The Geology of Rutland and the Parts of Lincoln, Leicester, Northhampton, Huntingdon, and Cambridge, Included in Sheet 64 of the One-inch Map of the Geological Survey: With an Introductory Essay on the Classification and Correlation of the Jurassic Rocks of the Midland District of EnglandH.M. Stationery Office, 1875 - 320 pagina's |
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Pagina xi
... Minerals . Two groups of beds in the area . Jurassic and Post - Tertiary . Difference of age . Unconformity of two series . Table of strata THE LIAS . Extent . Subdivisions . CHAPTER II . The Lower Lias . Classification of its beds ...
... Minerals . Two groups of beds in the area . Jurassic and Post - Tertiary . Difference of age . Unconformity of two series . Table of strata THE LIAS . Extent . Subdivisions . CHAPTER II . The Lower Lias . Classification of its beds ...
Pagina xii
... Mineral springs . Mineral Soils . Conclusion 260 APPENDIX I. TABLES of FOSSILS from the various Jurassic formations of the Midland district APPENDIX II . LIST of WORKS containing notices of the Geology of the district Chrono- logically ...
... Mineral springs . Mineral Soils . Conclusion 260 APPENDIX I. TABLES of FOSSILS from the various Jurassic formations of the Midland district APPENDIX II . LIST of WORKS containing notices of the Geology of the district Chrono- logically ...
Pagina xiii
... MINERAL CHARACTERS OF SEVERAL MEMBERS OF THE LOWER OOLITES IN THE MIDLAND DISTRICTS OF ENGLAND . In these vertical sections the maximum thickness of each formation in the particular area is represented . For the Bath district I have ...
... MINERAL CHARACTERS OF SEVERAL MEMBERS OF THE LOWER OOLITES IN THE MIDLAND DISTRICTS OF ENGLAND . In these vertical sections the maximum thickness of each formation in the particular area is represented . For the Bath district I have ...
Pagina 5
... mineral character , of very different age * -at once made clear the true order of sequence of the Great Oolite strata of the Southern Cotteswolds , concerning which such conflicting opinions had been before maintained . The separation ...
... mineral character , of very different age * -at once made clear the true order of sequence of the Great Oolite strata of the Southern Cotteswolds , concerning which such conflicting opinions had been before maintained . The separation ...
Pagina 6
... mineral character the English beds to which the names were originally applied . The fallacy of such nomenclature and its mischievous results have been pointed out by many authors , and by none with more force of argument and justice of ...
... mineral character the English beds to which the names were originally applied . The fallacy of such nomenclature and its mischievous results have been pointed out by many authors , and by none with more force of argument and justice of ...
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The Geology of Rutland and the Parts of Lincoln, Leicester, Northhampton ... John Wesley Judd Volledige weergave - 1875 |
The Geology of Rutland and the Parts of Lincoln, Leicester, Northhampton ... John Wesley Judd Volledige weergave - 1875 |
The Geology of Rutland and the Parts of Lincoln, Leicester, Northampton ... John Wesley Judd Volledige weergave - 1875 |
Veelvoorkomende woorden en zinsdelen
abundant Ammonites argillaceous Avicula bands Belemnites Boulder Clay brickyard calcareous carbonate Cardium character Collyweston Collyweston Slate colour compact containing Cornbrash Cotteswold d'Orb denudation deposits escarpment exhibit exposed exposures fault feet ferruginous beds formation fossils freestone Geddington Geol Geological Goldf gravels hard Helpstone Hill Inferior Oolite inliers iron ironstone Jurassic Ketton laminated light-blue Lima lime Lincolnshire Limestone Lincolnshire Oolite Limestone Lower Estuarine Series Lower Lias Lower Oolites Lycett Marlstone Marlstone Rock-bed marly masses Middle Lias Midland district Modiola nodules North Northampton Sand northwards occur Oolite Limestone Oolite series Ostrea outcrop outliers Oxford Clay Pecten Phil Pholadomya portion quarries Railway Rhynchonella rock sandy clay Schloth seen Sheet 64 shells species specimens Stamford stone strata surface Terebratula thickness thin traced Trigonia Upper Estuarine Series Upper Lias Clay usually valley village Welland Yorkshire Zone of Ammonites دو وو
Populaire passages
Pagina 295 - The Natural, Experimental, and Medicinal History of the Mineral Waters of Derbyshire, Lincolnshire, and Yorkshire...
Pagina 6 - Christmas, or to our hearts; or to both. In order to be convinced of this it is only necessary to compare the present with the past. In the old days of not so long ago the festival began to excite us in November. For weeks the house rustled with charming and thrilling secrets, and with the furtive noises of paper parcels being wrapped and unwrapped; the house was a whispering gallery. The tension of expectancy...
Pagina 136 - England, and at a period separated by a long interval of time from that of the last deposit in the area, the Upper Lias Clay, that a number of considerable rivers, flowing through the Palaeozoic district lying to the north-west, formed a great delta. Within the area of this delta the usual alternations of marine, brackish-water, and terrestrial conditions occurred, and more or less irregular accumulations of sand or mud, in strata of small horizontal extent, took place. Subsequently, and probably...
Pagina 237 - Clay was formerly largely dug and burnt as a substitute for gravel, a use to which the clays of this formation are frequently applied. At Ramsey Heights there are several brickyards...
Pagina 136 - We find in what is now the midland district of England, and at a period separated by a long interval of time from that of the last deposit in the area, the Upper Lias Clay, that a number of considerable rivers, flowing through the Palaeozoic district lying to the north-west, formed a great delta. Within the area of this delta the usual alternations of marine, brackish water, and terrestrial conditions occurred, and more or less irregular accumulations of sand or mud in strata of small horizontal...
Pagina 143 - Sowerbyi), local depression took place within an area having a diameter of something like 90 miles, the amount of depression being greatest within its centre. As a consequence of this local depression there was slowly accumulated, by the growth of coral reefs, and the action of marine currents sweeping small shells and their fragments along the sea-bottom, a mass of calcareous strata, presenting many variations in its local characters, and constituting...
Pagina 30 - ... few inches in thickness. It has consequently been found impracticable in this district to draw a line of boundary between the representatives of the Great and Inferior Oolite. Thus it has arisen that under the term " Northampton Sand " are included, in North Oxfordshire and South Northamptonshire, the whole mass of variable sandy strata, (passing at some points into imperfect ironstones, and at others into impure limestones,) which intervene between the Upper Lias Clay and the marly limestones...
Pagina 295 - An essay Towards a Natural, Experimental, and Medicinal History of the Principle Mineral Waters of ...... Northamptonshire, Leicestershire, and Nottinghamshire, Particularly those of Nevile Holt &e. 4to. Sheffield. 6. ______ Natural, Experimental, and Medicinal History of the Mineral Waters of England.
Pagina 180 - Ancaster, such as Newark and Grantham churches and other edifices in various parts of Lincolnshire, have scarcely yielded to the effects of atmospheric influences.
Pagina 183 - The slates are cleaved at any time after they are frosted. Three kinds of tools are used by the Collyweston slaters. The " cliving hammer," a heavy hammer with broad chisel-edge for splitting up the frosted blocks. The "batting hammer" or "dressinghammer," a lighter tool for trimming the surfaces of the slates and chipping them to the required form and size. The " bill and helve," the former consisting of an old file sharpened and inserted into the latter in a very primitive manner.