Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Irene B. Boland"'
Autor:
Piecuch, Jim
Publikováno v:
The North Carolina Historical Review, 2019 Jan 01. 96(1), 106-107.
Externí odkaz:
https://www.jstor.org/stable/45184993
Autor:
Gabriel, Michael P.
Publikováno v:
The South Carolina Historical Magazine, 2017 Jul 01. 118(3), 227-229.
Externí odkaz:
https://www.jstor.org/stable/45238240
Autor:
Aaron J. Palmer
Publikováno v:
Journal of Southern History. 84:710-711
Autor:
Palmer, Aaron J.
Publikováno v:
Journal of Southern History; July 2018, Vol. 84 Issue: 3 p710-711, 2p
Autor:
Robert M. Dunkerly, Irene B. Boland
An in-depth analysis of one of the War for Independence's bloodiest and least understood conflicts.The Battle of Eutaw Springs took place on September 8, 1781, and was among the last in the War of Independence. It was brutal in its combat and reprisa
Autor:
Issac D. Standard, Willis E. Hames, James P. Hibbard, Irene B. Boland, Sarah B. Lavallee, John S. Allen, Brent V. Miller
Publikováno v:
Geological Society of America Bulletin. 124:643-656
The Gold Hill shear zone is the most prominent pre-Carboniferous structure in the Southern Appalachian peri-Gondwanan tract of Carolinia. Common perception, based on indirect evidence, holds that it is an Acadian, dextral strike-slip shear zone. Howe
Autor:
Charles A. Boland, Irene B. Boland
Publikováno v:
Studies in Military Geography and Geology ISBN: 9781402031045
Atlantic Coastal Plain geology impacted Continental and British strategy in many ways prior to the Battle of Eutaw Springs during summer 1781. The elevation of the Upper Coastal Plain High Hills of Santee influenced General Nathanael Greene to encamp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2559f7bd3a7ac15417afe5409297f9c
https://doi.org/10.1007/978-1-4020-3105-2_11
https://doi.org/10.1007/978-1-4020-3105-2_11
Publikováno v:
Geology. 23:621
Detailed field mapping at the east end of the Pine Mountain terrane in central Georgia indicates that the Box Ankle fault is an ∼4-km-thick ductile shear zone separating Grenvillian basement of Laurentian affinity in the footwall from allochthonous
Publikováno v:
American Historical Review. Oct2017, Vol. 122 Issue 4, p1369-1382. 14p.