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Marine Permian of England
This book is concerned almost wholly with a diverse suite of carbonate rocks that were formed near the margins of shallow tropical seas during the last 5-7 million years of the Permian period (300-251 Ma). These unique rocks, collectively known as the Magnesian Limestone, have been studied for more than 160 years and the names of some of the early workers - Geinitz, Murchison, Phillips, Sedgwick, Sorby - would grace any geological hall of fame. Despite this formidable assault, and the efforts of a host of later workers, the Magnesian Limestone still retains many of its secrets. Permian marine rocks crop out on both sides of the Pennines, but those of the Zechstein Sea to the east are by far the thicker and more varied, and in these lie all but one of the sites selected for special protection. Detailed accounts of the rocks in 26 such sites form about half of this book and the normal and special features of these sites are compared, contrasted and placed in their mutual context in the remainder of the book. The sites were selected according to a range of criteria, including uniqueness, representativeness, historical importance and suitability for teaching purposes and research; most are inland quarries but a few are in the unrivalled coastal cliffs of classical County Durham where the main difficulty lies in deciding what not to select.
1117013327
Marine Permian of England
This book is concerned almost wholly with a diverse suite of carbonate rocks that were formed near the margins of shallow tropical seas during the last 5-7 million years of the Permian period (300-251 Ma). These unique rocks, collectively known as the Magnesian Limestone, have been studied for more than 160 years and the names of some of the early workers - Geinitz, Murchison, Phillips, Sedgwick, Sorby - would grace any geological hall of fame. Despite this formidable assault, and the efforts of a host of later workers, the Magnesian Limestone still retains many of its secrets. Permian marine rocks crop out on both sides of the Pennines, but those of the Zechstein Sea to the east are by far the thicker and more varied, and in these lie all but one of the sites selected for special protection. Detailed accounts of the rocks in 26 such sites form about half of this book and the normal and special features of these sites are compared, contrasted and placed in their mutual context in the remainder of the book. The sites were selected according to a range of criteria, including uniqueness, representativeness, historical importance and suitability for teaching purposes and research; most are inland quarries but a few are in the unrivalled coastal cliffs of classical County Durham where the main difficulty lies in deciding what not to select.
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Marine Permian of England

Marine Permian of England

by D.B. Smith
Marine Permian of England

Marine Permian of England

by D.B. Smith

Overview

This book is concerned almost wholly with a diverse suite of carbonate rocks that were formed near the margins of shallow tropical seas during the last 5-7 million years of the Permian period (300-251 Ma). These unique rocks, collectively known as the Magnesian Limestone, have been studied for more than 160 years and the names of some of the early workers - Geinitz, Murchison, Phillips, Sedgwick, Sorby - would grace any geological hall of fame. Despite this formidable assault, and the efforts of a host of later workers, the Magnesian Limestone still retains many of its secrets. Permian marine rocks crop out on both sides of the Pennines, but those of the Zechstein Sea to the east are by far the thicker and more varied, and in these lie all but one of the sites selected for special protection. Detailed accounts of the rocks in 26 such sites form about half of this book and the normal and special features of these sites are compared, contrasted and placed in their mutual context in the remainder of the book. The sites were selected according to a range of criteria, including uniqueness, representativeness, historical importance and suitability for teaching purposes and research; most are inland quarries but a few are in the unrivalled coastal cliffs of classical County Durham where the main difficulty lies in deciding what not to select.

Product Details

ISBN-13: 9789401045278
Publisher: Springer Netherlands
Publication date: 04/26/2013
Series: Emotions, Personality, and Psychotherapy
Edition description: 1995
Pages: 205
Product dimensions: 8.27(w) x 11.69(h) x 0.02(d)

Table of Contents

1 The Permian marine rocks of England.- Geological setting.- 2 North-west England.- Barrowmouth Beach Section, Saltom Bay.- 3 North-east England (Durham Province).- Trow Point (South Shields) to Whitburn Bay.- Fulwell Hills Quarries (mainly Southwick Quarry).- Hylton Castle Cutting.- Claxheugh Rock, Claxheugh (Ford) Cutting and Ford Quarry.- Dawson’s Plantation Quarry, Penshaw.- Humbledon Hill Quarry.- Tunstall Hills, Sunderland; Maiden Paps and the Tunstall Hills (Rock Cottage Exposure).- Tunstall Hills (south-east end) and Ryhope Cutting.- Gilleylaw Plantation Quarry.- Seaham.- Stony Cut, Cold Hesledon.- High Moorsley Quarry.- Hawthorn Quarry.- Horden Quarry.- Blackhalls Rocks.- Trimdon Grange Quarry.- Raisby Quarries.- 4 North-east England (Yorkshire Province).- River Ure Cliff, Ripon Parks.- Quarry Moor.- Newsome Bridge Quarry.- Micklefield Quarry.- South Elmsall Quarry.- Bilham Quarry.- Cadeby Quarry.- Ashfield Brick-clay Pit, Conisbrough.- New Edlington Brick-clay Pit.- Wood Lee Common, Maltby.- References.
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