, Thomas Hunt, John Frazer, David I. Hoopes, Elisha Fennemore, James Hoopes, James E
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Beach foreshore response to long-period waves in the swash-zone
No full textA field experiment designed to test the hypothesis that infragravity and lower frequency waves influence the patterns of erosion and deposition on the beach foreshore has been carried out. The data show coherent fluctuations in the foreshore sediment level which can be related to low frequency wave motions. The fluctuations have heights of up to 6 cm with typical time scales of 8 to 10 minutes. They can be characterized in two ways: by the progression of the fluctuations up the foreshore slope (landward), and by the decrease in the RNS height of the fluctuations as they progress landward. The velocity of migration also changes as the fluctuations progress landward. Analysis of runup time series obtained by time-lapse photography concurrent with the sediment level measurements reveals long-period waves of undetermined origin at frequencies and phases which strongly suggest that the waves force the original perturbation in sediment level. In order to better understand the characteristics of these sediment level fluctuations, a numerical model of sediment transport on the foreshore has been developed. Gradients in sediment transport define erosional and depositional areas on the foreshore. Runup velocities were modeled and the results were used in the sediment transport model. The model predicts that any perturbation in foreshore elevation will progress landward while decreasing in amplitude and in velocity, thereby matching the field observations. Relationships between beach slope and the profile response clarified by this model are used to explain the initial formation of the perturbations of sediment level
Development of the Chromium Public Health Goal
No full textThis site features a presentation about the development of a public health standard for chromium in drinking water in California. The presentation includes useful information about chromium availability, toxicity, and carcinogenic effects. Educational levels: Graduate or professional
(Table T7) Grain size, calcium carbonate and total organic carbon composition of ODP Hole 182-1131A
No full textSediment depth is given in mbsf. Note that exact distinctions of gravel and clay fraction were not given by the author
19740403 Metropolitan Apr 3 1974
No full textVol. 15, No. 22; Weekly edition; April fool's edition. Items scanned from microfilm of varying quality--some editions are difficult to read, mostly from 1972-1974
(Table T8) Grain size, calcium carbonate and total organic carbon composition of ODP Hole 182-1127B
No full textSediment depth is given in mbsf. Note that exact distinctions of gravel and clay fraction were not given by the author
