164,568 research outputs found
[Letter from Jeaneite T. O'Shea to Sheppard W. King, III - June 29, 1977]
No full textLetter from Jeaneite T. O'Shea to "Miss" Sheppard King, replying to a telegram from King. O'Shea explains that she would like to move out of her current apartment, which she shares with a person much older than she, and is seeking to possibly share an apartment with King
King, Howell T., October 26, 2010 [Interview]
No full textHowell T. King was interviewed on October 26, 2010, by Nicholas Oristian about his experiences during and after World War II.Williams, Ted; Kimmel, BillWorld War I
[Envelope from Jeaneite T. O'Shea to Sheppard W. King, III - June 29, 1977]
No full textEnvelope from Jeaneite T. O'Shea addressed to Srta. Sheppard King in Madrid
[Letter from Sheppard W. King, III to John J. Herrera - 1977]
No full textLetter from Sheppard W. King, III to John J. Herrera, asking "Johnnie" to forward a letter onto John Michael Herrera, who can reply to Jeaneite T. O'Shea. King also asks for a copy of the letter to show his friends for a good laugh while drinking
P-T-t-d evolution paths within the Gander Zone, NE Newfoundland
No full textThe Gander Lake Subzone of northeast Newfoundland preserves a complex tectonothermal evolution
resulting from continental collision of Gondwana and Laurentia following closure of the Iapetus
ocean. Field, petrographic, geothermobarometric studies and isotopic age data define five northeastsouthwest trending domains, each with a characteristic P-T-t-d evolutionary path, which reveal
elements of the overall tectonothermal evolution in this sector of the Appalachians.
Domain I preserves deformed low grade metasediments and east vergent flat-lying 02 folds formed at
c. 470 Ma. Domain 2 preserves focusing of later progressive deformation (D3wEST) into a steep, predominantly sinistral high strain zone characterised by andalusite ~ kyanite ~ sillimanite indicative of a clockwise metamorphic path (peak conditions c. 650°C, 5.5 kbar). In domain 3, deformed metasediments (D2-D3EAsT) display an eastward increase in structural complexity and metamorphic grade to a peak of c. 600°C. Domain 4 displays progressive amphibolite facies deformation (D3EAsT) characterised by prograde andalusite ~ sillimanite-bearing (c. 425 Ma) migmatites with peak conditions of c. 700°C, 4.5 kbar. Retrograde 04 deformation and
metamorphism is concentrated in steep narrow high strain zones. S4WES~amphibolite to greenschist
facies shear fabrics (predominantly dextral) overprint prograde fabrics (S3WEST)within domain 2 and
are cross-cut by the c. 427 Ma Middle Brook Granite, Locally in domains 3 and 4 prograde (D3EAsT)
fabrics are overprinted by amphibolite to upper greenschist facies S4EAST fabrics which also form the
dominant fabric in c. 417 Ma syntectonic granites. D5-06 retrogressive deformation is pervasive in a
c. 2 km wide mylonitic zone adjacent to the Dover Fault. D5 dextral greenschist-facies ductile
structures are cut by the c. 385 Ma Newport Granite which in tum is cut by 06 sub-greenschist facies
brittle dextral faults.
In combination, the domains preserve A) low grade deformation (Ordovician?) associated with easterly thrusting of the Dunnage Zone over the Gander Zone, B) Silurian rIletamorphism and deformation progressively partitioned into high strain zones and, C) Devonian retrograde ductile-brittle shearing and brittle faulting local to the Dover Fault. The spatial and temporal coincidence of transpressive deformation, moderate to high grade metamorphism and voluminous granite magmatism in the east portion of the Gander Zone is taken to relate to sinistrally oblique collision between two major crustal blocks during the Silurian. Devonian reactivation juxtaposed part of the high grade Gander Zone against the low grade Avalon block across the brittle-ductile Dover Fault
King, Hannah T.
No full textKing, Hannah T. (1809-1886) Wife of Thomas King. Author of "Women\u27s Exponent." Born near Cambridge, England
Letter from I. A. King, Vicksburg, Mississippi, to brother, March 21, 1862
No full textI. A. King was a soldier wounded in or around Vicksburg, Mississippi in March 1862. He writes his brother to request money for tobacco and other necessaries. One page is written on the back of a print of the song, Run, Yank, or Die, composed by T. W. Crowson of the Alabama Hickories
An article on well-known author Stephen King and his wife, author Tabitha King,
No full textAn article on well-known author Stephen King and his wife, author Tabitha King, native Mainers who live in Bangor and focus their low-profile philanthropy locally. Their many beneficiaries include Eastern Maine Medical Center, the Bangor and Old Town libraries, Bangor\u27s new Shawn T. Mansfield Baseball Stadium, area swimming pools, and the University of Maine, where both attended college. They have bought a local radio station to preserve local high-school and college sports coverage. Though wealthy enough to live anywhere, and despite King\u27s fame, they have chosen to raise their family in Bangor and live as regular members of the community. Headquarters for King\u27s fans is Betts Bookstore on Main Street
Citizenship Ceremonies in Spanish? Election Ballots in Chinese? (Dear Colleague letter from New York congressman Peter T. King)
No full textDear Colleague letter, July 30, 1996, from Peter T. King (New York congressman) in support of H.R. 123 - Bill Emerson English Language Empowerment Act of 1996 (Sam did not support this).https://digitalcommons.csumb.edu/samfarr_issues/1008/thumbnail.jp
Letter from Richard King to Isaac Partridge, 24 August 1827
No full textRichard T. King writes from Charleston, South Carolina, to Mr. [Newton?] Partridge (probably referring to Isaac N. Partridge) in Middletown, Connecticut, regarding the belongings and account of Hawkins King, a student at the American Literary, Scientific, and Military Academy in Middletown, Connecticut; please pack up and send Hawkins' clothing.Transcription by Raymond Bouchard. Transcriptions may be subject to error
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