A Report on the Limestones and Marls of the Coastal Plain of Georgia

J. E. Brantly

Verlag: The Blosser Company, 1916
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Book is in Good condition with brown boards and gilt lettering. Moderate foxing and darkening to textblock. Slight bumping to edges/corners & head/tail of spine and edgewear. Some white spotting to boards (more severe on back). Foxing to pastedowns and flyleafs. Fold-out map is intact. No jacket. A tight copy. 300 pgs. 4to - over 9¾" - 12" tall. Buchnummer des Verkäufers

Bibliografische Details

Titel: A Report on the Limestones and Marls of the ...
Verlag: The Blosser Company
Erscheinungsdatum: 1916
Einband: Hard Cover
Zustand: Good

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Brantly, J. E.
Verlag: The Blosser Co GA 1916 (1916)
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Buchbeschreibung The Blosser Co GA 1916, 1916. Softcover. Zustand: G. Zustand des Schutzumschlags: na. G na Softcover Some rubbing & edgewear; some splits & chips at spine; yellowing; text overall clean; includes fold-out map; 300 pages. Bestandsnummer des Verkäufers 12429

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Brantly, J. E.
Verlag: Geological Survey of Georgia, Atlanta, GA (1916)
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Buchbeschreibung Geological Survey of Georgia, Atlanta, GA, 1916. Hard Cover. Zustand: Very Good. Zustand des Schutzumschlags: No Dust Jacket. Ex-library not circulated. (10)300pp. Index. Fold-out map. Photo plates. Text illustrations. Attractive original cloth. Size: 8vo - over 7¾ - 9¾" Tall. AMERICAN HISTORY. Bestandsnummer des Verkäufers 079341

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J E Brantly
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ISBN 10: 1528203860 ISBN 13: 9781528203869
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Buchbeschreibung Forgotten Books, 2017. Paperback. Zustand: New. Language: English . Brand New Book ***** Print on Demand *****. Excerpt from A Report on the Limestones and Marls of the Coastal Plain of Georgia The region is a comparatively low plain sloping gently to the southeast. The highest elevations are along the Fall Line where they vary from 500 to 700 feet above sea level. A Slope of 3 or 4 feet per mile is general from this line to the Atlantic Coast. Although, when compared with the topography of those areas north of the Fall Line, the surface relief is slight it is not without distinctive features. The most notable topographic feature is that belt along the Fall Line known as the Fall Line Hills. This belt extends entirely across the State with a width varying from 30 to 40 miles, with the Fall Line the northern boundary. This area has a maximum relief of about 350 feet, considering the larger streams as the base, which shows a much more mature topography than the portion of the plain to the south. Cretaceous sands and clays, the principal materials underly ing the area, are easily eroded and have caused deep gullies and washes throughout the belt. To the north the Fall Line Hills merge into the Crystalline area and to the south into the Dougherty Plain, another distinctive topographic feature of the Coastal Plain. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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. Bestandsnummer des Verkäufers AAV9781528203869

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Buchbeschreibung Forgotten Books, 2017. Paperback. Zustand: New. Language: English . Brand New Book ***** Print on Demand *****.Excerpt from A Report on the Limestones and Marls of the Coastal Plain of Georgia The region is a comparatively low plain sloping gently to the southeast. The highest elevations are along the Fall Line where they vary from 500 to 700 feet above sea level. A Slope of 3 or 4 feet per mile is general from this line to the Atlantic Coast. Although, when compared with the topography of those areas north of the Fall Line, the surface relief is slight it is not without distinctive features. The most notable topographic feature is that belt along the Fall Line known as the Fall Line Hills. This belt extends entirely across the State with a width varying from 30 to 40 miles, with the Fall Line the northern boundary. This area has a maximum relief of about 350 feet, considering the larger streams as the base, which shows a much more mature topography than the portion of the plain to the south. Cretaceous sands and clays, the principal materials underly ing the area, are easily eroded and have caused deep gullies and washes throughout the belt. To the north the Fall Line Hills merge into the Crystalline area and to the south into the Dougherty Plain, another distinctive topographic feature of the Coastal Plain. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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. Bestandsnummer des Verkäufers AAV9781528203869

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J E Brantly
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Buchbeschreibung Forgotten Books, 2017. Paperback. Zustand: New. Language: English . This book usually ship within 10-15 business days and we will endeavor to dispatch orders quicker than this where possible. Brand New Book. Excerpt from A Report on the Limestones and Marls of the Coastal Plain of Georgia The region is a comparatively low plain sloping gently to the southeast. The highest elevations are along the Fall Line where they vary from 500 to 700 feet above sea level. A Slope of 3 or 4 feet per mile is general from this line to the Atlantic Coast. Although, when compared with the topography of those areas north of the Fall Line, the surface relief is slight it is not without distinctive features. The most notable topographic feature is that belt along the Fall Line known as the Fall Line Hills. This belt extends entirely across the State with a width varying from 30 to 40 miles, with the Fall Line the northern boundary. This area has a maximum relief of about 350 feet, considering the larger streams as the base, which shows a much more mature topography than the portion of the plain to the south. Cretaceous sands and clays, the principal materials underly ing the area, are easily eroded and have caused deep gullies and washes throughout the belt. To the north the Fall Line Hills merge into the Crystalline area and to the south into the Dougherty Plain, another distinctive topographic feature of the Coastal Plain. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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. Bestandsnummer des Verkäufers LIE9781528203869

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Verlag: Atlanta: The Blosser Company, 1916. (1916)
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Buchbeschreibung Atlanta: The Blosser Company, 1916., 1916. Hardcover. Zustand: Fine. 1st Edition. First printing. 4to. Frontispiece photograph. x, 300 pp. Illustrated, including a fold-out map. Original brown cloth binding stamped in gilt. Light wear at the extremities else tight, near fine; map fine. Bestandsnummer des Verkäufers 17625

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Buchbeschreibung Blosser Co, 1916. Hardcover. Zustand des Schutzumschlags: No Dust Jacket. No marks or writing, clean tight binding;; minor cracking of; edge wear to spine and corners;; Geological Survey of GA, Bulletin No. 21; detail study of the soils in GA with graphs, maps and photos; ; 300 pages Very Good- brn silk cloth over boards endsheets and slight aging. Bestandsnummer des Verkäufers 4973

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J E Brantly
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Buchbeschreibung Forgotten Books, 2017. Hardback. Zustand: New. Language: English . Brand New Book ***** Print on Demand *****. Excerpt from A Report on the Limestones and Marls of the Coastal Plain of Georgia The region is a comparatively low plain sloping gently to the southeast. The highest elevations are along the Fall Line where they vary from 500 to 700 feet above sea level. A Slope of 3 or 4 feet per mile is general from this line to the Atlantic Coast. Although, when compared with the topography of those areas north of the Fall Line, the surface relief is slight it is not without distinctive features. The most notable topographic feature is that belt along the Fall Line known as the Fall Line Hills. This belt extends entirely across the State with a width varying from 30 to 40 miles, with the Fall Line the northern boundary. This area has a maximum relief of about 350 feet, considering the larger streams as the base, which shows a much more mature topography than the portion of the plain to the south. Cretaceous sands and clays, the principal materials underly ing the area, are easily eroded and have caused deep gullies and washes throughout the belt. To the north the Fall Line Hills merge into the Crystalline area and to the south into the Dougherty Plain, another distinctive topographic feature of the Coastal Plain. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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. Bestandsnummer des Verkäufers APC9780266976479

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J E Brantly
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Buchbeschreibung Forgotten Books, 2017. Hardback. Zustand: New. Language: English . Brand New Book ***** Print on Demand *****.Excerpt from A Report on the Limestones and Marls of the Coastal Plain of Georgia The region is a comparatively low plain sloping gently to the southeast. The highest elevations are along the Fall Line where they vary from 500 to 700 feet above sea level. A Slope of 3 or 4 feet per mile is general from this line to the Atlantic Coast. Although, when compared with the topography of those areas north of the Fall Line, the surface relief is slight it is not without distinctive features. The most notable topographic feature is that belt along the Fall Line known as the Fall Line Hills. This belt extends entirely across the State with a width varying from 30 to 40 miles, with the Fall Line the northern boundary. This area has a maximum relief of about 350 feet, considering the larger streams as the base, which shows a much more mature topography than the portion of the plain to the south. Cretaceous sands and clays, the principal materials underly ing the area, are easily eroded and have caused deep gullies and washes throughout the belt. To the north the Fall Line Hills merge into the Crystalline area and to the south into the Dougherty Plain, another distinctive topographic feature of the Coastal Plain. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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. Bestandsnummer des Verkäufers APC9780266976479

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J E Brantly
Verlag: Forgotten Books (2017)
ISBN 10: 0266976476 ISBN 13: 9780266976479
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Buchbeschreibung Forgotten Books, 2017. Hardback. Zustand: New. Language: English . This book usually ship within 10-15 business days and we will endeavor to dispatch orders quicker than this where possible. Brand New Book. Excerpt from A Report on the Limestones and Marls of the Coastal Plain of Georgia The region is a comparatively low plain sloping gently to the southeast. The highest elevations are along the Fall Line where they vary from 500 to 700 feet above sea level. A Slope of 3 or 4 feet per mile is general from this line to the Atlantic Coast. Although, when compared with the topography of those areas north of the Fall Line, the surface relief is slight it is not without distinctive features. The most notable topographic feature is that belt along the Fall Line known as the Fall Line Hills. This belt extends entirely across the State with a width varying from 30 to 40 miles, with the Fall Line the northern boundary. This area has a maximum relief of about 350 feet, considering the larger streams as the base, which shows a much more mature topography than the portion of the plain to the south. Cretaceous sands and clays, the principal materials underly ing the area, are easily eroded and have caused deep gullies and washes throughout the belt. To the north the Fall Line Hills merge into the Crystalline area and to the south into the Dougherty Plain, another distinctive topographic feature of the Coastal Plain. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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. Bestandsnummer des Verkäufers LIE9780266976479

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