Description
Excerpt from Serpentinite and Rodingite in the Hunting Hill Quarry, Montgomery County, Maryland: Description of Rocks Exposed in the Quarry Near the Center of the Hunting Hill Ultramafite
The Hunting Hill serpentinite quarry is 4 miles west of Rockville, Montgomery County, about 17 miles N. 41° W. Of the Capitol in Washington, D.C. By road, the quarry is miles southwest of Maryland Route 28 at its junction with Travilah Road and mile west of Piney Meetinghouse Road, south of its junction with Travilah Road (fig. The quarry is near the center of a serpentinite mass 4 miles long and 1 mile wide, which trends N. 22° E. And is named for the settlement of Hunting Hill near its northeast end. The serpentinite is surrounded by the Wissahickon Formation, the foliation of which generally strikes about N. 20° E. And dip-s steeply to vertically (pl.
The quarry was opened in 1955 after a modest core-drilling pro gram by Rockville Crushed Stone, Inc., and when mapped in 1966 it had a maximum length of feet, an average width of 850 feet, and a maximum depth of approximately 210 feet (pl. The quarry originally was developed and operated in benches on all sides; recent work, however, has been by benching in a southwesterly direction only (fig.
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This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
The Hunting Hill serpentinite quarry is 4 miles west of Rockville, Montgomery County, about 17 miles N. 41° W. Of the Capitol in Washington, D.C. By road, the quarry is miles southwest of Maryland Route 28 at its junction with Travilah Road and mile west of Piney Meetinghouse Road, south of its junction with Travilah Road (fig. The quarry is near the center of a serpentinite mass 4 miles long and 1 mile wide, which trends N. 22° E. And is named for the settlement of Hunting Hill near its northeast end. The serpentinite is surrounded by the Wissahickon Formation, the foliation of which generally strikes about N. 20° E. And dip-s steeply to vertically (pl.
The quarry was opened in 1955 after a modest core-drilling pro gram by Rockville Crushed Stone, Inc., and when mapped in 1966 it had a maximum length of feet, an average width of 850 feet, and a maximum depth of approximately 210 feet (pl. The quarry originally was developed and operated in benches on all sides; recent work, however, has been by benching in a southwesterly direction only (fig.
About the Publisher
Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com
This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Details
Publisher - Forgotten Books
Language - English
Hardback
Contributors
Author
David M. Larrabee
Published Date -
ISBN - 9780331330168
Dimensions - 22.9 x 15.2 x 0.2 cm
Page Count - 39
Paperback
Contributors
Author
David M. Larrabee
Published Date -
ISBN - 9780331018165
Dimensions - 22.9 x 15.2 x 0.2 cm
Page Count - 41
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