 The foreman at this quarry was in the habit of calling certain sheets, marked by the absence of discoloration, "strain sheets," to distinguish them from the others. At one place a northwest-southeast compressive strain had actually extended the strain...  Bulletin of the United States Geological Survey - Seite 32von Geological Survey (U.S.) - 1907Vollansicht - Über dieses Buch
 | 1907 - 1026 Seiten
...strain. Another instance occurs at the quarry of the New England Granite Works, at Concord, K. II., recently visited by the writer. The foreman at this...sheets, marked by the absence of discoloration, " strain sheets,'1 to distinguish them from the others. At one place a northwest-southeast compressive strain... | |
 | Benjamin Kendall Emerson, Joseph Hartshorn Perry - 1907 - 700 Seiten
...compressive strain. Another instance occurs at the quarry of the Mew England Granite Works, at Concord, NH, recently visited by the writer. The foreman at this...vertical east-west channel 5 feet back of the • Sorby, II. 0., On the microscopic structure of crystals, Indicating the origin of minerals ami rocks: Quart.... | |
 | Thomas Nelson Dale - 1908 - 458 Seiten
...strain. Another instance occurs at the quarry of the New England Granite Works, at Concord, page 148. The foreman at this quarry was in the habit of calling...on a vertical east-west channel 5 feet back of the face, closing up the channel to half its original width. Evidences of compressive strain were also... | |
 | Thomas Nelson Dale - 1908 - 250 Seiten
...strain. Another instance occurs at the quarry of the New England Granite Works, at Concord, page 148. The foreman at this quarry was in the habit of calling...on a vertical east-west channel 5 feet back of the face, closing up the channel to half its original width. Evidences of compressive strain were also... | |
 | Thomas Nelson Dale, Herbert Ernest Gregory - 1911 - 698 Seiten
...compressive strain. Another instance occurs at the quarry of the New England Granite Works, at Concord, NH The foreman at this quarry was in the habit of calling...on a vertical east-west channel 5 feet back of the face, closing up the channel to half its original width. Evidences of compressive strain were also... | |
 | Allan Greenwell, J. Vincent Elsden - 1913 - 620 Seiten
...the fact that at the quarry of the New England Granite Works at Concord, Now Hampshire, the foreman was in the habit of calling certain sheets, marked...strain sheets," to distinguish them from the others. Mr. Dale has carefully examined the various theories which have been advanced in explanation of this... | |
 | 1907 - 1200 Seiten
...strain. Another instance occurs at the quarry of the New England Granite Works, at Concord, N. II., recently visited by the writer. The foreman at this...to distinguish them from the others. At one place a northwest -southeast compressive strain had actually extended the strain sheet about 5 feet, and also... | |
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