4,370 research outputs found
Poems / by M. Betham-Edwards Author Of "The White House By The Sea" ...
No full textPOEMS / BY M. BETHAM-EDWARDS AUTHOR OF "THE WHITE HOUSE BY THE SEA" ...
Poems / by M. Betham-Edwards Author Of "The White House By The Sea" ... (1)
Cover (1)
Title page (3)
Titelseite (5)
Widmung (7)
Note (8)
Contents (11)
Love (15)
Recollection - The Life That Is Life (17)
Religion (83)
The Praise Of Light - L'Envoi (85)
Nature (101)
Child's Summer Song - March Music (103)
Chapter (118)
The Work-A-Day World And Romance (119)
The Wife's Prayer - The English Shipwrecked Off Finistère (121)
Translations (187)
The Gascon's River - Verselets (189
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Crested Saguaro Walter Edwards Cactus
No full textClose up of a Crested Saguaro Walter Edwards Cactu
Invited Discussion on "What Shall We Teach in Environmental Statistics?" By: Walter Piegorsch and Don Edwards
No full text2 pages, 1 article*Invited Discussion on "What Shall We Teach in Environmental Statistics?" By: Walter Piegorsch and Don Edwards* (Altman, Naomi; Sullivan, Patrick) 2 page
Happy gay and debonaire, full of fun [first line of chorus]
No full textstrophic with choruspiano and voiceads on back cover for M. Witmark & Sons11071-6Johns Hopkins University, Levy Sheet Music Collection, Box
148, Item 081Book by Walter Browne. Music by Julian Edwards.Alfred E. Aarons Musical Production Miss Molly May; Grace La Rue as "Miss Molly May"unattrib. photo of Grace La Ru
Happy gay and debonaire, full of fun [first line of chorus]
No full textstrophic with choruspiano and voiceads on back cover for M. Witmark & Sons11071-6Johns Hopkins University, Levy Sheet Music Collection, Box
148, Item 081Book by Walter Browne. Music by Julian Edwards.Alfred E. Aarons Musical Production Miss Molly May; Grace La Rue as "Miss Molly May"unattrib. photo of Grace La Ru
Jonathan Edwards a life
No full text"Jonathan Edwards (1703-1758) is a towering figure in American history. A controversial theologian and the author of the famous sermon Sinners in the Hands of an Angry God, he ignited the momentous Great Awakening of the eighteenth century." "In this biography, Jonathan Edwards emerges as both a great American and a brilliant Christian. George M. Marsden evokes the world of colonial New England in which Edwards was reared - a frontier civilization at the center of a conflict between Native Americans, French Catholics, and English Protestants. Drawing on newly available sources, Marsden demonstrates how these cultural and religious battles shaped Edwards' life and thought. Marsden reveals Edwards as a complex thinker and human being who struggled to reconcile his Puritan heritage with the secular, modern world emerging out of the Enlightenment. In this, Edwards' life anticipated the deep contradictions of our American culture."--BOOK JACKET
Evolution of a Deep Fluid in a Surficial Environment Using Stable Isotopes of Carbon and Sulfur: Case of the Transitional Section of the Edwards Aquifer
No full textThe Edwards Aquifer in south central Texas (USA) features a distinct fault line defining the freshwater and saline water zones. We aim to elucidate the evolutionary behavior of carbon and sulfur emanating from deep environments and flowing in surficial environment so as to better understand the cycling of these metals in water environments. To characterize the evolution of carbon and sulfur species in surficial environment as the fluid emanates from a deep saline aquifer, we monitored the chemical and isotopic (δ13CDIC and δ34SSO4) parameters over a 700-m stretch on a streampond system situated on the saline-freshwater line of the Edwards Aquifer’s artesian zone. A three-tier evolution process associated with the interaction of a deep saline fluid with a fresh-ponded water was observed, namely: A deep fluid control zone characterized by decreasing pH values and relatively high total dissolved solids The Edwards Aquifer in south central Texas (USA) features a distinct fault line defining the freshwater and saline water zones. We aim to elucidate the evolutionary behavior of carbon and sulfur emanating from deep environments and flowing in surficial environment so as to better understand the cycling of these metals in water environments. To characterize the evolution of carbon and sulfur species in surficial environment as the fluid emanates from a deep saline aquifer, we monitored the chemical and isotopic (δ13CDIC and δ34SSO4) parameters over a 700-m stretch on a streampond system situated on the saline-freshwater line of the Edwards Aquifer’s artesian zone. A three-tier evolution process associated with the interaction of a deep saline fluid with a fresh-ponded water was observed, namely: A deep fluid control zone characterized by decreasing pH values and relatively high total dissolved solid
Best Management Practices and Standards, Training, and Tools to Increase Resilience of the Edwards Aquifer Water Supply During Emergency Fire Control
No full textIn 2019 the Institute for Water Resources Science and Technology at Texas A&M University-San Antonio began work funded by the Proposition 1 Edwards Aquifer Protection Venue Project to develop Best Management Practices (BMPs) for protecting Edwards Aquifer water supplies from inadvertent contamination by HAZMAT in water runoff during emergency response-related firefighting. Results of this work are now available for your use. Technical information is available for use in developing and updating emergency response planning documents (i.e., City of San Antonio Hazard Mitigation Action Plan and the Bexar County Emergency Management Plan), educational curricula can be used for training and public outreach, and BMPs along with associated tools are now available for on-site and post-event management and hazard mitigation. These have been developed for use in Bexar County and other areas where the aquifer is susceptible to contamination from disaster response on the land’s surface.https://digitalcommons.tamusa.edu/water_books/1008/thumbnail.jp
Geology of the West Flower Garden Bank
No full textIncludes bibliographical references (pages 183-196)"December 1971""This publication is partially supported by the National Sea Grant Program, National Oceanic and Atmospheric Administration within the United States Department of Commerce, through an institutional grant made to Texas A & M University"The West Flower Garden Bank, located on the outer edge of the Texas-Louisiana continental shelf at longitude 93°49.0' west and latitude 27°52.6' north, was investigated with respect to the subsurface structure of the pre-reef pinnacle, the environment currently surrounding the pinnacle and the carbonate sediments being deposited on the bank. Based on previous gravity work and on 3.5 kHz, 1 cubic inch air gun and bathymetric profiles taken during this survey, the topographic high is shown to have been formed by the intrusion of a shallow salt plug. The central section of the dome is a collapsed area, flanked on the east, west and north by banks rising to within 10.5 fms (19 m) of the surface. Based on erosional and depositional surfaces of the bank, stillstands of the Gulf of Mexico waters during the last transgression were at 67-73 fms (121-134 m) sometime prior to 18,000 years B.P.; 40-45 fms (73-82 m) at 17,000-15,000 years B.P.; 48-50 fms (89-90 m) at 14,000-13,000 years B.P. and 28 fms (51 m) 13,000-12,000 years B.P. The Holocene sediments of the bank are (1) a Diploria-Montastrea-Porites Facies from 10.5 fms (19 m) to 27 fms (50 m); (2) a Coral Detritus Facies that interfingers with the Diploria-Montastrea-Porites Facies at 17 fms (31 m) and the Gypsina-Lithothamnium Facies at 27 fms (50 m); (3) a Gypsina-Lithothamnium Facies from 25 fms (46 m) to 40-45 fms (73-82 m ); (4) the 1st Transition Facies from 28 fms (51 m) to 50 fms (91 m ); (5) an Amphistegina Facies from 40 fms (70 m) to 55 fms (100 m ); (6) the 2nd Transition Facies between the Amphistegina and Quartz-Planktonic Foraminiferal Facies; and (7) a Quartz-Planktonic Foraminiferal Facies from 50 fms (91 m) to the surrounding shelf. ..
(SNP021) Walter Carter interviewed by Ken Steeber, with Walter Smith, Gloria Updike and Howard Struthers, transcribed by Victoria M. Edwards
No full textRecords the reminiscences of Walter Carter, whose family owned apple orchards on Dickey Ridge, just south of Front Royal, Virginia, in the decades preceding the establishment of Shenandoah National Park. Describes the physical layout of the the orchards and surrounding towns. Discusses the demise of the apple industry in that part of the Shenandoah Valley due to a shrinking work force, as local families were evicted by the state to make room for the park. In the years prior to the Second World War, the primary customer for the Carter\u27s apples, the United Kingdom, placed restrictive tariffs on U.S. grown apples which made it impossible to compete with fruit from Canada and New Zealand. The second part of the interview consists of a driving tour of the orchard area, with Mr. Carter describing the former locations of buildings, roads, home sites and cemeteries. The group is joined by Mr. Carter\u27s wife, Caroline Carter, whose own recollections and comments are included in the discussion. The Carters make numerous references to local families and landowners. Includes comments on the construction of Skyline Drive, which, while providing north-south access along the crests of the Blue Ridge Mountains, resulted in the closing of numerous east-west routes across the mountains.https://commons.lib.jmu.edu/snp/1121/thumbnail.jp
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