| PAGE | |
| INTRODUCTION | [5] |
| THE SECONDARY ISLAND | [7] |
| CHALK FORMATION | [9] |
| THE MOSASAURUS | [10] |
| THE PTERODACTYLE | [11] |
| WEALDEN FORMATION | [14] |
| THE IGUANODON | [14] |
| THE HYLÆOSAURUS | [17] |
| OOLITE FORMATION | [19] |
| THE MEGALOSAURUS | [19] |
| PTERODACTYLES OF THE OOLITE | [22] |
| TELEOSAURUS | [22] |
| LIAS FORMATION | [25] |
| ENALIOSAURIA | [25] |
| THE ICHTHYOSAURUS | [25] |
| ICHTHYOSAURUS PLATYODON | [29] |
| ICHTHYOSAURUS TENUIROSTRIS | [30] |
| ICHTHYOSAURUS COMMUNIS | [30] |
| PLESIOSAURUS | [31] |
| PLESIOSAURUS MACROCEPHALUS | [31] |
| PLESIOSAURUS DOLICHODEIRUS | [32] |
| PLESIOSAURUS HAWKINSII | [33] |
| NEW RED SANDSTONE | [35] |
| BATRACHIA | [35] |
| LABYRINTHODON SALAMANDROIDES | [36] |
| LABYRINTHODON PACHYGNATHUS | [38] |
| DICYNODON | [38] |
GEOLOGY AND INHABITANTS OF THE ANCIENT WORLD.
INTRODUCTION.
Before entering upon a description of the restorations of the Extinct Animals, placed on the Geological Islands in the great Lake, a brief account may be premised of the principles and procedures adopted in carrying out this attempt to present a view of part of the annual creation of former periods in the earth’s history.
Those extinct animals were first selected of which the entire, or nearly entire, skeleton had been exhumed in a fossil state. To accurate drawings of these skeletons an outline of the form of the entire animal was added, according to the proportions and relations of the skin and adjacent soft parts to the superficial parts of the skeleton, as yielded by those parts in the nearest allied living animals. From such an outline of the exterior, Mr. Waterhouse Hawkins prepared at once a miniature model form in clay.
This model was rigorously tested in regard to all its proportions with those exhibited by the bones and joints of the skeleton of the fossil animal, and the required alterations and modifications were successively made, after repeated examinations and comparisons, until the result proved satisfactory.