| CHAP. | PAGE | |
| Table of clay rocks | [viii] | |
| I | Introduction. The chemical and physical properties of clays | [1] |
| II | Clay and associated rocks | [48] |
| III | The origins of clays | [70] |
| IV | The modes of accumulation of clays | [84] |
| V | Some clays of commercial importance | [103] |
| VI | Clay-substance: theoretical and actual | [135] |
| Bibliography | [168] | |
| Index | [170] |
LIST OF ILLUSTRATIONS
| FIG. | ||
| 1 | Quartz crystals | [9] |
| 2 | Pyrite | [14] |
| 3 | Marcasite | [14] |
| 4 | Illustrating the structure of a 'clay crumb' | [24] |
| 5 | Chart showing rates of drying | [27] |
| 6 | Seger Cones indicating a temperature of 1250° C. | [34] |
| 7 | Ludwig's Chart | [36] |
| 8 | Coal Measures sequence in North Staffordshire | [55] |
| 9 | Lias clay being worked for the manufacture of hand-made sand-faced roofing tiles | [58] |
| 10 | Oxford clay near Peterborough | [60] |
| 11 | Cliffs of Boulder clay at Filey lying on Calcareous Crag | [66] |
| 12 | China clay pit belonging to the North Cornwall China Clay Co. | [72] |
| 13 | Orthoclase Felspar | [75] |
| 14 | Illustrating the successive deposition of different strata | [90] |
| 15 | Lacustrine clay at Skipsea | [92] |
| 16 | Clay at Nostel, showing Marine Band | [94] |
| 17 | Kaolinite and Mica | [105] |
| 18 | Mining best Potter's clay in Devonshire | [111] |
THE CHIEF CLAY ROCKS (arranged geologically)
| Tertiary | ![]() | Recent (alluvial clay, silt, brick earths, boulder clay) | ||
| Pliocene Miocene Oligocene Eocene | ![]() | (brick earths, ball clays, coarse pottery clays) | ||
| Secondary | ![]() | Cretaceous (cement clays, brick clays) | ||
| Oolitic (brick and tile clays) | ||||
| Triassic (brick, tile and terra-cotta clays) | ||||
| Primary | ![]() | Permian (brick, tile and flower-pot clays) | ||
| Carboniferous (brick clays, fireclays, ganister) | ||||
| Devonian Silurian Ordovician Cambrian Pre-Cambrian | ![]() | (clay schists, slates and clay shales) | ||
| Igneous Rocks occur on several horizons (china clays and kaolins) | ||||
(In the above Table only the clay-bearing strata are mentioned. The formations named consist chiefly of other rocks in which the clays form strata of variable thickness.)


